the official portal of Karauli District, Rajasthan - DISTRICT ......Fairs and festivals have been the medium of culture in this area. The minerals found in this geographical area of

DISTRICT SURVEY REPORT, KARAULI

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DEPARTMENT OF MINES & GEOLOGY

GOVT. OF RAJASTHAN

KARAULI

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

Notification Date 25-07-2018)


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INDEX POINT

NO. PARTICULARS

1.0 INTRODUCTION

2.0 OVERVIEW OF MINOR MINERAL MINING ACTIVITY IN THE KARAULI DISTRICT

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

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

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

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

DUE TO MINING ACTIVITY

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

19.0 RECLAMATION OF MINED OUT AREA (BEST PRACTICE ALREADY IMPLEMENTED IN THE

DISTRICT, REQUIRMENT AS PER RULES AND REGULATION, PROPOSED RECLAMATION PLAN)

20.0 RISK ASSESSMENT & DIASASTER MANAGEMENT PLAN

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)

22.0 PLANTATION AND GREEN BELT DOVELOPMENT IN RESPECT OF LEASES ALREADY GRANTED IN

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 Dausa and Bharatpur districts, in the east by Dhaulpur

district, south by state of Madhya Pradesh and Sawai Madhopur 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‟, „Chambal

River Basin‟ and „Parbati River Basin‟.

Karauli is one of the holiest City of India 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 Raja Bijai Pal, a Jadon Rajput,

founded the modern princely state Karauli in 995. The local legends and Hindu

scholars believe that he was the 88th in descent of Lord Krishna. 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 Todabhim

spread over about 544 Sq.kms while population wise, Hindaun block has the highest

population and Nadoti has lowest population.

S.No BLOCK

NAME

Population

(Based on

2001census)

Area

(sq km)

% of

District

Area

Total

Number of

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. Mandrayal, 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 Karauli state along with

Hindaun and Gangapur of Jaipur 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 Jaipur state and became part of the United State of Greater Rajasthan. The

Government of Rajasthan 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, Chambal River, 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, Bharatpur district 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 Lalsot 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 Bayana. These rock units

are uncomfortably overlain by quartzites and metavolcanics of Alwar.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

Bhilwara 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, Rewa, 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


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Type Description

Hilly terrain in south,

southeastern part and

extremenorth-western part.

Hilly terrains are mainly confined to Karauli and

Sapotra blocks. The highestelevation is 525 m amsl

about 2.5 km. west of Chirawanda (in Nadauti block)

Isolated hills in

alluviumplain in central part

Major portion of district lying in northern, central

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

northernpart.

Hindaun, Nadauti, and Todabhim form mainly plain

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 Sawai Madhopur

district 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


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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 Jaipur district. 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 Udaipur and

enters Karauli district south and for a short distance forms the boundary with Tonk

district. 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

(sq. km) % Distribution

Older alluvium 145 2.88

Lies in parts of Todabhim and Nadauti

blocks. These are derived from

alluvium. They are non-calcareous, semi

consolidated to unconsolidated brown

soils, loamy sand to sandy loam in

texture. They are well drained and

occupy gently sloping terrains.

Lithosols and

Regosols of Hills 2359 46.82

Occupies the parts of Nadauti, Karauli,

Sapotra and Todabhim blocks. These are

formed on the Bhilwara hills, and hill

slopes. These soils are Shallow with

gravels very near the surface, light

textured, fairly drained, reddish brown

in colour. Cultivation is restricted

because of a limited root zone.

Recent Alluvium 2535 50.30

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

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:

S.No Particulars

Area

(Ha.)

Area (%)

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


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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.


22 | P a g e

Fig 1.6 Hydrogeology Map Of District Karauli


23 | P a g e

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


24 | P a g e

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.


25 | P a g e


26 | P a g e

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


27 | P a g e

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.


28 | P a g e

Fig 1.7 Index Map of District Karauli


29 | P a g e

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.


30 | P a g e

9.0 The List of Mining leases in the District with location, area and period of

validity, with EC Details-

s.no lease no Lessee Name

Mineral Name

Registration Date

Expiry Date Village/Tehs

il/District Total Area

DETAIL OF EC

DATE Capacity(in MT)

1 1/1992 Durga Prasad

Agrawal

Silica Sand

14-Mar-74 31-Jan-25

Dhoreri / Karauli / Karauli

4.68 24-5-16 266760

2 1/2205 Arvind Kumar Sharma

Sandstone

2-Nov-06 1-Nov-56

Mamchari / Karauli / Karauli

2.56 #N/A #N/A

3 11/2004 S.S.

Mineral Silica Sand

17-Jan-08 16-Jan-58

Barrif / Karauli / Karauli

4.78 2/6/201

6 140400

4 12/2005 Bacchu Sandsto

ne 23-Oct-08 22-Oct-58

Atewa / Karauli / Karauli

2.4 15-6-16 30000

5 138/2001 Mr.Pankaj

Kumar Mittal

Sandstone

28-Jul-03 27-Jul-53


1.17 2/6/201

6 19200

6 14/1989 Jhara

Granite Granite 1-Apr-90 3-Jan-40

Jhara / Nadauti /

Karauli 1

2/6/2016

30000

7 15/2009 Smt

Harpati Devi

Masonarystone, Millston

e

26-Mar-90 25-Mar-40

Talihil / Hindaun /

Karauli 1.27

2/6/2016

1000

8 157/2001 Ramesh Meena

Sandstone

16-Jan-05 15-Jan-55

Bugdar / Mandrayal /

Karauli 1.1 20-7-16 20000

9 2/1981 Bhori Lal

Jain Thekadar

Masonarystone, Sandsto

ne

6-Jul-61 31-Mar-25

Chobe Ki Gwari,Alwat

Ki Gwari / Sapotra /

Karauli

63.52 #N/A #N/A

10 36192 M/S

Ganesh Minirals

Silica Sand

1-Nov-03 30-Oct-53

Khirkhira / Karauli / Karauli

5 20-7-16 91080

11 20/2007 Fakeera Meena

Sandstone

18-Aug-08 17-Aug-58

Rajor / Karauli / Karauli

3.03 2/6/201

6 10000

12 213/2001 Vshnu Chand

Sharma

Sandstone

16-Sep-04 15-Sep-54

Bahadur Pur / Sapotra /

Karauli 1.17 NA NA


31 | P a g e

13 22/2001 Ashok Kumar Sharma

Sandstone

19-Oct-06 18-Oct-56


Karauli 1 NA NA

14 23/2006 Ajay Pratap

Singh Masonarystone

3-Nov-10 2-Nov-60

Dhugarh / Karauli / Karauli

1041 15-6-16 50000

15 25/1989 Smt.

Mamtesh Bhardwraj


ne

10-Jan-80 20-Sep-29

Bhadurpur,Bahadurpur /

Sapotra / Karauli

33.28 4/5/201

2 60000

16 27/1998 Indra

Agrawal Masonarystone

1-May-89 30-Apr-39

Manch / Karauli / Karauli

1 30-11-

16 80000

17 32/2000 Purshotta

m Lal Goyal

Masonarystone

6-Jun-03 5-Jun-53

Gunesara / Karauli / Karauli

1 NA NA

18 332/1981 Rajendra

Bharadwraj


ne

20-Jan-82 19-Jan-32

Bhadurpur / Sapotra /

Karauli 5.28 #N/A #N/A

19 4/1993 Rangilal Meena


ne

26-Nov-59 31-Mar-25 Karauli / Karauli

10 #N/A #N/A

20 27607 Haricharan

Lal Silica Sand

17-Nov-76 3-Jan-32

Gopal Garh / Karauli /

Karauli 4.58

2/6/2016

142400

21 40/1998 Pushpendr

a Kumar Sharma


ne

27-Feb-99 26-Feb-49

Bichpuri / Karauli / Karauli

2.03 2/6/201

6 30000

22 48/2009 Smt.

Koshllya Devi


ne

4-Oct-80 3-Oct-30

Lotda / Masalpur /

Karauli 18.54

3/8/2010

50000

23 5/2004 Om

Bhaibav Crushers

Masonarystone

20-Jan-07 19-Jan-57

Gunesari / Karauli / Karauli

1.01 23-5-16 85003

24 5/2013 Duarkapras

ad Gupta Masonarystone

11-Jan-13 10-Jan-63

Jahra / Nadauti /

Karauli 1 20-7-16 150280

25 50/2002 Prakash

Mali Masonarystone

15-Nov-02 14-Nov-52

Asthal / Karauli / Karauli

1 15-6-16 80000


32 | P a g e

26 54/1978 Bharosi

Devi


ne

19-Sep-79 18-Sep-29

Rajor / Karauli / Karauli

20.45 #N/A #N/A

27 55/2006 Janki Devi Ordinary

Clay 6-Jan-07 5-Jan-57

Bapoti / Sapotra /

Karauli 1.14 15-6-16 28840

28 7/1988 Mangi Lal Agrawal


ne

18-Jan-74 31-Mar-25

Piparani,Khunda /

Masalpur / Karauli

10 NA NA

29 7/2005 Ghanshyam Sharma

Sandstone

5-Dec-05 4-Dec-55

Bardeh / Mandrayal /

Karauli 1.05

2/6/2016

6000

30 74/1998 Jagan Lal Meena


ne

23-Jan-99 22-Jan-49

Gurdeh / Mandrayal /

Karauli 3.01 20-7-16 50000

31 8/1999 Kailaprasad Kumawat


ne

17-Jun-02 16-Jun-52

Parashari / Karauli / Karauli

4 2/6/201

6 10000

32 1/1989 Dwrika Prasad Gupta

Soapstone

14-Dec-98 13-Dec-48

Aam Ka Jhara /

Nadauti / Karauli

32.57 28-5-98 12000

33 10/2002 Kaptan Singh

Masonarystone

23-Jan-03 29-Jan-53

Manoharpura / Karauli /

Karauli 1

2/6/2016

30000

34 10/2003 Balveer Prasad Sharma

Sandstone

23-Sep-03 20-Sep-53

Batda / Mandrayal /

Karauli 1.72 20-7-16 20000

35 109/2001 Devkinandan Sharma

Sandstone

11-Jun-03 10-Jun-53


Karauli 1.23 20-7-16 10000

36 124/2004 Manju Devi Masonarystone

22-Dec-06 21-Dec-56

Bhartun / Sapotra /

Karauli 1 20-7-16 77314


33 | P a g e

37 13/2005

Integrated Glass

Materials Limited

Silica Sand

6-Jun-86 5-Jun-36

Manohar Pura /

Karauli / Karauli

4.95 #N/A #N/A

38 144/2001 Ramprasad

Gurjar Sandsto

ne 10-Jul-03 9-Jul-53

Mandi Bhat / Sapotra /

Karauli 1 NA NA

39 18/1995 Rajesh Kumar Gupta

Masonarystone

15-Apr-96 14-Apr-46

Salempur / Sapotra /

Karauli 1

9/5/2017

30000

40 19/1980 Tiwari

Jhumarlal Swrooplal


ne

8-Jan-82 31-Jan-25

Mahu,Karsai,Kalyani/Ma

mchari / Mandrayal,Karauli,Karaul

i / Karauli

98.38 29-12-

10 25225

41 192/2001 Indrajeet Sandsto

ne 11-Nov-05 10-Nov-55

Khera / Masalpur /

Karauli 1.89

2/6/2016

10000

42 193/2001 Indrajeet Sandsto

ne 11-Nov-05 10-Nov-55

Khera / Masalpur /

Karauli 2.04

2/6/2016

10000

43 2/1990 Indira Mittal

China Clay, Silica Sand

1-Jan-93 31-Dec-42

Ramhatra / Sapotra /

Karauli 4.9 20-7-16 165360

44 21/1994 Gopal Lal

Vyas


ne

7-Dec-95 6-Dec-45

Bhankari / Mandrayal /

Karauli 6.2

2/6/2016

15000

45 3/1997 Man Singh

Sain Masonarystone

30-May-98 29-May-48

Gunesasri / Karauli / Karauli

1 NA NA

46 3/2000 Indira Mittal


24-May-04 23-May-54

Ramhatra / Karauli / Karauli

4.09 2/6/201

6 50500


34 | P a g e

47 3/2002

Ms Jai Bhabhawa

ni Stone Companey

Masonarystone

26-Sep-02 25-Sep-52


Karauli 1

2/6/2016

50000

48 31/2004 Laxmi Devi

Sharma Sandsto

ne 10-Nov-04 9-Nov-54

Bahrai / Masalpur /

Karauli 1.05

3/6/2016

10000

49 34/2006 Smt Ginii

Devi

China Clay, Silica Sand, White Clay

6-Aug-09 5-Aug-59

Raghubansi / Karauli /

Karauli 4.8

2/6/2016

2980

50 35/1988 M/S Tajpur

Minerals Masonarystone

4-Jul-69 31-Mar-25

Baloti / Sapotra /


51 45/2002 Ramkumar

Sharma Sandsto

ne 30-Sep-05 29-Sep-55

Batda / Mandrayal /

Karauli 1 20-7-16 26260

52 5/1985 M/S Shri

Ram Mince & Minirals

China Clay,

Fireclay

3-Jan-86 2-Jan-36

Kaunti Pura / Sapotra /

Karauli 4.61 29-6-15 279000

53 51/2007 Arihant

Minerals

China Clay,

White Clay

27-Aug-08 26-Aug-58

Deep Pura / Karauli / Karauli

4.6 24.03.1

8 25168

54 52/2006 Hari Singh

Meena Sandsto

ne 26-Nov-10 25-Nov-60

Rundh Ka Pura /

Karauli / Karauli

1 20-7-16 40000

55 6/1992 Badri Lal Chouhan


ne

31-Dec-93 30-Dec-43 - 0.99 3/6/201

6 20000

56 67/2005 Pavan Kumar

Agarwal

Masonarystone

26-Oct-05 25-Oct-55

Chinayata / Hindaun /

Karauli 1

3/6/2016

30000

57 69/2002 Naval Singh Gurjar

Sandstone

27-Sep-03 27-Sep-53


1.12 15-6-16 10000


35 | P a g e

58 7/1970 Hind Khanij Silica Sand

5-Jan-77 4-Jan-27

Badreta / Todabhim /


59 7/1995 Manju Lata


ne

- 4-Apr-35

Batda / Mandrayal /

Karauli 8.05

27-10-16

24710

60 75/2002 Ramveer Meena

Sandstone

5-Dec-03 4-Dec-53

Manakhur / Mandrayal /

Karauli 1.09

3/6/2016

10000

61 76/1979 Jhoomar

Lal Agarwal


ne

9-Nov-79 8-Nov-29

Bahadurpur / Sapotra /

Karauli 115.36 NA NA

62 8/2002 Jaimata Di

Stone Kreshar

Masonarystone

15-Jan-03 14-Jan-53


Karauli 1

2/6/2016

50000

63 80/1992 Prahlad Gupta

Masonarystone

3-Sep-94 2-Sep-44


Karauli 0.53

9/5/2017

30000

64 87/1994 Kanhaiya

Lal Sharma


ne

26-Aug-96 25-Aug-46

P-N. 16, Halka No.- 13 / Karauli

/ Karauli

10 1/0/190

0 0

65 88/2004 Narendra

Kumar Sharma

Masonarystone

9-Dec-05 8-Dec-55

Kheri / Todabhim /

Karauli 1

2/6/2016

45000

66 97/2004 Vinay Kumar Goyal

Masonarystone

24-Dec-05 23-Dec-55

Kheri / Todabhim /

Karauli 1 20-7-16 90000

67 115/2004 Smt

Charan Bai Meena

Sandstone

24-Aug-05 23-Aug-55

Kanchanpur / Mandrayal

/ Karauli 1.03 20-7-16 30000


36 | P a g e

68 12/2000 Vishnu Chand Mittal


ne

4-Oct-00 3-Oct-50

Khorai / Karauli / Karauli

3.46 2/6/201

6 19200

69 125/2004 Arjun Singh Masonarystone

22-Dec-06 21-Dec-56

Bhartun / Sapotra /

Karauli 1 20-7-16 84480.5

70 13/1997 Babusingh

Rajput Masonarystone

31-Jul-97 30-Jul-47


1 15-6-16 50000

71 143/2001 Rajaram Gurjar

Sandstone

8-Jul-03 7-Jul-53


Karauli 1.12 NA NA

72 18/2002 Jaimata Di

Stone Kreshar

Masonarystone

23-Jan-03 20-Jan-53


Karauli 1

2/6/2016

50000

73 20/1999 Kaluram Meena

Masonarystone

18-Dec-89 17-Dec-39

Alikhamb Ka Pura,Jatwari / Sapotra /

Karauli

1 2/6/201

6 60000

74 25/1982 Nirmal Kumar Patni

Soapstone

- 31-Jan-25

Kamalpura / Todabhim /

Karauli 4.59 15-6-16 16070

75 25(N)/1998 Jai

Meenashwar Cre. Unit

Masonarystone

1-May-89 30-Apr-39


1 15-6-16 50000

76 26/1992 Prakash Chand Gupta


ne

16-Jun-82 15-Jun-32

Mandibhat / Sapotra /

Karauli 2.3

2/6/2016

15000

77 26/1998

M/S Jai Gurudev

Stone Cre. Co.

Masonarystone

1-May-89 30-Apr-39


1 9/5/201

7 70000

78 26/2003 Prakash

Chand Mali Masonarystone

16-Jul-04 15-Jul-54

Gopalpura / Karauli / Karauli

1.14 2/6/201

6 50000


37 | P a g e

79 26/2008

M/S Kumar Infrastruct

ure Developme

nts Pvt.

Silica Sand

16-Sep-13 15-Sep-63


Karauli 4.86

3/6/2016

190300

80 28/2004 Rajandar

Singh Masonarystone

- 10-Jan-55

Padla / Todabhim /

Karauli 1

2/6/2016

18000

81 30/1986 Rambharos

i Lal Sharma


ne

31-Aug-77 30-Aug-27

Gurdha / Mandrayal /

Karauli 16.32 NA NA

82 33/1992 Shrimati

Mulo Devi


ne

- 18-Oct-32

Baherda / Mandrayal /

Karauli 4.59 15-6-16 5000

83 38/2009 Pappi Devi Masonarystone

28-Jul-10 27-Jul-60

Bhanwarbra,32,33 /

Nadauti / Karauli

1 30-11-

16 44393

84 39/1986 Prabhu Lal

Agrawal


ne

19-Sep-59 31-Mar-25

Langara / Mandrayal /

Karauli 159.11 NA NA

85 39/2012 Aanandi

Lal Jangid

China Clay,

White Clay

23-Feb-18 22-Feb-68


4.875 9/5/201

6 35570

86 4/1997 Ramkesh

Mali Masonarystone

28-Jul-97 27-Jul-47


1 15-6-16 80000

87 4/2004 Shivshakti Minearals

Masonarystone

20-Feb-07 19-Feb-57

Guneshri / Karauli / Karauli

1 23-5-16 85002

88 48/2006

M/S Parul Infrastrech

ar Company Pvt.Ltd.

China Clay,

White Clay

23-Feb-18 22-Feb-68 JODI/SAPOTRA/KARAULI

4.854 30-11-

16 20800


38 | P a g e

89 5/2008 Sharda Meena

Masonarystone

26-Jul-10 25-Jul-60

Kheri / Todabhim /

Karauli 1 15-6-16 60000

90 55/1998 Giriraj Prasad Sharma


ne

3-Apr-00 2-Apr-50

Makanpur / Mandrayal /

Karauli 2.68 20-7-16 14000

91 58/2001 Mr.Manoj

Kumar Mittal

Sandstone

28-Jul-03 27-Jul-53


2.11 2/6/201

6 19200

92 60/2007 Rampati Meena

Masonarystone

- 20-Jan-59

Kheri / Todabhim /

Karauli 1

3/6/2016

112300

93 61/2007 Lakhan Singh

Masonarystone

4-Nov-09 3-Nov-59

Kheri / Todabhim /

Karauli 1

3/6/2016

97900

94 62/2007 Bhimsingh Masonarystone

4-Nov-09 3-Nov-59

Kheri / Todabhim /

Karauli 1

3/6/2016

98200

95 67/1998 Diwari Lal

Yadav


ne

31-Mar-99 30-Mar-49

Parashari / Karauli / Karauli

5 2/6/201

6 31200

96 68/2001 Ramraj

Mali Sandsto

ne 20-May-03 19-May-53

Baharda / Mandrayal /

Karauli 1.36 15-6-16 12000

97 7/1993 Thekedar Buddho

Devi


ne

- 2-Dec-43

Gari Ka Gavn /

Mandrayal / Karauli

4.55 20-7-16 15000

98 85/1980 Mahesh

Chand Om Praksah


ne

19-Sep-81 18-Sep-31 - - #N/A #N/A


39 | P a g e

99 9/1981 Kailash

Chand Jain

China Clay,

Soapstone

4-Mar-83 3-Mar-33

Pal / Nadauti /


100 99/2004 Shriram

Enterprises Masonarystone

24-Dec-05 23-Dec-55

Kheri / Todabhim /

Karauli 1 15-6-16 0

101 1/1973 Meetalal

Bohra Silica Sand

21-Dec-74 31-Mar-25

Kodai Gothra / Karauli / Karauli

263.05 NA NA

102 1/1984 Anjul Jadon


1-May-85 30-Apr-35

Dongari / Sapotra /

Karauli 4.95 15/6-16 107220

103 1/2004 Ram Shri Sandsto

ne 12-Apr-05 11-Apr-55

Dundapura / Karauli /

Karauli 1.27

3/6/2016

6000

104 1/2011 Anil Kumar

Goyal Silica Sand

16-Sep-13 15-Sep-63


Karauli 4.05 15-6-16 107220

105 16/1999 Nayim Kha Masonarystone

19-Feb-90 18-Feb-40


Karauli 0.85

9/5/2017

30000

106 16/2009 Jaisingh Rajput

Masonarystone

11-Nov-10 10-Nov-60

Khedi / Todabhim /

Karauli 1 15-6-16 60000

107 18/2003 Shailendra

Singh Gurjar

Masonarystone

- 13-Mar-58

Bhensina / Todabhim /

Karauli 1

3/6/2016

107970

108 20/2009 M/S

Mateshwari Minerals

Masonarystone

11-Nov-10 10-Nov-60

Khari / Todabhim /

Karauli 1 15-6-16 60000


40 | P a g e

109 209/2001 Banwari

Lal Sharma Sandsto

ne 6-Aug-04 5-Aug-54

Ledor Khurd / Masalpur /

Karauli 1.02

3/6/2016

10000

110 24/1990 Surendra

Kumar Sharma

Masonarystone, Millston

e

15-Jun-71 31-Mar-25

Talihill / Masalpur /

Karauli 4.96 NA NA

111 24/2008 Shivam Minrals

China Clay,

Felspar, Silica Sand, White Clay

23-May-12 22-May-62

Khavda / Sapotra /

Karauli 4.88 15-6-16 20787

112 25/2000 Vimla Devi Masonarystone

4-Apr-06 3-Apr-56

Kheri / Todabhim /

Karauli 1

2/6/2016

90000

113 26/1995 Sonu

Agrawal Ordinary

Clay 27-Jun-97 26-Jun-47

Kauntipura / Sapotra /

Karauli 1 #N/A #N/A

114 26/2007 Siya Suman

Stone Co .Keshpura

Sandstone

18-Feb-08 17-Feb-58

Keshpura / Masalpur /

Karauli 1 15-6-16 10000

115 28/1996 Kailash Chand Meena

Masonarystone

6-May-98 5-May-48


1 20-7-16 50000

116 33/1994 Kanhaiya

Lal Sharma


ne

9-Apr-96 8-Apr-46

Bhouder / Karauli / Karauli

8.89 27-10-

16 26520

117 35/2002 Bhagwati

Jatav Sandsto

ne 27-Jan-03 26-Jan-53


1.13 2/6/201

6 30000

118 4/1994

Ms Ramapura Minerals Pvt Ltd

Silica Sand

4-Oct-75 3-Oct-25

Ramapura / Karauli / Karauli

18.12 3/5/200

5 60000


41 | P a g e

119 48/2002 Ramswroo

p Mali Masonarystone

31-Mar-03 30-Mar-53


1 15-6-16 70000

120 5/1981 Satanand

Garg

China Clay,

Fireclay, Silica Sand

3-Dec-81 2-Dec-31

Khorra / Hindaun /

Karauli 4.5

2/6/2016

41280

121 50/2007 Milan

Minerals

China Clay,

White Clay

23-Aug-08 22-Aug-58


4.79 24-03-

18 21318

122 58/1997 Laxmi

Narayan Gupta

Masonarystone

- 23-Nov-38


Karauli 0.84

9/5/2017

30000

123 6/1993 Thekedar Buddho

Devi


ne

- 2-Dec-43

Gari Ka Ganv /

Mandrayal / Karauli

4.62 20-7-16 15000

124 6/2002

Ms. Jaibhawani

Stone Companey

Masonarystone

23-Jan-03 22-Jan-53


Karauli 1

2/6/2016

50000

125 63/2004 Jagmohan

Gurjar Sandsto

ne 24-May-08 23-May-58

Mahua Kheda / Karauli / Karauli

1.4 9/5/201

7 55764

126 9/1977 Dinesh Kumar Pandey


ne

4-Jul-77 3-Jul-27

Talbhari / Karauli / Karauli

144.91 #N/A #N/A

127 99/2001 Surendra

Singh Chouhan

Sandstone

12-May-03 11-May-53

Karsai / Karauli / Karauli

1 3/6/201

6 10000

128 1(N)/1999 Deepak Kumar Sharma


ne

26-Aug-00 25-Aug-50

Makan Pur / Mandrayal /

Karauli 4 20-7-16 10000


42 | P a g e

129 109/2004 Parmal Meena

Sandstone

20-Oct-05 19-Oct-55


1.92 23-02-

18 20000

130 11/2000

Rajasthan Sands & Clays Pvt

Ltd.

Silica Sand

6-Nov-71 31-Mar-25

Mijora / Sapotra /

Karauli 4.97 14-8-15 718000

131 16/1989 Kanhaiya

Lal Sharma


ne

9-Nov-79 8-Nov-29

B,Bahadurpur / Sapotra

/ Karauli 8.9 20-6-16 20000

132 16(N)/2000 Girraj

Prasad Gupta


ne

30-Sep-03 29-Sep-53

Kasara / Masalpur /

Karauli 4

20-07-2016

10000

133 164/2001 Hariom Sharma

Sandstone

4-Mar-03 3-Mar-53


1 20-7-16 17830

134 182/2001 Sirmohar Meena

Sandstone

1-May-03 30-Apr-53


Karauli 1.86

2/6/2016

10000

135 2/1994

Shree Bahirav Dham

Minerals

Silica Sand

20-May-75 19-May-25

Garain / Karauli / Karauli

4.8 21-8-15 223000

136 23/2000 Vimla Devi Masonarystone

16-Jun-03 15-Jun-53

Kheri / Todabhim /

Karauli 1

2/6/2016

90000

137 234/2001 Arun

Sharma Sandsto

ne 4-May-05 3-May-55

Bahrai / Masalpur /

Karauli 2

2/6/2016

10000

138 24/2000 Raghuraj

Singh Masonarystone

21-Aug-03 20-Aug-53

Kheri / Todabhim /

Karauli 1

2/6/2016

90000

139 25/1994 Rajendra Bhardwaj


ne

- 18-Jan-34

Batda / Mandrayal /

Karauli 10 19-6-10 8000


43 | P a g e

140 26/2008 Ramraj Gurjar

Sandstone

5-May-10 4-May-60

Raybeli / Sapotra /

Karauli 1.89

3/6/2016

190300

141 27/1980 Pushpenda

r Kumar Agrawal

Fireclay, Silica Sand

28-Dec-81 27-Dec-31

Ramapura / Karauli / Karauli

4.61 20-7-16 53500

142 27/1992 Prakash Chand Gupta


ne

18-Jun-82 17-Jun-32


Karauli 4.86

2/6/2016

15000

143 3/1990 Shubham Minerals

Silica Sand

10-Jun-93 9-Jun-43

Semerda / Karauli / Karauli

24.56 13-6-8 100000

144 3/2008 Mohamma

d Rafiq Khan

Silica Sand

16-Sep-13 15-Sep-63

Manohar Pura /

Karauli / Karauli

4.4 20-7-16 137410

145 31/2008 Mahipat

Lal Meena

China Clay,

Colidal Silica, Silica Sand, White Clay

21-Aug-14 20-Aug-64

Raghuvanshi / Karauli /

Karauli 4.75 24-5-16 65080

146 32/2001 Shshi

Bhardwaj Sandsto

ne 2-Mar-05 1-Mar-55


Karauli 1 NA NA

147 32/2004 Nawal Kishor

Sandstone

10-Nov-04 9-Nov-54

Bahrai / Masalpur /

Karauli 2.45

3/6/2016

10000

148 34/2009

Ms Jai Bhawani

Stone Crusher

Company


4-Jul-11 3-Jul-61

Guneshra / Karauli / Karauli

4 2/6/201

6 35000

149 36/1991 Kanti

Kumar Sharma


ne

13-Oct-81 12-Oct-31

Halka No 13 Karauli / Karauli / Karauli

10 NA NA


44 | P a g e

150 36/2001 Mamtesh Bhardwaj

Sandstone

8-May-03 7-May-53


Karauli 1.49 NA NA

151 4/1984 Shah

Surendra Kumar

Silica Sand,

Soapstone

21-Jan-65 31-Jan-25

Bhandari / Todabhim /

Karauli 4.98 15-6-16 8308

152 40/1987 Dhanno

Devi

Millstone,

Sandstone

24-Nov-77 23-Nov-27

Bapoti / Sapotra /

Karauli 0.72 NA NA

153 49/1986 Janardan

Singh Gahlot


ne

18-Oct-72 31-Jan-25

Sorya / Karauli / Karauli

180.05 30-4-10 45000

154 59/2001 Digambar

Dayal Chaturvedi

Sandstone

30-May-03 29-May-53

Makanpur , Batda /

Mandrayal / Karauli

3.15 20-7-16 10000

155 6/1982 Sudharsha

n Lal Silica Sand

3-May-83 2-May-33

Richoti / Karauli / Karauli

23.17 29-8-16 134500

156 6/1995 Narayan

Singh


ne

- 4-Apr-35

Batda / Mandrayal /

Karauli 8.25

27-10-16

19656

157 6/2000 Sunil

Kumar Sharma


ne

18-Jan-02 17-Jan-52


Karauli 3.23

2/6/2016

20000

158 62/2002 Bachchan

Singh Masonarystone

1-Jun-06 31-May-56

Jatwari / Sapotra /

Karauli 1 15-6-16 99000

159 67/2002 Reeta Devi Masonarystone

4-Sep-03 3-Sep-53

Khidrpur / Sapotra /

Karauli 1 15-6-16 90000


45 | P a g e

160 7/1976 Meetalal

Bohra Soapsto

ne 20-Feb-78 21-Feb-28

Gari / Todabhim /

Karauli 388.5 NA NA

161 8/1976 Shah

Surendra Kumar

Soapstone

- 31-Mar-25

Bhandari,Gadi Morda,

Rajoli / Todabhim /

Karauli

24.74 8/7/200

8 63000

162 9/2009 Shyam Gopal Singh

Masonarystone

19-Sep-11 18-Sep-61

Selampur (Tamoupura) / Sapotra /

Karauli

1 NA NA

163 91/2001 Piyush

Updhyay Sandsto

ne 10-Feb-04 9-Feb-54


Karauli 1 NA NA

164 96/2004 Hansram Meena

Masonarystone

24-Dec-05 23-Dec-55

Kheri / Todabhim /

Karauli 1 15-6-16 90000

165 98/2004 Maluk Chand Goyal

Masonarystone

24-Dec-05 23-Dec-55

Kheri / Todabhim /

Karauli 1 20-7-16 90000

166 1/1996 Shivkumar

Diwedi

Barytes, China Clay,

Fireclay, Quartz, Soapsto

ne

22-Apr-99 21-Oct-49

Talchira / Nadauti /

Karauli 133.08 18-2-99 26115

167 1/1998 Indira

Agrawal Silica Sand

3-May-79 2-May-29


Karauli 4.99 29-6-15 30000


Agarwal

White Clay

4-Dec-69 31-Mar-25

NAROLI/SAPOTRA/KARA

ULI 4.91

17-12-15

361000


46 | P a g e

169 12/1985 M/S Sagar Minerals


16-Dec-86 15-Dec-36

Bariya / Karauli / Karauli

4.89 15-6-16 60000

170 129/2001 Babu Dayal

Singh Masonarystone

6-Jan-03 5-Jan-53

Bhenesna / Todabhim /

Karauli 1

3/6/2016

67870

171 14/2006

Integrated Glass

Materials Limited

Silica Sand

4-Nov-08 3-Nov-58


12.36 8/7/200

8 310000

172 16/2002 Ashok Kumar

Agarwal

Masonarystone

31-May-04 30-May-54

Dantali / Todabhim /

Karauli 1

3/6/2016

108000

173 16/2004 Vidhya

Devi Silica Sand

28-Aug-06 27-Aug-56

Pura Ata / Karauli / Karauli

0.65 NA NA

174 163/2001 Sharad

Bhardwaj Sandsto

ne 3-Mar-05 2-Mar-55


Karauli 1.4

3/6/2016

36000

175 17/2000 Hanuman Sahay Sain


ne

22-May-03 21-May-53

Kasara / Masalpur /

Karauli 4.5

30-11-16

100000

176 17/2003 Beerbhadu

r Singh Masonarystone

- 13-Jan-58

Bhensina / Todabhim /

Karauli 1

3/6/2016

126300

177 19/1985 Arvind Tiwari


ne

9-Dec-91 8-Dec-41

Makan Pur Swami,Mak

anpur Swami /

Mandrayal / Karauli

40.36 NA NA


47 | P a g e

178 20/1994 M/S

Vatsala Minerals


ne

9-Jul-84 8-Jul-34

Gari Ka Gavn /

Mandrayal / Karauli

10 27-10-

16 30888

179 21/2009 Bhim Singh Masonarystone

11-Nov-10 10-Nov-60

Kheri / Todabhim /

Karauli 1

30-11-16

96000

180 22/2000 Gajraj Singh

Masonarystone

16-Jun-03 15-Jun-53

Kheri / Todabhim /

Karauli 1

2/6/2016

200000

181 28/2000 Kumer Meena


ne

13-Jul-00 12-Jul-50

Makanpur , Batda /

Mandrayal / Karauli

1.16 20-7-16 25000

182 3/1995 Indira

Agrawal Colidal Silica

31-Jan-77 30-Jan-27


Karauli 22.6 29-6-15 30000

183 30/1998 Dinesh Chand

Rajaram


ne

- 18-Sep-38

Makanpur , Batda /

Mandrayal / Karauli

8.99 27-10-

16 30036

184 33/2006 Anita

Sharma White Clay

12-May-14 11-May-64

Seba / Gangapur

City / Sawaimadh

opur

4.9 2/6/201

6 20900

185 34/2004 Jitendra Sharma

Sandstone

10-Nov-04 9-Nov-54

Bahrai / Masalpur /

Karauli 2.29

3/6/2016

10000

186 35/1991 Radhey Shyam Goyal

Millstone

15-Jun-71 31-Mar-25

Talihill / Masalpur /

Karauli 7.78 NA NA

187 39/2000 Vishan Lal

Meena


ne

29-Oct-01 28-Oct-51


Karauli 5 15-6-16 6000


48 | P a g e

188 4/1982

Silica Corporatio

n Gangapur

City

Silica Sand

3-May-83 4-May-33

Alampur / Karauli / Karauli

4.68 2/6/201

6 81850

189 42/1996 Rajesh Kumar Gupta

Masonarystone

13-Mar-00 12-Mar-50


Karauli 0.94

24-03-2018

49190.8

190 46/1997 Unkar Lal

Garg Masonarystone

29-May-98 28-Aug-48


Karauli 1

3/6/2016

42820

191 47/1988 Geeta Devi

Sharma


ne

9-Nov-79 8-Nov-29



192 49/1998 Munni Devi


ne

29-Aug-00 28-Aug-50


Karauli 1.38

31-11-16

50000

193 49(N)/1998 Shyam Lal

Mali Masonarystone

- 30-Nov-39


Karauli 1

31-11-16

50000

194 54/1998 Sitaram

Mali


ne

18-Jan-99 17-Jan-49


Karauli 2.51 20-7-16 11000

195 56/1986 Bhoru Singh

Jadoun


ne

30-Sep-77 29-Sep-27 / Karauli /


196 6/2006 Rajesh Meena

Masonarystone

14-Feb-07 13-Feb-57

Tamolipura / Sapotra /

Karauli 1

2/6/2016

216000

197 62/2005 Dronacharya Sharma

Masonarystone

26-Oct-05 25-Oct-55


Karauli 1

3/6/2016

30000


49 | P a g e

198 63/1997 Hajari Lal

Bariwa Masonarystone

28-Mar-98 27-Mar-48

Baloti / Sapotra /

Karauli 1

2/6/2016

90000

199 67/1991 Dev Vrat Meena


ne

27-Jun-72 31-Mar-25

Gurdah / Mandrayal /

Karauli 46.32 NA NA

200 75/2001 Rukmini Sharma

Sandstone

7-Jun-03 6-Jun-53

Makanpur , Batda /

Mandrayal / Karauli

1.17 20-7-16 25000

201 85/2004 Shri Ankit

Mittal Masonarystone

25-Jan-08 24-Jan-58

Kheri / Todabhim /

Karauli 1 15-6-16 150000

202 9/1995 Krishnanand Sharma

Masonarystone

21-Dec-95 20-Dec-45


Karauli 0.84

9/5/2017

30000

203 92/2004 Jai Balaji

Stone Cre. Masonarystone

11-Aug-08 10-Aug-58

Kheri / Todabhim /

Karauli 1

2/6/2016

60000

204 1/1998 Narayan

Singh Rajput


ne

- 5-May-38


Karauli 9.19 29-6-15 30000

205 1/2007 Sumer Singh

Masonarystone

1-Apr-08 31-Mar-58

Jatwari / Sapotra /

Karauli 1 20-7-16 98724

206 10/2006 Brahmanand Sharma

Sandstone

25-Jan-07 24-Jan-57

Batda / Mandrayal /

Karauli 1.01

2/6/2016

29999.5

207 105/2004 Jailal Mali Sandsto

ne 21-Aug-06 20-Aug-56


1.96 3/6/201

6 10000

208 108/2004 Nagesh Meena

Sandstone

13-Mar-08 12-Mar-58 / Sapotra /

Karauli 2.42 20-7-16 42321.2


50 | P a g e

209 12/1976 Prakash Chand

Murari Lal

Silica Sand

8-Aug-77 7-Aug-27

Dhorera / Karauli / Karauli

15.54 27-10-

16 225260

210 13/1989 Vijay Singh

Jadaun


ne

16-Dec-74 31-Mar-25

Binega / Masalpur /

Karauli 4.48

2/6/2016

5000

211 14/2001 Shivkumar

Diwedi Masonarystone

10-Sep-03 9-Sep-53

Talchira / Nadauti /

Karauli 1 NA NA

212 15/1997 Purshttom

Gupta Masonarystone

4-Aug-97 3-Aug-47


1 NA NA

213 15/2003 Jagdish Prasad Sharma

Sandstone

6-Nov-04 5-Nov-54

Batda / Mandrayal /

Karauli 0.99

2/6/2016

30000

214 16/1997 Shri.

Omprakash Mali

Masonarystone

31-Jul-97 30-Jul-47


1 15-6-16 70000

215 19/2003 Jamuna Lal

Mali Masonarystone

19-Sep-03 18-Sep-53


1 2/6/201

6 50000

216 2/1996

M/S Krishan Kumar Deepak Kumar Stone

Company


ne

28-Jan-77 27-Jan-27

Langra / Mandrayal /

Karauli 48.53

27-10-16

20000

217 27/2003 Jamuna Lal

Mali Masonarystone

16-Jul-04 15-Jul-54


1.27 2/6/201

6 50000

218 27/2004 Sidhdata

Stone Crusher

Masonarystone

- 10-Apr-55

Padla / Todabhim /

Karauli 1

2/6/2016

18000

219 3/1999

Ms Ramapura Minerals Pvt Ltd

Silica Sand

1-Nov-03 31-Oct-53


5 NA NA


51 | P a g e

220 3/2004 Ms

Ashutosh Minerals

Masonarystone

20-Feb-07 19-Feb-57


1 #######

# 85001

221 30/1990 Rajendra

Dayal Gupta


ne

7-Aug-81 6-Aug-31

Langra / Mandrayal /

Karauli 165.3

3/5/2012

18000

222 37/1994 Bhanwar

Singh


ne

7-Jan-98 6-Jan-48

Bhoder / Karauli / Karauli

4.89 3/6/201

6 180000

223 37/2006 Shreebhan

Singh Gurjar

Sandstone

25-Mar-08 24-Mar-58

Kheda / Karauli / Karauli

1 2/6/201

6 10000

224 4/1976 Ms.

Jagdamba Minerals

Silica Sand

3-Dec-76 2-Dec-26

Leida Khirkhira / Sapotra /

Karauli

23.73 2/9/201

6 150000

225 4/2008 Mahalaxmi

Minerls Silica Sand

16-Sep-13 15-Sep-63

Manohar Pura /

Karauli / Karauli

4.4 20-7-16 128570

226 5/1997 Ramotar

Singh Masonarystone

21-Aug-97 20-Aug-47


1 15-6-16 80000

227 5/2001 Jaganram

Meena Silica Sand

23-Aug-08 22-Aug-58

Bichpuriya / Karauli / Karauli

4.36 2/6/201

6 118780

228 53/2007 Anantraj

Mines And Minarals

China Clay,

White Clay

23-Aug-08 22-Aug-58


4.79 24-03-

18 10200

229 55/2003 Mohan Lal

Sharma Sandsto

ne 3-Jan-04 2-Jan-54

Harnagar / Karauli / Karauli

2.07 20-7-16 3000

230 6/1976 Rup

Narayan Pandey


ne

6-Oct-71 31-Mar-25

Kalayani / Karauli / Karauli

92.51 26-8-12 30000


52 | P a g e

231 7/1990 Mularam Meena


ne

15-Sep-80 14-Sep-30

Gari Ka Gaon /

Mandrayal / Karauli

4.87 20-7-16 15000

232 70/1998 Rupram Meena


ne

15-Jan-98 14-Jan-48


2.5 20-7-16 10000

233 74/2004 Ms Shriram

Laddu Baba

Masonarystone

9-Sep-09 31-Aug-59


Karauli 1

2/6/2016

50000

234 8/1979

Ms. Girrajdhara

n Enterprises

Silica Sand

25-Sep-80 24-Sep-30

Loharra / Karauli / Karauli

38.85 NA NA

235 8/2000 Jagdish Meena


ne

25-Feb-02 24-Feb-52


Karauli 4.95

2/6/2016

5000

236 11/2005 Ramsahay Sandsto

ne 20-Aug-08 19-Aug-58


2.4 NA NA

237 13/2003 B.L.

Bagouriya Sandsto

ne 30-Sep-03 29-Sep-53

Akolpura / Karauli / Karauli

1 2.6.201

6 10000

238 158/2001 Ramphool

Meena Sandsto

ne 24-Jul-03 23-Jul-53


Karauli 1.08 20-7-16 20000

239 16/2010 Anfal

Mineral

China Clay,

White Clay

21-Aug-14 20-Aug-64

Kaunti Pura / Sapotra /

Karauli 4.06

23-05-16

52062

240 165/2001 Khem Chand

Sharma

Sandstone

27-Apr-06 26-Apr-56

Bahrai / Masalpur /

Karauli 1.35

3/6/2016

10000


Agrawal

Silica Sand

18-Feb-74 31-Mar-25

Mijora / Sapotra /



53 | P a g e

242 20/2008 Gunjan Bindal

Masonarystone

- 2-Jan-60

Kheri Hewat / Hindaun /

Karauli 1

15-06-16

30000

243 200/2001 Nand

Kumar Sharma

Sandstone

14-Aug-03 13-Aug-53

Makanpur , Batda /

Mandrayal / Karauli

1.55 20-7-16 25000

244 22/2006 Sashi

Kanwar Masonarystone

3-Nov-10 2-Nov-60

Dhugarh / Karauli / Karauli

1 15-6-16 60000

245 228/2001 Geeta Devi

Sharma Sandsto

ne 23-Sep-03 20-Sep-53


Karauli 1.44 20-7-16 20000

246 29/2004 Chuttan Lal

Meena Masonarystone

11-Apr-05 10-Apr-55

Padla Jagir / Todabhim /

Karauli 1

2/6/2016

18000

247 33/2004 Devisharan

Shrma Sandsto

ne 10-Nov-04 9-Nov-54

Keshpura / Masalpur /

Karauli 2.22

3/6/2016

20000

248 34/1994 Kanta

Sharma


ne

28-Jan-98 27-Jan-48

Bhoder / Karauli / Karauli

10 27-10-

16 32614

249 34/1998 Mohm. Rafiq

Masonarystone

24-May-00 23-May-50


Karauli 1

31-11-16

50000

250 38/1998 Bhagwan

Singh Gurjar

Masonarystone

- 29-May-52

Jodhapur / Todabhim /

Karauli 0.8

1/0/1900

0

251 39/1991 Sunayana Sharma


ne

28-Oct-76 27-Oct-26

Gurdeh / Mandrayal /

Karauli 245

2/5/2012

27000


54 | P a g e

252 49/2002 Ramswroo

p Mali Masonarystone

31-Mar-03 30-Mar-53


1 15-6-16 70000

253 51/2012 M/S

Natural Minerals

China Clay,

White Clay

23-Feb-18 22-Feb-68


4.95 16-5-16 43910

254 57/1998 Ramji Lal Meena


ne

17-May-99 16-May-49


Karauli 3.85 20-7-16 20000

255 6/2004 Ghusmeswer Crushers

Masonarystone

20-Feb-07 19-Feb-57


1 #######

# 85000

256 62/2001 Narayan

Lal Meena Sandsto

ne 1-May-03 30-Apr-53


Karauli 1.6

2/6/2016

10000

257 63/2007 Laxminarayan Sharma

Masonarystone

- 20-Nov-59

Kheri / Todabhim /

Karauli 1 15-6-16 89212

258 66/2004 Udaybhan

Singh Sandsto

ne 30-Dec-04 29-Dec-54

Mahua Khera /

Masalpur / Karauli

1.04 2/6/201

6 10000

259 74/2002 Virendra Kumar

Sandstone

6-May-03 5-May-53

Lotda / Masalpur /

Karauli 1.92 15-6-16 10000

260 78/1979 Rambeti

Devi


ne

9-Nov-79 8-Nov-29

Bahadurpur / Sapotra /

Karauli 45.49 NA NA

261 8/1987 Arivand Kumar


ne

14-Jul-77 13-Jul-27

Guberda,Gurbera /

Masalpur / Karauli

150.93 23-4-12 15000


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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 - - -

262 8(N)/1987 Yogesh Kumar Gupta


ne

11-Jan-99 10-Jan-49



263 80/2002 Halki Sandsto

ne 24-Jul-03 23-Jul-53


Karauli 1.27

2/6/2016

10000

264 37865 Rama

Minerals Silica Sand

9-May-06 8-May-56

Manohar Pura /

Karauli / Karauli

5 20-7-16 128570

265 9/06 Pancham

Stone Company

Sandstone

18-Jun-07 17-Jun-57

Chobe Ki Gwari /

Sapotra / Karauli

1.57 #N/A #N/A

266 91/2004 Jai Balaji

Stone Cre. Masonarystone

8-Dec-55

Kheri / Todabhim /

Karauli 1

2/6/2016

60000


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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


60 | P a g e

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


61 | P a g e

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


62 | P a g e

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


63 | P a g e

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.


65 | P a g e

(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


70 | P a g e

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):

S.No. Year

No. of Patients

reported of

SILICOSIS

No. of Patients

reported of

TUBERCULOSIS

No. of Patients

reported of

Any other

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.

Documents

the official portal of Karauli District, Rajasthan - DISTRICT ......Fairs and festivals have been the medium of culture in this area. The minerals found in this geographical area of