DISTRICT SURVEY REPORT of Balodabazar - Bhatapara

2016

DISTRICT SURVEY REPORT OF BalodaBazar - Bhatapara

DIRECTORATE OF GEOLOGY AND MINING MINERAL RESOURCES DEPARTMENT Govt. of Chhattisgarh

DGM

24/06/2016 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.

1 LOCATION AND COMMUNICATION MAP – BALODA BAZAR DISTRICT

2 1. INTRODUCTION

With reference to the gazette notification dated 15th January 2016, ministry of Environment, Forest and Climate Change, the district- environment Impact Assessment Authority (DEIAA) and District - Environment Assessment Committee (DEAC) are to be constituted by the divisional commissioner for prior environmental clearance of quarry for minor minerals. The DEIAA and DEAC will scrutinize and recommend the prior environmental clearance of ministry of minor minerals on the basis of district survey report. The main purpose of preparation of District Survey Report is to identify the mineral resources and mining activities along with other relevant data of district. This report contains details of Lease, Sand mining and Revenue which comes from minerals in the district. This report is prepared on the basis of data collected from different concern departments.

Balodabazar Distrct forms part of the Raipur Commissionary in the Chhattisgarh Region and occupies the south eastern part of the upper Mahanadi basin. The Balodabazar including 6 tehsil namely Balodabazar , Kasdol, Bilaigarh, Bhatapara, Simga, and Palari. The toatal area of the District is 4680 km2. Balodabazar is the third populous district in the state with population of 13,05,343 Of which Male and Female where 65,1,474 and 6,53,869 Respectively . The Mahanadi is the main river, which runs throughthe centre of the district. The eastern boundry of the district run along Jonkriver which flows towards North joining the Mahanadi. A large number of small streams flow through the low lying area which are diverted to join the Mahanadi in the east . The district is well connected with other district headquarter of the state through the National & state highway number 9 ,10,13 and 14 also there is good network of other roads. Bhatapara is the main city of the district situated on the Bombay-Howrah broad-guage of SECR Raipur-Bilaspur section Air connectivity is furnished by Swami Vivekanand national airport. District Headquarter of BalodaBazar was named after the sale and purchases of Bail and Boda(Oxe and buffalo) Bailbodabazar followed by Balodabazar. BalodaBazar is situated in the north eastern part of the Raipur Division Headquarter. It falls in the survey of India degree sheet Nos. 64/G, K, and L between the Latitude 21°10' To 21°54' N And longtitude 81°43'00 To 81°54'00 The district is bounded by Janjgir and Bilaspur in the North Bemetara and Mungeli in the west Raigadh in the east and Mahasamund and the Raipur in the south.The district is well connected by road from Raipur, Bhatapara, Bilaspur, and Mahasamund.

3 2. OVERVIEW OF MINING ACTIVITY OF DISTRICT

Balodabazar District is famous for Sonakhan (Gold) and Cement in Chhattisgarh.Gold, Limestone(cement low grade)Leterite, Sandstone, Quartzite, River sand and flagstone are main mineral found in district. Cement Grade Limestone occur in the Karhi-Chandi, Bharwadih, Kukurdih, Sonpurishuklabhata, Arjuni, Rawan, Sonadih, Maldi-Mopat, Hirmi, Gaitara, Semradih, Mohra etc. Mining Leases have been given for cement grade limestone to Ambujacement, Shree cement, Emami cement, Ultratech, Grasim, and Lafarge. Dolomite deposit occurs around Bhatapara, Patpar,Tikolia and Nipaniya. Gold mineralisation has been confirmed, proved and auctioned for detailed exploration to the Vedanta Group in Sonakhan area (Baghmara Block). Beside above granite is capable of sustaining vagaries of weather for long duration. It takes good shine, when cut and polished. Owing to these properties, granites are in much demand in modern constructionwork as decorative stones. In the eastern and north eastern parts of Raipur district different shades of granite/ granite gneisses such as grey, pink and multy coloured have been located. Important localities are Sigupali, Mampali, Dongripali, Rampur, Laxmipur, Murakhar, Tekka, Gopalpur, Bhurkoni, Lakhanpur, Dhelwa, Ramadabri, Khallari, Koriya, Kotonpali, Soyrmar, Botha etc. Occurance of other important minerals like:Dolomiteare also reported in the district.

Based on limestone deposits 7 cement plant are existing in district and 2 are pipeline. 11 mining leases are given for cement plant as captive and 12 leases for other commercial purpose lease for 2 dolomite mineral at Dhanelivillage are sectioned.

4 General Information of Balodabazar District

Area Sub- No. of No. of No of No. of Villages Population % in division Tahsils Blocks Gram Habited Inhabited as per 2011 Literacy Sq. Panchayat 1 2 3 4 5 6 7 8 9 4680 4 6 6 611 946 14 1305343 70.63 Sq.

District Population & Literacy in 2011

Total Male Female Rural Urban % Population Literacy 1305343 651474 653869 1137160 166183 70.63

5 3.List of Mining Leases and Sand in the District with location, area and period of validity ftys esa Lohd`r fo|eku [kfuiV~Vksa dh lwph ¼i½ ftys esa pwukiRFkj [kfuiV~Vks dh lwph %&

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¼b½ ftyk cykSnkcktkj&HkkVkikjk ds rglhy HkkVkikjk eas Lohd`r mR[kfuiV~Vk dh lwph dza- iV~Vsnkj dk uke iw.kZ [kfut [knku xzke xzke rglhy jdck [klj yht irk lfgr iapk;r uacj vof/k 1 'ks[k fljktqy vk- Jh pwukiRFkj rqjek rqjek HkkVkikjk 1-316 134@ 25-9-2007 'ks[k egewn fuoklh gsDVj 1]2]4]1 ls cykSnkcktkj 63@1 24-9-2017 ]2] rd 164@ 4] 155@ 3]5] 157@ 3]5 2 Jh dsrqeku lkgw vk- Jh Q’khZiRFkj rjsaxk rqjek HkkVkikjk 0-866 422@ 12-8-2007 euksgj fuoklh rjsaxk @cksYMj gsDVj 2] ls ftyk jk;iqj 426@ 11-8-2017 1]2 3 Jh eukst Bkdqj vk- Jh pwukiRFkj

14 9 Jh lw;Zdkar ;nw vk- Jh pwukiRFkj rqjek rqjek HkkVkikjk 3-40 266@ 30-09- jke ukjk;.k ;nw fu- ,dM+ 1d] 2008 ls flfoy ykbZu 266@ 29-09- cykSnkcktkj 1 d] 2018 x 10 Jh nsosUn dqekj fuoklh pwukiRFkj rqjek rqjek HkkVkikjk 1-90 266@ 5-3-2010 rqjek rglhy HkkVkikjk ,dM 1d ls ftyk jk;iqj 4-3-2020 11 Jh fot; oekZ vk- Jh pwukiRFkj uokxkao uokxkao HkkVkikjk 2-50 385@ 5-3-2011 cStuke fuoklh uokxkao ,dM 1 ls HkkVkikjk 4-3-2021 12 Jh uanyky tlokuh vk- pwukiRFkj rqjek rqjek HkkVkikjk 2-52 63@1 28-12- Jh usHkunkl fu- ,dM ]6] 2011 ls egklrh okMZ HkkVkikjk 27-12- 2021 13 Jh :isUnz pkS/kjh ch 16 MksykekbZV /kusyh /kusyh HkkVkikjk 3-228 14-9-1998 lsDVj 16 U;w jktsUnz ls uxj jk;iqj 13-9-2018

¼bZ½ ftyk cykSnkcktkj&HkkVkikjk ds rglhy flexk eas Lohd`r mR[kfuiV~Vk dh lwph dza- iV~Vsnkj dk uke iw.kZ [kfut [knku xzke xzke rglhy jdck [klj yht irk lfgr iapk;r uacj vof/k 1 Ogh- ,l- baVjizkbZtsl pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 4-10 471@ 15-2-2007 fuoklh lqgsyk@flexk ,dM+ 2 ls 14-2-2017 2 Jh vfuy dqekj vk- Jh pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 2-70 91 3-10-2011 fd’kupan fuoklh ,dM+ ls HkkVkikjk] rglhy 2-10-2016 HkkVkikjk 3 lkabZ d`".kk LVksu pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 0-405 471@ 29-5-2006 bUMªLVªht izks- vkuan gsDVj 1 ls 'kqDyk fuoklh nsosUnz 28-5-2016 uxj] jk;iqj 4 Jh eukst Bkdqj vk- Jh pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 0-978 84] 27-7-2006 jke d`iky fuoklh gsDVj 85@1 ls u;kikjk HkkVkikjk ftyk ] 2] 26-6-2016 cykSnkcktkj&HkkVkikjk 86@2 rd ] 1 2 3 4 5 6 7 8 9 5 Jh lar: catkjs vk- Jh pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 4-35 93] 1-1-2011 lqdqy fuoklh jkuhtjkSn ,dM 94] ls rglhy flexk 95@1 31-12- ] 2 2021 6 Jh fjiqlqnu oekZ vk- Jh pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 4-10 471@ 16-1-2007 fj[khjke oekZ fuoklh ,dM+ 2 ls ls lqgsyk rglhy flexk 7 15-1-2017 7 Jh lat; eDdM+ vk- Jh pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 0-800 72@1 5-3-2008 tksxsUnj yky fuoklh gsDVj ] ls

15 HkkVkikjk 73@1 4-3-2018 rd 8 Jh f’koe~ LVksu dzs'kj izks- pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 0-348 34@2 7-11-2007 Jh jktk VqVstk vk- Jh gsDVj ] 35 ls ljnkj lksgu flag fu0 6-11-2017 HkkVkikjk rglhy rd HkkVkikjk 9 Jh m"kk eDdM ifr Jh pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 2-86 78] 01-08- lat; eDdM fuoklh ,dM+ 87] 2008 ls HkkVkikjk 102@ 31-07- 2 2018 10 Jh vt; 'kekZ vk- Jh pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 2-145 471@ 18-08- eksguyky 'kekZ fuoklh gsDVj 2 2008 ls Hkkjrh; LVsV cSad ds 17-08- ihNs] lqHkk"k okMZ 2018 rd HkkaVkikjk

11 Jh fufru Hkwwlkfu;k vk- pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 2-50 471@ 18-08- Jh Hkkxor izlkn ,dM+ 2 2008 ls fuoklh o rglhy 17-08- HkkVkikjk jkBkSj 2018 rd 12 J)k baVjizkbZtsl pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 4-50 471@ 08-10- Hkkxhnkj v’kksd pkSjfl;k ,dM+ 2 2008 ls vk- Lo- egkohj izlkn 07-10- pkSjfl;k fuoklh Hkuiqjh 2018 rd jk;iqj 13 Jh uanfd’kksj vxzoky pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 0-631 80] 15-01- vk- Jh fd’ku vxzoky gsDVj 81@1 2009 ls fu- frYnk usojk] ftyk ] 14-01- jk;iqj 81@2 2019 rd ] 81@3 ] 81@4 14 gjtl feujYl izks- pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 1-172 17] 15-01- Jherh fleju dkSj ifr gsDVj 29@1 2009 ls Jh txuhr flag fu- ] 14-01- lqgsyk HkkVkikjk 471@ 2019 rd 2

1 2 3 4 5 6 7 8 9

15 Jh /kujkt tlokuh pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 2-00 86] 6-6-2009 firk Jh eksVwey fuoklh gsDVj 57] ls HkkVkikjk ftyk jk;iqj 86@1 5-6-2019 ] 90@3 ] 102@ 1] 4 16 100] 90@2 ] 89 16 Jh 'kf’kdkar frokjh vk- pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 1-00 111] 14-2-2011 Jh yYyu flag fuoklh gsDVj 112 ls pkScs dkyksuh jk;iqj 13-2-2021 17 Jh lkSjHk feJk vk- Jh pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 4-50 471@ 11-9-2009 fo'oukFk feJk fu- ewjk ,dM 2 ls rglhy frYnk ftyk 10-9-2019 jk;iqj 18 Jh /khjt nEekuh vk- pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 1-821 471@ 26-4-2010 Jh jktdqekj nEekuh gsDVj 2 ls fuoklh jkexlkxjikjk 25-4-2020 jk;iqj 19 Jherh lhek iky ifr pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 1-600 471@ 6-10-2010 Jh iadt iky fuoklh gsDVj 2 ls ,drk uxj xqf<;kjh 5-10-2020 jk;iqj 20 Jh e;qj iVsy fuoklh pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 2-10 471@ 10-3-2010 lqgsyk rglhy flexk ,dM 2 ls ftyk jk;iqj 9-3-2020 21 Jh 'kf’kdkar frokjh vk- pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 2-05 96] 97 26-4-2010 Jh yYyu flag fu- pkScs ,dM ls dkyksuh jk;iqj 25-4-2020 22 Jh nhipan oekZ vk- Jh pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 0-62 38@1 8-4-2011 x.ks’k jke fu- jkuhtjkSn ,dM ]3 ls rg- flexk 7-4-2021 23 vxLr LVksu izks xksfoUn pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 0-98 130] 22-2-2012 jke lkgw fuoklh fgjeh ,dM 127] ls rlghy flexk 129@ 21-2-2022 1] 147@ 1 24 Jh ?ku’;ke flg ejdke pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 0-380 596@1 28-7-2010 vk- Jh vkuan jke gsDVj 4] ls ejdke fuoklh 598@1 27-7-2020 4] jkuhtjkSn rg- flexk 596@2 fty jk;iqj ] 598@2 ] 1 2 3 4 5 6 7 8 9 25 fufru nsoydj vk- Jh pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 0-332 82 24-12- Mh-ch- nsoydj fuoklh gsDVj 2010 ls jkuhtjkSn rglhy 23-12- flexk 2020 26 Jh lat; eDdM+ vk- Jh pwukiRFkj vkekdksuh vkekdksuh flexk 0-83 89] 1-7-2006 tksxsUnz fuoklh gsDVj 90] ls HkkVkikjk] ftyk jk;iqj 91] 30-6-2016 92] 93 rd 27 lR;e ekbUl ,aM pwukiRFkj vkekdksuh vkekdksuh flexk 1-348 27] 23-8-2007 feujYl ikVZuj HkwisUnz gsDVj 28] ls

17 flg vk- Jh /keZnRr 31] 22-8-2017 fuoklh f’kdkjhds’kyh 54] rd rglhy flexk 55] 57 28 Jherh izfrHkk Bkdqj ifr pwukiRFkj vkekdksuh vkekdksuh flexk 1-069 1] 2 31-12- Jh v’kksd Bkdqj gSDVj 2011 ls fuoklh HkkVkikjk 30-12- 2021 29 Jh jk/ks’;ke xksM vk- Jh pwukiRFkj vkekdksuh vkekdksuh flexk 2-70 23] 24 18-5-2011 cks/kh jke xksM+ fuoklh gSDVj ls vkekdksukh rglhy 17-5-2021 flexk 30 Jh jkef[kykou /kqzo vk- pwukiRFkj vkekdksuh vkekdksuh flexk 1-020 58 16-7-2007 Jh fijFkh /kzqo fuoklh gsDVj ls lqgsyk 15-7-2017 rd 31 Jh Hkwus’oj oekZ vk- Jh pwukiRFkj vkekdksuh vkekdksuh flexk 2-00 16] 3-3-2008 jk/ks”;ke fuoklh ,dM+ 17] ls u;kikjk lqgsyk flexk 18] 2-3-2018 19] 20 rd ]21] 22 32 Jh clar pdz/kkjh vk- pwukiRFkj vkekdksuh vkekdksuh flexk 3-40 208 26-4-2008 Jh 'k=qgu yky pdz/kkjh ,dM+ ls fuoklh eksgck cktkj 25-4-2018 jk;iqj ftyk jk;iqj rd 33 Jherh dqarh ckbZ oekZ pwukiRFkj vkekdksuh vkekdksuh flexk 3-00 208 26-4-2008 ifr Jh jke'kadj oekZ ,dM+ ls fuoklh vkekdksuh 25-4-2018 rglhy flexk ftyk rd jk;iqj 34 Jh fouksn 'kekZ vk- Jh pwukiRFkj cqM+xgu cqM+xgu flexk 2-70 171] 2-2-2010 lR;ukjk;.k 'kekZ ,dM+ 172@ ls fuoklh cqM+xgu rglhy 1 1-2-2020 flexk 35 Jh ckykth feujYl izks pwukiRFkj [kSjokjh cklhu flexk 1-788 391] 1-12-2007 Jh Hkh[kepan fu gsDVj 392] ls ekyoh; uxj nqxZ 393 31-12- 2017 rd

1 2 3 4 5 6 7 8 9

36 Jh lkfgy flag vk- Jh pwukiRFkj efV;k efV;k flexk 2-000 967 30-09- v’kksd flag fu- gsDVj 2008 ls ,evkbZth 25 'kadj 29-09- uxj] jk;iqj 2018 rd 37 Jh O;klukjk;.k ;nw pwukiRFkj efV;k efV;k flexk 1-554 96 6-6-2009 firk Jh tSrqjkefuoklh gsDVj ls [kEgfj;k rglhy 5-6-2019 HkkVkikjk

18 38 Jh ghrsUnz dqekj ;nq vk- pwukiRFkj nsojhMhg cqphikj flexk 1-60 212 19-12-09 Jh izse dqekj fu0 ,dM+ ls ejkZdksuk rg- flexk 18-12- ftyk jk;iqj 2019 39 Jh jtuhdkar flag vk- pwukiRFkj f'kdkjhdsl f'kdkjh flexk 0-353 518] 14-8-2007 Jh lar lsod flag yh dslyh gsDVj 520 ls fuoklh fidkMyh gksVy 13-8-2017 ds ihNs rd 40 Jh fufru Hkqlkfu;k pwukiRFkj f'kdkjhdsl f'kdkjhdsl flexk 0-50 636@ 23-8-2010 fuoklh HkkVkikjk yh yh ,dM 3 ls rglhy HkkVkikjk 22-8-2020 41 vxzoky feu0 Hkkxhnkj pwukiRFkj fcuSdk fcuSdk flexk 0-850 604 27-3-2008 lanhi vxzoky fu- gsDVj ls 7Mh&12 vuqie uxj] 26-3-2018 jk;iqj rd 42 Jh nsosUnz rkezdj firk pwukiRFkj dslnk dslnk flexk 3-20 317 2-3-2009 Jh jke rkezdj fu- ,dM ls flexk rglhy flexk 1-3-2019 ft- jk;iqj 43 Jh v:.k dqekj u'khus pwukiRFkj Qjgnk Qjgnk flexk 1-715 599] 26-11- vk- Jh ds-ds- fuoklh gsDVj 600 2009 ls mik/;k; uxj jk;iqj 25-11- 2019 44 Jh eksgu yky Hkheukuh feV~Vh fyerjk f>fj;k flexk 1-620 182 o 23-8-2010 vk- Jh eksVwey fu- gsDVj vU; 9 ls ljtw cxhtk fcykliqj [kljk 22-8-2020 45 Jh vkf’k"k dqekj vk- Jh pwukiRFkj cqM+xgu cqM+xgu flexk 5-90 177] 22-2-2012 fnyhi fuoklh frYnk ,dM 178] ls usojk 21-2-2022 46 Jh jkgqy lkafMY; vk- pwukiRFkj [kSjokjh cklhu flexk 0-760 499 19-5-2011 Jh ihds lkafMY; fuoklh gsDVj ls DokVj uacj Mh,l&3 18-5-2021 bUnzizLr dkyksuh] jk;iqj 47 Jherh vkuanh 'kekZ ifr pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 1-219 607] 16-8-2012 Jh izeksn 'kekZ fuoklh gsDVj 608] ls jkVkSj pkSd tokgj uxj 609@1] 15-8-2022 jk;iqj 609@2] 3] 4] 610@1] 2] 1 2 3 4 5 6 7 8 9 48 Jh jk/ks’;ke vk- Jh pwukiRFkj vkekdksuh vkekdksuh flexk 1-06 25 16-8-2012 cks/khjke /kqo fuoklh gsDVj ls pqp:axiqj rglhy 15-8-2022 flexk 49 Jh banj tXxh vk- Jh pwukiRFkj vkekdksuh vkekdksuh flexk 1-56 26 10-10- ukudpan tXxh fuoklh gsDVj 2012 ls 'kadj uxj jk;iqj 9-10-2022 50 lrxq: lkbZukFk ekbUl pwukiRFkj Vsdkjh Vsdkjh flexk 4-50 273] 8-4-2013 ,aM feujYl izk fyfe- ,dM 274] ls eSusftd Mk;jsDVj 275] 7-4-2023 19 Jherh dYiuk frokjh 276 51 'kqHke uRFkkuh vk- Jh pwukiRFkj Vsdkjh Vsdkjh flexk 3-50 271] 28-1-2013 vt; dqekj fuoklh ,dM 272 ls lnj cktkj HkkVkikjk 27-1-2023 52 Jh fufru Hkqlkfu;k vk- pwukiRFkj vkekdksuh vkekdksuh flexk 0-77 8] 98] 29-11- Jh Hkkxor izlkn gsDVj 2014 ls fuoklh d`".kk uxj 28-11- HkkVkikjk 2024 53 Jh v:.k dqekj ;nw vk- pwukiRFkj nsojhMhg nsojhMhg flexk 9-00 212 17-3-2011 Jh gjd fuoklh ,dM+ ls eksfV;kMhg flexk 16-3-2021 54 tSulal dSfj;j ekbfuax pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 1-462 30@1 25-2-2015 ,aM VªkUliksVZ dkWUVªsDVj gsDVj ] ls s 24-2- ikVZuj fnyhi tSu 33@1 2025 fuoklh ] 32] cykSnkcktkj&HkkVkikjk 51] 49] 50] 52] 54

Vhi %& bl izdkj ftys ds 6 rglhyksa esa dqy 7 feÍh] 1 MksyksekbV vkSj 7 Q'khZiRFkj ,oa 104 pwukiRFkj ds mR[kfuiV~Vk Lohd`r gSA

(ii) List of Quary lease in the district with location area and period of validity ftys dh v|ru fLFkfr esa fo|eku Lohd`r mR[kfuiV~Vksa dh lwph ¼v½ feV~Vh ¼Soil ½ INFORMATION ON SOILS FOR THE DISTRICT (AREA IN HA.)

S.No. Name of the Black Bhata (Red Soil) Matasi Soil Dosra Soil Total block Area % Area % Area % Area % Area

1 2 3 4 5 6 7 8 9 10 11 20 1 Balodabazar 9329 19.08 4989 20.96 19372 19.44 11303 20.00 44993 2 Palari 13166 26.94 470 1.97 17004 17.9 12022 21.97 42662 3 Bhatapara 5071 10.38 5199 21.84 15160 12.8 8419 14.77 33849 4 Simga 7685 1.63 6300 26.46 18405 16.32 10735 19.18 43125 5 Kasdol 7137 14.6 5244 9.42 19345 18.27 6813 1.95 38539 6 Bilaigarh 8305 16.99 4600 19.32 14407 15.25 6900 12.10 34212 Total 50693 89.62 26802 99.97 103693 99.98 56192 89.97 237380

4. (i)Details of Royalty or Revenue Received in Last Three Year Major Minerals ftykcykSnkcktkj varxZr izkIr jktLo dh tkudkjh ftyk cykSnkcktkj&HkkVkikjk varxZr foRrh; o"kZ 2013&14 ls 2015&16 rd eq[; [kfut izkIr jktLo dh tkudkjh

eq[; [kfut ls izkIr jktLo foRrh; ¼:i;ks esa½ o"kZ pwukiRFkj MksykskekbZV 2013&14 1040745948 671819

2014&15 1259652314 816818

2015&16 1620996580 0 ;ksx 3921394842 1488637

4. (ii)Details of Royalty or Revenue Received in Last Three Year Minor Minerals ftykcykSnkcktkjds varxZr izkIr jktLo dh tkudkjh ftyk cykSnkcktkj&HkkVkikjk varxZr foRrh; o"kZ 2013&14 ls 2015&16 rd xkS.k [kfut izkIr jktLo dh tkudkjh

foRrh; o"kZ xkS.k [kfut ls izkIr jktLo ¼:i;ks esa½

21 pwukiRFkj Q’khZiRFkj feV~Vh eq:e MksykekbZV

2013&14 54758524 0 90000 3755000 0

2014&15 73802380 0 32000 1069880 0

2015&16 77778810 0 83500 2591100 464659

;ksx 206339714 0 205500 7415980 464659

5. Details of Production of Sand or Bajari in last three years ftys esa ?kksf"kr jsr [knkuksa dh lwph ckyw (Sand) mR[kuu gsrq ftys esa egkunh]f'koukFk] tksad ,oa ckyensgh unh ,oa mlds lgk;d ukyksa esa dqy 15 jsr mR[kuu gsrq iapk;rks dks vuqefr nh xbZ gSA bu jsr [knkuks ls 401913 ?ku eh- jsr mR[kuu gqvk] ftlls jkW;YVh ds :i esa 80-38 yk[k :i;s 'kklu dks jktLo izkIr gqvkA

ftyk cykSnkcktj&HkkVkikjk esa ?kksf"kr jsr [knkuksa dh lwph dza- xzke iapk;rksa dk uke xzke tgka [kljk jdck i;kZoj.k vof/k ek=k ¼izfr o"kZ½ jsr [knku uacj Lohd`fr Lohdr gS A dzekad fnukad 01 xzke iapk;r gjnh rglhy gjnh 1435 4-047 1378@23- 03 o"kZ 80000 D;w eh- cykSnkpcktkj &HkkVkikjk gsDVj 12-2013

02 xzke iapk;r MksxjhMhg MksxjhMhg 632 2-000 1380@23- 03 o"kZ 40000 D;w eh- rglhy cykSnkcktkj tyk gsDVj 12-2013 cykSnkcktkj & HkkVkikjk

1 2 3 4 5 6 7 8 03 xzke iapk;r ijlkikyh ijlkikyh 612 2-000 1372@23- 03 o"kZ 40000 D;w eh- rglhy cykSnkcktkj gsDVj 12-2013 ftyk cykSnkcktkj & HkkVkikjk

04 xzke iapk;r frYnk frYnk 2099 5-000 1386@24- 03 o"kZ 33000 D;w eh- rglhy cykSnkcktkj gsDVj 12-2013

22 ftyk cykSnkcktkj & HkkVkikjk

05 xzke iapk;r eksgrjk fppiksy 01 2-000 1370@23- 03 o"kZ 40000 D;w eh- rglhy dlMksy ftyk gsDVj 12-2013 cykSnkcktkj & HkkVkikjk

06 xzke iapk;r fla?kkjh fla?kkjh 838 dk 10-000 4000@26- 02 o"kZ 150000 D;w eh- rglhy cykSnkcktkj Hkkx gsDVj 11-2015 ftyk cykSnkcktkj & HkkVkikjk

07 xzke iapk;r pjkSnk pjkSnk 1290 5-200 4056@30- 02 70200 ?ku eh rglhy iykjh ftyk dk gsDVj 11-2015 cykSnkcktkj & HkkVkikjk VqdMk

08 xzke iapk;r nrjsaxh nrjsaxh 1512 5-2000 4549@12-1- 02 78000 ?ku eh rglhy iiykjh ftyk gsDVj 2016 cykSnkcktkj & HkkVkikjk

09 xzke iapk;r eyiqjh eyiqjh 502 dk 5-0580 4562@27-1- 02 75000 ?ku eh rglhy iiykjh ftyk VqdM gsDVj 2016 cykSnkcktkj & HkkVkikjk

10 xzke iapk;r eksgku eksgku 293 6-075 4990/15-3- 02 50000 ?ku eh rglhy iykjh ftyk gsDVj 2016 cykSnkcktkj & HkkVkikjk

11 xzke iapk;r pdjok; pdjok; 1@1 5-179 36/6-4-2016 02 50000 ?ku eh rglhy flexk ftyk gsDVj cykSnkcktkj & HkkVkikjk

1 2 3 4 5 6 7 8 12 xzke iapk;r vksVscan rg- vksVscan 736 6-000 34/6-4-2016 02 90000 ?ku eh HkkVkikjk ftyk gsDVj cykSnkcktkj&HkkVkikjk

13 xzke iapk;r jhokMhg jhokMhg 450 dk 6-070 129/18-4- 02 90000 ?ku eh rglhy iykjh ftyk VqdMk gsDVj 2016

23 cykSnkcktkj & HkkVkikjk

14 xzke iapk;r [kSjk vkfJr ikagnk 1213 10-000 331/28-5- 02 100000 ?ku eh xzke ikagnk rg- iykjh dk Hkkx gsDVj 2016 ftyk cykSnkcktkj&HkkVkikjk

15 xzke iapk;r cEguh cEguh 654 dk 5-200 342/31-5- 02 520000 ?ku eh rglhy iykjh ftyk VqdMk 016 gsDVj cykSnkcktkj & HkkVkikjk

ftyk cykSnkcktkj&HkkVkikjk varxZr foRrh; o"kZ 2013&14 ls 2015&16 rd [kfut jsr dk izsf"kr ek=k@xzke iapk;r es tek jk;YVh jkf'k dh tkudkjh

dz- foRrh; o"kZ izsf"kr [kfut ¼jsr½ dh tek jk;YVh jkf’k ¼:i;ks esa ½ fjekdZ ek=k ¼?ku eh esa½

1 2013&14 & 185560 3711200 2 2014&15 & 128662 2573240 3 2015&16 & 401913 8038260

6. PROCESS OF DEPOSITION OF SEDIMENTS IN THE RIVERS Sedimentation of rivers of District

Process- 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

24 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 corrosion. 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. Cavitations 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. 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

25 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 salvation. 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 many loads 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’s 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 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

26 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.

7. General Profile of the District

S.No. Particulars Statistics 1 General Information Geographical Area 4680 Sq. km2 Geographical Position North Latitude 21°10' to 21°54' East Longitude 81°43" to 81°54" Administrative Division/Number of Tehsil No. of Panchayat/Villages 611

27 Population (As Per Census 2011) 130343 Population Density (As Per Census 2011) 279 2 Geography Major Physiographic Units Major Drainage Mahanadi, Seonath, Jonk, Balmadehi 3 Land use (Km2) Forest Area 96601.80 Hect. 4 Major Soil Types Black, Red ,Sandy & Lomy soil 5 Number of Ground Water Monitoring Stations of CGWB (10.05.2016) Water Level No. of Stop Dam No. of Anikat No. of Major Bridges 6 Hydrologeology Major Water Bearing Formation Pre-Monsoon depth of water level During 2012 Post Monsoon depth of water level during 2012 7 Mining Scenario Total No. of Mining Leases (Major Minerals 25 Total Area of Quarry Leases (Minor Minerals) Total Royalty or Revenue Received from Major 3928.88 Lakh Minerals in 2015-16 Total Royalty or Revenue Received from Minor 214.42 Lakh Minerals in 2015-16 Total No. Notified Sand Leas 15 Nos. Total Area of Sand Leases 74 Hect.

Total Production of Sand in 2015-16 401913 Cubic mtrs No. of Quarry lease extended As per Amended CGMMR 20150.

8. Land Utilition Pattern in the district: Forest, Agriculture, Horticulture, Mining etc.

(i) Forest :-

28 (ii)River :-

29 (iii)Agriculture and Irrigation:

9. Physiography of the District

30 plain. The district forms mostly a part of Mahanadi basin. Mahanadi, Seonath rivers and their tributaries constitute the surface drainange systerm of the area. The general gradient of most of the area is towards north.The maximum elevation in the area is ...... m above mean sea level as recorded at Sonakhan area in the eastern part of district, while the minimum elevation of 236m above mean sea level is recorded at 4.5 km north west of Kasdol.

10. Rainfall of District Raipur Month wise dz- ftyk fodkl[k.M lkekU; o"kkZ xr o"kZ dh o"kkZ o"kZ 2013 esa dqy xr o"kZ ls o"kkZ o"kkZ ¼fn- esa deh ;k o`f) 15@9@2013 dh fLFkfr esa 1 cykSnk cktkj 970-20 592-4 849-8 257-4 Growth 2 flexk 1057-70 893-7 1152-2 258-5 Growth 3 HkkVkikjk 969-10 953-0 887-0 66-0 Loss

31 4 cykSnk iykjh 880-80 957-8 930-8 27-0 Loss 5 cktkj dlMksy 1115-50 958-0 1129-2 171-2 Growth 6 fcykbZx<+ 1086-00 1227-0 1040-0 187-0 Loss vkSlr ftyk 1013-21 930-32 998-17 67-9 Growth

32 33 11. Geology and Mineral Wealth

Geology

Balodabazar district is situated in the eastern part of the Chhattisgarh State. . It falls in the survey of India degree sheet Nos. 64/G, K, and L between the Latitude 21°10' To 21°54' N And longtitude 81°43'00 To 81°54'00. The district is bounded by Bilaspur and janjgir districts in the north, Raigarh and Mahasamund districts of Chhattisgarh and Kalahandi district of Orissa State in the east, Koraput District of Orissa in the south and Dhamtarai and Durg districts in the west. Raipur, the district and State headquarters is situated in the mid-western part of the district. Bhatapara, Balodabazar,Kasdol, Sarsiwa some of the major towns/villages.

Physiographically, the northern part of district exhibits mostly the landform of structural plains with structural hills and valleys, denudational slop, denudational hills and valleys, pediments/pediplains and flood plains along the courses of Mahanadi, Kharunand and Seonath rivers. The southern part of district exhibits mostly the landform of pediment/pediplain with upper level and lower level structural plateaux, structural terrace/rocky bench,denudational slope, denudational hills and valleys and older flood plain. The district forms mostly a part of Mahanadi basin. Mahanadi, Seonath rivers and their tributaries constitute the surface drainange systerm of the area. The general gradient of most of the area is towards north.The maximum elevation in the area is ...... m above mean sea level as recorded at Sonakhan area in the eastern part of district, while the minimum elevation of 236m above mean sea level is recorded at 4.5 km north west of Kasdol in the north eastern part of district.

rock formations ranging in age from Archaean to Cainzoic are exposed in the district.

The rocks of Sonakhan Group of Palaeo Proterozoic age comprising meta- volcanic and associated meta-sedimentaries unconformably overlie the gneissic complex and are exposed in the northeastern part of district. Sonakhan Group is classified into 34 three formations viz. Baghmara, Arjuni and Bilari, Baghmara formation comprises metaultramafic, amphibolite, banded ferruginous chert, meta-rhyolite and tuff. Arjuni Formation comprises meta-conglomerate, meta-greywacke with minor volcanics, meta- argillite with banded ferruginous chert and alternate swquence of meta-basalt and meta- rhyolite &tuff. Bilari Formation comprises meta-conglomerate, meta-greeywacke,, meta- argillite, meta-basalt with basaltic conglomerate and agglomerate, meta-rhyolite with dacite and meta-tuff. The volcano-sedimentary sequence of Sonakhan Group is intruded by a large gabbroic complex of variable composition like peridotite, pyroxenite, gabbro and anorthositic gabbro.

Undeformed and unmetamorphosed sedimentaray sequence of rocks belonging to Chhattisgarh Supergroup of Meso to Neo Proterozoic age overlies the granitoids and rocks of Sonakhan Group. the Chhattisgarh Seupergroup occupies the central, northern and north eastern part of district and is represented by Chandarpur and Raipur groups. Chandarpur Group has been classified into two formations(viz. Lohardih and Kansapathar) in the central part of district. In the North eastern part of district, it is marked as unclassified Chandarpur Group. Lohardih Formation is mostly arenitic in nature and comprises arenitic to arkosic sandstone with polymictic conglomerate at the base. Kansapathar Formation is dominantly an arenitic facies and comprises highly matured glauconitic quartz arenite. Raipur Group is classified into six formations viz. Charmuria, Gunderdehi, Chandi, Tarenga, Hirri and Miniari formations. Charmuria Formation is dominantly a carbonate facies and is represented by phosphatic, argillaceous, cherty and dolomitic limestone and arenite. Gunderdehi Formation is dominantly a calc-argillite litho facies. It comprises calcareous, highly friable, purple shale associated with impersistent stromatolitic limestone bands, and intra-formational conglomerate lenses in the upper part. Chandi Formation is mostly a calcareous facies with intra-formational arenite. It comprises stromatolitic limestone and dolomite with argillaceous intercalations and ferruginous and glauconitic sandstone.

Tarenga Formation is dominantly a calc-argillite facies. It comprises dolomitic argillite, clay and shale with chert intercalations. Hirri Formation comprises mostly a dark grey bedded dolomite associated with light grey laminated argillaceous dolomite. Miniari Formation is the closing phase of Chhattisgarh basin and comprises shale with lenses and intercalation of dolomite, dolomitic limestone and gypsum.

Laterite capping of Cainozoic age is observed over the Chadarpur sandstone in the central part of district.

35 B

36 37 Mineral

The district is rich in terms of economic mineral wealth. The important economic mineral deposits/occurrences reported in the district are amaxonite, Gold, diamond, dolomite. limestone, Diamond incidences in placers.Dolomite outcrops associated with limestone are reported near Bhatapara. Deposits of cement grade limestone from Chandi Formation of Raipur Group, occur near Jhipan, Pendri, Rawan,Niparia Karhi, Chandi, Bharseli, Turma, Mantar and Bahesar. Potash in the form glauconite in sandstone of Chandarpur Group is reported around Kesla, Bhainsa and Halwai Khapri.

Other Information of the District Drainage system with description of main rivers Shivnath Sheonath is main river of District Durg. Shivnath river is tributary of Mahanadi river. Shivnath river originates from Mountain at height of 625 meter at Panabaras situated in south western parts of Rajnandgaon and flows towards north east direction. Shivnath River measures length about 345 KM. City Durg is situated on east bank of Shivnath River. It flows towards north east passing through Khujji, Rajnandgaon, Durg, Dhamdha and Nandghat and joins (meet) Mahanadi near Shivari Narayan of Bilaspur District.

Kharun Kharun river flows in eastern parts of the district starting from Petechua in Balod District. This river flows towards north and joins (meet) Shivnath River at Somnath near Simga. This river determines the boundary of Raipur and Durg district. The length of this river is about 120 KM.

Mahanadi

The Mahanadi is a major river in East Central India. It drains an area of around 141,600 square kilometres (54,700 sq mi) and has a total course of 858 kilometres (533 mi).[1] The river flows through the states of Chhattisgarh and Odisha.The word Mahanadi literally comes from two odia words 'maha' and nadi' meaning 'The Great River'.

Like many other seasonal Indian rivers, the Mahanadi too is a combination of many mountain streams and thus its precise source is impossible to pinpoint. However its farthestheadwaters lie 6 kilometres (3.7 mi) from Pharsiya village 442 metres (1,450 ft) above sea level south of Nagri town in Dhamtari district of Chhattisgarh.[2][3] The hills here are an extension of the Eastern Ghats and are a source of many other streams which then go on to join the Mahanadi.

38 For the first 80 kilometres (50 mi) of its course, the Mahanadi flows in a northerly direction and drains the Raipur district and touches eastern portions of Raipur city. It is a rather narrow river at this stage and the total width of its valley does not exceed 500–600 metres. Sand is mined from the bank of Mahanadi, Sheonath and Kharun, but most of the Retghat is running in Mahanadi river of Arang and Abhanpur Tehsil. The valley between the Mahanadi and the Kharun is marked by a long ridge of higher land extending from Kurud in the south, through Abhanpur, Lakholi, Kharora and Palari to Lahud in the north east direction. The low ridge bifurcates near Abhanpur and its western branch extends through Mandir Hasaud to Mandhar in the north. The Mahanadi main canal and its branches and distributaries have been constructed along these ridges or their off-shoots. A large number of small streams flow through the low-lying areas which are diverted to join the Mahanadi in the east, the Kharun in the west and the Seonath in the north. The drainage system in the plain as well as hilly areas is open dendritic consequent type.

Jonk river :-

Jonk River is a tributary of Mahanadi River that flows for approximately 210 kilometers through the Nuapada District and Bargarh District in the state of Odisha; and the Mahasamund District and Balodabazar District in the state of Chhattisgarh in India. The river starts from the Sundabeda plateau and enters Maraguda valley where it is joined by a stream called Gaidhas-nala near Patora village. The river forms Beniadhas fall (80 feet) and Kharaldhas fall (150 feet) before entering the valley.[2] It joins Mahanadi at Sheorinarayan of the Balodabazr district.

यातायातसुवधा :-

9 (रायपुरसेकोरबा) का 79.4 क .मी. 10 (कोटासेबलौदाबाजार) का 42 क .मी., 13 (पामगढ़सेसोहेलाउ़ डसा सीमा) का 42 क .मी., 14 (पथौ रासे कसड ो ल ) का 46 क .मी., 16 ( ) का 9.2 क .मी. 20 ( ) का 15.3 क .मी. भागबलौदाबाजारिजलेसेगुजरताहै।िजलामागमलवन -खरतोरा 40.6 क .मी., बलौदाबाजार-रसदा - हथबंध 48.6 क .मी., भाटापारा-नपनया 47.6 क .मी., भाटापारा-जरौद-सुहेला 28.8 क .मी.

90 बस (टाइमंग ), भाटापारामागपर 30, गधौ र -बला इगढ़ -भटगांव-सरसीवां-सारंगढ़मागपर 60, समगा -

39 सुहेलामागपर 10, बला सपु रमा गपर 15, बसना, पथौ रामागपर 2-2, आरंगमागपर 5 वकोरबामागपर 1 बससंचालतहो तीहै ।इसके अला वारायपु र-झारसुगडाहा याबलौ दाबाजाररे लमागको 12वीयोजनामशामलकयागयाह ै ।

LOCATION AND VILLAGES MAP - BALODABAZAR

40 कृषवसं चाइ :- बलौदाबाजारिजलेकछ : तहसीलकेअं तगतकृषकाकु लरकबा 269888 970 गांवक 10 : 86 4 ,

, नालेसथतहै , , शवना थ ,

1935-36 मलगभग 200 क .मी.

41 वन :- 875.27 - ,

जहांपयटनवभागवा रा सा, खैरवारडीह (बलौदाबाजार), धमनी, धाराशव (पलार ), कचलोन (समगा ), सुमा (भाटापारा)

42 GEOTECHN ICAL & NATURAL HAZARDS