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District Survey Report

Raipur AS PER NOTIFICATION NO. S.O. 141(E) NEW

DELHI, 15TH JANUARY, 2016 OF MINISTRY OF

ENVIRONMENT, FOREST AND CLIMATE

CHANGE

2016

DGM

Hewlett-Packard

01/01/2016

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 COMMUNICATION MAP OF THE RAIPUR 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 alongwith 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.

Raipur was named after King Brahmdeo Rai of Haihaya dynasty which

reined this part of state in the 15th centuray. Raipur was declred capital in 1818 by

British superitendent and almost total area of the exixting state was administered

centrally from here. The "RAIPUR" town has been in existence since the ninth

century, old site and ruins of the fort can be seen in the southern part of city.The

old inscriptions of Ratanpur, Rajim and Khallari refer to the reign of Kalchuri

kings. During the Maratha Rule from 1750 to 1815, Raipur was reduced to a

Pargana head Quarter. The territory was assumed by the British Government from

Bhonsla's of Nagpur and Chhattisgrh was declared a separate commisionary with

its head quarter at Raipur in 1854.

Raipur Distrct forms part of the Raipur Commissionary in the Chhattisgarh

Region and occupies the south eastern part of the upper Mahanadi basin, the

District is situated between the East longitudes 81°32’05” & 82°59’05” and by

North latitudes 19°46’35” & 21°53’00” and is covered by the survey of India

toposheets, either fully of partly by 64 G, H, K, and 65/O. The Land locked district

surrounded by Bilaspur and Baloda Bazar, in North Dhamtari district in south,

Mahasamundand Gariyaband in east and Durg in west.The shape of the district is

fairly compact and composed of 4 Tehsil and Blocks i.e. Dharsiwa, Arang,

Tildaand, Abhanpur.

The district head quarter RAIPUR is capital of Chhattisgarh. The Raipur city is

alsothe divisional Head Quarter or Raipur (Commissionar) including fourdistrict

namely Mahasamund, Balodabazar, Gariyaband and Dhamtari. The total area of

4

the district is 12,383 Sq. Km. As per official census 2011,Raipur is the most

populous district in the state with population of 40,63,872 of which male and

female were 20,48,186 and 20,15,686 respectively. The Mahanadi is the main

river which forms eastern boundary of the district. The western boundary district

runs along the kharun river which flows towards north joining the Shivnath about

8 Km. south west of Simga. A large number of small streams flow through the low

lying areas which are diverted to join the Mahanadi in the east.

The district is well connected with other cities of the State and country

through thenational highways NH, 30& NH53. Alsothere is a good network of

state highway.

Raipur is situated on the Bombay- Howrah broad-gauge of SECR Raipur- Bilaspur

Section. Air connectivity is furnished by Swami Vivekanand national airport of

Naya Raipur.

6

INDEX MAP OF RAIPUR DISTRICT

7

2. OVERVIEW OF MINING ACTIVITY OF DISTRICT

Raipur district is famous for its various grades of Limestone deposit viz high grade,

(cement grade) blendable/Beneficial grade, Low grade etc.

Minor mineral (Low grade limestone) Dolomite, Laterite, Sandstone, River sand

are also found in huge quantity in Tilda, Kesla, Mohrenga, Kathiya, Patharakundi,

number of Mining Lease have been sanctioned for cement grade limestone. CCI

Mandhar (abondoned), Century cement (Baikunth), Gangotri Limes (Dondekala), ORS

Minerals (Matiya) are main limestone based industry in the district.

137 Nos. of Quarry leases for limestone have sanctioned for road and building material,

16 otherof clay and flag stone for making bricks and tiles locally. The major limestone

belts of the district are:-

(1) Bangoli - Kharora - Mohrenga

(2) Murra-Dhansuli

(3) Pirda-Bahnakadhi

(4) Dondekala-Dondekhurd-Lalpur-Matiya

(5) Madhi-Khapri-Sontara.

Overall mining activity in the district are running in fullswing in term of

limestone as minor mineral (building and road material), 46 Leases sand mining in bank

of Mahanadi river at different villages and material like murrum ordinary stones are also

permitted for quarrying of material at number of places.

Picture showing mining of Limestone in Raipur District

8

General Information of Raipur District

Sub-

division

No. of

Tahsils

No. of

Blocks

No of

Gram

Panchayat

No. of Villages Population

as per 2011

%

Literacy Habited Inhabited

1 2 3 4 5 6 7 8

2 4 4 408 541 4 21,60,876 80.52

Block wise Statistical Profile (as per Census 2011)

Block Area (Sq.km.) Villages Gram Panchayat

Dharsiwa 652.31 84 78

Arang 900.39 168 104

Tilda 735.3 135 99

Abhanpur 603.98 104 91

Total 2891.98 491 408

District Population & Literacy in 2011

Total

Population

Male Female Rural Urban %

Literacy

21,60,876 11,00,861 10,60,015 8,84,224 12,76,652 80.52

9

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

period of validity

jk;iqj ftyk esa Lohd`r fo|eku [kfuiV~Vksa dh lwph ¼i½ ftys esa [kfuiV~Vks dh lwph %&

dza- [kfuiV~Vs/kkfj;ksa dk uke o irk [kfut dk uke

Lohd`r {ks= gsDVj esa

fLFkfr xzke o rglhy vof/k dk;Z’khy@f’kfFky

1 2 3 4 5 6 7 1 esllZ lsUpqjh VsDlVkbZYl bafM;k fyfe- cSdq.B pwukiRFkj 237-003 cgslj] V.Mok] rglhy

frYnk 04-8-99 ls 3-8-2029

dk;Z’khy

2 esllZ lsUpqjh VsDlVkbZYl ,.M lhesaV cSdq.B frYnk

pwukiRFkj 74-843 cgslj] rqylh] rglhy frYnk

30-9-02 ls 29-9-2032

dk;Z’khy

3 Jh vo/ks’k tSu firk Jh txnh’k tSu fu- lRrhcktkj jk;iqj ftyk jk;iqj

pwukiRFkj 7-044 iFkjkdqaMh rglhy frYnk 2-5-2008 ls 1-5-2028

dk;Z’khy

4 Jh HkwisUnz lkgw vk- Jh dqarjke lkgw fuoklh fljhZdyk

pwukiRFkj 2-933 efV;k rglhy jk;iqj 26-4-1999 ls 25-4-2019

dk;Z’khy

5 Jh vf[kys’k dqekj fuoklh eafnjglkSn pwukiRFkj 4-479 ykyiqj rglhy jk;iqj 26-7-1999 ls 25-7-2019

dk;Z’khy

6 Jh ;ksxsUnz oekZ vk- Lo- ds-,y-oekZ fuoklh [kjksjk ftyk jk;iqj

pwukiRFkj 4-527 eksgjsaxk] [kkSyhMcjh rglhy frYnk

19-11-2007 ls 18-11-2037

dk;Z’khy

7 Jh dsnkj vxzoky fuoklh [kjksjk pwukiRFkj 9-716 iFkjkdq.Mh rglhy frYnk 17-11-2000 ls 16-11-2020

dk;Z’khy

8 Jh v’kksd ljhu tsy jksM jk;iqj pwukiRFkj 10-121 e

10

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

jk;iqj ftyk dh v|ru fLFkfr esa fo|eku Lohd`r mR[kfuiV~Vksa dh lwph

¼v½ feV~Vh ¼Brick earth½

Øa iV~Vsnkj dk uke iw.kZ irs lfgr

[kfut Lohd`r vkns’k Øekad ,oa

fnukad

fu"iknu fnukad

dkykof/k xzke iapk;r

,oa rglhy

[kljk uEcj {ks=Qy

¼gsDVj esa½

1 2 3 4 5 6 7 8 9 1 Jh dkS’ky dqekj

xaxokuh fuoklh QkQkMhg jk;iqj

feV~Vh 61@2011@ 25-05-2011

21-07-2011 21-7-2011 ls 20-7-2016

ljksuk@jk;iqj

79@1] 113] 114] 115

6-80 ,dM+

2 Jherh lksuknsoh bZ’kjkuh fuoklh yk[ks uxj jk;iqj

feV~Vh 104@2007@ 11-04-2008

22-07-2008 22-07-08 ls 21-07-2018

ljksuk@jk;iqj

401] 402 5-00 ,dM+

3 Jh vfuy dqekj xkojh fuoklh yk[ks uxj jk;iqj

feV~Vh 9@2011@ 03-10-2011

26-01-2012 26-1-2012 ls 25-1-2017

ljksuk@jk;iqj

11 Vq-] 12 Vq- 4-40 ,dM+

4 Jh larks"k bZ’kjkuh fuoklh yk[ks uxj jk;iqj

feV~Vh 183@2007@ 22-12-2008

03-01-2009 3-1-2009 ls 2-1-2019

ljksuk@jk;iqj

6@2] 14@1 7-20 ,dM+

5 Jh v’kksd dqekj vkgwtk vk- Jh fd’kupan fu- ueZnkikjk jk;iqj

feV~Vh 204@2008@ 12-08-2009

06-11-2009 6-11-2009 ls 5-11-2019

dqEgkjh@jk;iqj

105] 109] 1]2

9-80 ,dM+

6 Jh fd’kupan vkgwtk vk- Jh is’kqey fu- ueZnkikjk jk;iqj

feV~Vh 118@2011@ 22-11-2012

24-12-2012 24-12-2012 ls 23-12-2017

dqEgkjh@jk;iqj

2@1] 3@1]4]5

3-74 ,dM+

7 Jh gjh’k 'kqDyk] vk- Lo- Jh :nzukjk;.k 'kqDyk] fu-& jksg.khiqje jk;iqj]

feV~Vh 17@2014 16-01-2014

01-08-2014 01-08-2014 ls 31-07-2019

dqEgkjh 138@1] 139@1

0-566 gs-

8 esllZ ckykth fczDl Ogh-ls- eqjyh/kj fuoklh VkVhca/k jk;iqj

feV~Vh 34@2010@ 22-03-2011

19-03-2011 19-03-2011ls 18-03-2021

cgslj@jk;iqj

91] 92] 93 94@1&2] 95@1]2]3]4

3-850 gsDVj

9 Jh lqjs’k ykyokuh vk- Jh d`ikynkl fu- Jhuxj jk;iqj

feV~Vh 72@2014@ 06-08-2004

08-08-2014 08-08-2014ls 07-08-2024

cgslj@jk;iqj

69@2] 69@3

2-267 gsDVj

10 t; Jh fczDl izks- Ogh- ls- eqnfy;kj fuoklh VkVhca/k

feV~Vh 101@2006@ 04-09-2006

14-09-2006 14-9-2006 ls 13-9-2016

cgslj@jk;iqj

61@1]2]3] 63@1]2] 64@2] 65

1-276 gsDVj

11 Jherh vesjk efyd fuoklh jk;iqj

feV~Vh 70@2007@ 25-06-2007

07-08-2007 7-8-2007 ls 6-8-2017

gjnh@ vkjax

165 3-95 ,

12 Jh x.ks’k dqEgkj firk Jh >kM+w lkgw fuoklh lklkgksyh frYnk

feVVh 127@06@ 29-09-2006

10-10-2006 10-10-2006 ls 9-10-2016

lklkoyh@frYnk

20 2-023 gs-

13 Jh nhuca/kq lkgw vk- Jh fNUNkjke lkgw

feV~Vh 238@09@ 07-01-2011

24-12-2010 24-12-2010ls 23-12-2020

yedsuh@vHkuiq

114 1-336 gs-

11

fuoklh

12

10-2017 8 Jh nsoth HkkbZ iVsy

firk /kuth HkkbZ iVsy fu- QkQkMhg jk;iqj

pwukiRFkj 164@2007@ 26-06-2008

04-09-2008 4-9-2008 ls 3-9-2018

/kulwyh@frYnk

403 1-508 gsDVj

9 es- egkek;k LVksu Mk;jsDVj Jh v’kksd vxzoky

pwukiRFkj 227@2008@ 13-01-2009

21-01-2009 21-1-2009 ls 20-1-2019

/kulwyh@frYnk

428@2 1-133

10 Jh Hkwus’oj ;kno fi- Jh txnso fu- /kulwyh frYnk jk;iqj

pwukiRFkj 39@11 28-09-2011

12-10-2011 12-10-2011ls 11-10-2021

/kulwyh@frYnk

475@1]2 488@1]2

1-172 gs-

11 lkabZ feujy izks- vfurk fl/kkfu;k

pwukiRFkj 78@2008@ 02-04-2008

19-09-2008 19-09-2008ls 18-09-2018

ewjk@frYnk

632] 633@1]2]3

3-86 ,

12 dkydk dLVªD’ku izks- 'ks[kukfteqn~nhu fuoklh jk;iqj

pwukiRFkj 26@2011@ 03-03-2012

04-03-2012 4-3-2012 ls 3-3-2017

ewjk@frYnk

628@3 2-00 ,dM+

13 Jh dsnkj vxzoky fuoklh [kjksjk rglhy frYnk

pwukiRFkj 266@2009@ 06-12-2010

03-12-2010 3-12-2010 ls 2-12-2020

ewjk@frYnk

634 Vq 1-25 ,dM+

14 Jh vrqy feJk fuoklh dksVk] jk;iqj

pwukiRFkj 03@2012@ 20-04-2012

02-05-2012 2-05-2012 ls 01-05-2022

ewjk@frYnk

594] 598] 599

0-296 gs-

15 Jherh Lo.kZyrk feJk ifr Jh larks"k feJk]fu-ewjk rg- frYnk

pwukiRFkj 87@2006@ 25-08-2006

10-10-2006 10-10-2006 ls 9-10-2016

ewjk@frYnk

623 0-506 gsDVj

16 nsodh uanu LVksu izk-fy- izks- Jh eukst vxzoky

pwukiRFkj 158@2011@ 12-04-2012

16-12-2012 16-12-2012 ls 15-12-2017

ewjk@frYnk

624] 625] 626

3-56 ,dM+

17 Jh;k feujYl ikVZuj eqls’k vxzoky vk-Jh xksihjke fu- LVs’ku jksM jk;iqj

pwukiRFkj 169@2006@ 16-08-2007

23-08-2007 23-8-2007 ls 22-8-2017

ewjk@frYnk

756@16] 18]802@2

2-412 gs-

18 Jh ewy th HkkbZ iVsy fuoklh o rglhy jk;iqj

pwukiRFkj 152@2006@ 05-10-2007

28-12-2007 28-12-2007 ls 27-12-2017

ewjk@frYnk

582@2] 583] 584

0-405 gsDVj

19 Jh gjfoanj flag vk- Jh xq:Hkst flag fuoklh [kjksjk rglhy frYnk

pwukiRFkj 94@2006@ 07-02-2007

29-06-2007 29-6-2007 ls 28-6-2017

ewjk@frYnk

821@2 0-728 gs-

20 es-thuekrk feujYl izks- foosd vxzoky firk Jh fot; vxzoky ftyk jk;iqj

pwukiRFkj 157@2008@ 13-01-2009

21-01-2009 21-1-2009 ls 20-1-2019

ewjk@frYnk

658@1]2]3]4]5]6]7

0-751 gs-

21 es-,e-,l- dLVªD'ku izks fgeka'kq dkSf'kd firk Jh jktsUnz oekZ fu- 'kkafr uxj jk;iqj

pwukiRFkj 156@2008@ 23-01-2009

06-04-2009 6-4-2009 ls 5-4-2019

ewjk@frYnk

807@2]5]7 0-558 gs-

22 Jh lkSjHk feJk vk- Jh fo'oukFk fu- ewjk rglhy frYnk ftyk jk;iqj

pwukiRFkj 06@2009@ 19-01-2009

21-07-2009 21-7-2009 ls 20-7-2019

ewjk@frYnk

606 0-666 gs-

13

23 esllZ egkek;k

feujYl Hkkxhnkj Jh iq:"kksRre vxzoky¼yht VªkalQj iwoZ uke Jh Hkjr iVsy½

pwukiRFkj 224@2007@ 08-01-2008

16-01-2008 16-01-2008 ls 15-1-2018

ewjk@frYnk

662@5]6 1-14 ,dM+

24 es- fo'o Hkkjrh feujYl ikVZuj uohu vxzoky vk- Jh lqjs'k dqekj vxzoky fuoklh jk;iqj

pwukiRFkj 225@2009@ 18-11-2009

24-11-2009 24-11-2009 ls 23-11-2019

ewjk@frYnk

468@1] 487@2] 492@2]

493@1] 499] 467@4] 491@4]6]

489

2-390 gs-

25 Jherh jktJh oekZ ifr Jh egs’k dqekj oekZ fu- rqylh iks- frYnk rglhy frYnk ftyk jk;iqj

pwukiRFkj 140@2010@ 10-01-2011

22-01-2011 22-01-2011 ls 21-01-2021

ewjk@frYnk

567@1] 568@1]2]3] 569@1] 569@3]

569@4] 570] 573

0-730 gs-

26 Jh lnkf’ko oekZ vk- Jh vf/kj oekZ fuoklh ewjk frYnk jk;iqj

pwukiRFkj 39@2012@ 04-12-2012

08-02-2013 08-02-2013ls 07-02-2018

ewjk@frYnk

822 0-722 gsDVj

27 Jh fot; vxzoky] vk- Lo- Jh 'kadj yky vxzoky fuoklh &eksok jk;iqj

pwukiRFkj 28-08-2014 23-08-2014 23-08-2014ls 22-08-2024

ewjk@frYnk

595] 596] 597]

604@1

0-900 gs-

28 Jh cyoku pgsfj;k] vk- Jh vksadkjey pgsfj;k] fuoklh & voafr fogkj] jk;iqj

pwukiRFkj 78@2014@ 05-03-2015

10-03-2015 10-03-2015 ls 09-03-2020

ewjk@frYnk

610 0-809 gsDVj

29 Jh 'kjn xks;y vk-Lo- Jh jes’k xks;y fuoklh&[kjksjk rglhy frYnk] jk;iqj

pwukiRFkj 79@2014@ 12-12-2014

02-01-2015 02-01-2015 ls 01-01-2020

ewjk@frYnk

608 1-60 ,dM+

30 esllZ ekW egk y{eh LVksu Ø’kj izks- Jh r:.k vxzoky

pwukiRFkj 34@2013@ 15-01-2014

22-01-2014 22-01-2014 ls 21-01-2024

ewjk@frYnk

664@11]13]2]3]12]4]6]8]10]1]5]

7]9] 665@3]6]

659

2-500 gs

31 Jh fuys’k vxzoky fi- Jh cyHknz fu- [kjksjk frYnk jk;iqj

pwukiRFkj 16-03-2011 23-03-2011 23-03-2011 ls 22-03-2021

cqMsjk@frYnk

419@1 1-06 ,dM+

32 eks- dkfle vk- Lo Jh tyhy vgen fuoklh cq

14

ch&19 jfouxj jk;iqj 35 Jh nsosUnz dqekj vk-

Jh 'kadj yky vxzoky fuoklh cSdq.B frYnk

pwukiRFkj 183@2006@ 13-11-2007

22-11-2007 22-11-2007 ls 21-11-2017

fcykM+h@frYnk

15] 16 1-214 gs-

36 Jh Lkfgy flag firk Jh v’kksd flag fuoklh ,e-vkbZ-th 'kadj uxj jk;iqj

pwukiRFkj 144@2008@ 26-09-2008

08-10-2008 8-10-2008 ls 7-10-2018

vksVxu@frYnk

578@1 1-800 gs-

37 Jh rkjkpan vkgwtk] vk- Jh fd’kupan vkgwtk] fu-&QkQkMhg xyh ua-&1 jk;iqj

pwukiRFkj 19-08-2014 27-08-2014 27-08-2014 ls 26-08-2019

udVh [kijh@frYnk

290@15] 290@16

4-60 ,dM+

38 Jh vkyksd 'kekZ fuoklh fly;kjh jk;iqj

pwukiRFkj 42@2013@ 29-01-2014

18-02-2014 18-02-2014 ls 17-02-2024

udVh [kijh@frYnk

290@18 1-00 ,-

39 Jherh vfurk tSu vk- Jh Jh;ka’k tSu fu0uokikjk@ jkfte ftyk jk;iqj

pwukiRFkj 68@2011@ 28-04-2012

19-12-2012 19-12-2012 ls 18-12-2022

nqyuk@vHkuiqj

432@3] 433@2

2-092 ,dM+

40 Jh vfer tSu vk- Jh dSyk’k tSu fuoklh uokikjk@jkfte ftyk jk;iqj

pwukiRFkj 231@2008@ 03-05-2008

28-11-2009 28-11-2009 ls 27-11-2019

nqyuk@vHkuiqj

688] 687@2]

0-76 ,-

41 Jh nmokjke lkgw fuoklh nqyuk

pwukiRFkj 12@2012@ 25-07-2012

22-09-2012 22-09-2012 ls 21-9-2022

nqyuk@vHkuiqj

433@1] 1-40 ,-

42 Jh nmokjke lkgw fuoklh nqyuk

pwukiRFkj 05@2011@ 25-01-2011

14-02-2011 14-02-2011 ls 13-2-2021

nqyuk@vHkuiqj

433@1] 590] 591

0-750

43 Jh gfjeksgu lkgw fuoklh

pwukiRFkj 62@2005@ 29-03-2006

20-09-2010 20-09-2010 ls 19-9-2020

nqyuk@vHkuiqj

686 2-22 gs

44 Jh x.ks’k izlkn [ksrku fuoklh ekgnkikjk jk;iqj

pwukiRFkj 93@2011@ 09-04-2012

08-05-2012 08-05-2012 ls 7-5-2022

csUnzh@vHkuiqj

100@3] 100@4

2-22 ,-

45 Jh vfuy dqekj vBokuh yk[ksuxj jk;iqj

pwukiRFkj 230@06@ 18-04-2007

28-05-2007 28-5-2007ls 27-5-2017

fijnk@jk;iqj

640 1-56 ,dM+

46 Jh iadt panzkdj fuoklh Vsejh jk;iqj

pwukiRFkj 10@2011@ 11-08-2011

01-05-2012 01-5-2012 ls 30-4-2022

udVh@jk;iqj

457@1] 458@2

1-79 ,dM+

47 Jh tktZ jktu fuoklh jk;iqj

pwukiRFkj 247@2009 25-01-2011

25-01-2012 25-1-2012ls 24-01-2022

lsjh[ksM+h@jk;iqj

689@1ls 3] 691

3-54 ,dM+

48 fpadkjk feujYl Hkkxhnkj Jh ftrsUnz iVsfj;k fuoklh jk;iqj

pwukiRFkj 217@2006@ 16-04-2007

03-05-2007 3-5-2007 ls 2-5-2017

lsjh[ksM+h@jk;iqj

690@3 0-809 gsDVj

49 Jherh izfrek iqtkjh pwukiRFkj 177@2005@ 03-01-2007 3-1-2007 ls Vsejh@jk 406 3-60

15

fuoklh lnjcktkj jk;iqj

31-10-2006 2-1-2017 ;iqj ,dM+

50 Jherh iq"ik csu iVsy fu-& U;w fVEcj ekdsZV jk;iqj

pwukiRFkj 14@2010@ 08-10-2010

14-10-2010 14-10-2010ls 13-10-2020

nkSansdyk@jk;iqj

463@1 0-840 gs-

51 Jh fgrs’k ukxokuh fuoklh nsosUnz uxj jk;iqj

pwukiRFkj 153@2009@ 13-07-2010

27-07-2010 27-7-2010 ls 26-7-2020

nkSansdyk@jk;iqj

482] 483]484]43

9

2-00 ,dM+

52 NRrhlxka>jh fuoklh nsosUnz uxj jk;iqj

pwukiRFkj 127@2007@ 05-07-2008

12-08-2008 12-8-2008 ls 11-8-2018

ujngk@vkjax

1967 2-60

57 d`".k dqekj lkgw vk- Jh eulkjke lkgw fuoklh lsyk’kiqjh jk;iqj

pwukiRFkj 65@2010@ 27-07-2010

13-08-2010 13-8-2010 ls 12-8-2020

ujngk@vkjax

1945 1-200 gs-

58 Jh banjdqekj ukxnso vk- tsmjke fu- tsyjksM jk;iqj

pwukiRFkj 04@2010@ 28-01-2011

02-02-2011 2-2-2011 ls 1-2-2021

ujngk@vkjax

1948 4-90 ,

59 Jh gjhyky iVsy vk- dkathHkkbZ iVsy fuoklh Hkuiqjh jk;iqj

pwukiRFkj 175@2006@ 08-12-2006

28-12-2006 28-12-06 ls 27-12-2016

ujngk@vkjax

1964 1-214

60 Jh izoh.k dqekj iVsy vk- Jh n;kHkkbZ nsosUnz uxj jk;iqj

pwukiRFkj 14@2007@ 01-03-2007

12-03-2007 12-3-07 ls 11-3-2017

ujngk@vkjax

1953@1] 1954@1

1-280

61 Jh fuf[ky frokjh gfjgj feujy] jk;iqj

pwukiRFkj 32@2006@ 01-08-2006

25-07-2006 25-7-06 ls 24-7-2016

ujngk@vkjax

1955@2] 1956] 1957

1-772 gs

62 Jh ;ksxs’k vxzoky vk- Jh jkeorkj vxzoky fuoklh eafnjglkSn rglhy vkjax

pwukiRFkj 4@2007@ 20-12-2007

03-01-2008 3-1-08 ls 2-1-2018

ujngk@vkjax

1426 1-896 gs

63 ts- ts- ,lksfl,VsV izks- Jh /kesZUnz jke iqjh;k fuoklh & ykyiqj jk;iqj

pwukiRFkj 105@2011@ 11-05-2012

25-09-2012 25-9-2012 ls 24-9-2022

ujngk@vkjax

1960 2-40 ,dM+

64 'kadj b.MLVªht jkts’k iVsy fuoklh QkQkMhg] jk;iqj

pwukiRFkj 112@07@ 07-08-2007

17-08-2007 17-8-2007 ls 16-8-2017

ujngk@vkjax

1951] 1952@2] 1953@2] 1954@3

1-991 gsDVj

65 Jh dqychj flag vk- pwukiRFkj 10@2008@ 17-03-2008 17-3-2008 ujngk@ 2001@1]2] 0-769

16

Jh jke Lusgh tkV fuoklh dVksjk rkykc jk;iqj

06-03-2008 ls 16-3-2018

vkjax 3 gsDVj

66 Jh izdk'k ctkt vk- Jh e?kuey fu- QkQkMhg jk;iqj

pwukiRFkj 98@2011@ 20-05-2014

02-05-2003 02-5-2013 ls 01-5-2023

ujngk@vkjax

1972] 1980 1982

Vq

2-744 gs

67 Jherh ehuk nsoh ctkt] ifr Jh pqUuhyky ctkt] fuoklh & QkQkMhg jk;iqj

pwukiRFkj 07@2013@ 27-02-2015

08-03-2014 08-03-2014 ls 07-03-2024

ujngk@vkjax

1962 3-50 ,dM+

68 Jh v’kksd ctkt] vk- Jh eaxwey ctkt] fuoklh %& QkQkMhg jk;iqj

pwukiRFkj 89@2011@ 27-02-2015

07-01-2013 07-01-2013 ls 06-01-2023

ujngk@vkjax

1993@1] 2] 3

4-92 ,dM+

69 Jh v’kksd ctkt] vk- Jh eaxwey ctkt] fuoklh %& QkQkMhg jk;iqj

pwukiRFkj 26@2013@ 19-02-2014

06-07-2014 06-07-2014 ls 05-07-2024

ujngk@vkjax

1987] 1989] 1990] 1991] 1992]

1993@3] 1995@1

1-888 gs-

70 esllZ ,l-,l- LVksu ekbZu izks- Jh v{k; dqekj JhokLro

pwukiRFkj 21-01-2014 22-01-2014 22-01-2014 ls 21-01-2024

ujngk@vkjax

2002@2 3-34 ,-

71 Jh t; dqekj ctkt vk- Jh eaxwey fu- QkQkMhg jk;iqj

pwukiRFkj 106@2006@ 29-03-2007

08-12-2007 08-12-2007 ls 7-12-2017

eafnjglkSn@vkjax

862@2]4]863] 864] 865]

866@1] 866@3] 868@1]2]

869

2-442 gs-

72 Jherh Hkxorh nsoh fizrokuh ifr Lo Jh vtqZu dqekj fizrokkuh fuoklhvktkn pkSd Fkkuk ls ikl jk;iqj

pwukiRFkj 233@2006@ 29-05-07

06-01-2008 6-1-2008 ls 5-1-2018

eafnjglkSn@vkjax

876@1]2 876@18]

879

4-60 ,-

73 Jherh yhyk csu iVsy ifr Lo- fot; iVsy fuoklh QkQkMhg jk;iqj

pwukiRFkj 38@2012@ 26-10-2012

12-11-2012 12-11-2012 ls 11-11-2022

eafnjglkSn@vkjax

553@1] 653@3

3-36 ,

74 Jh usoUnjke NkcfM+;k vk- yksdwey fuoklh yk[ksuxj jk;iqj

pwukiRFkj 08@2011@ 31-03-2011

07-02-2012 7-2-2012 ls 6-2-2022

eafnjglkSn@vkjax

709@3 3-50 ,

75 Jherh fuf/k ikaMs ifr Jh th-,y- ikaMs fuoklh lqanj uxj jk;iqj

pwukiRFkj 51@2011@ 30-08-2012

01-08-2012 01-9-2012 ls 31-08-2017

eafnjglkSn@vkjax

709@1]5] 711@4]5

4-85 ,

76 Jh panzgkl ikaMs fuoklh& jk;iqj

pwukiRFkj 52@2011@ 18-02-2014

26-02-2014 28-07-2012ls 27-07-2022

eafnjglkSn@vkjax

721@1] 721@2] 722] 749

1-94 ,dM+

17

77 Jherh Hkkouk csu iVsy ifr Jh lat; fu-&QkQkMhg jk;iqj

pwukiRFkj 62@2011@ 08-06-2011

06-06-2012 6-6-2012 ls 5-6-2022

eafnjglkSn@vkjax

678] 689 2-019 gs

78 Jh dY;k.k falg vk- Lo- Jh ,y-ch- flax fu- Jh is’kuckMh jk;iqj

pwukiRFkj 125@2011@ 12-07-2012

20-07-2012 20-07-2012ls 19-07-2017

eafnjglkSn@vkjax

714 1-54 ,-

79 Jherh laxhrk vxzoky ifr Jh dSyk’k vxzokyfuoklh vuqie uxj jk;iqj

pwukiRFkj 104@2011@ 26-06-2012

01-10-2012 1-10-2012 ls 30-09-2022

eafnjglkSn@vkjax

654] @1]2 657@1]4

4-14 ,

80 ljkst LVksu dzs’kj Hkkxhnkj vkuan fla?kkfu;k fu- nsosUnzuxj jk;iqj

pwukiRFkj 204@2007@ 21-07-2008

01-08-2008 01-08-2008 ls 31-07-2018

eafnjglkSn@vkjax

657@2]4]6]13

1-214 gsDVj

81 esllZ lh-th- ,xzks QkeZ Hkkxhnkj Jh fofiu vxzoky vk- Jh ds-lh- vxzoky fuoklh & vuqie uxj jk;iqj

pwukiRFkj 48@2014@ 15-09-2014

24-09-2014 24-09-2014 ls 23-09-2024

eafnjglkSn@vkjax

726@1] 726@2] 741] 742]

744

2-010 gsDVj

82 lksyj jkDl ikVZuj Jh vuqHko elhg vk- Jh izeksn elhg fu & iap’khy uxj jk;iqj

pwukiRFkj 17A@2013@ 09-01-2014

10-01-2014 10-01-2014 ls 09-01-2024

eafnjglkSn@vkjax

661] 666] 667]

668@1] 668@2

1-943 gsDVj

83 Jh vxzlsu [kfut m|ksx izks fnus’k xks;y vk- Jh izgykn fu-eafnjglkSn

pwukiRFkj 276@2009@ 13-01-2011

14-01-2011 14-1-2011 ls 13-1-2021

ckgukdkM+h@vkja

x

16 4-14 ,

84 Jh jkeorkj vxzoky vk- Jh fujatu vxzoky fuoklh eafnjglkSn vkjax

pwukiRFkj 174@ 28-11-2006

03-01-2007 3-1-2007 ls 2-1-2017

ckgukdkM+h@vkja

x

22 1-16

85 xks;y daLVªD’ku ikV- Jh jkevorkj vxzoky fu- fo’kky uxj jk;iqj

pwukiRFkj 24@2010@ 17-02-2011

25-02-2011 25-2-2011 ls 24-2-2021

ckgukdkM+h@vkja

x

494 4-16 ,

86 Jhfuokl LVksu Øsflax izks lqHkk"k vBokkuh vk Jh xq:eq[knkl fu- QkQkMhg

pwukiRFkj 145@2011@ 09-10-2012

20-10-2012 20-10-2012 ls 19-10-2022

ckgukdkM+h@vkja

x

28 2-70 ,

87 y{eh LVksu izks jkts’k tknokuh vk- Jh ujs’k fuoklh nsosUnz uxj jk;iqj

pwukiRFkj 147@2011@ 30-10-2012

18-11-2012 18-11-2012ls 17-11-2022

ckgukdkM+h@vkja

x

33] 34 1-132 gs

88 Jh euh"k vxzoky firk Lo- Jh lsyk’kpanz 6 fuoklh vuqie uxj jk;iqj

pwukiRFkj 100@2007@ 12-12-2007

02-01-2008 2-1-08 ls 1-1-2018

ckgukdkM+h@vkja

x

467] 469] 473]477@

1

1-844 gs

89 Jh fot; tknokuh vk- Lo- iksiVey tknokuh fuoklh Mh@192 nsosanz uxj

pwukiRFkj 152@2007@ 26-12-2007

26-04-2008 26-4-08 ls 25-4-2018

ckgukdkM+h@vkja

x

31]32@1] 46@2

2-387 gs

18

jk;iqj 90 Jherh ijohu csxe

ifr eksgEen vkfjQ fuoklh NksVkikjk jk;iqj

pwukiRFkj 139@2009@ 16-11-2009

06-02-2010 6-02-2010 ls 5-02-2020

ckgukdkM+h@ vkjax

498] 499] 500] 502]

503

1-400

91 Jh fouksn dqekj oekZ

pwukiRFkj 08-01-2007 08-01-2007ls 07-01-2017

ckgukdkM+h@vkja

x

12 0-300 gsDVj

92 jkds’k nwcs vk- Jh jkeizlkn nqcs fuoklh ’kadj uxj jk;iqj

pwukiRFkj 10-04-2013 10-04-2013 ls 09-04-2023

ckgukdkM+h@vkja

x

497@1 1-967 gsDVsj

93 Jh egkohj m|ksx izks izdk’k vMokuh vk- Jh eksVwey vMokuh fu- foosdkuan vkJe

pwukiRFkj 28-03-2013 28-03-2013 ls 27-03-2023

ckgukdkM+h@vkja

x

29]30 3-468 gsDVsj

94 esllZ /kulqyh ykbZe LVksu ekbZu izks- Jh vehj vyh

pwukiRFkj 73@2013@ 20-01-2014

17-02-2014 17-02-2014ls 16-02-2024

/kulwyh@vkjax

715] 718] 741] 721] 699@2] 714@2]3]

717] 719]720] 722

3-030 gs-

95 uohu iVsy vk- HkkuqHkkbZ iVsy fuoklh bafnjk fVEcj eklsaV Hkuiqjh jk;iqj

pwukiRFkj 203@2008@ 13-02-2009

02-03-2009 2-3-2009 ls 1-3-2019

/kulwyh@vkjax

919@2] 921@2

2-104

96 Jh jkts'k ijekj vk- Jh ycth HkkbZ ijekj fuoklh nsosUnz uxj jk;iqj

pwukiRFkj 20-02-2012 20-2-2012 ls 19-2-2022

/kulwyh@vkjax

928 2-20 ,

97 Jh fot; dqekj fizrokuh vk- Jhpan fizrokuh fu-&QkQkMhg jk;iqj

pwukiRFkj 131@2006@ 05-10-2007

09-10-2007 9-10-07 ls 8-10-2017

/kulwyh@vkjax

870 1-72

98 Jh oklwnso fizrokuh vk- Jh vVBwey fizrokuhfuoklh QkQkMhg jk;iqj

pwukiRFkj 172@2006@ 02-11-2007

17-11-2007 17-11-07 ls 16-11-2017

/kulwyh@vkjax

916 1-473 gs-

99 Jh fot; HkkbZ iVsy vk Jh ikyth HkkbZ iVsy fuoklh QkQkMhg jk;iqj

pwukiRFkj 28@2010 03-10-2010

03-10-2011 3-10-2011 ls 2-10-2021

/kulwyh@vkjax

677 3-00 ,

100 Jh deys'k vBokuh vk- Jh xq:eq[k vBokuhfuoklh yk[ks uxj jk;iqj

pwukiRFkj 161@2011 05-11-2012

30-11-2012 30-11-2012ls 29-11-2022

/kulwyh@vkjax

576] 653 8-00 ,

101 Jh dSyk'k cM+okuh vk- Jh thou yky cM+okuhfuoklh QkQkMhg jk;iqj

pwukiRFkj 148@2011 25-10-2012

30-10-2012 30-10-2012ls 29-10-2022

/kulwyh@vkjax

897 3-34 ,

102 Jh f=iriky flag vk - Jh gjHktu flag

pwukiRFkj 58@2012@ 12-11-2012

30-11-2012 30-11-2012ls 29-

/kulwyh@vkjax

883 2-56 ,

19

fuoklh QkQkMhg jk;iqj

11-2017

103 Jherh lrhUnj dkSj ifr Jh euizhr falg vjksjkfuoklh ';ke uxj jk;iqj

pwukiRFkj 117@2011 25-07-2012

29-11-2012 29-11-2012ls 28-11-2022

/kulwyh@vkjax

703 2-40 ,

104 Jh xksfoUn HkkbZ iVsy vk- Jh ckyth HkkbZ iVsyfuoklh Hkuiqjh jk;iqj

pwukiRFkj 21@2006 21-01-2007

03-02-2007 3-2-2007 ls 2-2-2017

/kulwyh@vkjax

880@1]2 881@2

2-84 ,

105 ek inekorh ekbUl izks ekyrh tSu ifr Jh lh-ih- tSu fuoklh nsosUnz uxj jk;iqj

pwukiRFkj 35@2006 10-07-2006

09-04-2007 9-4-2007 ls 8-4-2017

/kulwyh@vkjax

982 2-04 ,

106 Jh pqUuh yky ctkt vk- Jh eaxywey ctktfuoklh QkQkMhg jk;iqj

pwukiRFkj 48@2011 20-04-2012

18-05-2012 18-5-2012ls 17-5-2022

/kulwyh@vkjax

665] 669 2-80 ,

107 Jh jes'k dqekj iVsy vk- Jh thojke HkkbZ iVsy fu- U;w fVEcj eklsZV QkQkMhg jk;iqj

pwukiRFkj 29 ch@2011 03-01-2012

12-09-2012 12-9-2012 ls 11-9-2022

/kulwyh@vkjax

655@2 1-60 ,

108 Jherh m"kk tXxh ifr Jh lqjsUnz iky tXxh fuoklh 'kSysUnz uxj jk;iqj

pwukiRFkj 197@2006@ 07-02-2007

08-14-2007 8-1-07 ls 7-1-2017

/kulwyh@vkjax

917] 918 1-255 gs

109 vCnqy efyd vk- Lo- Jh eqlkHkkbZ fuoklh 31 xksYMu gksEl [kEgkjMhg jk;iqj

pwukiRFkj 206@2006@ 03-02-2007

19-01-2007 19-1-07 ls 18-1-2017

/kulwyh@vkjax

705] 706] 716

1-60 gs

110 Jh ukjk;.k HkkbZ iVsy vk- Jh dkarhHkkbZ fuoklh QkQkMhg jk;iqj

pwukiRFkj 74@2007@ 19-07-2007

14-08-2007 14-8-07 ls 13-8-2017

/kulwyh@vkjax

877 0-36 gs

111 Jhefr nqxsZ’k 'kqDyk ifr 'kjn 'kqDyk jk;iqj

pwukiRFkj 83@2011@ 24-11-2011

01-12-2011 01-12-2011 ls 30-11-2021

/kulwyh@vkjax

984 2-800

112 Jh ukses’k dqekj psyd firk Jh jru yky psyd fuoklh /kulqyh iks- ujngk rglhy vkjax ftyk jk;iqj

pwukiRFkj 31-01-2014 31-01-2014 ls 30-01-2024

/kulwyh@vkjax

762] 764] 765] 766]

767

1-060 gs

113 uRFkqyky Hkxokunkl izks- Jherh d`".kk vxzoky

pwukiRFkj 219@2009@ 19-11-2009

02-12-2009 02-12-2009 ls 3-12-2019

/kulwyh@vkjax

896 0-740

114 fcVqesd daLVªD’ku izks- Jh vfuy tlokuh iaMjh jk;iqj

pwukiRFkj 96@2011@ 04-05-2012

14-05-2012 14-05-2012 ls 13-05-2022

/kulwyh@vkjax

923 4-60 ,-

20

115 Jh fou; dqekj ctkt

pwukiRFkj 65@2012@ 16-01-2014 16-01-2014 ls 15-01-2024

/kulwyh@vkjax

916@3] 917@1

1-090 gsDVs;j

116 ljLorh LVksu izks- t;arhyky iVsy vk- Jh y[ku fuoklh Hkuiqjh jk;iqj

pwukiRFkj 17-01-2013 17-01-2013 ls 16-01-2023

/kulwyh@vkjax

872 4-35 ,dM+

117 Jh jes'k iVsy vk- Jh /khjth HkkbZ fuoklh QkQkMhg jk;iqj

pwukiRFkj 22@2006@ 09-02-2007

14-02-2007 14-2-2007 ls 13-2-2017

vdksyMhg

[kijh@vkjax

543 1-000

118 Jh _rqi.kZ xqIrk vk- Jh lrh"k dqekj fu- U;w 'kkafr uxj jk;iqj

pwukiRFkj 43@06 08-06-2006

22-06-2006 22-6-2006 ls 21-6-2016

vdksyMhg

[kijh@vkjax

129] 142 1-88,

119 Jh deys’k iVsy vk- Jh t;arh yky iVsy fuoklh Hkuiqjhjk;iqj

pwukiRFkj 181@06 10-04-2007

05-06-2007 5-6-07 ls 4-6-2017

vdksyMhg

[kijh@vkjax

544 Vq 0-769 gs

120 NRrhlx< fjlksZlsl ikV- lat; vxzoky dkafruxj fcykliqj

pwukiRFkj 182@2007@ 11-01-2008

04-02-2008 4-2-2008 ls 3-2-2018

vdksyMhg

[kijh@vkjax

500] 501] 573]

577]578

8-00 ,dM+

121 Jh eaxy HkkbZ iVsy vk- Jh ckykth HkkbZ fuoklh LVsV cSad dkWyksuh QkQkMhg jk;iqj

pwukiRFkj 35@2008@ 01-04-2008

11-04-2008 11-4-08 ls 10-4-2018

vdksyMhg

[kijh@vkjax

546@1] 547@2

1-676 gs

122 Jh ftrsUnz dqekj iVsy vk- Jh t;arh HkkbZ iVsy fuoklh ljnkj fVEcj eklsZV jk;iqj

pwukiRFkj 34@2008@ 01-04-2008

26-04-2008 26-4-08 ls 25-4-2018

vdksyMhg

[kijh@vkjax

547@1] 548] 549

1-318 gs

123 Jherh nhfidk iVsy ifr Jh furqu iVsy fu- ckykth xkMZu U;w fVEcj eklsZV jk;iqj

pwukiRFkj 212@2009@ 20-11-2009

07-12-2009 7-12-2009 ls 6-12-2019

vdksyMhg

[kijh@vkjax

553@2 1-460 gs-

124 e.khyky iVsy vk-Jh f'kox.k iVsy fu- U;w fVEcj eklsZV QkQkMhg jk;iqj

pwukiRFkj 214@2009@ 20-11-2009

07-12-2009 7-12-2009 ls 6-12-2019

vdksyMhg

[kijh@vkjax

553@1 1-040 gs-

125 vksfl;u LVksu izk-fy- Mk;- fodkl vxzoky fu- eksgkikyh jksM rg- [kjfl;k

pwukiRFkj 33@2009@ 28-02-2009

06-04-2009 6-4-2009 ls 5-4-2019

vdksyMhg

[kijh@vkjax

603] 633@4]5] 635] 638]

2-458 gs-

126 Jh eunhi vjksjk vk- Jh ljnkj dqanu flag fu-& rsyhcka/kk jk;iqj

pwukiRFkj 01-09-2014 01-09-2014 01-09-2014 ls 31-08-2024

vdksyMhg

[kijh@vkjax

539 3-00 ,dM+

127 d`".kk esVy odZ ikVZ- Jherh fdj.k xqIrk

pwukiRFkj 11@2012@ 23-06-2012

05-07-2012 05-07-2012ls 4-

vdksyMhg

331@1]2] 332] 340]

1-500 gsDVj

21

fuoklh 'kadj uxj jk;iqj

07-2022 [kijh@vkjax

342

128 jktdey fcYMlZ izk- fy- Mk;- Jh vfiZr lqjkuk fuoklh fcYMlZ dkyksuh bankSj

pwukiRFkj 43@2012@ 30-10-2012

05-11-2012 05-11-2012ls 4-11-2022

vdksyMhg

[kijh@vkjax

618] 619] 620] 621] 622] 623

1-20 ,dM

129 eksgEEn vyrkQ fi- Jh vCnqygd fuoklh tsy jksM lkbZ uxj jk;iqj

pwukiRFkj 63@2010@ 28-11-2011

06-01-2012 06-01-2012 ls 05-1-2022

vdksyMhg

[kijh@vkjax

386] 387] 477

0-820 gs-

130 vxzlsu feujYl Hkkxhnkj QeZ }kjk] Hkkxhnkj Jh lquhy vxzoky] fuoklh & 'kkWi ua- 214A f}rh; ry] _"kHk psacj] ,e-th- jksM+ jk;iqj

pwukiRFkj 02@2013 06-02-2014 06-02-2014 ls 05-02-2024

vdksyMhg

[kijh@vkjax

505] 511 1-640 gsDVj

131 Jh izoh.k vxzoky vk- Jh vkuan Lo:i fu- ek:rh fogkj jk;iqj

pwukiRFkj 99@2007@ 17-09-2007

14-08-2007 14-8-07 ls 13-8-2017

ipsM+k@vkjax

1214 0-280

132 Jherh T;ksfr vxzoky ifr Jh Lo=ar izdk'k vxzoky fu- ,pvkbZth ls DVj&1 'kadj uxj jk;iqj

pwukiRFkj 44@2007@ 16-12-2008

07-05-2009 7-5-2009 ls 6-5-2019

ipsM+k@vkjax

1162 0-809 gsDVj

133 esllZ Jh vkuan LVksu b.MLVªht izks- Jherh liuk fla?kkfu;k fuoklh ikjkxkao

pwukiRFkj 08-05-2012 08-05-2012ls 7-05-2022

ikjkxkao@vkjax

1859 2-39 ,-

134 Jh vejnkl vk- Jh egkohj dqjsZ fuoklh vkekflouh

pwukiRFkj 84@07@ 14-02-2008

11-03-2008 11-3-08 ls 10-3-2018

fulnk@vkjax

197 0-480

135 Jh lat; ;kno vk- Jh bUnzdqekj ;kno fu- jk;iqj

pwukiRFkj 188@2007 08-04-2008

01-05-2008 1-5-08 ls 30-4-2018

fulnk@vkjax

1345 2-30 ,

136 Jh izHkkr feJk vk- ,l-,u- feJk fuoklh fl)kFkZ pkSd fVdjkikjk jk;iqj

pwukiRFkj 199@2006@ 25-10-2007

17-11-2007 17-11-07 ls 16-11-2017

fulnk@vkjax

1344 0-145 gs

137 Jh larks"k ;kno fu- fulnk

pwukiRFkj 188@2007@ 08-04-2008

01-12-2010 1-12-2010ls 30-11-2020

fulnk@vkjax

1344 0-920

22

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

Major Minerals

ftyk jk;iqj varxZr izkIr jktLo dh tkudkjh

Ø- foRrh; o"kZ fu/kkZfjr

y{;

izkIr jktLo dh tkudkjh ;ksx izkfIr dk

izfr’kr eq[; [kfut xkS.k [kfut

1 2 3 4 5 6 7

1 2013&14 3750 yk[k 115412097 304770341 420182438 112-04%

2 2014&15 5320 yk[k 133188347 323639382 456827779 85-86%

3 2015&16 4890 yk[k 132337304 361878790 494216094 101-06%

Vhi %&foRrh; o"kZ 2015&16 esa [kfut pwukiRFkj uhyke en varxZr :i;s 52665180 ,oa [kfut

dks;yk varxZr :i;s 3308 yk[k dh i`Fkd ls jktLo izkfIr gqbZ gSA

5. Details of Production of Sand or Bajari in last three years

jk;iqj ftyk esa ?kksf"kr jsr [knkuksa dh lwph

Ø- jsr [knku dk uke

xzke iapk;r

@ fodkl[ka

M

[kljk ua-

jdck i;kZoj.k Dyh;jsal (MOEF) [knku lapkyudrkZ

[kuu dh vof/k

fjekdZ vkns'k Øa-@fnukad

izfr o"kZ

[kuu ek=k ¼?ku

eh- esa½ 1 Ikkjkxkao

¼Mh½

ikjkxkao

@vkjax

1598@

1872

2-000 gs- 905 @21-11-2013 50000 tuin

iapk;r vkjax

21-11-2013 ls

20-11-2016

lapkfyr

2 fp[kyh ¼,½ fp[kyh@

vkjax

1445 4-000 gs- 907@21-11-2013

100000

tuin

iapk;r vkjax

21-11-2013 ls

20-11-2016

lapkfyrA

3 pijhn ¼,½ pijhn@

vkjax

1509 4-000 gs- 1194@06-12-2013

100000

tuin

iapk;r vkjax

06-12-2013 ls

05-12-2016

lapkfyrA

4 xqYyq ¼,½ xqYyw@vk

jax

3009 50-00 ,- 1192@06-12-2013

500000

tuin

iapk;r vkjax

06-12-2013 ls

05-12-2016

lapkfyrA

5 dq:n ¼,½ dqVsyk@

vkjax

2742 2-000 gs- 1209@07-12-2013 50000 tuin

iapk;r vkjax

07-12-2013 ls

06-12-2016

lapkfyrA

6 xqnxqnk ¼,½

vesBh@

vkjax

436 4-000 gs- 1205@07-12-2013 100000 tuin

iapk;r vkjax

07-12-2013 ls

06-12-2016

lapkfyrA

7 dqEgkjh ¼,½ dqEgkjh@ 1882 4-000 gs- 1203@07-12-2013 100000 tuin 07-12-2013 ls lapkfyrA

23

vkjax iapk;r vkjax 06-12-2016

8 jkVkdkV¼,½ jkVkdkV

@vkjax

887 4-000 gs- 1201@07-12-2013 100000 tuin

iapk;r vkjax

07-12-2013 ls

06-12-2016

lapkfyrA

9 gjnhM+hg

¼,½

dkxnsgh

@vkjax

1221 4-00 gs- 1221@07-12-2013 100000 tuin

iapk;r vkjax

07-12-2013 ls

06-12-2016

lapkfyrA

10 xqnxqnk ¼ch½ vesBh@

vkjax

436 2-000 gs- 1362@23-12-2013 50000 tuin

iapk;r vkjax

23-12-2013 ls

22-12-2016

lapkfyrA

11 dksy;kjh

¼,½

dksy;kjh¼

y[kuk½@

vHkuiqj

766 6-000 gs- 1219@07-12-2013

150000

tuin

iapk;r

vHkuiqj

07-12-2013 ls

06-12-2016

lapkfyrA

12 y[kuk ¼,½ y[kuk@

vHkuiqj

866 3-000 gs- 1196@06-12-2013 75000 tuin

iapk;r

vHkuiqj

06-12-2013 ls

05-12-2016

lapkfyrA

13 Vhyk Vhyk@v

Hkuiqj

1891 6-00 gs- 4058@30-11-2015 108000

90000

xzke iapk;r

Vhyk

18-05-2015 ls

15-10-2015

30-11-2015 ls

29-11-2017

lapkfyrA

14 fp[kyh ¼ch½ fp[kyh@vkjax

1127 5-40 gs- 2022@07-08-2014 424@12-05-2015 4964@14-03-2016

120000 81000

xzke iapk;r fp[kyh

07-08-2014 ls 31-03-2015 01-04-2015 ls 15-10-2015 14-03-2016 ls 13-03-2018

lapkfyrA

15 pEikj.k ¼,½ pEikj.k@vHkuiq

j

3009 15-00 gs- 229@01-05-2014 1511@11-06-2015 4981@14-05-2016

252000 150000

tuin iapk;r vHkuiqj

01-05-2014 ls 31-03-2015 01-04-2015 ls 15-10-2015 14-03-2016 ls 13-03-2018

lapkfyrA

16 fulnk ¼,½ fulnk@vkjax

1351 6-40 gs- 569@06-06-2014 1704@12-06-2015 5043@17-03-2016

75000 50000

xzke iapk;r fulnk

06-06-2014 ls 31-03-2015 01-04-2015 ls 15-10-2015 17-03-2016 ls 16-03-2018

lapkfyrA

17 fp[kyh ¼lh½

fp[kyh@vkjax

1127 11-64 gs- 958@05-08-2014 1441@28-04-2015 5091@21-03-2016

230472 170000

xzke iapk;r fp[kyh

05-08-2014 ls 31-03-2015 01-04-2015 ls 15-10-2015 21-03-2016 ls 20-03-2018

lapkfyrA

18 dqEgkjh ¼ch½ dqEgkjh@vkjax

1882 15-00 gs- & & & & [kuu ;kstuk vuqeksfnr dj izsf"krA

19 Nqyuk nqyuk@vHkuiqj

1728] 1729

10-40 gs- & & & & [kuu ;kstuk vuqeksfnr dj izsf"krA

20 gjnhMhg ¼ch½

dkxnsgh@vkjax


21 gjnhMhg ¼lh½

dkxnsgh@vkjax

190 20-50 gs- & & & & [kuu ;kstuk vuqeksfnr dj

24

izsf"krA 22 dkxnsgh dkxnsgh

@vkjax 2400 24-00 gs- & & & & [kuu ;kstuk

vuqeksfnr dj izsf"krA

23 eqUMjk eqUMjk@vHkuiqj


24 jkVkdkV ¼ch½

jkVkdkV@vkjax


25 laqxsjk ¼,½ lqaxsjk@frYnk

231 5-00 gs- 441@24-05-2014 499@12-05-2015

100000 xzke iapk;r lqaxsjk

24-05-2014 ls 31-03-2015 01-04-2015 ls 15-10-2015

vuqeksfnr [kuu ;kstuk vkWuykbZu fnukad 07-10-2015 dks izsf"krA

26 ikjkxkao ¼ch½

ikjkxkao@vHkuiq

j

1225 10-00 gs- 251@01-05-2014 1686@11-06-2015

185250 tuin iapk;r vHkuiqj

01-05-2014 ls 31-03-2015 01-04-2015 ls 15-10-2015


27 vesBh ¼,½ vesBh@vkjax

1107 5-00 gs- 2070@07-08-2014 100000 xzke iapk;r vesBh

07-08-2014 ls 31-03-2015


28 Xkqnxqnk ¼lh½ vkjax 436 7-00 gs- & & & & vuqeksfnr [kuu ;kstuk vkWuykbZu fnukad 08-01-2016 dks izsf"krA

29 csuhM+hg ¼,½ jkVkdkV@vkjax

530 15-00 gs- & & & & vuqeksfnr [kuu ;kstuk vkWuykbZu fnukad 13-01-2016 dks izsf"krA

30 dqEgkjh dqEgkjh@/kjlhaok

1 14-00 gs- & & & & vuqeksfnr [kuu ;kstuk vkWuykbZu fnukad 14-01-2016 dks izsf"krA

31 xkSjHkkB ¼,½ xkSjHkkB@vkjax

1869 7-00 gs- 253@01-05-2014 1294@28-04-2015

126000 xzke iapk;r xkSjHkkV

01-05-2014 ls 31-03-2015 01-04-2015 ls 15-10-2015


32 [kV~Vh [kV~Vh@vHkuiqj

108 5-00 gs- & & & & [kuu ;kstuk vuqeksfnrA

33 [kSj[kqV ¼,½ cykSnh[kqnZ@frYnk

1 o 227 13-00 ,- 249@01-05-2014 517@12-05-2015

125000 xzke iapk;r [kSj[kqV

01-05-2014 ls 31-03-2015 01-04-2015 ls 15-10-2015

[kuu ;kstuk vuqeksfnrA

34 Ikkjkxkao ¼ch½

ikjkxkao@vkjax

1598@1872] 1862

22-50 gs- 897@18-05-2015 558421 xzke iapk;r ikjkxkao

18-05-2015 ls 15-10-2015

[kuu ;kstuk vizkIrA

35 Ikkjkxkao ¼,½

ikjkxkao@vHkuiqj

1127 11-64 gs- & & & & [kuu ;kstuk vizkIrA

36 Leksnk leksnk@vkjax


37 Josyh josyh@vHkuiqj


38 yedsuh ¼,½

yedsuh@vHkuiqj


39 Lsaejk lsejk@vHkuiqj


25

40 Cxnsgh cxnsgh@v

Hkuiqj 503 5-00 gs- & & & & [kuu ;kstuk

vizkIrA

41 csUnzh csUnzh@/kjlhaok


42 cjrukjk ¼,½

cjrukjk@/kjlhaok

238] 68] 79

10-00 gs- & & & & [kuu ;kstuk vizkIrA

43 Cgslj cgslj@/kjlhaok


44 cykSnh cykSnh@frYnk


45 y[kuk y[kuk@frYnk


46 Eksgesyk dkxnsgh@vkjax


6. PROCESS OF DEPOSITION OF SEDIMENTS IN THE RIVERS

Sendimentation 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

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

26

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

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

27

contrast, there is much less water. The river will therefore be shallow and slow-flowing.

It cannot carry as much material and so sand and shingle will be deposited. This is called

a point bar or slip off slope Due to erosion on the outside of a bend and deposition on the

inside, the shape of a meander will change over a period of time. Notice how erosion

narrows the neck of the land within the meander. In time, and usually during a flood, the

river will cut right through the neck. The river will then take the new, shorter route. The

fastest current, called the thalweg, will now tend to be in the centre of the river, and so

deposition is likely to occur in gentler water next to the banks. Eventually deposition

will block off the old meander to leave an oxbow lake. The oxbow lake will slowly dry

up , only refilling after heavy rain or during a flood. Streams lose velocity and make

deposits when their gradient decreases, when the volume of water decreases, when there

is an increase in cross section, when they encounter obstructions, or when they enter still

water. They deposit alluvial fans, alluvial cones, piedmont alluvial plains, channel fill,

bars, flood plains and deltas.

28

7. General Profile of the District

S.No. Particulars Statistics

1 General Information

Geographical Area 12383 km2

Geographical Position North Lattitude 19°46"35' to 21°53"

East Longtitude 81°32"05' to 82°59"05'

Administrative Division/Number of Tehsil 04- Raipur,Arang, Tilda, Abhanpur

04- Dharsiwa, Arang,Abhanpur, Tilda

No. of Panchayat/Villages 04/408

Population (As Per Census 2011) 4063872

Population Density (As Per Census 2011) 328

2 Geographology

Major Physiographic Units Alluvial Plain of Mahanadi Major Drainage Mahanadi , Kharun and its tributaries

Temprature Max. 45

Min. 25.6

3 Land use (Km2)

Forest Area 5259

4 Major Soil Types Vertisol , Ultisol 5 Number of Ground Water Monitoring Stations of CGWB (10.05.2016) Water Level Ultisol No. of Major Bridges 4 Nos. No. of Minor Bridges 13 Nos. 6 Hydrologeology

Major Water Bearing Formation Limestone, Sandstone

Pre-Monsoon depth of water level During 2012 13.6m

Post Monsoon depth of water level during 2012 2.83m

7 Mining Scenario

Total No. of Mining Leases (Major Minerals 16

Total Area of Mining Leases (Major Minerals) 182.273

Total Number of Quarry Lease (Minor Minerals) 137 Total area of Quarry Lease 270-564 Total Royalty or Revenue Received from Minor

Minerals in 2015-16 361878790

Total No. Notified Sand Lease 46

Total Area of Sand Leases 419.64

29

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

Mining etc.

i). Forest :-

S.No Content Raipur

1 Name of Division Raipur

2 Name of Sub Divivsion Raipur, New Raipur

3 Name of Rang 4

4 Total No. of R.A. Circle 3

5 Totoal No. of Beat 42

6 Total No. of Forest

Compartment 12383 Sq. Km.

7

Total Division Area of 29528 Sq. Km.

10.538 Sq. Km.

1.581 Sq. Km.

17.409 Sq. Km.

8

Total Forest of

(A) Reserved Forest (R.F.)

(B) Protected Forest (P.F.)

(C ) Mixed Forest

0%

9

% of Forest Cover of Division

Sq.Km.

Sq.Km.

15.457 Sq.Km.

10

Area Under

(A) Teak Forest

(B) Sal Forest

(C ) Mixed Forest

4863872

Male 2018186

Female 201586

11

Population of the Division (As

Per 2011 Census

4063872

Male 2048186

Female 201586

12

(A) No. of JFM commitees

(B) Member of JFM Commitees 06

Male - 734

Female - 731

30

Division Headquarter, Road type and Forest map of Raipur District

31

ii) Harticulture,Agriculture and Irrigaton :-

jksi.khokj ikS/k mRiknu] forj.k ,oa 'ks"k dh tkudkjh ekg& ekpZ 2015 dh fLFkfr esa] ftyk & jk;iqj

dz-

'kkl- m-ls- x

35

VEGETATION MAP OF RAIPUR DISTRICT

36

iii) Rivers: -Sediment deposition in the Mahanadi River

The Mahanadi river is perennial, which flows over granitic and quartzite terrain,

acquiring/ transporting resistant sediments of different (fine grain to pebble and boulder)

size by fluvial action during high-flood/rainy season and deposited in the river bed, point

and sandbars, fiver banks, floodplains, etc. Therefore the extracted sand is generally

recouped annually. River Mahanadi is situated in the East of the village Kumhari where

the declared area is demarcated on the sandbar combined with point bar ate riverbed for

excavation. Exposed sand is available for mining ate the bars after rains i.e. from October-

November having flowing water level at 1.0 m. Depth of surface water is gradually

increased and reaches to 3 meter maximum, before the monsoon i.e. during summer till

active monsoon period sand is also available at the riverbed for excavation.

Sand mining in Mahanadi River

37

Feasibility of sand mining:

Sand will be mined from surface, where entire removed material is the same.

The sand mining has no adverse effect. The post mining also has no undesirable impact on

land, air, groundwater, living animals, vegetation, organism/planktons. Sand has extensive

demand for all type of developmental activities. Sand resources of 4, 00,000 m3 are

estimated to exist up to 8 m depth. Initially the moderate quantity of sand shall be mined

as essential building material (minor mineral) for all types of constructions and yield

maximum quantity during summer till affective monsoon starts.

Mining :-

Newly formed state of Chhattisgarh has a large deposit of Coal, Iron Ore,

Limestone, and various other mineral ores, which prepared foundation for the

establishment of various industrial units in the state. The availability of excess amount of

Cement, Industrial raw material, cheap labour force, and absence of labor unrest has

contributed in substantial growth of industrial sectors across the state.

Sporadic mushrooming of these industrial units in Raipur city has gradually changed the

bowl of rice into a production hub of steel, cement and energy. However, growth in the

Industrial sectors has also resulted in rise in the pollution level of the state capital city.

Hence, in order to form a certain balance between the industrial growth, and

environmental pollution the Chhattisgarh Environment Conservation Board has been

formed.

iv) Transport :-

1. Railways :-

Raipur Junction railway station is situated on the Howrah-Nagpur-Mumbai line of

the Indian Railway (via Bhusawal, Nagpur, Gondia,Bilaspur, Kharagpur) and is connected

with some major cities like New Delhi, Mumbai, Bhopal, Jabalpur, Saugor, Katni, Itarsi,

Gondia, Kolkata, Jamshedpur, Chennai, Bangalore, Kota, Ahmedabad,Jaipur

Vishakapnam etc. Raipur still lacks direct rail connectivity with Indore, Ujjain, Ratlam,

Kolhapur, Jodhpur etc. A branch line from Raipur to Vizainagaram etc via Mahasamund –

38

Titlagarh originates from here and most of the products of Chhittisgarh reaches

Vishakhapatnam by this railway line. There is also a narrow gauge line connecting Raipur

to Rajim and Dhamtari via Abhanpur, which is being converted to broad gauge and

realigned to serve the city of Naya Raipur as well.

1. Railways :-

Raipur Junction railway station is situated on the Howrah-Nagpur-Mumbai line of

the Indian Railway (via Bhusawal, Nagpur, Gondia,Bilaspur, Kharagpur) and is connected

with some major cities like New

Delhi,Mumbai, Bhopal, Jabalpur, Saugor, Katni, Itarsi, Gondia,Kolkata, Jamshedpur, Che

nnai ,Bangalore, Kota, Ahmedabad, Jaipur Vishakapatnam, etc. Raipur still lacks direct

rail connectivity withIndore, Ujjain, Ratlam, Kolhapur, Jodhpur, etc. A branch line from

Raipur to Vizianagaram via Mahasamund - Titlagarh originates from here and most of the

produce of Chhattisgarh reaches Vishakhapatnam by this railway line. There is also a

narrow gauge line connecting Raipur to Rajim and Dhamtari via Abhanpur, which is

being converted to broad gauge and realigned to serve the city of Naya Raipur as well.

2. Roads :-

National Highways connecting Raipur to various cities:

National Highways

number Connecting cities

NH 6 Hajira-Dhule-Nagpur-Raipur- Mahasamund - Sambalpur -

Baharagora-Calcutta

NH 53

Raipur-Vizianagaram Junction with National Highway No. 5

near

Natavalasa

NH 200 Raipur-Bilaspur-Raigarh-Kanaktora-Jharsuguda-Kochinda-

Deogarh-Talcher-Chandhikhol

39

NH 217 Raipur- Mahasamund - Gopalpur

NH 12A Raipur-Jhansi

Asian Highway Number 46 - AH46 passes through Raipur.

3. Airport :-

Swami Vivekananda Airport,Raipur

Swami Vivekananda Airport or Mana Airport is primary airport serving the state

of Chhattisgarh.The airport is located, 15 km (9.3 mi) south of Raipur near Naya Raipur.

After recent modernization, is one of its kind in central India and presently connects

Raipur to most of the major Metro city of India.

A new integrated terminal designed to handle 700 passengers (including 200

international flyers at a time) and covering an area of 18,500 m2 (4.6 acres) was

inaugurated on 7 November 2012 by President of India Pranab Mukherjee. The new

terminal will be used for domestic flights, while the proposed international terminal is

being renovated to handle international operations.

Airlines Destinations

Air India Delhi, Mumbai, Nagpur, Visakhapatnam, Pune, Bhopal

IndiGo Ahemadabad, Bangalore, Delhi, Goa, Hyderabad, Indore, Kolkata, Mumbai, C

hennai

Jet

Airways Delhi, Mumbai, Bhopal

40

Vistara in future

Spicejet in future

Air Asia

India in future

Local transport

A city bus service is provided by Raipur City Bus Limited (RCBL) for the intra-city

travel. Raipur Municipal Corporation launched the Raipur City Bus service on 25

February 2008. The company runs 40 buses out of which 32 are low floor Tata Starbus.

Paratransit in the form of auto-rickshaws and tuk-tuk are available all over the city. 100

new city buses under JNNURM have been inducted by Raipur Nagar Nigam Transport

Limited (RNNTL), which serve the Raipur and connect Naya Raipur also.

9. Physiography of the District

Raipur district characterized by rocks belonging to Proterozoic age and the main

rocks is Limestone and dolomite and then Laterite and soil are found ranging age between

sub-recent to recent.

Physiographically the area in Raipur district having plains belonging to

Chhattisgarh basinal area with an elevation of 278 feet(298.16 meters) above m.s.i. and

the general slop is towards the north-east.

Geomorphologically the district is having matured type of land forms and can be

broadly divided into two prominent geomorphic units. These are

1. Dissected pediplain made by Proterozoic shale- limestone dolomite area.

2. Alluvial Plain formed by Seonath-Mahanadi Alluvium.

41

As per the US soil taxonomy only two soil types namely Vertisol and Ultisol

have been found in the district. The soil orders in US soil taxonomy and their

Indian equivalents, which are found in the district, are:

S. No. US soil taxonomy Indian equivalents

1 Vertisol Deep black soil

Medium black soil

2 Ultisol Lateritic soil

Red and yellow soil

42

Climate :-

Raipur has a tropical wet and dry climate, temperatures remain moderate

throughout the year, except from March to June, which can be extremely hot. The

temperature in April–May sometimes rises above 48 °C (118 °F).These summer months

also have dry and hot winds. In summers, the temperature can also go up to 50 °C. The

city receives about 1,300 millimetres (51 in) of rain, mostly in the monsoon season from

late June to early October. Winters last from November to January and are mild, although

lows can fall to 5 °C (41 °F).

10. Rainfall of District Raipur Month wise

dzekad ftyk@rglhy dk uke

2012-13 2013-14 2014-15

1 2 3 4 5

1 jk;iqj 1716.7 1599.00 1182.50 2 vkjax 1924.0 1959.00 1134.60 3 frYnk 1669.3 1702.03 1299.50 4 vHkuiqj 1509.0 1539.00 1167.90

1221.8 1704.8 1196.1

43

jk;iqj ftyk varxZr foxr rhu o"kksZ esa fxjh o"kkZ dh ekfld tkudkjh o"kkZ ekid dsUnz dk uke ¼o"kkZ fe-eh- esa½

46

11. Geology and Mineral Wealth

1. Geology:-

1.1 Regional:-

Raipur Group comprises three cycles of argillite-carbonate sequence each cycle

starting with a carbonate followed by argillite at places with lenticular areanaceous rocks

denoting regressive phase of the sea. These cycles are distinctly developed in the Hirri

sub-Basin particularly in the southern and central part. The cycles are represented by (1)

Charmuria Limestone-Gunderdehi Shale;(2) Chandi Limestone Tarenga Shale and (3)

Hirri Dolomite Maniari Shale.

The basal unit of Charmria Formation is represented by clay and chert well

developed in the south central parts of the basin. It is followed upwards by flaggy and

cherty limestone, which is feebly phosphatic, developed all along the southern part of the

basin. The overlying member is a dark grey, flaggy, pyritiferous limestone. The youngest

member Bagbura comprises purple argillaceous limestone, which is locally phosphatic.

Charmuriya Formation grades into overlying Gunderdehi Formation comprising shale and

sandstone. The formation denotes a renewed submergence of the basin with enhanced

supply of silty and shaly clastics in a warm oxidizing condition in subtidal zone. The

overlying Chandi Formation comprises mojor stromatolotic limestone sequence developed

around southern side of depocentre of Hirri sub-basin with arcuate outcrop pattern.

Throughout the northern part, the carbonate facies disappears or is present only as

intercalation discrete pockets or lenses in calcareous argillite. Chandi Formation has been

sub-divided into four member based on dominant carbonate facies. They, however

gradually fuse into single carbonate sequence towards west. The prolific growth of algae

in photic zone of sub tidal to intertidal flats of a very slowly sinking basin produced the

thick carbonate sequence towards west. Tarenga Formation conformably overlies the

Chandi Formation, which is sub- divided into Kusmi Member (argillite), Dagauri Member

(clay-chert and bhilha Mmber (dolomitic argillite) from bottom to top. The overlying

Pandaria Formation represents the calc-argillite facies developed all along the northern

part of the Hirri sub-basin. This litho-unit overlies the Chandarpur Arenite along the

northern margin and is charactrised by predominance of pink- to purprle calcareous shale

with lenses and pockets of bedded flaggy limestone, stromatolotic limestone and dolomite

and bedded limestone associated with the chert bands. These lenses and pockets vary

47

widely in dimension from a few metres to several hundred mets in length. Pandaria

Formation represents lateral facies variation of Charmuria (bedded) Limestone,

Gunderdehi Shale, Chandi (stromatolitic) Limestone and Tarenga Argillite, which are

distinctly developed as mappable unit in the southern part, but occurs as a member along

the northern part of the sub-basin. The Hirri Formation is well developed around the

central part of Hirri sub-basin and forms an oval outcrop pattern. Althouth it attains a

considerable thickness in south, it is very thin along the northern fringes and is interpreted

from outcrop exposures and or local excavations. The formation conformably overlies the

Tarenga Formation in the south and Pandaria Formation in the north. The dominant rock

type is dark grey, bedded dolomite, associated with light gre laminated argillaceous

dolomite, and black and white chert. At places intra- formational dolomite (

conglomeratic) and black shale contain gypsum as layers, parallel to bedding and as

disseminated grains/crystal. Stromatolitic dolomite is exposed in Hirri and Kodwa mines.

The stromatolites are columnar having a wide inter-columnar space. The youngest Maniari

Formation is named after the river along which the rock is best exposed and an oval-

shaped outcrop in the central part of the sub-basin . It represents the closing phase of

deposition in Chhattisgarh Basin and consists of lower gypsiferous grey siltstone, shale

followed by reddish brown calcareous/non-calcareous shale with limestone and dolomite.

A close study of stromatolites in Raipur Limestone indicates two different

assemblages, which can be assigned to two biozones. Gymnosolen, Inzeria, Baicalia,

Tungussia and Linella represent the lover biozone in the lower part by Baicalia, Anabaria,

Tungussia, Conophyton, Jacutophyton, Kussiella and Colonnela represent the upper one.

The upper biozone indicates an age range from late Riphaean to Vendian whereas the

lower assemblage indicates a middle Riphean age.

49

The geological succession of Raipur Region

Intrusives Dolerite dykes

CHHATTISGARH

GROUP

RAIPUR

GROUP

Manairi

Formation (70m)

Purple shale with dolomite,

dolomitic limestone and gypsum

Hirri Formation

(70m+)

Grey dolomite, argillaceous

dolomite

Tarenga

Formation(180m)

Bilha Member Purple dolomitic argillite

Dagauri Member Green clay, chet and shale

intercalation (tuffaceous?)

Kusmi Member

Chandi Formation

(67m)

Nipania Member Purple and bedded limestone

Purple argillaceous stromatolitic

dolomite

Pendri/Deodonger

Member

Purple and grey stromatolitic

limestone and dolomite with

flaggy limestone-shale

intercalation/ferruginous

glauconitic arenite and shale

Gunderdehi

Formation

Newari Member Pink and buff stromatolitic

limestone and dolomite

Andha/Dotopar

Member

Predominantly pink, purple and

grey shale with limestone

intercalations/arenite/buff to

green shale member in the middle

Charmuria

Formation

(490m)

Bagbura Member Purple limestone (phosphatic)

Kasdol Member Dark grey bedded

limestone/argillaceous limestone

with minor shale intercalations

Ranidhar Member Cherty limestone and dolomite

(phosphatic at places)

Sirpur Member Chert and clay intercalatin

2. Local Geology

Undeformed and unmetamorphosed sedimentary sequence of rocks

belonging to Chhattisgarh Supergroup of Meso to Neo Proterozoic age(2000-900 m.y.)

occupy the northeastern and mid-eastern part of district. Chhattisgarh Supergroup is

represented by Chandarpur and Raipur groups. Chandarpur Group comprises mostly

50

arenitic and at places ferruginous sandstone and polymictic conglomerate sandstone

shows shale parting at places. Raipur Group is classified into Charmuria, Gunderdehi and

Chandi formations. Charmuria Formation is dominantly a carbonate facies and is

represented by cherty limestone, dark grey, chertiferous and argillaceous limestone and

purple phosphatic limestone. Gunderdehi Formation is dominantly a calcareous- argillite

litho facies. It comprises calcareous, highly friable, purple shale associated with

imperistent stromatolitic limestone bands, and intra-formational arenite. It comprises

stromatolitic limestone and dolomitic limestone with ferruginous and glauconitic

sandstone.

The geological succession of Raipur district is as follows:

Age

Super

Group Group Formation Litho-units

Recent to - - Soil, Soil, alluvium, Moorum,

Sub-Recent

Laterite Laterite, Unconsolidated

Pebbly beds

upper Proterozoic to Chhattisgarh R Tarenga Banded redish-brown

To

super Group A

argillaceous dolomite,

Middle Proterozoic

I

porcellanite, purple calcarious shale.

P Chandi Purple impure dolomite shale,

U

Bedded Limestone, Flagy

R

limestone, Stromatolitic

limestone and Dolomite.

G Gunderdehi Red shale, limestone bands and

R

pockets of intra-

fromational

O

conglomerate,buff and

purple

U

calcareous shale.

P Charmuria Pinkish and gray limestone Dark

Grey bedded limestone Grey shaly

limestone, light Grey limestone.

51

3. Mineral Resources of Raipur District:-

The district is rich in terms of economic mineral wealth. The important economic

mineral deposits/occurrences reported in the district are clay, dolomite, limestone.

Limestone deposits found in Kesla, Kharora, Tilda, Tekari, Dondekhurd, Mandirhasaud,

Matiya, Bahesar,Dondekala etc. reported Dolomite associated with limestone is reported

from Tekari,Kunda,Madhi,Khapri etc. Despite flag stone are reported at and around

villages Nisda and Paragaon sandstone are also is being mined at Birbira, Doma,

Mokhetara etc. villages.

The major limestone belt of the district are :

(1)Bangoli - Kharora – Mohrenga

(2) Murra-Dhansuli

(3)Pirda-Bahnakadhi-

(4)Dondekala-Dondekhurd-Lalpur-Matiya

(5)Madhi-Khapri-Sontara.

Mining prospects of the district :-

Raipur district occupies a place of significance in respect of its mineral resources.

The important economic minerals occurs in the district are limestone of various grades,

from the low grade shaly limestone to the Cement and Blast Furnace Grade, the huge

quantity is suitable for the Iron and Steel Industry. The sandstone, flagstone, important

building materials and the decorative stones alsooccurs;this plays an eminent role to

generate the revenue for the district.

The minor mineral such as sand, murrum, earthen clay and soil are also present in

good quantity for construction and other uses.

52

Geology and Mineral Map of Raipur District, Chhattisgarh

53

Other Information of the District

Drainage system with description of main rivers

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.

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.

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