DISTRICT SURVEY REPORT FOR DISTRICT FOR

A. SAND MINING OR RIVER BED MINING B. MINERALS OTHER THAN SAND MINING OR RIVER BED MINING

(Revision 01)

Prepared under

A] Appendix –X of MoEFCC, GoI notification S.O. 141(E) dated 15.1.2016 B] Sustainable Sand Mining Guidelines C] MoEFCC, GoI notification S.O. 3611(E) dated 25.07.2018 Declaration

In compliance to the notifications, guidelines issued by Ministry of Environment, Forest & Climate Change, Government of , New Delhi, District Survey Report (Rev. 01) for is prepared and published.

Place : Nandurbar

Date : District Collector, Nandurbar

Index

Sr. Description Page No. No. 1 District Survey Report for Sand Mining Or River Bed Mining 1-54 1.0 Introduction 02 Brief Introduction of Nandurbar district 03 Salient Features of Nandurbar District 07 2.0 Overview of Mining Activity in the district 08 3.0 List of the Mining Leases in the district with Location, area 10 and period of validity Location of Sand Ghats along the Rivers in the district 13 4.0 Detail of Royalty/Revenue received in last three years from 14 Sand Scooping activity 5.0 Details of Production of Sand or Bajri or minor mineral in last 14 three Years 6.0 Process of Deposition of Sediments in the rivers of the 14 District Stream Flow Guage Map for rivers in Nandurbar district 18 Siltation Map for rivers in Nandurbar district 19 7.0 General Profile of the district 20 8.0 Land Utilization Pattern in the District : Forest, Agriculture, 23 Horticulture, Mining etc. 9.0 Physiography of the District 26 River Inventory of the district 28 Basin Map for Nandurbar r district is drawn as 29 Confluence Points for the rivers in the district 30 Rivers marked on toposheets 31 HFL Maps for rivers 32 L & Cross sections for rivers 37 10.0 Rain Fall Data for Nandurbar district 39 11.00 Geology and Mineral Wealth 40 Geological Map For Nandurbar District 42 District wise details of river or stream and other sand sources 43 District wise availability of sand and gravel or aggregate resources 44 Drainage System with description of main rivers 44 Salient Features of important rivers and streams 45 List of Sand Spots 45 Annual Deposition 48 2 District Survey Report for Minerals Other Than Sand Mining Or 55-105 River Bed Mining 1.0 Introduction 56 Brief Introduction of Nandurbar district 57 Salient Features of Nandurbar District 61 2.0 Overview of Mining Activity in the district 62 3.0 General Profile of the district 64 Location of leases on Map of District 66 4.0 Geology of the District 67 Minerals Available in the District 68 Geological Map of Nandurbar District 69 5.0 Drainage and irrigation Pattern 70 6.0 Land Utilization Pattern in the District : Forest, Agriculture, 71 Horticulture, Mining etc. Mining Area 73 7.0 Surface Water And Ground Water Scenario 74 8.0 Rainfall of the district and Climatic Conditions 77

9.0 Details of the mining leases in the district as per the following format 79 10.0 Details of Royalty or Revenue received in last three years 85 11.0 Details of Production of Minor Mineral in last three years 85 : (Approx. Quantity) 12.0 Mineral Map of District 85 13.0 List of Letter of Intent (LOI)Holders in the district along with its 87 validity as per following format 14.0 Total Mineral Reserves Available in the District 87 15.0 Quality / Grade of Mineral available in the District 87 16.0 Use of Mineral 87 17.0 Demand and Supply of the Mineral in last three years 87 18.0 Mining Leases marked on District Map 90 19.0 Details of the area of where there is a cluster of mining leases 91 viz. no. of mining leases. Location 20.0 Details of Eco sensitive area 92 21.0 Impact on the Environment (Air, Water, Noise Soil, Flora & Fauna, 94 Land Use, agriculture, forest etc.) due to mining activity 22.0 Remedial measures to mitigate the impact of mining on 95 Environment 23. Reclamation of Mined Out Area (best practice already implemented 97 in the district, requirement as per rules and regulations , proposed reclamation plan) 24. Risk Assessment 97 25. Disaster Management Plan 102 26. Plantation and Green Belt Development 104 27. Any other information 105 3 District Survey Report for Other Minerals 106- 107 1.0 Details of leases for other minerals like Coal, Limestone and dolomite 107 etc 4 Annexure 108 Annexure -1 Procedure to scrutinize Minor Mineral proposals 108 Annexure -2 Procedure to monitor compliances of Minor Mineral Leases 109 Annexure -3 Demand and Supply for Nandurbar District 110 Annexure -4 MoEFCC, GoI notification S.O. 3611(E) dated 25.07.2018 112 Annexure -5 L Sections and Cross Sections for rivers flowing through 113 Nandurbar district Annexure -6 Corporate Environmental Responsibility 116 Annexure -7 List & Sections for Sand Ghats 2019-20 (Amendment 118 Proposed for F.Y. 2019-20) Annexure -8 COMPLIANCE TO ENFORCEMENT AND MONITORING 122 GUIDELINES FOR SAND MINING 2020 (PUBLICATION OF ANNEXURES )

Amendments to DSR

Sr. Amendment Amendment Details Amendment Page No. Authorized by No. Sheet No. Date 1 01 Amendment in DSR Rev 01 dated---- Complete DSR District ---- Collector, Nandurbar/ D.M.O. Nandurbar

DISTRICT SURVEY REPORT FOR NANDURBAR DISTRICT

PART –A

FOR SAND MINING OR RIVER BED MINING

Prepared under

A] Appendix –X of MoEFCC, GoI notification S.O. 141(E) dated 15.1.2016 B] Sustainable Sand Mining Guidelines C] MoEFCC, GoI notification S.O. 3611(E) dated 25.07.2018

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1.0 Introduction :

Hon’ble Supreme Court of India vide its judgement dated February 27,2012 and further relief amendment dated April 16,2012 directed all state, union territories and ministry of Environment and Forest, Govt. of India, New Delhi to screen mining of minor minerals leases within the purview of EIA notification 2006 and made requirement of environmental clearance to minor minerals less than 5 ha compulsory.

Ministry of Environment & Forest , GoI vide its office Memorandum L-11011/47/2011.IA.II(M) dated 18.05.2012 directed mass to comply Ho’ble Supreme Court decision.

Further streamlining of environmental clearance procedures, MOEFCC, GoI amended EIA notification 2006 vide S.O. 141(E) dated 15.01.2016 where procedure for preparation of District Survey Report (DSR) for minor minerals has been prescribed.

Further the procedure for preparation of DSR and format is amended vide MOEFCC notification S.O. 3611(E) dated 25.07.2018. The subjected DSR is defined at “ Appendix -X (See Paragraph 7(iii)(a)” of the notification S.O.141(E)dated 15.01.2016 and S.O. 3611(E) dated 25.07.2018

Accordingly this document is prepared by DEIAA,Nandurbar, State.

Nnadurbar district has constituted District Environmental Impact Assessment Authority vide letter No. Aadesh/kramank/2016/gaukhani/kavi-182 Dated- 22/06/2016 and comprised as

Sr. No. Name of the Member/Expert Designation Role 1 District Collector, Nandurbar District Collector, Nandurbar Chairman 2 D.C.F.Nandurbar D.C.F.Nandurbar Member 3 Prof. G.S.Khandagle Expert Member (Non Govt. Member Official) 4 S.D.O.Nandurbar S.D.O.Nandurbar Member Secreatary

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Latur district has constituted District Expert Appraisal Committee Authority vide letter Aadesh/kramank/2016/gaukhani/kavi-182 Dated- 22/06/2016 and comprised as

Sr. No. Name of the Member/Expert Designation Role 1 Executive Engineer Irrigation Executive Engineer Irrigation Chairman Department, Nandurbar Department, Nandurbar 2 D.C.F.Nandurbar D.C.F.Nandurbar Member 3 Senior Geologist GSDA, Senior Geologist GSDA, Member Nandurbar Nandurbar 4 District Civil Surgeon, Nandurbar District Civil Surgeon, Nandurbar Member 5 Executive Engineer Rural Water Executive Engineer Rural Water Member Supply Divison, Z.P. Nandurbar Supply Divison, Z.P. Nandurbar 6 Sub Regional Officer, State Sub Regional Officer, State Member Pollution Control Board, Pollution Control Board, Dhule 7 Dr.V.R.Borane Jijamata Collage Nanaudrbar (Non Member Govt. Official) 8 Dr.B.B.Mangale JTP Collage Nandurbar (Non Govt. Member Official) 9 Prof. Smt. S.D.Patil Jijamata Collage Nanaudrbar (Non Member Govt. Official) 10 Executive Engineer, P.W.D., Executive Engineer, P.W.D., Member Nanaudrbar Nanaudrbar 11 District Mining District Mining Officer,Nandurbar Member Officer,Nandurbar Secreatary

Brief Introduction of Nandurbar district :

Nandurbar District is situated in the Northern part of the state of Maharashtra. Nandurbar district belongs to Division of Maharashtra State situated between 73.31 and 74.32 East longitude and 21.03 and 22.00 North latitude.The natural boundaries of satpuda hills along with form its boundaries.It is spread over a geographical area of 5,955 Sq. Kms. It is 1.62% of the total Geographical area of Maharashtra. District has 06 tehsils with 4 Municipal council,01 Nagar Panchayat and 595 Grampanchayats. The two major west flowing rivers Tapi and Narmada and its tributaries criss cross through the district.

Nandurbar is an administrative district in the northwest corner ( Region) of Maharashtra state in India . On 1 July 1998 Dhule was bifurcated as two separate districts now known as Dhule and Nandurbar. The district headquarters are located at Nandurbar city. The district occupies an area of 5955 km² and has a population of 16,48,295 of which 15.45% were urban. Nandurbar district is bounded to the south and south-east by , to the west

3 and north is the state of , to the north and north-east is the state of . The northern boundary of the district is defined by the great Narmada river.

Before 1 July 1998 Nandurbar was part of the larger Dhule district. Nandurbar, Dhule and districts formed what was known as the Khandesh district. Dhule was known as the west Khandesh whereas Jalgaon was known as the east Khandesh. So, much of history applicable to Khandesh and Dhule, is applicable to Nandurbar. Nandurbar is also known as Nandanagri as the king Named Nandaraja was the ruler of this territory. The ancient name of this region was Rasika. It is bounded on the east by Berar (ancient ), on the north by the Nemad district (ancient Anupa) and on the south by the (ancient Mulaka) and Bhir (ancient Asmaka) districts. Later the country came to be called as Seunadesa after king, Seunchandra of the Early Yadava dynasty, who ruled over it. Subsequently, its name was changed to Khandesh to suit the title Khan given to the Faruqi kings by Ahmad I of Gujarat.

The ancient name of this region was ‘Rasika’. Varahmihira places Rasika coupled Vidarbha and Mahisaka, later under the Yadavas,it was called as ‘Seunadesa’ after the Yadav king Seunachandra who ruled over it. With the advent of Muslims, the name was changed to Khandesh to suit the title ‘Khan’ given to the Faruki kings.The entire area of Khandesh included two districts viz. Dhule and Jalgaon.However in 1906 for administrative purpose the headquater created at Dhule. The Khandesh was divided into two districts known as West Khandesh and East Khandesh. In 1961 the name of the district changes from west Khandesh to Dhulia and later on Dhulia District.At present the Nandurbar district comprises six tehsils i.e. , Akrani, Taloda, Shahada, and Nandurbar. There are 943 villages in the district as percensus 2011. The district comprises 6 talukas. These talukas are Akkalkuwa, Akrani Mahal (also called ), Taloda, Shahada, Nandurbar and Navapur.

Drainage

Two major rivers Tapi & Narmada drain the district. The drainage network of Tapi includes number of tributaries like Nagan, Shivan, Gomai, Dehali etc while tributaries like Katri, Devnadi, Udai etc form the drainage network of Narmada river. Total drainage network of the district contains about 29 watersheds out of which 21 are in Tapi river basin & 08 are in Narmada basin

The catchment area of the Tapi river is principally situated in the northern and eastern district of Maharashtra and Nandurbar district. Except the northern part drained by Narmada River and its tributaries such as Kanni, Devnad / Devganga and Udai, the entire distirct is mainly drained by Tapi River and its tributaries such as Nagan, Shivan, Gomai and Dehli. The Tapi River has a total course of 86,905 sq km. in the district. Pebbly conglomerates and sand occur in the dry bed of the Tapi River either as braided channels, point bars, levees, etc. Annually, the sand is replenished in by the river the river channel and is auctioned as natural resource.

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Tributary of Tapi River in Nandurbar District:

Gomai, Shivan, Rangawali, Sarpini, Nagan, Sukhi and Susri etc.are the tributaries of Tapi River Gomai River is tributary of Tapi River. It originates in Satpura Mountain range and merge in Tapi river around 2Km east of . Gomai River itself has many small tributary rivers like Susri river (passing by Sultanpur), Tipiria river (passing by Mandane), Umri river, Sukhi river.

Climate The climate of the district is characterized by a hot summer and general dryness throughout the year except during the south-west monsoon season, i.e., June to September. The daily mean minimum temperature is 15.8°C and mean maximum temperature is 40.7°C. The average annual rainfall over the district is about 801 mm. It is the minimum in the eastern part of the district and increases westwards towards Nawapur and Akkalkuwa. The study of negative departures of the annual rainfall over normal reveals that north western and south western parts of the district experienced moderate and severe drought conditions for more than 20% of years. Hence this parts occupying almost entire Akkalkuwa taluka and parts of Akrani, Nawapur and Nandurbar talukas can be categorized as drought area. The average annual rainfall in the district varied from 645 mm (Shahada) to 1192 mm (Nawapur). Winds, in general, are light to moderate. But they are strengthened in force in summer and monsoon periods. Winds are mainly south-westerly to westerly during the south-west monsoon season. In the post- monsoon, they are light and variable in directions in the mornings and north-easterly to easterly in the afternoon. In winter and summer seasons they are generally from south-west directions to north-west.

Natural Economic Resources Deccan Traps cover a major part of the District. Trap rocks are very hard and compact and are dark grey in colour. Trap rocks being dense, hard and compact are extensively used as building stones, road metal, railway ballast and as an aggregate in cement concrete. Erosive agents and weathering together have formed good fertile soils near the river beds.

Forestry This includes all land classified as forest under any legal enactment dealing with forest or administered as forest, whether state owned or private and whether wooded or simply maintained as forest land. The total area under the forest is 104 Thousand hectares which is 20.78% of the total geographical area of the district. The forest in the district cover an area of 3465.79 sq. km., mostly in Dhadgaon, Akkalkuwa, Taloda and Navapur talukas. The maximum forest area is in Akkalkuwa taluka i.e. 42.34%.

Minerals and mining Minerals of great economic importance are not found in Nandurbar district. The major part of the district is covered by basaltic flows commonly known as Deccan Traps and dykes of Upper

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Cretaceous-Lower Eocene age. Tapi Alluvial deposits are observed in Tapi River valley occupying parts of Taloda, Shahada and Nandurbar talukas. Along the north-western corner of the district, pre-trappean Bagh Beds of Middle to Upper Cretaceous age are exposed over a small area along the valley of the Devganga River. Trap rocks are hard , dense and durable and are suitable for building /construction purposes. Economically important mneral required for ndustrialization not found in the district. Hence district has basalt mining for infrastructural requirements with natural river sand up to some extend. At some places some patches of agate are found but with inferior quality.

Soil and Cropping pattern On the basis of depth, texture and colour, the soil of the district are grouped into three categories viz., light soil, medium soil and deep black soils. Along the banks of Tapi River and its tributaries soil type is black cotton soil. It is enriched by lime, iron, magnesia and alkalies. In the northern part of the district the soil varies from dark brown to yellowish brown of lighter type on the hill slopes, with clayey deep soil of the Tapi River valley to its south. Medium soils are mostly located in the southern and central zones of the district below the Tapi River valley in Nawapur. The soil varies from dark brown to dark reddish brown in colour. Owing to the peculiarity of the soil, both Kharif and Rabi crops are cultivated in this zone.

Agriculture Most of the people of this District are engaged in agricultural activities. According to Census 2011, percentage of the total workers engaged as cultivators is 24.29% and as agricultural labourers is 44.26% (percent) in the District. Together they constitute 68.55 %(percent) of the total workers of the District. District is producing Kh. Jowar, Paddy,Bajri,Maiz,Toor, Mung,Soyabean,Groundnut seed and wheat as rabbi crop as most common agricultural crops. The District is divided in three subdivisions and six tahsils.

There are five Subdivisions and six talukas listed as

Name of Sub division Taluka 1. Nandurbar Nandurbar,Navapur 2. Taloda Taloda, Akkalkuva 3. Shahada Shahada, Akrani

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Salient Features of Nandurbar District :

Details of the Area District & State Nandurbar & Maharashtra Subdivision & Taluka 03 & 6 Nos. Villages 943 villages Area of district 5955 Sq. Km Minerals in district Basalt, River Sand Category ‘B’ LATITUDE LONGITUDE [E] Geographical Co-ordinates [N]

N 210 00’- N 22003” E 73°31’-E 74° 32’

Accessibility Road Connectivity District is well connected with MSH1,7, SH13,9,5,6,7,4,2 Railway Station at Nandurbar (Connecting - Rail Connectivity Ahmedabad,Chennai-Ahmedabad) Airport Nashik (Nearest Airport) General Climatic Conditions Wind Pattern during study period North to South Summer : 40 – 42 0C Maximum Temperature Winter : 10 – 12 0C Summer : 40 – 42 0C Minimum Temperature Winter : 10 – 12 0C Average Annual Rainfall (mm) 645 mm (Shahada) to 1192 mm (Nawapur) Details of the Project Elevation 300m-600m above sea level Historical / Important Places No archeological /historical place is notified by National Archaeological/Historical/Ancient Archeological Department Government of India within Monuments within district district. However there is one monument which is listed below is

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protected by State Governemt of Maharashtra. Mohida Tarf (Haveli) Names of the national park, sanctuary No sactuaries, tiger reserves, biosphere,ESA/ESZ are notified in the district. There is a part of Western ghat which is Biosphere reserve, Tiger Reserve, reported by MoEFCC, GoI for no mining /industrial zone as Elephant reserve, Forest per HLWG. Western ghat is defined vide draft notification S.O. 5135 dated 3.10.2018 for the district for two villages (RF/PF/Unclassified) (Kareghat & Khekada,Navapur Taluka) where mining or industrial activity is prohibited

2.0 Overview of Mining Activity in the district :

Latur district is rich in minor minerals such as building stone and sand. Mining activity is one of the main revenue source for the district.

District has 24 stone quarry leases (3 with valid environmental clearance but under stage of lease order)till March 2020 covering area 49.3ha. (Source info. District Mining Office Nandurbar)

There are 31 locations of sand ghats over Tapi, Rangvali,Sarpani rivers where sand deposition are allowed from replenishment and other safety point of view in the district. (Source info. District Mining Office, Nandurbar).

Villages marked on the district geological map is as below :

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3.0 List of the Mining Leases in the district with Location, area and period of validity :

As per the sand mining and auction policy of Government of Maharashtra, Sand ghats are identified for deposition by respective tahsildars and recommended by Tahsil Level Technical Committee comprising G.S.D.A. and other uthorities authorities of the district for mineable depth considering impact of sand scooping on ground water availability and stream. Hon’ble District Collector is a chairman and District Mining Officer who is a Geologist is member secretary of district level technical committee approving sand ghats. District Mining Officer is a project proponent to complete further procedures for auction including pricing and approval of Divisional Commissioner.

Tahsildar at Headquarter is the holder of the sand ghats. After auction of sand ghats for period specified in the auction policy of Govt. of Maharashtra dated 03.09.2019, all rights to comply the terms and conditions for scooping of sand from sand ghats are transferred to Successful Bidder.

List of the Sand Ghats with location, area and period of validity is tabled below.

Sr. Taluka Name Rive Nearest Details of Sand Scooping Govt/ Appro Area No. of r/ Gut No Pvt x Sand in ha Sand Stre Qty in Ghat am L(m) W(m) Appro Brass ved Depth (m)

126,127,12 Amalt 1 8 200 80 2 Govt. 11307 1.6 he 129 Kopar 238,239,24 2 200 80 2 Govt. 11307 1.6 li 1 Osara 3 10,11,14 190 75 2 Govt. 14700 1.425 li Nandur Aaral 4 Tapi 180,181 130 65 2 Govt. 5972 0.845 bar e Boral 5 19,20,21 260 80 2 Govt. 14700 2.08 e Nashi 6 17,18 200 80 2 Govt. 11307 1.6 nda Sujalp 7 330 260 80 2 Govt. 14700 2.08 ur

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8 Korit 7 260 80 2 Govt. 14700 2.08

Saval 60,61 125 45 1.5 0.562 9 Govt. 2981 da 5 Saran 10 gkhed 33,34 240 60 2 Govt. 10177 1.44 a-1 Saran 11 gkhed 38,39 250 60 2 Govt. 10600 1.5 a-2 Khaut 12 1/1,1/2 325 60 2 Govt. 13780 1.95 hal Kurav 1/1,1/2,1/ 13 250 85 2 Govt. 15017 2.125 ad 3 Bamk 149 280 60 2 14 heda Govt. 11872 1.68 tasa Biladi 1.127 15 9 205 55 2 Govt. 7968 tasa 5 Nand 125/2, 85 16 arkhe 300 70 2 Govt. 14840 2.1 lagat da Tapi a Palas 17 4 200 60 2 Govt. 8400 1.2 wada 4.531 18 Shelty 10,19,20 855 53 2 Govt. 32024 5 Sasde 19 564 130 70 2 Govt. 6431 0.91 1 Sasde 563 140 70 2 20 Govt. 6926 0.98 2 303/1,303/ 2,296/1,29 6/2,296/3, 294/4,294/ Temb 4.152 21 1,294/2,29 755 55 2 Govt. 40017 ha 5 4/3,293,28 8,287/1,28 7/2,286,28 4

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Bamk 22 heda 5 100 50 2 Govt. 3533 0.5 T. T Deur 23 kamk 56/2 220 60 2 Govt. 9329 1.32 heda Khair ve 24 109 210 50 2 Govt. 7420 1.05 Bhad gao 25 Fes 357/1 200 50 2 Govt. 7067 1 Dond 26 awad 26 215 50 2 Govt. 7597 1.075 e Torkh Gavthan 27 205 50 2 Govt. 7243 1.025 eda Lagat Lamb 28 6,7 90 50 2 Govt. 3180 0.45 ola

Bokalj Rang 0.187 29 52,53 75 25 2 Govt. 662 har avali 5 Navapu Nava 0.151 30 r 2 66 23 2 Govt. 1073 goan Sara 8 Karan pani 31,35,36,4 31 400 15 1 Govt. 2120 0.6 gwel 5

List of sand ghats proposed for auction :

Name of Details of Sand Scooping River/ Road/ Approx Taluka Sand Nearest Gut No Approved Stream L(m) B(m) Govt/Pvt SandQty Ghat Depth(m) Kaothal Tapi 1/1,1/2 325 60 2 tasa Govt. Kurhawad Tapi Shahada 1/1,1/2,1/3 250 85 2 tasa Govt. Tembhe Tapi 303/1,303/2,296/1, 308 75 2 Bu. 296/2,296/3 Govt.

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Location of Sand Ghats along the Rivers in the district are marked as :

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4.0 Detail of Royalty/Revenue received in last four years from Sand Scooping activity:

Financial Year Revenue in Rs. F.Y. 2015-16 16120000 F.Y. 2016-17 44404357 F.Y. 2017-18 18677777 F.Y. 2018-19 12158788 F.Y. 2019-20 Nil

5.0 Details of Production of Sand or Bajri or minor mineral in last four Years

Financial Year Scooping of River Scooping of River Scooping of River Bed Sand in Brass Bed Sand in Cum. Bed Sand in Tonnes F.Y. 2015-16 45227 127992 358378 F.Y. 2016-17 27375 77471 216919 F.Y. 2017-18 9907 28036 78503 F.Y. 2018-19 6007 16999 47599 F.Y. 2019-20 00 00 00

6.0 Process of Deposition of Sediments in the rivers of the District :

Sand is replenishable. Due to sparse rainfall over the last few years the river flows to an average height but flows to its maximum height only during and just after monsoon season. Mining of Building Grade sand from the river bed will not have any impact on the ground water body in the area. During heavy rains the floodwaters overflow the bank and inundate the fields and dry regions. The floods have its own ways of depositing sand not only at the bank but also on the dry surface region. Added to the deposition of sand on the river basin by stratification through lateral deposition of sands on the land surface is by Differential Lateral Deposition (DLD). The later grade is coarse, medium and fine sand to mud and soil beyond. In this soil, agricultural operation goes on from the bank to the cultivated land surface. The yearly deposition of sand is by natural filling during flood season with slight variation depending upon the amount of river flow, the quantity of water flowing and the amount of sand load carried during the river flow. The deposition pattern will be monitored every year & measurements will be carried out as soon as the monsoon comes to an end.

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Deposition rate for the year 2019-20 is monitored, calculated and mapped with the help of technical consultant. Data for gauging of stream is mapped and enclosed below. Data for Siltation is mapped and enclosed .. Based on siltation rate and survey every year sand ghats are proposed for scooping of sand and auctioned as per the State Government Policy empowered under rule 15 of Mines and Minerals (Development and Regulation) Act 1957 and amendments thereof.

Sediment refers to the conglomerate of materials, organic and inorganic, that can be carried away by water, wind or ice. While the term is often used to indicate soil-based, mineral matter (e.g. clay, silt and sand), decomposing organic substances and inorganic biogenic material are also considered sediment . Most mineral sediment comes from erosion and weathering, while organic sediment is typically detritus and decomposing material such as algae.

Sediment particles come in different sizes and can be inorganic or organic in origin.

These particulates are typically small, with clay defined as particles less than 0.00195 mm in diameter, and coarse sand reaching up only to 1.5 mm in diameter. However, during a flood or other high flow event, even large rocks can be classified as sediment as they are carried downstream . Sediment is a naturally occurring element in many bodies of water, though it can be influenced by anthropogenic factors .

In an aquatic environment, sediment can either be suspended (floating in the water column) or bedded (settled on the bottom of a body of water)

In other words water flow tries to scour its surface whenever it flows in the channel. Silt or gravels enen larger boulders are detached from its bed or banks. The moving water sweeps these detached particles in downstream along its flow. Silting and scouring is not very uncommon and must be avoided by proper designs. It reduces supply level of water. The channel section gets reduced by silt and reduces discharging capacity. Sediments seriously threatens various projects due to silt carried out by rivers up to point of interceptions. Sediment is also threatening denudation of forests. Sediment is a major obstruction on the flow line . It shorten longevity of channel. It causes soil erosion. Therefore data base must be needed for policy making and planning. Sediments are calculated as sediment load. There are three types of sediments

Coarse Sediments Particle size above 0.2mm Water sample passing through 100/72 mesh sieve (BSS). Residue over sieve is washed, dried and weighed It gives coarse sediments in gm/lit

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Medium Sediments Particle size ranging 0.075mm-0.2mm After removal of coarse sediments residual water passed through 200mesh sieve (BSS), we get medium sements Fine Sediments Particle size less than 0.075mm Filtrate and washing residue allowed to settle for 12hrs. About 5-10 % alum solution is added to hasten coagulation of colloidal silt Using Whatman Paper no02 filter paper, residue is filtered, dried and weighed. We will get fine sediments in gm/lit Co relation between Siltation & Sediment Load

Siltation is deposition by fine particulate terrestrial clastic material, with a particle size dominated by silt or clay. It refers both to the increased concentration of suspended sediments, and to the increased accumulation (temporary or permanent) of fine sediments on bottoms where they are undesirable. Siltation is most often caused by soil erosion or sediment spill.

Sometimes siltation is called sediment pollution. The total Sediment load includes all particles moving as bedload, suspended load, and wash load

Bedload

Bedload is the portion of sediment transport that rolls, slides or bounces along the bottom of a waterway. This sediment is not truly suspended, as it sustains intermittent contact with the streambed, and the movement is neither uniform nor continuous . Bedload occurs when the force of the water flow is strong enough to overcome the weight and cohesion of the sediment While the particles are pushed along, they typically do not move as fast as the water around them, as the flow rate is not great enough to fully suspend them. Bedload transport can occur during low flows (smaller particles) or at high flows (for larger particles). Approximately 5-20% of total sediment transport is bedload . In situations where the flow rate is strong enough, some of the smaller bedload particles can be pushed up into the water column and become suspended.

Suspended Load

While there is often overlap, the suspended load and suspended sediment are not the same thing. Suspended sediment are any particles found in the water column, whether the water is flowing or not. The suspended load, on the other hand, is the amount of sediment carried downstream within the water column by the water flow. Suspended loads require moving water, as the water flow creates small upward currents (turbulence) that keep the particles above the bed . The size of the particles that can be carried as suspended load is dependent on the flow rate . Larger particles are more likely to fall through the upward currents to the bottom, unless the flow rate increases, increasing the turbulence at the streambed. In addition, suspended sediment will not necessarily remain suspended if the flow rate slows.

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Wash Load

The wash load is a subset of the suspended load. This load is comprised of the finest suspended sediment (typically less than 0.00195 mm in diameter). The wash load is differentiated from the suspended load because it will not settle to the bottom of a waterway during a low or no flow period . Instead, these particles remain in permanent suspension as they are small enough to bounce off water molecules and stay afloat. However, during flow periods, the wash load and suspended load are indistinguishable.

Turbidity in lakes and slow moving rivers is typically due the wash load. When the flow rate increases (increasing the suspended load and overall sediment transport), turbidity also increases. While turbidity cannot be used to estimate sediment transport, it can approximate suspended sediment concentrations at a specific location.

River Dynamics (Physical) Manjara, tarwaja, tiru, lendi Rivers are in the matured stage of development running in wide serpentine course. The river meanders with convex & concave shape. The river in its course impinges on convex side. The concave side abounds with sand grain. The mining operation is most profitable on the concave side.

There is yearly deposition of sand as the amount of sand excavated gets redeposit in the pits by natural filing during flood season with slight variation depending upon the amount of river flow, the quantity of water flowing and the amount of sand load carried during the river flow. The deposition pattern will be monitored every year & measurements will be carried out as soon as the monsoon comes to an end and fresh excavation will be carried.

17

Stream Flow Guage Map for rivers in Nandurbar district :

*cum/min

18

Siltation Map for rivers in Nandurbar district :

19

7. General Profile of the district :

Nandurbar District is situated in the Northern part of the state of Maharashtra. Nandurbar district belongs to of Maharashtra State situated between 73.31 and 74.32 East longitude and 21.03 and 22.00 North latitude.The natural boundaries of satpuda hills along with Narmada river form its boundaries.It is spread over a geographical area of 5,955 Sq. Kms. It is 1.62% of the total Geographical area of Maharashtra. District has 06 tehsils with 4 Municipal council,01 Nagar Panchayat and 595 Grampanchayats. The two major west flowing rivers Tapi and Narmada and its tributaries criss cross through the district.

Nandurbar is an administrative district in the northwest corner (Khandesh Region) of Maharashtra state in India . On 1 July 1998 Dhule was bifurcated as two separate districts now known as Dhule and Nandurbar. The district headquarters are located at Nandurbar city. The district occupies an area of 5955 km² and has a population of 16,48,295 of which 15.45% were urban. Nandurbar district is bounded to the south and south-east by Dhule district, to the west and north is the state of Gujarat, to the north and north-east is the state of Madhya Pradesh. The northern boundary of the district is defined by the great Narmada river.

Before 1 July 1998 Nandurbar was part of the larger Dhule district. Nandurbar, Dhule and Jalgaon districts formed what was known as the Khandesh district. Dhule was known as the west Khandesh whereas Jalgaon was known as the east Khandesh. So, much of history applicable to Khandesh and Dhule, is applicable to Nandurbar. Nandurbar is also known as Nandanagri as the king Named Nandaraja was the ruler of this territory. The ancient name of this region was Rasika. It is bounded on the east by Berar (ancient Vidarbha), on the north by the Nemad district (ancient Anupa) and on the south by the Aurangabad (ancient Mulaka) and Bhir (ancient Asmaka) districts. Later the country came to be called as Seunadesa after king, Seunchandra of the Early Yadava dynasty, who ruled over it. Subsequently, its name was changed to Khandesh to suit the title Khan given to the Faruqi kings by Ahmad I of Gujarat.

The ancient name of this region was ‘Rasika’. Varahmihira places Rasika coupled Vidarbha and Mahisaka, later under the Yadavas,it was called as ‘Seunadesa’ after the Yadav king Seunachandra who ruled over it. With the advent of Muslims, the name was changed to Khandesh to suit the title ‘Khan’ given to the Faruki kings.The entire area of Khandesh included two districts viz. Dhule and Jalgaon.However in 1906 for administrative purpose the headquater created at Dhule. The Khandesh was divided into two districts known as West Khandesh and East Khandesh. In 1961 the name of the district changes from west Khandesh to Dhulia and later on Dhulia District.At present the Nandurbar district comprises six tehsils i.e. Akkalkuwa, Akrani, Taloda, Shahada, Navapur and Nandurbar. There are 943 villages in the district as percensus 2011. The district comprises 6 talukas. These talukas are Akkalkuwa, Akrani Mahal (also called Dhadgaon), Taloda, Shahada, Nandurbar and Navapur. The district can be divided into two broad physiographic parts. One is hilly terrain of Satpuda ranges prominently dominated by tribals i.e. Akrani, Akkalkuwa and Toloda. Second part is Tapi

20 river basin, which is comparatively more fertile and having good irrigation facilities, covered by the three remaining Tahsils i.e. Shahada, Nandurbar and Navapur Northern boundary of the district is defined by the great Narmada river. As a whole the district is divided into two river basins viz., Tapi and Narmada. Tapi river flow from east to west in the district. The Tapi river basin in the southern part is fertile plain. Narmada flow through Satpuda Mountain ranges a very few hilly part of the district lies in Narmada basin..

Nandurbar district is divided into the Natural physiographic regions viz., i) The Tapi (Tapti) valley, ii) The Satpura region, iii) The region of dykes and residual hills of the Sahyadri hills, iv) Nawapur and western Nandurbar region.

There are three Subdivisions and six talukas in Nandurbar District.

21

Location Map of District :

22

8.0 Land Utilization Pattern in the District : Forest, Agriculture, Horticulture, Mining etc: Land Use Map for Nandurbar district is as below:

23

Description Area in ('000ha) District Name Nandurbar District Area 503 Cultivable Area 297 Forest Area 105 Land under Non agricultural use 20 Permanent Pastures 27 Cultivable Waste Land 04 Land under Misc. Trees and groves 00 Barren and un cultivable land 24

Current Fallow 01 Other Fallow 25

Irrigation Details

Irrigation Area (‘000ha) Net Irrigated area 66.00

Gross irrigated area 91.00

Rainfed area 231

Cultivation by Canala/Rivers 10.90 (Area in ‘000ha)

Agriculture Crops: Major field crops Area in (‘000ha) by Major field crops Irrigation cultivated (Kharif) Rainfed cultivated (Rabi) Sorghum 46.1 Sorghum 22.4 Paddy 26.7 Wheat 6.4 Pearl Millet 21.3 Chick Pea 7.6 Maize 20.7 Ground nut -

24

Soyabean 5.3 - Cotton 53.3 -

# Source Agriculture Plan Nandurbar (ICAR-CRIDA)

Horticulture :

Horticulture Crops (Fruits) Area in (‘000ha) Mango 6.9 Ber 1.2 Custard apple 0.8 Guava 1.1 Sapota 0.7

Horticulture Crops (Vegetables) Area in (‘000ha) Chilli 9.0 Onion 2.2 Brinjal 0.3 Tomato 0.1

Medicinal and Aromatic Crops Area in (‘000ha) Citronella 0.01 Others 0.01

# Source Agriculture Plan Nandurbar (ICAR-CRIDA) Mining :

Area under Mining Area in ha River Bed Scooping 44.92 ha Stone Mining 49.3 ha

# Source District Mining Office Nandurbar

25

9.0 Physiography of the District :

Northern boundary of the district is defined by the great Narmada river. As a whole the district is divided into two river basins viz., Tapi and Narmada. Tapi river flow from east to west in the district. The Tapi river basin in the southern part is fertile plain. Narmada flow through Satpuda Mountain ranges a very few hilly part of the district lies in Narmada basin..

Nandurbar district is divided into the Natural physiographic regions viz., i) The Tapi (Tapti) valley, ii) The Satpura region, iii) The region of dykes and residual hills of the Sahyadri hills, iv) Nawapur and western Nandurbar region. i) The Tapi (Tapti) valley:

The vast fertile plain of the Tapi River is known as ‘Tapi-kath or ‘Tapi-Thadi’. The area is quite monotonous just enough to maintain a natural system of drainage. The Tapi River, one of the chief natural features, with its total course of 86,905 km. in the district flows in westerly direction. It receives many tributaries from southern as well as northern sides. These together form the most fertile central part of the district. The northern tributaries of the Tapi River are comparatively small in length due to the proximity of the high ranges of the Satpuras. ii) The Satpura region:

Towards the north the central alluvial plain rises into a difficult and rugged country. It is covered by the Satpura ranges which is thickly wooded and inhabited by the aborigines. It is about 30 km. broad and extends in the talukas viz., Dhadgaon, Akkalkuwa, Taloda and Shahada. hill constitutes a special natural feature of the district. It is a tall hill with a height about 1,155m. and an area of 41.5 sq. km. It lies at 210 52’ north latitude and 740 34’ east longitudes. There is an ancient crater lake with 2.70km. It is 594.360 mt. in breadth. Its depth is reported to be 40 m. There is also a smaller lake a few meters away from the larger lake. The over flow from both the lakes rush in the valley known as ‘Sitakund’ or ‘Sitakhai’ by a cascade of about 152m deep and straight. Towards the west of Toranmal hill, the Satpura breaks into two ranges of hills. These ranges enclose an irregular table-land of about 50km long and 25 km broad. The tribal hamlets are scattered in this stretch of lands. Few hamlets are seen on the banks of the Narmada River which forms the inter-state boundary of the district. The whole region is very rugged and ranges in height from 300 to 600 m. above mean sea level. The Ashtamba Dongar, associated with Ashwathama and hence held sacred, is one of the highest peaks with a height of 1,325 mt.

26 iii) The region of Dykes and Residual Hills:

The ridges of the Sahyadri (Western Ghats) over the tract forming a horse – shoe - shaped starting south of Nawapur. This region includes the Southern part of Nandurbar district. It consists of residual hills and dykes of poor, dry and stony soils intervened by well watered valleys. The slopes along the ridges are precipitous. The ridges of Sahyadri (Western Ghats) reach the highest altitude of 782 mt above mean sea level. iv) Nawapur and western Nandurbar region:

The Sahyadri (Western Ghats) comes to an end in the north-east corner of this sub-region. It is full of steep hill ranges covered with forests interspersed with hamlets and village. The westerly aspect below the Sahyadrian scarps accounts for the higher rainfall of this area as compared to the rest of the district.

Drainage :

Rain water is drained by the Tapi & Narmada River and its tributariel like Gomi,rangwali, sarpani .The following are the important rivers draining across the district. The vast fertile plain of the Tapi River is known as ‘Tapi-kath or ‘Tapi-Thadi’. The area is quite monotonous just enough to maintain a natural system of drainage. The Tapi River, one of the chief natural features, with its total course of 86,905 km. in the district flows in westerly direction. It receives many tributaries from southern as well as northern sides. These together form the most fertile central part of the district. The northern tributaries of the Tapi River are comparatively small in length due to the proximity of the high ranges of the Satpuras

27

River Inventory of the district :

28

Basin Map for Nandurbar district is drawn as:

29

Confluence Points for the rivers in the district :

30

Tapi River flowing through district:

31

River streams flowing through district: (Narmada River)

32

Tapi River :

33

Rangvali & Sarpani Rivers

34

High Flood Level Map for Nandurbar District :

35

As per directive received by State Environmental Appraisal Committee, a detailed L- Section and Cross Sections at specified locations are drawn over the river running length passing through Latur district for Manjara, Terana, Tarvaja,Lendi .

Length of all above four rivers passing through the district is as below

Sr.No. Name of River Length 1 Tapi 62 2 Shivan 31 3 Nagan 36 4 Karadi 27 5 Rangavali 34 6 Gomai 30 7 Dara 47 8 Deheli 22

36

L & C – Sections for Tapi River passing through Nandurbar district :

Refer hard copy for visibility of drawings

37

L & C – Sections for Rangavali River passing through Nandurbar district :

# Refer hard copy for visibility of drawings

38

10.0 Rain Fall Data for Latur district: Average rainfall for Latur district is 800mm per year. Rainfall data recorded for last two years is tabulated below :

Rain Sr. No. Month Fall mm 2018 2019 1 Jun 365 348 2 July 489 421 3 August 589 612 4 Sept 369.2 425 5 Oct 240 270 6 Nov 86.2 87 7 Dec 80.2 85 8 Jan 10.6 8 9 Feb 6.6 4 10 Mar 3.4 2.8 11 April 2.1 1 12 May 1.9 1.1

Compared to Rain fall data for last three years as tabulated above, year 2018 has a deficit of about 308 mm considering average rainfall for the district.

Average Talukawise Annual Rainfall in mm Sr. Talukas Average Rainfall in No mm 1 Nandurbar 644.9 2 Navapur 1122.9 3 Shahada 686.1 4 Taloda 772.7 5 Akkalkuwa 1027.1 6 Akrani 761.4

39

11.00 Geology and Mineral Wealth:

The major part of the district is covered by basaltic flows commonly known as Deccan Traps and dykes of Upper Cretaceous-Lower Eocene age. Tapi Alluvial deposits are observed in Tapi River valley occupying parts of Taloda, Shahada and Nandurbar talukas. Along the north-western corner of the district, pre-trappean Bagh Beds of Middle to Upper Cretaceous age are exposed over a small area along the valley of the Devganga River.

The Nandurbar District has three Stratigraphic sequence.  Bagh Beds: - In Khandesh Region of Maharashtra State, Bagh beds are mainly exposed along the edge of the Deccan traps and lie unconformably over the metamorphic rocks. Bagh beds occurred in isolated outcrops around Kewadi-Chapdi, Arethi-Sipanpalia, Jangthi-Jamapani and Mangeli- Wani villages in the Akkalkuwa Tahsil of the Nandurbar district. They are represented by limestone beds with NNE- SSW strike and a dip of about 50 to 100. (G.G. Deshpande 1998)

 Deccan Trap Rocks: - Geologically, most of the part of the Nandurbar district is covers Deccan trap except a few strips of alluvium both the sides of Tapi River. These trap rocks are the result of outpouring of enormous lava flows which is spread over hundreds of kilometers of Western, Central and southern India. The entire area of Nandurbar region shows flow of lava variation of ‘Aa’ type and ‘Pahoehoe’. Deccan trap shows different basaltic layers such as vesicular, amygdaloidal, fractured, jointed, porphyritic and massive. The separation of lava flows determined by inter- trappean bed such as red bole, the upper layer of lava flow vesicular basalt and lower is massive basalt.

 Alluvium: - Tapi River flowing through the Nandurbar district which is resulted, few strips of alluvium land on both sides of Tapi River. Nandurbar District area encountered thick alluvium of Quaternary age which is Boulder, Gravel, Sand, Silt and Clay. The depth of alluvium layer shows variation few meters to several 100 meters.

Conclusively, Deccan Trap includes several flows of basalt which are supposed to have extruded from fissure volcanoes. The flows are mainly of two types i.e., “Pahoehoe” and “aa” types, the former being very common. It is observed in north. The flows have been intruded by large number of doleritic dykes. The dykes are generally 1 m to 20 m in width. However, few dykes are as much as 50 m wide. The dykes are aligned in an ENE-WSW direction and a few gave N-S or WNE-ESE trends.

40

The district forms a part of Tapi & Narmada basin. Rain water is drained by the Tapi River and its tributaries like Rangavali, Sarpani, Gomti etc. and their sub tributaries like.

The entire district is underlain by the Basaltic lava flows of upper Cretaceous to lower Eocene age. The shallow Alluvial formation of Recent age also occur as narrow stretch along the major rivers flowing in the area

District has 24stone quarry leases (with 3 quarries under renewal)till March 2020 covering area 49.3 ha. (Source info. District Mining Office Nandurbar)

There are 33 locations of sand ghats over Tapi, Rangavali, Sarpani rivers where sand deposition are allowed from replenishment and other safety point of view in the district. (Source info. District Mining Office, Nandurbar).

Mineral Mineable Reserves in Million Tonnes Stone 16.56 (Approx.) Sand 2.60 (Approx.)

41

Geological Map For Nandurbar District :

# Source Geological Survey of India

42

District wise details of river or stream and other sand sources:

District is merged between Tapi & Narmada river basins. Northern part of district is a part of Narmada river watershed whereas Southern part of district forms a part of Tapi river watershed and its tributaries.. District river inventory is sketched below :

There are nine major rivers draining across the district viz. Tapi, Narmada, Rangavali, Sarpani, GomiSivan, Nagan, Karadi,Dara, Daheli and their streams.

Major river contributing to Nandurbar district is Tapi. The vast fertile plain of the Tapi River is known as ‘Tapi-kath or ‘Tapi-Thadi’. The area is quite monotonous just enough to maintain a natural system of drainage. The Tapi River, one of the chief natural features, with its total course of 86,905 km. in the district flows in westerly direction. It receives many tributaries from southern as well as northern sides. These together form the most fertile central part of the district. The northern tributaries of the Tapi River are comparatively small in length due to the proximity of the high ranges of the Satpuras.

Most of the sand ghats are on Tapi river and some of on Rangavali & Sarpani. Only exposed sand ghats are allowed by administration to recommend for scooping of sand every year after proper survey and satisfactory deposition keeping 2m of sand as a base.

District has few leases of stone producing mechanical sand by crushing and meeting as per IS standards for building grade sand. But demand is for river bed sand and hence scooping of sand

43 is a major activity to cater sand requirement to infrastructural development. However district authority is promoting to use mechanical sand to balance between river bed sand scooping.

District wise availability of sand and gravel or aggregate resources:

District has 33 Sand scooping sand ghats catering 328950 brass of sand. District has 24 stone quarries catering 30850 brass stone aggregates of different sizes like 6mm,20mm,40mm, 60mm and mechanical sand.

District wise details of existing mining leases of sand and aggregates : District administration every year survey the sand deposits as per rules framed by Govt. of Maharashtra policy dated 03.09.2019 and after all legal clearances auction for period of maximum one year excluding monsoon period of 10 June till 30 September. There are 54 about sand ghats identified by administration for scooping of sand.

No. of Leases of aggregates Total Area in ha Mineable Reserves Available in Million MT 33 44.92 ha 2.60 (approx.)

Drainage System with description of main rivers:

S.No. Name of River Area drained in Sq. Km. % Area drained in the District 1 Tapi River and its 4301 72.22 % tributaries 2 Other Rivers 1654 27.78 %

# Both the rivers includes their tributaries

44

Salient Features of important rivers and streams:

S.No. Name of Total Place of Origin Altitude at Origin River/Stream Length in (m) the district (in Km) 1 Tapi 62 The river originates from Multai in 752 m of Madhya Pradesh in the 2 Rangavali 34 Originate near Ukai 104 m 3 Gomai 30 The Gomai River in India is a tributary of the . It originates in the Satpura Mountain Range and merges with the Tapti River around 2 km east of Prakasha 4 Sarpani 22 Originate near Khalibardi 254 List of Sand Ghats: Sr. Taluka Name Rive Nearest Details of Sand Scooping Govt/ Appro Area No. of r/ Gut No Pvt x Sand in ha Sand Stre Qty in Ghat am L(m) W(m) Appro Brass ved Depth (m)

126,127,12 Amalt 1 8 200 80 2 Govt. 11307 1.6 he 129 Kopar 238,239,24 2 200 80 2 Govt. 11307 1.6 li 1 Nandur Osara 3 Tapi 10,11,14 190 75 2 Govt. 14700 1.425 bar li Aaral 4 180,181 130 65 2 Govt. 5972 0.845 e Boral 5 19,20,21 260 80 2 Govt. 14700 2.08 e

45

Nashi 6 17,18 200 80 2 Govt. 11307 1.6 nda Sujalp 7 330 260 80 2 Govt. 14700 2.08 ur

8 Korit 7 260 80 2 Govt. 14700 2.08

Saval 60,61 125 45 1.5 0.562 9 Govt. 2981 da 5 Saran 10 gkhed 33,34 240 60 2 Govt. 10177 1.44 a-1 Saran 11 gkhed 38,39 250 60 2 Govt. 10600 1.5 a-2 Khaut 12 1/1,1/2 325 60 2 Govt. 13780 1.95 hal Kurav 1/1,1/2,1/ 13 250 85 2 Govt. 15017 2.125 ad 3 Bamk 149 280 60 2 14 heda Govt. 11872 1.68 tasa Biladi 1.127 15 9 205 55 2 Govt. 7968 tasa 5 Nand Shahad 125/2, 85 16 arkhe Tapi 300 70 2 Govt. 14840 2.1 a lagat da Palas 17 4 200 60 2 Govt. 8400 1.2 wada 4.531 18 Shelty 10,19,20 855 53 2 Govt. 32024 5 Sasde 19 564 130 70 2 Govt. 6431 0.91 1 Sasde 563 140 70 2 20 Govt. 6926 0.98 2 303/1,303/ 2,296/1,29 Temb 6/2,296/3, 4.152 21 755 55 2 Govt. 40017 ha 294/4,294/ 5 1,294/2,29 4/3,293,28

46

8,287/1,28 7/2,286,28 4

Bamk 22 heda 5 100 50 2 Govt. 3533 0.5 T. T Deur 23 kamk 56/2 220 60 2 Govt. 9329 1.32 heda Khair ve 24 109 210 50 2 Govt. 7420 1.05 Bhad gao 25 Fes 357/1 200 50 2 Govt. 7067 1 Dond 26 awad 26 215 50 2 Govt. 7597 1.075 e Torkh Gavthan 27 205 50 2 Govt. 7243 1.025 eda Lagat Lamb 28 6,7 90 50 2 Govt. 3180 0.45 ola

Bokalj Rang 0.187 29 52,53 75 25 2 Govt. 662 har avali 5 Navapu Nava 0.151 30 r 2 66 23 2 Govt. 1073 goan Sara 8 Karan pani 31,35,36,4 31 400 15 1 Govt. 2120 0.6 gwel 5

Mineral Potential :

Boulder (MT) Bajari (MT) Sand(MT) Total Mineable Mineral Potential 16.56 2.60 MT 19.16 MT

47

Annual Deposition :

Annual deposition is calculated by considering watershed area in Km2 ,Annual Rainfall in mm3,, Average Watershed slope, Drainage density in Km-1,Vegetative cover factor, Annual precipitation in cm, mean annual runoff in cm, mean annual temperature for Tapi, Rangavali, Sarpani rivers and plotted on district map as :

48

#cum/min

49

*In million cum, Silt Sample is collected in Sept.2018 using Punjab Type Silt Sampler and analysed at Laboratory . Silt Found 4.8 gm/lit at Biladi

50

Sr.No Taluka Name of River/ Nearest Gut Details of Sand Govt/ Approx Area in . Sand Stream No Scooping Pvt Sand Qty ha Ghat in Brass L(m) W(m) Appr oved Depth (m)

126,127,128 1 Amalthe 200 80 2 Govt. 11307 1.6 129

2 Koparli 238,239,241 200 80 2 Govt. 11307 1.6

3 Osarali 10,11,14 190 75 2 Govt. 14700 1.425

4 Aarale 180,181 130 65 2 Govt. 5972 0.845

5 Nandurbar Borale Tapi 19,20,21 260 80 2 Govt. 14700 2.08

6 Nashinda 17,18 200 80 2 Govt. 11307 1.6

7 Sujalpur 330 260 80 2 Govt. 14700 2.08

8 Korit 7 260 80 2 Govt. 14700 2.08

60,61 125 45 1.5 9 Savalda Govt. 2981 0.5625

Sarangkhe 10 Shahada Tapi 33,34 240 60 2 Govt. 10177 1.44 da-1

51

Sarangkhe 11 38,39 250 60 2 Govt. 10600 1.5 da-2

12 Khauthal 1/1,1/2 325 60 2 Govt. 13780 1.95

13 Kuravad 1/1,1/2,1/3 250 85 2 Govt. 15017 2.125

Bamkheda 149 280 60 2 14 Govt. 11872 1.68 tasa

15 Biladi tasa 9 205 55 2 Govt. 7968 1.1275

Nandarkh 16 125/2, 85 lagat 300 70 2 Govt. 14840 2.1 eda

17 Palaswada 4 200 60 2 Govt. 8400 1.2

18 Shelty 10,19,20 855 53 2 Govt. 32024 4.5315

19 Sasde 1 564 130 70 2 Govt. 6431 0.91

563 140 70 2 20 Sasde 2 Govt. 6926 0.98

303/1,303/2,2 96/1,296/2,29 6/3,294/4,294 21 Tembha /1,294/2,294/ 755 55 2 Govt. 40017 4.1525 3,293,288,287 /1,287/2,286,2 84

52

Bamkheda 22 5 100 50 2 Govt. 3533 0.5 T. T Deur 23 56/2 220 60 2 Govt. 9329 1.32 kamkheda Khairve 24 109 210 50 2 Govt. 7420 1.05 Bhadgao

25 Fes 357/1 200 50 2 Govt. 7067 1

Dondawad 26 26 215 50 2 Govt. 7597 1.075 e

27 Torkheda Gavthan Lagat 205 50 2 Govt. 7243 1.025

28 Lambola 6,7 90 50 2 Govt. 3180 0.45

Rangav 29 Bokaljhar 52,53 75 25 2 Govt. 662 0.1875 ali

Navapur 30 Navagoan 2 66 23 2 Govt. 1073 0.1518 Sarapa ni 31 Karangwel 31,35,36,45 400 15 1 Govt. 2120 0.6

53

Name of Details of Sand Scooping River/ Road/ Approx Taluka Sand Nearest Gut No Approved Stream L(m) B(m) Govt/Pvt SandQty Ghat Depth(m) Kaothal Tapi 1/1,1/2 325 60 2 Govt. 13780 tasa Kurhawad Tapi 1/1,1/2,1/3 250 85 2 Govt. 15017 Shahada tasa Tembhe Tapi 303/1,303/2,296/1, 308 75 2 Govt. 16325 Bu. 296/2,296/3

 Above sand ghats are proposed for auction this year

54

DISTRICT SURVEY REPORT FOR NANDURBAR DISTRICT

PART –B

FOR MINOR MINERALS OTHER THAN SAND MINING OR RIVER BED MINING

Prepared under

A] Appendix –X of MoEFCC, GoI notification S.O. 141(E) dated 15.1.2016 B] Sustainable Sand Mining Guidelines C] MoEFCC, GoI notification S.O. 3611(E) dated 25.07.2018

55

1.0 Introduction :

Hon’ble Supreme Court of India vide its judgement dated February 27,2012 and further relief amendment dated April 16,2012 directed all state, union territories and ministry of Environment and Forest, Govt. of India, New Delhi to screen mining of minor minerals leases within the purview of EIA notification 2006 and made requirement of environmental clearance to minor minerals less than 5 ha compulsory.

Ministry of Environment & Forest , GoI vide its office Memorandum L-11011/47/2011.IA.II(M) dated 18.05.2012 directed mass to comply Ho’ble Supreme Court decision.

Further streamlining of environmental clearance procedures, MOEFCC, GoI amended EIA notification 2006 vide S.O. 141(E) dated 15.01.2016 where procedure for preparation of District Survey Report (DSR) for minor minerals has been prescribed.

Further the procedure for preparation of DSR and format is amended vide MOEFCC notification S.O. 3611(E) dated 25.07.2018. The subjected DSR is defined at “ Appendix -X (See Paragraph 7(iii)(a)” of the notification S.O.141(E)dated 15.01.2016 and S.O. 3611(E) dated 25.07.2018

Accordingly this document is prepared by DEIAA,Nandurbar, Maharashtra State.

Nnadurbar district has constituted District Environmental Impact Assessment Authority vide letter No. Aadesh/kramank/2016/gaukhani/kavi-182 Dated- 22/06/2016 and comprised as

Sr. No. Name of the Member/Expert Designation Role 1 District Collector, Nandurbar District Collector, Nandurbar Chairman 2 D.C.F.Nandurbar D.C.F.Nandurbar Member 3 Prof. G.S.Khandagle Expert Member (Non Govt. Member Official) 4 S.D.O.Nandurbar S.D.O.Nandurbar Member Secreatary

56

Latur district has constituted District Expert Appraisal Committee Authority vide letter Aadesh/kramank/2016/gaukhani/kavi-182 Dated- 22/06/2016 and comprised as

Sr. No. Name of the Member/Expert Designation Role 1 Executive Engineer Irrigation Executive Engineer Irrigation Chairman Department, Nandurbar Department, Nandurbar 2 D.C.F.Nandurbar D.C.F.Nandurbar Member 3 Senior Geologist GSDA, Senior Geologist GSDA, Member Nandurbar Nandurbar 4 District Civil Surgeon, Nandurbar District Civil Surgeon, Nandurbar Member 5 Executive Engineer Rural Water Executive Engineer Rural Water Member Supply Divison, Z.P. Nandurbar Supply Divison, Z.P. Nandurbar 6 Sub Regional Officer, State Sub Regional Officer, State Member Pollution Control Board, Dhule Pollution Control Board, Dhule 7 Dr.V.R.Borane Jijamata Collage Nanaudrbar (Non Member Govt. Official) 8 Dr.B.B.Mangale JTP Collage Nandurbar (Non Govt. Member Official) 9 Prof. Smt. S.D.Patil Jijamata Collage Nanaudrbar (Non Member Govt. Official) 10 Executive Engineer, P.W.D., Executive Engineer, P.W.D., Member Nanaudrbar Nanaudrbar 11 District Mining District Mining Officer,Nandurbar Member Officer,Nandurbar Secreatary

Brief Introduction of Latur district :

Brief Introduction of Nandurbar district :

Nandurbar District is situated in the Northern part of the state of Maharashtra. Nandurbar district belongs to Nashik Division of Maharashtra State situated between 73.31 and 74.32 East longitude and 21.03 and 22.00 North latitude.The natural boundaries of satpuda hills along with Narmada river form its boundaries.It is spread over a geographical area of 5,955 Sq. Kms. It is 1.62% of the total Geographical area of Maharashtra. District has 06 tehsils with 4 Municipal council,01 Nagar Panchayat and 595 Grampanchayats. The two major west flowing rivers Tapi and Narmada and its tributaries criss cross through the district.

Nandurbar is an administrative district in the northwest corner (Khandesh Region) of Maharashtra state in India . On 1 July 1998 Dhule was bifurcated as two separate districts now known as Dhule and Nandurbar. The district headquarters are located at Nandurbar city. The district occupies an area of 5955 km² and has a population of 16,48,295 of which 15.45% were urban. Nandurbar district is bounded to the south and south-east by Dhule district, to the west

57 and north is the state of Gujarat, to the north and north-east is the state of Madhya Pradesh. The northern boundary of the district is defined by the great Narmada river.

Before 1 July 1998 Nandurbar was part of the larger Dhule district. Nandurbar, Dhule and Jalgaon districts formed what was known as the Khandesh district. Dhule was known as the west Khandesh whereas Jalgaon was known as the east Khandesh. So, much of history applicable to Khandesh and Dhule, is applicable to Nandurbar. Nandurbar is also known as Nandanagri as the king Named Nandaraja was the ruler of this territory. The ancient name of this region was Rasika. It is bounded on the east by Berar (ancient Vidarbha), on the north by the Nemad district (ancient Anupa) and on the south by the Aurangabad (ancient Mulaka) and Bhir (ancient Asmaka) districts. Later the country came to be called as Seunadesa after king, Seunchandra of the Early Yadava dynasty, who ruled over it. Subsequently, its name was changed to Khandesh to suit the title Khan given to the Faruqi kings by Ahmad I of Gujarat.

The ancient name of this region was ‘Rasika’. Varahmihira places Rasika coupled Vidarbha and Mahisaka, later under the Yadavas,it was called as ‘Seunadesa’ after the Yadav king Seunachandra who ruled over it. With the advent of Muslims, the name was changed to Khandesh to suit the title ‘Khan’ given to the Faruki kings.The entire area of Khandesh included two districts viz. Dhule and Jalgaon.However in 1906 for administrative purpose the headquater created at Dhule. The Khandesh was divided into two districts known as West Khandesh and East Khandesh. In 1961 the name of the district changes from west Khandesh to Dhulia and later on Dhulia District.At present the Nandurbar district comprises six tehsils i.e. Akkalkuwa, Akrani, Taloda, Shahada, Navapur and Nandurbar. There are 943 villages in the district as percensus 2011. The district comprises 6 talukas. These talukas are Akkalkuwa, Akrani Mahal (also called Dhadgaon), Taloda, Shahada, Nandurbar and Navapur.

Drainage

Two major rivers Tapi & Narmada drain the district. The drainage network of Tapi includes number of tributaries like Nagan, Shivan, Gomai, Dehali etc while tributaries like Katri, Devnadi, Udai etc form the drainage network of Narmada river. Total drainage network of the district contains about 29 watersheds out of which 21 are in Tapi river basin & 08 are in Narmada basin

The catchment area of the Tapi river is principally situated in the northern and eastern district of Maharashtra and Nandurbar district. Except the northern part drained by Narmada River and its tributaries such as Kanni, Devnad / Devganga and Udai, the entire distirct is mainly drained by Tapi River and its tributaries such as Nagan, Shivan, Gomai and Dehli. The Tapi River has a total course of 86,905 sq km. in the district. Pebbly conglomerates and sand occur in the dry bed of the Tapi River either as braided channels, point bars, levees, etc. Annually, the sand is replenished in by the river the river channel and is auctioned as natural resource.

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Tributary of Tapi River in Nandurbar District:

Gomai, Shivan, Rangawali, Sarpini, Nagan, Sukhi and Susri etc.are the tributaries of Tapi River Gomai River is tributary of Tapi River. It originates in Satpura Mountain range and merge in Tapi river around 2Km east of Prakasha. Gomai River itself has many small tributary rivers like Susri river (passing by Sultanpur), Tipiria river (passing by Mandane), Umri river, Sukhi river.

Climate The climate of the district is characterized by a hot summer and general dryness throughout the year except during the south-west monsoon season, i.e., June to September. The daily mean minimum temperature is 15.8°C and mean maximum temperature is 40.7°C. The average annual rainfall over the district is about 801 mm. It is the minimum in the eastern part of the district and increases westwards towards Nawapur and Akkalkuwa. The study of negative departures of the annual rainfall over normal reveals that north western and south western parts of the district experienced moderate and severe drought conditions for more than 20% of years. Hence this parts occupying almost entire Akkalkuwa taluka and parts of Akrani, Nawapur and Nandurbar talukas can be categorized as drought area. The average annual rainfall in the district varied from 645 mm (Shahada) to 1192 mm (Nawapur). Winds, in general, are light to moderate. But they are strengthened in force in summer and monsoon periods. Winds are mainly south-westerly to westerly during the south-west monsoon season. In the post- monsoon, they are light and variable in directions in the mornings and north-easterly to easterly in the afternoon. In winter and summer seasons they are generally from south-west directions to north-west.

Natural Economic Resources Deccan Traps cover a major part of the District. Trap rocks are very hard and compact and are dark grey in colour. Trap rocks being dense, hard and compact are extensively used as building stones, road metal, railway ballast and as an aggregate in cement concrete. Erosive agents and weathering together have formed good fertile soils near the river beds.

Forestry This includes all land classified as forest under any legal enactment dealing with forest or administered as forest, whether state owned or private and whether wooded or simply maintained as forest land. The total area under the forest is 104 Thousand hectares which is 20.78% of the total geographical area of the district. The forest in the district cover an area of 3465.79 sq. km., mostly in Dhadgaon, Akkalkuwa, Taloda and Navapur talukas. The maximum forest area is in Akkalkuwa taluka i.e. 42.34%.

Minerals and mining Minerals of great economic importance are not found in Nandurbar district. The major part of the district is covered by basaltic flows commonly known as Deccan Traps and dykes of Upper

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Cretaceous-Lower Eocene age. Tapi Alluvial deposits are observed in Tapi River valley occupying parts of Taloda, Shahada and Nandurbar talukas. Along the north-western corner of the district, pre-trappean Bagh Beds of Middle to Upper Cretaceous age are exposed over a small area along the valley of the Devganga River. Trap rocks are hard , dense and durable and are suitable for building /construction purposes. Economically important mneral required for ndustrialization not found in the district. Hence district has basalt mining for infrastructural requirements with natural river sand up to some extend. At some places some patches of agate are found but with inferior quality.

Soil and Cropping pattern On the basis of depth, texture and colour, the soil of the district are grouped into three categories viz., light soil, medium soil and deep black soils. Along the banks of Tapi River and its tributaries soil type is black cotton soil. It is enriched by lime, iron, magnesia and alkalies. In the northern part of the district the soil varies from dark brown to yellowish brown of lighter type on the hill slopes, with clayey deep soil of the Tapi River valley to its south. Medium soils are mostly located in the southern and central zones of the district below the Tapi River valley in Nawapur. The soil varies from dark brown to dark reddish brown in colour. Owing to the peculiarity of the soil, both Kharif and Rabi crops are cultivated in this zone.

Agriculture Most of the people of this District are engaged in agricultural activities. According to Census 2011, percentage of the total workers engaged as cultivators is 24.29% and as agricultural labourers is 44.26% (percent) in the District. Together they constitute 68.55 %(percent) of the total workers of the District. District is producing Kh. Jowar, Paddy,Bajri,Maiz,Toor, Mung,Soyabean,Groundnut seed and wheat as rabbi crop as most common agricultural crops. The District is divided in three subdivisions and six tahsils.

There are three Subdivisions and six talukas listed as

Name of Sub division Taluka 1. Nandurbar Nandurbar,Navapur 2. Taloda Taloda, Akkalkuva 3. Shahada Shahada,Akrani

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Salient Features of Nandurbar District :

Details of the Area District & State Nandurbar & Maharashtra Subdivision & Taluka 03 & 6 Nos. Villages 943 villages Area of district 5955 Sq. Km Minerals in district Basalt, River Sand Category ‘B’ LATITUDE LONGITUDE [E] Geographical Co-ordinates [N]

N 210 00’- N 22003” E 73°31’-E 74° 32’

Accessibility Road Connectivity District is well connected with MSH1,7, SH13,9,5,6,7,4,2 Railway Station at Nandurbar (Connecting Mumbai- Rail Connectivity Ahmedabad,Chennai-Ahmedabad) Airport Nashik (Nearest Airport) General Climatic Conditions Wind Pattern during study period North to South Summer : 40 – 42 0C Maximum Temperature Winter : 10 – 12 0C Summer : 40 – 42 0C Minimum Temperature Winter : 10 – 12 0C Average Annual Rainfall (mm) 645 mm (Shahada) to 1192 mm (Nawapur) Details of the Project Elevation 300m-600m above sea level Historical / Important Places No archeological /historical place is notified by National Archaeological/Historical/Ancient Archeological Department Government of India within Latur Monuments within district district. However there is one monument which is listed below is

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protected by State Governemt of Maharashtra. Mohida Tarf (Haveli) Names of the national park, sanctuary No sactuaries, tiger reserves, biosphere,ESA/ESZ are notified in the district. There is a part of Western ghat which is Biosphere reserve, Tiger Reserve, reported by MoEFCC, GoI for no mining /industrial zone as Elephant reserve, Forest per HLWG. Western ghat is defined vide draft notification S.O. 5135 dated 3.10.2018 for the district for two villages (RF/PF/Unclassified) (Kareghat & Khekada,Navapur Taluka) where mining or industrial activity is prohibited

2.0 Overview of Mining Activity in the district :

Latur district is rich in minor minerals such as building stone and sand. Mining activity is one of the main revenue source for the district.

District has 24 stone quarry leases (3 with valid environmental clearance but under stage of lease order)till March 2020 covering area 49.3ha. (Source info. District Mining Office Nandurbar)

There are 31 locations of sand ghats over Tapi, Rangvali,Sarpani rivers where sand deposition are allowed from replenishment and other safety point of view in the district. (Source info. District Mining Office, Nandurbar).

Villages marked on the district geological map is as below :

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3. General Profile of the district :

Nandurbar District is situated in the Northern part of the state of Maharashtra. Nandurbar district belongs to Nashik Division of Maharashtra State situated between 73.31 and 74.32 East longitude and 21.03 and 22.00 North latitude.The natural boundaries of satpuda hills along with Narmada river form its boundaries.It is spread over a geographical area of 5,955 Sq. Kms. It is 1.62% of the total Geographical area of Maharashtra. District has 06 tehsils with 4 Municipal council,01 Nagar Panchayat and 595 Grampanchayats. The two major west flowing rivers Tapi and Narmada and its tributaries criss cross through the district.

Nandurbar is an administrative district in the northwest corner (Khandesh Region) of Maharashtra state in India . On 1 July 1998 Dhule was bifurcated as two separate districts now known as Dhule and Nandurbar. The district headquarters are located at Nandurbar city. The district occupies an area of 5955 km² and has a population of 16,48,295 of which 15.45% were urban. Nandurbar district is bounded to the south and south-east by Dhule district, to the west and north is the state of Gujarat, to the north and north-east is the state of Madhya Pradesh. The northern boundary of the district is defined by the great Narmada river.

Before 1 July 1998 Nandurbar was part of the larger Dhule district. Nandurbar, Dhule and Jalgaon districts formed what was known as the Khandesh district. Dhule was known as the west Khandesh whereas Jalgaon was known as the east Khandesh. So, much of history applicable to Khandesh and Dhule, is applicable to Nandurbar. Nandurbar is also known as Nandanagri as the king Named Nandaraja was the ruler of this territory. The ancient name of this region was Rasika. It is bounded on the east by Berar (ancient Vidarbha), on the north by the Nemad district (ancient Anupa) and on the south by the Aurangabad (ancient Mulaka) and Bhir (ancient Asmaka) districts. Later the country came to be called as Seunadesa after king, Seunchandra of the Early Yadava dynasty, who ruled over it. Subsequently, its name was changed to Khandesh to suit the title Khan given to the Faruqi kings by Ahmad I of Gujarat.

The ancient name of this region was ‘Rasika’. Varahmihira places Rasika coupled Vidarbha and Mahisaka, later under the Yadavas,it was called as ‘Seunadesa’ after the Yadav king Seunachandra who ruled over it. With the advent of Muslims, the name was changed to Khandesh to suit the title ‘Khan’ given to the Faruki kings.The entire area of Khandesh included two districts viz. Dhule and Jalgaon.However in 1906 for administrative purpose the headquater created at Dhule. The Khandesh was divided into two districts known as West Khandesh and East Khandesh. In 1961 the name of the district changes from west Khandesh to Dhulia and later on Dhulia District.At present the Nandurbar district comprises six tehsils i.e. Akkalkuwa, Akrani, Taloda, Shahada, Navapur and Nandurbar. There are 943 villages in the district as percensus 2011. The district comprises 6 talukas. These talukas are Akkalkuwa, Akrani Mahal (also called Dhadgaon), Taloda, Shahada, Nandurbar and Navapur. The district can be divided into two broad physiographic parts. One is hilly terrain of Satpuda ranges prominently dominated by tribals i.e. Akrani, Akkalkuwa and Toloda. Second part is Tapi

64 river basin, which is comparatively more fertile and having good irrigation facilities, covered by the three remaining Tahsils i.e. Shahada, Nandurbar and Navapur Northern boundary of the district is defined by the great Narmada river. As a whole the district is divided into two river basins viz., Tapi and Narmada. Tapi river flow from east to west in the district. The Tapi river basin in the southern part is fertile plain. Narmada flow through Satpuda Mountain ranges a very few hilly part of the district lies in Narmada basin..

Nandurbar district is divided into the Natural physiographic regions viz., i) The Tapi (Tapti) valley, ii) The Satpura region, iii) The region of dykes and residual hills of the Sahyadri hills, iv) Nawapur and western Nandurbar region.

There are three Subdivisions and six talukas in Nandurbar District.

Map of District :

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Location Map of District :

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4.0 Geology of the District:

The major part of the district is covered by basaltic flows commonly known as Deccan Traps and dykes of Upper Cretaceous-Lower Eocene age. Tapi Alluvial deposits are observed in Tapi River valley occupying parts of Taloda, Shahada and Nandurbar talukas. Along the north-western corner of the district, pre-trappean Bagh Beds of Middle to Upper Cretaceous age are exposed over a small area along the valley of the Devganga River.

The Nandurbar District has three Stratigraphic sequence.  Bagh Beds: - In Khandesh Region of Maharashtra State, Bagh beds are mainly exposed along the edge of the Deccan traps and lie unconformably over the metamorphic rocks. Bagh beds occurred in isolated outcrops around Kewadi-Chapdi, Arethi-Sipanpalia, Jangthi-Jamapani and Mangeli- Wani villages in the Akkalkuwa Tahsil of the Nandurbar district. They are represented by limestone beds with NNE- SSW strike and a dip of about 50 to 100. (G.G. Deshpande 1998)

 Deccan Trap Rocks: - Geologically, most of the part of the Nandurbar district is covers Deccan trap except a few strips of alluvium both the sides of Tapi River. These trap rocks are the result of outpouring of enormous lava flows which is spread over hundreds of kilometers of Western, Central and southern India. The entire area of Nandurbar region shows flow of lava variation of ‘Aa’ type and ‘Pahoehoe’. Deccan trap shows different basaltic layers such as vesicular, amygdaloidal, fractured, jointed, porphyritic and massive. The separation of lava flows determined by inter- trappean bed such as red bole, the upper layer of lava flow vesicular basalt and lower is massive basalt.

 Alluvium: - Tapi River flowing through the Nandurbar district which is resulted, few strips of alluvium land on both sides of Tapi River. Nandurbar District area encountered thick alluvium of Quaternary age which is Boulder, Gravel, Sand, Silt and Clay. The depth of alluvium layer shows variation few meters to several 100 meters.

Conclusively, Deccan Trap includes several flows of basalt which are supposed to have extruded from fissure volcanoes. The flows are mainly of two types i.e., “Pahoehoe” and “aa” types, the former being very common. It is observed in north. The flows have been intruded by large number of doleritic dykes. The dykes are generally 1 m to 20 m in width. However, few dykes are as much as 50 m wide. The dykes are aligned in an ENE-WSW direction and a few gave N-S or WNE-ESE trends.

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The district forms a part of Tapi & Narmada basin. Rain water is drained by the Tapi River and its tributaries like Rangavali, Sarpani, Gomti etc. and their sub tributaries like.

The entire district is underlain by the Basaltic lava flows of upper Cretaceous to lower Eocene age. The shallow Alluvial formation of Recent age also occur as narrow stretch along the major rivers flowing in the area

District has 24stone quarry leases (with 3 quarries under renewal)till March 2020 covering area 49.3 ha. (Source info. District Mining Office Nandurbar)

There are 33 locations of sand ghats over Tapi, Rangavali, Sarpani rivers where sand deposition are allowed from replenishment and other safety point of view in the district. (Source info. District Mining Office, Nandurbar).

Mineral Mineable Reserves in Million Tonnes Stone 16.56 (Approx.) Sand 2.60 (Approx.)

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Geological Map of Nandurbar District

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5.0 Drainage of irrigation Pattern: Irrigation Details for the district :

Irrigation By Source Area in (‘000ha) Net Irrigated Area 66.00

Gross Irrigated Area 91.00

Rainfed Area 231 .00

Total 388 Source of Irrigation : Source of Irrigation Area in (‘000ha) % of Total Irrigated Area Canal -- 00 % Open Wells/Bore Wells 33 59.56 % Lift Irrigation Systems 22.4 40.44 % Total 55.4 100 %

# Source ICAR-CRIDA report.

Drainage

Rain water is drained by the Tapi River and its tributaries like Rangvali, Gomai,Sarpani and their sub tributaries. Southern part of district comprising Dhadgaon tahsil is drained by Narmada river. The following are the important rivers draining across the district.

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6.0 Land Utilization Pattern in the District : Forest, Agriculture, Horticulture, Mining etc. Land Use Map for Nandurbar district is as below:

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Description Area in ('000ha) District Name Nandurbar District Area 503 Cultivable Area 297 Forest Area 105 Land under Non agricultural use 20 Permanent Pastures 27 Cultivable Waste Land 04 Land under Misc. Trees and groves 00 Barren and un cultivable land 24

Current Fallow 01 Other Fallow 25

Irrigation Details

Irrigation Area (‘000ha) Net Irrigated area 66.00

Gross irrigated area 91.00

Rainfed area 231

Cultivation by Canala/Rivers 10.90 (Area in ‘000ha)

Agriculture Crops: Major field crops Area in (‘000ha) by Major field crops Irrigation cultivated (Kharif) Rainfed cultivated (Rabi) Sorghum 46.1 Sorghum 22.4 Paddy 26.7 Wheat 6.4 Pearl Millet 21.3 Chick Pea 7.6 Maize 20.7 Ground nut -

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Soyabean 5.3 - Cotton 53.3 -

# Source Agriculture Plan Nandurbar (ICAR-CRIDA)

Horticulture :

Horticulture Crops (Fruits) Area in (‘000ha) Mango 6.9 Ber 1.2 Custard apple 0.8 Guava 1.1 Sapota 0.7

Horticulture Crops (Vegetables) Area in (‘000ha) Chilli 9.0 Onion 2.2 Brinjal 0.3 Tomato 0.1

Medicinal and Aromatic Crops Area in (‘000ha) Citronella 0.01 Others 0.01

# Source Agriculture Plan Nandurbar (ICAR-CRIDA) Mining :

Area under Mining Area in ha River Bed Scooping 44.92 ha Stone Mining 49.3 ha

# Source District Mining Office Nandurbar

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7.0 Surface Water And Ground Water Scenario :

7.1 Surface Water Scenario :

Latur district has ten main rivers Tapi, rangvali, sarpani , Narmada in the northern part of district rivers in the district.

River Inventory for the district is sketched as

Southernpart of Nandurbar district is a part of Narmada basin and southern and central part is a part Tapi basin of and merged between Tapi-Rangavali-Sarpani watersheds .

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Total Catchment area for both the rivers are tabulated below

Name of the Name of River RCatchment Area of District area in Sq. Km Catchment in Sq. Km. Nandurbar Tapi River and its 4301 72.22 % tributaries Other Rivers 1654 27.78 %

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7.2 Ground Water Scenario :

District is in “SAFE” Category from Ground Water Development point of view. Detailed Ground Water Scenario for the district is discussed below

Hydrogeology

The major part of the district is covered by basaltic flows commonly known as Deccan Traps and dykes of Upper Cretaceous-Lower Eocene age. Tapi Alluvial deposits are observed in Tapi River valley occupying parts of Taloda, Shahada and Nandurbar talukas. Along the north-western corner of the district, pre-trappean Bagh Beds of Middle to Upper Cretaceous age are exposed over a small area along the valley of the Devganga River.

Hydrogeology of District Latur

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Depth to Water Level – Premonsoon

The premonsoon depth to water level in the district ranges between 6.20 and 13.6 mbgl. Major part of the district is having water levels of 5-10 m bgl depth viz. Akkalkkuva, Akarni, Taloda, Shahada and almost all parts Nandurbar and small patched of Navapur. The moderately deeper water levels of 10 to 20 m bgl are observed in SW part of the district in Nawapur Taluka and in a small part of Nandurbar taluka in its southern part.

Depth to Water Level – Postmonsoon

The depth to water level during postmonsoon period ranges between 0.90 to 15.2 m bgl. The shallow water levels of less than 2 m bgl are seen the hilly areas of Akkalkkuva, Akarni (extreme northern part of the district) and in few very small isolated patch of Navapur taluka in its southern part. The water levels of 2 to 5 m bgl are observed in parts of Akkalkkuva, Akarni (Northern part), Nandurbar (NW part) and Navapur talukas. Majot part of the district is having water levels of 5-10 m bgl depth viz. Akkalkkuva (southern part), Akarni (southern part), Taloda (SW and NE parts), Shahada (almost entire taluka), Nandurbar(primarily in southern part) and Navapur (almost entire taluka except some patches in southern part). The moderately deeper water levels of 10 to 20 m bgl are seen in alluvial parts of Taloda and Shahada talukas as a longitudinal patch.

The overall stage of ground water development for the district is 37 % which is quite high. All the talukas and watersheds have been categorised as “Safe” .

8.0 Rainfall of the district and Climatic Conditions :

Average rainfall for Latur district is 800mm per year. Rainfall data recorded for last two years is tabulated below :

Rain Sr. No. Month Fall mm 2018 2019 1 Jun 365 348 2 July 489 421 3 August 589 612 4 Sept 369.2 425 5 Oct 240 270 6 Nov 86.2 87 7 Dec 80.2 85 8 Jan 10.6 8

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9 Feb 6.6 4 10 Mar 3.4 2.8 11 April 2.1 1 12 May 1.9 1.1

Compared to Rain fall data for last three years as tabulated above, year 2018 has a deficit of about 308 mm considering average rainfall for the district.

Average Talukawise Annual Rainfall in mm Sr. Talukas Average Rainfall in No mm 1 Nandurbar 644.9 2 Navapur 1122.9 3 Shahada 686.1 4 Taloda 772.7 5 Akkalkuwa 1027.1 6 Akrani 761.4

The Climate of the district is characterised by a hot summer and general dryness throughout the year except during the south-west monsoon season, i.e., June to September. The temperature rises rapidly after February till May, which is the hottest month of the year. The mean daily maximum temperature during May is 42.0°C and the mean daily minimum temperature during December is 12.0°C The normal annual rainfall varies from about 700 to 800 mm ..

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9.0 Details of the mining leases in the district as per the following format : (Valid Leases as of date 31/03/2020)

S.No. Name Name of Lessee Address & Contact No. of M.L. grant Area Period of ML of Lessee Order No. & of Mineral Date M.L. Area (ha)

From To

1 2 3 4 5 6 7 8 1 Stone SachinkumarManohar Nandarkhe, Nandurbar 149 Dated – 2 30.11.2009 29.11.2019 Borse 30.11.2009 2 Stone Rajendra Narayan Patil Dhandhane, Nandurbar 348 Dated – 0.4 06.04.2011 31.03.2021 06.04.2011 3 Stone Suresh Digambar Chaudhari Dhamdod, Nandurbar 58 Dated – 4.7 27.01.2014 26.01.2019 27.01.2014 4 Stone Shankarrao Gajmal More Dhandhane, Nandurbar 57 Dated – 2.56 27.01.2014 26.01.2019 27.01.2014 5 Stone Ravindra Vyankat Patil Vaul, Nandurbar 56 Dated – 1 27.01.2014 26.01.2019 27.01.2014 6 Stone Ranjitsingh Pratapsingh Dhandhane, Nandurbar 61 Dated – 1.21 27.01.2014 26.01.2019 Rajput 27.01.2014 7 Stone Avinash Vitthal Patil Akrale, Nandurbar 60 Dated – 4.7 27.01.2014 26.01.2019 27.01.2014 8 Stone Pravin Vitthal Patil Dhirajgaon, Nandurbar 59 Dated – 2.27 27.01.2014 26.01.2019 27.01.2014 9 Stone Kala Patil Pimpari, Nandurbar 62 Dated – 2.33 28.01.2017 27.01.2019 27.01.2014

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Stone Hashambhai Abbasbhai Chaupale, Nandurbar 63 Dated – 2.21 28.01.2014 28.01.2019 Vora 28.01.2014 10 Stone Rajesh Rupchand Patil Ranale, Nandurbar 64 Dated – 3.2 30.01.2014 29.01.2019 30.01.2014 11 Stone Chandrakant Keshavlal Nandarkhe, Nandurbar 70 Dated – 2.06 10.02.2014 09.02.2019 Lakhwani & Sahebrao 10.02.2014 Uttamrao Patil 12 Stone Kamalbai Dattatray Patil Vadvad, Nandurbar 97 Dated – 1.31 05.03.2014 04.02.2019 05.03.2014 13 Stone Rajkumar Jaykumar Ajmera Navagaon, Nandurbar 449 Dated – 2.4 30.09.2015 29.09.2020 & Padamkumar Jaykumar 30.09.2015 Ajmera 14 Stone Ranveersigh Vijaysigh Rawal ,Shahada 344 Dated – 0.81 01.04.2011 31.03.2021 01.04.2011

Stone Devandrsing Chatarsing Sarangkheda,Shahada 107 Dated – 0.6 01.03.2012 01.03.2017 Rawal 01.03.2012 15 Stone Nilesh Uttam Patil Varul, Shahada 55 Dated – 1 27.01.2014 26.01.2019 27.01.2014 16 Stone Bhagwan Khushal Patil Tembhe Bh, Shahada 46 Dated – 0.8 04.02.2014 03.02.2019 04.02.2014 17 Stone Liyakt Ahmad Farid Ahmad Tembhe Bh, Shahada 113 Dated – 0.7 05.03.2014 04.03.2019 Mujawar 05.03.2014 18 Stone Shirishkumar Swarupsingh Kothada, Navapur 171 Dated – 2.02 17.05.2001 06.04.2022 Naik 07.04.2012 19 Stone Sangitabai Bharat Gavit Nandwan, Navapur 346 Dated – 0.4 06.04.2011 05.04.2021 06.04.2011

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20 Stone Sunilkumar Sitaram Sharma Tinmauli, Navapur 162 Dated – 2 12.04.2012 11.04.2022 12.04.2012 Stone Ajay Sitaram Sharma Kothda, Navapur 157 Dated – 4 31.03.2008 31.03.2018 31.03.2008 21 Stone Raya Devaji Mavachi Zhamanzar, Navapur 219 Dated – 2 18.08.2016 17.08.2021 18.08.2016 22 Stone Raya Devaji Mavachi Khatgaon, Navapur 479 Dated – 1.6 14.12.2017 13.12.2022 14.12.2017 23 Stone Sumantai Yashwant Kame Guliumbar, Akkalkuwa 131 Dated – 0.4 21.05.2010 20.05.2020 21.05.2010 24 Stone Kasaturi Dullabh Pawara Chulwad, Akrani 69 Dated – 0.62 14.02.2014 13.02.2019 14.02.2014

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Contd…. Period of ML(1st/2nd Date of Status(Working/Non Captive/ Non Obtained Environmental Method of Renewal) Commencement Working/ Temp Captive Clearance (Yes/No) If Mining of Operation Working for Yes Letter No. with date (Opencast / Despatch) of grant of EC. Underground)

From To

9 10 11 12 13 14 16 30.11.2009 Temp Working Captive --- Opne Cast Mining 06.04.2011 Working Captive --- Opne Cast Mining 27.01.2014 Temp Working Captive SEIAAEC-0000002261, Opne Cast Dated, 08/01/2020 Mining 27.01.2014 Temp Working Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining 27.01.2014 Temp Working Non Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining 27.01.2014 Temp Working Non Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining 27.01.2014 Temp Working Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining 27.01.2014 Temp Working Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining

28.01.2017 Temp Working Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining 28.01.2014 Non Working Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining

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30.01.2014 Temp Working Non Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining 10.02.2014 Temp Working Non Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining

05.03.2014 Temp Working Captive --- Opne Cast Mining 30.09.2015 Working Captive SEAC-20114/CR.321/TC-2 Opne Cast ,Dated 17/05/2015 Mining 01.04.2011 Working Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining 01.03.2012 Temp Working Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining 27.01.2014 Temp Working Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining 04.02.2014 Temp Working Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining 05.03.2014 Temp Working Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining 1st 06.04.2022 07.04.2012 Working Captive --- Opne Cast Renewal Mining 07.04.2012 06.04.2011 Working Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining 12.04.2012 Working Captive --- Opne Cast Mining 31.03.2008 Temp Working Non Captive --- Opne Cast Mining 18.08.2016 Working Captive SEAC-20114/CR.321/TC-2 Opne Cast ,Dated ,17 April,2015 Mining 14.12.2017 Working Captive DEAC-2017 -06/11/2017 Opne Cast

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& DEIAA-2017 - Mining 07/11/2017 21.05.2010 Temp Working Captive --- Opne Cast Mining 14.02.2014 Non Working Non Captive SEAC-2013/CR.205/TC-2 Opne Cast ,Dated 26/12/2013 Mining

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10. Details of Royalty or Revenue received in last three years :

Financial Year Revenue in Rs. F.Y. 2015-16 1,20,22,359/- F.Y. 2016-17 1,23,65,281/- F.Y. 2017-18 1,24,62,271/- F.Y. 2018-19 1,23,40,288/- F.Y. 2019-20 1,70,04538/-

11. Details of Production of Minor Mineral in last three years : (Approx. Quantity)

Financial Year Minor Mineral in Brass Minor Mineral in Million Tonnes F.Y. 2015-16 30055 0.2381 F.Y. 2016-17 30913 0.2449 F.Y. 2017-18 31155 0.2468 F.Y. 2018-19 30850 0.2444 F.Y. 2019-20 42511 0.3368

12. Mineral Map of District :

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Mineral Map of District

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13. List of Letter of Intent (LOI)Holders in the district along with its validity as per following format:

Location of Name Area of Use Sl. Address & Contact Letter of Intent Grant Order Validity ML of Name of Lessee M.L. to be Captive/Non No. No. of LOI Holder No. & Date of LoI Mineral allotted Captive

1 2 3 4 5 6 7 8 9 Dhamdod Suresh Digambar Dhamdod, kramank/2019/gaukhani/kavi- 6 1 Stone 4.7 Captive Chaudhari Nandurbar 1179 Dated - 19/11/2019 Months

kramank/2019/gaukhani/kavi- Dhandhane Shankarrao Gajmal Dhandhane, 6 2 Stone 409 Dated - 10/06/2019 2.56 Captive More Nandurbar Months

kramank/2020/gaukhani/kavi- Dhandhane Ranjitsingh Dhandhane, 12 Dated - 13/01/2020 6 3 Stone 1.21 Non Captive Pratapsingh Rajput Nandurbar Months

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14. Total Mineral Reserves Available in the District :

Mineral Mineable Reserves in Million Tonnes Stone 16.56 (Approx.) Sand 2.60 (Approx.)

15. Quality / Grade of Mineral available in the District :

Quality of stone available in Latur district is building grade stone confirming IS standards IS:7779 (Part II/Sec 3) of 1979.

16. Use of Mineral :

Basalt stone is used for building, construction works , road works as an aggregate.

17.Demand and Supply of the Mineral in last three years :

Basalt stone with variable sizes from 6mm,20mm,40mm,60mm,100mm are used for construction and road works as an aggregate material. Latur district has a long stretch of joining - at one end and at another surrounded by Karnataka stae boundary on South East district. To cater infrastructural requirements and local demand stone quarries are emerged catering demand for 6 tahsils. In general demand for district is ranging between 0.23-0.25 Million MT/Annum generating revenue of around 1.25 Cr. Approximately. This demand is perpetual to market requirements depending on growth of infrastructural index of the area , state and country. Detailed demand calculated for F.Y. 2019-20 is as below

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Information on demand and supply of district for sand

Name of Dostrict Total Sand Demand of Total Sand available in District in Brass district in Brass

Akola 167000 23837

Name of Tahsil Total Sand Demand of Total Sand available in District in Brass district in Brass

Akola 40500 10301 Akot 13000 0 Telhara 13000 1259 Balapur 55800 5314 Patur 11200 0 Murtizapur 22500 6963 Barshitakli 11000 0 Total 167000 23837

Ongoing Governemet, Civil, Infrastructural work in the district

Name of Govt. Details of Work Approx. qty. of sand in Deptt/Scheme Brass P.W.D. Sub Division-1 20000 P.W.D. Sub Division-2 10000 P.W.D. Sub Murtizapur 10000 Irrigation/Sinchan Anushesh Ner Dhamana, 17000 Kasodcanal,Popatkhed,Wai M.I. Projects

National Highway 50000 Gharkul Yojana 60000 Total qty. in Brass 167000

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18. Mining Leases marked on District Map

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19. Details of the area of where there is a cluster of mining leases viz. no. of mining leases. Location :

Land Area Date of Lease Lease up Name of Lessee Mineral Village S.No. Type in ha Grant From to No Cluster is formed till March 2020

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20.0 Details of Eco sensitive area

No ecosensitive area is notified within the district as per forest area. Where as Western ghat is defined vide draft notification S.O. 5135 dated 3.10.2018 for the district for two villages (Kareghat & Khekada,Navapur Taluka) where mining or industrial activity is prohibited

Map showing western ghat is as below

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Map showing western ghat in the district :

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21. Impact on the Environment (Air, Water, Noise Soil, Flora & Fauna, Land Use, agriculture, forest etc.) due to mining activity :

Air Environment : Anticipated Impacts Stone/metal mining is carried out by opencast manual method. The air borne particulate matter generated by mining and handling operations, transportation and screening of stone chips at crusher is the main air pollutant. The emissions of Sulphur dioxide (SO2), Oxides of

Nitrogen (NOX) contributed by tractor trolley. As the number of trips of tractor trolley are less, the pollutant levels are well within prescribed limits . Prediction of impacts on air environment has been carried out taking into consideration proposed production and net increase in emissions. Air pollution sources in the operating mine are classified into three categories

a. Point sources b. Area sources c. Line sources  Drilling & Blasting and crusher operations of the mine are considered as point sources  As the cumulative impacts for cluster of stone quarries are to be considered, thus the cluster of stone mines is described as area sources  Transportation of stone chips from mining pit to crusher is considered as line sources The other source of air pollution is the dust generated during the movement of tractor trolley. Water tankers with spraying arrangement will be used for regular water sprinkling on the haul roads to ensure effective dust suppression. The tractor trolley are well maintained so that exhaust smoke does not contribute abnormal values of noxious gases and un-burnt hydrocarbons.

Noise Environment : Anticipated Impacts:

The main sources of noise in the mine are classified as follows:  Transportation Vehicles/tractor trolley  Drilling & Blasting  Crushing & Screening Exposure of Noise may lead to hearing losses and may impact of mental health of Workers working in the vicinity.

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Water Environment : Anticipated Impacts:

Mining activities cause adverse impacts due to mine drainage and siltation due to storm water. The impact on water environment has been considered under the following heads:

 Water consumption  Mine seepage and impact on ground water  Impact on surface water bodies  Storm water management Soil Environment : Anticipated Impacts

Most of the stone quarries are operated at the barren area where outcrops of basalt are exposed having very thin layer of soil and overburden. This soil is removed and stacked separately for plantation around peripheral area of 7.5 m.

Land Use :

These stone quarries are very small in area. After removal of stone these abandoned quarries are used as water tank for irrigation purpose by lessee.

Forest :

No quarry is permitted within district within 250m of forest boundary and within 10 km buffer area of Eco Sensitive Area.

22. Remedial measures to mitigate the impact of mining on Environment:

Remedial measures to mitigate air environment

 Dust suppression arrangements like water tankers on haulage road and at all dust generation points  Dust extractors during crushing/ screening  Grading of haul roads time to time and cleaning to remove the accumulated dusty material  Regular maintenance of the tractor trolley.  Practicing wet drilling.

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 Controlled blasting using delay detonators.  Usage of sharp drill bits for drilling of holes  Avoiding of overloading of 10T tippers and covering of loaded tippers with tarpaulins during stone chip transportation  Dust mask provision to workers  Adequate barrier zone will be maintained all along the mine lease boundary and green belt will be maintained in the barrier zone  Periodical monitoring of air quality to take steps to control the pollutants

Remedial measures to mitigate noise environment: The operations of the mining equipment, plying of tractor trolley and mine machinery like drill operations are the major sources of undesirable noise in the proposed project area. The following control measures are proposed for bringing down the noise levels-  The vibration due to blasting is minimized by careful planning, supervision and execution of each blast and using milli-second(M.S) delay detonators and proper stemming to prevent blow out of holes  Green belt will be made around the working areas to screen the noise and also for arresting fugitive dust  Maintenance and tuning of machinery would be ensured to reduce undesirable noise  Earplugs and earmuffs will be provided to the workmen  Limiting the speed of haulage tractor  Rubber lining in the chutes of Crushing/ screening plant

Remedial measures to mitigate water environment:

The only pollution anticipated in the surface drainage water is the suspended solids, due to wash off. For this purpose retaining wall with garland drain is proposed. The discharge from this drain is diverted to a settling tank unused pit workings, which allows the sediments to settle. Further to arrest the silted drainage entering into the area down below, check dams and gully plugs shall be erected in the existing natural drains. These check dams also assist in the recharge of ground water system.

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Deliberate attempt has been made to collect this in to a garden drain. This water will be available for uses integrated above. Percolation losses will be negligible.

23. Reclamation of Mined Out Area (best practice already implemented in the district, requirement as per rules and regulations , proposed reclamation plan)

As per Maharashtra Minor Mineral Extraction & Development Rule 2013,quarry after exhaustion of mineral and on abandonment , the pit be used as a water tank or be used for fish culture or be used for Municipal solid waste dump yard.

As per requirement of Maharashtra Minor Mineral Extraction & Development Rule 2013 every stone quarry after exhaustion of minerals will plan Final Mine Closure Plan with the approval of Directorate of Geology and Mining GoM and abandon the stone quarry as per method of approval within time frame prescribed and approved by authority.

In the district, till date no mine for stone is abandoned and Final Closure Work is under operation. Details area as

Name of Area in Gut No Village/Taluka Lease Order Details Reason for Closure Lessee ha Nil Nil Nil Nil Nil Nil

24. Risk Assessment and Disaster Management Plan :

Risk Assessment

The proposed project involves Stone mining through semi mechanized opencast mining. The anticipated risks are mentioned below:

Inundation There is no chance of inundation of mine pits from surface waters such as rivers or nalas as it is situated a long away from river. The lease hold area is located in the Latur district of Maharashtra and the area in general receives appreciable amount of rain fall, which is in the range of 900mm (annual average). Pit slope & dump slope failures Mining is restricted to an average depth of 18 m from surface levels. No permanent dumps are proposed. Blasting Controlled blasting using delay detonators is proposed

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Surface Fire There are no ignitable materials in Basalt deposit. Sufficient fire extinguishers of suitable type and make will be made available at strategic locations in the mine lease area to control any fire/explosion incident. Dust from the screening & crushing operations The hazard is the inhalation of dust which is created during the screening & crushing operations which may result in the various respiratory diseases to the workers. While it is not presently possible to totally remove the hazard, properly applied control measures can substantially reduce the risk.

The dust generated during the screening & crushing operations can be controlled by providing proper enclosure to the plant area and by installing rain guns at transfer points inside the plant. Water sprinkling at the crushing and screening plant units also forms an effective measure of controlling dust generation. Provision of green belt surrounding the plant area will further suppress the spread of airborne dust to the surrounding atmosphere. The workers engaged in these operations will be provided with dusk masks. Noise Loading, screening & crushing operations give rise to harmful levels of noise. Noise generated by screening & crushing can be well controlled by providing enclosure and the green belt. The workers engaged will be provided with ear muffs.

The noise created is harmful to anyone who is within a zone around screening & crushing machines at which the noise level is above that considered to be safe for persons to work without having to use control measures. Therefore wherever necessary, the workers engaged will be provided with ear muffs.

The noise levels around screening & crushing equipment should be measured and the risk assessed. Unless control measures are in place no-one, except those necessary for the work in hand, should be allowed inside the designated noisy area.

In most cases this will be the operators. The risk is highest at older machines. Newer large machines are provided with sound insulated systems which control the noise levels to acceptable levels.

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Other control measures will include training operators and providing them with ear protection, although the later should only be seen as an interim precaution until a permanent solution can be found.

The risk is very high when no control measures are provided. However if all the control measures specified as above are provided the risk will be low. Loading The main hazard associated with loading is the Mineral falling on to the loading labour/tractor, tractor toppling over due to uneven ground, failure of hydraulic systems. Good housekeeping practices, regular cleaning of the haulage roads and regular maintenance of the tractors, loading operations under supervision of competent persons, etc will be done to avoid such accidents. Heavy Vehicles Tractor used for excavation and loading and 20 tonne dumpers used for mineral and waste transport are the major heavy vehicles in the proposed mine. The main hazards arising from the use of such machines are incompetent drivers, brake failure, lack of all around visibility from the drivers position, access to the cab, vehicle movements particularly reversing, roll over, vibration, noise, dust and maintenance. Those most at risk are the driver and company employees likely to be struck by the vehicle, and drivers of smaller vehicles, which cannot be seen from the cabs of large vehicles. Visibility defects can be reduced by the use of visibility aids such rear view mirrors.

Good maintenance and regular testing are necessary to reduce the possibility of brake failure. An area shall be set out as a testing area where regular tests are carried out on the effectiveness of a vehicles braking system.

Protection guards will be provided for moving parts of the equipment and handling heavy components during maintenance work. Those most at risk will be the users of the system, vehicle operators and also company employees working in such areas may also be at risk. Explosives No magazine is within lease hold area. Contractual blasting is proposed. House keeping The provision and maintenance of a safe and healthy workplace is the most basic principle of health and safety. Dirty and untidy workplaces or walkways contribute to a very large proportion of trip and fall accidents. In the context of surface mining the provision of well defined roadways and walkways clear of obstruction and regular cleaning up of spillage will

99 greatly reduce the potential risk for this type of accidents. Lack of maintenance may lead to roadways and walkways being unsuitable for use. The Work The application of risk assessment depends upon a full understanding of all aspects of the job being undertaken. In carrying out a risk assessment in relation to a particular task the evaluation must include a review of the knowledge, experience and training of those persons carrying out the work. Personal Competence It follows that the knowledge, experience and training of personnel involved in work is critical to evaluate any risk assessment. A knowledgeable, experienced well-trained and competently supervised workforce will be at a lower risk of accidents occurring than a poorly trained and badly supervised workforce. For this purpose all the supervisory and managerial staff qualified under MMR 1957 shall only be employed. Co-ordination A competent person should be given the responsibility for overseeing and coordinating work as required under the MMMEDR 2013. It is essential that the coordinator ensures that everyone engaged in the work is capable and understands the role of others and their responsibility for each other. This is particularly important when contract workers undertake part or all of the work to be carried out. Equipments The prerequisite for the risk assessment is that equipments are suitable for the work being undertaken and have been designed, manufactured and installed to at least the minimum standards for health and safety. Failure to meet the standard will result in people being at higher risk and remedial steps have to be implemented to compensate the shortfall. Other interim arrangements should be implemented to protect any persons exposed to latent danger. Maintenance of plant and equipment to agreed specification, whether original or upgraded to the latest health and safety standards, is essential. Dangerous parts of machinery Parts of machinery such as revolving parts, in running nips and entrapment between reciprocating parts as defined in European and National standards should be protected meeting those standards. Health hazards For the purposes of this document health hazards should be interpreted as being harmful dust and noise which is emitted during surface mining operations, as well as the handling of heavy loads. While complete elimination and often suppression at source is not practicable, in many cases, the normal threshold values of health standards should be made applicable.

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Personal Protective Equipment (PPE) The PPE should be of good construction, where ever possible ISI certified, suitable for the hazard e.g. a dust respirator fitted with the correct filter to capture the particular hazardous dust and maintained to recommended standards. As personal protective equipment only affords limited protection it should only be used as a last resort and then as an interim arrangement until other steps are taken to reduce the risk of personal injury to an acceptable level. Traffic Movement The traffic movement should only take place within designated areas and over suitable roadways. Adopting one way traffic movement systems are preferred to two directional traffic systems. The risk of accidents due to traffic movement is much less with a one way traffic. Whenever mineral is mined the first step in winning the product is the preparation of the site. The four main stages in the site preparation are: 1. Planning 2. Surveying 3. Clearing of site 4. Laying out Planning The risk of injuries can be significantly reduced if sufficient regard is given to health and safety at the planning stage of a new or developing mine. Using trained drivers can largely eliminate the danger of being struck by large moving vehicles and providing the vehicles with suitable appliances, such as aids to ensure the driver has all round visibility. Designing and implementing one-way traffic systems and ensuring that open edges of roadways are suitably protected with parapet wall to prevent accidental driving off the edge can further reduce the danger. Additionally, ensuring that the vehicles are properly maintained in good working condition, particularly the braking system will go a long way to help the driver control the vehicle. Well-designed access and working platforms will also reduce the possibility of a fall. Surveying Surveying has its hazards, for example surveyors are likely to be seriously injured if they fall from heights or are thrown out of overturning vehicles. Since the hazards are created by ground formation it is unlikely that they can be removed.

Those normally at risk would be the surveying team of the surveyor and assistants. Individuals working at the edge of vertical face or on very steep undulating ground are at greater risk than those working on level ground. Driving over steep rough terrain is more dangerous than driving over gentle slopes. It is necessary to give clear positive instruction and ensure vehicles used to

101 gain access to the areas to be surveyed are well maintained and suitable for the terrain over which access is to be gained.

Clearance Clearance covers all the activities associated with preparing a site ready for laying out primary roads for working a face. The primary hazards are being struck by falling trees and debris from demolition of buildings, use of power saws, equipment used in the removal of the top layers of earth and trucks used to convey it to storage areas, and the possibility of being struck by trucks.

The hazards are created in clearing the site. While the clearing of the site cannot be avoided adopting the safest methods to carry out the work can control hazards. For example, fully trained persons should be used in tree felling operations. Well-maintained fully protected power saws should be used and the operatives should wear full personal protection e.g. safety helmets, ear defenders, face shields, gloves, full protection for legs (trousers) and boots.

Laying out There are many different ways of opening and development of mines but careful planning particularly concerning the mine layout will reduce hazards. Well maintained equipment is essential to reduce the risk of injuries.

If suitable equipment is not used, for example if poor and badly constructed scaffolding is used there is a much higher probability of persons falling from heights or the scaffolding collapsing than if good properly constructed scaffolding is used.

To reduce the risk of injuries while using large earth moving equipment and vehicles the equipment drivers and those giving signals should be well trained. The lack of training and competence in the use of such equipment is the biggest cause of such type of accidents.

25. Disaster Management Plan

The following natural/industrial hazards may occur during normal operation.  Inundation of mine pit due to flood/excessive rains;  Slope failure of pits  Accident due to explosives;  Accident due to heavy mining equipment; and

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In order to take care of above hazard/disasters, the following control measures have been adopted.  Checking and regular maintenance of garland drains and earthen bunds to avoid any inflow of surface water in the pit  Provision of suitable pumps for pumping out water from the pit during heavy rains  Entry of unauthorized persons is prohibited  Fire fighting and first-aid provisions in the mines office complex and mining area  Provisions of all the safety appliances such as safety boot, helmets, goggles etc. are made available to the employees and regular check for their use  Training and refresher courses for all the employees working in hazardous premises  Working of mine, as per approved plans and regularly updating the mine plans  Cleaning of mine faces is regularly done  Regular maintenance and testing of all mining equipment as per manufacturer’s guidelines  Suppression of dust on the haulage roads  Increasing the awareness of safety and disaster through competitions, posters and other similar drives

The management is able to deal with the situation efficiently to reduce confusion keeping in view of the likely sources of danger in the mine.

Out Line Of Disaster Management Plan

The purpose of disaster management plan is to restore the normalcy for early resumption of mining operation due to an unexpected, sudden occurrence resulting to abnormalities in the course of mining activity leading to a serious danger to workers or any machinery or the environment.

System of communication An internal communication system for the department head and to their line of command should be maintained. Having the telephone nos and addresses of adjoining mines, rescue station, police station, Fire service station, local hospital, electricity supply agency and standing consultative committee members is another essential aspect.

Consultative committee A standing consultative committee of 3 persons headed by Mines Manager will be formed. Facilities & Accommodation

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Accommodation and facilities for medical centre, rescue room and for various working groups will be provided.

First Aid & medical facilities The mine management is having first aid for use in emergency situation. All casualties would be registered and will be given first aid.

Stores and equipment A detailed list of equipment available its type & capacity and items reserved for emergency will be maintained.

Transport services A well-defined transport control system will be provided to deal with the situation.

Functions of public relations group A cordial relation with government officials and other social service organization and working groups shall be maintained. To liaise with representatives of the mine workers to ameliorate the situation of panic, tension, sentiments, grievances and misgivings created by any disaster. To ameliorate the injured, survivors and family members of affected persons by providing material, moral support, finance and establishing contact with relatives of victims.

Security Strict manning of security posts during the disaster will be done.

Catering & Refreshment Arrangements will be made for the victims, rescue teams and others for their Catering & Refreshment services.

26. Plantation and Green Belt Development in respect of leases already granted in the district:

District administration on yearly basis collects the compliance w.r.t. green clearance along with photographic evidences of plantation and safety measures the green belt development plan along with quarry owners individually and with their associations. District has developed a very handsome inventory of trees with pollution control measure implementation system.

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27. Any other information :

Nil

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DISTRICT SURVEY REPORT FOR NANDURBAR DISTRICT

PART –C

FOR OTHER MINERALS EXCLUDING RIVERBED SAND, BUILDING STONE

Prepared under

A] Appendix –X of MoEFCC, GoI notification S.O. 141(E) dated 15.1.2016 B] Sustainable Sand Mining Guidelines C] MoEFCC, GoI notification S.O. 3611(E) dated 25.07.2018

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1.0 Details of leases for other minerals like Coal, Limestone and dolomite are tabled below :

No exploration work for other minerals (excluding Riverbed sand, building stone) is proposed or under existence for the district.

This district Survey report is reviewable and for district information. Copying of technical data without approval of district authority is restricted.

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Annexure -1 : Procedure to scrutinize Minor Mineral proposals

Procedure to scrutinize Minor Mineral proposals

1] Receipt of Application as per MMMEDR 2013 with required documents

2] Receipt of S.D.O. Report over 14 points stipulated by administration.

3] Site Visit by representative of Mining Office, Latur/District Mining Officer, Nandurbar.

4] correlating demand and supply for the taluka, nearest town or any specific demand for specific project on feasibility of requirement of stone quarry.

5] Issuance of Letter of Intent.

6] Procedure for award of Lease.

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Annexure -2 : Procedure to monitor compliances of Minor Mineral Leases

Procedure to monitor compliances of Minor Mineral Leases

1] After award of lease, first compliance to prior EC conditions are to be submitted by Leasee for ground work carried out.

2] Yearly Compliance to Lease Agreement for royalty clearance, Lease conditions and prior EC conditions(scrutiny based on photographic and documentary evidences with site visit).

3] Penal Action : failure to submit compliance as per sr. no. 2, district administration reserves right to hold the royalty passes or to suspend of cancel lease agreement subject to fulfillment of compliance.

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Annexure -3 : Demand and Supply for Latur District

Demand and Supply for :Nandurbar District

For Stone

Sr. No. District Particulars 2020-2021 Quantity in Brass 1 PWD 12000 2 Irrigation Dept. 5000 Domestic Requirement including Govt. Nandurbar Contractors,Local Lease/ Quarry Operators 3 17000 4 NHAI/Central Road Fund 3500 5 Railway 3500 Total 41000

For Sand

Name of Dostrict Total Sand Demand of Total Sand available in district in District in Brass Brass

Nandurbar 230267 45122

Name of Tahsil Total Sand Demand of Total Sand available in district in District in Brass Brass

Nandurbar 24127 0 Navapur 19818 0 Shahada 111811 45122 Akrani 24766 0 Taloda 27077 0 Akkalkuwa 22668 0 Total 230267 45122

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Ongoing Governemet, Civil, Infrastructural work in the district

Name of Govt. Deptt/Scheme Details of Work Approx. qty. of sand in Brass Gharkul Pradhanmantri 81669 Yojana,Gharkul Yojana,Shabri Yojana,Ramai Yojana Irrigation Projects 14852 NHAI 2667 PWD Building, Bridges, Roads 5740

Minor Irrigation Deptt. Recharge Bunds,Repairing 10438 of percolation tanks,village talav,cement nalla bund

Nagarpaliks 27650 PMGSY Gram Sadak Yojana 20585 MSRDC 66666 Total qty. in Brass 230267

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Annexure -4 MoEFCC, GoI notification S.O. 3611(E) dated 25.07.2018

112

Annexure -5 L Sections and Cross Sections for rivers flowing through Nandurbar district

113

L & C SECTIONS TAPI RIVER

114

L & C SECTIONS RANGAVALI RIVER

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Annexure -6 Corporate Environmental Responsibility Nandurbar District for Stone Quarries

116

Annexure-6 Corporate Environmental Responsibility Nandurbar District for Stone Quarries

Corporate Environmental Responsibility Plan as per OM F 22-65/2017-IA.III dated 01.05.2018

( For all Stone Quarries : Latur District)

Type of Project as per OM : Greenfield Project

Capital Investment : Rs. 50.00 Lakh per quarry (approx.)

Amount to be allocated to : Rs. 1.00 Lakh per quarry Implement CER

Proposed CER with Budgetary provision

Sr.No. Proposed CER Activity Amount 01 Community Plantation ( 500 trees/year) excluding 75000.00 plantation defined in EMP @ Rs. 150/ tree 02 Provision for supply of pit water accumulated during 25000.00 monsoon to nearby farmers after settling including pumping cost to nearby farmers Total 100000.00

Above attribute may change subject to approval of district authority/conditions of prior environmental clearance.

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Annexure -7 Sections for Sand Ghats 2019-20 (Amendment Proposed for F.Y. 2019-20)

118

119

120

121

Annexure -8 COMPLIANCE TO ENFORCEMENT AND MONITORING GUIDELINES FOR SAND MINING 2020 (PUBLICATION OF ANNEXURES )

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COMPLIANCE TO ENFORCEMENT AND MONITORING GUIDELINES FOR SAND MINING 2020 (PUBLICATION OF ANNEXURES )

Details of Sand/M Sand Sources: Annexure-I

a) Rivers

Taluka Name of River/ Nearest Gut No Details of Sand Scooping Road/ Approx Type of Sand Ghat Stream L(m) B(m) Approved Govt/Pvt SandQty River Depth(m)

Shahada Kaothal Tapi 1/1,1/2 325 60 2 Govt. 13780 Perennial tasa Kurhawad Tapi 1/1,1/2,1/3 250 85 2 Govt. 15017 tasa Tembhe Tapi 303/1,303/2,296/1, 308 75 2 Govt. 16325 Bu. 296/2,296/3

b) De siltation Locations (Lakes,Ponds,Dams)

Nil

C) Patta Lands/Khatedari Land

Nil

123 d) M-Sand Plants

Inclusion of M Sand/Patta Land in DSR not give landowners/operators right to operate M-sand Plant/Sand Mining Lease. All the sand ghats referred above are in the stage of various clearance on district administration level.

No crusher is notified for manufacturing of M-Sand in the district.

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List of Potential Mining Leases (Existing & Proposed) Annexure-II A] Rivers (Mineral Sand)

Taluka Name of River/ Nearest Gut No Details of Sand Scooping Road/ Approx Type of Sand Ghat Stream L(m) B(m) Approved Govt/Pvt SandQty River Depth(m)

Shahada Kaothal Tapi 1/1,1/2 325 60 2 Govt. 13780 Perennial tasa Kurhawad Tapi 1/1,1/2,1/3 250 85 2 Govt. 15017 tasa Tembhe Tapi 303/1,303/2,296/1, 308 75 2 Govt. 16325 Bu. 296/2,296/3

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B] De siltation Locations (Lakes,Ponds,Dams)

Nil

C] Patta Lands/Khatedari Land

Nil

D] M-Sand Plants

Nil Inclusion of M Sand/Patta Land in DSR not give landowners/operators right to operate M-sand Plant/Sand Mining Lease. All the sand ghats referred above are in the stage of various clearance on district administration level.

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Cluster & Contiguous Cluster Details Annexure-III

Clusters:

River Cluster No Lease No Location Village Area in Ha Total Total Name River Excavation Mineral Bed/Patta (Ton) Excavation Land (Ton)

NIL

Contiguous Clusters:

River Contiguous Cluster Number Location(River Distance Village Area of Total Name No of Bed/Patta between Cluster Mineral Leases Land) clusters in ha Excavation in the (Ton) cluster

NIL

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Transportation routes for individual leases ANNEXURE IV

Lease Transportat No of Length Type of road Recommended Road will Route ion route tippers/tractors of route (Black action for road be Map per day topped/Paved) constructed Location by Govt./Lease owner Kaothal tasa Individual 27 260 Paved Provision for By Individual Kurhawad tasa Details are 28 740 +Blacktopped compaction contractor Details Tembhe Bu. in EMP 32 860 and gradation and Govt. are in with in different EMP maintenance modes is made as part of EMP

Transportation routes for leases in cluster

No cluster is formed…..

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Final List of Potential Leases (existing and proposed) Annexure –V

A] Rivers (Mineral Sand)

Taluka Name of Sand River/ Nearest Gut No Details of Sand Scooping Total Road/ Approx Ghat Stream L(m) B(m) Approved Depth in m Govt/Pvt SandQty Depth(m) Shahada Kaothal tasa Tapi 1/1,1/2 325 60 2 4 Govt. 13780 Kurhawad Tapi 1/1,1/2,1/3 250 85 2 4 Govt. 15017 tasa Tembhe Bu. Tapi 303/1,303/2,296/1, 308 75 2 4 Govt. 16325 296/2,296/3

B] De siltation Locations (Lakes,Ponds,Dams)

Nil

C] Patta Lands/Khatedari Land

Nil

D] M-Sand Plants

Plant Name Owner District Tehsil Village Geo Qty location TOnnes/Annum No notified M Sand units in the district Inclusion of M Sand/Patta Land in DSR not give landowners/operators right to operate M-sand Plant/Sand Mining Lease. All the sand ghats referred above are in the stage of various clearance on district administration level.

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Cluster & Contiguous Cluster Details Annexure-VI

Clusters:

River Cluster No Lease No Location Village Area in Ha Total Total Name River Excavation Mineral Bed/Patta (Ton) Excavation Land (Ton)

NIL

Contiguous Clusters:

River Contiguous Cluster Number Location(River Distance Village Area of Total Name No of Bed/Patta between Cluster Mineral Leases Land) clusters in ha Excavation in the (Ton) cluster

NIL

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Final Transportation routes for individual leases ANNEXURE VII

Lease Transportat No of Length Type of road Recommended Road will Route ion route tippers/tractors of route (Black action for road be Map per day topped/Paved) constructed Location by Govt./Lease owner Kaothal tasa Individual 27 260 Paved Provision for By Individual Kurhawad tasa Details are 28 740 +Blacktopped compaction contractor Details Tembhe Bu. in EMP 32 860 and gradation and Govt. are in with in different EMP maintenance modes is made as part of EMP

Transportation routes for leases in cluster

No cluster is formed…..

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