district survey report of balodabazar...

DISTRICT SURVEY REPORTOF BalodaBazar - Bhatapara

2016

DGM

24/06/2016

DIRECTORATE OF GEOLOGY AND MININGMINERAL RESOURCES DEPARTMENT

Govt. of Chhattisgarh

1

Note:

The information provided in this report has been prepared from the existing andlatest data collected from the concerned authorities. Although utmost care has beentaken during editing and printing, still there may be some minor corrections for whichthe Directorate of Geology & Mining, Regional office Raipur Sonakhan Bhawan, cannotbe held responsible. The queries in this regard are most welcome by the concernedoffice.

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LOCATION AND COMMUNICATION MAP – BALODA BAZAR DISTRICT

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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) andDistrict - Environment Assessment Committee (DEAC) are to be constituted by the divisionalcommissioner for prior environmental clearance of quarry for minor minerals. The DEIAA and DEACwill scrutinize and recommend the prior environmental clearance of ministry of minor minerals on thebasis of district survey report.

The main purpose of preparation of District Survey Report is to identify the mineral resourcesand 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 thebasis of data collected from different concern departments.

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

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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.

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General Information of Balodabazar District

Areain

Sq.

Sub-division

No. ofTahsils

No. ofBlocks

No ofGram

Panchayat

No. of Villages Populationas per 2011

%LiteracyHabited Inhabited

1 2 3 4 5 6 7 8 94680Sq.

4 6 6 611 946 14 1305343 70.63

District Population & Literacy in 2011

TotalPopulation

Male Female Rural Urban %Literacy

1305343 651474 653869 1137160 166183 70.63

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3.List of Mining Leases and Sand in the District with location, area andperiod of validity

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6-11-2017rd

9 Jh m"kk eDdM ifr Jhlat; eDdM fuoklhHkkVkikjk


78]87]

102@2

01-08-2008 ls31-07-2018

10 Jh vt; 'kekZ vk- Jheksguyky 'kekZ fuoklhHkkjrh; LVsV cSad dsihNs] lqHkk"k okMZHkkaVkikjk


471@2

18-08-2008 ls17-08-

2018 rd

11 Jh fufru Hkwwlkfu;k vk-Jh Hkkxor izlknfuoklh o rglhyHkkVkikjk jkBkSj


471@2

18-08-2008 ls17-08-

2018 rd12 J)k baVjizkbZtsl

Hkkxhnkj v’kksd pkSjfl;kvk- Lo- egkohj izlknpkSjfl;k fuoklh Hkuiqjhjk;iqj


471@2

08-10-2008 ls07-10-

2018 rd

13 Jh uanfd’kksj vxzokyvk- Jh fd’ku vxzokyfu- frYnk usojk] ftykjk;iqj


80]81@1

]81@2

]81@3

]81@4

15-01-2009 ls14-01-

2019 rd

14 gjtl feujYl izks-Jherh fleju dkSj ifrJh txuhr flag fu-lqgsyk HkkVkikjk


17]29@1

]471@

2

15-01-2009 ls14-01-

2019 rd

1 2 3 4 5 6 7 8 9

15Jh /kujkt tlokuhfirk Jh eksVwey fuoklhHkkVkikjk ftyk jk;iqj


86]57]

86@1]

90@3]

102@1] 4

6-6-2009ls

5-6-2019

mailto:73@1mailto:34@2mailto:102@2mailto:471@2mailto:471@2mailto:471@2mailto:81@1mailto:81@2mailto:81@3mailto:81@4mailto:29@1mailto:471@2mailto:86@1mailto:90@3mailto:102@1

17

100]90@2] 89

16 Jh 'kf’kdkar frokjh vk-Jh yYyu flag fuoklhpkScs dkyksuh jk;iqj


111]112

14-2-2011ls

13-2-202117 Jh lkSjHk feJk vk- Jh

fo'oukFk feJk fu- ewjkrglhy frYnk ftykjk;iqj

pwukiRFkj jkuhtjkSn jkuhtjkSn flexk 4-50,dM

471@2

11-9-2009ls

10-9-2019

18 Jh /khjt nEekuh vk-Jh jktdqekj nEekuhfuoklh jkexlkxjikjkjk;iqj


471@2

26-4-2010ls

25-4-2020

19 Jherh lhek iky ifrJh iadt iky fuoklh,drk uxj xqf

18

flg vk- Jh /keZnRrfuoklh f’kdkjhds’kyhrglhy flexk

31]54]

55] 57

22-8-2017rd

28 Jherh izfrHkk Bkdqj ifrJh v’kksd Bkdqjfuoklh HkkVkikjk

pwukiRFkj vkekdksuh vkekdksuh flexk 1-069gSDVj

1] 2 31-12-2011 ls30-12-2021

29 Jh jk/ks’;ke xksM vk- Jhcks/kh jke xksM+ fuoklhvkekdksukh rglhyflexk

pwukiRFkj vkekdksuh vkekdksuh flexk 2-70gSDVj

23] 24 18-5-2011ls

17-5-2021

30 Jh jkef[kykou /kqzo vk-Jh fijFkh /kzqo fuoklhlqgsyk

pwukiRFkj vkekdksuh vkekdksuh flexk 1-020gsDVj

58 16-7-2007ls

15-7-2017rd

31 Jh Hkwus’oj oekZ vk- Jhjk/ks”;ke fuoklhu;kikjk lqgsyk flexk

pwukiRFkj vkekdksuh vkekdksuh flexk 2-00,dM+

16]17]18]

19] 20]21]22

3-3-2008ls

2-3-2018rd

32 Jh clar pdz/kkjh vk-Jh 'k=qgu yky pdz/kkjhfuoklh eksgck cktkjjk;iqj ftyk jk;iqj


208 26-4-2008ls

25-4-2018rd

33 Jherh dqarh ckbZ oekZifr Jh jke'kadj oekZfuoklh vkekdksuhrglhy flexk ftykjk;iqj


208 26-4-2008ls

25-4-2018rd

34 Jh fouksn 'kekZ vk- JhlR;ukjk;.k 'kekZfuoklh cqM+xgu rglhyflexk

pwukiRFkj cqM+xgu cqM+xgu flexk 2-70,dM+

171]172@

1

2-2-2010ls

1-2-2020

35 Jh ckykth feujYl izksJh Hkh[kepan fuekyoh; uxj nqxZ

pwukiRFkj [kSjokjh cklhu flexk 1-788gsDVj

391]392]393

1-12-2007ls

31-12-2017 rd

1 2 3 4 5 6 7 8 9

36Jh lkfgy flag vk- Jhv’kksd flag fu-,evkbZth 25 'kadjuxj] jk;iqj

pwukiRFkj efV;k efV;k flexk 2-000gsDVj

967 30-09-2008 ls29-09-

2018 rd37 Jh O;klukjk;.k ;nw

firk Jh tSrqjkefuoklh[kEgfj;k rglhyHkkVkikjk

pwukiRFkj efV;k efV;k flexk 1-554gsDVj

96 6-6-2009ls

5-6-2019

mailto:172@1

19

38 Jh ghrsUnz dqekj ;nq vk-Jh izse dqekj fu0ejkZdksuk rg- flexkftyk jk;iqj

pwukiRFkj nsojhMhg cqphikj flexk 1-60,dM+

212 19-12-09ls

18-12-2019

39 Jh jtuhdkar flag vk-Jh lar lsod flagfuoklh fidkMyh gksVyds ihNs

pwukiRFkj f'kdkjhdslyh

f'kdkjhdslyh

flexk 0-353gsDVj

518]520

14-8-2007ls

13-8-2017rd

40 Jh fufru Hkqlkfu;kfuoklh HkkVkikjkrglhy HkkVkikjk

pwukiRFkj f'kdkjhdslyh

f'kdkjhdslyh

flexk 0-50,dM

636@3

23-8-2010ls

22-8-202041 vxzoky feu0 Hkkxhnkj

lanhi vxzoky fu-7Mh&12 vuqie uxj]jk;iqj

pwukiRFkj fcuSdk fcuSdk flexk 0-850gsDVj

604 27-3-2008ls

26-3-2018rd

42 Jh nsosUnz rkezdj firkJh jke rkezdj fu-flexk rglhy flexkft- jk;iqj

pwukiRFkj dslnk dslnk flexk 3-20,dM

317 2-3-2009ls

1-3-2019

43 Jh v:.k dqekj u'khusvk- Jh ds-ds- fuoklhmik/;k; uxj jk;iqj

pwukiRFkj Qjgnk Qjgnk flexk 1-715gsDVj

599]600

26-11-2009 ls25-11-2019

44 Jh eksgu yky Hkheukuhvk- Jh eksVwey fu-ljtw cxhtk fcykliqj

feV~Vh fyerjk f>fj;k flexk 1-620gsDVj

182 ovU; 9[kljk

23-8-2010ls

22-8-202045 Jh vkf’k"k dqekj vk- Jh

fnyhi fuoklh frYnkusojk

pwukiRFkj cqM+xgu cqM+xgu flexk 5-90,dM

177]178]

22-2-2012ls

21-2-202246 Jh jkgqy lkafMY; vk-

Jh ihds lkafMY; fuoklhDokVj uacj Mh,l&3bUnzizLr dkyksuh] jk;iqj

pwukiRFkj [kSjokjh cklhu flexk 0-760gsDVj

499 19-5-2011ls

18-5-2021

47 Jherh vkuanh 'kekZ ifrJh izeksn 'kekZ fuoklhjkVkSj pkSd tokgj uxjjk;iqj


607]608]

609@1]609@2]3] 4]

610@1]2]

16-8-2012ls

15-8-2022

1 2 3 4 5 6 7 8 948 Jh jk/ks’;ke vk- Jh

cks/khjke /kqo fuoklhpqp:axiqj rglhyflexk


25 16-8-2012ls

15-8-2022

49 Jh banj tXxh vk- Jhukudpan tXxh fuoklh'kadj uxj jk;iqj


26 10-10-2012 ls9-10-2022

50 lrxq: lkbZukFk ekbUl,aM feujYl izk fyfe-eSusftd Mk;jsDVj

pwukiRFkj Vsdkjh Vsdkjh flexk 4-50,dM

273]274]275]

8-4-2013ls

7-4-2023

mailto:636@3mailto:609@1mailto:609@2mailto:610@1

20

Jherh dYiuk frokjh 27651 'kqHke uRFkkuh vk- Jh

vt; dqekj fuoklhlnj cktkj HkkVkikjk

pwukiRFkj Vsdkjh Vsdkjh flexk 3-50,dM

271]272

28-1-2013ls

27-1-202352 Jh fufru Hkqlkfu;k vk-

Jh Hkkxor izlknfuoklh d̀".kk uxjHkkVkikjk


8] 98] 29-11-2014 ls28-11-2024

53 Jh v:.k dqekj ;nw vk-Jh gjd fuoklheksfV;kMhg flexk

pwukiRFkj nsojhMhg nsojhMhg flexk 9-00,dM+

212 17-3-2011ls

16-3-202154 tSulal dSfj;j ekbfuax

,aM VªkUliksVZ dkWUVªsDVjikVZuj fnyhi tSufuoklhcykSnkcktkj&HkkVkikjk


30@1]

33@1] 32]51]49]50]

52] 54

25-2-2015ls s 24-2-2025

Vhi %& bl izdkj ftys ds 6 rglhyksa esa dqy 7 feÍh] 1 MksyksekbV vkSj 7 Q'khZiRFkj ,oa 104pwukiRFkj 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 Lohdr̀ mR[kfuiV~Vksa dh lwph

¼v½ feV~Vh ¼Soil ½

INFORMATION ON SOILS FOR THE DISTRICT (AREA IN HA.)

S.No. Name of theblock

Black Bhata (Red Soil) Matasi Soil Dosra Soil TotalArea % Area % Area % Area % Area

1 2 3 4 5 6 7 8 9 10 11

mailto:30@1mailto:33@1

21

1 Balodabazar 9329 19.08 4989 20.96 19372 19.44 11303 20.00 449932 Palari 13166 26.94 470 1.97 17004 17.9 12022 21.97 426623 Bhatapara 5071 10.38 5199 21.84 15160 12.8 8419 14.77 338494 Simga 7685 1.63 6300 26.46 18405 16.32 10735 19.18 431255 Kasdol 7137 14.6 5244 9.42 19345 18.27 6813 1.95 385396 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 YearMajor Minerals

ftykcykSnkcktkj varxZr izkIr jktLo dh tkudkjh

ftyk cykSnkcktkj&HkkVkikjk varxZr foRrh; o"kZ 2013&14 ls 2015&16 rd eq[; [kfut izkIr jktLo dhtkudkjh

4. (ii)Details of Royalty or Revenue Received in Last Three YearMinor 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 dhtkudkjh

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

foRrh;o"kZ

eq[; [kfut ls izkIr jktLo¼:i;ks esa½

pwukiRFkj MksykskekbZV

2013&14 1040745948 671819

2014&15 1259652314 816818

2015&16 1620996580 0

;ksx 3921394842 1488637

22

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 yearsftys 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 ukyksaesa dqy 15 jsr mR[kuu gsrq iapk;rks dks vuqefr nh xbZ gSA bu jsr [knkuks ls 401913 ?ku eh- jsrmR[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 tgkajsr [knkuLohdr gS A

[kljkuacj

jdck i;kZoj.kLohd̀frdzekadfnukad

vof/k ek=k ¼izfr o"kZ½

01 xzke iapk;r gjnh rglhy

cykSnkpcktkj &HkkVkikjk

gjnh 1435 4-047

gsDVj

1378@23-

12-2013

03 o"kZ 80000 D;w eh-

02 xzke iapk;r MksxjhMhg

rglhy cykSnkcktkj tyk

cykSnkcktkj & HkkVkikjk

MksxjhMhg 632 2-000

gsDVj

1380@23-

12-2013

03 o"kZ 40000 D;w eh-

1 2 3 4 5 6 7 803 xzke iapk;r ijlkikyh

rglhy cykSnkcktkj

ftyk cykSnkcktkj &

HkkVkikjk

ijlkikyh 612 2-000

gsDVj

1372@23-

12-2013

03 o"kZ 40000 D;w eh-

04 xzke iapk;r frYnk

rglhy cykSnkcktkj

frYnk 2099 5-000

gsDVj

1386@24-

12-2013

03 o"kZ 33000 D;w eh-

mailto:1378@23-mailto:1380@23-mailto:1372@23-mailto:1386@24-

23

ftyk cykSnkcktkj &

HkkVkikjk

05 xzke iapk;r eksgrjk

rglhy dlMksy ftyk


fppiksy 01 2-000

gsDVj

1370@23-

12-2013

03 o"kZ 40000 D;w eh-

06 xzke iapk;r fla?kkjh

rglhy cykSnkcktkj

ftyk cykSnkcktkj &

HkkVkikjk

fla?kkjh 838 dk

Hkkx

10-000

gsDVj

4000@26-

11-2015

02 o"kZ 150000 D;w eh-

07 xzke iapk;r pjkSnk

rglhy iykjh ftyk


pjkSnk 1290

dk

VqdMk

5-200

gsDVj

4056@30-

11-2015

02 70200 ?ku eh

08 xzke iapk;r nrjsaxh

rglhy iiykjh ftyk


nrjsaxh 1512 5-2000

gsDVj

4549@12-1-

2016

02 78000 ?ku eh

09 xzke iapk;r eyiqjhrglhy iiykjh ftykcykSnkcktkj & HkkVkikjk

eyiqjh 502 dkVqdM

5-0580gsDVj

4562@27-1-2016

02 75000 ?ku eh

10 xzke iapk;r eksgku

rglhy iykjh ftyk


eksgku 293 6-075

gsDVj

4990/15-3-

2016

02 50000 ?ku eh

11 xzke iapk;r pdjok;

rglhy flexk ftyk


pdjok; 1@1 5-179

gsDVj

36/6-4-2016 02 50000 ?ku eh

1 2 3 4 5 6 7 812 xzke iapk;r vksVscan rg-

HkkVkikjk ftyk

cykSnkcktkj&HkkVkikjk

vksVscan 736 6-000

gsDVj

34/6-4-2016 02 90000 ?ku eh

13 xzke iapk;r jhokMhg

rglhy iykjh ftyk

jhokMhg 450 dk

VqdMk

6-070

gsDVj

129/18-4-

2016

02 90000 ?ku eh

mailto:1370@23-mailto:4000@26-mailto:4056@30-mailto:4549@12-1-mailto:4562@27-1-mailto:1@1

24


14 xzke iapk;r [kSjk vkfJr

xzke ikagnk rg- iykjh

ftyk

cykSnkcktkj&HkkVkikjk

ikagnk 1213

dk Hkkx

10-000

gsDVj

331/28-5-

2016

02 100000 ?ku eh

15 xzke iapk;r cEguh

rglhy iykjh ftyk


cEguh 654 dk

VqdMk

5-200

gsDVj

342/31-5-

016

02 520000 ?ku eh

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

dz- foRrh; o"kZ izsf"kr [kfut ¼jsr½ dhek=k ¼?ku eh esa½

tek jk;YVh jkf’k ¼:i;ks esa ½ fjekdZ

1 2013&14185560 3711200

&

2 2014&15128662 2573240

&

3 2015&16401913 8038260

&

6. PROCESS OF DEPOSITION OF SEDIMENTS IN THE RIVERSSedimentation 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

mailto:k@xzke

25

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

26

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

27

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 Statistics1 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 TehsilNo. of Panchayat/Villages 611

28

Population (As Per Census 2011) 130343Population Density (As Per Census 2011) 279

2 GeographyMajor Physiographic UnitsMajor Drainage Mahanadi, Seonath, Jonk,

Balmadehi3 Land use (Km2)

Forest Area 96601.80 Hect.4 Major Soil Types Black, Red ,Sandy & Lomy soil5 Number of Ground Water Monitoring Stations of CGWB (10.05.2016)

Water LevelNo. of Stop DamNo. of AnikatNo. of Major Bridges

6 HydrologeologyMajor Water Bearing FormationPre-Monsoon depth of water level During 2012Post Monsoon depth of water level during 2012

7 Mining ScenarioTotal No. of Mining Leases (Major Minerals 25Total Area of Quarry Leases (Minor Minerals)Total Royalty or Revenue Received from MajorMinerals in 2015-16

3928.88 Lakh

Total Royalty or Revenue Received from MinorMinerals in 2015-16

214.42 Lakh

Total No. Notified Sand Leas 15 Nos.Total Area of Sand Leases 74 Hect.

Total Production of Sand in 2015-16 401913 Cubic mtrsNo. of Quarry lease extended As per AmendedCGMMR 20150.

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

(i) Forest :-

29

(ii)River :-

30

(iii)Agriculture and Irrigation:

9. Physiography of the District

Physiographically, the northern part of district exhibits mostly the landform ofstructural plains with structural hills and valleys, denudational slop, denudational hillsand valleys, pediments/pediplains and flood plains along the courses of Mahanadi,Kharunand and Seonath rivers. The southern part of district exhibits mostly the landformof pediment/pediplain with upper level and lower level structural plateaux, structuralterrace/rocky bench,denudational slope, denudational hills and valleys and older flood

31

plain. The district forms mostly a part of Mahanadi basin. Mahanadi, Seonath rivers andtheir tributaries constitute the surface drainange systerm of the area. The generalgradient 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 ofdistrict, while the minimum elevation of 236m above mean sea level is recorded at 4.5km north west of Kasdol.

10. Rainfall of District Raipur Month wise

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1 cykSnk cktkj 970-20 592-4 849-8 257-4 Growth2 flexk 1057-70 893-7 1152-2 258-5 Growth3 HkkVkikjk 969-10 953-0 887-0 66-0 Loss

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32

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iykjh 880-80 957-8 930-8 27-0 Loss5 dlMksy 1115-50 958-0 1129-2 171-2

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11. Geology and Mineral Wealth

Geology

Balodabazar district is situated in the eastern part of the Chhattisgarh State. . Itfalls 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 Bilaspurand janjgir districts in the north, Raigarh and Mahasamund districts of Chhattisgarh andKalahandi district of Orissa State in the east, Koraput District of Orissa in the south andDhamtarai and Durg districts in the west. Raipur, the district and State headquarters issituated in the mid-western part of the district. Bhatapara, Balodabazar,Kasdol, Sarsiwasome of the major towns/villages.

Physiographically, the northern part of district exhibits mostly the landform ofstructural plains with structural hills and valleys, denudational slop, denudational hillsand valleys, pediments/pediplains and flood plains along the courses of Mahanadi,Kharunand and Seonath rivers. The southern part of district exhibits mostly the landformof pediment/pediplain with upper level and lower level structural plateaux, structuralterrace/rocky bench,denudational slope, denudational hills and valleys and older floodplain. The district forms mostly a part of Mahanadi basin. Mahanadi, Seonath rivers andtheir tributaries constitute the surface drainange systerm of the area. The generalgradient 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 ofdistrict, while the minimum elevation of 236m above mean sea level is recorded at 4.5km north west of Kasdol in the north eastern part of district.

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

The rocks of Sonakhan Group of Palaeo Proterozoic age comprising meta-volcanic and associated meta-sedimentaries unconformably overlie the gneissic complexand are exposed in the northeastern part of district. Sonakhan Group is classified into

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three formations viz. Baghmara, Arjuni and Bilari, Baghmara formation comprisesmetaultramafic, amphibolite, banded ferruginous chert, meta-rhyolite and tuff. ArjuniFormation 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 withdacite and meta-tuff. The volcano-sedimentary sequence of Sonakhan Group is intrudedby a large gabbroic complex of variable composition like peridotite, pyroxenite, gabbroand anorthositic gabbro.

Undeformed and unmetamorphosed sedimentaray sequence of rocks belonging toChhattisgarh Supergroup of Meso to Neo Proterozoic age overlies the granitoids androcks of Sonakhan Group. the Chhattisgarh Seupergroup occupies the central, northernand north eastern part of district and is represented by Chandarpur and Raipur groups.Chandarpur Group has been classified into two formations(viz. Lohardih andKansapathar) in the central part of district. In the North eastern part of district, it ismarked as unclassified Chandarpur Group. Lohardih Formation is mostly arenitic innature and comprises arenitic to arkosic sandstone with polymictic conglomerate at thebase. Kansapathar Formation is dominantly an arenitic facies and comprises highlymatured glauconitic quartz arenite. Raipur Group is classified into six formations viz.Charmuria, Gunderdehi, Chandi, Tarenga, Hirri and Miniari formations. CharmuriaFormation is dominantly a carbonate facies and is represented by phosphatic,argillaceous, cherty and dolomitic limestone and arenite. Gunderdehi Formation isdominantly a calc-argillite litho facies. It comprises calcareous, highly friable, purpleshale associated with impersistent stromatolitic limestone bands, and intra-formationalconglomerate lenses in the upper part. Chandi Formation is mostly a calcareous facieswith intra-formational arenite. It comprises stromatolitic limestone and dolomite withargillaceous 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 greybedded dolomite associated with light grey laminated argillaceous dolomite. MiniariFormation is the closing phase of Chhattisgarh basin and comprises shale with lensesand intercalation of dolomite, dolomitic limestone and gypsum.

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

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Mineral

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

Other Information of the District

Drainage system with description of main riversShivnath

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 insouth western parts of Rajnandgaon and flows towards north east direction. ShivnathRiver measures length about 345 KM. City Durg is situated on east bank of ShivnathRiver. It flows towards north east passing through Khujji, Rajnandgaon, Durg, Dhamdhaand 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 BalodDistrict. This river flows towards north and joins (meet) Shivnath River at Somnath nearSimga. This river determines the boundary of Raipur and Durg district. The length ofthis river is about 120 KM.

Mahanadi

The Mahanadi is a major river in East Central India. It drains an area of around 141,600square 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 wordMahanadi literally comes from two odia words 'maha' and nadi' meaning 'The GreatRiver'.

Like many other seasonal Indian rivers, the Mahanadi too is a combination of manymountain streams and thus its precise source is impossible to pinpoint. However itsfarthestheadwaters 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 hillshere are an extension of the Eastern Ghats and are a source of many other streams whichthen go on to join the Mahanadi.

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For the first 80 kilometres (50 mi) of its course, the Mahanadi flows in a northerlydirection and drains the Raipur district and touches eastern portions of Raipur city. It is arather narrow river at this stage and the total width of its valley does not exceed 500–600metres.

Sand is mined from the bank of Mahanadi, Sheonath and Kharun, but most of theRetghat is running in Mahanadi river of Arang and Abhanpur Tehsil. The valleybetween the Mahanadi and the Kharun is marked by a long ridge of higher landextending from Kurud in the south, through Abhanpur, Lakholi, Kharora and Palari toLahud in the north east direction. The low ridge bifurcates near Abhanpur and itswestern branch extends through Mandir Hasaud to Mandhar in the north. The Mahanadimain canal and its branches and distributaries have been constructed along these ridgesor their off-shoots. A large number of small streams flow through the low-lying areaswhich are diverted to join the Mahanadi in the east, the Kharun in the west and theSeonath in the north. The drainage system in the plain as well as hilly areas is opendendritic consequent type.

Jonk river :-

Jonk River is a tributary of Mahanadi River that flows for approximately 210kilometers through the Nuapada District and Bargarh District in the state of Odisha; andthe 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 isjoined by a stream called Gaidhas-nala near Patora village. The river forms Beniadhasfall (80 feet) and Kharaldhas fall (150 feet) before entering the valley.[2] It joinsMahanadi at Sheorinarayan of the Balodabazr district.

यातायातसुवधा :-

9 (रायपुरसेकोरबा) का 79.4 क .मी.10 (कोटासेबलौदाबाजार) का 42 क .मी., 13

(पामगढ़सेसोहेलाउ़ डसा सी मा) का 42 क .मी., 14 (पथौ रा से 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-रसद ा -हथबंध 48.6 क .मी., भाटापारा-नपनया 47.6 क .मी., भाटापारा-जरौद-सुहेला 28.8 क .मी.

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

40

सुहेलामागपर 10, बला सप ु रमा गपर 15, बसना, पथौ रा मा गपर 2-2, आरंगमागपर 5 वकोरबामागपर 1बससंचालतहो ती है ।इसके अला वा रा यपु र-झारसुगडाहा या बलौ दा बा जा ररे लमागको12वीयोजनामशा मलकयागयाह ै ।

LOCATION AND VILLAGES MAP - BALODABAZAR

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कृषवसं चाइ :-बलौदाबाजारिजलेकछ : तहसीलकेअं तगतकृषकाकु लरकबा 269888

970 गांवक 10: 86

4 ,

, नालेसथतह ै ,, शवना थ ,

1935-36 मलगभग 200 क .मी.

,

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वन :-875.27 -

,

जहांपयटनवभा गवा रासा, खैरवारडीह (बलौदाबाजार), धमनी, धाराशव (पलार ), कचलोन (समगा ), सुमा (भाटापारा)

GEOTECHN

ICAL & NATURAL HAZARDS

district survey report of balodabazar...

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