Scanned with CamScanner DISTRICT SURVEY REPORT-

CHPATER -1 INTRODUCTION

As per Gazette Notification of 15th January, 2016 of Ministry of Environment, Forest and Climate Change a survey shall be carried out by the District Environment Impact Assessment Authority (DEIAA) with assistance of Irrigation department, Drainage department, Forest department, Mining department and Revenue department in district of preparation of District Survey Report as per the sustainable sand mining guidelines, 2016 to ensure identification of area of aggradations or deposition where mining can be allowed, and identification of areas of erosion and proximity to infrastructural structures and installation where mining should be prohibited and calculation of annual rate of replenishment and allowing time for replenishment after mining in thatarea.

Every effort has been made to cover sand mining locations, areas and overviews of mining activity in the district with all the relevant features pertaining to geology and mineral wealth in replenish- able and non-replenish-able areas of rivers, stream and other sources. The mineral potential is calculated based on field investigation taking coordinates of the area and gather all relevant information and geology of the catchment area of the river or stream.

Also as per the site condition and location depth of mineable mineral is defined. The area of removal of mineral in the river and stream is decided on geomorphology and other factors, it can be 50% to 60% of the area of a particular river or stream. This District Survey Report shall form the basis of application for environmental, preparation of reports and appraisal of projects.

HISTORICAL PERSPECTIVE:

The district „Hingoli‟ was created bifurcating the district and formed on 24th April 1999. Earlier to this, it was a tahsil in the district. In the medieval period „Hingoli‟ wasknownas„Wingully‟.Itisquitelikelythatthepresentname„Hingoli‟isaderivative of„Wingully‟,WingamulhandlaterLingoli.Therefinedname„Hingoli‟cameintobeingin the year1866.

Until 1853, the area of was an indivisible part of the ancient Vidharbha region. During the British rule it was the border line of the Nizam state of Hyderabad. It was a base camp for the Nizam‟s troops. Military hospital, veterinary hospital for the benefit of troops was available in the area. Because of these, the area became a military cantonment and a famous town in the erstwhile Hyderabad State. There are still some localities like Phaltan, Risala, Tofkhana, and

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DISTRICT SURVEY REPORT-HINGOLI

Pensionpura, Sadar Bazar etc., which reminds the oldkingdom.

As stated earlier, Hingoli was part of the . Hingoli was famous as a placewherethesuppressionofthingscommencedin1838.Italsoformedacantonment till 1903. Afterwards some of the Nizam‟s troops were stationed here. Today Hingoli district is well known as a trade centre and is linked both by road and rail. A market yard was established at Hingoli in 1933. Though churches are comparatively less in number, temples and mosques are plenty in the district. Among them, the temple „Aundha‟ (Nagnath) is famous probably, the only one structure which reminds the old history of the district. Today Hingoli district has an area of 4827.0Km2.

LOCATION AND GEOGRAPHICAL DATA:

Hingoli district has been separated from Parbhani district and existed as an independent district from 01.05.1999. It is one of the eight districts of . It is located at eastern site of State.

Hingoli is situated at the northern part of Marathwada in Maharashtra. Borders of Hingoli are surrounded by and Yeotmal in northern side, Parbhani in Western side and at South-Eastern side. The district came into existence by division of Parbhani district on 1st May, 1999. Latitude of Hingoli district is 19.43 N and Longitude is 77.11 E. The geographical area of the district is 4526 Sq. kms; which is 1.47% of area of the MaharashtraState.

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DISTRICT SURVEY REPORT-HINGOLI

Source: www.mapofindia.com

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DISTRICT SURVEY REPORT-HINGOLI

LOCATION OF HINGOLI DISTRICT IN THE MAP OF MAHARASHTRA:

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DISTRICT SURVEY REPORT-HINGOLI

Source: www.mapofindia.com

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DISTRICT SURVEY REPORT-HINGOLI

ADMINISTRATIVE:

Hingoli district comes under Administrative Division. The district of Hingoli consists of 5 tehsils, namely, Hingoli, , , Aundha and .

S. No. Sub Division Taluka 1. Hingoli Hingoli,, Sengaon 2. Basmath Aundha, Basmath 3. Kalamnuri Kalamnuri

Source: www.mapofindia.com

TOPOGRAPHY:

The district has a grographical area of 4526 sq.kms; which forms 1.47% of the total geographical area of Maharashtra State. The Sengaon, Hingoli and Aundhanaganath tehsils of the district are surrounded by small hills. The district is 600 meters high from sea level.

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DISTRICT SURVEY REPORT-HINGOLI

DEMOGRAPHY:

As per census 2011, Hingoli had population of 1, 177,345 of which male and female were 606,294 and 571,051 respectively. In 2001 census, Hingoli had a population of987,160 of which males were 505373 and remaining 481787 were females. Its population growth rate over the decade 2001-2011 was 19.43%. Hingoli has a sexratio of 942 females for every 1000 males, and a literacy rate of78.17%.

Marathi is the official and the most spoken language in the district. Nearly 83% of the population speaks Marathi as the mother tongue. Native speakers of Deccani , and Banjari/Labhani languages are also present in significant numbers.

Source: Census of 2011

RIVER AND DRAINAGE:

The district is well drained by river systems, which are dendritic type and have matured valleys. There are three main drainage systems viz: Penganga river, PurnaKayadu Rivers.

The river Penganga originates from Ajanta hills in . It enters in the district from Sengaon Taluka towards northeastern corner and by making a jorney of about

Kilometres in the district moves towards district. Isapur Dam is constructed on the river. It is one of the most important rivers of and whole district of Hingoli falls in its greatbasin.

The direct tributary of the river is Kayadhu. This tributary raises from the hill ranges near Risodtaluka of . The length of the river in the district is 80.50 kms. It is a seasonal river, which dries up in summer.

The River rises from Ajnata hill ranges. It enters in the district from . After making a journey of nearly 100 kms, it moves towards Parbhani district. Yeldari and Sidheshwar dams are constructed on the river.

SOIL:

The Soils of the district are derived from the basaltic lava flows. Thickness of the soil cover is less in northern and western parts where ground elevations are higher and consequently soil regur, gravels, murum are transported down to lower regions through gravity, transported down to lower regions through gravity, water or winds. Soils in central, southern and eastern regions of the

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DISTRICT SURVEY REPORT-HINGOLI district near the banks of Penganga and Purna rivers are thicker. Here soils, ranging in depth from 1 to 2 m, are black and rich in plantnutrients.

CLIMATIC CONDITIONS:

The district has dry and tropical climate with hot summer and mild winter with humid SW monsoon season of moderate rainfall. In Hingoli district, monsoon starts from the month of June and ends in September. In the remaining period the weather is very dry. The average rainfall in the district is 895 mm. About 83% of the rainfall occurs during

June to September and July is the rainiest month. The maximum temperature of the district is 42.6 degree Celsius and minimum temperatures are 10.6 Degree Celsius.

The air is generally dry over the district except during the southwest monsoon when the relative humidity is high. Winds are generally light to moderate with increase in speed during the latter half of the hot season and in monsoon season. The winds blow predominantly from directions between west and north during the hot season. They are mostly from directions between southwest and northwest during the southwest monsoonseason.

CONNECTIVITY:

The Hingoli district map provides information about various routes to reach Hingoli. Hingoli is well connected to the rest of the state and India by road and railway connections.

BY ROAD:

The district of Hingoli is well served by a network of roads. There is a National Highway connecting - Jahangir-Washim-Kanhergaon Naka-Hingoli-Kalamnuri- Nanded- Deglur-Sangareddy-Hyderabad named National Highway-161. Intra-city road transportation is good in Hingoli.

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DISTRICT SURVEY REPORT-HINGOLI

Source: www.mapofindia.com

BY RAIL:

Hingoli Railway Station is a railway station on Purna-Akola section of Hyderabad (HYB) Division of South Central Railway (SCR). After Divisional adjustments in 2003, which saw the bifurcation of Hyderabad Division, Hingoli now comes under Nanded(NED) Division of SCR. Hingoli is well connected to cities like Hyderabad, , Jaipur, Kota, Ajmer, Indore, New , Bhopal. Agra, Tirupati, Chandigarh, Amritsar and Sri Ganganagar.

The major railway stations near to Hingoli are Nanded railway station (84 km), Parbhani railway station (75 km) & Akola railway station (135 km) which are connected to all majorcities.

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DISTRICT SURVEY REPORT-HINGOLI

Source: www.mapofindia.com

By Air:

The nearest domestic airport is in Nanded (80 km) which serves as a common airport for Nanded, Parbhani and Hingoli districts. Presently there are no commercial flights to and from Nanded. Chikalthana Airport, Aurangabad (232 km) operates regular flights to Mumbai &Delhi

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DISTRICT SURVEY REPORT-HINGOLI

Source: www.mapofindia.com

CHPATER -2 OVERVIEW OF MINING ACTIVITY IN THE DISTRICT

As Hingoli district lies on Basaltic Deccan Trap. Occurrences of major minerals are not reported from this area till date. But minor mineral which used as construction material like river sand, stone, murrum and soil are comprises economical wealth of district.

Sand mining in district is mainly carried out in exposed river bed of Purna and Kayadhu rivers. These two rivers are major source of river sand in district. The sand plots where river sand deposits are thick and necessary to mined to maintain its natural flow and HFL level (like point bar) are allowed for sand mining. As per NGT direction only manual mining of sand is allowed.

Stone quarries are important to maintain continuous flow of construction material like gitti to the infrastructural development. Temporary Permits/License are also permitted in district for murrum, stone and soil mining so that potter, brick manufactures and road builders can maintain their routine as well as government development work smoothly andcontinuously.

APPROACH TO SAND MINING:

River sand mining is a common practice as habitation concentrates along the rivers and the mining locations are preferred near the markets or along the transportation route, for reducing the transportation cost. River sand mining can damage private and public properties as well as aquatic habitats. Excessive removal of sand may significantly distort the natural equilibrium of a stream channel. The river sand found in the entire district. The main source of the river sand is from Purna River and KayadhuRiver.

Mainly three types of minor minerals constituents such as sand, stone and Bajri are required for any type of construction apart from other material like cement and steel.

In earlier times, the houses / buildings were constructed in form of small dwellings with walls made up of mud plaster, stone and interlocking provided with wooden frames and there were

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DISTRICT SURVEY REPORT-HINGOLI negligible commercial as well as developmental activities resulting in less demand of building material. However with the passage of time, new vistas of developmental activities were started. The quantity of minor minerals consumption in a particular area is a thermometer to assess the development of the area. Thus with the pace of development activities, the consumption of minor minerals also increased. As such the demand of minor minerals in the district has started an increasing trend. In order to meet the requirement of raw material for construction, the extraction of sand is being carried out exclusively from the river beds. In Hingoli district, the demand of sand (river borne collection) and of Bajri/Grit (river borne collection or through manufactured grit by stone crushers) is mainly met by the supply from Purna and Kayadhu river beds.

MAIN OBJECTIVES OF SUSTAINABLE SAND MINING:

. To ensure that sand and gravel mining is done in environmentally sustainable and socially responsiblemanner. . To ensure availability of adequate quantity of aggregate in sustainablemanner. . To improve the effectiveness of monitoring of mining and transportation of mined outmaterial. . Ensure conservation of the river equilibrium and its natural environment by protection and restoration of the ecologicalsystem. . Avoid aggradations at the downstream reach especially those with hydraulic structures such as jetties, water intakesetc. . Ensure that the rivers are protected from bank and bed erosion beyond its stable profile. . No obstruction to the river flow, water transport and restoring the riparian rights and in streamhabitats. . Avoid pollution of river water leading to water qualitydeterioration. . To prevent depletion of ground water reserves due to excessive draining out of groundwater. . To prevent ground water pollution by prohibiting sand mining on fissures where it works as filter prior to ground waterrecharge. . To maintain the river equilibrium with the application of sediment transport principles in determining the locations, period and quantity to beextracted. . Streamlining and simplifying the process for grant of environmental clearance (EC) for sustainablemining. MAHARASHTRA SUB BASINS

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Source: www.mapofindia.com

CHPATER -3

THE LIST OF MINING LEASE IN THE DISTRICT WITH LOCATION,AREA AND PERIOD OF VALIDITY

There are no major minerals available in the district. However, sand & stones, which are required for construction of buildings, are available in thedistrict.

Details of the minor mineral mining leases in the district are as follows:-

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LIST OF MINOR MINERAL IN HINGOLI

Name of Name of the Lessee Letter of Area of private/ uptoV Location of the Sr. the holder/adderss Contact Intent Mouza/ Survey No Mining lease Governmen period aildity Mining lease No Mineral No. Grant Tahsil to be allotted t land (Latitiude& Order No. Longitude) & date Longitude Latitiude 2015-2016 1 Nil Nil Nil Nil Nil Nil Nil Nil Nil Nil Nil Nil 2016-2017

1 NIL NIL NIL NIL NIL NIL NIL NIL NIL NIL Nil NIL 2017-2018

Ja.kr.2018/ Gau.Kh./Kha MarsulT.S 77o09'22.9 19o28'52. 1 Stone Ashish Ashok 940497477 .P/ Aadesh/CR endursan 3,15,31 3.40 Private 1 year 31.03. " to 1" to Kasat at Basmat 0 - Dated a 6 2019 77o09'34.5 " 19o28'58" 09.04.2018

N19o17'17. E77o07'50 Ja.kr.2018/ 23 .85 Gau.Kh./Kh. N19o17'17. E77o07'45 2 Stone M/s Patil Const. 020- P/ aadesh/CR Pimpala 53 2.40 Private 4 Years 31.03. 72 .75 at Basmat 24479626 - Dated Choure 2022 N19o17'23. E77o07'48 08.02.2018 90 .53 N19o17'23. E77o07'51 75 .67 ManojChand Ja.Kr.2018/ N19o55'16. E76o48'31 3 Stone rkantSantre 992243221 Gau.Kh./Kh. PanKanerga 197 1.00 Private 4 Years 31.03. 65 .16

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DISTRICT SURVEY REPORT-HINGOLI

Name of Name of the Lessee Letter of Area of private/ uptoV Location of the Sr. the holder/adderss Contact Intent Mouza/ Survey No Mining lease Governmen period aildity Mining lease No Mineral No. Grant Tahsil to be allotted t land (Latitiude& Order No. Longitude) & date Longitude Latitiude at.Nijampur 1 P/Aadesh/CR on 2022 N19o55'16. E76o48'28 30 .37 o o Tq.RisodDistWashi - Dated N19 55'20. E76 48'27 22 .91 m 23.07.2018 o o N19 55'20. E76 48'30 64 .72 0 0 4 stone Sanjay 7774009414 Ja.kr.2019/gau. Bhabhulag 115 1.00 Privet 3 31.03. N19 53’02. E77 02”04’ aon 2022 NamdevraoKawarkhe kh./kha.p./aade 37 .32 0 0 At Po sh/kavi-318 N19 53”02’. E77 02”00’ GoregaonTqSengaon dinak 42 .26 DistHingoli 04/09/2019

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LIST OF SAND GHAT (YEAR 2015 -2016)

S. Name of River Bed Lenth X Width X Depth Area in No. Taluka Sand Ghat Gat No along the river bed Ha Brass L B D

1 Hingoli Amla Kayadu 263to270,283,288,291,292,295to297,323to325, 268 21 0.30 0.56 600 328,337,338

2 Hingoli Mop Penganga 2,87,28,82,89,290 101 35 0.40 0.35 500

3 Hingoli Sarkadi Kayadu 166 17 0.30 0.28 300 249 त2े 52, 254 त,े 262, 264, 265, 270,271,48,21

त2े 4, 28,33,34,35,37,38,41,42,43,47

4 Hingoli Limbala P.W. Penganga 4/3,03,32,30/2,30/3,30/5,30/6,31/1,29/6,29/9, 188 30 0.40 0.56 800 29/7,29/2.

5 Hingoli Wanzhola Penganga 75 to 82,92,95,96,105 177 28 0.40 0.50 700

6 Hingoli Samga Kayadu 204,17,271 505 14 0.40 0.71 1000

7 Sengaon Limbala (A) Purna river 3,2,36,35,34,28,27, 113 15 0.50 0.17 300

8 Sengaon Bhramwadi Purna river 14,31,41,135 141 20 0.50 0.28 500

9 Kalamnuri Sawangi (BHU) Kayadu 38,45,55,59,61,62,64,70,71,79,80 416 17 0.40 0.71 1000

10 Kalamnuri Kasbedhawanda Kayadu 61 7 0.40 0.04 60 48,43,42,41,40,39, 56 त5े 9, 61, 62, 64, 65, 66, 67,38,60/1,55/1,2,54,53,51,50,49

11 Kalamnuri DongargoanPul Kayadu 10,17,18,20,21,33,34 52 9 0.30 0.05 50

12 Basmath PimpalgaonKute Purna 17,5,76,78,339,340,359, 136 13 0.40 0.18 250

13 Basmath Bhramangaon Purna river 7,1,8,9 138 12 0.30 0.17 175

14 Basmath Mategaon Purna 2,34,221,222, 94 17 0.30 0.16 170

15 Aundha(NAG) Tapovan Purna 283,284,285, 234 29 0.50 0.68 1200

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S. Name of River Bed Lenth X Width X Depth Area in No. Taluka Sand Ghat Gat No along the river bed Ha Brass L B D

16 Aundha(NAG) Chimegaon Purna 1,4,6,92,71,68,69,65,63,11,56,55,53, 119 19 0.50 0.23 400

17 Aundha(NAG) Pota (KH) Purna 20,37,38,40,46,47 132 50 0.30 0.66 700

18 Aundha(NAG) Nalegaon Purna 2,49,248 206 55 0.30 1.13 1200

LIST OF SAND GHAT (YEAR 2016 -2017)

Lenth X Width X S. Name of River Taluka Sand Ghat Gat No along the River bed Depth Area in Ha Brass No. Bed L B D 1 Hingoli Hingni Kayadhu 365,367,368,370,371,314,06,21,14,01,252,251, 262 505 28 0.20 1.41 1000 279,496,495,499,402,492,491,460,459, 458,457, 456,455,454,452,451,450,449,429,428,426,423, 2 Hingoli Iroli Kayadhu 128 22 0.50 0.28 500 422, 421,420,408TO419,391,380,379,377,376,270 TO 283,288,291,292,295 to 297

3 Kalamnuri Bu. Kayadhu 1,3,4,6,7,13,46,124,127,197 51 22 0.50 0.11 200 4 Kalamnuri Yegaon Kayadhu 45,49 85 22 0.30 0.19 200 5 Kalamnuri Nandapur Kayadhu 47,64,77,50,15,02,503 246 23 0.40 0.57 800 6 Aundha Na. Matha Purna 2,91,29,22,93,298 157 30 0.30 0.47 500 7 Sengaon BardaPimpri Purna 98,153,187,186 94 12 0.50 0.11 200 8 Kalamnuri Sapli Kayadhu 2,3,6,7,8,9,10,11,13,14,15,16 216 23 0.40 0.50 700

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Lenth X Width X S. Name of River Taluka Sand Ghat Gat No along the River bed Depth Area in Ha Brass No. Bed L B D 14,126,129,130,131,132,133,134,139,141,142,143, 9 Kalamnuri Kondhur Kayadhu 265 25 0.30 0.65 700 144,145,201,202,205,206 10 Aundha Na. Nalegaon Purna 35,36,95,89,86,87 356 45 0.30 1.60 1700 11 Aundha Na. Ajarsonda Purna 403404 566 40 0.20 2.26 1600 12 Vasmat SawangiKhu. Purna 10, 11, 12, 13, 21, 22, 23, 24, 25, 26, 27 139 36 0.50 0.50 883 13 Vasmat Sawangi Bhu. Purna 1,3,360,367,368 280 36 0.50 1.01 1780 SonnarTarfeHatta 13 Vasmat Purna 2,3,45,141,152 323 32 0.20 1.03 730 BrahmangaonKhu. 14 Vasmat Purna 7,1,8,9 371 37 0.20 1.37 970 15 Sengaon LimbalaHudi Purna 6,7,8 101 35 0.40 0.35 500

LIST OF SAND GHAT (YEAR 2017 -2018)

Name of Gat No along the Area Upset Price S. No Taluka Sand plot Brass BP- 1 BP-2 BP- 3 BP- 4 River Bed river bed. in Ha. (Rs) Hingoli 19°53'35.71"N 19°53'36.45"N 19°53'37.85"N 19°53'39.78"N 1 Kherda Kayadhu 87,90,91,211,214 0.47 500 5,56,875 77°14'51.52"E 77°14'50.60"E 77°14'52.10"E 77°14'53.59"E 17,18,19,67,65, Hingoli Durgdhamani Kayadhu 79,63,62,61,60, 7,79,625 19°39.'35.56N 19°39.'35.11N 19°39.'30.85N 19°39.'31.31N 2 59,58,221,220, 0.66 700 77°11'10.64"E 77°11'12.22"E 77°11'10.73"E 77°11'09.17"E 219,218,217,216, 215

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Name of Gat No along the Area Upset Price S. No Taluka Sand plot Brass BP- 1 BP-2 BP- 3 BP- 4 River Bed river bed. in Ha. (Rs) Sengaon 03,02,36,35,34, 19°43'58.06"N 19°43'59.43"N 19°43'58.47"N 19°43'57.31"N 3 Limbala Amari Purna River 0.71 500 12,99,750 28,27 76°46'49.11"E 76°46'48.23"E 76°46'45.93"E 76°46'45.94"E 31,32,34,35,37, 19°29'47.81"N 19°29'48.48"N 19°29'44.73"N 19°29'44.09"N 4 Kalamnuri Chikhali Kayadhu 40,41,42,38,115, 0.47 500 9,42,750 77°27'56.91"E 77°27'57.80"E 77°28'00.73"E 77°27'59.83"E 116,1,2,6 54,56,57,58,60, 19°35'31.72"N 19°35'33.03"N 19°35'34.13"N 19°35'36.84"N 5 Kalamnuri Chapnath Kayadhu 1.70 1800 21,51,900 61,62,65,66 77°18'06.36"E 77°18'07.64"E 77°18'05.57"E 77°18'02.28"E 27,31,32,33,34, 13,36,875 19°30'14.95"N 19°30'14.20"N 19°30'13.49"N 19°30'12.30"N 6 Kalamnuri Kanhegaon Kayadhu 0.36 500 200,210,202,203 77°26'53.47"E 77°26'54.44"E 77°26'55.69"E 77°26'54.83"E 88/2,88/1,89,9/1, 19°35'07.79"N 19°35'07.15"N 19°35'05.53"N 19°35'04.88"N 7 Kalamnuri Ta. Kayadhu 34,35,39,40,43, 0.28 500 6,06,000 77°18'21.29"E 77°18'20.96"E 77°18'23.38"E 77°18'22.48"E 44 38,45,56,55,59, 8,16,750 19°36'13.55"N 19°36'12.17"N 19°36'11.10"N 19°36'12.47"N 8 Kalamnuri Sawangi Bhu. Kayadhu 62,61,64,70,71, 0.64 900 77°13'16.15"E 77°13'15.79"E 77°13'20.62"E 77°13'20.98"E 79,80 384,383,371,372, 19°35'54.55"N 19°35'53.11"N 19°35'52.21"N 19°35'51.82"N 9 Kalamnuri Sodegaon Kayadhu 1.13 1200 10,89,000 311,310,308,392 77°15'28.94"E 77°15'29.21"E 77°15'24.87"E 77°15'20.69"E 186,187,188,189, 19°36'15.78"N 19°36'17.24"N 19°36'17.78"N 19°36'15.66"N 10 Kalamnuri Salegaon Kayadhu 276,298,289,220, 1.42 1500 17,93,250 77°16'10.93"E 77°16'10.90"E 77°16'21.71"E 77°16'21.74"E 219,218,216,214 19°31'01.46"N 19°31'00.28"N 19°30'56.93"N 19°30'53.31"N 11 Aundha Na. Anjanwadi Purna 6,10,11,22,20 2.36 2500 1,12,33,125 76°57'39.74"E 76°57'41.10"E 76°57'36.86"E 76°57'33.67"E

38,96,100 19°31'05.33"N 19°31'08.22"N 19°31'11.58"N 19°31'10.37"N 12 Aundha Na. Bhagwa Purna 53,54,55 1.71 1800 76°57'47.08"E 76°57'52.57"E 76°57'57.04"E 76°57'58.08"E 20,37,38,40,46, 19°29'45.43"N 19°29'50.27"N 19°30'01.52"N 19°30'05.82"N 13 Aundha Na. PotaKh. Purna 2.93 2300 103,34,475 47 76°57'24.68"E 76°57'27.97"E 76°57'24.75"E 76°57'24.00"E

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Name of Gat No along the Area Upset Price S. No Taluka Sand plot Brass BP- 1 BP-2 BP- 3 BP- 4 River Bed river bed. in Ha. (Rs) 4,5,6,7,8,46,48, 19°29'24.40"N 19°29'16.76"N 19°29'08.23"N 19°29'08.85"N 14 Aundha Na. Pota Bk. Purna 49,50,52,53,55, 2.41 1700 16,11,600 76°56'47.34"E 76°56'48.43"E 76°56'51.37"E 76°56'52.88"E 56 347,348,349,355, 364,365,366,367, 19°29'33.34"N 19°29'34.75"N 19°29'32.91"N 19°29'31.80"N 15 Aundha Na. Ankhali Purna 1.27 1800 38,96,100 372,376,344,390, 76°57'09.72"E 76°57'09.13"E 76°57'04.79"E 76°57'00.26"E 396,400 19°27'44.17"N 19°27'44.17"N 19°27'39.79"N 19°27'39.77"N 16 Aundha Na. Nandkheda Purna 3,5 0.57 400 6,93,600 76°55'52.97"E 76°55'51.52"E 76°55'51.43"E 76°55'52.87"E 12,13,10,11,79, 19°26'33.46"N 19°26'27.71"N 19°26'25.96"N 19°26'23.15"N 17 Aundha Na. Tapowan Purna 1.91 1350 17,55,675 80,70,69 76°55'13.24"E 76°55'15.89"E 76°55'17.62"E 76°55'21.80"E

18 Aundha Na. Daregaon Purna 8,9,11 2.27 1600 60,84,000 19°25'32.17"N 19°25'34.23"N 19°25'36.65"N 19°25'42.25"N 76°55'09.26"E 76°55'15.06"E 76°55'17.76"E 76°55'20.71"E 160,161,162,163, 164,165,136,137, 19°42'14.87"N 19°42'14.40"N 19°42'06.45"N 19°42'06.89"N 19 Hingoli Hingoli Kayadhu 0.7 500 7,42,500 157,240,241,242, 77°08'15.42"E 77°08'15.06"E 77°08'25.70"E 77°08'26.08"E 243,244,245,23 363 to 370,4,5, 333,330,329,326, 311,312,313,314, 19 to 22,14,15, 19°37'54.66"N 19°37'57.29"N 19°37'59.34"N 19°38'03.76"N 20 Hingoli Hingani Kayadhu 17,310,305,304, 1.41 1000 14,85,000 77°11'50.25"E 77°11'52.72"E 77°11'55.46"E 77°11'58.45"E 302,301,300,299, 274,273,271,269, 265,264,263,262, 202,201,251

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Name of Gat No along the Area Upset Price S. No Taluka Sand plot Brass BP- 1 BP-2 BP- 3 BP- 4 River Bed river bed. in Ha. (Rs) 19°42'25.10"N 19°42'27.00"N 19°42'27.71"N 19°42'27.10"N 21 Sengaon Chikhalgar Purna River 31, 157, 111, 156 0.47 500 17,33,000 76°49'05.59"E 76°49'09.48"E 76°49'12.92"E 76°49'13.06"E 16,15,14,12,09, 19°48'17.34"N 19°48'18.07"N 19°48'21.61"N 19°48'20.88"N 22 Sengaon Salegaon Purna River 08,07,05,104, 0.70 1250 28,75,000 76°35'52.68"E 76°35'52.32"E 76°36'01.29"E 76°36'01.64"E 101,100 1, 2, 4, 5, 6, 7, 31, 19°33'29.48"N 19°33'28.82"N 19°33'36.25"N 19°33'38.61"N 23 Kalamnuri Sapali Kayadhu to 35, 16, 18,30, 1.41 1000 16,27,000 77°21'56.07"E 77°21'56.58"E 77°22'10.05"E 77°22'12.96"E 36, 37, 24, 28,29 149,193,194,195, 196,1,2,3,6,10, 19°33'26.79"N 19°33'26.18"N 19°33'27.03"N 19°33'28.22"N 24 Kalamnuri Pimpuri Bu. Kayadhu 1.13 800 28,52,000 11,15,150,192, 77°25'20.85"E 77°25'20.76"E 77°25'13.10"E 77°25'07.39"E 190,187,185,181 291 to 293, 298, 19°32'09.02"N 19°32'00.37"N 19°31'59.04"N 19°31'57.71"N 25 Aundha Na. Matha Purna 0.70 750 46,13,250 312 to 314 76°58'04.05"E 76°58'04.80"E 76°58'04.58"E 76°58'03.87"E 19°28'58.10"N 19°28'57.34"N 19°28'52.32"N 19°28'49.09"N 26 Aundha Na Takalgavhan Purna 13 to 18 3.12 2200 15,64,200 76°56'48.85"E 76°56'50.24"E 76°56'46.95"E 76°56'44.63"E 19°31'51.80"N 19°31'50.87"N 19°31'45.16"N 19°31'43.64"N 27 Aundha Na Chimegaon Purna 71, 92 4.25 4500 97,40250 76°57'56.33"E 76°57'57.89"E 76°57'54.15"E 76°57'53.78"E 21,25,26,30,31, 19°34'01.32"N 19°34'02.32"N 19°33'59.94"N 19°33'58.89"N 28 Kalamnuri Dongatgaon Kayadhu 0.50 700 18,71,625 33,34,22,23,24 77°23'45.78"E 77°23'46.40"E 77°23'50.50"E 77°23'49.83"E 1,2,3,4,5,222, 223,224,225,226, 19°37'16.75"N 19°37'18.04"N 19°37'22.12"N 19°37'20.84"N 29 Aundha Na. Pur Purna 1.13 1200 25,97,400 234,235,237,238, 77°12'05.95"E 77°12'06.67"E 77°11'59.18"E 77°11'58.46"E 239,240,242

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LIST OF SAND GHAT (YEAR 2018 -2019)

Sr. Name of Length X Width Area in Upset Taluka Sand plot Gat No along the river bed Brass BP- 1 BP-2 BP- 3 BP- 4 No. River Bed X Depth(Mtr) Ha. Price (Rs) 19°53'37.36"N 19°53'40.85"N 19°53'41.30"N 19°53'37.81"N 1 Hingoli Kherda Pengang 87,90,91,211,214 135x35x0.30 0.47 501 598194 77°14'53.24"E 77°14'56.06"E 77°14'54.91"E 77°14'52.09"E 19°35'12.74"N 19°35'02.45"N 19°35'01.97"N 19°35'12.26"N 2 Kalamnuri Digras T. Ko. Kayadhu 34,9/1,8/2,89,89/1,88/2 370x25x0.40 0.93 1307 1560558 77°18'19.07"E 77°18'25.65"E 77°18'24.95"E 77°18'18.37"E

17,18,19,67,65,79,63,62,61,60, 19°39'31.75"N 19°39'36.06"N 19°39'35.69"N 19°39'31.38"N 3 Hingoli Durgdhamani Kayadhu 59,58,221,220,219,218,217, 138x48x0.30 0.66 702 838188 77°11'09.07"E 77°11'10.41"E 77°11'12.02"E 77°11'10.67"E 216,215 19°36'12.31"N 19°36'14.89"N 19°36'14.13"N 19°36'11.55"N 4 Kalamnuri Sawangi Bhu. Kayadhu 38,45,56,55,59,62,61,64,70,71, 350x23x0.40 0.81 1138 1358772 79,80 77°13'22.50"E 77°13'34.20"E 77°13'34.21"E 77°13'22.51"E 19°30'02.47"N 19°29'48.91"N 19°29'48.90"N 19°30'02.46"N 5 AundhaNa. PotaKhu. Purna 20,37,38,40,46,47 433x31x0.40 1.34 1897 2265018 76°57'23.86"E 76°57'27.88"E 76°57'26.78"E 76°57'22.76"E 363,364,368,369,370,334,335, 333,330,329,326,311,312,313, 19°38'00.46"N 19°38'07.22"N 19°38'07.67"N 19°38'00.91"N 6 Hingoli Hingani Kayadhu 314,22,21,20,19,17,15,14,310, 242x39x0.30 0.94 1000 1194000 305,304,302,301,300,299,274, 77°11'56.69"E 77°12'00.94"E 77°11'59.67"E 77°11'55.42"E 273,71,269,265,264,263,262, 202,201,251 19°33'32.04"N 19°33'24.99"N 19°33'25.84"N 19°33'32.88"N 7 Kalamnuri Sapali Kayadhu 4,5,6,7,31to37,57,58,61,62,63 397x30x0.30 1.19 1263 1508022 77°22'03.41"E 77°21'51.99"E 77°21'51.48"E 77°22'02.90"E 19°48'11.15"N 19°48'16.22"N 19°48'17.04"N 19°48'11.98"N 8 Sengaon Salegaon Purna 16,15,14,12,9,8,7,5,104,101, 223x30x0.30 0.67 709 846546 100 76°35'47.96"E 76°35'53.44"E 76°35'52.87"E 76°35'47.39"E 19°33'28.02"N 19°33'26.87"N 19°33'26.09"N 19°33'27.24"N 9 Kalamnuri Pinpri Bu. Kayadhu 9,10,6,3,2,1,199,196,195,194, 295x24x0.40 0.71 1001 1195194 193 77°25'10.89"E 77°25'20.94"E 77°25'20.95"E 77°25'10.90"E 4,5,6,7,46,47,48,50,52,53,55, 19°29'25.37"N 19°29'11.64"N 19°29'11.63"N 19°29'25.35"N 10 AundhaNa. Pota Bu. Purna 423x29x0.30 1.23 1300 1552200 56,57,58 76°56'52.08"E 76°56'52.96"E 76°56'51.96"E 76°56'51.08"E

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Sr. Name of Length X Width Area in Upset Taluka Sand plot Gat No along the river bed Brass BP- 1 BP-2 BP- 3 BP- 4 No. River Bed X Depth(Mtr) Ha. Price (Rs) 404,403,405,416,417,426,427, 19°27'25.97"N 19°27'17.62"N 19°27'18.07"N 19°27'26.42"N 11 AundhaNa. Ajarsonda Purna 311x29x0.40 0.90 1275 1522350 430,435,466,437,467 76°55'44.93"E 76°55'38.90"E 76°55'38.03"E 76°55'44.05"E 19°32'15.22"N 19°32'05.95"N 19°32'05.93"N 19°32'15.19"N 12 Kalamnuri Sewala Kayadhu 7,8,19,17,20,21,26/1,26/2,26/3 285x25x0.40 0.71 1007 1202358 77°26'30.42"E 77°26'30.09"E 77°26'30.94"E 77°26'31.27"E 19°28'32.70"N 19°28'25.14"N 19°28'25.88"N 19°28'33.45"N 13 AundhaNa. Nalegaon Purna 2,18,255,253,24,233,232,231 350x27x0.30 0.95 1002 1196388 76°56'20.69"E 76°56'11.71"E 76°56'11.22"E 76°56'20.18"E 1,2,3,4,5,222,223,224,225,226, 19°37'22.39"N 19°37'15.68"N 19°37'16.46"N 19°37'23.17"N 14 AundhaNa. Pur Purna 400x29x0.30 1.16 1230 1468620 234,235,237,238,239,240,242 77°11'55.41"E 77°12'07.17"E 77°12'07.73"E 77°11'55.96"E 19°34'49.82"N 19°34'45.31"N 19°34'44.81"N 19°34'49.32"N 15 Kalamnuri Kondhur Kayadhu 140 to 144 198x20x0.50 0.40 700 835800 77°18'37.24"E 77°18'42.09"E 77°18'41.66"E 77°18'36.81"E 347,348,349,355,364,365,366, 19°29'36.40"N 19°29'30.55"N 19°29'29.63"N 19°29'35.48"N 16 AundhaNa. Ankhali Purna 472x30x0.30 1.42 1501 1792194 322,376,374,390,396,400 76°57'10.40"E 76°56'55.43"E 76°56'55.78"E 76°57'10.75"E 19°34'12.72"N 19°34'08.71"N 19°34'09.16"N 19°34'13.50"N 17 Kalamnuri Dongargaon Kayadhu 33,34 306x25x0.40 0.77 1081 1290714 77°23'33.54"E 77°23'42.55"E 77°23'43.27"E 77°23'33.77"E 19°30'53.33"N 19°30'29.14"N 19°30'29.21"N 19°30'53.74"N 18 AundhaNa. Anjanwadi Purna 6,10,11,22,20 765x32x0.30 2.45 2595 3098430 76°57'33.75"E 76°57'33.50"E 76°57'32.41"E 76°57'32.74"E 19°31'04.94"N 19°31'08.28"N 19°31'07.45"N 19°31'04.10"N 19 AundhaNa. Bhagwa Purna 53,54,55 201x30x0.40 0.60 852 1017288 76°57'46.34"E 76°57'52.26"E 76°57'52.78"E 76°57'46.86"E 19°31'44.58"N 19°31'37.80"N 19°31'37.51"N 19°31'44.54"N 20 AundhaNa. Chimegaon Purna 71,92 221x29x0.40 0.64 906 1081764 76°57'53.93"E 76°57'55.59"E 76°57'54.70"E 76°57'52.94"E 19°29'45.39"N 19°29'41.80"N 19°29'42.45"N 19°29'46.03"N 21 Kalamnuri Chikhli Kayadhu 116 143x33x0.30 0.47 500 597000 77°27'58.61"E 77°28'01.73"E 77°28'02.63"E 77°27'59.51"E 30,31,27,28,29,21,25,26,13, 19°26'28.71"N 19°26'22.32"N 19°26'21.53"N 19°26'27.92"N 22 AundhaNa. Tapowan Purna 315x33x0.30 1.04 1102 1315788 289,290,288,284,287 76°55'17.84"E 76°55'26.28"E 76°55'25.52"E 76°55'17.08"E

19°25'40.58"N 19°25'31.09"N 19°25'32.02"N 19°25'40.83"N 23 AundhaNa. Daregaon Purna 6/1,6/2 463x32x0.20 1.48 1047 1250118 76°55'21.22"E 76°55'10.42"E 76°55'09.92"E 76°55'20.15"E

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Sr. Name of Length X Width Area in Upset Taluka Sand plot Gat No along the river bed Brass BP- 1 BP-2 BP- 3 BP- 4 No. River Bed X Depth(Mtr) Ha. Price (Rs) 29,292,293,298,312,313,314, 19°32'12.02"N 19°32'02.18"N 19°32'02.17"N 19°32'12.00"N 24 AundhaNa. Matha Purna 305x31x0.30 0.95 1002 1196388 315 76°58'03.80"E 76°58'05.16"E 76°58'04.10"E 76°58'02.73"E 19°35'37.60"N 19°35'32.38"N 19°35'30.51"N 19°35'35.72"N 25 Kalamnuri Chanfnath Kayadhu 54,55,56,57,58,60,61,62,65,66 309x55x0.30 1.70 1802 2151588 77°18'00.40"E 77°18'09.46"E 77°18'09.09"E 77°18'00.03"E 19°30'21.61"N 19°30'15.77"N 19°30'16.22"N 19°30'22.06"N 26 Kalamnuri Kanhegaon Kayadhu 6 190x25x0.30 0.48 504 601776 77°26'48.60"E 77°26'50.74"E 77°26'51.48"E 77°26'49.34"E 19°49'23.10"N 19°49'24.64"N 19°49'23.70"N 19°49'22.16"N 27 Sengaon Ban Purna 393,372,364,253,142 200x30x0.40 0.60 848 18,90,192 76°31'53.26"E 76°31'59.94"E 76°32'00.21"E 76°31'53.53"E 1,28,127,129,153,155,157,161, 19°49'14.23"N 19°49'16.61"N 19°49'15.70"N 19°49'13.32"N 28 Sengaon WazarKh. Purna 200x30x0.40 0.60 848 18,90,192 162,165,166,171-173,188,351 76°32'37.98"E 76°32'44.38"E 76°32'44.74"E 76°32'38.34"E BrahmangaonK 19°21'37.52"N 19°21'26.89"N 19°21'27.43"N 19°21'38.05"N 29 Basmat Purna 1,7-9 420x32x0.40 1.34 1900 42,35,100 h. 76°53'31.40"E 76°53'22.36"E 76°53'21.40"E 76°53'30.46"E 19°23'31.95"N 19°23'19.60"N 19°23'19.63"N 19°23'31.99"N 30 Basmat Dhawalgaon Purna 207-209,211 400x30x0.50 1.20 2120 35,17,080 76°54'10.76"E 76°54'06.46"E 76°54'05.40"E 76°54'09.70"E 19°23'54.80"N 19°23'40.90"N 19°23'40.90"N 19°23'54.80"N 31 Basmat Mategaon Purna 3-7 450x32x0.50 1.44 2544 42,20,496 76°54'17.38"E 76°54'12.55"E 76°54'11.41"E 76°54'16.22"E 19°24'47.32"N 19°24'54.03"N 19°24'54.61"N 19°24'47.89"N 32 Basmat Parli Purna 348,352,354-356 350x30x0.50 1.05 1855 41,34,795 76°55'00.97"E 76°55'10.66"E 76°55'09.76"E 76°55'00.07"E PimpalgaonKu 19°19'10.98"N 19°19'25.50"N 19°19'25.22"N 19°19'10.70"N 33 Basmat Purna 13,59,75,76,78,337,338,340 500x33x0.60 1.65 3498 77,97,042 te 76°53'55.07"E 76°54'03.72"E 76°54'02.31"E 76°53'53.63"E 19°22'52.57"N 19°22'39.49"N 19°22'39.53"N 19°22'52.60"N 34 Basmat Sawangi Bk. Purna 1,3,360,367,368 410x34x0.60 1.39 2955 65,86,695 76°53'34.04"E 76°53'31.33"E 76°53'30.10"E 76°53'32.91"E SonaTarfHatt 19°20'51.97"N 19°21'03.61"N 19°21'03.40"N 19°20'51.76"N 35 Basmat Purna 2-5 410x15x0.50 0.62 1087 24,29,610 a 76°53'29.54"E 76°53'22.68"E 76°53'22.22"E 76°53'29.08"E 19°25'16.47"N 19°25'04.66"N 19°25'04.57"N 19°25'16.36"E 36 Parbhani Jodparli Purna 24,52-55,57,61-65,272-276, 400x35x0.50 1.40 2473 55,12,317 284-288,293 76°55'04.57"E 76°55'10.26"E 76°55'11.50"E 76°55'06.06"E Pimpalgaon 19°19'44.42"N 19°19'33.40"N 19°19'33.40"N 19°19'44.42"N 37 Parbhani Purna 146-149 350x25x0.50 0.875 1546 34,46,034 Tong 76°53'58.19"E 76°54'01.20"E 76°54'02.08"E 76°53'59.07"E

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Sr. Name of Length X Width Area in Upset Taluka Sand plot Gat No along the river bed Brass BP- 1 BP-2 BP- 3 BP- 4 No. River Bed X Depth(Mtr) Ha. Price (Rs) 19°21'20.20"N 19°21'12.11"N 19°21'12.09"N 19°21'20.18"N 38 Parbhani Sambar-1 Purna 349-352 250x20x0.50 0.50 883 19,68,207 76°53'17.87"E 76°53'17.02"E 76°53'17.71"E 76°53'18.55"E 19°22'23.53"N 19°22'31.55"N 19°22'31.65"N 19°22'23.62"N 39 Parbhani SawangiKh. Purna 10-13,21-27 250x20x0.50 0.50 883 19,68,207 76°53'31.10"E 76°53'29.75"E 76°53'30.48"E 76°53'31.78"E 19°49'03.58"N 19°49'05.86"N 19°49'07.56"N 19°49'5.27"N 40 Jintur Wazar Bk.-1 Purna 466,469,470,472,480,582 250x50x0.50 1.25 2208 49, 21,632 76°32'30.62"E 76°32'22.38"E 76°32'22.37"E 76°32'30.61"E 19°49'14.40"N 19°49'20.03"N 19°49'21.26"N 19°49'15.63"N 41 Jintur Wazar Bk.-2 Purna 673,674,677,678,681 250x50x0.50 1.25 2208 49, 21,632 76°32'15.36"E 76°32'09.17"E 76°32'10.28"E 76°32'16.48"E

LIST OF PROPOSED SAND GHAT (YEAR 2019 -2020)

Total Auction able sand Quantity Location Sr. Name of Name of Area Taluka Survey No./Gut No. No. Village River Quantity Length Width Depth (Ha) Lat Long (Brass) Basmat 1. Savangi Bu. Purna 1,3,367,368,360 580 25 0.5 2562 1.45 N19022’50.1” E76053’34.3” Basmat Purna 2. Dhavulgaon 1,3,4,8,9,13,14,15,211,212 594 30 0.5 3148 1.78 N19023’19.9” E76054’06.2” Basmat Purna 3. Mategaon 2,3,4,220,222 558 29 0.5 2859 1.62 N19024’7.1” E76054’33.4” Basmat Purna 4. Parli 3,45,35,63,58,342 532 25 0.5 2350 1.33 N19024’55.0” E76055’11.5” Basmat Purna 5. Bramhangaon 9,8,7,1,114 482 25 0.6 2555 1.21 N19021’45.8” E76053’34.1” Purna 6. Aundha Na. Bhagwa 53,54,55 374 32 0.5 2114 1.19 Aundha Na Purna 7. Takalgavhan 13,14,15,16,17,18 408 26 0.5 1874 1.06 N19028’46.4” E76056’39.8”

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211,212,213,214,06,10,11, Aundha Na Purna 8. Anjanvadi 20,22,207,208,209 516 38 0.5 3464 1.96 N19031’03.9” E76057’42.0” ,210,215,216,217,218 Aundha Na Purna 9. Nandkheda 3, 4, 5 576 35 0.5 3562 2.01 N19027’48.5” E76055’50.1” Aundha Na Purna 2,18,255,252, 10. Nalegaon 460 30 0.4 1950 1.38 N19028’34.5” E76056’21.2” 253,24,233,232,231 Aundha Na Purna 404, 403, 405, 416, 417, 426, 427, 11. Aajarsoda 350 35 0.4 1657 1.22 N19026’45.6” E76055’15.3” 430, 435, 466, 437, 467, 474, 476 Aundha Na Purna 13, 21, 25 To 31, 284, 287 To 290, 12. Tapovan 580 35 0.8 5738 2.03 N19026’39.5” E76055’15.0” 476 Aundha Na Purna 13. Matha 291, 292, 293, 298, 312, 313, 314 545 30 0.4 2310 1.63 N 19043’05.8” E 77008’59.5” 347, 348, 349, 355, 364, 365, Aundha Na Purna 14. Anakhali 366, 367, 322, 376, 374, 390, 372, 380 30 0.5 2014 1.14 N19029’30.2” E76056’53.6” 396, 400 Purna 4,5,6,7,46,48,47, 15. Aundha Na Pota Bu. 435 30 0.5 2305 1.3 N19029’12.8” E76056’51.8” 50,53,55,56,57,58

16. Kalmanuri Chafnath Kayadhu 54,55,56,58 400 25 0.6 2120 1 N19036’1.5” E77014’32.7” Kalmanuri Kayadhu 17. Nandapur 405,406,422,426 465 25 0.5 2054 1.16 N19035’26.5” E77018’16” Kalmanuri Kayadhu 18. Sodegaon 440,441,404,391 490 22 0.5 1905 1.08 N19035’53.0” E77015’23.3” Kalmanuri Kayadhu 19. SavangiBhu 38,55,56,59,61,62,64,65 623 18 0.5 1981 1.12 N19036’15.6” E77013’33.4”

Kalmanuri Salegaon Kayadhu 20. 186,187,188 510 20 0.5 1802 1.02 N19036’17.4” E77016’30.9” (West) Kalmanuri Kayadhu 21. Kondur 140,141,142,143,144,145 700 19 0.5 2350 1.33 N19034’01.2” E77019’10.4” Kalmanuri Kayadhu 22. DigresT.Ko, 34,9/1,8/2,89,89/1,88/1 800 15 0.5 2120 1.2 N19034’29.5” E77018’59.7” Kalmanuri Kayadhu 23. DongargaonPul 16,18 565 18 0.5 1797 1.02 N19034’01.7” E77023’46.7” Kalmanuri Kayadhu 24. Sapli 4,5,6,7,8 530 20 0.5 1873 1.06 N19033’36.5” E77022’10.5”

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Kalmanuri Kayadhu 25. Shevala 8,19 570 20 0.6 2417 1.14 N19032’34.7” E77026’21.0” Kalmanuri Kayadhu 26. Yegaon 43,45 585 21 0.5 2170 1.23 N19032’40.0” E77026’10.1” Kalmanuri Kayadhu 27. Primpri Bu. 197,196,195,194,193,199 560 18 0.5 1781 1.01 N19033’26.3” E77025’36.8” Kalmanuri Kayadhu 28. Kasvedhavanda 56,57,38/2,39,40,41,42,43,48 731 18 0.6 2790 1.32 N19033’08.40” E77021’34.5” Kalmanuri Kayadhu 29. Kanhegaon 6,26,27 490 22 0.5 1905 1.08 N19030’25.0” E77026’47.5” Kalmanuri Kayadhu 30. Chikhli 3,2,1,31,32/1,34 530 21 0.5 1966 1.11 N19029’44.8” E77027’58.2”

226, 234, 235, 237, 238, 31. Aundha Na. Pur Kayadhu 380 25 0.4 1343 0.95 239, 229, 230, 231, 233 266, 265, 269, 271, 273, 274, 32. Hingoli Hingni Kayadhu 486 26 0.6 2679 1.26 N19037’59.4” E77011’54.70” 314, 330, 329, 326, 311, 312, 314

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CHPATER -4 DETAILS OF ROYALTY OR REVENUE RECEIVED IN LAST THREEYEARS

The detail of royalty collection from the financial year 2016-17 to 2018-19 and for April – May 2019 is asfollows:

LIST OF DETAILS OF ROYALTY OR REVENUE RECEIVED IN LAST THREE YEARS

Year Sand Stone/ Boulder Murrum Soil S. No. Royalty/ Revenue (In Lakhs Rs.) 1. 2016 -2017 224.16 1098.56 142.17 101.44 2. 2017-2018 104.27 1817.98 113.15 187.85 3. 2018-2019 -- 874.00 1552.00 15.20 4. 1-04-2019 93.31 62.49 142.65 -- To 31-05-2019

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CHPATER -5 DETAILS OF PRODUCTION OF SAND OR MINOR MINERALIN LAST THREE YEARS

The details of production of sand or Bajri or minor minerals in last three years are as follows.

PRODUCTION DETAILS FOR LAST THREE YEARS

S. Year Sand Stone/ Boulder Murrum Soil No. Production (in Brass) 1. 2016 – 2017 12963 274640 35542 63400 2. 2017 – 2018 7395 454495 28287 117406 3. 2018 - 2019 218500 355000 3500

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CHPATER -6 PROCESS OF DEPOSITION OF SEDIMENTS IN THE RIVERS OFTHE DISTRICT

The mineral potential is calculated based on field investigation and geology of the catchment area of the river/ streams. As per the policy of the State and location, depth of minable mineral is defined. The area for removal of mineral in a river or stream can be decided depending on geomorphology and other factors, it can be 50% to 60% of the area of a particular river/stream, e.g. in river mineral constituents like sand up to a depth of three meter are considered as resource mineral. Other constituents like clay and silt are excluded as waste while calculating the mineral potential of particular river/stream.

The specific gravity of each mineral constituent is different. The percent of mineral constituent like boulder, river Bajri, and sand also varies for different river and streams. While calculating the mineral potential the percentage of each mineral constituent is taken as, Sand 25- 30% and 5- 10% for silt and clay.

The quantum of deposition varies from stream to stream depending upon factors like catchment lithology, discharge, river profile and geomorphology of the river course. There are certain geo- morphological features developed in the river beds such as channel bar, point bar etc. where annual deposition is more even two to three meters.

PROCESS OF DEPOSITION:

Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water and/or by the force of gravity acting on the particles. Sediments are most often transported by water. Sediment is transported based on the strength of the flow that carries it and its own size, volume, density, and shape. Stronger flows will increase the lift and drag on the particle, causing it to rise, while larger or denser particles will be more likelyto fall through the flow.

Deposition is the processes where material being transported by a river is deposited. Deposition occurs when a river loses energy. This can be when a river enters a shallow area (this could be when it floods and comes into contact with theflood plain) or towards its mouth where it meets another body of water.

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Deposition is the geological process in which sediments, soil and rocks are added to a landform or land mass. Wind, ice, and water, as well as sediment flowing via gravity, transport previously eroded sediment, which, at the loss of enough kinetic energy in the fluid, is deposited, building up layers ofsediment. Rivers flood on a regular basis. The area over which they flood is known as the floodplain and this often coincides with regions where meanders form. Meanders support the formation of flood plains through lateral erosion. When rivers flood the velocity of water slows. As the result of this the river's capacity to transport material is reduced and deposition occurs. This deposition leaves a layer of sediment across the whole floodplain. After a series of floods layers of sediment form along the flood plain. MODES OF SEDIMENT TRANSPORT The sediment load of a river is transported in various ways although these distinctions are to some extent arbitrary and not always very practical in the sense that not all of the components can be separated in practice:  Dissolvedload  Suspendedload  Intermittent suspension (saltation)load  Washload  Bedload

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The sand deposits being an integral part of the dynamic river system to which it belongs. Therefore, as a part of natural cycle, the monsoon flow of every river carries with it replenishment of silt and washed out soil and clay from upstream areas in the catchment. This silt shall be removed during the sieving of sand before it is loaded into truck/tipper/trailer to carry to theconsumers.

Sand mining is critical to infrastructure development around the globe. Sand is an essential minor mineral used extensively across the country as a useful construction constituent and variety of other uses in sports, agriculture, glass making (a form of sand with high silica content) etc. The rivers are the most important source of Sand. It acts as source of transportation and deposition of sand etc.

ANNUAL REPLENISHMENT OF MINERAL IN RIVER BED AREA/ SEDIMENTATION:

The deposition in a river bed is more pronounced during rainy season although the quantum of deposition varies from stream to stream depending upon numbers of factors such as catchment, lithology, discharge, river profile and geomorphology of the river course where annual deposition is one meters, but it is noticed that during flood season whole of the pit so excavated is completely filled up and as such the excavated area is replenished with new harvest of minerals.

In order to calculate the mineral deposits in the stream beds, the mineral constituents have been categorized as clay, silt, sand, Bajri and boulder. However, during present calculation, the waste material i.e. silt which varies from 10 to 20% in different streams has also been included in the total production. Further the Survey of India Topo-Sheets are used as base map to know the extent of river course. The mineral reserves have been calculated only upto 1m depth although there are some portions in the river beds such as channel bars, point bars and central islands where the annual deposition is raising the level of river bed thus causing shifting of the rivers towards banks resulting in to cutting of banks and at such locations, removal of this material upto the bed level is essential to control the river flow in its central part to check the bank cutting. While calculating the mineral potentials, the mineral deposits lying in the sub- tributaries of that particular stream/river has not been taken into consideration. Since these mineral deposits are addingannually.

Sedimentation is generally considered by geologists in terms of the textures, structures, and fossil

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DISTRICT SURVEY REPORT-HINGOLI content of the deposits lay down in different geographic and geomorphic environments. The factors which affects the “Computation of Sediment”:

 Geomorphology & Drainage Pattern: The following geomorphic units plays importantrole: . StructuralPlain . StructuralHill . StructuralRidge . Denudation Ridge &Valley . Plain &Plateau . Highly Dissectedpediment . Undissectedpediment  Distribution of Basin Area River wise  Drainage System/Pattern of the area, Rainfall & Climate: Year wise Rainfall data

REPLENISHMENT CALCULATION OF SAND GHAT

The Joint Survey carried out by Geologist of GSDA, Hingoli along with District Mining Officer and concerned Tehsildar has estimated the depth and area of each sand ghat. Details of the survey are provided in followingtable:

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As per GSDA, Hingoli As per Joint Survey (Reported in Sand Ghats S. Name of Sand Ghat Survey Certificate) No. 2017-2018 2018-2019 2019-20 Sand Layer Sandexcavat Sand Sand Sand Proposed sand in m ion in m Layer excavation in Layer excavation in m in m m in m 1. Kherda 2.30 0.30 2.30 0.30 ## ## 2. Digras T. Ko. 2.50 0.50 2.40 0.40 2.50 0.50 3. Durgdhamani 2.30 0.30 2.30 0.30 ## ## 4. Sawangi Bhu. 2.40 0.40 2.40 0.40 2.50 0.50 5. PotaKhu. 2.20 0.20 2.40 0.40 2.50 0.50 6. Hingani # # 2.30 0.30 2.60 0.60 7. Sapali # # 2.30 0.30 2.50 0.50 8. Salegaon 2.30 0.30 2.30 0.30 2.50 0.50 9. Pimpri Bu. # # 2.40 0.40 2.50 0.50 10. Pota Bu. 2.20 0.20 2.30 0.30 2.50 0.50 11. Ajarsonda # # 2.40 0.40 2.40 0.40 12. Sewala # # 2.40 0.40 2.60 0.60 13. Nalegaon # # 2.30 0.30 2.40 0.40 14. Pur 2.30 0.30 2.30 0.30 2.40 0.40 15. Kondhur # # 2.50 0.50 2.50 0.50 16. Ankhali 2.40 0.40 2.30 0.30 2.50 0.50 17. DongargaonPul 2.40 0.40 2.40 0.40 2.50 0.50 District Survey Report-Hingoli Page 35

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As per GSDA, Hingoli As per Joint Survey (Reported in Sand Ghats S. Name of Sand Ghat Survey Certificate) No. 2017-2018 2018-2019 2019-20 Sand Layer Sandexcavat Sand Sand Sand Proposed sand in m ion in m Layer excavation in Layer excavation in m in m m in m 18. Anjanwadi 2.30 0.30 2.30 0.30 2.50 0.50 19. Bhagwa 2.30 0.30 2.40 0.40 2.50 0.50 20. Chimegaon 2.30 0.30 2.40 0.40 ## ## 21. Chikhli 2.30 0.30 2.30 0.30 2.50 0.50 22. Tapowan 2.20 0.20 2.30 0.30 2.80 0.80 23. Daregaon 2.20 0.20 2.20 0.20 ## ## 24. Matha # # 2.30 0.30 2.40 0.40 25. Chafnath 2.30 0.30 2.30 0.30 2.60 0.60 26. Kanhegaon 2.40 0.40 2.30 0.30 2.50 0.50 27. Ban 2.40 0.40 2.40 0.40 ## ## 28. WazarKh. 2.40 0.40 2.40 0.40 ## ## 29. BrahmangaonKh. 2.40 0.40 2.40 0.40 2.60 0.60 30. Dhawalgaon 2.50 0.50 2.50 0.50 ## ## 31. Mategaon 2.50 0.50 2.50 0.50 ## ## 32. Parli 2.50 0.50 2.50 0.50 2.50 0.50 33. PimpalgaonKute 2.60 0.60 2.60 0.60 ## ## 34. Sawangi Bk. 2.60 0.60 2.60 0.60 2.50 0.50 35. SonaTarfHatta 2.50 0.50 2.50 0.50 ## ##

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# Not proposed

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CHPATER -7

GENERAL PROFILE OF THE DISTRICT

Hingoli is situated at the northern part of Marathwada in Maharashtra. Borders of Hingoli are surrounded by Akola and Yeotmal in northern side, Parbhani in Western side and Nanded at South-Eastern side. The district came into existence by division of Parbhani district on 1st May, 1999. Latitude of Hingoli district is 19.43 N and Longitude is 77.11 E. The geographical area of the district is 4526 Sq. kms; which is 1.47% of area of the Maharashtra State. Majority of districts population is engaged in agricultural activities and there is little industrialization in the district. Out of 12 main Jyotirling in the country, one of the AundhaNaganathJyotirling situated in thedistrict.

Hingoli district comes under Aurangabad Administrative Division. The district of Hingoli consists of 5 tehsils, namely, Hingoli, Kalamnuri, Sengaon, Aundha and Basmath.

At the district level the collector is the Administrative Head, while the Tahsildars of each tahsil run the administration as per collector‟s instruction. The ZillaParishad of the district is responsible for implementation of rural development programme.

The Sengaon, Hingoli and Aundha tehsils of the district are surrounded by small hills. The district is 600 meters high from sea level.

DISTRICT AT A GLANCE:

S. No. Particulars Statistics 1. GENERAL INFORMATION Geographical Area 4526 Sq.km Talukas 05 Villages 707 Grampanchayat 563 Population (Census, 2011) 11,78,973 Normal Annual Rainfall 824.4 mm 2. GEOMORPHOLOGY Major Physiographic unit Ajintha Hills Major Drainage Kayadhu, Purna, Painganga 3. SOIL TYPE Black Cotton Soil 4. GEOLOGY Basaltic Deccan Trap 5. HYDROGEOLOGY Water Bearing Formation Fractured, Jointed, Vesicular, & Weathered Basalt. Ground Water Quality Drinkable however localized fluoride contamination aquifer and nitrate contamination in some parts of urban areas of Hingoli town and localized places in ruralareas.

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CLIMATIC CONDITIONS:

The meteorology has no direct impact on the river sand. The atmospheric temperature varies between the lowest of 24.50C & the maximum of 43.50C. In winter the minimum will be 12.60C with a maximum of 350C. The annual atmospheric temperature varying between 200C & 290C will have no effect on the river sand or riverwater.

Wind speed, another metrological factor is at an average of 3 kms to 5 kms/hr and has no effect on the sand lying immersed in the river basin.

During the monsoons the average rainfall is 824.40 mm when the river water flows at a high speed shifting the coarser from medium to fineparts.

FORESTS:

The total area under forest is about 37700 hectares, which is about 7.96% of the district‟s geographical area. The major forest area in the district is in Aundhataluka which is about 10432 hectares. The forest produce includes Beedi leaves, gum, honey, etc.

Forest resources contribute significantly to the economy of district. Most of vegetation in district are Sag, Dhawada, Aian, Khair, Mahua and Tembhurni are the populated trees in district. Whereas raj, rosha are the grass verity which found in good quantity in district. Main resources of forest are Tendupatta, Dink and seasonable collection of Charoli from forest. Main resources of forest are Tendupatta, Dink and seasonable collection of Charoli fromforest.

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DEMOGRAPHIC FEATURES OF THE DISTRICT:

POPULATION PROFILE:

The study area comprises of 711 villages of Hingoli District. The total population of the Hingoli District is 1,177,345 accommodating in households 228,271 with an average households size of approx. 5 members per family

GENDER DISTRIBUTION:

The males in Hingoli District constitute 51.50% and females constitute 48.50%. The gender ratio of the study area is 942 per thousand male.

LITERACY PROFILE:

The average literacy rate of Hingoli District is 67.16% as per Census of India, 2011. The male literacy is 74.31% with respect to male population and the female literacy is 59.57% with respect to female population. The literacy gap between male & female is approx. 14.74%. There are 32.84% people in our study area is illiterate.

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OCCUPATIONAL STRUCTURE:

Occupational structure of the workforce indicates the economic activity of the region. The occupational patterns include cultivators, agricultural labourers, and household industry workers. The work participation rate is 48.34% in which males are 54.58% with respect to the male population and females are 41.73% with respect to the female population. The employment rate in Hingoli District for main workers, marginal workers and non-workers are as follows:

 The Main workers constitute 90.37% in which male worker’s participation is 93.18% with respect to the male working population whether as female worker’s participation is 86.47% with respect to the female working population.  The Marginal workers constitute 9.63% with the male workers of 6.82% with respect to the male working population and female workers of 13.53% with respect to the female workingpopulation.  The Non Workers constitute 51.66%; and there is distribution of men 45.42% with respect to the male population and women 58.27% with respect to the female population.

DEMOGRAPHIC PROFILE OF SC & ST:

The total population of Schedule Caste in Hingoli District is 182,565(15.51%) in which 51.15% is male and 48.85% is female. The total population of Schedule Tribes in Hingoli District is 111,954 (9.51%) in which 51.52% is male and 48.478% is female.

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INDUSTRIAL AREA (MIDC):

Hingoli MIDC has developed the Hingoli Industrial Area, with the objective to attract industrialists and local entrepreneurs to set up industries and invest in the region. The industrial development will also attract foreign direct investments in the region. MIDC has provided the best possible infrastructure to facilitate industrial development and every assistance is provided for theirgrowth.

Hingoli Industrial Area is situated on the Hignoli-Aundha-Parbhani State Highway which connects to all the major road networks of the state and is very close to the Hingoli city. The nearst railway station is at Hingoli which is about 8 kms from the Industrial Area.

DETAILS OF THE INDUSTRIAL AREA:

Particulars Details Total area acquired 204.90 Hectares Area developed 41.11 Hectares Nos of plots allotted 79 Nos. ( 31.22 Hectares) Unit in production 16 Nos. Unit under construction 2 Nos. Plots available for allotment 59 Nos. Land available for allotment 9.89 Hectares Source: http://trimbakeshwar.in/maharashtra/Hingoli/Hingoli-MIDC.aspx

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CONNECTIVITY:

RAILWAY:

Hingoli Railway Station is a railway station on Purna-Akola section of Hyderabad (HYB) Division of South Central Railway (SCR). After Divisional adjustments in 2003, which saw the bifurcation of Hyderabad Division, Hingoli now comes under Nanded(NED) Division of

SCR. Hingoli is well connected to cities like Hyderabad, Mumbai, Jaipur, Kota, Ajmer, Indore, New Delhi, Bhopal. Agra, Tirupati, Chandigarh, Amritsar and Sri Ganganagar.

The major railway stations near to Hingoli are Nanded railway station (84 km), Parbhani railway station (75 km) & Akola railway station (135 km) which are connected to all majorcities.

ROADWAYS:

The district of Hingoli is well served by a network of roads. There is a National Highway connecting Akola-Malegaon, Jahangir-Washim-Kanhergaon, Naka-Hingoli-Kalamnuri- Nanded- Deglur-Sangareddy-Hyderabad named National Highway-161. Intra-city road transportation is good in Hingoli.

MINERALS:

There are no major minerals available in the district. However, sand & stones, which are required for construction of buildings, are available in the district.

In Hingoli district, the demand of sand (river borne collection) and of Bajri/Grit (river borne collection or through manufactured grit by stone crushers) is mainly met by the supply from Purna and Kayadhu river beds.

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Source: www.mapsofindia.com

ECONOMY:

Hingoli is predominantly an agricultural district. Sorghum is the main crop in both kharif and rabbi seasons and Wasmattaluka leads in its production. Cotton is another important cash crop in the district. Sugarcane is gaining popularity in the district as more and more land is being brought under its cultivation. Kalamnuri and Wasmattalukas being irrigated, sugarcane is grown in these talukas on a large scale. In addition, banana, grapes, chilli and garlic are alsogrown.

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CHPATER -8

LAND UTILIZATION PATTERN IN THE DISTRICT: FOREST,AGRICULTURE, HORTICULTURE, MINING ETC.

The land use / land cover pattern of any region is an outcome of natural and socio - economic factors and their utilization by man in time and space. Land is becoming a limited resource due to immense agricultural and demographic pressure. Hence, information on land use land cover and possibilities for their most advantageous use is essential for the selection, planning and implementation of land use schemes to meet the increasing demands for basic human needs and welfare. This information also assists in monitoring the dynamics of land use resulting out of changing demands of increasingpopulation.

The present land-use pattern is shown below.

S. No. Particulars Area Details (In Sq.km) 1. Area not available for cultivation 192 2. Other uncultivable land 294.2 3. Area under forest 192 4. Fallow land 595.6 5. New sown area 3253

LAND-USE PATTERN, DISTRICT (AREA IN SQ.KM)

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FOREST:

Forest resources contribute significantly to the economy of district. Most of vegetation in district are Sag, Dhawada, Aian, Khair, Mahua and Tembhurni are the populated trees in district. Whereas raj, rosha are the grass verity which found in good quantity in district. Main resources of forest are Tendupatta, Dink and seasonable collection of Charoli from forest. Main resources of forest are Tendupatta, Dink and seasonable collection of Charoli fromforest.

For details refer Chapter -7

AGRICULTURE:

Agriculture is a key sector in the Hingoli district. There are three harvesting seasons for crop farming, namely kharif, rabi and summer. Kharif is the main seasonal crop in the taluka. The kharif season commences from mid Juneupto the end of November. The major kharif crops are cereals likejowar, bajari (millet), maka (maize), and pulses like tur, mug, udid, oilseeds like soybeans, bhuimug, til, suryaful (sunflower) and cash crops like cotton.

Source: www.mapofindia.com

HORTICULTURE:

Hingoli district is under high Level of Production in Horticultural Crops - Horticulture level of horticultural development has found in thedistrict.

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HORTICULTURE CROPS – FRUITS:

Banana, Orange (Santra), Sweet Orange (Mosambi), Mango, Papaya, Anola

HORTICULTURE CROPS – VEGETABLES:

Tomato, Brinjal, Okra (Bhendi),Chilli

Mining:

There are no major minerals available in the district. However, sand & stones, which are required for construction of buildings, are available in thedistrict.

Available mineral resources in the district:

 Stone

 Murrum

 Sand

 Clay

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CHPATER -9 PHYSIOGRAPHIC OF THE DISTRICT

Hingoli is situated at the northern part of Marathwada in Maharashtra. Borders of Hingoli are surrounded by Akola and Yeotmal in northern side, Parbhani in Western side and Nanded at South-Eastern side. The district came into existence by division of Parbhani district on 1st May, 1999. Latitude of Hingoli district is 19.43 N and Longitude is 77.11 E. The geographical area of the district is 4526 Sq. kms; which is 1.47% of area of the MaharashtraState.

PHYSIOGRAPHY:

Hingoli district falls in the center part of state. It lies on the Deccan plateau, about 500 m above sea level. Kayadhu and Purnariver drained through some part of district. Paingangariver makes a boundary within Hingoli-Washim& which also denotes the boundary between Marathwada& Region. Entire District falls in Middle Godavari riverbasin.

District Hingoli is member of the of Maharashtra state. it lies in Godavari basin and falls under the Painganaga basin with Kayadhu-Purna sub-basin. Village Malhiwara is the highest point having 598 mts from msl of Hingolitahasil. While on the other hand 400 mts is lowest point which lies in Basmathtahasil of district. Malhiwara hill ranges separate the Kayadhu and Purna river basins. Due to erosion and weathering of adjacent hills and rock thick alluvium deposits founds in some places. In district Deccan trap having horizontal layers of basalt are predominant. No other major minerals are found in district.

GEOMORPHOLOGY:

The area represents a plateau with low to moderate relief and it has few mesas and buttes structures. The general slope of the district is towards south and southeast with general elevation of 450 m amsl. The predominant Malhivra hill range of the district divides Penganga and Kayadu basin.

The Black cotton or Regur type soil occurs in the district. It comprises of lime, Iron, Magnesium. The pH of soil is 8.36 and therefore it is of alkaline nature.

The district is well drained by river systems, which are dendritic type and have matured valleys. There are three main drainage systems viz: Penganga, Purna and Kayadu rivers.

The river Penganga originates from Ajanta hills in Buldhana. It enters in the district

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DISTRICT SURVEY REPORT-HINGOLI fromSengaonTalukatowardsnortheasterncornerandbymakingajorneyofabout 80.45 Kilometres in the district moves towards Yavatmal district. Isapur Dam is constructed on the river. It is one of the most important rivers of Deccan plateau and whole district of Hingoli falls in its greatbasin.

The direct tributary of the river is Kayadhu. This tributary rises from the hill ranges near Risodtaluka of Washim district. The length of the river in the district is 80.50 kms. It is a seasonal river, which dries up insummer.

The Purna River rises from Ajnata hill ranges. It enters in the district from Jalna district. After making a journey of nearly 100 kms, it moves towards Parbhani district. Yeldari and Sidheshwar dams are constructed on the river.

Source: GSDA, Hingoli

SOILS:

The Soils of the district are derived from the basaltic lava flows. Thickness of the soil cover is less in northern and western parts where ground elevations are higher and consequently soil regur, gravels, murum are transported down to lower regions through gravity, transported down to lower regions through gravity, water or winds. Soils in central, southern and eastern regions of the

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DISTRICT SURVEY REPORT-HINGOLI district near the banks of Penganga and Purna rivers are thicker. Here soils, ranging in depth from 1 to 2 m, are black and rich in plantnutrients.

CHPATER -10

RAINFALL: MONTH-WISE

In India, the year has been divided into four seasons.

 Winter Season: December toFebruary

 Summer Season: March toMay

 Monsoon Season: June toSeptember

 Post Monsoon Season: October toNovember

The climate of the district is characterized by a hot summer and a general dryness throughout the year except during the southwest monsoon season, which is from June to September while October and November constitute the post monsoon season. The winter season commences towards the end of November when temperatures begin to fall rapidly. December is the coldest month with the mean maximum temperature of 28.9° C, while the mean minimum temperature is 10.3 °C. From the beginning of March, the daily temperature increases continuously. May is the hottest month with the mean maximum temperature of 39.8 °C and the mean minimum temperature of 24.6° C. With the onset of the south-west monsoon by about the second week of June, the temperature falls appreciably. Except during the southwest monsoon season, when the relative humidity is high, the air is generally dry over the district. The summer months are the driest when the relative humidity is generally between 20 and 25 % in the afternoon. Winds are generally light to moderate with increase in speed during the latter half of the hot season and in the monsoon season. The winds flow predominantly from directions between west and north during the hot season. They are mostly from directions between southwest and northwest during the southwest monsoon season. They blow mostly from the directions between northeast and southeast during the rest of the year becoming southwesterly to north westerly in January and February. The normal annual rainfall over the district varies from 500 mm to 800 mm.

Rainfall data discussed in the table below is the mean rainfall (mm) received in Hingoli district during the year 2018.

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DISTRICT SURVEY REPORT-HINGOLI

MONTH WISE RAINFALL DATA OF (2019) OF HINGOLI DISTRICT

Normal Actual Rainy Month Rain Rain Days January 5.1 - - February 6.2 - - March 7.9 - - April 6.4 - - May 12.8 - - June 168.5 87.9 10 July 258.9 232.1 15 August 251 193.2 13 September 160.1 234.9 17 October 46.3 166.7 16 November 20.6 23.8 1 December 12.5 2.1 0 Total 956.3 940.7 72 Source: Agriculture Department, Maharashtra

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CHPATER -11 GEOLOGY AND MINERAL WEALTH GEOLOGY:

As district lies on part of Deccan Plateau, locally known as Ajanta Plateau, with slope towards southwest and southeast and has a varies topography consisting of hills, plains and undulating topography near river-banks. The district falls in a part of Godavari basin. The Ajanta Plateau comprises of low-lying hills forming water divide. Many of the tributaries to originate from the Ajanta Plateau.

Recent : Alluvium Upper Cretaceous- Basalt (Deccan Traps) Lower Eocene :

The geology of the district is composed of Deccan Traps. In general typical alternating layers of varying thickness of vesicular amygdaloidal basalt and massive basalt are observed everywhere. At places adjoining the river beds the local alluvium in variable thickness is observed.

Source: GSDA,

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HYDROGEOLOGY:

The groundwater is mainly augmented from dug wells and bore wells. The depth of the dug wells ranges from 8m to 18m, while for bore wells depth ranges from 50m to90m.

For irrigation generally dug wells are preferred. Horizontal boreholes are drilled in the contacts of two layers, in most of the wells, to increase the yield. The water level ranges from 3.50m in post monsoon period (winter season) to 9.00m in pre monsoon period (summerseason).

GROUND WATER RESOURCES:

Central Ground Water Board and Ground Water Survey and Development Agency (GSDA) have jointly estimated the ground water resources of Hingoli district based on GEC-97 methodology. As per the estimation, the total annual ground water recharge is 1084.22 MCM with the natural discharge of 54.21 MCM, thus the net annual ground water availability comes to be 1030.01 MCM. The gross draft for all uses is estimated at

380.07 MCM with irrigation sector being the major consumer having a draft of 362.44 MCM. The domestic and industrial water requirements are worked as 17.63 MCM. The net ground water availability for future irrigation is estimated as 632.30 MCM.

Stage of ground water development varies from 31.22% (Aundha) to 44.47 % (Kalamnuri). The overall stage of ground water development for the district is 36.90%. Taluka wise assessments indicate that out of 5 talukas, no 10 Talukas fall under “Over- Exploited”, Semi critical and Critical category, all the talukas fall under “Safe” category. Watershed wise, all the 23 watersheds fall under “Safe category”.

MINERAL RESOURCES:

There are no major minerals available in the district. However, sand & stones, which are required for construction of buildings, are available in thedistrict.

For more details refer Chapter 2.

DRAINAGE PATTERN AND SAND SOURCE:

The district is well drained by river systems, which are dendritic type and have matured valleys. There are three main drainage systems viz: Penganga River, PurnaKayadu Rivers. The applied lease area part of the River Penganga, Purna and Kayadu Rivers.

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Source: GSDA, Amravati

MINING:

The mineral resources of Hingoli district playing massive role in industrial, social and economic development of the district.

DETAILS OF RIVER OR STREAM AND OTHER SAND SOURCE OF THE DISTRICT:-

The rivers of the district bring out the sediment as bed load and suspended load during the monsoon period and post monsoon when the carrying capacity of river decreases it deposit the sediment as braided deposit, point bars, etc. these are the main source of sand in the district.

a) DISTRICTWISEDETAILOFRIVERORSTREAMANDOTHERSANDSOURCE:-

There are three main drainage systems viz: Penganga River, PurnaKayadu Rivers.

PURNA RIVER:

The Purna River is a major left-bank tributary of Godavari River originating in the Ajanta Range of hills in Aurangabad District, Maharashtra.The river lies in the rain shadow region of Maharashtra, on the Deccan Plateau, flowing through the districts

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DISTRICT SURVEY REPORT-HINGOLI of Aurangabad, Buldana, Jalna, Hingoli and Parbhani with a large catchment area measuring about 15,579 km2.This enormous catchment area is often tagged as a sub-basin of Godavari River and along with its tributaries forms a dendritic drainage pattern. It is a prime river in the Marathwada region of Maharashtra running for about 373 km before it confluences with Godavari River south of Purna city in the Parbhani district.Purna River flows from Southern part of Sengaon. It flows further south from Aundha and Basmattalukas.

KAYADHU RIVER:

This is also main river and flows through Sengaon, Hingoli, Aundha, Nagnath and Kalamnuri. It meets further to in .

PENGANGA RIVER:

Painganga River is the main river in the district. It flows in the northern region of the district. The river passes through Sengaon and Kalamnuritalukas.

b) AVAILABILITY OF SAND OR GRAVEL OR AGGREGATE RESOURCES :-

Purna, Kayadhu, and Penganga River is major sand source and in the district. The rivers of the district bring out the sediment as bed load and suspended load during the monsoon period and post monsoon when the carrying capacity of river decreases it deposit the sediment as braided deposit, point bars, etc. these are the main source of sand in the district.

c) EXISTING MINERAL LEASE OF SAND AND AGGREGATES :-

Refer to Chapter -3

DRAINAGE SYSTEM WITH DESCRIPTION OF MAIN RIVERS:

S. Area Drained (Sq. Name of River % Area Drained No. Km.) 1. Purna 114 2.52 2. Kayadhu 40 0.88 3. Painganga 92 2.03

SALIENT FEATURES OF IMPORTANT RIVERS AND STREAMS:-

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Total Length in the S. Name of River Altitude at district (in Place of Origin No. Origin Km) 1 Purna 149 Near Village Khorwad 471 2 Kayadhu 114 Near Village Kankarwadi 552 3 Painganga 108 Near Village Yeoti 488

METHODOLOGY ADOPTED FOR CALCULATING OF MINERAL POTENTIAL:-

The mineral potential is calculated based on field investigation and geology of the catchment area of the river/ streams. As per the policy of the State and location, depth of minable mineral is defined. The area for removal of mineral in a river or stream can be decided depending on geomorphology and other factors, it can be 50% to 60% of the area of a particular river/stream. Other constituents like clay and silt are excluded as waste while calculating the mineral potential of particular river/stream.

The specific gravity of each mineral constituent is different. While calculating the mineral potential, the average specific gravity is taken as 2.25. The percent of mineral constituent like boulder, river Bajri, and sand also varies for different river and streams. While calculating the mineral potential the percentage of each mineral constituent is taken as, Sand 25- 30% and 5- 10% for silt andclay.

The quantum of deposition varies from stream to stream depending upon factors like catchment lithology, discharge, river profile and geomorphology of the river course. There are certain geo- morphological features developed in the river beds such as channel bar, point bar etc. where annual deposition is more even two to three meters.

The details are given below:

Portion of Length of the Average Mineable the recommended width of the Area mineral S. recommended area for recommended recommended Potential No. Name of area mineral area for mineral (in metric River for concession for mineral concession tonne) mineral (inKm.) concession (in Sq. Mtr.) (60% of concession (In mt.) total (Ha) mineral Potential) 1 Purna 22.31 7.370 30.33 223100 182079

2 Kayadhu 19.77 9.415 20.76 197700 157756.5

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Total for 42.08 420800 339835.5 the District Note: Density of sand =1.6 ton/m3

MINERAL POTENTIAL IS CALCULATED IN FOLLOWING WAY:

MINERAL POTENTIAL:

Sand (MT) Total Mineable Mineral Potential (MT) 339835.5 339835.5 Annual Deposition (Consider 70% of potential minable sand mineral) 237884.85 237884.85

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References

1. CGWB GW Information Hingoli District.

2. http://krishi.maharashtra.gov.in

3. https://hingoli.nic.in/

4. https://www.gsi.gov.in

5. Secondary Data Collected from District Mining Office, Hongoli

6. https://gsda.maharashtra.gov.in

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