district survey report of balodabazar -...

DISTRICT SURVEY REPORT

OF BalodaBazar - Bhatapara

2016

DGM

24/06/2016

DIRECTORATE OF GEOLOGY AND MINING

MINERAL RESOURCES DEPARTMENT

Govt. of Chhattisgarh

1

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.

2

LOCATION AND COM M UNICATION M AP – BALODA BAZAR DISTRICT

3

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.

4

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.

5

General Information of Balodabazar District

Area

in

Sq.

Sub-

division

No. of

Tahsils

No. of

Blocks

No of

Gram

Panchayat

No. of Villages Population

as per 2011

%

LiteracyHabited Inhabited

1 2 3 4 5 6 7 8 9

4680

Sq.

4 6 6 611 946 14 1305343 70.63

District Population & Literacy in 2011

Total

Population

Male Female Rural Urban %

Literacy

1305343 651474 653869 1137160 166183 70.63

6

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

period of validity

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4 v kse d zs’ kj m| ksx i zks-J h e ax y p an z

fu o kl h l j kb Zi ky h

e g kl e qan

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g sDVj

10@ 1 5-5-2007

l s

4-5-2017

5 J h g ksj hy ky p an zkfu o kl h e fV; k

r g l hy d l Mksy

ft y k j k; i qj

p wu ki RFkj l fy g k l fy g k?kkV fc y kb Zx < 0-750

g sDVj

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167@ 9]

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177@ 1

20-02-

2008 l s

19-02-

2018

6 J h d e y t y ku v k-J h Hkhj d s’ k fu o kl h

l j l hao k r g l hy

fc y kb Zx < +

p wu ki RFkj t ksx sl j VkVk fc y kb Zx < 1-620

g sDVj

501 29-6-2007

l s

28-6-2017

7 J h fo t ; Hkw"k. ki k. Ms; v k- J h

c wt Hkw"k. k fu - l kj ax <

r g - l kj ax <

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25-9-2009

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24-9-2019

8 J he r h l d quMg fj ; k i fr J h

f’ ko d qe kj Mg fj ; k

fu o kl h ’ kr kCn h u x j

j k; i qj

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25-5-2025

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v o f/ k d s

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fu . kZ;

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Mh f[ ky kj h fu -

d Vksj k r ky kc j k; i qj

p wu ki RFkj l fy g k l fy g k fc y kb Zx < 4-00

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25-5-2025

r d d h

v o f/ k d s

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p wu ki RFkj l fy g k l fy g k?kkV fc y kb Zx < 0-53

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7-9-2010

l s

6-9-2020

11 J h l qj s’ k d qe kj v k-J h j ke p an fu o kl h

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p wu ki RFkj fc l u i qj fc l u i qj fc y kb Zx < 1-85

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234 11-2-2011

l s

10-2-2021

12 J h fu j at u v x zo ky p wu ki RFkj c sy fVd j h c sy fVd j h fc y kb Zx < 0-980 785@ 2] 1-8-2012

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fi r k J h

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31-7-2022

13 J h j kg qy Fko kb Zrv k- J h ’ ; ke y ky

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f’ ko j hu kj k; . k

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266@ 2]

31-8-2012

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30-8-2022

14 J h x ksfo Un ’ ke kZ v k-J h fc g kj h fu o kl h

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p wu ki RFkj / kkj kf’ ko / kkj kf’ ko fc y kb Zx < 1-77

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23-4-2013

l s

22-4-2023

15 y { e h fe u j Yl i zksJ he r h b afn j k p an zk

i fr J h e qj y h/ kj

p wu ki RFkj l ksg kx i qj l ksg kx i qj fc y kb Zx < 0-426

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569@ 2]

567@ 1]

568@ 1]

569@ 1

23-9-2014

l s

22-9-2024

16 v fu y t a?ksy v k- J hHkx r j ke t a?ksy

fu o kl h ’ ; ke u x j

j k; i qj

p wu ki RFkj c sy fVd j h c sy fVd j h fc y kb Zx < + 3-00

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4-7-2012

sl s 06-

7-2017

¼n ½ ft y k c y kSn kc kt kj & HkkV ki kj k d sr g l hy c y kSn kc kt kj e as Lo hd ‘r mR[ kfu i V ~V k d h l wp h


i r k l fg r

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fy ; s i V~Vk

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p wu ki RFkj d s’ kMc j h < kc kMhg c y kSn k

c kt kj

1-10

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45 2-8-2012

l s

1-8-2022

2 J h l at ; v x zo ky v k-J hj ke v x zo ky fu o kl h

c y kSn kc kt kj

p wu ki RFkj < kc kMhg < kc kMhg c y kSn k

c kt kj

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184@

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31-12-

2012 l s

30-12-

2017

3 l at ; v x zo ky fu o kl hc y kSn kc kt kj

p wu ki RFkj < kc kMhg < kc kMhg c y kSn k

c kt kj

4-55

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184@

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17-02-

2009 l s

16-2-2019

4 J h t u d j ke o e kZ v k-J h Q qy p an o e kZ fu -

e q< +hi kj r g l hy

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p wu ki RFkj e q< +hi kj Hkn zki ky h c y kSn k

c kt kj

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2]

176]

175

15-1-2007

l s

14-1-2017

1 2 3 4 5 6 7 8 9

5J he r h me k c kb Z o e kZ

i fr J h Mkse u y ky o e kZ

fu o kl h e q< hi kj

p wu ki RFkj e q< hi kj Hkn zki ky h c y kSn k

c kt kj

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2]3]4]

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2]3]4]

24-5-2011

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23-5-2021

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19-3-2017

7 J he r h j ksg u h n so h o e kZi fr J h j kd s’ k o e kZ

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34]

154

01-06-

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31-5-2017

8 J h d Sy k’ k d sfM; k v k-J h v ac sp an fu o kl h

fo o sd ku an e kx Z

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p wu ki RFkj d s’ kMc j h < kc kMhg c y kSn k

c kt kj

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7@ 1

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17-3-2018

9 J h t ; v ac s LVksu d zs’ kji zks- v ’ kksd d qe kj fu -

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c y kSn kc kt kj

p wu ki RFkj e q< +hi kj Hkzn ki ky h c y kSn k

c kt kj

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165]

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1]2

2-4-2008

l s

1-4-2018

10 J h fg j sUn z v x zo ky v k-J h c n zh fo ’ kky fu o kl h

c y kSn kc kt kj

p wu ki RFkj e q< +hi kj Hkzn ki ky h c y kSn k

c kt kj

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24-8-2007

l s

23-8-2017

11 J h d kse y fd ’ kksj fe J kv k- J h u an fd ’ kksj

fu o kl h Me :

c y kSn kc kt kj

p wu ki RFkj Me : Me : c y kSn k

c kt kj

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11 11-9-2007

l s

10-9-2017

12 J h v ku an d qe kj ; n w v k-J h j ke s’ o j fu o kl h

i St u h c y kSn kc kt kj

p wu ki RFkj d qEg kj h d qEg kj h c y kSn k

c kt kj

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340@

1

22-1-2007

l s

21-1-2017

13 J h ft r sUn z l kg w v k- J hi zse y ky

fu - i zse l k; d y LVksl Z

e su j ksM c y kSn kc kt kj

p wu ki RFkj l y ksu h l y ksu h c y kSn k

c kt kj

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918 1-10-2009

l s

30-9-2019

14 J h l q[ kn so d ao j v k- J hd Su fl g

fu - r kj kf’ ko

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fe V~Vh r kj kf’ ko r kj kf’ ko c y kSn k

c kt kj

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1420

3-12-2009

l s

3-12-2019

15 J h e ksg u i kaMs v k- J hfp ar k fu o kl h

c y kSn kc kt kj

fe V~Vh r kj kf’ ko r kj kf’ ko c y kSn k

c kt kj

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19]

24]

29] 30

29-1-2011

l s

28-1-2021

1 2 3 4 5 6 7 8 9

16J h l an hi d qe kj o e kZ v k-

J h t u d j ke o e kZ

fu o kl h c y kSn kc kt kj

p wu ki RFkj e q< hi kj Hkn zki ky h c y kSn k

c kt kj

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g sDVj

134]

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1

13-7-2012

l s

12-7-2022

17 J h / kqu hj ke c at kj s v k- p wu ki RFkj i j l i ky h Mksasx j hMhg c y kSn k 0-48 184@ 18-7-2012

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14

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¼b ½ ft y k c y kSn kc kt kj & HkkV ki kj k d sr g l hy HkkV ki kj k e as Lo hd ‘r mR[ kfu i V ~V k d h l wp h


i r k l fg r

[ kfu t [ kn ku x zke x zke

i ap k; r


u ac j

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v o f/ k

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c y kSn kc kt kj

p wu ki RFkj r qj e k r qj e k HkkVki kj k 1-316

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1]2]4]1

63@ 1

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164@

4]

155@

3]5]

157@

3]5

25-9-2007

l s

24-9-2017

r d

2 J h d sr qe ku l kg w v k- J he u ksg j fu o kl h r j sax k

ft y k j k; i qj

Q ’ khZi RFkj

@ c ksYMj

r j sax k r qj e k HkkVki kj k 0-866

g sDVj

422@

2]

426@

1]2

12-8-2007

l s

11-8-2017

3 J h e u kst Bkd qj v k- J hv kj -d s-, l Bkd qj fu o kl h

u ; ki kj k o kMZ HkkVki kj k

p wu ki RFkj < kc kMhg < kc kMhg HkkVki kj k 1-716

g sDVj

244 17-8-2007

l s

16-8-2017

r d

4 J h p j . k / kzqo v k- J hc l ar / kqzo fu o kl h r j sax k

ft y k j k; i qj

Q ’ khZi RFkj

@ c ksYMj

r j sax k < kc kMhg HkkVki kj k 1-323

g sDVj

486@

1] 487

20-8-2007

l s

19-8-2017

5 J h j kt s’ k v x zo ky v k-J h e qj kj h v x zo ky fu -

x ka/ kh e afn j o kMZ

HkkVki kj k

p wu ki RFkj x qM+sfy ; k x qM+sfy ; k HkkVki kj k 1-295

g sDVj

898@

2

29-10-

2007 l s

28-10-

2017

6 J h fu fr ’ k v k- J h e qj kj hv x zo ky fu - x ka/ kh e afn j

o kMZ HkkVki kj k

p wu ki RFkj x qM+sfy ; k x qM+sfy ; k HkkVki kj k 0-90

g sDVj

898@

2

3-11-2007

l s

2-11-2017

r d

1 2 3 4 5 6 7 8 9

7 J h d sr qe ku l kg w v k- J he u ksg j y ky l kg w

fu o kl h r j sax k

Q ’ khZi RFkj

@ c ksYMj

r j sax k r j sax k HkkVki kj k 0-945

g sDVj

549@

2]3]6]

553@

1]2]3

23-2-2008

l s

22-2-2018

8 J h l an hi v x zo ky v k-Lo - J h Lo : i p an

fu o kl h Mh& 12 v u qi e

u x j j k; i qj

p wu ki RFkj p e kj x qM+k i Fkfj ; k HkkVki kj k 0-890

g sDVj

80@ 1 15-4-2008

l s

14-4-2018

r d

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9 J h l w; Zd kar ; n w v k- J hj ke u kj k; . k ; n w fu -

fl fo y y kb Zu

c y kSn kc kt kj


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266@

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x

30-09-

2008 l s

29-09-

2018

10 J h n so sUn d qe kj fu o kl hr qj e k r g l hy HkkVki kj k

ft y k j k; i qj


, d M

266@

1d

5-3-2010

l s

4-3-2020

11 J h fo t ; o e kZ v k- J hc St u ke fu o kl h u o kx kao

HkkVki kj k

p wu ki RFkj u o kx kao u o kx kao HkkVki kj k 2-50

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385@

1

5-3-2011

l s

4-3-2021

12 J h u an y ky t l o ku h v k-J h u sHku n kl fu -

e g kl r h o kMZ HkkVki kj k


, d M

63@ 1

]6]

28-12-

2011 l s

27-12-

2021

13 J h : i sUn z p kS/ kj h c h 16l sDVj 16 U; w j kt sUn z

u x j j k; i qj

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l s

13-9-2018

¼b Z½ ft y k c y kSn kc kt kj & HkkV ki kj k d sr g l hy fl e x k e as Lo hd ‘r mR[ kfu i V ~V k d h l wp h

d za- i V ~V sn kj d k u ke i w. kZ

i r k l fg r

[ kfu t [ kn ku x zke x zke

i ap k; r


u ac j

y ht

v o f/ k

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p wu ki RFkj j ku ht j kSn j ku ht j kSn fl e x k 4-10

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471@

2

15-2-2007

l s

14-2-2017

2 J h v fu y d qe kj v k- J hfd ’ ku p an fu o kl h

HkkVki kj k] r g l hy

HkkVki kj k


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91 3-10-2011

l s

2-10-2016

3 l kab Z d ‘". kk LVksub UMªLVªht i zks- v ku an

’ kqDy k fu o kl h n so sUn z

u x j ] j k; i qj


g sDVj

471@

1

29-5-2006

l s

28-5-2016

4 J h e u kst Bkd qj v k- J hj ke d ‘i ky fu o kl h

u ; ki kj k HkkVki kj k ft y k

c y kSn kc kt kj & HkkVki kj k


g sDVj

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27-7-2006

l s

26-6-2016

r d

1 2 3 4 5 6 7 8 9

5 J h l ar : c at kj s v k- J hl qd qy fu o kl h j ku ht j kSn

r g l hy fl e x k


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93]

94]

95@ 1

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1-1-2011

l s

31-12-

2021

6 J h fj i ql qn u o e kZ v k- J hfj [ khj ke o e kZ fu o kl h

l qg sy k r g l hy fl e x k


, d M+

471@

2 l s

7

16-1-2007

l s

15-1-2017

7 J h l at ; e Dd M+ v k- J ht ksx sUn j y ky fu o kl h


g sDVj

72@ 1

]

5-3-2008

l s

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8 J h f’ ko e ~ LVksu d zs’ kj i zks-J h j kt k VqVst k v k- J h

l j n kj l ksg u fl ag fu 0

HkkVki kj k r g l hy

HkkVki kj k


g sDVj

34@ 2

] 35

7-11-2007

l s

6-11-2017

r d

9 J h m"kk e Dd M i fr J hl at ; e Dd M fu o kl h

HkkVki kj k


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78]

87]

102@

2

01-08-

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31-07-

2018

10 J h v t ; ’ ke kZ v k- J he ksg u y ky ’ ke kZ fu o kl h

Hkkj r h; LVsV c Sad d s

i hN s] l qHkk"k o kMZ

HkkaVki kj k


g sDVj

471@

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18-08-

2008 l s

17-08-

2018 r d

11 J h fu fr u Hkwwl kfu ; k v k-J h Hkkx o r i zl kn

fu o kl h o r g l hy

HkkVki kj k j kBkSj


, d M+

471@

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18-08-

2008 l s

17-08-

2018 r d

12 J ) k b aVj i zkb Zt slHkkx hn kj v ’ kksd p kSj fl ; k

v k- Lo - e g ko hj i zl kn

p kSj fl ; k fu o kl h Hku i qj h

j k; i qj


, d M+

471@

2

08-10-

2008 l s

07-10-

2018 r d

13 J h u an fd ’ kksj v x zo kyv k- J h fd ’ ku v x zo ky

fu - fr Yn k u so j k] ft y k

j k; i qj


g sDVj

80]

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81@ 3

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81@ 4

15-01-

2009 l s

14-01-

2019 r d

14 g j t l fe u j Yl i zks-J he r h fl e j u d kSj i fr

J h t x u hr fl ag fu -

l qg sy k HkkVki kj k


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15-01-

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14-01-

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15J h / ku j kt t l o ku h

fi r k J h e ksVwe y fu o kl h

HkkVki kj k ft y k j k; i qj


g sDVj

86]

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102@

1] 4

6-6-2009

l s

5-6-2019

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16 J h ’ kf’ kd kar fr o kj h v k-J h y Yy u fl ag fu o kl h

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111]

112

14-2-2011

l s

13-2-2021

17 J h l kSj Hk fe J k v k- J hfo ’ o u kFk fe J k fu - e wj k

r g l hy fr Yn k ft y k

j k; i qj


, d M

471@

2

11-9-2009

l s

10-9-2019

18 J h / khj t n Ee ku h v k-J h j kt d qe kj n Ee ku h

fu o kl h j ke x l kx j i kj k

j k; i qj


g sDVj

471@

2

26-4-2010

l s

25-4-2020

19 J he r h l he k i ky i frJ h i ad t i ky fu o kl h

, d r k u x j x qf< ; kj h

j k; i qj


g sDVj

471@

2

6-10-2010

l s

5-10-2020

20 J h e ; qj i Vsy fu o kl hl qg sy k r g l hy fl e x k

ft y k j k; i qj


, d M

471@

2

10-3-2010

l s

9-3-2020

21 J h ’ kf’ kd kar fr o kj h v k-J h y Yy u fl ag fu - p kSc s

d ky ksu h j k; i qj


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l s

25-4-2020

22 J h n hi p an o e kZ v k- J hx . ks’ k j ke fu - j ku ht j kSn

r g - fl e x k


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8-4-2011

l s

7-4-2021

23 v x Lr LVksu i zks x ksfo Unj ke l kg w fu o kl h fg j e h

r l g hy fl e x k


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127]

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147@

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22-2-2012

l s

21-2-2022

24 J h ?ku ’ ; ke fl g e j d kev k- J h v ku an j ke

e j d ke fu o kl h

j ku ht j kSn r g - fl e x k

ft y j k; i qj


g sDVj

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]

28-7-2010

l s

27-7-2020

1 2 3 4 5 6 7 8 9

25 fu fr u n so y d j v k- J hMh-c h- n so y d j fu o kl h

j ku ht j kSn r g l hy

fl e x k


g sDVj

82 24-12-

2010 l s

23-12-

2020

26 J h l at ; e Dd M+ v k- J ht ksx sUn z fu o kl h

HkkVki kj k] ft y k j k; i qj

p wu ki RFkj v ke kd ksu h v ke kd ksu h fl e x k 0-83

g sDVj

89]

90]

91]

92] 93

1-7-2006

l s

30-6-2016

r d

27 l R; e e kb Ul , aMfe u j Yl i kVZu j Hkwi sUn z


g sDVj

27]

28]

23-8-2007

l s

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18

fl g v k- J h / ke Zn Rr

fu o kl h f’ kd kj hd s’ ky h

r g l hy fl e x k

31]

54]

55] 57

22-8-2017

r d

28 J he r h i zfr Hkk Bkd qj i frJ h v ’ kksd Bkd qj

fu o kl h HkkVki kj k


g SDVj

1] 2 31-12-

2011 l s

30-12-

2021

29 J h j k/ ks’ ; ke x ksM v k- J hc ks/ kh j ke x ksM+ fu o kl h

v ke kd ksu kh r g l hy

fl e x k


g SDVj

23] 24 18-5-2011

l s

17-5-2021

30 J h j ke f[ ky ko u / kqzo v k-J h fi j Fkh / kzqo fu o kl h

l qg sy k


g sDVj

58 16-7-2007

l s

15-7-2017

r d

31 J h Hkwu s’ o j o e kZ v k- J hj k/ ks” ; ke fu o kl h

u ; ki kj k l qg sy k fl e x k


, d M+

16]

17]

18]

19] 20

]21]

22

3-3-2008

l s

2-3-2018

r d

32 J h c l ar p d z/ kkj h v k-J h ’ k= qg u y ky p d z/ kkj h

fu o kl h e ksg c k c kt kj

j k; i qj ft y k j k; i qj


, d M+

208 26-4-2008

l s

25-4-2018

r d

33 J he r h d qar h c kb Z o e kZi fr J h j ke ’ kad j o e kZ

fu o kl h v ke kd ksu h

r g l hy fl e x k ft y k

j k; i qj


, d M+

208 26-4-2008

l s

25-4-2018

r d

34 J h fo u ksn ’ ke kZ v k- J hl R; u kj k; . k ’ ke kZ

fu o kl h c qM+x g u r g l hy

fl e x k

p wu ki RFkj c qM+x g u c qM+x g u fl e x k 2-70

, d M+

171]

172@

1

2-2-2010

l s

1-2-2020

35 J h c ky kt h fe u j Yl i zksJ h Hkh[ ke p an fu

e ky o h; u x j n qx Z

p wu ki RFkj [ kSj o kj h c kl hu fl e x k 1-788

g sDVj

391]

392]

393

1-12-2007

l s

31-12-

2017 r d

1 2 3 4 5 6 7 8 9

36J h l kfg y fl ag v k- J h

v ’ kksd fl ag fu -

, e v kb Zt h 25 ’ kad j

u x j ] j k; i qj

p wu ki RFkj e fV; k e fV; k fl e x k 2-000

g sDVj

967 30-09-

2008 l s

29-09-

2018 r d

37 J h O; kl u kj k; . k ; n wfi r k J h t Sr qj ke fu o kl h

[ kEg fj ; k r g l hy

HkkVki kj k

p wu ki RFkj e fV; k e fV; k fl e x k 1-554

g sDVj

96 6-6-2009

l s

5-6-2019

mailto:172@1

19

38 J h g hr sUn z d qe kj ; n q v k-J h i zse d qe kj fu 0

e j kZd ksu k r g - fl e x k

ft y k j k; i qj

p wu ki RFkj n so j hMhg c qp hi kj fl e x k 1-60

, d M+

212 19-12-09

l s

18-12-

2019

39 J h j t u hd kar fl ag v k-J h l ar l so d fl ag

fu o kl h fi d kMy h g ksVy

d s i hN s

p wu ki RFkj f’ kd kj hd sl

y h

f’ kd kj h

d sl y h

fl e x k 0-353

g sDVj

518]

520

14-8-2007

l s

13-8-2017

r d

40 J h fu fr u Hkql kfu ; kfu o kl h HkkVki kj k

r g l hy HkkVki kj k

p wu ki RFkj f’ kd kj hd sl

y h

f’ kd kj hd sl

y h

fl e x k 0-50

, d M

636@

3

23-8-2010

l s

22-8-2020

41 v x zo ky fe u 0 Hkkx hn kjl an hi v x zo ky fu -

7Mh& 12 v u qi e u x j ]

j k; i qj

p wu ki RFkj fc u Sd k fc u Sd k fl e x k 0-850

g sDVj

604 27-3-2008

l s

26-3-2018

r d

42 J h n so sUn z r ke zd j fi r kJ h j ke r ke zd j fu -

fl e x k r g l hy fl e x k

ft - j k; i qj

p wu ki RFkj d sl n k d sl n k fl e x k 3-20

, d M

317 2-3-2009

l s

1-3-2019

43 J h v : . k d qe kj u ’ khu sv k- J h d s-d s- fu o kl h

mi k/ ; k; u x j j k; i qj

p wu ki RFkj Q j g n k Q j g n k fl e x k 1-715

g sDVj

599]

600

26-11-

2009 l s

25-11-

2019

44 J h e ksg u y ky Hkhe u ku hv k- J h e ksVwe y fu -

l j t w c x ht k fc y kl i qj

fe V~Vh fy e r j k f> fj ; k fl e x k 1-620

g sDVj

182 o

v U; 9

[ kl j k

23-8-2010

l s

22-8-2020

45 J h v kf’ k"k d qe kj v k- J hfn y hi fu o kl h fr Yn k

u so j k

p wu ki RFkj c qM+x g u c qM+x g u fl e x k 5-90

, d M

177]

178]

22-2-2012

l s

21-2-2022

46 J h j kg qy l kafMY; v k-J h i hd s l kafMY; fu o kl h

Do kVj u ac j Mh, l & 3

b Un zi zLr d ky ksu h] j k; i qj

p wu ki RFkj [ kSj o kj h c kl hu fl e x k 0-760

g sDVj

499 19-5-2011

l s

18-5-2021

47 J he r h v ku an h ’ ke kZ i frJ h i ze ksn ’ ke kZ fu o kl h

j kVkSj p kSd t o kg j u x j

j k; i qj


g sDVj

607]

608]

609@ 1]

609@ 2]

3] 4]

610@ 1]

2]

16-8-2012

l s

15-8-2022

1 2 3 4 5 6 7 8 9

48 J h j k/ ks’ ; ke v k- J hc ks/ khj ke / kqo fu o kl h

p qp : ax i qj r g l hy

fl e x k


g sDVj

25 16-8-2012

l s

15-8-2022

49 J h b an j t Xx h v k- J hu ku d p an t Xx h fu o kl h

’ kad j u x j j k; i qj


g sDVj

26 10-10-

2012 l s

9-10-2022

50 l r x q: l kb Zu kFk e kb Ul, aM fe u j Yl i zk fy fe -

e Su sft d Mk; j sDVj

p wu ki RFkj Vsd kj h Vsd kj h fl e x k 4-50

, d M

273]

274]

275]

8-4-2013

l s

7-4-2023

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20

J he r h d Yi u k fr o kj h 276

51 ’ kqHke u RFkku h v k- J hv t ; d qe kj fu o kl h

l n j c kt kj HkkVki kj k

p wu ki RFkj Vsd kj h Vsd kj h fl e x k 3-50

, d M

271]

272

28-1-2013

l s

27-1-2023

52 J h fu fr u Hkql kfu ; k v k-J h Hkkx o r i zl kn

fu o kl h d ‘". kk u x j

HkkVki kj k


g sDVj

8] 98] 29-11-

2014 l s

28-11-

2024

53 J h v : . k d qe kj ; n w v k-J h g j d fu o kl h

e ksfV; kMhg fl e x k

p wu ki RFkj n so j hMhg n so j hMhg fl e x k 9-00

, d M+

212 17-3-2011

l s

16-3-2021

54 t Su l al d Sfj ; j e kb fu ax, aM VªkUl i ksVZ d kWUVªsDVj

i kVZu j fn y hi t Su

fu o kl h



g sDVj

30@ 1

]

33@ 1

] 32]

51]

49]

50]

52] 54

25-2-2015

l s s 24-2-

2025

V hi %& b l i zd kj ft y s d s 6 r g l hy ksa e sa d qy 7 fe Í h] 1 Mksy kse kbV v kSj 7 Q ’ khZi RFkj , oa 104

p wu ki RFkj d smR[ kfu i V ~V k Lohd ‘r g SA

(ii) List of Quary lease in the district with location area and period of validity

ft y sd h v | r u fLFkfr e sa fo | e ku Lo hd ‘r mR[ kfu i V ~V ksa d h l wp h

¼v ½ fe V ~V h ¼Soil ½

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

S.No. Name of theblock

Black Bhata (Red Soil) M atasi Soil Dosra Soil Total

Area % 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 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

ft y kc y kSn kc kt kj v ar x Zr i zkIr j kt Lo d h t ku d kj h

ft y k c y kSn kc kt kj & HkkV ki kj k v ar x Zr fo Rr h; o "kZ 2013& 14 l s 2015& 16 r d e q[ ; [ kfu t i zkIr j kt Lo d h

t ku d kj h

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

Minor Minerals

ft y kc y kSn kc kt kj d sv ar x Zr i zkIr j kt Lo d h t ku d kj h

ft y k c y kSn kc kt kj & HkkV ki kj k v ar x Zr fo Rr h; o "kZ 2013& 14 l s 2015& 16 r d x kS. k [ kfu t i zkIr j kt Lo d h

t ku d kj h

fo Rr h; o"kZ x kS. k [ kfu t l s i zkIr j kt Lo ¼: i ; ks e sa½

fo Rr h;

o "kZ

e q[ ; [ kfu t l s i zkIr j kt Lo

¼: i ; ks e sa½

p wu ki RFkj Mksy kske kb ZV

2013& 14 1040745948 671819

2014& 15 1259652314 816818

2015& 16 1620996580 0

; ksx3921394842 1488637

22

p wu ki RFkj Q ’khZi RFkj fe V ~V h e q: e Mksy ke kb ZV

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

ft y se sa ?kksf"kr j sr [ kn ku ksa d h l wp h

c ky w(Sand) mR[ ku u g sr q ft y s e sa e g ku n h]f’ ko u kFk] t ksad , o a c ky e n sg h u n h , o a ml d s l g k; d u ky ksa

e sa d qy 15 j sr mR[ ku u g sr q i ap k; r ks d ks v u qe fr n h x b Z g SA b u j sr [ kn ku ks l s 401913 ?ku e h- j sr

mR[ ku u g qv k] ft l l s j kW; YVh d s : i e sa 80-38 y k[ k : i ; s ’ kkl u d ks j kt Lo i zkIr g qv kA

ft y k c y kSn kc kt j & HkkV ki kj k e sa ?kksf"kr j sr [ kn ku ksa d h l wp h

d za- x zke i ap k; r ksa d k u ke x zke t g ka

j sr [ kn ku

Lo hd r g S A

[ kl j k

u ac j

j d c k i ; kZo j . k

Lo hd ‘fr

d ze kad

fn u kad

v o f/ k e k= k ¼i zfr o "kZ½

01 x zke i ap k; r g j n h r g l hy

c y kSn kp c kt kj & HkkVki kj k

g j n h 1435 4-047

g sDVj

1378@ 23-

12-2013

03 o "kZ 80000 D; w e h-

02 x zke i ap k; r Mksx j hMhg

r g l hy c y kSn kc kt kj t y k


Mksx j hMhg 632 2-000

g sDVj

1380@ 23-

12-2013

03 o "kZ 40000 D; w e h-

1 2 3 4 5 6 7 8

03 x zke i ap k; r i j l ki ky h

r g l hy c y kSn kc kt kj

ft y k c y kSn kc kt kj &

HkkVki kj k

i j l ki ky h 612 2-000

g sDVj

1372@ 23-

12-2013

03 o "kZ 40000 D; we h-

04 x zke i ap k; r fr Yn k


fr Yn k 2099 5-000

g sDVj

1386@ 24-

12-2013

03 o "kZ 33000 D; w e h-

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

23


HkkVki kj k

05 x zke i ap k; r e ksg r j k

r g l hy d l Mksy ft y k


fp p i ksy 01 2-000

g sDVj

1370@ 23-

12-2013

03 o "kZ 40000 D; w e h-

06 x zke i ap k; r fl a?kkj h



HkkVki kj k

fl a?kkj h 838 d k

Hkkx

10-000

g sDVj

4000@ 26-

11-2015

02 o "kZ 150000 D; w e h-

07 x zke i ap k; r p j kSn k

r g l hy i y kj h ft y k


p j kSn k 1290

d k

Vqd Mk

5-200

g sDVj

4056@ 30-

11-2015

02 70200 ?ku e h

08 x zke i ap k; r n r j sax h

r g l hy i i y kj h ft y k


n r j sax h 1512 5-2000

g sDVj

4549@ 12-1-

2016

02 78000 ?ku e h

09 x zke i ap k; r e y i qj h

r g l hy i i y kj h ft y k


e y i qj h 502 d k

Vqd M

5-0580

g sDVj

4562@ 27-1-

2016

02 75000 ?ku e h

10 x zke i ap k; r e ksg ku



e ksg ku 293 6-075

g sDVj

4990/15-3-

2016

02 50000 ?ku e h

11 x zke i ap k; r p d j o k;

r g l hy fl e x k ft y k


p d j o k; 1@ 1 5-179

g sDVj

36/6-4-2016 02 50000 ?ku e h

1 2 3 4 5 6 7 8

12 x zke i ap k; r v ksVsc an r g -

HkkVki kj k ft y k


v ksVsc an 736 6-000

g sDVj

34/6-4-2016 02 90000 ?ku e h

13 x zke i ap k; r j ho kMhg


j ho kMhg 450 d k

Vqd Mk

6-070

g sDV j

129/18-4-

2016

02 90000 ?ku e h

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

24


14 x zke i ap k; r [ kSj k v kfJ r

x zke i kag n k r g - i y kj h

ft y k


i kag n k 1213

d k Hkkx

10-000

g sDVj

331/28-5-

2016

02 100000 ?ku e h

15 x zke i ap k; r c Eg u h



c Eg u h 654 d k

Vqd Mk

5-200

g sDVj

342/31-5-

016

02 520000 ?ku e h

ft y k c y kSn kc kt kj & HkkV ki kj k v ar x Zr fo Rr h; o "kZ 2013& 14 l s 2015& 16 r d [ kfu t j sr d k

i zsf"kr e k= k@ x zke i ap k; r e s t e k j k; YV h j kf’ k d h t ku d kj h

d z- fo Rr h; o"kZ i zsf"kr [ kfu t ¼j sr ½ d h

e k= k ¼?ku e h e sa½

t e k j k; YV h j kf’k ¼: i ; ks e sa ½ fj e kd Z

1 2013& 14185560 3711200

&

2 2014& 15128662 2573240

&

3 2015& 16401913 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

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 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

28

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

Minerals in 2015-16

3928.88 Lakh

Total Royalty or Revenue Received from Minor

Minerals 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 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 :-

29

(ii)River :-

30

(iii)Agriculture and Irrigation:

9. Physiography of the District

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

31

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

d z- ft y k fo d kl [ k. M l ke kU; o "kkZ x r o "kZ d h o "kkZ o "kZ 2013 e sa d qy

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15@ 9@ 2013 d h

fLFkfr e sa

x r o "kZ l so "kkZ

e sa d e h ; k o ‘f)

1 c y kSn k c kt kj 970-20 592-4 849-8 257-4 Growth2 fl e x k 1057-70 893-7 1152-2 258-5 Growth3 HkkVki kj k 969-10 953-0 887-0 66-0 Loss

mailto:15@9mailto:@2013

32

4 c y kSn k

c kt kj

i y kj h 880-80 957-8 930-8 27-0 Loss

5 d l Mksy 1115-50 958-0 1129-2 171-2

Growth6 fc y kb Zx < + 1086-00 1227-0 1040-0 187-0 Loss

v kSl r ft y k 1013-21 930-32 998-17 67-9 Growth

34

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

35

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.

38

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 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 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.

39

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 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 1

बससंचालतहो ती है ।इसके अला वा रा यपु र-झारसुगडाहा या बलौ दा बा जा ररे लमागको

12वीयोजनामशा मलकयागयाह ै ।

LOCATION AND VILLAGES MAP - BALODABAZAR

41

कृषवसं चाइ :-बलौदाबाजारिजलेकछ : तहसीलकेअं तगतकृषकाकु लरकबा 269888

970 गांवक 10

: 86

4 ,

, नालेसथतह ै ,

, शवना थ ,

1935-36 मलगभग 200 क .मी.

,

42

वन :-875.27 -

,

जहांपयटनवभा गवा रा

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

GEOTECHN

ICAL & NATURAL HAZARDS

district survey report of balodabazar -...

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