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DISTRICT MINERAL SURVEY REPORT

DISTRICT LEVEL ENVIRONMENT IMPACT

ASSESSMENT AUTHORITY


2

(DEIAA)

CHITRADURGA DISTRICT

District mineral survey report

Sl.NO. Contents Page

No.

1 Introduction

2 Brief History Of The District

3 Salient Feature Chitradurga

4 Geology and Geolmorphology

5 Geohydrology and Occurance of Ground water.

6 Drainage System of Chitradurga.

7 Details of Availability of Sand

8 Mineral resources of Chitradurga


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INTRODUCTION

Chitradurga District is located 200km NW from Bangalore, bounded by

the geographical coordinates North Latitudes 13º 34' 20" to 15º 47' 10" to East

Longitudes 76º 01' 30" 77º 01' 35". The District is having a geographic area

of 8388.78 sq kms.

BRIEF HISTORY OF THE DISTRICT

Chitradurga district has a hoary past dating back to the pre-historic and

legendary times. According to a tradition, it was near the Jatinga Rameshvar hill

of this district that Jatayu challenged Ravana when, having abducted Sita, the

latter was passing through this part of the country with her on his way to Lanka.

According to another, during the period of their exile the Pandava brothers and

their mother Kunti stayed for some time near Chitradurga hills.

Some of the pot-shreds discovered in the pre-historic sites of the district

are stated to be similar to those found in the Indus Valley, Sumer and Crete of

the 3rd millennium B.C. Further, the ancient local culture which has been

designated as "Roppa Culture" is said to be similar to the campiguin culture of

France belonging to the period from 8000 B.C. to 6000 B.C.

Chitradurga features bold rock hills and picturesque valleys, huge towering

boulders in unimaginable shapes. It is known as the "stone fortress" (Kallina

Kote). The landscape looks much like a mischievous giant's playground, with

boulders thrown around, forming silhouettes against the sky. According to a

story in the Epic Mahabharatha, a man-eating gaint named Hidimbasura lived

on the Chitradurga hill and was a source of terror to everyone around. When the

Pandavas came with their mother Kunti in the course of their exile, Bhima had a

duel with Hidimba. Hidimba was slain by Bhima and peace returned to the area.

Legend has it the boulders were part of the arsenal used during that duel. In fact,

the boulders on which major part of the city rests belong to the oldest rock

formation in the country.


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Timmana Nayaka a chieften under the Vijayanagar empire rose to the rank of

governor of Chitradurga as a reward for his excellence in military achievements,

from the Vijayanagara ruler. This was the beginning of the rule of the Nayakas

of Chitradurga. His son Obana Nayaka is known by the name Madakari Nayaka

1588 CE. Madakari Nayaka's son Kasturi Rangappa 1602 succeeded him and

consolidated the kingdom to rule peacefully. As he had no heirs to succeed him,

his adopted son, the apparent heir was enthroned but was killed in few months

by the Dalavayis.

Chikkanna Nayaka1676 the brother of Madakari Nayaka II sat on the throne,

and his brother succeeded him with the title Madakari Nayaka III in 1686. The

unwillingness of Dalawayis to accept Madakari Nayaka III's rule gave an

opportunity to one of their distant relatives, Bharamappa Nayaka to ascend the

throne in 1689. He is known as dthe greatest of the Nayaka rulers. Somehow,

the subjects of Chitradurga did not experience a good reign of the successive

rulers as they ruled on the throne for very brief periods. The Hiri Madakari

Nayaka IV 1721, Kasturi Rangappa Nayaka II 1748, Madakari Nayaka V 1758

ruled this area but there is not much to mention of their rule.

Chitradurga Fort:-

The old walled Town houses the impressive fort, built on the north eastern base

of a cluster of rocky hills, qualifying it to be a Giridurga, or hill fortress.

Known as Yelu Suthina Kote, the fort is fortified by seven circular walls, three

of which are on the ground and four on the hill. Chitradurga fort is said to have

had 19 majestic doors, 38 smaller doors, 35 special entry points and four secret

entrances. The fort is entered through four gateways of the outermost wall. The

foothills of the fort constitute the main residential area of the town. The Mel

Durgas, forts on the hill are embellished with extensive fortifications, ramparts,

bastions, batteries, watchtowers and entrances located at strategic points and


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house fourteen temples. Some of the fort’s important landmarks are Thuppada

Kola Betta, Hidimbagiri, Zadaa Battery (Flag battery), Kahale Battery (Trumpet

battery), Lal Battery (Red battery) and Nellikai Battery (Gooseberry battery).

The main entrance to the fort, Kamanbhavi, has carvings of the seven – hooded

cobra the legendary twin headed bird, Gandaberunda, the royal

swan,Rajhamsa and lotus flowers.

CHITRADURGA DISTRICT SALIENT FEATURE 1. AREA-

a)Total Geographical area 8388.78Sq.kms

b) Cultivated land 5022.80 Sq.kms

c) Un Cultivated land 245.03 Sq.kms

d) Fallow land 808.51 Sq.kms

e) Forest land 737.19 Sq.kms

) Non Agriculture use land 512

g) Irrigation land

-Major Irrigation (12140.00 hecter) 2560 hect.

-Minor Irrigation (21451.81 hecter) 5419 hect

-Ground water net Irrigation 2014-15 - 24417 hect.

2.GEOGRAPHICAL Long 76º 01'30" to 77º 01' 35"

COORDINATES Lat 13º 34' 20" to 15º 47' 10"

3. TALUKS:

1.Chitradurga

2.Chalkere

3.Hiriyur

4.Holalkere


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5.Hosadurga

6.Molkalmur.

4.VILLAGES: Habitated 948 nos

Un Habitated 112 nos (As per 2011 census)

5. BASIN: Krishna (8321.91 Sq.kms)

6.SUB BASIN: a) Tungabadra 956.04 Sq Kms

b) Vedavathi 7365.87 Sq.kms

7.COMMAN CROPS: Khariff : Ground nut, sun flower, Jower,small millets

and pulse

8. TEMPARATURE Mean minimum Temperature 16.70 to 280C December

Coldest month. Mean minimum Temperature Hottest month April 34.90C

10.GEOLOGY: Mainly Comprises of Granite, Granite Gneis, Schistose

And Lime stone / Dolomite & Dykes.

11.Average Annual Rain fall - 2015: 438 mm

12.METEOROLOGICAL ASPECTS: a) Climate : Arid to Semiarid

b) Humidity

1) The least mean relative humidity value of 40% is noticed in February &

March.

2) The high mean relative humidity value of 70% is noticed in june to

september the Vapour pressure varies from 10.3 to 11.6mm Hg during

December to March.

3) The vapour pressure increases to 16.4 to 17mm hg during SW monsoon

season.

4) The low wind speed of 6.2 to 6.3 kmphs is found during june and july

month.

5) The high wind speed of 14.2 to 14.9 kmphs is found during june and july

month.

6) January & feb months are Dry seasons March,April & May months are

pre monsoon June, July,Auguest,September & October months are

Monsoon.

November December months Post monsoon.

13. Monitoring system : 47 Observation Wells In The District

Dug wells in the Network-06

Bore well in the Network -41


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GEOLOGY:-

The main rock types, their distribution and mode of occurrence of ground water in the

different rock are as below.

Main rock types are Igneous and Metamorphic rocks are as follows:

I. Igneous rocks: Granites, Dykes and Pegmatites

II Metamorphic rocks: Chlorite Schist, Hornblend Schist , Granitic Gneiss

Both the Schistose and Gneiss rocks are Striking in NNW-SSE direction,

and are light green to grayish in colour where as granitic gneiss is light gray to

dark gray in color, with medium to fine grained in texture and compact in nature

and are vertically dipping East. Granite are located at NE part District i.e in

Molkalmur Taluk and central part i.e, NNW of Chitradurga Taluk in and to


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some extent in the NW part of the District, and the Central part of Hosdurga

Taluk extending up to South of Holalkere Taluk.

Sl.No Taluka

Geological area distribution

in Sq.Kms. Total

Granite Gneiss Schist

1 Challkere 85 1938 40 2063

2 Chitradurga 270 457 649 1376

3 Hiriyur 0 660 1041 1701

4 Holalkere 28 677 390 1095

5 Hosadurga 140 990 286 1416

6 Molakalmur 495 215 0 710

District total area 1018 4937 2406 8361

Distribution of rocks in Chitrdurga District.

Approximate Areal extent Rock Types

Prominent Aquifers.

87.80 % Metamorphic rocks Schist (2406 Sqkms)

Gneiss (4937 Sq.kms)

12.20 % Igneous rocks Granites (1018 Sq.kms)

SUB SURFACE LITHOLOGY.

Prominent lithology, encountered and their variations.

1. Top soil 0.15 to 4m

2. gravelly soil 0.30 to 2m

3. Highly weathered rock: 1.50 to 20m ( Granite, Granite Gneiss,

Schistose)

4. Weathered rock: 20 to 30m ( Granite, Granite Gneiss, Schistose,

with joint//fractures)

5. Semi weathred rock: 30 to 60m (Granite, Granite Gneiss, Schistose,

with joint / fractures)

6. Hard rock with fracture: 60 to 90m


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7. Hard rock with isolated fractures 90 to 120m

8. Fresh parent rock >120m

GEOHYDROLOGY AND OCCURANCE OF GROUND WATER.

The above major rock units are Hard, crystalline Rocks, which have been

subjected to Tectonic Movements. The process of weathering produces joints

primarily by means of Temperature effect on Rock, as well as by Chemical and

physical action of Flowing Water. So produced joints by weathering rapidly lies

down within the upper 30 to 50mts in most Cases.

The most dense joint sets of the above origin can be observed in the upper

portion of the hard rock massifs. These joints may either open filled

(mineralized) fill being represented by sandy, clayey material or veins of

Quartz.

The character and extent of joint depends upon the composition and

hardness of the rocks. Harder rocks are less rapidly disintegrated, hence joint

penetrate them down to smaller depths.

In hard rock formation cut by differently oriented and mutually

intersecting joints can also be seen. Granites and other crystalline rocks often

contain little water. Which extend down to the depths of 30 to 50 meters and

very rarely 100mts.

The distribution and migration of ground water in jointed rocks are

variable, being dependent upon the Character, origin, and size of the cracks.

Joints in hard rock contain both Semi confined and unconfined ground water.

Ground water head is commonly produced by the Hydrostatic pressure in

intersecting joints, some of which occur in a recharge area at higher altitudes,

where the rain water and surface water infiltrate into the ground, in other places,

the water pressure in cracks in cracks is related to the pressure of gases

ascending from lower zones of the lithosphere. Major fracture zones also


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contain ground water and these acts as good aquifer. Metamorphic rocks are

mainly Hornblende Schist and Chlorite Schist and Granite Gneiss.

The prominent water bearing zones are Secondary structures such as pore

space, joints and fractures in the different rock types that act as good Aquifers.

The depth of weathering zone varies from 10 to 20m. The depth of joint/

fracture zone varies from 20 to 90 m and the isolated fracture and joints may

extend down to a depth greater than 90m but less than 120m. Major structural

features, are fractures and fissures that occur in the rocks, than these features

acts as sub surface reservoir to hold and discharge ample quantity of ground

water.

GEOLOGY AND AQUIFER SYSTEM.

The rainfall precipitation is the only source for ground water recharge.

The total recharged water will be stored approximately at the following depth in

all geological setup. The thickness of the water bearing formation i..e, aquifer as

follows.

Maximum water will be stored in weathered / jointed / fractured rock

formations, up to a depth of 30m below ground level(bgl) and it accounts

approximately to tune of 65%to 75% of the total estimated ground water

recharge and 10% to 15% of the ground water will be stored at a depths ranges

from the 30 to 60m (bgl) in semi weathered rock formations (Granite, Granite

Gneiss, Schist) with joint / fractures, and 5%-10% of the ground water will be

stored at a depths ranges from the 60 to 90m (bgl) in hard rocks with fractures

and less than 5% of ground water will be stored at a depths ranges 90-

130m(bgl) in hard rock, with isolated fractures.

Review of ground water quality changes.

The objectives of the water quality monitoring net work is to:

Establish the Bench mark for different water quality parameters


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Compare the different parameters against the national standards.

Detect water quality changes with time

Identify potential areas that show rising trend

Detect potential pollution sources

Study the impact of land use and industrialization on ground water quality.

To study the ground water chemistry, ground water quality-monitoring

network, has been established at 47 villages. From all the stations Base and

Trend water samples are collected and analyzed since many years. It is

observed from the analyzed report that Base samples shows higher

concentration of the substances or Characteristics like PH, CaCo3, Cl, Fe,

TDS, SO4,F and NO3 when compared with Trend samples Characteristic

Values. Ti is also noticed that concentration of the substances became low

and dispersion will be more in large area in Trend samples. The frequency of

monitoring for ground water quality is changed as base line monitoring where

as samples are collecting once in a year (one time a year) wells showing

abnormal parameters for trend monitoring (2 times a year) where as wells for

surveillance monitoring nil.

AQUIFER SYSTEM IN CHITRADURGA DISTRICT.

Sl.

No

Probable total estimated

ground

Water in %

Water storage

(Holding )

Capacity at different

depths

Aquifer condition

1 60-70% 0-30m bgl Weathered / jointed / fractured

formation

2 10-15% 30-60m bgl

In semi weathered rock granite,

granite gneiss, Schistose with joint

/fractures.

3 5-10% 60-90m bgl Hard rock with fractures

4 <5% 90-130m bgl Hard rock with isolated fractures.


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The overall aquifer system is unconfined and in many instances static water level exhibits a

pheatic water levels and in the semi confined aquifer, water level exhibits tendency according

to pressure head.

The geophysical, vertical electrical soundings were conducted to know sub surface

conditions of the aquifer system. It reveals the above sub surface condition of the

water bearing strata.

SOIL TYPES.

Major soil group in the District is red sandy soil followed by mixed red and

black cotton soil, deep black soil, red loamy and medium black cotton soil. Red sandy

soils are playing vital role in ground water recharge aspect. All above-mentioned soil

types except deep black cotton soil are favorable for ground water recharge.

Dynamic Data Monitored by the District Office.

1 Manual water level monitoring

Manual water level readings a year

from 06 out of 08 dug wells

Manual water level readings a year

from 41 borewells

2. Water quality

Water quality data from 47 stations for

base line, 30 stations for trend for

surveillance

3. Village wise Hydro geological

information

Hydrogeolgical information of the

villages falling in this District.

4. Ground water Estimation

Periodical estimation of ground water

resource in the District based on Micro

watershed.

HYDROGEOLOGICAL INFORMATION SYSTEM (HIS).

The water level monitoring network consists of 06 observation Dug

wells, which are Govt., owned, tapping the phreatic aquifer down to a maximum

depth of 18 mts. Apart from the dug wells the network comprises of 41

dedicated piezometers. Which have been constructed exclusively for water level

and water quality monitoring. The piezometers tap the shallow unconfined

aquifer / semi confined aquifer down to a depth of 50 to 60mts.


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Total number of Observation wells: 63

Number of OBW stations at present working: 45

The objectives of the water level monitoring is to:

Detect impact of ground water recharge and abstraction

Monitoring the Ground water levels changes

Assess depth to water level

Detect the long term trend

Compute the ground water resources availability

Assess the Stage of Development

Design management strategies at regional level.

Data collection for the Reporting year:-

The number of wells that generated,

1.Complete data a) 06 Dug wells

b) 41 Bore wells

Total 47

2. Partial data: Frequency of monitoring for Ground water levels

a) Bore wells and Dug wells 564 per year.

REVIEW OF RAINFALL

Rainfall pattern from 2001-2015

Period Rainfall in mm Percentage of

deviation Received Rain fall Normal

2001 494.60 486.57 (+) 01.65

2002 443.90 486.57 (-) 8.03

2003 329.60 486.57 (-) 32.26

2004 544.90 486.57 (+) 11.98

2005 794.60 486.57 (+) 63.30

2006 459.90 486.57 (-) 5.48

2007 688.30 486.57 (-) 41.45

2008 638.50 486.57 (+) 40.47

2009 814.4 486.57 (+) 67.37

2010 888.6 486.57 (+) 82.62

2011 363.00 486.57 (-) 25.38


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2012 528.00 486.57 (+) 8.51

2013 548.00 486.57 (+)12.62

2014 768.00 486.57 (+) 57.89

2015 739.00 486.57 (-) 9.98

Figure: Rainfall pattern - Chitradurga district

Drainage System of Chitradurga.


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30 0 30 60 Kilometers

N

EW

S

DRAINAGE MAP OF CHITRADURGA DISTRICT

Reservoir, River, Tanks

Stream

The major rivers are and Vedavathi and Suvarnamukhi Rivers. Vedavathi River is

flowing from West to East and in Hosdurga TQ where in Hiriyur TQ Suvarnamukhi River

joins this Vedavathi River and flows towards North in Challkere taluka and reaches Hagari

River and ultimately it joins Tungabadra River. No flood patterns and flow periods are

noticed in recent past periods.

III. DRAINAGE CHARACTERISTICS MAP.

Details of Basin /Sub basin/ minor basins area in Chitradurga District.

Table showing drainage Details of Major Basins and Sub –Basins

Sl.N

o Taluks Covered

Catchments

Area in

Sq.kms

Total

Catchments

Area in

Sq.kms

A. VEDHAVATHI

1 B.G. Kerehalla (98) Molakalmur 128.75

222.49 Challakere 93.74

2 Belagurhalla(86) Hosdurga 83.00 83.00

3 Bharamagirihalla(84) Hiriyur 242.50 405.72


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Hosadurga 101.87

Holalkere 50.20

Chitradurga 11.15

4 Chalkere (103) Challakere 223.75 233.75

Chitradurga 10.00

5 Chinnahagari LB (95) Molakalmur 333.00 333.00

6 Chinnahagari RB (97) Molakalmur 259.00 259.00

7 Chitradurga(79) Chitradurga 255.00


8 Dharmpura (119) Hiriyur 281.00


9 Garanihalla LB(100) Challakere 244.00 244.00

10 Garanihalla RB(101) Challakere 220.00 220.00

11 Garanihalla (102) Challakere 250.00 250.00

12 Gundihalla (83)

Hosadurga 73.12

188.12 Chitradurga 3.75

Holalkere 111.25

13 Hirehalla(99) Challakere 70.50 70.50

14 Hulikuntehalla (117) Challakere 268.12

282.32 Hiriyur 14.20

16 Janigihalla(81) Chitradurga 177.50

206.87 Holalkere 29.37

17 Janigihalla LB(76) Chitradurga 235.62

238.74 Holalkere 3.12

18 Janigihalla RB(77) Chitradurga 183.12 183.12

19 Kannihalla (60) Holalkere 53.00

286.75 Hosadurga 233.75

20 Kattehole (106) Hiriyur 113.00

116.75 Hosadurga 3.75

21 Kodihalla(60) Holalkere 380.00

380.00 Hosadurga 00

22 Madderhalla (107) Hiriyur 349.35 349.35

23 Maradihalli halla(104)

Chitradurga 100.00


Hiriyur 180.00

24 Parasurampura (118) Challakere 458.12 458.12

25 Shivaganga halla(80) Holalkere 128.70 128.70

26 Srirampura halla(85)

Hosadurga 530.00 537.50

Hiriyur 7.50

27 Turuvanur halla(78) Chitradurga 129.00


28 Yaraballi (105) Hiriyur 281.20 281.20

TOTAL (B) 7063.9 7063.9


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B. SUVARNAMUKHI

1 Kerekore(108) Hiriyur 104.60 104.60

2 Kariyalahalla(109) Hiriyur 31.00 31.00

3 Suvarnamuki (120) Hiriyur 111.25 111.25

TOTAL © 246.85 246.85

GRAND TOTAL (A+B) 7310.75

Sl.

No Basins Tot. Area in Sq.kms

1 VEDHAVATHI 7064.9Sq.kms

2 SUVARNAMUKHI 246.85 Sq.kms

TOTAL 7310.75 Sq.kms

Mineral Resources of Chitradurga District Chitradurga

district is one of the mineral rich district in the state, where many types of minerals. Thin

bands and lenses of barytes upto 1 m wide and 200 m long occur in association with the

fuchsite quartzite bands of Sargur Group in the Ghattihosahalli and adjacent areas.

Copper, Gold, Silver: A belt of polymetallic sulphide mineralisation

with a copper, lead, zinc, antimony, arsenic, gold and silver, has been traced over a strike

length of about 40 km, along the eastern part of the schist belt. This mineralised belt

designated as the Chitradurga sulphide belt, extends from Chikkahonnanahalli in the north to

Yarahalli in the south. Copper mineralisation is prominent in the Belligudda-Ingaldhalu-

Kunchiganahalu sector over a strike length of about 5 km. The Ingaldhalu mines is located in

this sector. At Ingaldhalu, chalcopyrite with minor pyrite, pyrrhotite, galena and sphalerite

occur as disseminations, stringers and fracture fillings in quartz veins occupying narrow shear

zones in the meta-basalts. The Belligudda-Ingaldhalu-Kunchiganahallu section has been

explored by drilling, jointly by GSI and the Dept. of Mines and Geology, Govt. of Karnataka.

On the basis of drilling data and the mine development data, reserves of 2.14 million tonnes

with an average copper content of 1.22% are estimated in the mine blocks, northwest and

northeast block. The copper ores also carry considerable silver and gold content.

INGALDHAL COPPER MINE (CENTRAL BLOCK) : This mine is situated

south of Chitradurga. HGML has got Mining Lease (ML No: 2490, Period: 06.03.1993 to

05.03.2013). Mining activities at Ingaldhal Copper Mine were carried out from 1965 to 1994.


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So, Mining work was suspended in 1994. due to world globalization and cause decline in Cu

price as well M/s. Hindustan Copper Limited had stopped buying of copper concentrate. It is

planned to carry out further detailed exploration by exploratory mining, reclamation. For this

statutory works are in progress.

GUDDADA RANGAVANA HALLI (G.R.HALLI):

Guddadarangavanahalli Gold Deposit is situated 7km North East of Chitradurga and

is 15km North West of Chitradurga Gold Unit and is situated on Bangalore-Sholapur

National Highway No.13 with a 1.5km mud road takes to the deposit. This is a polymetallic

deposit, reopening of the mine is under consideration. It is planned to carry out further

detailed exploration by exploratory diamond drilling followed by reclamation and mining.

For this statutory works are in progress.

List of the Minerals found in Chitradurga district are as follows:

Sl.

No.

Type of

Mineral

Village and Taluk

1 Amphibole

Supergroup

Holalkere taluk, Chitradurga District

2 Arsenopyrite Ingaldhal copper deposits ("Ingladhal" copper deposit;

Ingaldal),

3 Baryte Gattihosahalli, Holalkere taluk

4 Biotite' Kudinirkatte, Holalkere taluk

5 Bornite Ingaldhal copper deposits ("Ingladhal" copper deposit;

Ingaldal),

6 Chalcocite Ingaldhal copper deposits ("Ingladhal" copper deposit;

Ingaldal),

7 Chalcopyrite Ingaldhal copper deposits ("Ingladhal" copper deposit;

Ingaldal),

8 Cobaltite Ingaldhal copper deposits ("Ingladhal" copper deposit;

Ingaldal),

9 Galena Ingaldhal copper deposits ("Ingladhal" copper deposit;

Ingaldal),

10 Kyanite Kudinirkatte, Gattihosahalli, Holalkere taluk,

11 Muscovite Kudinirkatte, Gattihosahalli Holalkere taluk,

12 Muscovite var: Gattihosahalli, Holalkere taluk,

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http://www.mindat.org/loc-214464.html


















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Iron and Manganese Ore mines: Karnataka has over 9,000 million tonnes of iron

ore resources, of which the bulk is in the magnetite form. The production during the year

2007-08 crossed 47 million tons. The districts of Bellary and Hospet are the main districts,

whereas Chitradurga, Bagalkot and Tumkur districts are also produce significant amounts of

iron ore. The chunk of the iron ore is exported to be used in steel manufacture and pig iron

and sponge iron plants. Some of the Iron Ore mines are also associated with manganese,

dolomite, and limestone.

The details of the Major mineral Leases are given below.

Sl. No.

M.L. No.

Mineral Granted for

Mining Lease

Date of Grant

Period Village Sy. No. Extent in Hectares

1 3 4 5 6 7 8 9 10

Fuchsite

13 Muscovite var:

Sericite

Gattihosahalli, Holalkere taluk,

14 Paragonite Kudinirkatte, Holalkere taluk,

15 Pyrite Ingaldhal copper deposits ("Ingladhal" copper deposit;

Ingaldal), Chitradurga

Gattihosahalli, Holalkere taluk,

16 Pyrrhotite Ingaldhal copper deposits ("Ingladhal" copper deposit;


17 Quartz Gattihosahalli, Holalkere taluk,

18 Rutile Gattihosahalli, Holalkere taluk,

19 Sillimanite Holalkere taluk,

20 Sphalerite Ingaldhal copper deposits ("Ingladhal" copper deposit;


21 Stromeyerite Ingaldhal copper deposits ("Ingladhal" copper deposit;


22 Tennantite Ingaldhal copper deposits ("Ingladhal" copper deposit;


23 corrundum Parashurampura, challakere taluk

24 Asbestos Hoykallu village, Challakere taluk

http://www.karnataka.com/bellary/about-bellary/

http://www.karnataka.com/hospet/about-hospet/

http://www.karnataka.com/bagalkot/about-bagalkot/

http://www.karnataka.com/tumkur/about-tumkur/
































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1 2346 Iron ore and Manganese

07-10-1992

20 Chitradurga B.B. Halli 3,4,5 103.81

2 2294 Iron ore 04-02-1997

20 Chitradurga Megalahalli 21P &

35 42.6

3 2236 Iron Ore 28-10-1992

20 Chitradurga Megalahalli 21 163.5


19-12-2002

20 Hosadurga Kenchanahalli 1 & 2 28.07

5 1575/ 2557

Iron ore and Manganese

15-02-1999

20 Hosadurga D.B. Kere 59, 38 12.58

6 1784/ 2585


16-04-1999

20 Hosadurga D.B. Kere 59 60.7

7 2566 Iron Ore 08-06-1997

20 Hosadurga Lakkihalli 64 & 104

7.85

8 2626/ 2639


15-04-2001

20 Hosadurga D.B. Kere & C.B.

Kere 59, 118

& 99 40.48


31-05-2008

20 Hosadurga K.K. Kaval 1 21.44

10 2599 Iron Ore 09-03-2009

20 Holalkere Mahadevanakatte 23 P 16.19

11 2658 Iron ore 25-02-2011

30 Holalkere Dindadahalli 23/1P2 10.87

12 2388 Iron ore 10-04-1992

20 Chitradurga B.B. Halli 6 57

13 2499 Iron ore 12-08-2005

20 Chitradurga B.B. Halli 4 1.52

14 2519 Iron ore 20-04-2006

20 Chitradurga B.B. Halli 156,

158 & 159

4.55

15 2062 Manganese and Iron ore

01-03-1988

20 Holalkere Sadarahalli 14, 19 16.19

16 2631 Iron Ore 23-04-2010

20 Hosadurga K.K. Kaval 1 74.86

17 1760/ 2603


22-06-1981

20 Hosadurga D.B. Kere 38 3.24

18 2517 Iron Ore 13-08-

1997 20 Hosadurga K.K. Kaval 1 12.87

19 1534/ 2560


08-06-1977

20 Hosadurga Kenkere 63 19.98


27-05-2011

20 Hosadurga Ramajjana Halli,

Kavalu & Mallapura Village.

2P1, 3P4, 35,

36P, 37P,

38P, & 39P of

Mallapura, & 113P,

114P of Ramajjanahalli.

122.22

21 966/ 2596

Iron ore 01-04-1990

20 Chitradurga B.B. Halli 6 6.07


21

22 993/5

93 Iron Ore

15-07-1965

20 Holalkere Herekandavadi 80.94

23 2630 Iron Ore 11-07-1989

20 Hosadurga Linga Devarahalli 11 24.5

24 2556 Iron Ore 03-09-1989

20 Hosadurga Sanna Kittadahalli 26.3

25 1584 Manganese 22/03/1979 20

Chitradurga Bahaddur Ghatta,

Gummanuru 39, 102

20.23

26 1125 Copper 22/01/1993 20 Chitradurga Ingaladalu 27 157.88

27 1997 Manganese 03/03/1984 20 Chitradurga Bheema samudra 123 40.47

28 2490 Copper 06-03-1993

20 Chitradurga Ingaladal 27 259

29 2453 Manganese 16-12-1997

20 Holalkere Mahadevapura 8, 50 &

51 23.48

30 2634 Manganese 26-05-2010

20 Holalkere Mahadevapura 60/1A2, 60/1B2,

59/B 3.64

31 2638 Manganese 31-05-2010

20 Holalkere Mahadevapura

58/1, 58/2,

57/3 & 57/4

2.83

32 2281 Green Quartz

08-04-1995

20 Holalkere Gatti Hosahalli 45 17


13-11-2001

20 Holalkere Arasinaghatta 67 & 78 60.7


02-12-1995

20 Holalkere Gatti Hosahalli 47 9.71

35 2342 Lime Stone 08-04-2001

20 Hosdurga Mathod 169, 171

111.3

36 1839/2643

Lime Stone 15-10-2002

20 Hosdurga Kanchipura 120 122.67

37 2473 Lime Stone 18-01-2003

20 Hosdurga Ittegehalli 42.9 80.9

38 2472 Lime Stone 18-01-2003

20 Hosdurga Ittegehalli 56 20.24

39 2304 Lime Stone 02-05-1999

20 Hosdurga Mallapura 30, 13

& 9 , 10 339.27

40 2337 Lime Stone 04-02-2002

20 Hosdurga Kenkere 10, 12 & 14

212.46

41 2381 Lime Stone 11-08-2000

20 Hosdurga Tarikere 171 84.98

42 2284 Lime Stone 22-09-2000

20 Hosdurga K.K. Kaval & Bukkasagara

1 9

43 2184 Lime Stone 02-09-1994

20 Hosdurga Nagathihalli 8 19.72

44 2260 Manganese

& Lime Stone

24-05-1980

20 Hosdurga Ittegehalli 100,

102, 9, 56

242.92

45 2367 Manganese

& Lime Stone

25-08-2001

20 Hosdurga D.B. Halli 38 40.87

46 2372 Pink Quartz 17-09- 20 Hosdurga Hosaralu 23 4.85


22

2002

47 2659 Manganese 26-04-2011

20 Hosdurga K K Kaval 1 9.71

48 2591 Lime Stone & Dolamite

29-01-2009

20 Hosdurga K K Kaval 1 4.25

49 2377 Quartz 25-10-2002

20 Hiriyur Maradihalli 113 4.04

50 1908 Manganese 29/09/1983 20 Holalkere Herekandavadi 98 10.11

51 2037 Manganese 18/04/1987 20 Hosdurga C.B. Kere 99 35.2

52 1882 Limestone Dolamite

07/05/1983 20 Hosdurga

Mathodu, Kappanayakana

Halli, Siddagondana halli

171, 4P 44P, 52P

388.5

53 2350 Limestone & Manganese

Ore 20/10/1982 20 Hosdurga D.B. Kere 38 48.58

54 1863 Limestone &

Dolamite 18/01/1983 20 Hosdurga Kanchipura 89 48.56

55 1937 Manganese 11/04/1984 20 Hosdurga Sheranakatte 91 40.48

56 1965 Limestone 07-02-1985

20 Hiriyur Obalapura 14, 28 13, 31

101.17

Ornamental Quarry Leases: In Molakalmuru Taluk of chitradurga,

District, Grey granite quarry Leases have been granted and working.

List is given below:

Minor Minerals: More than 550 building stone lease have been granted in

chitradurga district. Out of which only 85 building ston Quarry Leases are

working. List of the leases are given below.

Statement showing the Active Quarry Leases in Chitradurga Dist.,

Sl.

No.

Q.L.

No.

Date of

Grant

Period

(in

Years

Type of

Land Village

Sy.

No.

Ext

ent Mineral

1 2 4 5 6 7 8 9 10

CHITRADURGA TALUK

1 472/527 25/02/2012 5 Gomala Siddapura 86 2.00 Building

Stone

2 528 30/04/2015 5 Gomala Siddapura 86 1.00 Building

Stone


23

3 532 11/09/2015 10 Patta Jagadalipura 51 1.20 Building

Stone

4 536 18/11/2015 5 Hullubanni

Kharabu M.K. Hatti 57 1.00

Building

Stone

5 538 26-02-2016 5 Gomala G.R. Halli 199 2.00 Building

Stone

6 541 10-03-2016 5 Gomala G.R. Halli 199 1-

28

Building

Stone

7 542 15-03-2016 5 Gomala G.R. Halli 199 8-

05

Building

Stone

8 457/539 08-03-2016 5 Govt.,


Building

Stone

9 458/540 08-03-2016 5 Govt.,


Building

Stone

10 517 21/11/2011 5 Patta J.N. Kote 253/¦2 3.20 Building

Stone

11 534 19/10/2015 10 Govt., Siddapura 88 2.00 Building

Stone

12 552 17-05-2016 5 Govt.,

Gomala Jagadalipura 5 5.00

Building

Stone

CHALLAKERE TALUK

13 430/R 25-06-2016 5 Govt., Varavu Kaval 662 2.00 Building

Stone

14 454/553

20-05-2016

w.e.f. 11-10-

2014

5 Govt., Challakere 260 5.00 Building

Stone

15 503/R

11-07-2016

w.e.f. 04-07-

2015

5 Govt., Varavu Kaval 75 1.00 Building

Stone

16 505 07-04-2011 5 Govt., Varavu Kaval 214 2.00 Building

Stone


Stone

18 509 24-05-2011 5 Govt.,

Banjaru Nannivala 263 1.03

Building

Stone


Stone


24

20 515 17-11-2011 5 Govt.,

Kharabu Pagadalabande 34 3.00

Building

Stone

21 519 18-03-2014 5 Govt.,

Kharabu Pagadalabande 34 3.00

Building

Stone

22 417/522 16/04/2013 5 Govt., Varavu Kaval 75 1.00 Building

Stone

23 416/523 16/04/2013 5 Govt., Varavu Kaval 75 2.00 Building

Stone

24 529 30/04/2015 10 Govt.,

Hullubanni Challakere 260 3.00

Building

Stone

25 530 30/04/2015 10 Govt.,


Building

Stone

26 455/

543

22-04-2016

w.e.f. 27-10-

2014

5 Gomala Manne Kote 292/P 2.00 Building

Stone

27 544 22-04-2016 5 Gomala Manne Kote 292/P 2.00 Building

Stone


Stone


Stone


Stone


Stone


Stone

33 551 12-05-2016 5 Hullubanni

Kharabu Nannivala 297 6.00

Building

Stone

34 553 20-05-2016 10 Govt.,


Building

Stone

35 554 13-06-2016 10 Govt.,


Building

Stone

36 430R 25-06-2016 5 Govt., Varavu Kaval 662 2.00 Building

Stone

37 503/R 11-07-2016 5 Govt.,

Kallubande Varavu Kaval 75 1.00

Building

Stone

HOLALKERE TALUK

38 514 10-11-2011 5 Gomala Halehalli 61 0.20 Building

Stone


25

39 521 08-07-2012 5 Gomala Marapura 13 2.00 Building

Stone

40 531 23/07/2015 10 Hullubanni

Kharabu Chatnahalli 10 2.00

Building

Stone

41 524 28.01.2015 5 Govt.,

Kharabu

T. Emmiga

nuru 142 4.00

Building

Stone

42 526 24/04/2015 5 Govt.,

Muffath Holalkere 338 4.00

Building

Stone

43 550 26-04-2016 5 Hullubanni

Kharabu Kenchapura 26 2.00

Building

Stone

HOSADURGA TALUK

44 535 30-10-2015 5 Govt.,

Gomala Huralihalli 15 2.00

Building

Stone

45 518 26-11-2011 5 Govt.,

Hullubanni Attimagge 77 1.00

Building

Stone

46 520 16.10.2014 5 Govt.,

Kharabu Gulihalli 1.00

Building

Stone

47 525 18-02-2015 5 Govt.,

Hullubanni Jammapura 11 3.00

Building

Stone

48 537 10-12-2015 5 Govt.,

Muffath Bokikere 34 2.00

Building

Stone

MOLAKALMURU TALUK

49 513 20-10-2011 5 Govt.,

Kharabu Nagasamudra 250 2.10

Building

Stone

Sand Details: Chitradurga district has only one river called vedavathi

river which originates in the chikmagalur district and flows through

Hosadurga, Hiriyur and Challakere Taluks of chitradurga district. Major

Sand sourse being the vedavathi river. A total of 23 sand potential blocks

have been identified in the district and Have obtained EC clearance from

the SEIAA. These blocks were assigned to PWD , now, has to be

auctioned as per the KMMC (amendment rules) 2016,

The details of the blocks are given below.


26

Sl.

no.

Village Block No. Area in

acres

Hiriyuru Taluk

1 Hoovin Hole 1 15.00

2 Hoovin Hole 2 15.00

3 Bidarakere 1 20.00

4 Bidarakere 2 20.00

5 Hosahalli 1 20.00

6 Hosahalli 2 20.00

7 Saluhunase 1 20.00

8 Saluhunase 1 20.00

Challakere Taluk

9 Mylanahalli 1 20.00

10 Mylanahalli 2 20.00

11 Gorlathu 1 20.00

12 Tore Biranahalli 1 20.00

13 Tore Biranahalli 2 20.00

14 Kalamarahalli 1 20.00

15 Kalamarahalli 2 15.00

Hosadurga Taluk

16 Kellodu 1 20.00

17 Lingadahalli 1 16.00

18 Jogammanahalli 1 15.00

19 Muttha Gondi 1 16.00

20 Kellodu 2 23.00

21 Kannagondi 1 15.00

22 Mettinahole, karla

mavinahalli

1 20.00

23 Ballalasamudra kaval 1 23.00

district mineral survey reportenvironmentclearance.nic.in/writereaddata/district/... · 2018. 2....

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