District Survey Report Raipur AS PER NOTIFICATION NO

2016

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

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

DGM Hewlett-Packard 01/01/2016

Note:

The information provided in this report has been prepared from the existing and latest data collected from the concerned authorities. Although utmost care has been taken during editing and printing, still there may be some minor corrections for which the Directorate of Geology & Mining, Regional office Raipur Sonakhan Bhawan, cannot be held responsible. The queries in this regard are most welcome by the concerned office.

LOCATION AND COMMUNICATION MAP OF THE RAIPUR DISTRICT

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 15 th 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 3

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.

INDEX MAP OF RAIPUR DISTRICT

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

General Information of Raipur District

Sub- No. of No. of No of No. of Villages Population % division Tahsils Blocks Gram Habited Inhabited as per 2011 Literacy Panchayat 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 Male Female Rural Urban % Population Literacy 21,60,876 11,00,861 10,60,015 8,84,224 12,76,652 80.52

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 %&

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(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 ¼ Brick earth ½ Øa iV~Vsnkj dk uke [kfut Lohd`r vkns’k fu"iknu dkykof/k xzke [kljk uEcj {ks=Q iw.kZ irs lfgr Øekad ,oa fnukad iapk;r y fnukad ,oa rglhy ¼gsDV j esa½ 1 2 3 4 5 6 7 8 9 1 Jh dkS’ky dqekj feV~Vh 61@2011@ 21-07-2011 21-7-2011 ls ljksuk@ 79@1] 113] 6-80 xaxokuh fuoklh 25-05-2011 20-7-2016 jk;iqj 114] 115 ,dM+ QkQkMhg jk;iqj 2 Jherh lksuknsoh feV~Vh 104@2007@ 22-07-2008 22-07-08 ls ljksuk@ 401] 402 5-00 bZ’kjkuh fuoklh yk[ks 11-04-2008 21-07-2018 jk;iqj ,dM+ uxj jk;iqj 3 Jh vfuy dqekj feV~Vh 9@2011@ 26-01-2012 26-1-2012 ls ljksuk@ 11 Vq-] 12 Vq- 4-40 xkojh fuoklh yk[ks 03-10-2011 25-1-2017 jk;iqj ,dM+ uxj jk;iqj 4 Jh larks"k bZ’kjkuh feV~Vh 183@2007@ 03-01-2009 3-1-2009 ls ljksuk@ 6@2] 14@1 7-20 fuoklh yk[ks uxj 22-12-2008 2-1-2019 jk;iqj ,dM+ jk;iqj 5 Jh v’kksd dqekj feV~Vh 204@2008@ 06-11-2009 6-11-2009 ls dqEgkjh@ 105] 109] 9-80 vkgwtk vk- Jh 12-08-2009 5-11-2019 jk;iqj 1]2 ,dM+ fd’kupan fu- ueZnkikjk jk;iqj 6 Jh fd’kupan vkgwtk feV~Vh 118@2011@ 24-12-2012 24-12-2012 dqEgkjh@ 2@1] 3-74 vk- Jh is’kqey fu- 22-11-2012 ls 23-12- jk;iqj 3@1]4]5 ,dM+ ueZnkikjk jk;iqj 2017 7 Jh gjh’k 'kqDyk] vk- feV~Vh 17@2014 01-08-2014 01-08-2014 dqEgkjh 138@1] 0-566 Lo- Jh :nzukjk;.k 16-01-2014 ls 31-07- 139@1 gs- 'kqDyk] fu-& 2019 jksg.khiqje jk;iqj] 8 esllZ ckykth fczDl feV~Vh 34@2010@ 19-03-2011 19-03-2011ls cgslj@ 91] 92] 93 3-850 Ogh-ls- eqjyh/kj 22-03-2011 18-03-2021 jk;iqj 94@1&2] gsDVj fuoklh VkVhca/k 95@1]2]3]4 jk;iqj 9 Jh lqjs’k ykyokuh feV~Vh 72@2014@ 08-08-2014 08-08-2014ls cgslj@ 69@2] 2-267 vk- Jh d`ikynkl 06-08-2004 07-08-2024 jk;iqj 69@3 gsDVj fu- Jhuxj jk;iqj 10 t; Jh fczDl izks- feV~Vh 101@2006@ 14-09-2006 14-9-2006 ls cgslj@ 61@1]2]3] 1-276 Ogh- ls- eqnfy;kj 04-09-2006 13-9-2016 jk;iqj 63@1]2] gsDVj fuoklh VkVhca/k 64@2] 65 11 Jherh vesjk efyd feV~Vh 70@2007@ 07-08-2007 7-8-2007 ls gjnh@ 165 3-95 fuoklh jk;iqj 25-06-2007 6-8-2017 vkjax , 12 Jh x.ks’k dqEgkj feVVh 127@06@ 10-10-2006 10-10-2006 lklkoyh 20 2-023 firk Jh >kM+w lkgw 29-09-2006 ls 9-10-2016 @frYnk gs- fuoklh lklkgksyh frYnk 13 Jh nhuca/kq lkgw vk- feV~Vh 238@09@ 24-12-2010 24-12-2010ls yedsuh 114 1-336 Jh fNUNkjke lkgw 07-01-2011 23-12-2020 @vHkuiq gs- 10

fuoklh

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¼l½ pwukiRFkj (Limestone) %&

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23 esllZ egkek;k pwukiRFkj 224@2007@ 16-01-2008 16-01-2008 ewjk@frY 662@5]6 1-14 feujYl Hkkxhnkj Jh 08-01-2008 ls 15-1- nk ,dM+ iq:"kksRre vxzoky¼yht 2018 VªkalQj iwoZ uke Jh Hkjr iVsy½ 24 es- fo'o Hkkjrh pwukiRFkj 225@2009@ 24-11-2009 24-11-2009 ewjk@frY 468@1] 2-390 feujYl ikVZuj uohu 18-11-2009 ls 23-11- nk 487@2] gs- vxzoky vk- Jh lqjs'k 2019 492@2] dqekj vxzoky fuoklh 493@1] 499] jk;iqj 467@4] 491@4]6] 489 25 Jherh jktJh oekZ ifr pwukiRFkj 140@2010@ 22-01-2011 22-01-2011 ewjk@frY 567@1] 0-730 Jh egs’k dqekj oekZ 10-01-2011 ls 21-01- nk 568@1]2]3] gs- fu- rqylh iks- frYnk 2021 569@1] rglhy frYnk ftyk 569@3] jk;iqj 569@4] 570] 573 26 Jh lnkf’ko oekZ vk- pwukiRFkj 39@2012@ 08-02-2013 08-02- ewjk@frY 822 0-722 Jh vf/kj oekZ fuoklh 04-12-2012 2013ls 07- nk gsDVj ewjk frYnk jk;iqj 02-2018 27 Jh fot; vxzoky] vk- pwukiRFkj 28-08-2014 23-08-2014 23-08- ewjk@frY 595] 596] 0-900 Lo- Jh 'kadj yky 2014ls 22- nk 597] gs- vxzoky fuoklh &eksok 08-2024 604@1 jk;iqj 28 Jh cyoku pgsfj;k] pwukiRFkj 78@2014@ 10-03-2015 10-03-2015 ewjk@frY 610 0-809 vk- Jh vksadkjey 05-03-2015 ls 09-03- nk gsDVj pgsfj;k] 2020 fuoklh & voafr fogkj] jk;iqj 29 Jh 'kjn xks;y vk- pwukiRFkj 79@2014@ 02-01-2015 02-01-2015 ewjk@frY 608 1-60 Lo- Jh jes’k xks;y 12-12-2014 ls 01-01- nk ,dM+ fuoklh&[kjksjk 2020 rglhy frYnk] jk;iqj 30 esllZ ekW egk y{eh pwukiRFkj 34@2013@ 22-01-2014 22-01-2014 ewjk@frY 664@11]1 2-500 LVksu Ø’kj izks- Jh 15-01-2014 ls 21-01- nk 3]2]3]12]4] gs r:.k vxzoky 2024 6]8]10]1]5] 7]9] 665@3]6] 659 31 Jh fuys’k vxzoky fi- pwukiRFkj 16-03-2011 23-03-2011 23-03-2011 cqMsjk@f 419@1 1-06 Jh cyHknz fu- [kjksjk ls 22-03- rYnk ,dM+ frYnk jk;iqj 2021 32 eks- dkfle vk- Lo Jh pwukiRFkj 201@2009@ 03-12-2009 3-12-2009 cqMsjk@f 419@9 0-750 tyhy vgen fuoklh 20-11-2009 ls 2-12- rYnk gs- cq

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36 Jh Lkfgy flag firk pwukiRFkj 144@2008@ 08-10-2008 8-10-2008 vksVxu 578@1 1-800 Jh v’kksd flag 26-09-2008 ls 7-10- @frYnk gs- fuoklh ,e-vkbZ-th 2018 'kadj uxj jk;iqj 37 Jh rkjkpan vkgwtk] pwukiRFkj 19-08-2014 27-08-2014 27-08-2014 udVh 290@15] 4-60 vk- Jh fd’kupan ls 26-08- [kijh@f 290@16 ,dM+ vkgwtk] fu-&QkQkMhg 2019 rYnk xyh ua-&1 jk;iqj 38 Jh vkyksd 'kekZ pwukiRFkj 42@2013@ 18-02-2014 18-02-2014 udVh 290@18 1-00 ,- fuoklh fly;kjh 29-01-2014 ls 17-02- [kijh@f jk;iqj 2024 rYnk 39 Jherh vfurk tSu pwukiRFkj 68@2011@ 19-12-2012 19-12-2012 nqyuk@ 432@3] 2-092 vk- Jh Jh;ka’k tSu 28-04-2012 ls 18-12- vHkuiqj 433@2 ,dM+ fu0uokikjk@ jkfte 2022 ftyk jk;iqj 40 Jh vfer tSu vk- Jh pwukiRFkj 231@2008@ 28-11-2009 28-11-2009 nqyuk@ 688] 0-76 dSyk’k tSu fuoklh 03-05-2008 ls 27-11- vHkuiqj 687@2] ,- uokikjk@jkfte 2019 ftyk jk;iqj 41 Jh nmokjke lkgw pwukiRFkj 12@2012@ 22-09-2012 22-09-2012 nqyuk@ 433@1] 1-40 fuoklh nqyuk 25-07-2012 ls 21-9- vHkuiqj ,- 2022 42 Jh nmokjke lkgw pwukiRFkj 05@2011@ 14-02-2011 14-02-2011 nqyuk@ 433@1] 0-750 fuoklh nqyuk 25-01-2011 ls 13-2- vHkuiqj 590] 591 2021 43 Jh gfjeksgu lkgw pwukiRFkj 62@2005@ 20-09-2010 20-09-2010 nqyuk@ 686 2-22 gs fuoklh 29-03-2006 ls 19-9- vHkuiqj 2020 44 Jh x.ks’k izlkn [ksrku pwukiRFkj 93@2011@ 08-05-2012 08-05-2012 csUnzh@v 100@3] 2-22 fuoklh ekgnkikjk 09-04-2012 ls 7-5-2022 Hkuiqj 100@4 ,- jk;iqj 45 Jh vfuy dqekj pwukiRFkj 230@06@ 28-05-2007 28-5-2007ls fijnk@j 640 1-56 vBokuh 18-04-2007 27-5-2017 k;iqj ,dM+ yk[ksuxj jk;iqj 46 Jh iadt panzkdj pwukiRFkj 10@2011@ 01-05-2012 01-5-2012 udVh@ 457@1] 1-79 fuoklh Vsejh jk;iqj 11-08-2011 ls 30-4- jk;iqj 458@2 ,dM+ 2022 47 Jh tktZ jktu pwukiRFkj 247@2009 25-01-2012 25-1-2012ls lsjh[ksM+h 689@1ls 3-54 fuoklh jk;iqj 25-01-2011 24-01-2022 @jk;iqj 3] 691 ,dM+ 48 fpadkjk feujYl pwukiRFkj 217@2006@ 03-05-2007 3-5-2007 ls lsjh[ksM+h 690@3 0-809 Hkkxhnkj Jh ftrsUnz 16-04-2007 2-5-2017 @jk;iqj gsDVj iVsfj;k fuoklh jk;iqj

49 Jherh izfrek iqtkjh pwukiRFkj 177@2005@ 03-01-2007 3-1-2007 ls Vsejh@jk 406 3-60 14

fuoklh lnjcktkj 31-10-2006 2-1-2017 ;iqj ,dM+ jk;iqj 50 Jherh iq"ik csu iVsy pwukiRFkj 14@2010@ 14-10-2010 14-10- nkSansdyk 463@1 0-840 fu-& U;w fVEcj ekdsZV 08-10-2010 2010ls 13- @jk;iqj gs- jk;iqj 10-2020

51 Jh fgrs’k ukxokuh pwukiRFkj 153@2009@ 27-07-2010 27-7-2010 nkSansdyk 482] 2-00 fuoklh nsosUnz uxj 13-07-2010 ls 26-7- @jk;iqj 483]484]43 ,dM+ jk;iqj 2020 9 52 NRrhlx<+ feujy izks- pwukiRFkj 96@2006@ 06-08-2007 6-8-2007 ls Niksjk@ 777] 778 5-10 eks- vlxj fu- 13-08-2007 5-8-2017 jk;iqj ,dM+ ekSngkikjk jk;iqj 53 vuqlwfpr tutkfr pwukiRFkj 104@05@ 09-08-2006 9-8-2006 ls Niksjk@ 767 0-76 lewg fuoklh nkSansdyk 08-08-2006 8-8-2016 jk;iqj ,dM+ 54 Jh ,p-,l vjksjk vk- pwukiRFkj 236@2009@ 14-12-2010 3-11-2010 ujngk@ 1997 3-00 , Jh dqanu flag fu- 04-11-2010 ls 2-11- vkjax ';ke uxjjk;iqj 2020 55 Jh fnus'k dqekj pwukiRFkj 146@2010@ 24-12-2012 24-12- ujngk@ 1946 4-10 , cM+okuh vk- 25-10-2012 2012ls 23- vkjax fupynkl fu- 12-2022 QkQkMhg jk;iqj 56 Jh izhfe;j esVy izks- pwukiRFkj 127@2007@ 12-08-2008 12-8-2008 ujngk@ 1967 2-60 vt; >ka>jh fuoklh 05-07-2008 ls 11-8- vkjax nsosUnz uxj jk;iqj 2018 57 d`".k dqekj lkgw vk- pwukiRFkj 65@2010@ 13-08-2010 13-8-2010 ujngk@ 1945 1-200 Jh eulkjke lkgw 27-07-2010 ls 12-8- vkjax gs- fuoklh lsyk’kiqjh 2020 jk;iqj 58 Jh banjdqekj ukxnso pwukiRFkj 04@2010@ 02-02-2011 2-2-2011 ls ujngk@ 1948 4-90 , vk- tsmjke fu- 28-01-2011 1-2-2021 vkjax tsyjksM jk;iqj 59 Jh gjhyky iVsy vk- pwukiRFkj 175@2006@ 28-12-2006 28-12-06 ls ujngk@ 1964 1-214 dkathHkkbZ iVsy 08-12-2006 27-12-2016 vkjax fuoklh Hkuiqjh jk;iqj 60 Jh izoh.k dqekj iVsy pwukiRFkj 14@2007@ 12-03-2007 12-3-07 ls ujngk@ 1953@1] 1-280 vk- Jh n;kHkkbZ nsosUnz 01-03-2007 11-3-2017 vkjax 1954@1 uxj jk;iqj 61 Jh fuf[ky frokjh pwukiRFkj 32@2006@ 25-07-2006 25-7-06 ls ujngk@ 1955@2] 1-772 gfjgj feujy] jk;iqj 01-08-2006 24-7-2016 vkjax 1956] gs 1957 62 Jh ;ksxs’k vxzoky vk- pwukiRFkj 4@2007@ 03-01-2008 3-1-08 ls 2- ujngk@ 1426 1-896 Jh jkeorkj vxzoky 20-12-2007 1-2018 vkjax gs fuoklh eafnjglkSn rglhy vkjax 63 ts- ts- ,lksfl,VsV izks- pwukiRFkj 105@2011@ 25-09-2012 25-9-2012 ujngk@ 1960 2-40 Jh /kesZUnz jke iqjh;k 11-05-2012 ls 24-9- vkjax ,dM+ fuoklh & ykyiqj 2022 jk;iqj 64 'kadj b.MLVªht pwukiRFkj 112@07@ 17-08-2007 17-8-2007 ujngk@ 1951] 1-991 jkts’k iVsy fuoklh 07-08-2007 ls 16-8- vkjax 1952@2] gsDVj QkQkMhg] jk;iqj 2017 1953@2] 1954@3 65 Jh dqychj flag vk- pwukiRFkj 10@2008@ 17-03-2008 17-3-2008 ujngk@ 2001@1]2] 0-769 15

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67 Jherh ehuk nsoh pwukiRFkj 07@2013@ 08-03-2014 08-03-2014 ujngk@ 1962 3-50 ctkt] 27-02-2015 ls 07-03- vkjax ,dM+ ifr Jh pqUuhyky 2024 ctkt] fuoklh & QkQkMhg jk;iqj 68 Jh v’kksd ctkt] pwukiRFkj 89@2011@ 07-01-2013 07-01-2013 ujngk@ 1993@1] 4-92 vk- Jh eaxwey ctkt] 27-02-2015 ls 06-01- vkjax 2] 3 ,dM+ fuoklh %& QkQkMhg 2023 jk;iqj 69 Jh v’kksd ctkt] pwukiRFkj 26@2013@ 06-07-2014 06-07-2014 ujngk@ 1987] 1-888 vk- Jh eaxwey ctkt] 19-02-2014 ls 05-07- vkjax 1989] gs- fuoklh %& QkQkMhg 2024 1990] jk;iqj 1991] 1992] 1993@3] 1995@1 70 esllZ ,l-,l- LVksu pwukiRFkj 21-01-2014 22-01-2014 22-01-2014 ujngk@ 2002@2 3-34 ekbZu izks- Jh v{k; ls 21-01- vkjax ,- dqekj JhokLro 2024 71 Jh t; dqekj ctkt pwukiRFkj 106@2006@ 08-12-2007 08-12-2007 eafnjglkS 862@2]4]8 2-442 vk- Jh eaxwey fu- 29-03-2007 ls 7-12- n@vkjax 63] 864] gs- QkQkMhg jk;iqj 2017 865] 866@1] 866@3] 868@1]2] 869 72 Jherh Hkxorh nsoh pwukiRFkj 233@2006@ 06-01-2008 6-1-2008 ls eafnjglkS 876@1]2 4-60 fizrokuh ifr Lo Jh 29-05-07 5-1-2018 n@vkjax 876@18] ,- vtqZu dqekj fizrokkuh 879 fuoklhvktkn pkSd Fkkuk ls ikl jk;iqj 73 Jherh yhyk csu pwukiRFkj 38@2012@ 12-11-2012 12-11-2012 eafnjglkS 553@1] 3-36 , iVsy ifr Lo- fot; 26-10-2012 ls 11-11- n@vkjax 653@3 iVsy fuoklh 2022 QkQkMhg jk;iqj 74 Jh usoUnjke NkcfM+;k pwukiRFkj 08@2011@ 07-02-2012 7-2-2012 ls eafnjglkS 709@3 3-50 , vk- yksdwey fuoklh 31-03-2011 6-2-2022 n@vkjax yk[ksuxj jk;iqj 75 Jherh fuf/k ikaMs ifr pwukiRFkj 51@2011@ 01-08-2012 01-9-2012 eafnjglkS 709@1]5] 4-85 , Jh th-,y- ikaMs 30-08-2012 ls 31-08- n@vkjax 711@4]5 fuoklh lqanj uxj 2017 jk;iqj 76 Jh panzgkl ikaMs pwukiRFkj 52@2011@ 26 -02 -2014 28 -07 - eafnjglkS 721@1] 1-94 fuoklh& jk;iqj 18-02-2014 2012ls 27- n@vkjax 721@2] ,dM+ 07-2022 722] 749

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105 ek inekorh ekbUl pwukiRFkj 35@2006 09-04-2007 9-4-2007 ls /kulwyh 982 2-04 , izks ekyrh tSu ifr 10-07-2006 8-4-2017 @vkjax Jh lh-ih- tSu fuoklh nsosUnz uxj jk;iqj 106 Jh pqUuh yky ctkt pwukiRFkj 48@2011 18-05-2012 18-5-2012ls /kulwyh 665] 669 2-80 , vk- Jh eaxywey 20-04-2012 17-5-2022 @vkjax ctktfuoklh QkQkMhg jk;iqj 107 Jh jes'k dqekj iVsy pwukiRFkj 29 ch@2011 12-09-2012 12-9-2012 /kulwyh 655@2 1-60 , vk- Jh thojke HkkbZ 03-01-2012 ls 11-9- @vkjax iVsy fu- U;w fVEcj 2022 eklsZV QkQkMhg jk;iqj 108 Jherh m"kk tXxh ifr pwukiRFkj 197@2006@ 08-14-2007 8-1-07 ls /kulwyh 917] 918 1-255 Jh lqjsUnz iky tXxh 07-02-2007 7-1-2017 @vkjax gs fuoklh 'kSysUnz uxj jk;iqj 109 vCnqy efyd vk- Lo- pwukiRFkj 206@2006@ 19-01-2007 19-1-07 ls /kulwyh 705] 706] 1-60 gs Jh eqlkHkkbZ fuoklh 03-02-2007 18-1-2017 @vkjax 716 31 xksYMu gksEl [kEgkjMhg jk;iqj 110 Jh ukjk;.k HkkbZ iVsy pwukiRFkj 74@2007@ 14-08-2007 14-8-07 ls /kulwyh 877 0-36 gs vk- Jh dkarhHkkbZ 19-07-2007 13-8-2017 @vkjax fuoklh QkQkMhg jk;iqj 111 Jhefr nqxsZ’k 'kqDyk pwukiRFkj 83@2011@ 01-12-2011 01-12-2011 /kulwyh 984 2-800 ifr 'kjn 'kqDyk 24-11-2011 ls 30-11- @vkjax jk;iqj 2021 112 Jh ukses’k dqekj pwukiRFkj 31-01-2014 31-01-2014 /kulwyh 762] 764] 1-060 psyd firk Jh jru ls 30-01- @vkjax 765] 766] gs yky psyd fuoklh 2024 767 /kulqyh iks- ujngk rglhy vkjax ftyk jk;iqj 113 uRFkqyky Hkxokunkl pwukiRFkj 219@2009@ 02-12-2009 02-12-2009 /kulwyh 896 0-740 izks- Jherh d`".kk 19-11-2009 ls 3-12- @vkjax vxzoky 2019 114 fcVqesd daLVªD’ku izks- pwukiRFkj 96@2011@ 14-05-2012 14-05-2012 /kulwyh 923 4-60 Jh vfuy tlokuh 04-05-2012 ls 13-05- @vkjax ,- iaMjh jk;iqj 2022

115 Jh fou; dqekj pwukiRFkj 65@2012@ 16-01-2014 16-01-2014 /kulwyh 916@3] 1-090 ctkt ls 15-01- @vkjax 917@1 gsDVs;j 2024

116 ljLorh LVksu izks- pwukiRFkj 17-01-2013 17-01-2013 /kulwyh 872 4-35 t;arhyky iVsy vk- ls 16-01- @vkjax ,dM+ Jh y[ku fuoklh 2023 Hkuiqjh jk;iqj 117 Jh jes'k iVsy vk- Jh pwukiRFkj 22@2006@ 14-02-2007 14-2-2007 vdksyMh 543 1-000 /khjth HkkbZ fuoklh 09-02-2007 ls 13-2- g QkQkMhg jk;iqj 2017 [kijh@ vkjax 118 Jh _rqi.kZ xqIrk vk- pwukiRFkj 43@06 22-06-2006 22-6-2006 vdksyMh 129] 142 1-88, Jh lrh"k dqekj fu- 08-06-2006 ls 21-6- g U;w 'kkafr uxj jk;iqj 2016 [kijh@ vkjax 119 Jh deys’k iVsy vk- pwukiRFkj 181@06 05-06-2007 5-6-07 ls vdksyMh 544 Vq 0-769 Jh t;arh yky iVsy 10-04-2007 4-6-2017 g gs fuoklh Hkuiqjhjk;iqj [kijh@ vkjax 120 NRrhlx< fjlksZlsl pwukiRFkj 182@2007@ 04-02-2008 4-2-2008 ls vdksyMh 500] 501] 8-00 ikV- lat; vxzoky 11-01-2008 3-2-2018 g 573] ,dM+ dkafruxj fcykliqj [kijh@ 577]578 vkjax 121 Jh eaxy HkkbZ iVsy pwukiRFkj 35@2008@ 11-04-2008 11-4-08 ls vdksyMh 546@1] 1-676 vk- Jh ckykth HkkbZ 01-04-2008 10-4-2018 g 547@2 gs fuoklh LVsV cSad [kijh@ dkWyksuh QkQkMhg vkjax jk;iqj 122 Jh ftrsUnz dqekj pwukiRFkj 34@2008@ 26-04-2008 26-4-08 ls vdksyMh 547@1] 1-318 iVsy vk- Jh t;arh 01-04-2008 25-4-2018 g 548] 549 gs HkkbZ iVsy fuoklh [kijh@ ljnkj fVEcj eklsZV vkjax jk;iqj 123 Jherh nhfidk iVsy pwukiRFkj 212@2009@ 07-12-2009 7-12-2009 vdksyMh 553@2 1-460 ifr Jh furqu iVsy 20-11-2009 ls 6-12- g gs- fu- ckykth xkMZu U;w 2019 [kijh@ fVEcj eklsZV jk;iqj vkjax 124 e.khyky iVsy vk-Jh pwukiRFkj 214@2009@ 07-12-2009 7-12-2009 vdksyMh 553@1 1-040 f'kox.k iVsy fu- U;w 20-11-2009 ls 6-12- g gs- fVEcj eklsZV 2019 [kijh@ QkQkMhg jk;iqj vkjax 125 vksfl;u LVksu izk-fy- pwukiRFkj 33@2009@ 06-04-2009 6-4-2009 ls vdksyMh 603] 2-458 Mk;- fodkl vxzoky 28-02-2009 5-4-2019 g 633@4]5] gs- fu- eksgkikyh jksM rg- [kijh@ 635] 638] [kjfl;k vkjax

126 Jh eunhi vjksjk vk- pwukiRFkj 01-09-2014 01-09-2014 01-09-2014 vdksyMh 539 3-00 Jh ljnkj dqanu flag ls 31-08- g ,dM+ fu-& rsyhcka/kk jk;iqj 2024 [kijh@ vkjax 127 d`".kk esVy odZ ikVZ- pwukiRFkj 11@2012@ 05-07-2012 05-07- vdksyMh 331@1]2] 1-500 Jherh fdj.k xqIrk 23-06-2012 2012ls 4- g 332] 340] gsDVj

fuoklh 'kadj uxj 07-2022 [kijh@ 342 jk;iqj vkjax 128 jktdey fcYMlZ izk- pwukiRFkj 43@2012@ 05-11-2012 05-11- vdksyMh 618] 619] 1-20 fy- Mk;- Jh vfiZr 30-10-2012 2012ls 4- g 620] 621] ,dM lqjkuk fuoklh fcYMlZ 11-2022 [kijh@ 622] 623 dkyksuh bankSj vkjax

129 eksgEEn vyrkQ fi- pwukiRFkj 63@2010@ 06-01-2012 06-01-2012 vdksyMh 386] 387] 0-820 Jh vCnqygd fuoklh 28-11-2011 ls 05-1- g 477 gs- tsy jksM lkbZ uxj 2022 [kijh@ jk;iqj vkjax

130 vxzlsu feujYl pwukiRFkj 02@2013 06-02-2014 06-02-2014 vdksyMh 505] 511 1-640 Hkkxhnkj QeZ }kjk] ls 05-02- g gsDVj Hkkxhnkj Jh lquhy 2024 [kijh@ vxzoky] fuoklh & vkjax 'kkWi ua- 214A f}rh; ry] _"kHk psacj] ,e- th- jksM+ jk;iqj 131 Jh izoh.k vxzoky vk- pwukiRFkj 99@2007@ 14-08-2007 14-8-07 ls ipsM+k@ 1214 0-280 Jh vkuan Lo:i fu- 17-09-2007 13-8-2017 vkjax ek:rh fogkj jk;iqj 132 Jherh T;ksfr vxzoky pwukiRFkj 44@2007@ 07-05-2009 7-5-2009 ls ipsM+k@ 1162 0-809 ifr Jh Lo=ar izdk'k 16-12-2008 6-5-2019 vkjax gsDVj vxzoky fu- ,pvkbZth ls DVj&1 'kadj uxj jk;iqj 133 esllZ Jh vkuan LVksu pwukiRFkj 08-05-2012 08-05- ikjkxkao 1859 2-39 b.MLVªht izks- Jherh 2012ls 7- @vkjax ,- liuk fla?kkfu;k 05-2022 fuoklh ikjkxkao 134 Jh vejnkl vk- Jh pwukiRFkj 84@07@ 11-03-2008 11-3-08 ls fulnk@ 197 0-480 egkohj dqjsZ fuoklh 14-02-2008 10-3-2018 vkjax vkekflouh 135 Jh lat; ;kno vk- pwukiRFkj 188@2007 01-05-2008 1-5-08 ls fulnk@ 1345 2-30 , Jh bUnzdqekj ;kno 08-04-2008 30-4-2018 vkjax fu- jk;iqj 136 Jh izHkkr feJk vk- pwukiRFkj 199@2006@ 17-11-2007 17-11-07 ls fulnk@ 1344 0-145 ,l-,u- feJk fuoklh 25-10-2007 16-11-2017 vkjax gs fl)kFkZ pkSd fVdjkikjk jk;iqj 137 Jh larks"k ;kno fu- pwukiRFkj 188@2007@ 01-12-2010 1-12-2010ls fulnk@ 1344 0-920 fulnk 08-04-2008 30-11-2020 vkjax

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 izkIr jktLo dh tkudkjh ;ksx izkfIr dk

y{; eq[; [kfut xkS.k [kfut izfr’kr

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 xzke [kljk jdck i;kZoj.k Dyh;jsal (MOEF) [knku [kuu dh fjekdZ dk uke iapk;r ua- vkns'k Øa- izfr lapkyudrkZ vof/k @ @fnukad o"kZ fodkl[ka [kuu M ek=k ¼?ku eh- esa½ 1 Ikkjkxkao ikjkxkao 1598@ 2-000 gs- 905 @21-11-2013 50000 tuin 21-11-2013 ls lapkfyr ¼Mh½ @vkjax 1872 iapk;r vkjax 20-11-2016 2 fp[kyh ¼,½ fp[kyh@ 1445 4-000 gs- 907@21-11-2013 tuin 21-11-2013 ls lapkfyrA vkjax 100000 iapk;r vkjax 20-11-2016 3 pijhn ¼,½ pijhn@ 1509 4-000 gs- 1194@06-12-2013 tuin 06-12-2013 ls lapkfyrA vkjax 100000 iapk;r vkjax 05-12-2016 4 xqYyq ¼,½ xqYyw@vk 3009 50-00 ,- 1192@06-12-2013 tuin 06-12-2013 ls lapkfyrA jax 500000 iapk;r vkjax 05-12-2016 5 dq:n ¼,½ dqVsyk@ 2742 2-000 gs- 1209@07-12-2013 50000 tuin 07-12-2013 ls lapkfyrA vkjax iapk;r vkjax 06-12-2016 6 xqnxqnk ¼,½ vesBh@ 436 4-000 gs- 1205@07-12-2013 100000 tuin 07-12-2013 ls lapkfyrA vkjax iapk;r vkjax 06-12-2016 7 dqEgkjh ¼,½ dqEgkjh@ 1882 4-000 gs- 1203@07-12-2013 100000 tuin 07-12-2013 ls lapkfyrA

vkjax iapk;r vkjax 06 -12 -2016 8 jkVkdkV¼,½ jkVkdkV 887 4-000 gs- 1201@07-12-2013 100000 tuin 07-12-2013 ls lapkfyrA @vkjax iapk;r vkjax 06-12-2016 9 gjnhM+hg dkxnsgh 1221 4-00 gs- 1221@07-12-2013 100000 tuin 07-12-2013 ls lapkfyrA ¼,½ @vkjax iapk;r vkjax 06-12-2016 10 xqnxqnk ¼ch½ vesBh@ 436 2-000 gs- 1362@23-12-2013 50000 tuin 23-12-2013 ls lapkfyrA vkjax iapk;r vkjax 22-12-2016 11 dksy;kjh dksy;kjh¼ 766 6-000 gs- 1219@07 -12 -2013 tuin 07 -12 -2013 ls lapkfyrA ¼,½ y[kuk½@ 150000 iapk;r 06-12-2016 vHkuiqj vHkuiqj 12 y[kuk ¼,½ y[kuk@ 866 3-000 gs- 1196@06-12-2013 75000 tuin 06-12-2013 ls lapkfyrA vHkuiqj iapk;r 05-12-2016 vHkuiqj 13 Vhyk Vhyk@v 1891 6-00 gs- 4058@30-11-2015 108000 xzke iapk;r 18-05-2015 ls lapkfyrA Hkuiqj 90000 Vhyk 15-10-2015 30-11-2015 ls 29-11-2017 14 fp[kyh ¼ch½ fp[kyh@ 1127 5-40 gs- 2022@07-08-2014 120000 xzke iapk;r 07-08-2014 ls lapkfyrA vkjax 424@12-05-2015 fp[kyh 31-03-2015 4964@14-03-2016 81000 01-04-2015 ls 15-10-2015 14-03-2016 ls 13-03-2018 15 pEikj.k ¼,½ pEikj.k 3009 15-00 gs- 229@01-05-2014 252000 tuin 01-05-2014 ls lapkfyrA @vHkuiq 1511@11-06-2015 iapk;r 31-03-2015 j 4981@14-05-2016 150000 vHkuiqj 01-04-2015 ls 15-10-2015 14-03-2016 ls 13-03-2018 16 fulnk ¼,½ fulnk@ 1351 6-40 gs- 569@06-06-2014 75000 xzke iapk;r 06-06-2014 ls lapkfyrA vkjax 1704@12-06-2015 fulnk 31-03-2015 5043@17-03-2016 50000 01-04-2015 ls 15-10-2015 17-03-2016 ls 16-03-2018 17 fp[kyh fp[kyh@ 1127 11-64 gs- 958@05-08-2014 230472 xzke iapk;r 05-08-2014 ls lapkfyrA ¼lh½ vkjax 1441@28-04-2015 fp[kyh 31-03-2015 5091@21-03-2016 170000 01-04-2015 ls 15-10-2015 21-03-2016 ls 20-03-2018 18 dqEgkjh ¼ch½ dqEgkjh@ 1882 15-00 gs- & & & & [kuu ;kstuk vkjax vuqeksfnr dj izsf"krA 19 Nqyuk nqyuk@ 1728] 10-40 gs- & & & & [kuu ;kstuk vHkuiqj 1729 vuqeksfnr dj izsf"krA 20 gjnhMhg dkxnsgh 703 11-50 gs- & & & & [kuu ;kstuk ¼ch½ @vkjax vuqeksfnr dj izsf"krA 21 gjnhMhg dkxnsgh 190 20-50 gs- & & & & [kuu ;kstuk ¼lh½ @vkjax vuqeksfnr dj 23

izsf"krA 22 dkxnsgh dkxnsgh 2400 24 -00 gs- & & & & [kuu ;kstuk @vkjax vuqeksfnr dj izsf"krA 23 eqUMjk eqUMjk@ 1 5-00 gs- & & & & [kuu ;kstuk vHkuiqj vuqeksfnr dj izsf"krA 24 jkVkdkV jkVkdkV 887 12 -50 gs- & & & & [kuu ;kstuk ¼ch½ @vkjax vuqeksfnr dj izsf"krA 25 laqxsjk ¼,½ lqaxsjk@f 231 5-00 gs- 441@24-05-2014 100000 xzke iapk;r 24-05-2014 ls vuqeksfnr [kuu rYnk 499@12-05-2015 lqaxsjk 31-03-2015 ;kstuk vkWuykbZu 01-04-2015 ls fnukad 07-10-2015 15-10-2015 dks izsf"krA

26 ikjkxkao ikjkxkao 1225 10-00 gs- 251@01-05-2014 185250 tuin 01-05-2014 ls vuqeksfnr [kuu ¼ch½ @vHkuiq 1686@11-06-2015 iapk;r 31-03-2015 ;kstuk vkWuykbZu j vHkuiqj 01-04-2015 ls fnukad 31-10-2015 15-10-2015 dks izsf"krA

27 vesBh ¼,½ vesBh@ 1107 5-00 gs- 2070@07 -08 -2014 100000 xzke iapk;r 07 -08 -2014 ls vuqeksfnr [kuu vkjax vesBh 31-03-2015 ;kstuk vkWuykbZu fnukad 13-01-2016 dks izsf"krA 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 530 15-00 gs- & & & & vuqeksfnr [kuu @vkjax ;kstuk vkWuykbZu fnukad 13-01-2016 dks izsf"krA 30 dqEgkjh dqEgkjh@ 1 14 -00 gs- & & & & vuqeksfnr [kuu /kjlhaok ;kstuk vkWuykbZu fnukad 14-01-2016 dks izsf"krA 31 xkSjHkkB ¼,½ xkSjHkkB@ 1869 7-00 gs- 253@01-05-2014 126000 xzke iapk;r 01-05-2014 ls vuqeksfnr [kuu vkjax 1294@28-04-2015 xkSjHkkV 31-03-2015 ;kstuk vkWuykbZu 01-04-2015 ls fnukad 18-05-2016 15-10-2015 dks izsf"krA 32 [kV~Vh [kV~Vh@ 108 5-00 gs- & & & & [kuu ;kstuk vHkuiqj vuqeksfnrA 33 [kSj[kqV ¼,½ cykSnh[kq 1 o 227 13-00 ,- 249@01-05-2014 125000 xzke iapk;r 01-05-2014 ls [kuu ;kstuk nZ@frYnk 517@12-05-2015 [kSj[kqV 31-03-2015 vuqeksfnrA 01-04-2015 ls 15-10-2015 34 Ikkjkxkao ikjkxkao@ 1598@1 22-50 gs- 897@18-05-2015 558421 xzke iapk;r 18-05-2015 ls [kuu ;kstuk ¼ch½ vkjax 872] ikjkxkao 15-10-2015 vizkIrA 1862 35 Ikkjkxkao ikjkxkao@ 1127 11-64 gs- & & & & [kuu ;kstuk ¼,½ vHkuiqj vizkIrA 36 Leksnk leksnk@v 1260 5-00 gs- & & & & [kuu ;kstuk kjax vizkIrA 37 Josyh josyh@vHk 1 5-00 gs- & & & & [kuu ;kstuk uiqj vizkIrA 38 yedsuh yedsuh@ 1 10 -16 gs- & & & & [kuu ;kstuk ¼,½ vHkuiqj vizkIrA 39 Lsaejk lsejk@vHk 998 5-00 gs- & & & & [kuu ;kstuk uiqj vizkIrA 24

40 Cxnsgh cxnsgh@v 503 5-00 gs- & & & & [kuu ;kstuk Hkuiqj vizkIrA 41 csUnzh csUnzh@/kj 80 5-00 gs- & & & & [kuu ;kstuk lhaok vizkIrA 42 cjrukjk cjrukjk@ 238] 68] 10 -00 gs- & & & & [kuu ;kstuk ¼,½ /kjlhaok 79 vizkIrA 43 Cgslj cgslj@/kj 1 5-00 gs- & & & & [kuu ;kstuk lhaok vizkIrA 44 cykSnh cykSnh@fr 1 5-00 gs- & & & & [kuu ;kstuk Ynk vizkIrA 45 y[kuk y[kuk@fr 9 5-00 gs- & & & & [kuu ;kstuk Ynk vizkIrA 46 Eksgesyk dkxnsgh@ 283 12-00 gs- & & & & [kuu ;kstuk vkjax vizkIrA

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

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 26

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.

7. General Profile of the District

S.No. Particulars Statistics 1 General Information Geographical Area 12383 km 2 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 (Km 2) 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 361878790 Minerals in 2015-16 Total No. Notified Sand Leas e 46 Total Area of Sand Leases 419.64

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 Total No. of Forest 6 Compartment 12383 Sq. Km. Total Division Area of 29528 Sq. Km. 10.538 Sq. Km. 7 1.581 Sq. Km. 17.409 Sq. Km. Total Forest of (A) Reserved Forest (R.F.) 8 (B) Protected Forest (P.F.) (C ) Mixed Forest

0% % of Forest Cover of Division Sq.Km. 9 Sq.Km. 15.457 Sq.Km. Area Under 4863872 (A) Teak Forest Male 2018186 10 (B) Sal Forest Female 201586 (C ) Mixed Forest Population of the Division (As 4063872 11 Per 2011 Census Male 2048186 Female 201586 (A) No. of JFM commitees (B) Member of JFM Commitees 06 12 Male - 734 Female - 731

Division Headquarter, Road type and Forest map of Raipur District

ii) Harticulture,Agriculture and Irrigaton :-

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VEGETATION MAP OF RAIPUR DISTRICT

iii) River s: -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

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 m 3 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 :-

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 Connecting cities number

Hajira-Dhule-Nagpur-Raipur- Mahasamund - Sambalpur -

NH 6 Baharagora-Calcutta

Raipur-Vizianagaram Junction with National Highway No. 5 near NH 53 Natavalasa

Raipur-Bilaspur-Raigarh-Kanaktora-Jharsuguda-Kochinda-

NH 200 Deogarh-Talcher-Chandhikhol

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

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

IndiGo hennai

Jet Delhi, Mumbai, Bhopal

Airways

Vistara in future

Spicejet in future

Air Asia in future

India

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.

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

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).

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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

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.

The geological succession of Raipur Region

Intrusives Dolerite dykes CHHATTISGARH RAIPUR Manairi Purple shale with dolomite, GROUP GROUP Formation (70m) dolomitic limestone and gypsum Hirri Formation Grey dolomite, argillaceous (70m+) dolomite Tarenga Bilha Member Purple dolomitic argillite Formation(180m) Dagauri Member Green clay, chet and shale intercalation (tuffaceous?) Kusmi Member Chandi Formation Nipania Member Purple and bedded limestone (67m) Purple argillaceous stromatolitic dolomite Pendri/Deodonger Purple and grey stromatolitic Member limestone and dolomite with flaggy limestone-shale intercalation/ferruginous glauconitic arenite and shale Gunderdehi Newari Member Pink and buff stromatolitic Formation limestone and dolomite Andha/Dotopar Predominantly pink, purple and Member grey shale with limestone intercalations/arenite/buff to green shale member in the middle Charmuria Bagbura Member Purple limestone (phosphatic) Formation (490m) 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

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:

Super Age 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 pockets of intra - R fromational conglomerate,buff and O purple U calcareous shale. P Charmuria Pinkish and gray limestone Dark Grey bedded limestone Grey shaly limestone, light Grey limestone.

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.

Geology and Mineral Map of Raipur District, Chhattisgarh

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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