DISTRICT MINERAL SURVEY REPORT

DISTRICT LEVEL ENVIRONMENT

IMPACT ASSESSMENT

AUTHORITY

(DEIAA)

HAVERI DISTRICT

DISTRICT MINERAL SURVEY REPORT

Sl. No Contents Page No.

1 Introduction 1

2 Administrative setup 2

3 General Profile of the District 4

4 Transportation and Communication 6

5 Land use pattern 9

6 Climate and Rainfall 9

7 Geology and Mineral wealth 12

8 Overview of Mining Activity in the District 16

9 Process of Deposition of Sediments in river bed 20

1. Introduction :

Haveri district is situated in the western sector of the Karnataka state.

The district encompasses an area 485156 hectares laying between the

latitudinal parallels of 14019

0 North to 15

009

0 North and the longitudes

of 75001

0 East to 75

050

0 East. In its shape the district may be regarded

as roughly resembling an inverted square shape. Its greatest length

from north to south is about 111 kms and its great breath from east to

west is about 87 km. The district is bounded on the North by the

districts of Dharwad and Gadag; on the south by the district of

Davangere and Shimoga and the west by the district of North Kanara.

All these districts which surround Haveri belong to Karnataka state

itself. Varada river act as the central part of the district and it flows

west to east direction about 128 kms on the north-east and south, the

Tungabhadra river flows in between Haveri-Gadag, Shimoga,

Davangere and Bellary districts.

2. Administrative Setup The district is divided into seven taluks having a total

geographical area of 4848 sq. kms. The district is also divided into two sub

divisions with taluks Shiggaon, Hangal, Savanur coming under Savanur

subdivision and taluks Haveri, Hirekerur, Byadagi and Ranibennur coming

under Haveri sub division.

Haveri is the administrative and political headquarters of the district,

whereas Ranebennur in the south is a business hub. The important towns and

villages in Haveri District are:

Haveri: The district's administrative, culture and political headquarters, it

also famous for its cattle markets, oil mills and cotton markets. Haveri is

also known for "Haveri Nyaya". a typical method of settling the disputes.

Haunsabhavi: Famous Place for Education (Mruthyunjaya vidya peeta).

Hangal: Taluk headquarters. Place of the beautiful Tarkeshawar temple.

Akki-Alur: City in Hanagal Taluk. Rice bowl of Haveri District. Famous for

its lake and gardens.

Kumar Pattanam: Place of Birla industries on the bank of the

river Tungabhadra.

Byadgi: Famous for Byadgi chilli.

Bankapura: Notified as Bankapur Conservation Reserve offering a safe

haven for peacocks.

Ranebennur: Important trade centre in central Karnataka.

Kaginele: Kaginele Kanaka Guru Peetha, a religious Math (institution)

dedicated to sage Kanakadasa is present here.

Rattihalli : City in hirekerur taluk. Place for beautiful kadambeshwar temple.

3. General profile of the district;

Semi-malnad Semi-malnad lies in the Western part of the district and

covers Shiggoan, Hanagal, Hirekerur and Byadagi talukas. It covers half

of the districts total area. It consists of a typical landscape having low

ranges with monsoonal forest cover. The hill ranges of Dundshi and

Hanagal are rounded and subdued in topography. The hill range of Masur

and Marvalli spread towards the extreme south.

Maidan To the East of the semi-malnad belt lies the undulated plain

region called “Maidan Area”. It is characterized by isolated hills like

Devagirigudda, NelogalGudda, SiddapurGudda and MalthihalliGudda.

The isolated hills are 609 mts. above the sea level. The whole ranges

from 527 to 610 mts. above the sea level. The maidan region extends over

the talukas of Haveri, Ranebennur, Savanur and Eastern part of Byadgi

4. Transportation and Communication

Transportation plays a vital role in bringing goods and services, an

interaction between the people residing in different surrounding areas of a

particular district, state or any other region of the world. It is well recognized fact

that the absence of transportation facilities results in the subsistence level of

economy in any region.

Talukawise Extent of Roads in Kms – 2011-12

Sl.No Taluk National

Highway

State

Highway

Main

Roads

Rural

Roads

Others

1 Byadagi 13.00 46.60 188.32 424.50 12.20

2 Hanagal - 114.48 321.40 896.70 0.00

3 Haveri 20.00 113.06 280.46 776.20 8.40

4 Hirekerur - 95.86 347.37 781.05 0.00

5 Ranebennur 32.00 83.03 288.56 770.00 0.00

6 Savanur 5.00 34.69 236.01 507.45 0.00

7 Shiggaon 31.00 99.49 181.55 644.70 0.00

Total 103.00 587.21 1843.67 4800.60 20.60

The study region has a well developed transportation network. The

district has 103 kms of national highways, 587.21 kms of state highways,

1843.67 kms of main district roads, 4800.60 kms of rural village roads and only

20.60 kms of other district roads (table 2.16). The national highways NH4

which connected Pune to Bangalore passes through Haveri city, Shiggaon and

Ranebennur talukas.

TRANSPORTATION MAP OF HAVERI DISTRICT

The state highways and main roads constitute about 2430.88 kms. It is

observed that the rural roads are to the extent of 4800.60 kms which pictures the

thrust accorded to rural sector/rural infrastructure. The roads laid under

NABARD and schemes are tending towards rural sectors maintaining high

quality work, because

of NABARDs thrust on laying quality roads almost all rural roads will be

converted into unmetalled to metalled or tar roads within few years

Talukawise Railway Lines in Kms – 2011-12

Sl.No. Taluk Kms Number of

Stations

1 Byadagi 15 (Broad-Gauge) 01

2 Hanagal Nil Nil

3 Haveri 31 (Broad-Gauge) 02

4 Hirekerur Nil Nil

5 Ranebennur 27 (Broad-Gauge) 03

6 Savanur 26 (Broad-Gauge) 03

7 Shiggaon Nil Nil

Total 99 (Broad-Gauge) 09

In the district there is a broad-gauge railway network with 99 kms except

Hanagal, Hirekerur and Shiggaon talukas. The railway line passes through all

the other four talukas connecting important suburban or town centres in the

district. There are 9 important railway stations in the study region. Railways are

used for transportation of maize, groundnut and other agricultural goods.

5. Land Use Pattern

Land utilization by the Forest Agriculture, Horticulture and Mining Activity

etc., given in the table below.

Area utilization of land for the Quarrying Activity (2015-16) Source :- Mines

and Geology

Minor Mineral Quarry lease areas utilize details.

Sl

No

Purpose Total in

No’s

Extent

(in acres)

1 Active building Stone Quarry lease 59 98.00

2 Expired/ Determined/Surrendered

building stone quarry lease

25 30.30

4 RRC Issued building stone quarry

lease

78 73.19

5 RRC Issued building Sand lease 23 162.68

6. Climate & Rainfall

Climate is one of the important factors, through which the

activities of mankind find their place on the surface of earth. The

climatic of any locality or a region is not determined by a single

factor element, but rather by the combinations of climatic elements

and ofweather types prevailing there. The climatic condition of a

Agriculture, Horticulture and Sericulture and Forest Year 2015-16

Land Utilization (Hectares)

Sl

No

Taluk Geogra

phical

Area

Forest Non

agricul

ture

Barr

en

Total Cultiv

able

waste

Perme

nent

Pasteu

re

Tree

s &

Gro

ves

Total

1 Byadagi 43656 4889 2145 501 2646 190 1109 20 1319

2 Hangal 77525 8474 6501 1885 8386 734 2061 1535 4330

3 Haveri 79985 3849 5519 466 5985 1178 1754 2 2934

4 Hirekerur 80694 8876 6818 712 7530 0 2701 298 2999

5 Ranebennur 90475 10614 6275 834 7109 552 2417 100 3069

6 Savanur 53901 801 2585 624 3209 0 722 181 903

7 Shiggaon 58920 9951 3464 771 4235 335 1445 154 1934

Total 485156 47454 33307 5793 39100 2989 12209 2290 17488

region also depends upon man made features like industrial, upon

the intensity of the transportation system, the density of population

and the green spaces in the towns and villages of theregion.

The climate of the Haveri district is characterized by the tropical

monsoon, which indicates the seasonal weather throughout the year,

and it is product of the inter play of the two opposing air masses

of the South-West and North East monsoon over Haveri district. The

districts dry season combined with a moderate annual range of

temperature. According to recent Indian climatic classification the

district falls in the semi- humid zones. The summers are

uncomfortably hot. Summers are milder in the in the North Western

part of the district rather then in the in eastern part these are Hanagal

and Shiggaon talukas, etc., in the district on the whole the climate of

the district is healthy and agreeable.

The climate of any region is determined by the combination of

climatic elements such as temperature, rainfall, relative humidity

and wind direction, etc.

Through the district is exposed to both the monsoons, it

receives most of the rainfall from the south-west monsoon. The

monsoon usually starts from the first week of June. Continuous

rainfall is found in the malnad region, till the end of September with

abreak of few days in the middle. The yearly rainfall of Haveri district

is given in table

Actual Rainfall of Haveri District DURING 2015, 2016

Sl.No. Month Normal(mm) 2015 (mm) 2016 (mm)

1 January 0.40 0 0.20

2 February

0.60 0 0.10

3 March 4.10 17.9 1.30

4 April 43.6 10.50 12.42

5 May 78.4 99.70 55.26

6 June 114.9 162.40 161.18

7 July 170.00 63.30 124.04

8 August 111.30 79.00 65.82

9 September 99.40 72.50 47.65

10 October 118.90 97.90 6.27

11 November 43.9 24.40 17.01

12 December 7.30 0.00

.00

Dist. Total 792.80 627.60 491.25

The average annual rainfall for the district as a whole is 792.80

mm. The area lying western part of receives a higher amount of rainfall.

In the eastern belt near Ranebennur for instance the average annual

rainfall is about 459 mm. In contrast in the western most parts around

Hanagal the rainfall averages to about 859 mm per annum. The

south-west monsoon is relatively more active in the western zone and

account for nearly 70 percent of the annual rainfall. The north-east

monsoon is however more active in the eastern zone where it accounts

for about 25 percent of the rainfall. Towards the end of April and

onward most parts of the district receive per-monsoon showers. By the

middle of May, the west wind begins to fresher and lasts through the

day. After the west breeze has set in sharp thunder storms with rain and

hail are common. These early showers are very useful as these fill the

ponds and soften the soil. Towards the end of May the west wind

begins to blow stronger, banks of clouds gather in the south-west and

end early in June the south-west monsoon sets in. In eastern half

September and October are the other with heavy downpour.

7. Geology and Mineral wealth

The district lies on the deccan plateau and comprises mainly Dharwad

system as it bed rocks Dharwad and Haveri. The Dharwad belt

passes through the western part Haveri district in a south east direction,

with an average width of 17 kms to 20 kms. The major portion of

this schist belt has no mineral deposits of any commercial importance,

excepting the eastern part of Haveri district. The rocks show a

considerable variation in texture, are usually massive and they are pink

to grey in colour. Bands of conglomerates occur in the northern region

of the district and these pebbles and holders comprise granite

felsites appetite, quartzite and schist’s. Laterite is found to occur in

several parts, but chiefly in the west as capping over granite, gneiss

and quartzite. The mineral wealth of the district includes low grade

gold, copper, iron and manganese beside gryewacks which is most

useful as a building stone used as construction material and

extensively quarried in all parts of the Haveri district.

Amongst the district situated in central (middle) maidan of the state

Haveri district, especially its western portion is relatively rich in

flora and fauna. The district consists of various types of crystalline

schists and some acid and basic intrusive rocks commonly found in

other part of the state.

GEOLOGY, STRUCTURE AND GOLD MINERALIZATION IN

HAVERI DISTRICT

Ganajur- Karajgi PL area located in the Eastern part of the

Dharwar –Shimoga (D-S) belt, also called basin, in the foreland region

of the Dharwar craton. D-S basin has been known for ancient artisanal

gold mining e.g. Chinmulgunda and Karajgi which have been explored

in detail by geological Survey of India. The D-S belt contains a myriad

of banded cherty iron formations (BIF) amidst greywacke. The BIFs in

the western part of the area are magnetite bearing where as in the eastern

part they are sulphidic and also auriferous.

The regional trend of bedding and foliation are parallel and vary

from NW to WNW with steep northeasterly dips. Structurally the rocks

are deformed into isoclinals folds, sometimes-folded folds with steeply

dipping axial planes. These folds are defined by BIF bands, which act as

marker horizons. A number of NNW-NW trending shere zones occur

within the basin. Shearing has brought about fracturing of the competent

BIF bands and associated acid volcanic.

The geology of the Ganajur-Karajagi P.L. block comprises of

greywacke and inter bedded banded sulphidic chert (BIF). The general

strike direction strike direction of the banded sulphidic chert varies

between N40-600 W and dips at 35 0to 500 towards NE. Geological map

of Ganajur Karajgi area

Gold mineralization is confined to sulphide facies of banded iron

formation, and the mineralization is both syngenetic, strata bound and

epigenetic. The gold mineralization is associated with strong

suphidation, shlorite-sericite, carbonate alteration along with minor

biotite. The mineralized zones are characterized by the presence of

significant sulphide minerals (10-12%) such as pyrite, chalcopyrite and

arseno-pyrite. Positive correlation is noticed between gold values and

amount of sulphides.

The highly potential Ganajur gold prospect is hosted in banded

cherty sulphidic iron formation located at the nose region of

northwesterly plunging regional ant formal structure. The mineralized

body is bound by a thick sequence of greywacke

The gold mineralization in the Ganajur Main deposit is associated

with a deformed iron formation hosted in a polydeformed par gneiss

sequence. The gold mineralization is characterized by strong sulphide

mineralization, silica breccias and quartz carbonate veining developed

within a sulphidic chert unit. The gold mineralization is epigenetic in

nature but strata bound because it is confined to the cherty iron

formation. The main gold zones form a moderately to steeply dipping

tabular body trending northwest to north-northwest and dipping

northeast. Fractures are filled with remobilized silica or quartz carbonate

veinlets. The amount of gold is directly proportional to the amount of

sulphides. Mineralization dominantly occurs as dissemination with small

amount in fine veinlets.

GEOLOGICAL MAP OF HAVERI DISTRICT

8. Over view of Quarrying Activity:

Quarrying activity in the Haveri district is as follows: In this district

Minor Mineral leases like Building stone existed and operated

Talukwise in Haveri, Ranebennur, Shiggaon, Hirekerur, Byadgi.

Major mineral like gold is under process in Ganajur Village of Haveri

Taluk.

In this district for the year 2015-16 there are 59 Minor Mineral

Building stone Leases. The details are as below.

Sl.

No

Name of the Q.L

Holder

QL

No

Date of

Grant

Perio

d

Extent Village R.Sy.N

o

1 2 3 4 5 6 7 8

Haveri Taluk

1 Kasturi .P.

Shivannanavar

111/6 27/9/11 10 1.00 Nelogal 102

2 Basavaraj Belavadi 107/594 29/8/10 5 1.00 Nelogal 102

3 Ashok .S. Banakar 115/598 7/10/10 10 1.00 Nelogal 102

4 Vanishree .N.

Shivannanavar

112/600 7/11/10 10 1.00 Nelogal 102

5 Beerappa .B.

Dilleppanavar

42 8/6/10 5 0.20 Hombardi 5/C

6 Channappa

Malladad

53 01/10/2010 5 1.00 Kallihal 15

7 Manjunath Malladad 54 01/10/2010 5 2.00 Kallihal 15

Ranebennur Taluk

1 Paramappa .S.

Shivannanavar

471/01 20/3/08 10 1.00 Kajjari 75

2 V.R.Bellary 108/37 13/5/13 10 4.00 Kajjari 67

3 S.R.Bellary 113/77

4

23/6/14 10 4.00 Kunabevu 137/B

4 Rudrappa .M.

Lamani

114/2 27/1/15 10 4.00 Hunshikatti 19/1X

5 Suresh .A. Dilliwal 47 5/8/10 5 0.20 Kamdod 49/1 §

6 Channabasappa

Vaddar

57 16/11/10 5 0.20 Kunabevu 137/b

7 Nagappa .B. Javali 59 16/11/10 5 0.20 Kunabevu 137/b

8 Imamsab Mulla 60 16/11/10 5 0.20 Kunabevu 137/b

9 Somappa .M.

Nelogal

61 16/11/10 5 0.20 Kunabevu 137/b

10 Laxman .B.

Balannanavar

58 16/11/10 5 1.00 Kunabevu 143/x-1

11 Santosh .V.

Hiremath

68 29/9/08 10 2.00 Kajjari 85

12 Ravi Ajreddy 70 10/1/11 5 0.20 Kajjari 193/1

13 H.R. Pushpa 71 11/1/11 5 1.00 Kamdod 49/2A

14 Hanumanthappa .H.

Kichadera

80 14/7/10 5 1.00 Kunabevu 143/x-1

15 Jagadish .C. Bellary 81 1/4/11 5 1.00 Kunabevu 137//B

16 K.U.Manjeshwar 85 14/12/11 5 0.20 Kamdod 49/2A

17 Prathibha .V.

Hiremath

94 29/4/11 10 3.00 Kajjari 72

18 B.C.Haverimath 101 27/3/15 10 1.00 Kajjari 73

19 Santosh .V.

Hiremath

102 27/3/15 10 3.00 Kajjari 73

20 V.S. Hosahallimath 103 27/3/15 5 1.00 Kajjari 72

21 Deepak .V.

Hiremath

104 27/3/15 10 1.20 Kajjari 72

22 Raghavendra Barki 105 1/6/15 5 2.00 Hunshikatti 19/2

Byadgi Taluk

1 B.C.Haverimath 65 19/5/08 10 0.20 Chatra 21

2 Santosh .V.

Hiremath

66 20/11/08 10 2.00 Chatra 21

3 Santosh .V.

Hiremath

67 26/6/10 10 1.00 Chatra 21

4 S.R.Bellary 609 03/12/05 10 1.10 Motebennur 419

5 B.C.Haverimath 69 18/5/10 10 0.20 Chatra 21

6 V.R.Bellary 50 7/9/10 5 5.00 Budapanhalli 82/PÀ/2

7 Ashok Dummal 84 22/10/11 5 1.00 Alalgeri 11B/2

8 Pushapa M.

Shetasandi

98 26/02/14 5 0.20 Lakmajikopp

a

23/1

Hirekerur Taluk

1 Kubergowda Patil 95 9/1/2014 5 1.00 Chatnalli 36

Shiggaon Taluk

1 L Srinivasrao 96 2/6/11 5 0.30 Shigga 433/a

2 Ramesh.V.

Teggihalli

109/72

5

13/5/13 10 1.00 Hunaguda 152/1

3 Ramesh.V.

Teggihalli

110 22/9/15 10 3.00 Bada 54/3

4 Nagaraj .H. Vaddar 46 30/7/10 5 0.20 Shiggaon 433/A

5 Ramanna .L. Vaddar 51 7/9/10 5 1.00 Donnegudda 354

6 Prakash .R.

Bhovivaddar

62 13/12/10 5 0.20 Shiggao 433/A

7 Giddappa .T. Vaddar 63 13/12/10 5 0.20 Shiggao 433/A

8 Basappa .C. Vaddar 64 13/12/10 5 0.20 Shiggao 433/A

9 Dharamgowd .V.

Honnangowdra

97 21/2/14 5 1.00 Shingapur 51

10 Jagadish .V. Baligar 99 3/2/15 5 0.20 Aratal 89/2

Hangal Taluk

1 Ajjangowda .M.

Doddamani

82 9/6/11 5 1.00 Hulagaddi 123/7

2 D.R.N

Infrastructure,Hubli

87 28/2/12 5 5.20 Bingapur 28/A

3 D.R.N

Infrastructure,Hubli

88 20/3/12 5 3.00 Bingapur 28/A

4 Shivappa .G.

Hattiyavar

89 25/5/13 5 1.00 Negavanagi 62/3

5 Basavanneppa .S.

Hattiyavar

90 25/5/13 5 1.00 Negavanagi 62/4

6 Ashok .V. Patil 91 27/5/13 5 5.00 Bingapur 28/A

7 Vijaylaxmi .S.

Deshpande

92 27/5/13 5 5.00 Bingapur 28/A

8 D.R.N

Infrastructure,Hubli

93 17/9/13 5 10.00 Nellibidu 106/A1

9 Ravi Deshpande 100 12/3/15 10 1.00 Belagalpete 28/3

10 Hanumanthappa .S.

Devagiri

106 22/7/15 5 1.00 Nellibeedu 106/A1

1 Nagappa Policy 44 9/7/10 5 1.00 Adur 97

Details of Royalty Or Revenue received in last three Year

9. Process of Deposition of Sediments in the Tunghabhadra river

The Tungabhadra River is a river in India that starts and flows through

the state of Karnataka during most of its course, before flowing along the

border between Karnataka and Andhra Pradesh and ultimately joining

the Krishna River along the border of Andhra Pradesh and Telangana.

In the epic Ramayana, the Tungabhadra River was known by the name

of Pampa.

The Tungabhadra River is formed by the confluence of the Tungha River

and the Bhadra River at Koodli which flow down the eastern slope of

the Western Ghats in the state of Karnatka.The 2 rivers originate in

Chikmagalur district of Karnataka along with the Nethravathi (west-

flowing river, joining the Arabian Sea near Mangalore), the Tunga and

the Bhadra rise at Gangamoola, in Varaha Parvatha in the Western Ghats

Sl No Year MINOR

MINERAL IN

LAKHS

MAJOR

MINERAL

1 2013-14 1593.47 Nil

2 2014-15 2158.69 Nil

3 2015-16 2124.91 Nil

at an elevation of 1198 metres. The Bhadra river flows through the

industrial city Bhadravathi. More than 100 tributaries, streams, creeks,

rivulets and the like contribute to the two rivers. The journey of the

Tunga and the Bhadra is 147 km (91 mi) and 171 km (106 mi)

respectively, till they join at Koodli, at an elevation of about 610 metres

near Holehonnur, about 15 km (9.3 mi) from Shivamogga, areca granary

of the country. It is a confluence of both the Dwaitha and the Adwaitha

philosophies. From there, the Tungabhadra meanders through the plains

to a distance of 531 km (330 mi) and mingles with the Krishna at

Gondimalla, near the famous Alampur in Mahaboobnagar District of

Telangana. The Varada flowing through Shimoga, Uttara Kannada and

Haveri districts and Hagari in Chitradurga, Bellary district, Koppal

District and Raichur Districts in Karnataka and the Handri in Kurnool

distriict of A.P. are the main tributaries of the Tungabhadra. Many

rivulets and streams join these tributaries.

There are many holy places all along the rivers: primarily temples

of Saiva Cult on the banks of the Bhadra and all the cults on the banks of

the Tunga. Sringeri, Sarada Petham established by the Adi

Shankaracharya is the most famous one on the left bank of the Tunga,

about 50 km (31 mi) downstream of its origin. Manthralayam Sree

Raghavendra Swamy Muth in Kurnool District and Alampur in

Mahaboobnagar District, Jogulamba is the presiding deity, known as

Dakshina Kashi are the other important pilgrimage centres. There is a

cluster of Nava Brahma temples constructed by the early Chalukyas.

In Haveri district the river and streams originate from small water sheds

and entered in to a number of tanks scattered in the district.

Geomorphologically drainage pattern is semi dendric to dendric .

RIVER BASINS AND DRAINAGE SYSTEM MAP OF

HAVERI DISTRICT

The district being a rain shadow zone, experiences semi arid climate.

The period from March to May are the hottest temperature ranging from

38-43 Degree. Rainfall is scanty and erratic and major portion of rain fall

is received from south west monsoon during the months of May to Sept.

Sediments refers to the conglomerate of materials ,organic and inorganic

,that can be carried away by water or by the wind.The term often used to

indicate soil based, mineral matter (eg: clays,silt and sand )decomposing

organic substances and inorganic biogenic material are also considered

sediment. Most mineral sediment comes from weathering and

transported through the rain water and deposited in the Tungabhadra

river

In Haveri district the Thingabhadra river flows through Hirekerur,

Ranebennur and Haveri Taluks. The approximate length of the

Thughabhadra river is 110 kms. Fairly good sand deposits in

Thungabhadra river bed of Haveri district jurisdiction. The particulates

present in these rivers at typically small with clay defined as particles

less than 0.00195mm and coarse sand reaching up to 2mm in diameter.

Sand along the sediments deposited in the rivers of the district up to

average 2-4mt.

From the last 3 years PWD dept quarried quantity of sand and supplied

to the govt works and general public is as below.

Sl

No

Year Quantity (cum)

1 2013-14 177764.36

2 2014-15 110356.14

3 2015-16 111692.02

As per the new sand policy during the month of Oct 2016 the following

sand blocks are identified and notified the details are as follows

Identified and notified sand blocks in the District Sl

No

Block

No Adjacent R.Sy.No Extent(Acre) Village

Latitude & Longitude

1 HNR-1 263,264(p),254 12.83 Havnur

N 14051’49.4” E 75

042’05.5”

N 14051’50.1” E 75

042’02.1”

N 14052’06.1” E 75

042’05.6”

N 14052’05.5” E 75

042’09.0”

2 HNR-2 226(p), 272, 278(p), 12.5 Havnur

N 14052’06.1” E 75

042’09.2”

N 14052’06.5” E 75

042’08.8”

N 14052’22.4” E 75

042’08.6”

N 14052’21.8” E 75

042’11.9”

3 HBR-2 280(p),281,282,283(p) 12.11 Hirebidri

N 14039’28.6” E 75

048’29.8”

N 14039’19.1” E 75

048’38.4”

N 14039’17.0” E 75

048’39.7”

N 14039’15.3” E 75

048’36.7”

N 14039’17.1” E 75

048’35.5”

N 14039’26.6” E 75

048’26.9”

4 FTR-1 28(p),9,29(p) 12.1 Fathepur

N 14025’12.4” E 75

038’22.9”

N 14025’12.8” E 75

038’27.5”

N 14025’25.3” E 75

038’28.1”

N 14025’25.0” E 75

038’24.1”

5 MDR-1 438(p), 243(p), 12.14 Medleri

N 14040’38.1” E 75

045’14.8”

N 14040’36.5” E 75

045’17.9”

N 14040’34.5” E 75

045’28.3”

N 14040’37.7” E 75

045’29.3”

N 14040’41.5” E 75

045’15.4”

6 MDR-2 222(p), 221(p), 12.3 Medleri

N 14040’46.14” E 75

044’57.98”

N 14040’49.35” E 75

044’58.76”

N 14040’42.59” E 75

045’13.88”

N 14040’39.31” E 75

045’13.10”

7 HGR-3 178,179,180,181,182,183,184

,185,186 & 187 15 Haranagiri

N 14045’15.6” E 75

043’13.9”

N 14045’36.5” E 75

043’16.6”

N 14045’36.1” E 75

043’19.8”

N 14045’15.3” E 75

043’16.9”

8 HGR-4 201,202,2013,207,208,209

,210,211 & 212 25 Haranagiri

N 14044’23.1” E 75

042’29.1”

N 14044’42.7” E 75

042’50.9”

N 14044’39.3” E 75

042’53.7”

N 14044’21.0” E 75

042’31.6”

9 CDP-1 2,8,47 & 55 60 Chandapur

N 14047’57.1” E 75

040’16.0”

N 14047’54.7” E 75

040’32.9”

N 14047’51.0” E 75

040’42.3”

N 14047’50.6” E 75

040’44.2”

N 14047’40.5” E 75

040’57.5”

N 14047’33.6” E 75

041’02.6”

N 14047’29.7” E 75

040’57.9”

N 14047’36.6” E 75

040’53.5”

N 14047’42.3” E 75

040’46.9”

N 14047’45.7” E 75

040’41.8”

N 14047’46.5” E 75

040’39.9”

N 14047’50.2” E 75

040’30.8”

N 14047’51.5” E 75

040’15.3”

10 UGT-1 2(p), 1,94,93 (p) 12.2 Udagatti

N 14041’41.5” E 75

044’14.6”

N 14041’41.1” E 75

044’17.9”

N 14041’24.3” E 75

044’15.3”

N 14041’25.0” E 75

044’12.2”

11 UGT-2 2 (p),3, 4(p), 12.3 Udagatti

N 14041’23.32” E 75

044’12.23”

N 14041’22.69” E 75

044’15.25”

N 14041’15.20” E 75

044’15.44”

N 14041’6.55” E 75

044’17.31”

N 14041’7.34” E 75

044’14.70”

N 14041’15.28” E 75

044’12.70”

12 ARN-2 88(p),89,91,92(p), 12.3 Airani

N 14034’34.54” E 75

048’52.00”

N 14034’35.87” E 75

048’54.80”

N 14034’22.26” E 75

049’04.08”

N 14034’21.11” E 75

049’01.26”

13 ARN-3 92 (p),93 12.3 Airani

N 14034’05.48” E 75

049’06.25”

N 14034’05.54” E 75

049’09.56”

N 14034’10.78” E 75

049’09.41”

N 14034’20.81” E 75

049’04.92”

N 14034’19.49” E 75

049’02.09”

14 BLR-3 93,123,124,133,134,135,1

36,137,138,140 & 141 60 Belur

N 14043’56.2” E 75

044’35.4”

N 14044’08.9” E 75

044’56.8”

N 14044’09.6” E 75

044’58.8”

N 14044’13.0” E 75

045’05.6”

N 14044’16.8” E 75

045’15.9”

N 14044’17.4” E 75

045’19.4”

N 14044’11.9” E 75

045’20.6”

N 14044’10.4” E 75

045’14.9”

N 14044’07.6” E 75

045’14.5”

N 14044’04.7” E 75

045’02.4”

N 14044’05.9” E 75

045’01.9”

N 14044’05.5” E 75

045’00.8”

N 14044’04.6” E 75

044’59.0”

N 14043’51.7” E 75

044’37.7”

Identification of new sand blocks is in progress.