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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
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LOCATION MAP OF GARIYABAND DISTRICT
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(INTRODUCTION)
DEIAA DEAC
(Minor Mineral ) (Sand) (Mining)
(Environment Clearance)
HL&I " ΄ " ΄
" ΄ " ΄
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Overview of Mining Activity in the District
Lease
Sand
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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
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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
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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
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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
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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
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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
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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
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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.
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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
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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
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कोदो, कुटकी, चना, तिवरा, मसरू, उड़द, मूूंग
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Physiography of the District
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1 2 3 4 5
', -48 ' -46" 82', -28 ' -38''
2 ', -57 ' -46" 81', -53 ' -05"
3 ', -37 ' -58" 82', -3 ' -37"
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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
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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
SEAC
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”” ” ”