district survey report gariyaband...

DISTRICT SURVEY REPORT

GARIYABAND (Chhattisgarh) AS PER NOTIFICATION NO. S.O. 141(E) NEW

DELHI, 15TH JANUARY, 2016 OF MINISTRY OF

ENVIRONMENT, FOREST AND CLIMATE

CHANGE

2016

DGM [Type the company name]

06/06/2016

C:\Users\user\Desktop\Gariyaband_DSR1.docx

LOCATION MAP OF GARIYABAND DISTRICT


(INTRODUCTION)

DEIAA DEAC

(Minor Mineral ) (Sand) (Mining)

(Environment Clearance)

HL&I " ΄ " ΄

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Overview of Mining Activity in the District

Lease

Sand


List of Mining Leases and Sand in the District with location, area and period

of validity

1 2 3 4 5 6 7 8 9

1 159

30-05-2006

2 20/6/2006

3 ” 50

20-07-2006

4 76

18-09-2006

5

75 19/10/2008

6 46

15/11/2006

7 24/8/2005


8 29/10/2007

9 220

06-12-2007

10 128

29-08-2007

11 29/1/2008

12 9/5/2008

13 170

29-04-2008

14 150

03-05-2010

15 23

22-07-2010

16 23/8/2010

17 15/9/2010

18 14/11/2010


19 11

22/2/2011

20 17/3/2011

21 2/2/2011

22 147

04-03-2011

23 78

19-01-2011

24 30/6/2011

25

25 05-01-2012

26 141

29-12-2011

27 139

29-12-2011

28 140

29-12-2011

29 5/1/2012

30 170

19-11-2012


31 4/12/2011

32 4/2/2012

33 70

24/11/2012

34 4/2/2012

35 6516

17-05-2012

36 142

24/1/2012

37 935

17-02-2014

38 61

1411/2011

39 133

10-10-2014


40 935

17-02-2014

1 2 3 4 5 6 7 8 9

1

2907

20-10-

2011

1 2 3 4 5 6 7 8 9


Details of Royalty or Revenue Received in Last Three Year

Major Minerals

Details of Royalty or Revenue Received in Last Three Year

Sand

2

11703 A

16-11-

2012


Sendimentation of rivers of District

Deposition of sediments in the rivers of the district is due to the heavy rains and flooding in the upperstream.

Erosion is natural process, wathering, corrosion, or abrasion can reduce a

material into smaller particles. Normally, these smaller units are relocated by water,

wing, ice, or man. Erosion removes tosoil, organic material, and other valuable

resources.

Once a material is broken free of the larger mass, it can be carried away

an deposited elsewhere. This process of depositing eroded material is known as

sedimentation. Some indications of sedimentation are sand dunes, mud in the street

around drains, and decreased water holding capacity of stream, reservoir, or pond.

Sediment is responsible for more stream and river degardation than any

other pollutant. Deposits of sediments in ditches, streams, and rivers reduce their

capacity to store water resulting in more frequent and severe flooding and increased

property damage. Accumulations of sediment may result in severe damage to storm


drain systers. Many millions of dollars are spent each year to dredge our state

waterways, to remove sediments from storm drain systerms, reseroirs, and water

treatment plants, and to repair flood damage.

Sediment in streams and rivers causes the most damage to aduatic life by

severely impacting aquatic animal habitats and degrading water quality. Areas needed

for reproduction and food sources are destroyed when fine silts cover the sand and

gravel streambed. Decreased clarity of the water prevents sunlight from reaching plants

resulting in loss of aquatic plant communities. The result is a reduction in the number

and variety of fish and other aquatic life. This impact ofter can seen for many miles

downstream.

Several "best management practices" (BMPs) have been developed to

control erosion and sedimentation. Erosion control prevents soil from dislodging

and becoming suspended in runoff. Sediment control removes soil from the

runoff.


SAND DEPOSITION AT BANK OF RIVER

Stopping soil from eroding in the first place is more effective but also much moe

difficult to integrate into a construction schedule. Controlling erosion by

establishing vegetative cover is by far the most effective type of erosion control.

Clearing and grading in phases as needed reduces the area of exposed soil and

preserves topsoil. Seeding and mulching, both temporary and permanent, must be

done several times over the course of construction to maintain adequate soil

protection.

Silt fences, settling ponds, and inlet protectors all trap sediment on construction

sites. They receive runoff, allow time for suspended solids to settle out, and then

let the water slowly continue on its way. They do not work as filters to strain out

soil particles or the pollutants they transport but reduce thier entrance to our

waterways. Even at their best they have limited efficiency. A good job of erosion

and sediment control might be 75% effective. Some off-site sedimentation is

unavoidable.

These erosion control measures, properlyimplemented and maintained, are the

best management practices of sediment control on construction sites.

During all phases of construction it is neccessary to prevent silt and sediment

fromentering the storm drains that empty directly into the nearest creek or pond.

This is done by covering the storm drain inlets downstream from construction

activities with a dam of geotextile fabric. A gap at the top edge provides and

overflows in event of extream flooding. These inlet covers slow the water flow to

allow settling time for the sediment and to let clean water slowly seep through the

mesh.

Temporary ponding in the street and around storm drain inlets is common and

may last several hours or a day. Ponding can be dept to a minimum by frequent

cleaning of the filters and roads. Even if construction is not taking place adjacent

to the inlets they must be protected from sediment carried in from work areas by


construction vehicles. Some flooding is inevitable, but with patience and

cooperation we can make a positive impact on the health of our streams and

rivers.

7.General Profile of District ( )

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Land Utilition Pattern in the district: Forest, Agriculture, Horticulture,

Mining etc.

धान, मक्का,

mailto:rglhy@fodkl[k.M


कोदो, कुटकी, चना, तिवरा, मसरू, उड़द, मूूंग


Physiography of the District


1 2 3 4 5

', -48 ' -46" 82', -28 ' -38''

2 ', -57 ' -46" 81', -53 ' -05"

3 ', -37 ' -58" 82', -3 ' -37"


4 19', -53 ' -55" 82', -14 ' -03"

5 ', -17 ' -36" 82', -14 ' -03"

Rainfall of District Durg Year wise

2008-09 2009-10 2010-11 2011-12 2012-13

1 2 3 4 5 6 7

974.0 1115.3 947.0 1029.0 1124


2 2440.8 917.8 1403 1338.6 1623.0

3 1171.3 1091.8 1135.9 1415.2 1248.1

4 1450.0 971.0 1810.7 1366.0 1410.1

5 1413.1 959.0 1239.2 948.1 1015.0

7449.2 5054.9 6535.8 6096.9 6420.2

Geology and Mineral Wealth

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MAP SHOWING GEOLOGY AND MINERAL DETAILS OF GARIYABAND DISTRICT

जिलेकीनदिय ाँ - पैरीनिीइसनदीकाउद्गमस्थलमैनपुरववकासखण्डमुख्यालयसेलगभग 3 ककलोमीटरदरूस्स्थिभाटीगढ़पहाड़ीहै।मैनपुरएवूंगररयाबूंदववकासखण्डसेप्रवाहहिहोिेहुएक ूं गेश्वरववकासखण्डमेंस्स्थिप्रयागनगरीरास्िममेंमहानदीमेंसमाहहिहोिािीहै।गररयाबूंदववकासखण्डकेग्रामपूंटोराकेपाससोंढूरनदीपैरीनदीमेंममलिीहै। सोंढूरनिीगररयाबूंदऔरधमिरीस्िलाकीसीमारेखाबनािेहुएप्रवाहहिहोिीहै, िोग्राममोहेराएवूंपूंटोराकेपासपरैीनदीमेंममलिािीहै।

SEAC


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SEAC


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