Notice
“District survey Report, Rajnandgaon” has prepared as per the terms and conditions of Appendix-10 of Notification No. S.O. 141 (A) New Delhi, 15 January, 2016 of Ministry of Environment, Forest and Climate Change, introduced through the Enviornment (Protection) Act, 1986. The draft of District Survey Report, Rajnandgaon is placed on the website of the NIC, Rajnandgaon as well notice board of DEAC, Rajnandgaon for inviting comments/suggestions from the general public, persons and entities concerned. The last date for receipt of the comments/suggestions is 21 day from the publication of this Reprot i.e. 19 th June, 2016. The comments/suggestions may be sent by e-mail to the following ID: [email protected] It may kindly be ensured that the comments are sent on MS-Office Word file. Alternatively, comments/suggestions may also be sent by post to the following address:
Member Secretary , District Level Expert Appraisal Committee (DEAC) Room No 41, Collectorate Building, Rajnandgaon -491 441
The envelope may kindly be super scribed on the top with :― "Comments/suggestions on the District Survey Report, Rajnandgaon".
2016
District Survey Report Rajnandgaon AS PER NOTIFICATION NO. S.O. 141(E) NEW DELHI, 15TH JANUARY, 2016 OF MINISTRY OF ENVIRONMENT, FOREST AND CLIMATE CHANGE
DIRECTORATE OF GEOLOGY AND MINING MINERAL RESOURCES DEPARTMENT Govt. of Chhattisgarh
Date: 30/05/2016
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LOCATION AND COMMUNICATION MAP - RAJNANDGAON
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1. Introduction
Rajnandgaon district was carved out from Durg and came into existence on 26 January 1973.As per Survey of India's’ location sheet no.64 C,G,D, it exists from 20°07' to 21°50' north latitude and 80°29' to 81°13' east longitude. This district is surrounded by Kawardha in north, Durg & Balod in east, Kanker in south and Maharashtra in west, covering land area of 8022.5 sq. km. It is the largest district of the state and 2695.91 sq.km. area is under forest cover. District includes 9 tehsil and 1653 villages.
Headquarter Rajnandgaon is located in the eastern corner of the district with Khairagarh,Gandai,Dongargarh,Dongargaon,Ambagarh Chowki, Mohla Manpur are the major towns of the district. Rajnandgoan is well connected by rail, road and air. Rajnandgoan railway station located at Howrah Mumbai railway line and by road N.H. 53 passing at mid of city. The nearest airport is in Raipur, 88 km from district headquarter. District survey report has been prepared as per the guidelines mentioned in appendix-10 of the notification No. S.O. 141 (E) New Delhi, 15 January, 2016 of Ministry of Environment, Forest and Climate Change. This report has prepared by the Regional head, DGM Raipur as per instructions issued by the Director, Geology & Mining (C.G.), Raipur by its letter no. 5103-05/geology-1/f.no.11/2015-16, dated 22/04/2016. The report primarily is focused on the Geological Details i.e. minerals its occurrence, deposit and mining. Along with the mineral data, geographical and infrastructure information is also included. District Environment Impact Assessment Authority and District Environment Assessment Committee will utilize this report in favour of the environment concerned activities and act accordingly. Also this report will act as reference for the lease holders of minerals and those willing to apply for lease.
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2. Overview of Mining Activity in the District
Minerals of economic importance are found in Rajnandgaon mainly Iron ore, Limestone, Flourite, Quartz, Quartzite, Soapstone, Ochre, Clay etc. Building materials like aggregate, flooring stone, sand, murrom, brick clay are also found in enough quantity. Two Mines of iron ore, one for Godavari Power & Ispat Ltd. and the second for Sarda Energy & Minerals ltd. are functional in Boriya Tibbu and Dongarbore area. Limestone mine has been allotted to Jaiswal Necco at Khaira Bhatgaon. 76 quarries of limestone, useful for building material functional in Tekapar, Kalkasa, Baldeopur, Chaweli, Khapri, Dumrdihkala, Dumardi ahkhurd, Mudhipar, Joratarai, Ghorda, Arjuni, Deodongar etc. Similarly 4 stone quarries at Baghnara, Haedalkodo, Mohanpur and Khallari have been leased out.
13 quarries have been allotted for mining of soil to prepare brick at Dhiri, Ira, Bakal, Banhardi, Hardi, Bharregaon, Bhodiya, Ghorda, kirgi, chikhaldah and other villages. Out of 31 newely declared minor minerals, lease for 8 have been granted for quartz, quartzite, silicasand and china clay, white clay. 40 Sand Quarry on the bank of different rivers have been leased out at different villages for sand mining. 2 banks for runner moulding sand have also been granted at Bakal and Bharregaon village. Approximately 169.35 lakh Rupees royalty is earned from all minerals in the district, out of which 107.62 lakh from major minerals and 51.76 from minor minerals.
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3. List of Mining Leases (Major Minerals) in the District with location, area and period of validity
¼i½ ftys esa [kfuiV~Vksa dh lwph %&
ftyk&jktukanxkao vUrxZr fnukad 15 -05 -2016 dh fLFkfr esa Lohd`r [kfuiV~Vksa dh lwph %&
jdck xzke dk dz [knku ekfyd dk uke [kfut [k-dz- rglhy fdLe Hkwfe vof/k ¼,dM+ esa½ uke
1 2 3 4 5 6 7 8 9
juj eksfYMax 'kkl- ¼ikuh ds 13.09.04 to 1 Jherh vpzZuk nkl 406 12.00 ckady jktukanxkWo ls.M uhps½ 12.09.34
esllZ lqtkrk 'kkl- ¼ikuh ds 05.03.95 to 2 eksfYMax ls.M 910 7.00 HkjsZxkao jktukanxkWo Mkdfy;k uhps½ 04.03.15
es- tk;loky fuDdks [kSjk & 07.03.98 to 3 pwuk iRFkj 450 11.50 jktukanxkWo 'kkl- ¼?kkal½ fyfe- HkVxkao 06.03.18
110.00 compartment es- xksnkojh ikWoj ,.M Hec cksfj;k frCcw 15.03.10 to 4 vk;ju vksj No. p.535 ekuiqj [kaMxkao ou jsat bLikr fyfe0 jk;iqj 272.00 ou{ks= 14.03.30 P.536 Acr
80.710 'kkjMk ,uthZ ,oa Com. no. 537 Hec 15.05.02 to 5 vk;ju vksj Mksaxjcksj ekuiqj ou Hkwfe feujYl fyfeVsM part 199.00A 14.05.32 cr
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(ii) List of Quarry Lease in the district with location, area and period of validity
jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe vof/k ¼,dM+ esa½
(1) (2) (3) (4) (5) (6) (7) (8) (9) 1 nhid 'kekZ pwuk iRFkj 320/14, 15 4.55 tksjkrjkbZ jktukanxkao futh 12.08.13 to 11.08.18
2 Jh HkkxhjFkh pdz/kkjh pwuk iRFkj 166 3.75 tksjkrjkbZ jktukanxkao 'kkldh; 14.12.11 to ¼igkM+ 13.12.16 pV~Vku½ Hkwfe
3 Jh HkkxhjFkh pdz/kkjh pwuk iRFkj 166 1.60 tksjkrjkbZ jktukanxkao 'kkldh; 04.01.11 to ¼igkM+ 03.01.21 pV~Vku½ Hkwfe
4 Jh foDVj fjfiz"V;ku pwuk iRFkj 164 Part 1.50 tksjkrjkbZ jktukanxkao 'kkldh; 01.06.11 to ¼igkM+ 31.05.16 pV~Vku½ Hkwfe
5 Jh larks"k dqekj pwuk iRFkj 165/4 part 3.00 tksjkrjkbZ jktukanxkao 'kkldh; 07.07.11 to yksgkuh ¼?kkal½ Hkwfe 06.07.21
6 Jh izoh.k dqekj tSu pwuk iRFkj 320/2, 13 4.75 tksjkrjkbZ jktukanxkao futh 16.10.07 to 15.10.17
7 Jherh puizhr dkSj pwuk iRFkj 64/2, 65/2, 66/2, 3.00 tksjkrjkbZ jktukanxkao futh 09.10.07 to 67, 68,71/2, 08.10.17 72/2, 73/1,74/2, 75/2, 76/2, 77/2 8 vfizZr feujYl izks- pwuk iRFkj 320/7 3.00 tksjkrjkbZ jktukanxkao futh 14.09.11 to lquhrk fc;kuh 13.09.21
9 Jh izcy dqekj 'kekZ pwuk iRFkj 320/10,11 2.00 tksjkrjkbZ jktukanxkao futh 03.11.11 to 02.11.16
10 Jh f'koyky pdz/kkjh pwuk iRFkj 320/3,4 4.10 tksjkrjkbZ jktukanxkao futh 12.10.11 to 11.10.16
11 vkse feujYl] izks- pwuk iRFkj 165/4 2.00 tksjkrjkbZ jktukanxkao 'kkldh; 30.09.10 to ftrsUnz gklokuh ¼?kkal½ 29.09.20 pkjkxkg Hkwfe
12 Jh jktukjk;.k flag pwuk iRFkj 2 3.50 tksjkrjkbZ jktukanxkao 'kkldh; 28.02.07 to ¼igkM+ 27.02.17 pV~Vku½ Hkwfe
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jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe vof/k ¼,dM+ esa½
(1) (2) (3) (4) (5) (6) (7) (8) (9) 13 Jh vVy xksnokuh pwuk iRFkj 269/1,2,3,4 5.54 tksjkrjkbZ jktukanxkao futh 20.07.12 to 263/1,2,3 265/1,2 19.07.17 266/1,2 270/2
14 Jh egs'k yksgkuh pwuk iRFkj 87,89,90,91 2.75 tksjkrjkbZ jktukanxkao futh 30.01.13 to 29.01.18
15 Jh f'kodqekj xksaM+ pwuk iRFkj 164 1.81 tksjkrjkbZ jktukanxkao 'kkldh; 18.04.12 to ¼igkM+ 17.04.17 pV~Vku½ Hkwfe
16 jkepanz xksnokuh pwuk iRFkj 18,19,20 2.50 tksjkrjkbZ jktukanxkao futh 09.07.13 to 08.07.18
17 Jh egsUnz 'kekZ pwuk iRFkj 259/1, 260/1 3.84 tksjkrjkbZ jktukanxkao futh 25.05.11 to 24.05.21
18 egs'k yksgkuh pwuk iRFkj 167/5 1.80 tksjkrjkbZ jktukanxkao futh 05.12.12 to 04.12.17
19 Jh Hkkxpan tSu pwuk iRFkj 401 0.90 posyh jktukanxkao futh 02.09.11 to 01.09.16
20 Jh fxj/kkjh yky pwuk iRFkj 360 2.15 posyh jktukanxkao futh 16.01.10 to ryjstk 15.01.20
21 Jherh 'kf'kdyk xqIrk pwuk iRFkj 391/2 2.49 posyh jktukanxkao futh 26.02.15 to 25.02.25
22 uhye iksn~nkj pwuk iRFkj 391/1 5.00 paoj 23 Jh lat; flaxh pwuk iRFkj 391/1 2.00 paoj 24 Jh fot; dqekj pwuk iRFkj 391/1 4.80 paoj 25 Jherh iq"ikyrk pwuk iRFkj 566/1, 568 2.78 paoj 7 jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe vof/k ¼,dM+ esa½ (1) (2) (3) (4) (5) (6) (7) (8) (9) 26 vrqy xks;y pwuk iRFkj 342 4.14 nsoMksaxj jktukanxkao 'kkldh; 18.11.11 to ¼igkM+ 17.11.16 pV~Vu½ Hkwfe 27 Jh v'kksd vxzoky pwuk iRFkj 60, 341 4.28 nsoMksaxj jktukanxkao 'kkldh; 29.07.06 to ¼igkM+ 28.07.16 pV~Vu½ Hkwfe 28 Jh xksiky HkkbZ iVsy pwuk iRFkj 179 1.95 MqejMhgdyk jktukanxkao futh 25.05.13 to 24.05.23 29 Jh v:.k jaxykuh pwuk iRFkj 37/1 4.00 MqejMhgdyk jktukanxkao futh 28.07.14 to 27.07.18 30 Jh iwue 'kekZ pwuk iRFkj 56 1.80 MqejMhgdyk jktukanxkao futh 01.12.10 to 30.11.20 31 dqlqe LVksu feujYl pwuk iRFkj 167,168, 169 1.10 MqejMhgdyk jktukanxkao futh 18.01.12 to izks- Jherh vkjrh 17.01.22 eqnfy;kj 32 Jh fufr'k vxzoky pwuk iRFkj 105 1.73 MqejMhgdyk jktukanxkao futh 10.04.10 to 09.04.20 33 Jh vkj-ih- vxzoky pwuk iRFkj 113 1.15 MqejMhgdyk jktukanxkao 'kkldh; 10.11.12 to ¼?kkal½ Hkwfe 09.11.17 34 Jh lat; flaxh pwuk iRFkj 42/1,3 and 62 2.80 MqejMhgdyk jktukanxkao 'kkldh; 19.12.11 to ¼igkM+ 18.12.21 pV~Vku½ Hkwfe 35 Jh vfer vxzoky pwuk iRFkj 116/3 2.35 MqejMhgdyk jktukanxkao futh 24.10.12 to 23.10.17 36 Jherh jktJh vxzoky pwuk iRFkj 114/2 2.40 MqejMhgdyk jktukanxkao futh 29.01.12 to 28.01.22 37 Jh fot; vxzoky pwuk iRFkj 103/5 1.80 MqejMhgdyk jktukanxkao futh 06.06.12 to 05.06.17 38 Jh eukst dqekj tSu pwuk iRFkj 20, 22 4.50 MqejMhgdyk jktukanxkao futh 11.04.13 to 10.04.18 8 jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe vof/k ¼,dM+ esa½ (1) (2) (3) (4) (5) (6) (7) (8) (9) 39 Jh furh'k vxzoky pwuk iRFkj 106/1 2.36 MqejMhgdyk jktukanxkao futh 10.04.13 to 09.04.18 40 ;ksxs'k Mkdfy;k pwuk iRFkj 108 1.80 MqejMhgdyk jktukanxkao 'kkldh; 13.07.11 to ¼igkM+ 12.07.21 pV~Vku½ Hkwfe 41 inepan tSu] pwuk iRFkj 173/2, 172/2, 174, 4.30 MqejMhgdyk jktukanxkao futh 21.11.11 to 175 20.11.16 42 Jh eukst dqekj tSu pwuk iRFkj 35/2 1.70 MqejMhgdyk jktukanxkao futh 04.07.13 to 03.07.18 43 Jherh fnO;k Mkdfy;k pwuk iRFkj 55/2, 55/3 to 10 4.11 MqejMhgdyk jktukanxkao futh 04.05.10 to etc. 03.05.20 44 Jherh vfurk lkgw pwuk iRFkj 60 1.50 MqejMhgdyk jktukanxkao futh 08.07.11 to 07.07.21 45 Jherh laxhrknsoh pwuk iRFkj 181/1 3.20 MqejMhgdyk jktukanxkao futh 26.08.13 to :axVk 25.08.18 46 Jherh laxhrknsoh pwuk iRFkj 181 2.47 MqejMhgdyk jktukanxkao futh 27.02.14 to :axVk 26.02.24 47 Jh fiz;ad flag ifjgkj pwuk iRFkj 108 4.00 MqejMhgdyk jktukanxkao 'kkldh; 05.08.11 to ¼igkM+ 04.08.21 pV~Vku½ Hkwfe 48 Jh f'ko vxzoky pwuk iRFkj 125/3 1.30 MqejMhgdyk jktukanxkao futh 03.01.08 to 02.01.18 49 Jh jes'k ik.Ms; pwuk iRFkj 339, 340, 342, 4.00 c?ksjk jktukanxkao futh 22.01.14 To 344 21.10.19 50 Jh lqjsUnz 'kekZ pwuk iRFkj 188/2 2.47 eq<+hikj jktukanxkao futh 06.11.07 to 05.11.17 51 Jh nhid pkoM+k pwuk iRFkj 204 3.10 eq<+hikj jktukanxkao 'kkldh; 07.06.12 to ¼?kkal½ Hkwfe 06.06.17 9 jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe vof/k ¼,dM+ esa½ (1) (2) (3) (4) (5) (6) (7) (8) (9) 52 Jh iz.ks'k tSu pwuk iRFkj 202 1.70 eq<+hikj jktukanxkao futh 15.04.12 to 14.04.22 53 Jh egsUnz 'kekZ pwuk iRFkj 226 2.30 eq<+hikj jktukanxkao 'kkldh; 26.02.12 to ¼?kkal½ Hkwfe 25.02.17 54 Jh vfuy pdz/kkjh bZV feV~Vh 615, 624-629, 6.82 /khjh jktukanxkao futh 10.10.07 to 633-635 09.10.17 55 Jh fnyhi pdz/kkjh bZV feV~Vh 589 and other 4.43 /khjh jktukanxkao futh 21.01.12 to 20.01.22 56 Jherh dkSf'kY;k nsoh bZV feV~Vh 555/2 10.90 bZjk jktukanxkao futh 22.01.12 to 21.01.17 57 dapu csu bZV feV~Vh 287 6.85 ckady jktukanxkao futh 16.10.12 to 15.10.17 58 Jherh jk/kk frokjh bZV feV~Vh 401 4.19 ckady jktukanxkao futh 18.08.11 to 17.08.16 59 Jh lanhi flag bZV feV~Vh 425 and other 9.16 gjnh jktukanxkao futh 06.02.12 to 05.02.22 60 Jherh js[kk bZV feV~Vh 530, 531, 532, 6.85 gjnh jktukanxkao futh 20.11.07 to 533/1,2 , 534, 535 19.11.17 61 Jh ;ksxs'k lkjFkh bZV feV~Vh 438 and other 3.41 gjnh jktukanxkao futh 14.06.11 to 13.06.21 62 Jh iou pdz/kkjh bZV feV~Vh 536 and other 3.00 gjnh jktukanxkao futh 06.01.11 to 05.01.21 63 Jh iapjke bZV feV~Vh 401, 402/1,2 2.00 HkjsZxkao jktukanxkao futh 23.05.12 to 22.05.17 64 Jh larks"k pdz/kkjh bZV feV~Vh 31-33, 40, 41 3.00 HkksfM;k jktukanxkao futh 10.10.12 to 09.10.17 10 jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe vof/k ¼,dM+ esa½ (1) (2) (3) (4) (5) (6) (7) (8) (9) 65 Jh f'k[kjpan tSu Q'khZiRFkj 126/2,3,4 2.47 vtqZuh Mksaxjxkao futh 18.04.12 to 17.04.22 66 Qusnz tSu Q'khZiRFkj 66/7 1.70 lkfyd Mksaxjxkao futh 12.07.11 to f>fV;k 11.07.21 67 Jh vHk; dqekj tSu Q'khZiRFkj 379/2, 380/1 3.18 vtqZuh Mksaxjxkao futh 18.04.12 to 17.04.22 68 Jh gfjpan lkgw Q'khZiRFkj 365/3, 364/1 1.48 vtqZuh Mksaxjxkao futh 18.04.12 to 17.04.22 69 Jh euh"k dqekj tSu Q'khZiRFkj 65/4,8,9 &59/2 2.10 lkfyd Mksaxjxkao futh 02.03.12 to f>fV;k 01.03.22 70 Jh rkjkpan NktsM+ Q'khZiRFkj 379/1, 6.31 vtqZuh Mksaxjxkao futh 15.03.12 to 395/6,7,8,9, 14.03.22 396/7, 27, 28 and 394/2,3 71 Jh uohu dqekj tSu Q'khZiRFkj 345/2, 352/1, 5.88 vtqZuh Mksaxjxkao futh 03.03.14 to 352/2, 352/5, 02.03.24 353/1, 353/3, 384/2, 382/4 72 Jh gsear lkgw Q'khZiRFkj 16/2, 17, 18/1 2.02 vtqZuh Mksaxjxkao futh 03.03.14 to 02.03.24 73 es- lqtkrk feujYl izks- pwuk iRFkj 100/1, 101 1.10 jkeiqj Mksaxjxkao futh 10.12.12 to Jherh lqtkrk 09.12.22 Mkdfy;k 74 Hkkjr fcYMlZ pwuk iRFkj 34/3,4,5,6 1.70 ijuk Mksaxjxkao futh 19.05.06 to izks- 'kkafrnsoh tSu 18.05.16 75 esllZ egkohj pwuk iRFkj 431/1,2 , 4.84 cugjnh Mksaxjxkao futh 06.02.12 to daLVªD'ku daiuh] ikVZ- 432/1,2,3 433/1 05.02.17 iz'kkar ckssgjk 76 Jh euh"k [kaMsyoky pwuk iRFkj 326/2, 327 1.75 cugjnh Mksaxjxkao futh 05.04.13 to 04.04.18 77 Jh fueZypan tSu pwuk iRFkj 372/1,2 and 373 4.84 ?kksjnk Mksaxjxkao futh 27.06.08 to 26.06.18 11 jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe vof/k ¼,dM+ esa½ (1) (2) (3) (4) (5) (6) (7) (8) (9) 78 esllZ t; vEcs fczDl bZV feV~Vh 578 and other 3.80 ?kksjnk Mksaxjxkao futh 31.05.12 to izks- eukst cSn] 30.05.22 79 Jh ujs'kyky ryjstk bZV feV~Vh 32 3.50 fdjxh Mksaxjxkao futh 28.10.14 to 27.10.24 80 Jh eugj.k xksaM+ lk- iRFkj 247/1, 247/2, 248 2.50 [kykjh Mksaxjx<+ futh 05.03.14 to 04.03.24 81 Jh jkeizns'k oekZ lk- iRFkj 616 3.36 eksguiqj Mksaxjx<+ 'kkldh; 17.02.12 to ¼?kkal½ Hkwfe 16.02.22 82 Jh larks"k dqekj pwuk iRFkj 425/1, 624/1 2.10 ipisM+h [kSjkx<+ futh 26.10.12 to 25.10.22 83 Jh ftrsUnz eqnfy;kj pwuk iRFkj 68/1,2,5 3.30 ipisM+h [kSjkx<+ futh 23.11.07 to 22.11.17 84 Jh pan pkpM+k pwuk iRFkj 240/2, 241 1.60 dydlk [kSjkx<+ futh 02.02.12 to 01.02.17 85 essllZ ftLdks pwuk iRFkj 455/3 1.20 dydlk [kSjkx<+ futh 16.10.11 to baVjizkbtsl] zikVZuj] 17.10.16 Hkjr :axVk 86 Jh lat; lksekuh pwuk iRFkj 526/6 1.00 dydlk [kSjkx<+ futh 25.12.12 to 24.12.17 87 esllZ egkohj pwuk iRFkj 471, 472, 473/2 3.20 dydlk [kSjkx<+ futh 15.12.12 to daLVªD'ku daiuh] ikVZ- 14.12.17 iz'kkar ckssgjk 88 essllZ ftLdks pwuk iRFkj 229/2, 230/2, 3.10 dydlk [kSjkx<+ futh 16.10.07 to baVjizkbtsl] zikVZuj] 231/2, 232 15.10.17 Hkjr :axVk 89 Jh iz'kkar dkadfj;k pwuk iRFkj 102/2,3,6, 108/2,4 2.30 dydlk [kSjkx<+ futh 28.04.12 to 27.04.17 90 Jherh lqqeu flag pwuk iRFkj 476,482/1 1.40 cYnsoiqj [kSjkx<+ futh 08.10.10 to 07.10.20 12 jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe vof/k ¼,dM+ esa½ (1) (2) (3) (4) (5) (6) (7) (8) (9) 91 in~ek ,lksfl;sVl izks- pwuk iRFkj 468/3 3.70 lkYgsHkjhZ [kSjkx<+ futh 21.09.07 to nhid vxzoky 20.09.17 92 Jh izzohj dqekj nkl pwuk iRFkj 876 2.50 cYnsoiqj [kSjkx<+ futh 09.03.13 to 08.03.18 93 ij?kfu;k xksM+ pwuk iRFkj 311/2 2.10 cYnsoiqj [kSjkx<+ futh 04.12.12 to 03.12.17 94 Jh HkkÅjke pdz/kkjh pwuk iRFkj 869, 870, 876, 3.20 cYnsoiqj [kSjkx<+ futh 07.05.12 to 877 part 06.05.17 95 dfork LVksUl izks- pwuk iRFkj 907, 909/1 1.65 cYnsoiqj [kSjkx<+ futh 28.04.12 to dfork ikj[k 27.04.17 96 Jherh vfnrh flag pwuk iRFkj 303/1,3,4 2.00 cYnsoiqj [kSjkx<+ futh 25.06.10 to 24.06.20 97 Jh HkwisUnz flag nso pwuk iRFkj 867 2.50 cYnsoiqj [kSjkx<+ 'kkldh; 11.08.11 to ¼igkM+ 10.08.16 pV~Vku½ Hkwfe 98 Jherh jk[kh VwjgkVss pwuk iRFkj 875/1 to7 2.75 cYnsoiqj [kSjkx<+ futh 21.02.12 to 20.02.22 99 Jh euhUnz ukFk ik= pwuk iRFkj 348/3, 4, 5, 6 2.00 cYnsoiqj [kSjkx<+ futh 31.12.13 to 30.12.18 100 Jh ik;yerh flag bZV feV~Vh 268/1 4.00 fp[kynkg [kSjkx<+ futh 03.12.12 to 02.12.17 101 Jh lq/khl [k.Msyoky lk- iRFkj 282 4.00 HkqjHkqlh va- pkSdh 'kkldh; 26.02.12 to ¼igkM+ 25.02.17 pV~Vku½ Hkwfe 102 Jh r:.k xka/kh lk- iRFkj 532 5.00 gSnydksM+ks Nqfj;k 'kkldh; 02.06.12 to ¼igkM+ 01.06.22 pV~Vku½ Hkwfe ;ksx %& 299.44 uohu ?kksf"kr xkS.k [kfut 103 Jh xkSrepan Mkdfy;k DokVZtkbV 19 24.00 >wjkMcjh jktukanxkWo 'kkl- ¼igkM+ 29.01.07 to ,.M pV~Vku½ 28.01.27 flydk ls.M 13 jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe vof/k ¼,dM+ esa½ (1) (2) (3) (4) (5) (6) (7) (8) (9) 104 Jh xkSrepan Mkdfy;k DokVZtkbV 130 17.00 fcgkocksM+ jktukanxkWo 'kkl ¼igkM+ 30.10.05 to ,.M pV~Vku½ 29.10.35 flydk ls.M 105 xkSre pan DokVZtkbZV 340 11.00 fogkocksM jktukanxkWo 'kkl0¼igkM+ 30.09.05 to ,oa pV~Vku½ 29.09.25 flydkls.M 106 Jh lat; pksiM+k DokVZtkbV 708 10.00 fiiykdNkj [kSjkx<+ 'kkl ¼igkM+ 20.12.02 to ,.M pV~Vku½ 19.12.22 flydk ls.M 107 Jh vt; dksVfM;k OgkbZV Dys 97,98/1,2, 103, 13.60 VsdkgjkZ MksaxjxkWo futh 08.05.01 to 104/1, 106 07.05.21 108 dqychj flag NkcM+k DokVZt 169 20.00 cgksj.kHksM+h va- pkSdh 'kkl ¼igkM+ 24.05.06 to pV~Vku½ 23.05.36 109 Jh feujYl] ikz- DokVZt 661/1 and 661/2 11.59 ckxjsdlk Mksaxjx<+ 'kkl ¼igkM+ 03.11.11 to deys'k flag] nqxZ pV~Vku½ 02.11.41 110 Jh enuyky 'kekZ pk;uk Dys 962 5.65 jsaxkdBsjk Mksaxjx<+ futh 07.07.99 to 06.07.19 ;ksx %& 112.84 14 (iii) List of Quarry Lease to be extended as per CGMMR, 2015 N-x- xkS.k [kfut la'kks/ku fu;e] 2015 ds fu;e 38 d ¼3½ ds rgr~ foLrkfjr gksus okys mR[kfuiV~VsA jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe ¼,dM+ esa½ (1) (2) (3) (4) (5) (6) (7) (8) 1 Jherh lquhrk tSu] pwukiRFkj 462 dk Vq- 0.70 dydlk [kSjkx<+ futh Hkwfe 2 Jh lehj iksnnkj vk- pwukiRFkj 341 0.90 nsoMksaxj jktukanxkao 'kkldh; Hkwfe 3 'kkafr fot; feujYl pwukiRFkj 487 3.00 posyh jktukanxkao futh Hkwfe 4 esllZ egkohj feujYl izks- lk-iRFkj 505@1 7.00 djsBh Mksaxjxkao 'kkldh; Hkwfe mRrepan lapsrh 5 Jh 'kadj yky Kkupankuh pwukiRFkj 12] 23 1.96 MqejMhgdyk jktukanxkao futh Hkwfe 6 Jherh oanuk tSu Q'khZiRFkj 125 1.00 vtqZuh Mksaxjxkao futh Hkwfe 7 Jh vt; flag pwukiRFkj 113] 434@1 1.20 eks[kyh Mksaxjxkao futh Hkwfe 8 Jh iYVw jke mbds pwukiRFkj 78@2 1.50 jkeiqj Mksaxjxkao futh Hkwfe 9 Jh jes'k yky ryjstk pwukiRFkj 487 1.75 posyh jktukanxkao 'kkldh; Hkwfe ¼igkM+ pV~Vku ½ 10 Jh jes'k yky ryjstk pwukiRFkj 392] 394 1.00 posyh jktukanxkao futh Hkwfe 11 Jherh v:.kk tksxsokj pwukiRFkj 252 2.10 dydlk [kSjkx<+ 'kkldh; Hkwfe 15 jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe ¼,dM+ esa½ (1) (2) (3) (4) (5) (6) (7) (8) 12 Jh d`iky xksaM+ pwukiRFkj 344] 350@1] 2] 3] 351] 352] 353 4.82 nsoMksaxj jktukanxkao futh Hkwfe 13 Jh vVy xksnokuh pwukiRFkj 170@4] 5 1.10 tksjkrjkbZ jktukanxkao futh Hkwfe 14 Jh nsoyky lkgw pwukiRFkj 255@2] 258@2] 254@3] 253@2 1.20 tksjkrjkbZ jktukanxkao futh Hkwfe 15 Jh egs'k dqekj iVsy pwukiRFkj 61@4] 67] 69] 70@4 2.83 [kqlhZikj [kSjkx<+ futh Hkwfe 16 Jh ijkx c<+s lk-iRFkj 94 dk Hkkx 14.00 dyMcjh jktukanxkao 'kkldh; Hkwfe ¼igkM+ pV~Vku ½ 17 Jh nkSyr flag pansy] pwukiRFkj 260@1 dk Hkkx 3.00 uokxkao jktukanxkao 'kkldh; Hkwfe ¼pkjkxkg ½ 18 Jherh xhrkcsykokyk pwukiRFkj 36 ls 41] 42@2] 43@2] 44@2] 45] 2.50 tksjkrjkbZ jktukanxkao futh Hkwfe 46@2 19 Jherh 'kkjnk tSu pwukiRFkj 155 ls 159 3.50 tksjkrjkbZ jktukanxkao futh Hkwfe 20 Jh lat; flaxh pwukiRFkj 391@1 4.60 paoj<+ky jktukanxkao 'kkldh; Hkwfe 21 Jh lR;ukjk;.k 'kekZ dzs'kj pwukiRFkj 259@2 1.50 tksjkrjkbZ jktukanxkao futh Hkwfe 22 Jh nkSyr flag pansy] pwukiRFkj 261@1 0.70 uokxkao jktukanxkao 'kkldh; Hkwfe ¼pkjkxkg½ 23 es- ,l-,l-Mh- baVjizkbZtsl pwukiRFkj 164 dk Hkkx 2.50 tksjkrjkbZ jktukanxkao 'kkldh; Hkwfe izks- Jh lquhy xksnokuh ¼pkjkxkg½ 24 Jh ujs'kyky ryjsstk pwukiRFkj 487 dk Hkkx 1.50 posyh jktukanxkao 'kkldh; Hkwfe ¼igkM+ pV~Vku½ 16 jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe ¼,dM+ esa½ (1) (2) (3) (4) (5) (6) (7) (8) 25 Jh jktho dqfj;kdks"k] pwukiRFkj 398 2.63 posyh jktukanxkao futh Hkwfe 26 Jh ukjk;.k nkl yksgkuh] pwukiRFkj 165@4 1.20 tksjkrjkbZ jktukanxkao 'kkldh; Hkwfe ¼pkjkxkg½ 27 Jh vVy xksnokuh] pwukiRFkj 260@1 dk Hkkx 3.25 tksjkrjkbZ jktukanxkao 'kkldh; Hkwfe ¼pkjkxkg½ 28 Jherh jktqy tSu pwukiRFkj 345@5 2.00 posyh jktukanxkao futh Hkwfe 29 Jh dUgS;k vksloky] pwukiRFkj 107 1.45 MqejMhgdyk jktukanxkao futh Hkwfe 30 Jherh ehuk jaxykuh] pwukiRFkj 242] 235 3.70 dydlk [kSjkx<+ futh Hkwfe 31 Jherh 'kksHkkrkbZ [kksczkx 32 Jh eusUnz flag xjpk] pwukiRFkj 106@2] 3 1.50 MqejMhgdyk jktukanxkao futh Hkwfe 33 Jherh yhykorh gklokuh] pwukiRFkj 165@2] 3 2.00 tksjkrjkbZ jktukanxkao futh Hkwfe 34 esllZ ,l-,l-Mh- pwukiRFkj 164 dk Hkkx 3.00 tksjkrjkbZ jktukanxkao 'kkldh; Hkwfe bUVjizkbZtsl] izks- Jh lquhy xksnokuh] 35 Jh 'kSysUnz dqekj lkgw] pwukiRFkj 209 dk Hkkx 1.90 eksgHkV~Bk Mksaxjxkao 'kkldh; Hkwfe 36 Jherh laxhrk tSu] pwukiRFkj 352@2 3.00 Hkkuiqjh jktukanxkao futh Hkwfe 37 Jh larks"k dqekj f=ikBh bZaV feV~Vh 293 2.13 ckady jktukanxkao futh Hkwfe 17 jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe ¼,dM+ esa½ (1) (2) (3) (4) (5) (6) (7) (8) 38 Jh jktsUnz dqekj eksgcs pwukiRFkj 164 1.99 tksjkrjkbZ jktukanxkao 'kkldh; Hkwfe 39 Jh vVy dqekj xksnokuh pwukiRFkj 260@1 3.25 uokxkao jktukanxkao 'kkldh; Hkwfe 40 Jherh lqeu flag pwukiRFkj 867 2.10 cYnsoiqj [kSjkx<+ 'kkldh; Hkwfe 41 Jh ih;w"k JhokLro pwukiRFkj 208@2] 3] 6 3.27 MqejMhgdyk jktukanxkao futh Hkwfe 42 Jherh 'kkafr nsoh izks- Hkkjr pwukiRFkj 34@2] 4] 5 ,oa 6 1.70 ijuk Mksaxjxkao futh Hkwfe fcYMlZ] 43 Jh nsoyky oekZ pwukiRFkj 26@3] 27] 29 2.09 eks[kyh Mksaxjxkao futh Hkwfe ,oa 'kkldh; Hkwfe 44 esllZ DokfyVh daLVªD'ku izks- pwukiRFkj 190 2.35 eq<+hikj jktukanxkao 'kkldh; Jh th-Mh- tlokuh ?kkal Hkwfe 45 Jh f'koyky pdz/kkjh bZaV feV~Vh 447 ,oa vU; 11.59 bZjk jktukanxkao futh Hkwfe 46 Jh iz'kkar flag bZaV feV~Vh 252]268] 263] 255@3] 279] 267] 8.48 lfygk [kSjkx<+ futh Hkwfe 262] 250] 270] 261@2] 278] 264] 260] 248] 255@1] 255@2] 266] 253] 269] 265] 261@1] 257] 258] 272] 276@1] 259] 287] 276@2] 286] 273] 290] 305@1] 305@2 47 Jh ijs'k dqekj pwukiRFkj 254 3.00 dydlk [kSjkx<+ 'kkldh; Hkwfe 48 Jh xq:pj.k flag HkkfV;k pwukiRFkj 194 ,oa 195 3.69 eq<+hikj jktukanxkao futh Hkwfe 49 Jh lat; dqekj lapsrh Q'khZiRFkj@ 64@1 2.21 lkfyd Mksaxjxkao futh Hkwfe pwukiRFkj f>fV;k 50 Jh larks"k dqekj pdz/kkjh bZaV fesV~Vh 488@1] 2] 489] 547] 548] 558 1.25 flaxnbZ jktukanxkao futh Hkwfe 18 jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe ¼,dM+ esa½ (1) (2) (3) (4) (5) (6) (7) (8) 51 jktukanxkao dqVhj m|ksx izks- bZaV fesV~Vh 423@1]3]4] 424@3] 463] 464] 7.72 gjnh jktukanxkao futh Hkwfe Jherh pEik xqIrk 466] 467] 476] 477] 478] 479] 481] 482] 483@1]2] 484] 487] 488] 491 52 Jh lquhy xksnokuh pwukiRFkj 320@5 2.00 tksjkrjkbZ jktukanxkao futh Hkwfe 53 Jh nkSyr flag pansy pwukiRFkj 260@1 dk Hkkx 2.40 uokxkao jktukanxkao “kkldh; Hkwfe ¼pkjkxkg½ 54 Jherh m"kk ialkjh pwukiRFkj 226 3.00 eq<+hikj jktukanxkao 'kkldh; Hkwfe 55 Jherh yrk frokjh pwukiRFkj 164 dk Hkkx 2.00 tksjkrjkbZ jktukanxkao 'kkldh; Hkwfe 56 Jherh psruk ekusd pwukiRFkj 51] 57 2.01 MqejMhgdyk jktukanxkao 'kkldh; Hkwfe 57 Jh ;ksxs'k Mkdfy;k pwukiRFkj 37@3 1.00 MqejMhgdyk jktukanxkao futh Hkwfe 58 esllZ vkuan baVjizkbZtst] DokVZtkbZV 231@1 12.00 fcgkocksM+ jktukanxkao 'kkldh; Hkwfe izks- ds-lh- ckQuk] 59 Jh v'kksd dqekj vxzoky pwukiRFkj 341] 60 4.28 nsoMksaxj jktukanxkao futh Hkwfe 60 esllZ f'kok feujYl] izks- DokVZt 62] 64 ,oa 65 11.33 dkaik Nqfj;k 'kkldh; Hkwfe Jherh dqlqe csu] 61 Jh ekssgu yky pdz/kkjh bZaV feV~Vh 414 2.40 gjnh jktukanxkao futh Hkwfe 62 Jh izoh.k dqekj pØ/kkjh bZaV feV~Vh 422 5.00 gjnh jktukanxkao futh Hkwfe 63 Jh larks"k dqekj f=ikBh bZV feV~Vh 283] 284@2] 284@3] 806@3 4.15 ckady jktukanxkao futh Hkwfe 19 jdck dz [knku ekfyd dk uke [kfut [k-dz- xzke dk uke rglhy fdLe Hkwfe ¼,dM+ esa½ (1) (2) (3) (4) (5) (6) (7) (8) 64 Jh f'koyky pdz/kkjh] bZV feV~Vh 447 ,oa vU; 11.59 bZjk jktukanxkao futh Hkwfe 65 Jh mRre flag pwukiRFkj 36@1] 36@2 ,oa vU; 7.41 [kqlhZikj [kSjkx<+ futh Hkwfe 66 Jh izcy 'kekZ pwukiRFkj 320@10] 11 2.00 tksjkrjkbZ jktukanxkao futh Hkwfe 67 Jh Hkkxpan tSu pwukiRFkj 401 0.90 posyh jktukanxkao futh Hkwfe 68 Jherh dkS'kY;k nsoh bZaV feV~Vh 549@1] 550] 551] 553] 554@1] 2] 10.90 bZjk jktukanxkao futh Hkwfe pzd/kkjh 555@2] 3] 4] 557] 558@2] 559 ls 561] 577] 578] 581@1] 581@2 69 Jh vrqy xks;y pwukiRFkj 342 4.14 nsoMksaxj jktukanxkao 'kkldh; Hkwfe 70 Jh lat; flaxh pwukiRFkj 391@1 2.00 paoj<+ky jktukanxkao 'kkldh; Hkwfe 71 esllZ egkohj feujYl izks- pwukiRFkj 431@1] 2] 432@1] 2] 3] 433@1 4.84 cugjnh Mksaxjxkao futh Hkwfe mRrepan lapsrh ;ksx%& 245.26 20 4. Details of Royalty or Revenue Received in Last Three Year Major Minerals S.No. Mineral Royalty or Revenue Received 2013-14 2014-15 2015-16 1 Limestone 0.00 9300.00 9300.00 2 Quartz 268802.00 419480.00 NA 3 Quartzite 327768.00 463821.00 NA 4 White Clay 23000.00 0.00 NA 5 China Clay 0.00 64800000.00 NA 6 Iron Ore 0.00 0.00 107500000.00 7 Moulding Sand 84177.00 67680.00 111600.00 8 Red Ochre 0.00 22000.00 NA Total :- 703747.00 65782281.00 107620900.00 Note :- Minerals as Quartz, Quartzite, White Clay, China Clay and Red Ochre are decleared Minor Mineral wef notification dated 10.02.2015. Details of Royalty or Revenue Received in Last Three Year Minor Minerals S.No. Mineral Royalty or Revenue Received 2013-14 2014-15 2015-16 1 Limestone 32223476.00 46883851.00 48566924.00 2 Clay for making Bricks 790365.00 1091660.00 742740.00 3 Sand Stone 959580.00 1027900.00 926800.00 4 Murum 1728500.00 4249180.00 1003000.00 5 Ordinary Stone 286450.00 50000.00 529113.00 6 Quartz NA NA 157000.00 7 Quartzite NA NA 22400.00 Total :- 35988371.00 53302591.00 51768577.00 21 5. Details of Production of Sand or Bajari in last three years Sand is mined from the bank of , Petesri, Kotri, Darrekasa and, Amner, Surhi river. Motinala and Tehri Nala also contribute the sand mining from the respective villages along their bank. Details of Production & Royalty of Sand in last Three years Ordanary Sand S.No. Financial Year Production of Sand (in M 3) Royalty Recieved in Rs. 1 2013-14 198749 3974980 2 2014-15 444949 8898980 3 2015-16 164535 3290700 ftyk jktukanxkao esa fnukad 15 -05 -2016 dh fLFkfr esa ?kksf"kr jsr ?kkVksa dh tkudkjh O;fDr@QeZ@,tsalh dk [kljk jdck vf/klwfpr Ø- LFkku dk uke rglhy fjekdZ uke Øekad ¼gsDVs;j esa½ fnukad 1 2 3 4 5 6 7 8 lq[kjh 106 dk 1 xzke iapk;r] NqbZ[knku Mksaxjxkao 2.023 12/01/2009 Ik;kZoj.k lEefr izkIr ¼NqbZ[knku½ VqdM+k 2 vkjxkao xzke iapk;r] vkjxkao Mksaxjxkao 336@1 6.072 05/12/2014 Ik;kZoj.k lEefr izkIr 3 vkljk xzke iapk;r] vkljk Mksaxjxkao 359] 360 6.514 04/04/2015 Ik;kZoj.k lEefr izkIr 4 bZjk xzke iapk;r] bZjk jktukanxkao 688 6.073 20/05/2015 Ik;kZoj.k lEefr izkIr 5 vkfy[kqaVk xzke iapk;r] vkjxkao Mksaxjxkao 381 5.466 20/05/2015 Ik;kZoj.k lEefr izkIr 6 es<+k xzke iapk;r] flaxkjiqj Mksaxjxkao 395 8.709 27/10/2014 Ik;kZoj.k lEefr izkIr 7 ch:Vksyk xzke iapk;r] vk;cka/k Nqfj;k 1 6.073 26/05/2014 Ik;kZoj.k lEefr izkIr 8 /kuxkao xzke iapk;r] /kuxkao Nqfj;k 749 5 05/05/2015 Ik;kZoj.k lEefr izkIr Ik;kZoj.k lEefr gsrq 7.692 24/07/2014 9 cxekj xzke iapk;r] HkVxquk jktukanxkao 1 SEIAA dks izsf’kr Ik;kZoj.k lEefr gsrq 6.073 21/10/2010 10 [kqTth xzke iapk;r] [kqTth Mksaxjxkao 1 SEIAA dks izsf’kr Ik;kZoj.k lEefr gsrq 8 28/12/2015 11 dgxkao xzke iapk;r] dgxkao ekuiqj 1 SEIAA dks izsf’kr Ik;kZoj.k lEefr gsrq 6.883 16/01/2014 12 lkadjk xzke iapk;r] lkadjk jktukanxkao 1028 SEIAA dks izsf’kr Ik;kZoj.k lEefr gsrq 5.668 06/02/2014 13 ukfn;k xzke iapk;r] ukfn;k Nqfj;k 542 SEIAA dks izsf’kr Ik;kZoj.k lEefr gsrq 7.222 21/12/2015 14 fcgjh[kqnZ xzke iapk;r] fcgjhdyk vEckx<+ pkSdh 1 SEIAA dks izsf’kr Ik;kZoj.k lEefr gsrq 6.8 03/03/2014 15 flaxkjiqj xzke iapk;r] flaxkjiqj Mksaxjxkao 180 SEIAA dks izsf’kr Ik;kZoj.k lEefr gsrq 16 lkYgs xzke iapk;r] lkYgs Nqfj;k 1@1 5.668 23/05/2014 SEIAA dks izsf’kr 22 O;fDr@QeZ@,tsalh dk [kljk jdck vf/klwfpr Ø- LFkku dk uke rglhy fjekdZ uke Øekad ¼gsDVs;j esa½ fnukad 1 2 3 4 5 6 7 8 Ik;kZoj.k lEefr gsrq 6.073 28/01/2016 17 jkrkik;yh xzke iapk;r] jkrkik;yh Mksaxjxkao 1@1 SEIAA dks izsf’kr Ik;kZoj.k lEefr gsrq 6 24/02/2016 18 23 6. PROCESS OF DEPOSITION OF SEDIMENTS IN THE RIVERS Rivers have a lot of energy and because they have energy, they do stuff. The obvious things rivers do with their energy is flow but, besides this, they also transport load, erode load and erode the channel through which they flow. Erosion is the breaking down of material by an agent. In the case of a river, the agent is water. The water can erode the river’s channel and the river’s load. A river’s load is bits of eroded material, generally rocks, which the river transports until it deposits its load. A river’s channel is eroded laterally and vertically making the channel wider and deeper. The intensity of lateral and vertical erosion is dictated by the stage in the river’s course, discussed in more detail here but essentially, in the upper stage of the river’s course (close to the source of the river) there is little horizontal erosion and lots of vertical erosion. In the middle and lower stages vertical erosion is reduced and more horizontal erosion takes place. There are several different ways that a river erodes its bed and banks. The first is hydraulic action, where the force of the water removes rock particles from the bed and banks. This type of erosion is strongest at rapids and waterfalls where the water has a high velocity. The next type of erosion is corrasion. This is where the river’s load acts almost like sandpaper, removing pieces of rock as the load rubs against the bed & banks. This sort of erosion is strongest when the river is transporting large chunks of rock or after heavy rainfall when the river’s flow is turbulent. Corrosion is a special type of erosion that only affects certain types of rocks. Water, being ever so slightly acidic, will react with certain rocks and dissolve them. Corrosion is highly effective if the rock type of the channel is chalk or limestone (anything containing calcium carbonate) otherwise, it doesn’t have much of an effect. Cavitation is an interesting method of erosion. Air bubbles trapped in the water get compressed into small spaces like cracks in the river’s banks. These bubbles eventually implode creating a small shockwave that weakens the rocks. The shockwaves are very weak but over time the rock will be weakened to the point at which it falls apart. The final type of erosion is attrition. Attrition is a way of eroding the river’s load, not the bed and banks. Attrition is where pieces of rock in the river’s load knock together, breaking chunks of rock off of one another and gradually rounding and shrinking the load. 24 Transportation, when a river erodes the eroded material becomes the river’s load and the river will then transport this load through its course until it deposits the load. There are a few different ways that a river will transport load depending on how much energy the river has and how big the load is. The largest of particles such as boulders are transported by traction. These particles are rolled along the bed of the river, eroding the bed and the particles in the process, because the river doesn’t have enough energy to move these large particles in any other way. Slightly smaller particles, such as pebbles and gravel, are transported by saltation. This is where the load bounces along the bed of the river because the river has enough energy to lift the particles off the bed but the particles are too heavy to travel by suspension. Fine particles like clay and silt are transported in suspension; they are suspended in the water. Most of a river’s load is transported by suspension. Solution is a special method of transportation. This is where particles are dissolved into the water so only rocks that are soluble, such as limestone or chalk, can be transported in solution. Capacity & Competence Rivers can only carry so much load depending on their energy. The maximum volume of load that a river can carry at a specific point in its course is called the river’s capacity. The biggest sized particle that a river could carry at a specific point is called the river’s competence. Deposition to transport load a river needs to have energy so when a river loses energy it is forced to deposit its load. There are several reasons why a river could lose energy. If the river’s discharge is reduced then the river will lose energy because it isn’t flowing as quickly anymore. This could happen because of a lack of precipitation or an increase in evaporation. Increased human use (abstraction) of a river could also reduce its discharge forcing it deposit its load. If the gradient of the river’s course flattens out, the river will deposit its load because it will be travelling a lot slower. When a river meets the sea a river will deposit its load because the gradient is generally reduced at sea level and the sea will absorb a lot of energy. As rivers get nearer to their mouths they flow in increasingly wide, gentle sided valleys. The channel increases in size to hold the extra water which the river has to receive from its tributaries. As the river gets bigger it can carry larger amounts of material. This material will be small in size, as larger rocks will have broken up on their way from the mountains. Much of the material will be carried in suspension and will erode the river banks by abrasion. When rivers flow 25 over flatter land, they develop large bends called meanders. As a river goes around a bend most of the water is pushed towards the outside causing increased erosion. The river is now eroding sideways into its banks rather than downwards into its bed, a process called lateral erosion. On the inside of the bend, in contrast, there is much less water. The river will therefore be shallow and slow-flowing. It cannot carry as much material and so sand and shingle will be deposited. This is called a point bar or slip off slope. Due to erosion on the outside of a bend and deposition on the inside, the shape of a meander will change over a period of time. Notice how erosion narrows the neck of the land within the meander. In time, and usually during a flood, the river will cut right through the neck. The river will then take the new, shorter route. The fastest current, called the thalweg, will now tend to be in the centre of the river, and so deposition is likely to occur in gentler water next to the banks. Eventually deposition will block off the old meander to leave an oxbow lake. The oxbow lake will slowly dry up, only refilling after heavy rain or during a flood. Streams lose velocity and make deposits when their gradient decreases, when the volume of water decreases, when there is an increase in cross section, when they encounter obstructions, or when they enter still water. They deposit alluvial fans, alluvial cones, piedmont alluvial plains, channel fill, bars, flood plains and deltas. 26 7. General Profile of the District S.No. Particulars Statistics 1 General Information Geographical Area 8022.55 km 2 Geographical Position N 20°07' - 21°50' E 80°29' - 81°13' Administrative Division/Number of Tehsil 9 No. of Panchayat/Villages 1653 Population (As Per Census 2011) 1537133 Population Density (As Per Census 2011) 192 2 Geographology Major Physiographic Units Granite, Limestone, Sand Stone, Flag Stone, Quartzite, etc. Major Drainage , Peteshri, Sukha River, Kotri River, Dalekasa Nala, Tehri Nala, Matiyamoti Nala, Temprature (in °C) Min. 10 Max. 45 3 Land use (Km 2) Forest Area 2695.91 4 Major Soil Types 5 Number of Ground Water Monitoring Stations of CGWB (10.05.2016) Number of Dugwells 53 Water Level No. of Major Bridges 60 6 Hydrologeology Major Water Bearing Formation Limestone Pre-Monsoon depth of water level During 2012 Attached Post Monsoon depth of water level during 2012 Attached 7 Mining Scenario Total No. of Mining Leases (Major Minerals 5 Total Area of Mining Leases (Major Minerals) 203.036 Hact. Total Royalty or Revenue Received from Minor 1076.209 Lac. Minerals in 2015-16 Total No. of Mining Leases (Minor Minerals) 110 Total No. of Mining Leases (Minor Minerals) 166.914 Hact. Total Royalty or Revenue Received from Minor 517.685 Lac. Minerals in 2015-16 Total No. Notified Sand Leases 39 Total Area of Sand Leases 253.221 Hact. Total Production of Sand in 2015-16 164535 m 3 No. of Quarry lease extended as per Amended 71 CGMMR 2015 27 28 8. Land Use Pattern in the district: Forest, Agriculture, Horticulture, Mining etc . i) Forest : Total forest area under Rajnandgaon District is 2695.91 sq. km. comparising Rajnandgaon Forest Division, Khairgarh Forest division and Panabaras Project Division. S.No Forest Division Area (Sq. Km.) 1 Rajnandgaon 891.82 2 Khairagarh 1305.00 3 Panabaras Project 499.09 Total 2695.91 No sanctuary or any other reserved area of forest is situated at Rajnandgaon ii) Agriculture and Irrigaton: Total cultivable area is 447000 ha. or 4470.00 sq km. Mainly paddy is cultivated here. In 1653 villages more than 12.64 lakh population is mainly dependent on agriculture. Approx 76 % of district population is literate irriagtion is mainly dependent on streams and rivers namely , patesri, kotri, tehri nala, darekasa and motinala are popular on which traffic bridge has been constructed. iii) River s: is the main river which forms the eastern border of the distt. Many tributaries of Shivanth flow towards east from west. Petesri and khokha river flow in the southern area, Amner river is in the khairagarh region. Only 23 % of the distt is under irrigation hence stop dam and anicut construction is must. iv) Transportation: Road is the major means of transportation. Rajnandgaon and dongargarh tehsil headquarter is connected by rail line.N.H. joins the distt. H.Q.with Nagpur and Raipur, all other major towns are connected by state highways.Most of the villages are connected under PMGSY and MMGSY. 29 Geomorphic Forms/Elements 30 9. Physiography of the District Physiographically, the district in general exhibits pediment/pediplain landfrom with structural and denudational hills and valleys' with few structural plains, denudationa plateaux and flood plain (including in-filled river beds) in the northern part. The district forms mostly a part of Shivnath Sub-basin with the areas in western and southern part forming part of Wainganga sub-basin. Shivnath and Amner rivers and its triburaries constitute the surface drainange systerm of the area. The general gradient of most of the area is towards east direction with the southern part bearing wainganga sub-basin showing gradient towards south direction. The maximum elevation in the area is 770m above mean sea level as recorded in the northwestern part while the minimum elevation of 296 m above mean sea level is noted around 11 km southwest of Rajnandgaon. Shivnath River constitutes main drainage basin of the district. Main tributaries are Amner, Surhi rivers. River Shivnath forms the eastern boundary of the district Therefore most of the rivers forming its tributaries flow from west to east. Only in north western part of the district some small nalas flow from east to west forming tributaries of Wainganga river. Kotri and Khohka rivers flow in the southern part of the district. 31 10. Rainfall of District Rajnandgaon Month wise jktukanxkao ft yk varxZr foxr rhu o"kksZ esa fx jh o"kkZ dh ekfld tkudkjh o"kkZ ekid d sUnz dk uke ¼o"kkZ fe -eh - esa½ o"kZ 2013&14 ekg x.MbZ NqbZ[knku [kSjkx<+ Mksaxjx<+ jktukanxkao Nqfj;k Mksaxjxko pkSdh eksgyk ekuiqj rFkk o"kZ Apr-13 0.00 0.00 4.0 16.4 40.2 9.0 8.0 0.0 20.1 0.0 May-13 0.0 0.0 0.0 0.0 3.4 0.0 0.0 0.0 0.0 0.0 Jun-13 140.6 129.0 290.0 302.0 384.2 341.0 236.2 386.8 356.2 382.4 Jul-13 485.3 278.8 461.8 621.0 606.2 557.0 530.2 673.4 795.8 715.5 Aug-13 281.0 166.4 280.8 345.0 264.2 227.0 277.2 419.3 384.0 476.2 Sep-13 111.6 108.0 149.8 110.6 99.6 123.0 101.0 51.8 32.0 159.0 Oct-13 148.5 125.0 122.0 103.6 213.3 94.0 176.5 161.4 246.0 298.2 Nov-13 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 Dec-13 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 Jan-14 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 Feb-14 78.0 30.0 29.0 31.4 15.3 16.0 36.4 34.6 43.8 21.0 Mar-14 66.0 22.0 42.0 34.0 8.1 8.0 26.2 32.0 4.0 58.0 o"kZ 2014&15 ekg x.MbZ NqbZ[knku [kSjkx<+ Mksaxjx<+ jktukanxkao Nqfj;k Mksaxjxkao pkSdh eksgyk ekuiqj rFkk o"kZ Apr-14 0.0 0.0 0.0 21.2 23.9 0.0 0.0 7.4 0.0 0.0 May-14 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 Jun-14 112.0 88.0 56.6 113.0 79.6 93.0 131.2 129.2 118.0 41.2 Jul-14 308.0 327.0 545.6 495.0 605.6 458.0 404.8 566.2 482.2 782.0 Aug-14 160.5 89.0 149.6 193.8 125.2 265.0 180.6 335.0 266.0 284.0 Sep-14 126.0 73.0 93.2 198.4 237.2 229.0 295.4 307.8 378.0 422.0 Oct-14 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 Nov-14 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 Dec-14 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 Jan-15 26.0 34.0 3.0 13.4 5.0 42.0 10.3 12.0 29.0 5.0 Feb-15 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 Mar-15 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 32 o"kZ 2015&16 ekg x.MbZ NqbZ[knku [kSjkx<+ Mksaxjx<+ jktukanxkao Nqfj;k Mksaxjxkao pkSdh eksgyk ekuiqj rFkk o"kZ Apr-15 0.0 0.0 0.0 7.0 0.0 0.0 0.0 0.0 0.0 0.0 May-15 0.0 0.0 0.0 4.6 37.0 0.0 0.0 0.0 0.0 0.0 Jun-15 136.0 145.0 105.2 277.0 307.2 157.0 192.8 167.1 235.0 399.2 Jul-15 250.0 121.6 144.8 207.8 214.0 166.0 139.4 151.6 168.0 235.0 Aug-15 152.0 115.2 199.8 238.8 193.4 121.4 128.6 161.2 180.0 234.0 Sep-15 101.3 127.0 190.8 321.2 153.4 168.1 170.2 182.7 250.0 218.5 Oct-15 0.0 10.0 0.0 0.0 1.4 0.0 0.0 0.0 0.0 0.0 Nov-15 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 Dec-15 0.0 0.0 0.0 0.0 12.3 0.0 0.0 0.0 0.0 0.0 Jan-16 0.0 0.0 0.0 0.0 1.2 0.0 0.0 0.0 0.0 0.0 Feb-16 18.0 0.0 0.0 0.0 2.8 0.0 0.0 0.0 0.0 0.0 Mar-16 35.2 12.5 18.2 43.6 43.2 46.4 33.2 40.4 70.0 42.0 33 Geohydrology Map of Rajnandgao District 34 11. Geology and Mineral Wealth 1. Geology :- 1.1 .Archaean :- Rock formations ranging in age from Archaean to Cenozoic are exposed in the district. The oldest rocks in the area are represented by Amagaon Geisic complex of Archaean age (>2500 Ma) Amgaon Gneissic complex exposed in the southern part comprises gneiss and granitic gneiss with enclaves of quartz-mica shist, mica schist, kyanite-sillimanite schist, fuchsite quartzite, quartzite, phyllite, banded magnetite quartzite and banded iron formation. Bailadila Group of Aarchaean to Palaeo Proterozoic age (2500-2200 Ma) exposed in the southereastern extent comprises quartzite, banded iron formation, banded hematite quartzite, ferruginous shale and tuff. 1.2. Palio Proterozoic :- Nandgaon Group of Palaeo Proterozoic age (2200-2000 Ma)Comprises meta-rhyolite, agglomerate, granophyre, granophyre, rhyolite tuff, meta-basalt, meta-andesite, shale, conglomerate, acid tuff, arkosic wacke, gabbro and ultramafic rock. The meta-rhyolite with agglomerate, granophyre, rhyolitic tuff and meta- basalt with meta- andesite are the major lithounits of this group and occupy the southeastern, mid-western an northwestern part of district. Rest of the litho units of Nandgaon Group ae exposed in the southeastern part of the district. The litho-sequence of Nangaon Group is intruded by Dongargarh Granite in the southern part and Malanjkhand Granitoids in the northwestern part of the district. The Dongargarh Granite varies in composition through grandiprite to diorite and is profusely intruded by quartz veins/reefs, pegmatite and dolerite dykes. Malanjkhand granitoids range in compositions throuth granodiorite to quartz diorite. 35 1.3. Meso Proterozoic: - Chilpi Group of rocks of Palaeo to Meso Proterozoic age (2200- 1600 m.y.) are exposed in the northwestern part of the district. It comprises slate, shale, quartzite and grewack. Khairagarh Group of rocks of Meso Proterozoic age comprising alternate sequence of the sedimentaries and volcanics are represented by Bortalao, Sitagota, Karutola, Mangikhuta, Ghogra and Kotima formation. It is exposed in the north western part of the district. Bortalao Formation comprises sandstone with a linear conglomerate band. Sitagota Formation comprises gray, porphyritic to non-porphyritic andsite and occasional dacite, minor tuffs and agglomerate at places. Karutola Formation comprises medium to coarse grained, pure and gerruginous orthoquartzite. Mangikhuta Formation comprises non-vesicular, porphyritic to non - porphyritic andesite. Ghogra formation comprises ferruginous and feldspathic sandstone. Kotima Formation comprises andsite with relatively high proportion of ignimbrites and minor associated tuff. Khairagarh Group of rock have faulted contact with Chhattisgarh Supergroup but at places unconformable contact has also been noticed. 1.4.Meso to Neo Proterozoic :- Undeformed and unmetamorphosed sedimentary sequence of rocks belonging to Chhattisgarh Supergroup of Meso to Neo Proterozoic age(2000-900 m.y.) occupy the northeastern and mid-eastern part of district. Chhattisgarh Supergroup is represented by Chandarpur and Raipur groups. Chandarpur Group comprises mostly arenitic and at places ferruginous sandstone and polymictic conglomerate sandstone shows shale parting at places. Raipur Group is classified into Charmuria, Gunderdehi and Chandi formations. Charmuria Formation is dominantly a carbonate facies and is represented by cherty limestone, dark grey, phritiferous and argillaceous limestone and purple phosphatic limestone. Gunderdehi Formation is dominantly a calcareous- argillite litho facies. It comprises calcareouse, highly friable, purple shale associated with imperistent stromatolitic limestone bands, and intra-formational arenite. It comprises stromatolitic 36 limestone and dolomitic limestone with ferruginous and glauconitic sandstone. 1.5. Palaeogene :- Deccan trap of cretaceous to Palaeogene age (65-60 m.y.) is noticed 21 km west- northwest of Khairagarh. It is represented by porphyritic to non-porphyritic basaltic lava flows with a 10to 25 m thick lateritic cover. Laterite forms and extensive capping over Chilpi Group of rocks in the northwestern part of District.it is also noticed on the other formations. Minerals :-The district is rich in terms of economic mineral wealth. The important economic mineral deposits/occurrences reported in the district are clay, dolomite, fluorite, gold, limestone, arsenopyrite, nickel, ochre, potash and radioactive minerals. A 5 m thick band of white clay has been reported at Musalijob. Other small deposits of clay are reported at Charbhata, Mohanpur, Korelagarh, Dabka, Dhaba, Markakasa, Rangakathera, and Kohka. Flurite deposits associated with quartz veins/reefs as lenticles occur in a 19Km long belt stretching from Kotapani to Lamti Dongri. Chandi Dongri is a major Fluorite deposit located in the area. Gold is reported in the amner River section near Khairagarh and in quartz veins at Tappa. The occurrences o farsenopyrite in meta-basalt and meta-andesite are reported at Kaurikasa. Occurrence of Radiocative Mineral within shear zones in meta-basalt, meta- rhyolite and granite is reported at Bhandaritola, Bodal, Sitagaon and Aundhi. Potash occurrence in glauconitic sandstone is reported at Balgaon. Limestone deposits in Raipur Group are reported near Murhipar, Achholi and Awardha. Dolomite associated with limestone is reported from Khairagah. Ochre is reported at Gandai and Thakurtola. 37 Geology and Mineral Map of Rajnandgaon District, Chhattisgarh 38 39 Other Information of the District Drainage system with description of main rivers Sand is mined from the bank of , Petesri, Kotri, Darekasa and,Amner, Surhi river. Motinala and Tehri Nala also contribute to the sand mining from the respective area along their bank.The lease for sand minning is granted to local Panchyat. ¼i½ egRoiw.kZ ufn;ksa vk Sj /k kjkvksa dh eq[;&eq[; tkudkjh l-dz- unh ;k /kkjk dk uke ftys esa dqy nwjh mn~xe dk LFkku mn~xe ij ÅapkbZ fjekdZ ¼fd -eh - esa½ 1 2 3 4 5 6 1 f'koukFk unh 144 xksnzh 440 ehVj 2 isVsJh unh 44 ykSg>jh 420 ehVj 3 lw[kk unh 47 cklikgkj 420 ehVj 4 nkjsdlk unh 44 BsydknaM 492 ehVj 5 Vsgjh ukyk 37 rsUnqHkkaBk 340 ehVj ¼xBqyk] ikjhZukyk½ 6 efV;keksrh ukyk 33 /kkscuh 415 ehVj 7 ?kqefj;k ukyk 53 egdk 450 ehVj 8 dksrjh unh 45 lqfM;ky 498 ehVj ¼eksgyk½ ¼ii ½ egRoiw.kZ ufn;ksa vk Sj /kkjkvksa dh eq[;&eq[; tkudkjh l-dz- unh ;k /kkjk dk uke fudklh {ks= oxZ fd -eh - ftys ds fudklh % {ks= ¼ftys esa fudklh {ks=½ oxZ fd -eh - 1 2 3 4 1 f'koukFk unh 28-88 30% 2 isVsJh unh 5-28 100% 3 lw[kk unh 5-17 100% 4 Mkysdlk unh 4-40 100% 5 Vsgjh ukyk ¼xBqyk] ikjhZukyk½ 3-70 100% 6 efV;keksrh ukyk 2-97 100% 7 ?kqefj;k ukyk 4-77 100% 8 dksrjh unh 4-05 100% 40 Geohydrology Map of Rajnandgaon 41 Geotechnical and Natural Hazards Map of Rajnandgaon District 42 Landuse Map of Rajnandgaon District 43 Note: The information provided in this report has been prepared from the existing and latest data collected from the concerned authorities. Although utmost care has been taken during editing and printing, still there may be some minor corrections for which the Directorate of Geology & Mining, Regional office Raipur Sonakhan Bhawan, cannot be held responsible. The queries in this regard are most welcome by the concerned office. 44