DISTRICT SURVEY REPORT,

DISTRICT SURVEY REPORT-2019 (Under Ministry of Environment, Forest & Climate Change, New Delhi

Notification Date 25-07-2018)

DEPARTMENT OF MINES & GEOLOGY GOVT. OF KARAULI

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INDEX POINT PARTICULARS NO.

1.0 INTRODUCTION

2.0 OVERVIEW OF MINOR MINERAL MINING ACTIVITY IN THE

3.0 GENERAL PROFILE OF KARAULI DISTRICT

4.0 GEOLOGY OF KARAULI DISTRICT

5.0 DRAINAGE OR IRRIGATION PATTERN OF KARAULI DISTRICT

6.0 LAND UTILIZATION PATTERN IN THE KARAULI DISTRICT

7.0 GROUND & SURFACE WATER SCENARIO OF KARAULI DISTRICT

8.0 CLIMATE & RAINFALL

THE LIST OF MINING LEASES IN THE KARAULI DISTRICT WITH LOCATION, AREA AND PERIOD OF 9.0 VALIDITY

10.0 DETAILS OF ROYALTY OR REVENUE RECEIVED IN LAST THREE YEARS

11.0 DETAILS OF PRODUCTION OF MINOR MINERAL IN LAST THREE YEARS

12.0 MINERAL MAP OF THE DISTRICT

13.0 TOTAL MINERAL RESERVE AVAILABLE IN THE DISTRICT

14.0 QUALITY/GRADE OF MINERAL AVAILABLE IN THE DISTRICT

15.0 USE OF MINERALS

16.0 DETAILS OF ECO-SENSITIVE AREA, IF ANY IN THE DISTRICT

IMPACT ON THE ENVIRONMENT (Air, Water, Soil, Noise, Flora & Fauna, Land Use, Agriculture, Forest ect.) 17.0 DUE TO MINING ACTIVITY

18.0 REMEDIAL MEASURES TO MITIGATE THE IMPACT OF MINING ON THE ENVIRONMENT

RECLAMATION OF MINED OUT AREA (BEST PRACTICE ALREADY IMPLEMENTED IN THE 19.0 DISTRICT, REQUIRMENT AS PER RULES AND REGULATION, PROPOSED RECLAMATION PLAN)

20.0 RISK ASSESSMENT & DIASASTER MANAGEMENT PLAN

DETAILS OF THE OCCUPATIONAL HEALTH ISSUES IN THE DISTRICT (LAST FIVE YEAR DATA OF 21.0 NUMBER OF PATIENT OF SILICOSIS & TUBERCULOSIS IS ALSO NEEDS TO BE SUBMITTED) PLANTATION AND GREEN BELT DOVELOPMENT IN RESPECT OF LEASES ALREADY GRANTED IN 22.0 THE DISTRICT

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1. INTRODUCTION: Karauli district is located in the eastern part of Rajasthan. It is bounded in the north by and Bharatpur districts, in the east by Dhaulpur district, south by state of and district in the west. It stretches between 26° 01' 27.02” to 27° 00' 11.61” north latitude and 76° 28' 34.98‟‟ to 77° 24' 12.00‟‟ east longitude covering an area of 4,985 sqkms. This district is part of four river basins namely „Gambhir River Basin‟, „Banas River Basin‟, „ River Basin‟ and „Parbati River Basin‟.

Karauli is one of the holiest City of as there are more than 300 temples. According to the ancient history, region of Karauli was under Matsya Kingdom before the 11th century. It is to be highly noted that Bijai Pal, a Jadon Rajput, founded the modern Karauli in 995. The local legends and Hindu scholars believe that he was the 88th in descent of Lord . On the other hand, historians and scholars cite that it was Maharaja Arjun Dev who founded the princely state of Karauli in 1348. It is to be remembered that till the 19th century, Karauli was an independent principality. In 1818, this region came under the direct rule of the Rajputana Agency.

Karauli district is administratively divided into five blocks. The following table summarizes the basic statistics of the district at block level. Sapotra block is the largest in area occupying about 1955 Sq.kms whereas the smallest block is spread over about 544 Sq.kms while population wise, block has the highest population and Nadoti has lowest population.

S.No BLOCK Population Area % of Total NAME (Based on (sq km) District Number of 2001census) Area Towns and Villages 1 Hindaun 347264 649.50 13.0 128

2 Karauli 288860 1227.80 24.6 204

3 Nadoti 126089 608.70 12.20 95

4 Sapotra 232513 1954.90 39.30 224

5 Todabhim 214939 544.10 10.90 150

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Fig. 1.1 Rajasthan Administration Map

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Fig. 1.2 Karauli District Administration Map

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2.OVERVIEW OF MINOR MINERAL MINING ACTIVITY IN THE DISTRICT: The mineral resources of Karauli district have played a great role in industrialization, social and economic development of the district as well as State Rajasthan.Karauli district is rich in minerals such as.

A. Masonry Stone. B. Silica Sand. C. China Clay D. White Clay E. Soap Stone F. Sand Stone G. Slate stone

H. Hand Mill Stone

I. Clay/Ordinory Clay/Brick Clay

3.0 GENERAL PROFILE OF DISTRICT: The importance of Karauli district, which is situated in the eastern part of Rajasthan, cannot be underestimated. It was established as 32nd district of the state on 19th July 1997 and this geographical part of the state is home to high diversity. The district has been divided into 6 administrative sub-divisions, while geographically the land area can be divided into three areas namely: Dang Area, Hilly, and Plainland areas.

There is a lot of cultural diversities in the Karauli district. It is culturally divided into two areas namely: Madh and Jagroti. An influence of Brij culture can be seen across the Karauli district. Fairs and festivals have been the medium of culture in this area.

The minerals found in this geographical area of the district are recognized regionally and globally. , Masalpur, Sapotara, Todabheem and Hindaun areas have reserves of various types minerals. Silica stone found here is used in large quantity in the manufacturing of glasses for vehicles, while the use of sandstone in the construction of historical and modern buildings describes the importance of the district.

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Green hilly ranges are splendour of Karauli district, while chirping and musical sounds of birds around waterfalls, lakes, and dams provide the picturesque environment. It‟s gorgeous palace walls and gates narrate the story of historical ups and downs, while attractive Chataris, historic forts and monuments document and portray the tale of its unbelievable glorious past.

Litterateurs and artists of this land have contributed immensely to the prestige and glory of the land through getting a national recognition to thoughts and sacraments of this area. Whereas sportsmen and soldiers in national service who were born and brought up in village environment of the land, also added prestige to their motherland. Presence of “Char Dham” in Karauli along with religious and communal peace is a unique example of eye-catching tourism splendour which is a god gift.

District Karauli falls under “Nizamat” of ancient regions of along with Hindaun and Gangapur of state. It was named Kalyanpuri by Yaduwanshi rulers. Karl Marx and Colonel James Todd had mentioned in their book about Karauli. Karauli state was merged with Matasya group in April 1949. It was merged with and became part of the United State of Greater Rajasthan. The announced creation of Karauli district which was carved out of five Tehsils of Sawai Madhopur on 1st March 1997. Notification of formation of Karauli district was issued on 15th July 1997 and then Chief Minister Shri Bhairo Singh Shekhawat inaugurated the district on 19th July 1997. According to the Census 2011 population of the district is 14, 58, 459 and its area is 5,043 Sq. Km. The main river of state, , separates it from Madhya Pradesh. Numerous Forts and Fortresses points to it's glorious history. Out of these forts, Timangarh, Untgiri, and Mandrayal tell the story of the medieval period of the country. The Timangarh fort remained under principality of Yadhuvansh. During the period from 1093 to 1159 King Timanpal, the powerful King of the dynasty, got the Timangarh fort constructed. There are numerous „Chataris‟ of historic legendary personalities still standing straight. The presence of relic evidences related to sculpture and architecture in Timangarh, Karauli, Hindaun etc indicate presence of magnificent temples in earlier times. Old remains are still available in King Mordhwaj‟s city Gadmora in the Karauli district.

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Karauli District, with population of about 14.6 lakh is Rajasthan's the 12th least populous district, located in the state Rajasthan in India. Total geographical area of Karauli district is 5524 km2 and it is the 11th smallest district by area in the state. Population density of the district is 264 persons per km2. There are 6 sub districts in the district, among them Hindaun is the most populous sub district with population of about 4.2 lakh and Mandrail is the least populous sub district with population of about 75 thousand.There are 3 cities in the district which comes under the district administration, those are - Hindaun, Karauli and TodabhimMunicipalities.

DEMOGRAPHICS

The district is home to about 14.6 lakh people, among them about 7.8 lakh (54%) are male and about 6.7 lakh (46%) are female. 53% of the whole population are from general caste, 24% are from schedule caste and 22% are schedule tribes. Child (aged under 6 years) population of Karauli district is 17%, among them 54% are boys and 46% are girls. There are about 2.6 lakh households in the district and an average 6 persons live in every family.

The majority of the population, nearly 85% (about 12.4 lakh) live in Karauli District rural part and 15% (about 2.2 lakh) population live in the Karauli District urban part. Rural population density of Karauli district is 228 and urban population density is 2347 persons per km2.

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4.0 GEOLOGY OF KARAULI DISTRICT: Geologically, the largest part of district is covered by thick mantle of soil, blown sand and alluvium. Karauli is a land locked district bounded by Dausa,Dhaulpur, Sawai Madhopur, and the Madhya Pradesh state. It extends over in the southeastern part of Rajasthan and falls in parts of survey of India topo-sheete nos. 54/B. Physiographically, the district is characterized by the northern extension of the great Vindhyan Plateau covering the south-easternpart of the district Geologically, the terrain comprises pre-Cambrian metamorphic igneous and sedimentary rocks belonging to pre-Aravallis Vindhyas. Alluvium and soil primarily confined to the vicinity of the Chambal, Moral, Gambhir, and Banas Rivers cover the area between the Great Boundary Fault and the hill ranges. Pre-Aravalli rock units comprising quartzites, micashists, gneisses and migmatities cover the north-western part of the district between tvan'cl west of . These rock units are uncomfortably overlain by quartzites and metavolcanics of .Formation of the Delhi Group. Rocks of Gwalior Formation comprising interlayered sequence of banded haematite jasper, quartzite. Limestone and intrusive delerite and occurring in east and south-east of Hindaun have been grouped under pre-Aravalli rock units on the basis of stratigraephy and structure. The different rock units of Karauli district show evidence of superposed deformation. The earlier major folds on north-east- south-west (NE-SW) to northnorth-east-south-south-west (NNE-SSW) axial plane

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have been affected by secondary fold system' on north-northwest south-south east (NNW-SSE) to north-west-south-east (NW-SE) and south-east axial plane. An alternate succession of sandstone and shele with intervening carbonate phase and their associated primary structures of Vindhyans reval a shallow marine environment of deposition with signs of mild tectonism. Similary, the alternate sequence of quartzite andphyllites within Delhi's essentially reflects stable shelf tectonic frameworks of sedimentation with alternate period. The quiescence and movement is followed by similar tectonic episodes of greater enteritis.

Quaternary alluvium occupies a large area of about 2453 sq. km. It is composed of silt, sand,clay, kankar and gravel and is deposited by major rivers and streams. It occupies the major partof Todabhim, Nadauti, Hindaun blocks underlained by Super Group of rocks(comprising of interbedded sequence of shale slate schist quartzite phyllite and limestone)separated with Vindhyan Super Group of formations (represented by Semri, , BhanderGroups consisting mainly of various types of Shales, Sandstones and Limestones) in entire east,south eastern part by the Great Boundary Fault. The extreme north-western stretch in small areais underlain by Delhi Super Group of rocks. The Delhi Super Group of rocks are foundunconformably overlying the mica schist and gneisses of Bhilwara Super Group. The AlwarGroup of rocks are folded forming the strike ridges. Conglomerates and conglomeratic quartzitesare exposed as narrow outcrop to the south of Todabhim.Talus and Scree are found in localpatches near hilly catchments having width from a few tens of metres to 500 metres andthickness from 40 to 55 m. Exploratory drilling has indicated a wide variation in thickness ofalluvium ranging from 10 m in west to 65 m in eastern part.

Geologically, the district lies under Vindhyan, Delhi and Bhilwara Super Groups. The eastern part of the district is separated from the western part by Great Boundary Fault. Thelatter consists of the rock formation of Bhander Group i.e. Sandstone, Shale and Limestone. The Delhi Super Group occupies the northwest part of the district which consist Quartzite,Schist of Ajabgarh and Alwar Group. A small isolated patch of Ranthambhor Group also occupies the center area of the district, which consists of Quartzite, Schist and Gneiss.

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Fig 1.3 Geological Map of District Karauli

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Mineral wealth of the District:Various minerals are found in Karauli district. Details of their occurrences are given below:

I. Silica Sand: The reserves of silica sand have been estimated to be in good account in the district. These reserves are only preliminary reserves and actual reserves would be much moreSufficient reserves of silica are available in Karauli and Sapotra tehsil. This stone is basically used in industry related to glass work. This is used 85 to 90 percent in glass and 10 to 15 percent in feldspar and limestone. The stones are found in the white and brownish colour which is used for making glass bangles and artifacts. These are not used at the local level and are sent to Delhi, Haryana, Uttar Pradesh, Uttranchal states after mining. The Mineral department has leased only 34 mines in the district, which provides employment to approximately 500 workers every day. The mines of Silica exists in villages - Ramapur, Atalpura, Richhoti, Khirkhida, Gairai, Dhaoreta, Ghoreti, Kadhai, Gothra, Mijhaura of the district. Mines work is done on a large scale with Ahasi India Limited Company of Khirkhida Village and Rajasthan sands and clays private limited in Mijhaura. Silica stone is liquefied after grinding by the crasher in glass factories which is used by converting it into different shapes. Colloidal silica is used for polish; this is sent to different cities of the state for the use of nail polish, boot polish.

II. China Clay: The clay is usually white to milky whitw in colour, but is occasionally stained reddish, yellowish and brownish. Clay content ranged from 37- 58% by weight. The clay has a water of plasticity of 32%.

III. Soapstone: Soapstone is mainly used in beauty products and it is found in white, light green and brown shades. A few mines are found in Nadoti and Todabhim areas of the Karauli District. It is also known as Soapstone. Apart from the beauty products industry, it is also used in paper and rubber industry as filler. Its mines are situated in Mora, Ghaat, Dhawaan, Dhauleta, Rewali, Pal and Jeetki villages in Karauli. This mineral after mining in the district in its original form and after crushing in crasher, is sent to the other cities and provinces of the state. Especially it is majorly supplied in the states of Delhi and Haryana. Mineral Department has leased 11 mines of “Soapstone” in the district, which provides employment to approximately 100 labourers per day.

IV. Clay: Two types of clay are found in Karauli – China clay and White clay. This

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mineral is used in ceramic industries and parties industries from which utensils, insulating equipments and toys are made. China clay and white clay are found in “Sapotra” area of the district.The Mineral department has issued mine lease for 9 places, including Narauli Dang Bholupura, Padampura, Bapoti, Kavtipura areas where the mining work is done and it provides employment to approximately 300 people per day.

V. Hand-mill stone: Since time immemorial hand-mill stone used for grinding grains were made with hard and strong stones but light-weight. Hand-mill stones of the Tali village in Masalpur area of Karauli District are not only famous in nearby areas but also in other states. This deep reddish coloured stone is known for its robustness. The Mineral department has leased 5 mines in Masalpur area which provides employment to 50 persons directly and 100 persons indirectly.

VI. Apart from this, Barytes mineral reserves found in Karauli. This mineral is used in digging oil wells, colouring and in the manufacturing of Vorium chemical. Reserves of this mineral are also found in Sapotra area. Reserves of white chalk are also found in the district. Mineral department has leased 2 mines of chalk, which provides employment to 50 persons per day. This is used for painting buildings, making chalks and making plaster of Paris.

5.0 DRAINAGE OR IRRIGATION PATTERN OF KARAULI DISTRICT: Physiography, Drainage and Soils: Physiography: The surface elevation of the district ranges from 223 to 525 m above mean sea level. Thesouthand south eastern part of the district comprises hilly terrain. Hills have generally NE-SW trend.Along the north-western border of the district between Todabhim and Raisana, a series of hillranges belonging to Pre-Aravalli and Delhi Super Groups of rocks exist. These are also trendingin NE-SW direction. Physiographically, the district is divided into three main parts as givenbelow. The general elevation of these hill lies between 384 and 525 m above mean sea level. The geomorphological divisions of Karauli district are shown in Table below.

Table Geomorphological Divisions of Karauli District 13 | P a g e

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Type Description Hilly terrain in south, Hilly terrains are mainly confined to Karauli and southeastern part and Sapotra blocks. The highestelevation is 525 m amsl extremenorth-western part. about 2.5 km. west of Chirawanda (in Nadauti block) Isolated hills in Major portion of district lying in northern, central alluviumplain in central part andnorth-western part, comprises alluvial plains with isolated hills. Development of ravines is seen inarea along Chambal river and its tributaries Alluvial plain in the Hindaun, Nadauti, and Todabhim form mainly plain northernpart. terrain. The generalelevation lies between 226 and 262 m amsl.

Drainage: The drainage system of the district is well developed. Main rivers in the district are Chambal, Gambhir & Morel and their tributaries. Chambal is the only perennial river and flows in northeasterly direction along interstate border of the district with Madhya Pradesh. Banas river making short boundary touches the boundary at Hadoti and joins. Morel river enters district 3 km south of Khera (in Sapotra block) and flows for a short distance in south direction and joins Banas river at Hadoti. Gambhir river originates from the hills near Karauli and follows a northernly course till Lapavali from where it takes turn and flows in the easterly direction. Near village Pali, it leaves the district and enters Bharatpur district.

Drainage in the rocky terrain is sub-parallel type, while in plain area, it is dendritic type. Thedrainage density in the district increases gradually towards south. Between Todabhim andNadauti, it is less than 0.30 km/sq.km. The drainage density around Nayagaon, Begrama andwest of Nadauti, is between 0.30 and 0.50 km/sq.km. Around Karauli, north of Sapotra, Hindaunand entire norht-eastern part of district, it ranges from 0.5 to 0.70 km/sq.km. In the southern partof district, the drainage density is more than 0.70 km/sq.km.

Gambhir River:- It emerges from the hills in Nadauti tahsil. It flows through the upper Hindaun and lower Todabhim tahsils flowing in the district for about 42km and then passes to Bharatpur district river Churahao, after flowing in Todabhim tahsil, joins river Gambhir. It leaves the district near village Pali. River Churahao, after flowing in Todabhim tahsil, joins it. Other villages on its bank in the district are Katkar, Samet, Kandrah, Saikhpur, Ankhera, Mudanpur, Lipaopli, Salempur, Tigria, and Deor 14 | P a g e

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besides Pali .The banks of the Gambhir are clearly defined in clay and Kankar soil and are much cut up by nullahs. The whole of the drainage of area ofthe hills to the west of Hindaun, from Todabhim as for as 6 Khera, falls m to this river.

Morel River:- It is a tributary of Banas.lt rises in the hills near Dhuli in . It is joined by the river Dhund and onwards by Khari River. The Khari River rises in Todabhim and lalsot ranges of hills, about 15km north of Bamanwas and after flowing south ultimately joins the Morel River.

Banas River:- It rises in the hills near Saimar in the Aravalli range, to the west of and enters Karauli district south and for a short distance forms the boundary with . In the hot months the riverbed is dry but it becomes treacherous after the rains. The banks are well defined and the river is on an average30ft.deep. The Banas river in Karauli flows in easterly direction till it receives the Morel river coming north-east and than goes south and finally meets the Chambal river at Rameshwargha in khandar tahsil. The Banas forms a common boundary between sub-divisions ofKarauli and Sawai Madhopur and its length in the district is nearly 106km. Village on the banks of Banas are Raipur, Barar, Kundel, Devalda, Goti, Baroda, Samoti and Hadoti.

Chambal River:-

The river Chambal forms the border between this district and the state of M.P on the south-eastern portion it enters the district near village Karamapura and after flowing for nearly 84km.Leavels it near village Saherh.Its bed is sandy and rocky and the Morel and the Banas are its important tributaries in the district. Village falling on its banks in the district are Banghera, Kachhi, Gunwala, Gota, Simath and Dans.

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Fig 1.4 Drainage and Topographical map

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Soil Profile: The general texture of the soils in the district ranges from deep medium heavy and black grayish dark drown soils to deep yellowish brown soils. There are four main types. Soils found in Bamanwas and parts of Gangapur and Swai Madhopur Panchayat Samities are deep medium to heavy textured and black, grayish or dark brown in colour. Todabhim, Hindaun and small part of Panchayat Samiti areas have deep light textured yellowish brown soils, while soils found in parts of Karauli, Sapotra tehsil and parts of Panchayat Samities are shallow to very shallow light brown. In parts of Karauli and Sapotra Panchayat Samitis, there are ravines caused by Chambal.

The soil types in Karauli district have been presented in table as given below:

Soil Area % Distribution (sq. km) Lies in parts of Todabhim and Nadauti blocks. These are derived from alluvium. They are non-calcareous, semi Older alluvium 145 2.88 consolidated to unconsolidated brown soils, loamy sand to sandy loam in texture. They are well drained and occupy gently sloping terrains. Occupies the parts of Nadauti, Karauli, Sapotra and Todabhim blocks. These are formed on the Bhilwara hills, and hill Lithosols and 2359 46.82 slopes. These soils are Shallow with Regosols of Hills gravels very near the surface, light textured, fairly drained, reddish brown in colour. Cultivation is restricted because of a limited root zone. Rests in parts of Nadauti, Hindaun, Todabhim, Sapotra and Karauli blocks. These are found along the flood plains of Chambal and Gambhir rivers and are Recent Alluvium 2535 50.30 developed on alluvium and covers about 2535 sq. km of district.The soil are deep, well drained, sandy loam to loam in texture and noncalcareous

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Fig 1.5 Geomorphological Map

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6.0 LAND UTILIZATION PATTERN IN THE KARAULI DISTRICT:

Area Area (%) S.No Particulars (Ha.)

1 Forest Area 172646 34.30 2 Agriculture Area 24110 4.80 3 Cultivated Land Area 202042 40 4 Non Agriculture Land Area 48867 9.70 5 Non- Cultivated Land Area 42575 8.40

7.0 GROUND & SURFACE WATER SCENARIO OF DISTRICT: Hydrogeology The ground water occurs both in unconsolidated and consolidated formations of the district as

A. Consolidated Formation Consolidated formation covers about 2495 sq. km (49.52%) of district and forms the principal aquifer in the district. It covers the southern, eastern and extreme north western strip of the district. The consolidated formations include sandstone and shale of Vindhyan Super Group and quartzites and schists of Delhi Super Group. The ground water occurs under unconfined condition in weathered and fractures portion of consolidated formations. These form generally poorer aquifer than alluvium and are tapped by open wells, dug cum borewells and bore wells.The ground water condition in various formations is described as below:

1. Vindhyan Sandstone and Shale: It encompasses about 2280 sq. km area and lies in southern and entire eastern part of the district. It forms the most prominent aquifer after alluvium in areal extent. The quartzitic sandstone occurring around Sapotra, Ramsar Bad and Khiskar in southern part of district are fine grained, compact and massive. These are highly resistant to weathering. Ground water occurs under unconfined conditions in fractures and jointed space. This forms poor aquifer and many wells in these got dry during summers. These Sandstones are horizontal to sub-horizontal and more

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or less tectonically undisturbed; as a result, vertical joints are very rare. Bhander sandstone occur as aquifer in southern and eastern part of the district around Bhankri, Machilpur and Langra. This is also resistant to weathering and has two sets of joints. Ground water in these occurs under phreatic conditions. The aquifer is tapped by open wells, dug cum borewells and tubewells/ borewells. In general, the diameter and depth of open wells varies from 2.5 to 3.5 m and 12 m to 30 m, respectively whereas depth of bore wells lies between 50 m and 210 m. The yield of open wells/ dug cum bore wells in majority of cases ranges from 20 to 70 m3/day, whereas discharge of borewells from 4.5 m3/hr to 22.50 m3/hr.

2. Quartzites and schists Quartzites and Schists of Delhi Super Group constitute poor aquifer and occur in a limited area in extreme north western strip of district (forming western part of Nadauti block) and covers an area of about 215 sq.km. Ground water occurs under unconfined conditions in weathered portion of rock units and in joints, fractures and other structural weaker zones. The extent of weathering is low and varies from 2 to 10 m in thickness. Yield of open wells depends on extent of weathering and the diameter of wells. Generally the yield of dug wells tapping these formation ranges from 30 to 70 m3/day.

B. Unconsolidated Formation The ground water occurs under unconfined to confined conditions in the unconsolidated formation (alluvium of Quaternary age) which is tapped through various ground water abstraction structures viz. dug well, dug cum borewell and tubewell.

1. Alluvium Quaternary alluvium occupying an area of about 2453 sq. km., forms aquifer in large part. It lies in central, northern, western parts of the district and in extreme south-eastern patch along Chambal River. It consists of silt, sand, clay, kankar and gravel. Out of these sandy clay and silty clay with kankar forms the most dominating constituent which generally occur in upper zone and is being tapped by dug wells. Gravel generally occurs at depth near the basement and these too generally do not form continuous layer. Quaternary alluvium forms most important aquifer which is being tapped by dug wells, dug cm borewells and tubewells. The ground water occurs under unconfined, semi-confined and 20 | P a g e

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confined conditions in this formation. Eleven exploratory wells, five slim holes and eight piezometers have been drilled as on March, 2014. The boreholes data revealed that the thickness of alluvium in major part of alluvial area varies from 10 m in western part to 65 m in eastern part. However, at Soroth thickness of alluvium reaches up to 91 m. The yield of dug wells in majority of cases varies from 40 to 150 m3/day. Higher yield is found where gravel bed is encountered. A few pumping tests have been conducted on open wells tapping alluvium. The data revealed that discharge of open wells lies between 9.06 m3/hr and 31.6 m3/hr. The draw down varies from 0.88 m to 3.76 m on 45 to 180 minutes of pumping. The time required for complete recuperation ranges from 150 to 240 minutes. The specific capacity ranges from 0.030 to 0.255 m3/min/m of draw down and optimum yield from 0.050 to 0.64 m3/min. The yield of open wells and dug cum borewells tapping alluvial formation varies from 175 to 900 lpm having drawdown from 0.609 to 12.17 m depending upon the locations. The specific capacity of wells ranges from 0.0383 to 0.1131 m3/m/m. The optimum yield (Karanjack‟s method) of wells varies from 106 to 374 lpm. The permeability of wells tapping quartzite ranges from 0.016 to 0.045 m/hr and maximum water inflow capacity from 8.61 to 32.99 m3/hr.

2. Talus and Scree The Talus and Scree forms important aquifer in the district. These generally occur along fault zone in foot hill regions. These occur in flanks of high hills mainly Delhi Quartzites ranges lying in north-western part of district in Nadauti and Todabhim blocks and in central western part of district in Sapotra and Karauli blocks. The width of the talus and scree zone varies from a few tens of metres to 500 metres. These are composed to fine to coarse sand with angular fragments of rocks together with loess. Exploratory drilling at Todabhim and Patoli indicated that the thickness of talus and scree deposit varies from 40 to 55 m. Yield of dug wells tapping this formation ranges from 100 to 1000 m3/day. The talus and scree forms aquifer around Gidani, Chirawada, Chainpura, Timawa and Pal in Nadauti Block; around Todabhim, Patoli, Bhandari and Parli in Todabhim Block and also to south west of Sapotra in Sapotra Block.

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Fig 1.6 Hydrogeology Map Of District Karauli

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Water Level Scenario The total number of hydrograph stations in the district is 26 including 17 dug wells and 9 piezometers. The depth to water level varies from 0.18 to 34.06 m during pre- monsoon 2014 and 1.33 to 34.06 m during post-monsoon 2014. According to the depth to water level map of pre monsoon 2014, water level ranges between 5 to 20 mbgl in the major part of block except some north western & central parts where it ranges between 20 to 40 mbgl and some south central parts where it is shallower upto 2 mbgl and even less. The water levels during post monsoon are almost similar to pre monsoon except the areas under 5 to 10 mbgl and 2 to 5 mbgl has increased

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Analysis of long term water level data of selected hydrograph stations for the last ten years (2005-2014) indicates that most of the selected representative wells from each block have shown rising water levels. The Badh Kamla station of Hindaun Block, Keladevi station of Karauli Block and Langra station of Sapotra Block have shown water level rises of 0.14, 0.06, 0.07 m/year, respectively. A very small water level falls have been seen at Karanpura station of Todabhim Block and Nadauti station of Nadauti Block during this period. The long term trends of selected stations are given below in Table 3 and hydrographs for these are given in figure as below.

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GROUND WATER QUALITY: The ground water is alkaline type having pH value more than 7. According to ground water chemical quality data for Premonsoon 2014, the electrical conductivity value ranges from 550μmhos/cm at 25°C (at Mamachari in Karauli Block) to a maximum of 6999 μmhos/cm at 25°C (at Sahar in Nadauti Block). However, in general it varies from 500 to 5000 μmhos/cm at 25°C. In major part of all the blocks, the electrical conductivity between 750 and 1500μmhos/cm at 25°C is found. And in another larger part, it varies between 1500 to 3000μmhos/cm at 25°C except few western areas the block. EC value ranging between 2000 and 3000 is constituted by 11% of the samples and 20% of stations rest beyond 3000 μmhos/cm at 25°C occupying the south western part of Hindaun Block, southern part of Nandauti Block, some western part of Karauli Block and northern part of Sapotra Block.

The ground water in shallow aquifers is alkaline type having pH value more than 7. The electrical conductivity value ranges from 280 μmhos/cm at 25°C (at Atewa in Karauli Block) to a maximum of 8400 μmhos/cm at 25°C (Bardala in Nadauti Block). However, in general it varies from 500 to 5000 μmhos/cm at 25°C. In major part of all the blocks, the electrical conductivity between 750 and 3000 μmhos/ cm at 25°C is found. Electrical conductivity less than 750 μmhos/ cm at 25°C is found in major part of Nadauti block and locally in Todabhim, Hindaun, Karauli and Sapotra blocks.The isolated patches falling in Nadauti, Todabhim and Hindaun blocks, have been noticed between 3000 and 5000 μmhos/ cm at 25°C electrical conductivity values. Electrical conductivity more than 5000 μmhos/ cm at 25°C is observed in isolated pockets lying in southern part of Nadauti block (Figure 13). EC more than 3000μmhos/cm at 25°C is constituted by 12% of ground water samples analyzed. The Nitrate content ranges from 2 ppm (minimum at Sai Markarpura in Karauli Block) to 571 ppm (miximum at Sahar in Nadauti Block). However, in general it lies between 10 ppm and 268 ppm. The analysis of data reveals that 66% of water samples analyzed fall within acceptable limit i.e. 45 ppm of drinking water standards and 34% beyond the limit which is not relaxable. The nitrate concentration is noticed within permissible limit of 45 ppm in major part of all the blocks. However, isolated pockets in Nadauti, Todabhim, Hindaun, Karauli and Sapotra Blocks, Nitrate concentration beyond acceptable limit of 45 ppm are

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observed. The Fluoride content mostly fall within permissible limit of 1.5 mg/l. However, it ranges in the district from traces to 6.45 mg/l (maximum at Gudachanderji in Nadauti Block). However, in general it falls between traces and 2.60 mg/l. The statistical analysis of data indicates that 82.03% of samples have Fluoride concentration within permissible limit i.e. 1.5 mg/l of drinking water standards and 18% beyond the limit. The Fluoride concentration less than 1.5 mg/l (permissible limit as per drinking water standards) is observed in major part of all the blocks in the district. However, isolated patches having Fluoride content more than 1.5 mg/l have been observed in northern part of Nadauti Block and in extreme part of Hindaun Block.

8.0 CLIMATE & RAINFALL: The climate of the district can be classified as semi-arid. It is characterized by very hot summers and very cold winters with poor rainfall during south-west monsoon period. In May and June, the maximum temperature may sometimes goes up to 48oC. The potential evapotranspiration rates are quite high, especially during May and June. The total annual potential evapotranspiration is 1502.6mm.The normal rainfall of district is 559 mm with 67.12% of humidity. The height of mean sea level for the district varies from 400 to 600 m amsl

The general distribution of rainfall across the district can be visualized from isohyets presented in the Plate – III where most of the district seems to have received rainfall in the range of 600-700 mm in year 2010. The total annual average rainfall is 646.8 mm based on the data of available blocks. Sapotra block received highest rainfall of 913.0mm whereas lowest was in Nadoti block (560.8mm). Maximum average annual rainfall recorded in Sapotra block about 705.2mm.

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Fig 1.7 Index Map of District Karauli

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TEMPERATURE: There is only one recently started meteorological observatory in the district at Karauli.Hence, in the following description the meteorological records of the observatories in the neighboring districts which provide a fair idea of the temperature and other meteorological conditions that prevail in the district have also been taken in to account. The period from March to June is one of continuous rise in temperature May and the first half June being the hottest part of the year. The mean daily maximum temp. In May is about 45.55° C and the mean daily minimum temp. Is about 25°C. Night temp. In June are little higher than May.The maximum temp. In May and June, may, on individual days, go unto about 47°C. The setting in of the south-west monsoon by about the third week of June lovers the temp. Somewhat but relief from teat is not marked because of the added discomfort from increase in humidity brought in by the south-west monsoon air. After the withdrawal of the monsoon by about the third week of September, days become hotter and in October a secondary maximum day temp. Is recorded. The nights become progressively cooler. Both day and night temp. Drop rapidly after mid-November till January, which is the coldest month, with a mean daily maxi. Temp. Of about 23° C and a mean daily minimum of about 3° C. In association with cold waves which sometimes affect the district in the wave of western disturbances.

HUMIDITY: Relative humilities are generally over 60% during the south-west monsoon during the rest of the year the air is dry. The driest part of the year is the summer season, when the afternoon relative humidity may be as low as 10 to 15%

WINDS Winds are generally tight to moderate with some strengthening in force in the summer and early south-west monsoon season. Winds blow mainly from the westerly and south-westerly directions during the south-west monsoon season. In the post-monsoon and winter months, winds are mostly from directions between west and north. In the summer season, the winds blow from directions between south-west and north-west.

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9.0 The List of Mining leases in the District with location, area and period of validity, with EC Details-

DETAIL OF EC Lessee Mineral Registrati Village/Tehs Total s.no lease no Expiry Date Name Name on Date il/District Area Capacity DATE (in MT) Durga Dhoreri / Silica 1 1/1992 Prasad 14-Mar-74 31-Jan-25 Karauli / 4.68 24-5-16 266760 Sand Agrawal Karauli Arvind Mamchari / Sandsto 2 1/2205 Kumar 2-Nov-06 1-Nov-56 Karauli / 2.56 #N/A #N/A ne Sharma Karauli Barrif / S.S. Silica 2/6/201 3 11/2004 17-Jan-08 16-Jan-58 Karauli / 4.78 140400 Mineral Sand 6 Karauli Atewa / Sandsto 4 12/2005 Bacchu 23-Oct-08 22-Oct-58 Karauli / 2.4 15-6-16 30000 ne Karauli Mr.Pankaj Atewa / Sandsto 2/6/201 5 138/2001 Kumar 28-Jul-03 27-Jul-53 Karauli / 1.17 19200 ne 6 Mittal Karauli Jhara / Jhara 2/6/201 6 14/1989 Granite 1-Apr-90 3-Jan-40 Nadauti / 1 30000 Granite 6 Karauli Masona Smt Talihil / rystone, 2/6/201 7 15/2009 Harpati 26-Mar-90 25-Mar-40 Hindaun / 1.27 1000 Millston 6 Devi Karauli e Bugdar / Ramesh Sandsto 8 157/2001 16-Jan-05 15-Jan-55 Mandrayal / 1.1 20-7-16 20000 ne Karauli Chobe Ki Masona Bhori Lal Gwari,Alwat rystone, 9 2/1981 Jain 6-Jul-61 31-Mar-25 Ki Gwari / 63.52 #N/A #N/A Sandsto Thekadar Sapotra / ne Karauli M/S Khirkhira / Silica 10 36192 Ganesh 1-Nov-03 30-Oct-53 Karauli / 5 20-7-16 91080 Sand Minirals Karauli Rajor / Fakeera Sandsto 2/6/201 11 20/2007 18-Aug-08 17-Aug-58 Karauli / 3.03 10000 Meena ne 6 Karauli Vshnu Bahadur Pur Sandsto 12 213/2001 Chand 16-Sep-04 15-Sep-54 / Sapotra / 1.17 NA NA ne Sharma Karauli

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Ashok Bahadur Pur Sandsto 13 22/2001 Kumar 19-Oct-06 18-Oct-56 / Sapotra / 1 NA NA ne Sharma Karauli Dhugarh / Ajay Pratap Masona 14 23/2006 3-Nov-10 2-Nov-60 Karauli / 1041 15-6-16 50000 Singh rystone Karauli Masona Bhadurpur,B Smt. rystone, ahadurpur / 4/5/201 15 25/1989 Mamtesh 10-Jan-80 20-Sep-29 33.28 60000 Sandsto Sapotra / 2 Bhardwraj ne Karauli Manch / Indra Masona 30-11- 16 27/1998 1-May-89 30-Apr-39 Karauli / 1 80000 Agrawal rystone 16 Karauli Purshotta Gunesara / Masona 17 32/2000 m Lal 6-Jun-03 5-Jun-53 Karauli / 1 NA NA rystone Goyal Karauli Masona Rajendra Bhadurpur / rystone, 18 332/1981 Bharadwra 20-Jan-82 19-Jan-32 Sapotra / 5.28 #N/A #N/A Sandsto j Karauli ne Masona Rangilal rystone, Karauli / 19 4/1993 26-Nov-59 31-Mar-25 10 #N/A #N/A Meena Sandsto Karauli ne Gopal Garh Haricharan Silica 2/6/201 20 27607 17-Nov-76 3-Jan-32 / Karauli / 4.58 142400 Lal Sand 6 Karauli Masona Pushpendr Bichpuri / rystone, 2/6/201 21 40/1998 a Kumar 27-Feb-99 26-Feb-49 Karauli / 2.03 30000 Sandsto 6 Sharma Karauli ne Masona Smt. Lotda / rystone, 3/8/201 22 48/2009 Koshllya 4-Oct-80 3-Oct-30 Masalpur / 18.54 50000 Sandsto 0 Devi Karauli ne Om Gunesari / Masona 23 5/2004 Bhaibav 20-Jan-07 19-Jan-57 Karauli / 1.01 23-5-16 85003 rystone Crushers Karauli Jahra / Duarkapras Masona 24 5/2013 11-Jan-13 10-Jan-63 Nadauti / 1 20-7-16 150280 ad Gupta rystone Karauli Asthal / Prakash Masona 25 50/2002 15-Nov-02 14-Nov-52 Karauli / 1 15-6-16 80000 Mali rystone Karauli

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Masona Rajor / Bharosi rystone, 26 54/1978 19-Sep-79 18-Sep-29 Karauli / 20.45 #N/A #N/A Devi Sandsto Karauli ne Bapoti / Ordinary 27 55/2006 Janki Devi 6-Jan-07 5-Jan-57 Sapotra / 1.14 15-6-16 28840 Clay Karauli Masona Piparani,Khu Mangi Lal rystone, nda / 28 7/1988 18-Jan-74 31-Mar-25 10 NA NA Agrawal Sandsto Masalpur / ne Karauli

Bardeh / Ghanshya Sandsto 2/6/201 29 7/2005 5-Dec-05 4-Dec-55 Mandrayal / 1.05 6000 m Sharma ne 6 Karauli

Masona Gurdeh / Jagan Lal rystone, 30 74/1998 23-Jan-99 22-Jan-49 Mandrayal / 3.01 20-7-16 50000 Meena Sandsto Karauli ne Masona Parashari / Kailaprasa rystone, 2/6/201 31 8/1999 17-Jun-02 16-Jun-52 Karauli / 4 10000 d Kumawat Sandsto 6 Karauli ne Aam Ka Dwrika Soapsto Jhara / 32 1/1989 Prasad 14-Dec-98 13-Dec-48 32.57 28-5-98 12000 ne Nadauti / Gupta Karauli

Manoharpur Kaptan Masona 2/6/201 33 10/2002 23-Jan-03 29-Jan-53 a / Karauli / 1 30000 Singh rystone 6 Karauli

Balveer Batda / Sandsto 34 10/2003 Prasad 23-Sep-03 20-Sep-53 Mandrayal / 1.72 20-7-16 20000 ne Sharma Karauli

Bugdar / Devkinand Sandsto 35 109/2001 11-Jun-03 10-Jun-53 Mandrayal / 1.23 20-7-16 10000 an Sharma ne Karauli

Bhartun / Masona 36 124/2004 Manju Devi 22-Dec-06 21-Dec-56 Sapotra / 1 20-7-16 77314 rystone Karauli

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Integrated Manohar Glass Silica Pura / 37 13/2005 6-Jun-86 5-Jun-36 4.95 #N/A #N/A Materials Sand Karauli / Limited Karauli

Mandi Bhat Ramprasad Sandsto 38 144/2001 10-Jul-03 9-Jul-53 / Sapotra / 1 NA NA ne Karauli

Rajesh Salempur / Masona 9/5/201 39 18/1995 Kumar 15-Apr-96 14-Apr-46 Sapotra / 1 30000 rystone 7 Gupta Karauli

Mahu,Karsai Masona ,Kalyani/Ma Tiwari rystone, mchari / 29-12- 40 19/1980 Jhumarlal 8-Jan-82 31-Jan-25 98.38 25225 Sandsto Mandrayal,K 10 Swrooplal ne arauli,Karaul i / Karauli

Khera / Sandsto 2/6/201 41 192/2001 Indrajeet 11-Nov-05 10-Nov-55 Masalpur / 1.89 10000 ne 6 Karauli Khera / Sandsto 2/6/201 42 193/2001 Indrajeet 11-Nov-05 10-Nov-55 Masalpur / 2.04 10000 ne 6 Karauli China Ramhatra / Indira Clay, 43 2/1990 1-Jan-93 31-Dec-42 Sapotra / 4.9 20-7-16 165360 Mittal Silica Karauli Sand

Masona Bhankari / Gopal Lal rystone, 2/6/201 44 21/1994 7-Dec-95 6-Dec-45 Mandrayal / 6.2 15000 Vyas Sandsto 6 Karauli ne

Gunesasri / Man Singh Masona 45 3/1997 30-May-98 29-May-48 Karauli / 1 NA NA Sain rystone Karauli

China Ramhatra / Indira Clay, 2/6/201 46 3/2000 24-May-04 23-May-54 Karauli / 4.09 50500 Mittal Silica 6 Karauli Sand

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Ms Jai Manoharpur Bhabhawa Masona 2/6/201 47 3/2002 26-Sep-02 25-Sep-52 a / Karauli / 1 50000 ni Stone rystone 6 Karauli Companey Bahrai / Laxmi Devi Sandsto 3/6/201 48 31/2004 10-Nov-04 9-Nov-54 Masalpur / 1.05 10000 Sharma ne 6 Karauli China Clay, Raghubansi Smt Ginii Silica 2/6/201 49 34/2006 6-Aug-09 5-Aug-59 / Karauli / 4.8 2980 Devi Sand, 6 Karauli White Clay Baloti / M/S Tajpur Masona 50 35/1988 4-Jul-69 31-Mar-25 Sapotra / 2.2 #N/A #N/A Minerals rystone Karauli

Batda / Ramkumar Sandsto 51 45/2002 30-Sep-05 29-Sep-55 Mandrayal / 1 20-7-16 26260 Sharma ne Karauli

M/S Shri China Kaunti Pura 52 5/1985 Ram Mince Clay, 3-Jan-86 2-Jan-36 / Sapotra / 4.61 29-6-15 279000 & Minirals Fireclay Karauli

China Deep Pura / Arihant Clay, 24.03.1 53 51/2007 27-Aug-08 26-Aug-58 Karauli / 4.6 25168 Minerals White 8 Karauli Clay Rundh Ka Hari Singh Sandsto Pura / 54 52/2006 26-Nov-10 25-Nov-60 1 20-7-16 40000 Meena ne Karauli / Karauli Masona Badri Lal rystone, 3/6/201 55 6/1992 31-Dec-93 30-Dec-43 - 0.99 20000 Chouhan Sandsto 6 ne

Pavan Chinayata / Masona 3/6/201 56 67/2005 Kumar 26-Oct-05 25-Oct-55 Hindaun / 1 30000 rystone 6 Agarwal Karauli

Naval Atewa / Sandsto 57 69/2002 Singh 27-Sep-03 27-Sep-53 Karauli / 1.12 15-6-16 10000 ne Gurjar Karauli

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Badreta / Silica 58 7/1970 Hind Khanij 5-Jan-77 4-Jan-27 Todabhim / 101.4 #N/A #N/A Sand Karauli

Masona Batda / rystone, 27-10- 59 7/1995 Manju Lata - 4-Apr-35 Mandrayal / 8.05 24710 Sandsto 16 Karauli ne

Manakhur / Ramveer Sandsto 3/6/201 60 75/2002 5-Dec-03 4-Dec-53 Mandrayal / 1.09 10000 Meena ne 6 Karauli

Masona Bahadurpur Jhoomar rystone, 61 76/1979 9-Nov-79 8-Nov-29 / Sapotra / 115.36 NA NA Lal Agarwal Sandsto Karauli ne

Jaimata Di Manoharpur Masona 2/6/201 62 8/2002 Stone 15-Jan-03 14-Jan-53 a / Karauli / 1 50000 rystone 6 Kreshar Karauli

Salempur / Prahlad Masona 9/5/201 63 80/1992 3-Sep-94 2-Sep-44 Sapotra / 0.53 30000 Gupta rystone 7 Karauli

Masona P-N. 16, Kanhaiya rystone, Halka No.- 1/0/190 64 87/1994 26-Aug-96 25-Aug-46 10 0 Lal Sharma Sandsto 13 / Karauli 0 ne / Karauli

Narendra Kheri / Masona 2/6/201 65 88/2004 Kumar 9-Dec-05 8-Dec-55 Todabhim / 1 45000 rystone 6 Sharma Karauli

Vinay Kheri / Masona 66 97/2004 Kumar 24-Dec-05 23-Dec-55 Todabhim / 1 20-7-16 90000 rystone Goyal Karauli

Smt Kanchanpur Sandsto 67 115/2004 Charan Bai 24-Aug-05 23-Aug-55 / Mandrayal 1.03 20-7-16 30000 ne Meena / Karauli

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Masona Vishnu Khorai / rystone, 2/6/201 68 12/2000 Chand 4-Oct-00 3-Oct-50 Karauli / 3.46 19200 Sandsto 6 Mittal Karauli ne Bhartun / Masona 69 125/2004 Arjun Singh 22-Dec-06 21-Dec-56 Sapotra / 1 20-7-16 84480.5 rystone Karauli Asthal / Babusingh Masona 70 13/1997 31-Jul-97 30-Jul-47 Karauli / 1 15-6-16 50000 Rajput rystone Karauli

Mandi Bhat Rajaram Sandsto 71 143/2001 8-Jul-03 7-Jul-53 / Sapotra / 1.12 NA NA Gurjar ne Karauli

Jaimata Di Manoharpur Masona 2/6/201 72 18/2002 Stone 23-Jan-03 20-Jan-53 a / Karauli / 1 50000 rystone 6 Kreshar Karauli

Alikhamb Ka Kaluram Masona Pura,Jatwari 2/6/201 73 20/1999 18-Dec-89 17-Dec-39 1 60000 Meena rystone / Sapotra / 6 Karauli

Nirmal Kamalpura / Soapsto 74 25/1982 Kumar - 31-Jan-25 Todabhim / 4.59 15-6-16 16070 ne Patni Karauli

Jai Manch / Masona 75 25(N)/1998 Meenashw 1-May-89 30-Apr-39 Karauli / 1 15-6-16 50000 rystone ar Cre. Unit Karauli Masona Prakash Mandibhat / rystone, 2/6/201 76 26/1992 Chand 16-Jun-82 15-Jun-32 Sapotra / 2.3 15000 Sandsto 6 Gupta Karauli ne M/S Jai Manch / Gurudev Masona 9/5/201 77 26/1998 1-May-89 30-Apr-39 Karauli / 1 70000 Stone Cre. rystone 7 Karauli Co.

Gopalpura / Prakash Masona 2/6/201 78 26/2003 16-Jul-04 15-Jul-54 Karauli / 1.14 50000 Chand Mali rystone 6 Karauli

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M/S Kumar Infrastruct Manoharpur Silica 3/6/201 79 26/2008 ure 16-Sep-13 15-Sep-63 a / Karauli / 4.86 190300 Sand 6 Developme Karauli nts Pvt.

Padla / Rajandar Masona 2/6/201 80 28/2004 - 10-Jan-55 Todabhim / 1 18000 Singh rystone 6 Karauli

Masona Rambharos Gurdha / rystone, 81 30/1986 i Lal 31-Aug-77 30-Aug-27 Mandrayal / 16.32 NA NA Sandsto Sharma Karauli ne

Masona Baherda / Shrimati rystone, 82 33/1992 - 18-Oct-32 Mandrayal / 4.59 15-6-16 5000 Mulo Devi Sandsto Karauli ne

Bhanwarbra Masona ,32,33 / 30-11- 83 38/2009 Pappi Devi 28-Jul-10 27-Jul-60 1 44393 rystone Nadauti / 16 Karauli

Masona Langara / Prabhu Lal rystone, 84 39/1986 19-Sep-59 31-Mar-25 Mandrayal / 159.11 NA NA Agrawal Sandsto Karauli ne China Deep Pura / Aanandi Clay, 9/5/201 85 39/2012 23-Feb-18 22-Feb-68 Karauli / 4.875 35570 Lal Jangid White 6 Karauli Clay Asthal / Ramkesh Masona 86 4/1997 28-Jul-97 27-Jul-47 Karauli / 1 15-6-16 80000 Mali rystone Karauli Guneshri / Shivshakti Masona 87 4/2004 20-Feb-07 19-Feb-57 Karauli / 1 23-5-16 85002 Minearals rystone Karauli M/S Parul China Infrastrech Clay, JODI/SAPOT 30-11- 88 48/2006 ar 23-Feb-18 22-Feb-68 4.854 20800 White RA/KARAULI 16 Company Clay Pvt.Ltd.

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Kheri / Sharda Masona 89 5/2008 26-Jul-10 25-Jul-60 Todabhim / 1 15-6-16 60000 Meena rystone Karauli

Masona Giriraj Makanpur / rystone, 90 55/1998 Prasad 3-Apr-00 2-Apr-50 Mandrayal / 2.68 20-7-16 14000 Sandsto Sharma Karauli ne

Mr.Manoj Atewa / Sandsto 2/6/201 91 58/2001 Kumar 28-Jul-03 27-Jul-53 Karauli / 2.11 19200 ne 6 Mittal Karauli

Kheri / Rampati Masona 3/6/201 92 60/2007 - 20-Jan-59 Todabhim / 1 112300 Meena rystone 6 Karauli

Kheri / Lakhan Masona 3/6/201 93 61/2007 4-Nov-09 3-Nov-59 Todabhim / 1 97900 Singh rystone 6 Karauli

Kheri / Masona 3/6/201 94 62/2007 Bhimsingh 4-Nov-09 3-Nov-59 Todabhim / 1 98200 rystone 6 Karauli

Masona Parashari / Diwari Lal rystone, 2/6/201 95 67/1998 31-Mar-99 30-Mar-49 Karauli / 5 31200 Yadav Sandsto 6 Karauli ne

Baharda / Ramraj Sandsto 96 68/2001 20-May-03 19-May-53 Mandrayal / 1.36 15-6-16 12000 Mali ne Karauli

Masona Gari Ka Thekedar rystone, Gavn / 97 7/1993 Buddho - 2-Dec-43 4.55 20-7-16 15000 Sandsto Mandrayal / Devi ne Karauli

Masona Mahesh rystone, 98 85/1980 Chand Om 19-Sep-81 18-Sep-31 - - #N/A #N/A Sandsto Praksah ne

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China Pal / Kailash Clay, 99 9/1981 4-Mar-83 3-Mar-33 Nadauti / 5.65 #N/A #N/A Chand Jain Soapsto Karauli ne

Kheri / Shriram Masona 100 99/2004 24-Dec-05 23-Dec-55 Todabhim / 1 15-6-16 0 Enterprises rystone Karauli

Kodai Meetalal Silica Gothra / 101 1/1973 21-Dec-74 31-Mar-25 263.05 NA NA Bohra Sand Karauli / Karauli China Dongari / Anjul Clay, 102 1/1984 1-May-85 30-Apr-35 Sapotra / 4.95 15/6-16 107220 Jadon Silica Karauli Sand

Dundapura Sandsto 3/6/201 103 1/2004 Ram Shri 12-Apr-05 11-Apr-55 / Karauli / 1.27 6000 ne 6 Karauli

Manoharpur Anil Kumar Silica 104 1/2011 16-Sep-13 15-Sep-63 a / Karauli / 4.05 15-6-16 107220 Goyal Sand Karauli

Salempur / Masona 9/5/201 105 16/1999 Nayim Kha 19-Feb-90 18-Feb-40 Sapotra / 0.85 30000 rystone 7 Karauli

Khedi / Jaisingh Masona 106 16/2009 11-Nov-10 10-Nov-60 Todabhim / 1 15-6-16 60000 Rajput rystone Karauli

Shailendra Bhensina / Masona 3/6/201 107 18/2003 Singh - 13-Mar-58 Todabhim / 1 107970 rystone 6 Gurjar Karauli

M/S Khari / Masona 108 20/2009 Mateshwar 11-Nov-10 10-Nov-60 Todabhim / 1 15-6-16 60000 rystone i Minerals Karauli

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Ledor Khurd Banwari Sandsto 3/6/201 109 209/2001 6-Aug-04 5-Aug-54 / Masalpur / 1.02 10000 Lal Sharma ne 6 Karauli

Masona Surendra Talihill / rystone, 110 24/1990 Kumar 15-Jun-71 31-Mar-25 Masalpur / 4.96 NA NA Millston Sharma Karauli e

China Clay, Felspar, Khavda / Shivam 111 24/2008 Silica 23-May-12 22-May-62 Sapotra / 4.88 15-6-16 20787 Minrals Sand, Karauli White Clay

Kheri / Masona 2/6/201 112 25/2000 Vimla Devi 4-Apr-06 3-Apr-56 Todabhim / 1 90000 rystone 6 Karauli

Kauntipura / Sonu Ordinary 113 26/1995 27-Jun-97 26-Jun-47 Sapotra / 1 #N/A #N/A Agrawal Clay Karauli

Siya Suman Keshpura / Sandsto 114 26/2007 Stone Co 18-Feb-08 17-Feb-58 Masalpur / 1 15-6-16 10000 ne .Keshpura Karauli

Kailash Gunesari / Masona 115 28/1996 Chand 6-May-98 5-May-48 Karauli / 1 20-7-16 50000 rystone Meena Karauli Masona Bhouder / Kanhaiya rystone, 27-10- 116 33/1994 9-Apr-96 8-Apr-46 Karauli / 8.89 26520 Lal Sharma Sandsto 16 Karauli ne Atewa / Bhagwati Sandsto 2/6/201 117 35/2002 27-Jan-03 26-Jan-53 Karauli / 1.13 30000 Jatav ne 6 Karauli Ms Ramapura / Ramapura Silica 3/5/200 118 4/1994 4-Oct-75 3-Oct-25 Karauli / 18.12 60000 Minerals Sand 5 Karauli Pvt Ltd

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Gunesara / Ramswroo Masona 119 48/2002 31-Mar-03 30-Mar-53 Karauli / 1 15-6-16 70000 p Mali rystone Karauli

China Clay, Khorra / Satanand 2/6/201 120 5/1981 Fireclay, 3-Dec-81 2-Dec-31 Hindaun / 4.5 41280 Garg 6 Silica Karauli Sand China Deep Pura / Milan Clay, 24-03- 121 50/2007 23-Aug-08 22-Aug-58 Karauli / 4.79 21318 Minerals White 18 Karauli Clay

Laxmi Salempur / Masona 9/5/201 122 58/1997 Narayan - 23-Nov-38 Sapotra / 0.84 30000 rystone 7 Gupta Karauli

Masona Gari Ka Thekedar rystone, Ganv / 123 6/1993 Buddho - 2-Dec-43 4.62 20-7-16 15000 Sandsto Mandrayal / Devi ne Karauli

Ms. Manoharpur Jaibhawani Masona 2/6/201 124 6/2002 23-Jan-03 22-Jan-53 a / Karauli / 1 50000 Stone rystone 6 Karauli Companey Mahua Jagmohan Sandsto Kheda / 9/5/201 125 63/2004 24-May-08 23-May-58 1.4 55764 Gurjar ne Karauli / 7 Karauli Masona Dinesh Talbhari / rystone, 126 9/1977 Kumar 4-Jul-77 3-Jul-27 Karauli / 144.91 #N/A #N/A Sandsto Pandey Karauli ne Surendra Karsai / Sandsto 3/6/201 127 99/2001 Singh 12-May-03 11-May-53 Karauli / 1 10000 ne 6 Chouhan Karauli

Masona Deepak Makan Pur / rystone, 128 1(N)/1999 Kumar 26-Aug-00 25-Aug-50 Mandrayal / 4 20-7-16 10000 Sandsto Sharma Karauli ne

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Karsai / Parmal Sandsto 23-02- 129 109/2004 20-Oct-05 19-Oct-55 Karauli / 1.92 20000 Meena ne 18 Karauli Rajasthan Mijora / Sands & Silica 130 11/2000 6-Nov-71 31-Mar-25 Sapotra / 4.97 14-8-15 718000 Clays Pvt Sand Karauli Ltd. Masona B,Bahadurp Kanhaiya rystone, 131 16/1989 9-Nov-79 8-Nov-29 ur / Sapotra 8.9 20-6-16 20000 Lal Sharma Sandsto / Karauli ne Masona Girraj Kasara / rystone, 20-07- 132 16(N)/2000 Prasad 30-Sep-03 29-Sep-53 Masalpur / 4 10000 Sandsto 2016 Gupta Karauli ne Karsai / Hariom Sandsto 133 164/2001 4-Mar-03 3-Mar-53 Karauli / 1 20-7-16 17830 Sharma ne Karauli

Bhankari / Sirmohar Sandsto 2/6/201 134 182/2001 1-May-03 30-Apr-53 Mandrayal / 1.86 10000 Meena ne 6 Karauli

Shree Garain / Bahirav Silica 135 2/1994 20-May-75 19-May-25 Karauli / 4.8 21-8-15 223000 Dham Sand Karauli Minerals

Kheri / Masona 2/6/201 136 23/2000 Vimla Devi 16-Jun-03 15-Jun-53 Todabhim / 1 90000 rystone 6 Karauli

Bahrai / Arun Sandsto 2/6/201 137 234/2001 4-May-05 3-May-55 Masalpur / 2 10000 Sharma ne 6 Karauli

Kheri / Raghuraj Masona 2/6/201 138 24/2000 21-Aug-03 20-Aug-53 Todabhim / 1 90000 Singh rystone 6 Karauli

Masona Batda / Rajendra rystone, 139 25/1994 - 18-Jan-34 Mandrayal / 10 19-6-10 8000 Bhardwaj Sandsto Karauli ne

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Raybeli / Ramraj Sandsto 3/6/201 140 26/2008 5-May-10 4-May-60 Sapotra / 1.89 190300 Gurjar ne 6 Karauli

Pushpenda Fireclay, Ramapura / 141 27/1980 r Kumar Silica 28-Dec-81 27-Dec-31 Karauli / 4.61 20-7-16 53500 Agrawal Sand Karauli

Masona Prakash Mandi Bhat rystone, 2/6/201 142 27/1992 Chand 18-Jun-82 17-Jun-32 / Sapotra / 4.86 15000 Sandsto 6 Gupta Karauli ne Semerda / Shubham Silica 143 3/1990 10-Jun-93 9-Jun-43 Karauli / 24.56 13-6-8 100000 Minerals Sand Karauli Manohar Mohamma Silica Pura / 144 3/2008 d Rafiq 16-Sep-13 15-Sep-63 4.4 20-7-16 137410 Sand Karauli / Khan Karauli

China Clay, Colidal Raghuvanshi Mahipat Silica, 145 31/2008 21-Aug-14 20-Aug-64 / Karauli / 4.75 24-5-16 65080 Lal Meena Silica Karauli Sand, White Clay

Bahadur Pur Shshi Sandsto 146 32/2001 2-Mar-05 1-Mar-55 / Sapotra / 1 NA NA Bhardwaj ne Karauli

Bahrai / Nawal Sandsto 3/6/201 147 32/2004 10-Nov-04 9-Nov-54 Masalpur / 2.45 10000 Kishor ne 6 Karauli Ms Jai China Bhawani Guneshra / Clay, 2/6/201 148 34/2009 Stone 4-Jul-11 3-Jul-61 Karauli / 4 35000 Silica 6 Crusher Karauli Sand Company

Masona Halka No 13 Kanti rystone, Karauli / 149 36/1991 Kumar 13-Oct-81 12-Oct-31 10 NA NA Sandsto Karauli / Sharma ne Karauli

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Bahadur Pur Mamtesh Sandsto 150 36/2001 8-May-03 7-May-53 / Sapotra / 1.49 NA NA Bhardwaj ne Karauli

Silica Shah Bhandari / Sand, 151 4/1984 Surendra 21-Jan-65 31-Jan-25 Todabhim / 4.98 15-6-16 8308 Soapsto Kumar Karauli ne

Millston Bapoti / Dhanno e, 152 40/1987 24-Nov-77 23-Nov-27 Sapotra / 0.72 NA NA Devi Sandsto Karauli ne Masona Janardan Sorya / rystone, 153 49/1986 Singh 18-Oct-72 31-Jan-25 Karauli / 180.05 30-4-10 45000 Sandsto Gahlot Karauli ne

Makanpur , Digambar Sandsto Batda / 154 59/2001 Dayal 30-May-03 29-May-53 3.15 20-7-16 10000 ne Mandrayal / Chaturvedi Karauli

Richoti / Sudharsha Silica 155 6/1982 3-May-83 2-May-33 Karauli / 23.17 29-8-16 134500 n Lal Sand Karauli Masona Batda / Narayan rystone, 27-10- 156 6/1995 - 4-Apr-35 Mandrayal / 8.25 19656 Singh Sandsto 16 Karauli ne

Masona Sunil Bhankari / rystone, 2/6/201 157 6/2000 Kumar 18-Jan-02 17-Jan-52 Mandrayal / 3.23 20000 Sandsto 6 Sharma Karauli ne

Jatwari / Bachchan Masona 158 62/2002 1-Jun-06 31-May-56 Sapotra / 1 15-6-16 99000 Singh rystone Karauli Khidrpur / Masona 159 67/2002 Reeta Devi 4-Sep-03 3-Sep-53 Sapotra / 1 15-6-16 90000 rystone Karauli

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Gari / Meetalal Soapsto 160 7/1976 20-Feb-78 21-Feb-28 Todabhim / 388.5 NA NA Bohra ne Karauli

Bhandari,Ga Shah di Morda, Soapsto 8/7/200 161 8/1976 Surendra - 31-Mar-25 Rajoli / 24.74 63000 ne 8 Kumar Todabhim / Karauli

Selampur Shyam Masona (Tamoupura 162 9/2009 Gopal 19-Sep-11 18-Sep-61 1 NA NA rystone ) / Sapotra / Singh Karauli

Bahadur Pur Piyush Sandsto 163 91/2001 10-Feb-04 9-Feb-54 / Sapotra / 1 NA NA Updhyay ne Karauli

Kheri / Hansram Masona 164 96/2004 24-Dec-05 23-Dec-55 Todabhim / 1 15-6-16 90000 Meena rystone Karauli

Maluk Kheri / Masona 165 98/2004 Chand 24-Dec-05 23-Dec-55 Todabhim / 1 20-7-16 90000 rystone Goyal Karauli

Barytes, China Clay, Talchira / Shivkumar 166 1/1996 Fireclay, 22-Apr-99 21-Oct-49 Nadauti / 133.08 18-2-99 26115 Diwedi Quartz, Karauli Soapsto ne

Salempur / Indira Silica 167 1/1998 3-May-79 2-May-29 Sapotra / 4.99 29-6-15 30000 Agrawal Sand Karauli

Durga NAROLI/SAP White 17-12- 168 11/1998 Prasad 4-Dec-69 31-Mar-25 OTRA/KARA 4.91 361000 Clay 15 Agarwal ULI

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China Bariya / M/S Sagar Clay, 169 12/1985 16-Dec-86 15-Dec-36 Karauli / 4.89 15-6-16 60000 Minerals Silica Karauli Sand

Bhenesna / Babu Dayal Masona 3/6/201 170 129/2001 6-Jan-03 5-Jan-53 Todabhim / 1 67870 Singh rystone 6 Karauli

Integrated Khirkhira / Glass Silica 8/7/200 171 14/2006 4-Nov-08 3-Nov-58 Karauli / 12.36 310000 Materials Sand 8 Karauli Limited

Ashok Dantali / Masona 3/6/201 172 16/2002 Kumar 31-May-04 30-May-54 Todabhim / 1 108000 rystone 6 Agarwal Karauli

Pura Ata / Vidhya Silica 173 16/2004 28-Aug-06 27-Aug-56 Karauli / 0.65 NA NA Devi Sand Karauli

Dundapura Sharad Sandsto 3/6/201 174 163/2001 3-Mar-05 2-Mar-55 / Karauli / 1.4 36000 Bhardwaj ne 6 Karauli

Masona Kasara / Hanuman rystone, 30-11- 175 17/2000 22-May-03 21-May-53 Masalpur / 4.5 100000 Sahay Sain Sandsto 16 Karauli ne

Bhensina / Beerbhadu Masona 3/6/201 176 17/2003 - 13-Jan-58 Todabhim / 1 126300 r Singh rystone 6 Karauli

Makan Pur Masona Swami,Mak Arvind rystone, anpur 177 19/1985 9-Dec-91 8-Dec-41 40.36 NA NA Tiwari Sandsto Swami / ne Mandrayal / Karauli

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Masona Gari Ka M/S rystone, Gavn / 27-10- 178 20/1994 Vatsala 9-Jul-84 8-Jul-34 10 30888 Sandsto Mandrayal / 16 Minerals ne Karauli

Kheri / Masona 30-11- 179 21/2009 Bhim Singh 11-Nov-10 10-Nov-60 Todabhim / 1 96000 rystone 16 Karauli

Kheri / Gajraj Masona 2/6/201 180 22/2000 16-Jun-03 15-Jun-53 Todabhim / 1 200000 Singh rystone 6 Karauli

Masona Makanpur , Kumer rystone, Batda / 181 28/2000 13-Jul-00 12-Jul-50 1.16 20-7-16 25000 Meena Sandsto Mandrayal / ne Karauli

Salempur / Indira Colidal 182 3/1995 31-Jan-77 30-Jan-27 Sapotra / 22.6 29-6-15 30000 Agrawal Silica Karauli

Masona Makanpur , Dinesh rystone, Batda / 27-10- 183 30/1998 Chand - 18-Sep-38 8.99 30036 Sandsto Mandrayal / 16 Rajaram ne Karauli

Seba / Gangapur Anita White 2/6/201 184 33/2006 12-May-14 11-May-64 City / 4.9 20900 Sharma Clay 6 Sawaimadh opur Bahrai / Jitendra Sandsto 3/6/201 185 34/2004 10-Nov-04 9-Nov-54 Masalpur / 2.29 10000 Sharma ne 6 Karauli Radhey Talihill / Millston 186 35/1991 Shyam 15-Jun-71 31-Mar-25 Masalpur / 7.78 NA NA e Goyal Karauli Masona Dundapura Vishan Lal rystone, 187 39/2000 29-Oct-01 28-Oct-51 / Karauli / 5 15-6-16 6000 Meena Sandsto Karauli ne

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Silica Corporatio Alampur / Silica 2/6/201 188 4/1982 n 3-May-83 4-May-33 Karauli / 4.68 81850 Sand 6 Gangapur Karauli City

Rajesh Salempur / Masona 24-03- 189 42/1996 Kumar 13-Mar-00 12-Mar-50 Sapotra / 0.94 49190.8 rystone 2018 Gupta Karauli

Chinayata / Unkar Lal Masona 3/6/201 190 46/1997 29-May-98 28-Aug-48 Hindaun / 1 42820 Garg rystone 6 Karauli

Masona Bahadur Pur Geeta Devi rystone, 191 47/1988 9-Nov-79 8-Nov-29 / Sapotra / 3.4 #N/A #N/A Sharma Sandsto Karauli ne

Masona Makanpur / Munni rystone, 31-11- 192 49/1998 29-Aug-00 28-Aug-50 Mandrayal / 1.38 50000 Devi Sandsto 16 Karauli ne

Salempur / Shyam Lal Masona 31-11- 193 49(N)/1998 - 30-Nov-39 Sapotra / 1 50000 Mali rystone 16 Karauli

Masona Makan Pur / Sitaram rystone, 194 54/1998 18-Jan-99 17-Jan-49 Mandrayal / 2.51 20-7-16 11000 Mali Sandsto Karauli ne

Masona Bhoru rystone, / Karauli / 195 56/1986 Singh 30-Sep-77 29-Sep-27 7.91 #N/A #N/A Sandsto Karauli Jadoun ne

Tamolipura Rajesh Masona 2/6/201 196 6/2006 14-Feb-07 13-Feb-57 / Sapotra / 1 216000 Meena rystone 6 Karauli

Chinayata / Dronachar Masona 3/6/201 197 62/2005 26-Oct-05 25-Oct-55 Hindaun / 1 30000 ya Sharma rystone 6 Karauli

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Baloti / Hajari Lal Masona 2/6/201 198 63/1997 28-Mar-98 27-Mar-48 Sapotra / 1 90000 Bariwa rystone 6 Karauli Masona Gurdah / Dev Vrat rystone, 199 67/1991 27-Jun-72 31-Mar-25 Mandrayal / 46.32 NA NA Meena Sandsto Karauli ne

Makanpur , Rukmini Sandsto Batda / 200 75/2001 7-Jun-03 6-Jun-53 1.17 20-7-16 25000 Sharma ne Mandrayal / Karauli

Kheri / Shri Ankit Masona 201 85/2004 25-Jan-08 24-Jan-58 Todabhim / 1 15-6-16 150000 Mittal rystone Karauli

Salempur / Krishnanan Masona 9/5/201 202 9/1995 21-Dec-95 20-Dec-45 Sapotra / 0.84 30000 d Sharma rystone 7 Karauli

Kheri / Jai Balaji Masona 2/6/201 203 92/2004 11-Aug-08 10-Aug-58 Todabhim / 1 60000 Stone Cre. rystone 6 Karauli

Masona Narayan Makan Pur / rystone, 204 1/1998 Singh - 5-May-38 Mandrayal / 9.19 29-6-15 30000 Sandsto Rajput Karauli ne

Jatwari / Sumer Masona 205 1/2007 1-Apr-08 31-Mar-58 Sapotra / 1 20-7-16 98724 Singh rystone Karauli

Batda / Brahmana Sandsto 2/6/201 206 10/2006 25-Jan-07 24-Jan-57 Mandrayal / 1.01 29999.5 nd Sharma ne 6 Karauli

Karsai / Sandsto 3/6/201 207 105/2004 Jailal Mali 21-Aug-06 20-Aug-56 Karauli / 1.96 10000 ne 6 Karauli Nagesh Sandsto / Sapotra / 208 108/2004 13-Mar-08 12-Mar-58 2.42 20-7-16 42321.2 Meena ne Karauli

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Prakash Dhorera / Silica 27-10- 209 12/1976 Chand 8-Aug-77 7-Aug-27 Karauli / 15.54 225260 Sand 16 Murari Lal Karauli Masona / Vijay Singh rystone, 2/6/201 210 13/1989 16-Dec-74 31-Mar-25 Masalpur / 4.48 5000 Jadaun Sandsto 6 Karauli ne Talchira / Shivkumar Masona 211 14/2001 10-Sep-03 9-Sep-53 Nadauti / 1 NA NA Diwedi rystone Karauli Asthal / Purshttom Masona 212 15/1997 4-Aug-97 3-Aug-47 Karauli / 1 NA NA Gupta rystone Karauli

Jagdish Batda / Sandsto 2/6/201 213 15/2003 Prasad 6-Nov-04 5-Nov-54 Mandrayal / 0.99 30000 ne 6 Sharma Karauli

Shri. Asthal / Masona 214 16/1997 Omprakas 31-Jul-97 30-Jul-47 Karauli / 1 15-6-16 70000 rystone h Mali Karauli

Gopalpura / Jamuna Lal Masona 2/6/201 215 19/2003 19-Sep-03 18-Sep-53 Karauli / 1 50000 Mali rystone 6 Karauli

M/S Krishan Masona Kumar Langra / rystone, 27-10- 216 2/1996 Deepak 28-Jan-77 27-Jan-27 Mandrayal / 48.53 20000 Sandsto 16 Kumar Karauli ne Stone Company

Gopalpura / Jamuna Lal Masona 2/6/201 217 27/2003 16-Jul-04 15-Jul-54 Karauli / 1.27 50000 Mali rystone 6 Karauli

Sidhdata Padla / Masona 2/6/201 218 27/2004 Stone - 10-Apr-55 Todabhim / 1 18000 rystone 6 Crusher Karauli

Ms Khirkhira / Ramapura Silica 219 3/1999 1-Nov-03 31-Oct-53 Karauli / 5 NA NA Minerals Sand Karauli Pvt Ltd

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Ms Gunesari / Masona ####### 220 3/2004 Ashutosh 20-Feb-07 19-Feb-57 Karauli / 1 85001 rystone # Minerals Karauli Masona Rajendra Langra / rystone, 3/5/201 221 30/1990 Dayal 7-Aug-81 6-Aug-31 Mandrayal / 165.3 18000 Sandsto 2 Gupta Karauli ne Masona Bhoder / Bhanwar rystone, 3/6/201 222 37/1994 7-Jan-98 6-Jan-48 Karauli / 4.89 180000 Singh Sandsto 6 Karauli ne Shreebhan Kheda / Sandsto 2/6/201 223 37/2006 Singh 25-Mar-08 24-Mar-58 Karauli / 1 10000 ne 6 Gurjar Karauli Leida Ms. Silica Khirkhira / 2/9/201 224 4/1976 Jagdamba 3-Dec-76 2-Dec-26 23.73 150000 Sand Sapotra / 6 Minerals Karauli Manohar Mahalaxmi Silica Pura / 225 4/2008 16-Sep-13 15-Sep-63 4.4 20-7-16 128570 Minerls Sand Karauli / Karauli Asthal / Ramotar Masona 226 5/1997 21-Aug-97 20-Aug-47 Karauli / 1 15-6-16 80000 Singh rystone Karauli

Bichpuriya / Jaganram Silica 2/6/201 227 5/2001 23-Aug-08 22-Aug-58 Karauli / 4.36 118780 Meena Sand 6 Karauli

China Anantraj Deep Pura / Clay, 24-03- 228 53/2007 Mines And 23-Aug-08 22-Aug-58 Karauli / 4.79 10200 White 18 Minarals Karauli Clay Harnagar / Mohan Lal Sandsto 229 55/2003 3-Jan-04 2-Jan-54 Karauli / 2.07 20-7-16 3000 Sharma ne Karauli Masona Rup Kalayani / rystone, 230 6/1976 Narayan 6-Oct-71 31-Mar-25 Karauli / 92.51 26-8-12 30000 Sandsto Pandey Karauli ne

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Masona Gari Ka Mularam rystone, Gaon / 231 7/1990 15-Sep-80 14-Sep-30 4.87 20-7-16 15000 Meena Sandsto Mandrayal / ne Karauli

Masona Karsai / Rupram rystone, 232 70/1998 15-Jan-98 14-Jan-48 Karauli / 2.5 20-7-16 10000 Meena Sandsto Karauli ne

Ms Shriram Manoharpur Masona 2/6/201 233 74/2004 Laddu 9-Sep-09 31-Aug-59 a / Karauli / 1 50000 rystone 6 Baba Karauli

Ms. Loharra / Girrajdhara Silica 234 8/1979 25-Sep-80 24-Sep-30 Karauli / 38.85 NA NA n Sand Karauli Enterprises

Masona Bhankari / Jagdish rystone, 2/6/201 235 8/2000 25-Feb-02 24-Feb-52 Mandrayal / 4.95 5000 Meena Sandsto 6 Karauli ne

Atewa / Sandsto 236 11/2005 Ramsahay 20-Aug-08 19-Aug-58 Karauli / 2.4 NA NA ne Karauli Akolpura / B.L. Sandsto 2.6.201 237 13/2003 30-Sep-03 29-Sep-53 Karauli / 1 10000 Bagouriya ne 6 Karauli

Bugdar / Ramphool Sandsto 238 158/2001 24-Jul-03 23-Jul-53 Mandrayal / 1.08 20-7-16 20000 Meena ne Karauli

China Kaunti Pura Anfal Clay, 23-05- 239 16/2010 21-Aug-14 20-Aug-64 / Sapotra / 4.06 52062 Mineral White 16 Karauli Clay Khem Bahrai / Sandsto 3/6/201 240 165/2001 Chand 27-Apr-06 26-Apr-56 Masalpur / 1.35 10000 ne 6 Sharma Karauli Durga Mijora / Silica 241 2/1992 Prasad 18-Feb-74 31-Mar-25 Sapotra / 4.26 #N/A #N/A Sand Agrawal Karauli

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Kheri Hewat Gunjan Masona 15-06- 242 20/2008 - 2-Jan-60 / Hindaun / 1 30000 Bindal rystone 16 Karauli

Makanpur , Nand Sandsto Batda / 243 200/2001 Kumar 14-Aug-03 13-Aug-53 1.55 20-7-16 25000 ne Mandrayal / Sharma Karauli

Dhugarh / Sashi Masona 244 22/2006 3-Nov-10 2-Nov-60 Karauli / 1 15-6-16 60000 Kanwar rystone Karauli

Makanpur / Geeta Devi Sandsto 245 228/2001 23-Sep-03 20-Sep-53 Mandrayal / 1.44 20-7-16 20000 Sharma ne Karauli

Padla Jagir / Chuttan Lal Masona 2/6/201 246 29/2004 11-Apr-05 10-Apr-55 Todabhim / 1 18000 Meena rystone 6 Karauli

Keshpura / Devisharan Sandsto 3/6/201 247 33/2004 10-Nov-04 9-Nov-54 Masalpur / 2.22 20000 Shrma ne 6 Karauli

Masona Bhoder / Kanta rystone, 27-10- 248 34/1994 28-Jan-98 27-Jan-48 Karauli / 10 32614 Sharma Sandsto 16 Karauli ne

Salempur / Mohm. Masona 31-11- 249 34/1998 24-May-00 23-May-50 Sapotra / 1 50000 Rafiq rystone 16 Karauli

Bhagwan Jodhapur / Masona 1/0/190 250 38/1998 Singh - 29-May-52 Todabhim / 0.8 0 rystone 0 Gurjar Karauli

Masona Gurdeh / Sunayana rystone, 2/5/201 251 39/1991 28-Oct-76 27-Oct-26 Mandrayal / 245 27000 Sharma Sandsto 2 Karauli ne

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Gunesara / Ramswroo Masona 252 49/2002 31-Mar-03 30-Mar-53 Karauli / 1 15-6-16 70000 p Mali rystone Karauli

China M/S Deep Pura / Clay, 253 51/2012 Natural 23-Feb-18 22-Feb-68 Karauli / 4.95 16-5-16 43910 White Minerals Karauli Clay

Masona Makan Pur / Ramji Lal rystone, 254 57/1998 17-May-99 16-May-49 Mandrayal / 3.85 20-7-16 20000 Meena Sandsto Karauli ne

Gunesari / Ghusmesw Masona ####### 255 6/2004 20-Feb-07 19-Feb-57 Karauli / 1 85000 er Crushers rystone # Karauli

Bhankari / Narayan Sandsto 2/6/201 256 62/2001 1-May-03 30-Apr-53 Mandrayal / 1.6 10000 Lal Meena ne 6 Karauli

Kheri / Laxminaray Masona 257 63/2007 - 20-Nov-59 Todabhim / 1 15-6-16 89212 an Sharma rystone Karauli

Mahua Udaybhan Sandsto Khera / 2/6/201 258 66/2004 30-Dec-04 29-Dec-54 1.04 10000 Singh ne Masalpur / 6 Karauli Lotda / Virendra Sandsto 259 74/2002 6-May-03 5-May-53 Masalpur / 1.92 15-6-16 10000 Kumar ne Karauli Masona Bahadurpur Rambeti rystone, 260 78/1979 9-Nov-79 8-Nov-29 / Sapotra / 45.49 NA NA Devi Sandsto Karauli ne

Masona Guberda,Gu Arivand rystone, rbera / 261 8/1987 14-Jul-77 13-Jul-27 150.93 23-4-12 15000 Kumar Sandsto Masalpur / ne Karauli

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Masona Yogesh Bahadur Pur rystone, 262 8(N)/1987 Kumar 11-Jan-99 10-Jan-49 / Sapotra / 1.82 #N/A #N/A Sandsto Gupta Karauli ne

Bhankari / Sandsto 2/6/201 263 80/2002 Halki 24-Jul-03 23-Jul-53 Mandrayal / 1.27 10000 ne 6 Karauli

Manohar Rama Silica Pura / 264 37865 9-May-06 8-May-56 5 20-7-16 128570 Minerals Sand Karauli / Karauli Chobe Ki Pancham Sandsto Gwari / 265 9/06 Stone 18-Jun-07 17-Jun-57 1.57 #N/A #N/A ne Sapotra / Company Karauli

Kheri / Jai Balaji Masona 2/6/201 266 91/2004 8-Dec-55 Todabhim / 1 60000 Stone Cre. rystone 6 Karauli

10.0 DETAILS OF ROYALTY OR REVENUE RECEIVED IN LAST THREE YEARS:

S.No. Year Revenue received (In Rs. lacs) 1 2015-16 2490.31 2 2016-17 2164.55 3 2017-18 1663.03

11.0 DETAILS OF PRODUCTION OF MINOR MINERAL IN LAST THREE YEARS: (Production inTonnes) S.No. Mineral 2015-16 2016-17 2017-18 (a) Masonry Stone 206217 322544 410237 (b) Silica Sand 331214 355957.15 529663.55 (c) Soap Stone 11347 43866 24693.77 (d) Clay 30433 64120 85539.94 (e) Hand Mill Stone 1340 860 1201.46 (f) Brick Clay - 35720 79464.24 (g) Sand stone 59181 100090.32 662257.95 (h) Ordinary Clay 500 266.66 23205.68 (i) Bajri - - -

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12.0 MINERAL MAP OF THE DI

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13.0 TOTAL MINERAL RESERVE AVAILABLE IN THE DISTRICT:

The reserve of mineral available in district is much sufficient for many years

14.0 QUALITY/GRADE OF MINERAL AVAILABLE IN THE DISTRICT:

The grade of available minerals in the district is good quality grad.

15.0 USE OF MINERALS: Mining industry plays an important role in economic sector in India. Rajasthan is rich in mineral wealth. The state is endowed with major and minor mineral resources. The region, where the project is situated is mostly dependent on agriculture and mineral resources. The developments of mining are provide direct and indirect employment opportunities, infrastructure development, communication and socio-economic infrastructure.

A. Silica Sand: Crystalline silica is an essential component of materials which have an abundance of uses in industry and are a vital component in many things used in our everyday lives. It is impossible to imagine houses without bricks, mortar or windows, cars without engines or windscreens, life without roads or other transport infrastructures and everyday items made of glass or pottery.Industrial silica is used in a vast array of industries, the main ones being the glass, foundries, construction, ceramics, and the chemical industry.Silica in its finest form is also used as functional filler for paints, plastics, rubber, and silica sand is used in water filtration and agriculture.Crystalline silica is also irreplaceable in a series of high-tech applications, for example in optical data transmission fibres and precision casting. It is also used in the metallurgical industry as the raw material for silicon metal and ferrosilicon production. Another specialized application is in the oil extraction.

B. China Clay: it is used in ceramics, toys and paper industries.

C. Soap Stone: It is used in Talc, Paper and Soap & Cosmatic Industries.

16.0 DETAILS OF ECO-SENSITIVE AREA, IF ANY IN THE DISTRICT:In the district Kaila Devi wildlife sanctuary & Swarn Jayanti Park & some part of Ranthomber National Park is the ECO Sensitive zones & many numbers of RF & PF in district.

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17.0 IMPACT ON THE ENVIRONMENT (Air, Water, Soil, Noise, Flora & Fauna, Land Use, Agriculture, Forest ect.) DUE TO MINING ACTIVITY: Environmental Impact arising out of mining operations may be defined as an alteration of environmental conditions or creation of a new set of environmental conditions caused or induced by the mining operations. The purpose of identifying and assessing the existing environmental parameters is to know the basic conditions prevailing before getting the targeted production. Depending on the nature of activities and existing status, the impacts are assessed for their importance. On the basis of the impact analysis, the mitigating action and future monitoring requirement are focused in the Environmental Management Plan for counting or minimizing adverse impacts.

The environmental impact on land, air, water, noise, climate, flora & fauna and socioeconomic conditions arising out of mining operations need be assessed and thereafter mitigation measures are to be adopted. Impact due to mining on each of the environmental component are detailed below in accordance with the parameter of environment likely to be affected. The parameters, which are relevant in the context, are given below:  Land Environment

 Water quality

 Soild Waste Managment

 Air quality

 Noise levels and ground vibration

 Biological Environment

 Socio-economic conditions The environmental impacts can be categorized as either primary or secondary. Primary impacts can be attributed directly to the mining project. The secondary impacts due to mining project are indirect or induced & typically include changed patterns of social & economic activities likely to be stimulated or induced by the improvement in economy of the region caused by increased money circulation amongst the population.

The different activities envolved before & during mining are narrated below, which helps to asses the impact on environment?

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• Exploration: A mining project can only commence with knowledge of the extent and value of the mineral ore deposit. Information about the location and value of the mineral ore deposit is obtained during the exploration phase. This phase includes surveys, field studies, and drilling test boreholes and other exploratory excavations. The exploratory phase may involve clearing of wide areas of vegetation (typically in lines), to allow the entry of heavy vehicles mounted with drilling rigs. Many countries require a separate EIA for the exploratory phase of a mining project because the impacts of this phase can be profound and because further phases of mining may not ensue if exploration fails to find sufficient quantities of high-grade mineral ore deposits of economical values.

• Development If the mineral ore exploration phase proves that there is a large enough mineral ore deposit, of sufficient grade, then the project proponent may begin to plan for the development of the mine. This phase of the mining project has several distinct components.

• Site preparation If a mine site is located in a remote, undeveloped area, the project proponent may need to begin by clearing land for the construction of staging areas that would house project personnel and equipment. Even before any land is mined, activities associated with site preparation and clearing can have significant environmental impacts, especially if they are within or adjacent to ecologically sensitive areas. The EIA must assess, separately, the impacts associated with site preparation and clearing.

• Active mining Once a mining company has constructed access roads and prepared staging areas that would house project personnel and equipment, mining may commence. All types of active mining share a common aspect, i.e. the extraction and concentration (or beneficiation) of a metal from the earth. Proposed mining projects differ considerably in the proposed method for extracting and concentrating the metallic ore. In almost every case, metallic ores are buried under a layer of ordinary soil or rock (called „overburden‟ or „waste rock‟) that must be moved or excavated to allow access to the

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ore deposit. The first way in which proposed mining projects differ is the proposed method of moving or excavating the overburden. What follows are brief descriptions of the most common methods.

• Open-pitmining Open-pit mining is a type of strip mining in which the ore deposit extends very deep in theground, necessitating the removal of layer upon layer of overburden and ore. In many cases, logging of trees and clear-cutting or burning of vegetation above the oredeposit may precede removal of the overburden. The use of heavy machinery, usuallybulldozers and dump trucks, is the most common meas of removing overburden. Openpitmining often involves the removal of natively vegetated areas, and is thereforeamong the most environmentally- destructive types of mining, especially within tropicalforests.

• Underground mining In underground mining, a minimal amount of overburden is removed to gain access to theore deposit. Access to this ore deposit is gained by tunnels or shafts. Tunnels or shafts leadto a more horizontal network of underground tunnels that directly access the ore. In anunderground mining method called „stoping‟ or „block caving,‟ sections or blocks of rockare removed in vertical strips that leave a connected underground cavity that is usuallyfilled with cemented aggregate and waste rock.Although underground mining is a less environmentally-destructive means of gainingaccess to an ore deposit, it is often more costly and entails greater safety risks than stripmining, including open-pit mining. While most large- scale mining projects involve openpitmining, many large underground mines are in operation around the world.

• Disposal of overburden and waste rock In almost every project, metallic ores are buried under a layer of ordinary soil or rock(called „overburden‟ or „waste rock‟) that must be moved or excavated to allowaccess to the metallic ore deposit. For most mining projects, the quantity ofoverburden generated by mining is enormous. The ratio of the quantity ofoverburden to the quantity of mineral ore (called the „strip ratio‟)is usually greater than one, and can be much higher. For example, if a proposedmining project involves the extraction of 100 million metric tons of mineral ore, thenthe proposed mining

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project could generate more than one billion metric tons ofoverburden and waste rock.

• Site reclamation and closure When active mining ceases, mine facilities and the site are reclaimed and closed. Thegoal of mine site reclamation and closure should always be to return the site to acondition that most resembles the pre-mining condition. Mines that are notorious fortheir immense impact on the environment often made impacts only during theclosure phase, when active mining operations ceased. These impacts can persist fordecades and even centuries. Therefore, the EIA for every proposed mining projectmust include a detailed discussion of the mine Reclamation and Closure Plan offeredby the mining proponent.Mine reclamation and closure plans must describe in sufficient detail how the miningcompany will restore the site to a condition that most resembles pre-miningenvironmental quality; how it will prevent – in perpetuity – the release of toxiccontaminants from various mine facilities (such as abandoned open pits and tailingsimpoundments); and how funds will be set aside to insure that the costs of reclamationand closure will be paid for.

• Human displacement and resettlement According to the International Institute for Environment and Development:The displacement of settled communities is a significant cause of resentment andconflict associated with large-scale mineral development. Entire communitiesmay be uprooted and forced to shift elsewhere, often into purpose-builtsettlements not necessarily of their own choosing. Besides losing their homes, communities may also lose their land, and thus their livelihoods. Communityinstitutions and power relations may also be disrupted. Displaced communitiesare often settled in areas without adequate resources or are left near the mine,where they may bear the brunt of pollution and contamination. Forcedresettlement can be particularly disastrous for indigenous communities who havestrong cultural and spiritual ties to the lands of their ancestors and who may findit difficult to survive when these are broken.

 Impacts ofmining projects on air quality:- The largest sources of air pollution in mining operationsare: Particulate matter transported by the windas a result ofexcavations, blasting, and transportation of materials, wind erosion (more frequent in open-pitmining), fugitive dustfrom tailings

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facilities, stockpiles, waste dumps, and haul roads. Exhaust emissions frommobile sources (cars, trucks, heavy equipment) raise these particulate levels; and gasemissions from the combustion of fuels in stationary and mobile sources, explosions, andmineral processing. Once pollutants enter the atmosphere, they undergo physical andchemical changes before reaching a receptor. Thesepollutants cancause seriously effectstopeople‟shealthandto the environment.Large- scalemininghas thepotentialtocontribute significantly to air pollution, especially inthe operation phase. All activities during ore extraction, processing, handling, andtransport depend on equipment, generators, processes and materials that generatehazardous airpollutants such asparticulatematter, heavymetals, carbon monoxide, sulfurdioxide,and nitrogenoxides.

 Transportation sources Transporation sources of air pollutants include heavy vehicles used in excavation operations,cars that transport personnel at the mining site, and trucks that transport mining materials.The level of polluting emissions from these sources depends on the fuel and conditions of theequipment. Even though individual emissions can be relatively small, collectively theseemissionscanbeof real concern. In addition, mobile sources are a major sourceofparticulatematter, carbon monoxide, and volatile organic compounds that contribute significantly to theformationof ground-level ozone.

 Stationary sources The main gaseous emissions are from combustion of fuels in power generationinstallations, and drying, roasting, and smelting operations. Many producers of preciousmetals smelt metal on-site, prior to shipping to off-site refineries. Typically, gold andsilver is produced in melting/fluxing furnaces that may produce elevated levels ofairborne mercury, arsenic, sulfur dioxide, and other metals.

 Fugitive emissions Common sources of fugitive emissions include: storage and handling of materials; mineprocessing; fugitive dust, blasting, construction activities, and roadways associated withmining activities; leach pads, and tailing piles and ponds; and waste rock piles. Sourcesandcharacteristics of fugitive emissions dust in mining operations vary in each case, as dotheir impacts. Impacts are difficult to predict and calculate but

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should be consideredsince they could be a significant source of hazardous air pollutants.

 Noise and vibration Noise pollution associated with mining may include noise from vehicle engines, loadingand unloading of rock into steel dumpers, chutes, power generation, and other sources.Cumulative impacts of shoveling, ripping, drilling, blasting, transport, crushing, grinding,and stock-piling can significantly affect wildlife and nearby residents.Vibrations are associated with many types of equipment used in mining operations, butblasting is considered the major source. Vibration has affected the stability ofinfrastructures, buildings, and homes of people living near large-scale open-pit miningoperations. According to a study commissioned by the European Union in 2000:“Shocks and vibrations as a result of blasting in connection with mining can lead to noise,dust and collapse of structures in surrounding inhabited areas. The animal life, on whichthe local population may depend, might also be disturbed.”

18.0 REMEDIAL MEASURES TO MITIGATE THE IMPACT OF MINING ON THE ENVIRONMENT: To minimize the probable & possible impact on the Environment due to mining activities an Environmental management plan is aimed at mitigating the possible adverse impact of a project and for ensuring to maintain the existing environmental quality. The Environmental Management Plan (EMP) is a site specific plan to ensure that the activities of the project are implemented in sustainable manner. EMP also ensures that the project implementation is carried out taking appropriate meditative measures to reduce adverse environmental impacts due to developing projects. The Environment Management Plan (EMP) aims to mitigate measures to restore and conserve the ecosystem of the possible adverse impacts due to proposed project. The mitigation steps are used to minimize or prevent negative impacts on environment due to proposed project of mining. The EMP contains planned improvements with adopting some control measures viz. fugitive dust reduction on roads & measures to alleviate problems in affected villages near project area and planning for the closure of mine.

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Mitigation Measures for Land Environment The mining in the area is being done from long time, therefore, land has already been degraded. The land affected due to mining will not be backfilled, mined out area will be converted into water reservoir. The water of this reservoir will very useful for fauna and domestic Animals of the area. This also recharges the groundwater table. Entire dumps in the area will be reclaimed by plantation. Wire fencing around the excavated area is proposed to restrict the inadvertent entry of human beings as well as animals. (i) Measures for proper utilization of top soil will be ensured. (ii) The waste dump will be properly stacked and reclaimed by plantation. (iii) Minimum land shall be used for waste dumping and other infrastructures. (iv) The bigger voids formed during mining will be converted into water reservoirs as suggested in the report.

Mitigation Measures for Air Environment (i) Water spraying arrangement will be done on haul roads in the mining area to suppress the dust. (ii) Dust extractors will be provided in drilling machines to suppress air borne dust. Wherever possible wet drilling will be done. (iii) Air monitoring will be done once in 6 months from a NABL/MOEF/Govt. Approved Laboratory. (iv) Workers engaged at dusty zones will be provided masks.

Mitigation Measures for Water Environment (i) Retaining wall and garland drain will be maintained around the dumps to check wash off during rainy season. (ii) The dumps will be kept properly sloped. (iii) Dense plantation will be done in lower side of the dumps to check the runoff. (iv) The garland drain will be maintained around the working pits to check entry of rain water during rainy season

Mitigation Measures forNoise Environment (i) Proper maintenance of machineries will be done to minimize noise. Adequate silencers will be provided in diesel engines of machineries, compressors, dumpers and trucks.

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(ii) Earplugs will be provided to the workers while working in higher noise zone. (iii) Creating thick greenbelt to attenuate noise pollution in the mine area.

Mitigation Measures for Noise Environment (i) Minimum dust gets generated during movement of dumpers on haul roads which are regularly sprinkled with water (ii) The approach roads from mine to nearest transportation Road will be strengthened (iii) The top soil generated by the mining activities will be utilized for plantation purposes and it will be stacked separately. (iv) Green belt will be developed along the both side of road to arrestany degradation of land/soil

Mitigation Measures for Socio Economic Development (i) All the workers have been employed from nearby villages. (ii) The Association will take interest for the welfare amenities Scheme in the area with the help of local people. Provision of Scholarship for meritorious students will be given those who getting highest mark in district level/State level exams. (iii) All other facilities like Medical help for the children & women/ widow etc., arrange medical camps in nearby area.

19.0 RECLAMATION OF MINED OUT AREA (BEST PRACTICE ALREADY IMPLEMENTED IN THE DISTRICT, REQUIRMENT AS PER RULES AND REGULATION, PROPOSED RECLAMATION PLAN)

Land degradation due to dumping of waste/ mineral for future sale:

The overburden dumps of masonry stone in the form of quartzite is be dump in the hopper installed at mine site to make gitty and sold out & used in maintenance of haul roads, so in this mining project not any specified location for staging the waste dumps. The overburden dumps of top surface may be covered with soil and planted /developed as green belt.

Aesthetic Environment: Topography and landscape of the area is hilly terrain and small undulation near the deposit. The mining operation affects the topography and landscape characteristic of the area. Thus it has a visual intrusion. Dust concentration affects the visual quality of air environment. Area after exploitation & reclamation

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will get aesthetic beauty by proposed plantation.

Siltation of agricultural field & water courses: Rain water may carry silt while flowing from waste dumps etc and may adversely affect surface water sources. It is therefore proposed to construct suitable size catch grains/ garland drains around waste dumps/non saleablequartzite dumps to allow rain water to flow downwards, with suitably located siltation ponds enroot to arrest the silt and allowing only clean water to flow onwards. These siltation ponds will require periodical cleaning to maintain flow of only clean water.

Impact on soil: No major impact on soil of the study area is envisaged due to mining activities. The mining activity shall remain confined locally within working areaand emission at haul road will be controlled by water sprinkling and plantation. Minimum dust gets generated during movement of dumpers on haul roads which are regularly sprinkled with water. The approach roads from mine to nearest transportation Road will be strengthened. Only emissions from truck trailers on these roads will be there but will get quickly dissipated. Therefore, no visible/significant effect on quality of soil is anticipated.

Mitigation Measures:  The construction/ strengthening of approach roads for evacuation of mineral masonry stone produce will not cause any degradation of land/soil.

 On closure of mining activity, excavated area will be used as water reservoirs.

 The top soil generation is minimal and will be utilized for plantation purposes and it will be stacked separately.

 Haulage roads will be kept moist by water sprinkling to reduce air pollution.

 Green belt will be developed along the both side of road to arrest the fugitive emission due to transportation and will minimize the propagation of air borne dust.

20.0 RISK ASSESSMENT & DIASASTER MANAGEMENT PLAN: Any type of mining activities requires stringent safety measures to avoid unwanted incidences which may damage life & machineries. It may cause widespread harm to assets and serious disruption at site as well as outside. Such situation requires quick

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action and emergency response plans which can be executed without the loss of time. Time factor is the essence in dealing emergencies to minimize the loss of human life and disruption of work. Any accident may develop into a major emergency even with the best safety measures and programmes in mining. Disaster management plan is formulated with an aim of taking precautionary steps to avert disaster and also to take such action after the disaster which limits the damage to the minimum. Hence, an emergency preparedness plan will be planned properly and documented for ease of implementation at the time of need without losing time and avoiding and delays.

OBJECTIVES OF DISASTER MANAGEMENT PLAN The objectives of DMP describe the company‟s emergency vigilance. The resource availability and actions in response to disaster, to deal with various types of situations that can occur at mines in short span of time. Thus the overall objectives of the emergency plan are summarized as:-

 To identify and assess emergencies, including risk impact assessment.  Rapid control of hazardous situation  Minimizing the risk and impact of event/ accident.  Effective prevention of damage to property.  Protect employees and people in vicinity by information about the risk and the role to be played in them in the event of emergency.  Records, equipment, etc. should be preserved and organize investigation in cause of emergency and preventive measures to stop its recurrence.  In order to achieve objectives of emergency planning, the critical elements that form the spine of Disaster Management Plan (DMP) are:-  Reliable and early detection of an emergency and immediate careful plan for action.

 The command, co-ordination and response organization structure along with availability of efficient trained personnel.

 The accessibility of resources for managing emergency situation.

 Appropriate emergency response action.

 Effective announcement and communication facility to inform at site.

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 Regular evaluation and revise DMP.

 Training of the concerned personnel.

 Steps taken for minimizing the effects may include rescue operations, first aid, evacuation, habilitation and communicating promptly to people living nearby.

Identification of Hazards and Mitigation Measures The following types of hazards are identified and precautions to be taken against them are enumerated below:- the following natural/industrial problems may be encountered during the mining operation:

 Slope failures at the mine faces.  Inundation-Filling of the mine pit due to excessive rains/flooding.  Accident due to fire.

Mitigation Measures for fall of Sides & Roof  Flatter slope angles are adopted where occurrences of loose earth are encountered.  Insurmountable heights are not created.  Loose rocks are properly dressed.  Nature and structure of the rocks are properly studied for their slips.  Bench height will be kept with respect to the digging depth of excavating equipment.  No overhang/ under cutting will be allowed to be created in benches by the excavating equipment‟s.  Overloading of dumpers strictly prohibited. Large dimension of material will not be loaded at the top of the dumpers to prevent falling and causing injury to persons.

Inundation-Filling of the mine pit due to excessive rains/flooding  Drainage will be maintained to reduce inundation of working pits during rain from surface run-off.  Garland drains will be constructed to prevent the water entering inside the mine.  Adequate capacity Sumps with will be developed inside the mine.  Adequate pumping capacity will be build up to deal of accumulated water.  Dumping area will be benched and sloped at the top towards the low altitude side.

Fire Fire generally occurs due to electrical short circuits, storage/handling of fuel oil, human carelessness, etc. Potential Impacts of fires are the burns, injuries and even

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loss of human life, property and loss of livelihood. Fire may interrupt services like power and communication. Environmental impacts include air pollution due to emission of harmful gases which may affect nearby settlements. Casualties during fire, some preventive measures will be taken to prevent the big damage to human life and property  Proper care should be taken during the storage/handling of fuel oil without any negligence is the key to protect the fire hazard. First aid will be provided for burning case and immediate treatment will be provided.  Adequate fire safety equipment‟s e.g. extinguishers, dry chemicals, carbon dioxide, foam spray, water spray should be kept.  Good cables should be used for preventing short circuits.  Move person to fresh air. Seek medical attention for discomfort or if coughing or other symptoms.  Rinse eyes thoroughly with water to remove all particles. Seek medical attention for abrasions and burns.

Accidents  Accidents High vehicular speed results in greater stopping distances and turning radii which lead to possibilities of accidents.  Transporting devices also contributes to serious accidents having potential to become fatal for the persons associated with such operations as well as those present in the vicinity at the time of accident.

Occupational Health and Safety The steps will to taken to minimize the impacts of mining activities and to ensure occupational health and safety during commissioning, operations and maintenance of mining equipment/machinery. It can be minimized by adopting below mentioned measures:-

 Periodic examination and testing of equipment, machineries and equipment handling substances.  Firefighting training to workers and Staff for first aid, safe handling of materials and integrating safety.  Suitable notices / boards displayed at several locations indicating appropriate hazards

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warning as well as DOs and DON‟T for ensuring operational and personal Safety for information of workers / staff and visitors.  Personnel protective equipment is provided to prevent the noise hazards.

Health and Safety Monitoring Plan  Each employee will undergo a proper medical examination.  All other employees will be medically examined as per rules that are 20% strength every year.

21.0 DETAILS OF THE OCCUPATIONAL HEALTH ISSUES IN THE DISTRICT (LAST FIVE YEAR DATA OF NUMBER OF PATIENT OF SILICOSIS & TUBERCULOSIS IS ALSO NEEDS TO BE SUBMITTED): No. of Patients No. of Patients No. of Patients reported of S.No. Year reported of reported of Any other SILICOSIS TUBERCULOSIS reportable diseases. 1. 2013-14 - 2. 2014-15 729 3. 2015-16 2114 4. 2016-17 1803 5. 2017-18 645

22.0 PLANTATION AND GREEN BELT DOVELOPMENT IN RESPECT OF LEASES ALREADY GRANTED IN THE DISTRICT: The greenbelt development plan aims to overall improvement in the environmental conditions of the region. The plan with a five-fold objective addresses issues such as prevention of land degradation due to activities during Mining operation, enhancing the forest cover for increasing the biodiversity of the region, providing aesthetic value to the project area for enhancing the ecological equilibrium of the area and to a large proportion in combating soil erosion.

NEED FOR GREENBELT DEVELOPMENT PLANWITHSCHEME FOR GREENBELT DEVELOPMENT The implementation for development of green belt will be paramount importance as it will not only add up as an aesthetic feature, but also act as a pollution sink.

The scheme of plantation in-side the cluster area is given as follows:

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(i) The species to be grown in the area should be dust tolerant and fast growing species so that permanent green belt is created.

(ii) The Green belt development will be done along the haul roads.

(iii) The Green Belt Development will be done nearby the mining leases to minimize the pollution level.

(iv) The green belt will be put under a protective regulatory framework to ensure that it is not degraded or disturbed. No ecologically disruptive activity will be allowed in this zone.

(v) The Green Belt Development should be Approx. 33% of the area of the mining lease.

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