District Survey Report Balod (Chhattisgarh) As Per Notification No

2019

DISTRICT SURVEY REPORT BALOD (CHHATTISGARH) AS PER NOTIFICATION NO. S.O. 3611(E), NEW DELHI, 25TH JULY, 2018 OF MINISTRY OF ENVIRONMENT, FOREST AND CLIMATE CHANGE

DIRECTORATE OF GEOLOGY AND MINING MINERAL RESOURCES DEPARTMENT GOVT. OF CHHATTISGARH

DGM

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 MAP

1. INTRODUCTION The Balod district is one of the densely populated and situated in the central part of the Chhattisgarh State covers an area of 3527 sq km. It falls in Survey of India Degree Sheet Nos. 64C, 64D, 64G and 64H bounded by latitude 20°23' to 21°03' N and longitude 80°48' to 81°30 E. It is surrounded by Durg districts in the north, Rajnandgaon District in the west, Dhamtari district in the east and Kanker district in the south.

Balod is the district headquarters and is well connected by road and railway. National Highway No. 930 and connects Balod with Dhamtari. Balod is also connected by road with Dalli Rajhara, Doundi - Lohara, Bhanupratappur, Gurur, Dhamtari, Rajnandgaon, Gunderdehi and Durg with the other important towns in the district.

According to Notification of Environment, Forest and Climate Change Ministry, Goverment of India dated 25 July 2018, as prescribed in Para 7(iii) and Annexure (x); District Survey Report has been prepared.

District Survey report will be prepared in every district for Sand mining or River bed mining and other small minerals mining. The main purpose of preparation of district survey report is to identify the land increase or depositional areas and its infrastructure, Structure and installation distance from where the mining is prohibited and recalculation of annual replenishment and time required for replenishment after mining.

This District Survey report contains mainly Geology Mineral wealth details of rivers, Details of Lease and Mining activity in the District along with Sand mining and revenue of minerals.

This report also contains details of Forest, Rivers, Soil, Agriculture, Road, Transportation climate etc.

The district survey report will be based for evaluation of the application for project and environment clearance of mining activity in the district.

2. OVERVIEW OF MINING ACTIVITY IN THE DISTRICT

Balod District is important district for Iron Ore deposite in Chhattisgarh. The Minor Mineral is Low grade Limestone, Flagstone, Laterite, Sandstone, Quartzite and Quartz. Mineral Sand is also found in huge quantity in river and nala flowing in district. Total 54 Leases are given in the district. Four Mining leases of Major Mineral of Iron Ore at Doundi Tehsil. 49 Quarry leases of Minor Mineral Deposit those 10 Quarry Leases for limestone and 33 Quarry Leases for Flagstone are given for road and building material in different villages of Gunderdehi and Doundi - Lohara Tehsil.Other Minor Mineral Leases for soil for making bricks in killn at villages Devri, Baghmara, Doundi – Lohara, Khursuni, Limora etc. In all total 06 Leases are given for soil in the district for brick making in killn. Temperory Permit leases of mururm are also given in this district.

44 Ret Ghat for sand mining on the bank of Sukha nala and Tandula River have been senctioned at different villages for sand mining.

Approximately 78932.70 lakh Rupees royalty is earned from all minerals in the district in the last three years, out of which 78520.36 lakh from major minerals and 412.31 lakh from minor minerals.

State Government, is carrying on various Infrastructure development projects in all district , like Narva , Gauthan, Rain Water Harvesting System, Dams, Over bridge, Anicut on rivers/nala, approach roads etc. , all above civil works require Sand in different site which is in huge quantity in the district.

3. LIST OF MINING LEASES/ QUARRY LEASES/ SAND LEASES THE DISTRICT WITH LOCATION, AREA AND PERIOD OF VALIDITY lwph%& ¼d½ [kfut@ykSg v;Ld [kfuiV~Vks dh lwph

dz0 iV~Vsnkj dk uke [kfut xzke rglhy [kljk ua0 jdck iV~Vs dh vof/k ,oa ¼gsDVj esa½ irk

1 2 3 4 5 6 7 8 fHkykbZ bLikr ykSg iaMjh dIikVZ esaV ua0 142]143 1- la;a=] v;Ld nYyhjktgjk MkS.Mh 27-04-2003 ls 220-42 gs0 fHkykbZ igkM 26-04-2023 fHkykbZ bLikr ykSg nYyh QkjsLV 2- la;a=] MkS.Mh dIikVZ esaV ua0148]149]170 21-08-2003 ls v;Ld 100-00 gs0 fHkykbZ 20-08-2023 fHkykbZ bLikr dIikVZ esaV ua0 ykSg 3- la;a=] jktgjk fgYl MkS.Mh 142]143]144]145]146]148]1 01-06-2003 ls v;Ld 719-60 gs0 fHkykbZ 49 31-05-2023 fHkykbZ bLikr ykSg egkek;k dIikVZ esaV ua0 4- la;a=] MkS.Mh 04-11-2001 ls v;Ld nqYdh 158]159]160]879]880]881 1522-67gs0 fHkykbZ 03-11-2021

¼[k½ pwukiRFkj [kfuiV~Vks dh lwph dz- iV~Vsnkj dk uke xzke rglhy [kljk ua0 {ks=Qy [kfut Lohd`r vof/k ,oa iw.kZ irk gs0 esa 1 2 3 4 5 6 7 8 1 Jh gjh'k HkkbZ pkoMk vk0 Jh Pkkjkpkj xq.Mjnsgh 273@8] 73@13] 1-80 gs0 pwukiRFkj 11-02-2010 ls n;kjke pkoMk fu0 xq.Mjnsgh 273@14] 3@18] 10-02-2040 ftyk ckyksn 273@19] 73@7 2 Jh chjHkku fVyokuh fu0 pkjkpkj xq.Mjnsgh 273@3]4]5]6 Hkkx] 1-16 gs0 pwukiRFkj 24-10-2009 ls izksQslj dkyksuh jk;iqj 274@9 Hkkx 23-10-2039 3 Jh gjh'k dqekj lksudj fu0 pkjkHkkBk xq.Mjnsgh 66] 67] 69] 70 0-258gs0 pwukiRFkj 12-04-2010 ls xq.Mjnsgh 11-04-2040 4 Jh fnus'k pan u[kr vk0 Jh fiudkikj MkS.Mh 1265 0-49 gs0 pwukiRFkj 02-07-2007 ls xqykc pan u[kr fu0 lnj yksgkjk 01-07-2037 ykbZu Mksxjxkao fu0 jktukanxkao

5 Jh nkus'oj oekZ vk0 Jh fryksnk xq.Mjnsgh 309@1 Hkkx 1-50 gs0 pwukiRFkj 21-08-2003 ls dstwjke oekZ fu0 xzke cksny 20-08-2033 rg0 ikVu ftyk ckyksn 6 jkseuyky Bkdqj] fu0 xzke cjcliqj xq.Mjnsgh 904] 906] 907] 910] 1-47 gs0 pwukiRFkj 20-10-2011 ls fppyxksanh] rg0 xq.Mjnsgh 911] 912] 913 19-10-2041 7 ftrsUnz dqekj tSu] fu0 xzke cjcliqj xq.Mjnsgh 887@2 1-82 gs0 pwukiRFkj 13-09-12 ls cjcliqj] rg0 xq.Mjnsgh 12-09-22

8 Jh deys'k ikM+s vk0 Jh fryksnk xq.Mjnsgh 292] 293@1] 390@2 4-83 gs0 pwukiRFkj 12-01-2018 ls xksiky ikM+s] fuoklh 11-01-2048 dksfygkiqjh] ftyk nqxZ

9 Jh jkepj.k fljnkj fu0 fiudkikj MkS.Mh 1117] 1122@1&2] 0-57 gs0 pwukiRFkj 06-05-2010 ls QxMwVksyk rg0 Nqfj;k ftyk yksgkjk 1124] 1125 05-05-2040 jktukanxkao 10 Jh fclsyky vk0 Jh gjhyky pkjkHkkBk xq.Mjnsgh 95@1] 95@2 0-63 gs0 pwukiRFkj 15-09-2007 ls lkgw fu0 xzke pkjHkkBk rg0 14-09-2037 xq.Mjnsgh ftyk ckyksn

¼x½ [kfut feV~Vh ¼bZV fuek.kZ gsrq½ mR[kfuiV~Vksa dh lwph& dz- iV~Vsnkj dk uke xzke rglhy [kljk ua0 {ks=Qy [kfut Lohd`r vof/k ,oa iw.kZ irk gs0 esa 1 2 3 4 5 6 7 8 1 Jh vfuy dqekj pkoM+k vk0 Jh fyeksjk xq.Mjnsgh 278] 281]282]288] 30-09-1997 ls n;kjke 284@2] 1-38 gs0 feV~Vh 29-09-2027 289]290]291]294 2 Jherh y{eh nsoh] ifr Jh 'kadj yky c?kejk xq.Mjnsgh 18-06-2009 ls 125]126]129]130@3] irk&okMZ ua- 27 ikVadj dkyksuh 17-06-2039 130@7]159@1]2] 2-19 gs0 feV~Vh

LVs’ku jksM ckyksn 160]161@1]2] 162

3 Jh mft;kj flag ikoj vk0 Jh lsod [kqjlquh xq.Mjnsgh flag iokj fu0 bZ ikdsV&5 ch ejksnk 20-02-2007 ls 3 Hkkx 1-00 gs0 feV~Vh lsDVj fHkykbZ 19-02-2037

4 Jh izhryky lkgw vk0 Lo0 Jh cynso c?kejk ckyksn 1571 Hkkx] 29-12-2009 ls lkgw] fu0 ghjkiqj] rg0 ckyksn ftyk 2-10 gs0 feV~Vh 1572@2Hkkx]1573 28-12-2019 nqxZ 5 Jh bUnz dqekj gYck MkSa0yks0 MkSa0yks0 01-09-2009 ls 703 0-225 gs0 feV~Vh 30-08-2019 6 Jh Nsnhyky pdz/kkjh nqxZ nssojh xq.Mjnsgh 5@2]3]4]6 3-81 gs0 feV~Vh 07-09-2005 ls 06- 09-2035

¼?k½ Q'khZiRFkj ds mR[kfuiV~Vks dh lwph

dz- iV~Vsnkj dk uke xzke rglhy [kljk uEcj {ks=Qy [kfut dk Lohd`r vof/k ,oa iw.kZ irk gs0 esa uke 1 2 3 4 5 6 7 8 Jh jkts'k dqekj ns'keq[k] fu0 19-11-2004 ls 1 fldkslk xq.Mjnsgh 961@1 Hkkx 2-36 gs0 Q'khZ iRFkj LVs'ku jksM nqxZ 18-11-2034 Jh ve`r yky flUgk] fu0 03-05-2001 ls 2 fldkslk xq.Mjnsgh 961 0-607 gs0 Q'khZ iRFkj fldkslk 02-05-2031 Jh nsoyky HkkÅ vk0 Jh 20-06-2007 ls 3 lnfy;k fu0 fldkslk fldkslk xq.Mjnsgh 960 0-56 gs0 Q'khZ iRFkj 19-06-2037 xq.Mjnsgh 368 Hkkx] es0 xqIrk ekcZYl] izks0 07-12-1996 ls 4 dqjnh xq.Mjnsgh 378 Hkkx] 0-65 gs0 Q'khZ iRFkj f'kodqekj xqIrk ckykssn 06-12-2026 379 Hkkx Jh nqokZlk izlkn nsokaxu fu0 19-11-2004 ls 5 dqjnh xq.Mjnsgh 660@2 Hkkx 2-25 gs0 Q'khZ iRFkj dqjnh 18-11-2034 Jh th VkbZYl izks0 fgEer 716ih] 737@1ih] 09-06-2005 ls 6 dqekj iVsy fu0 xzke dqjnh dqjnh xq.Mjnsgh 1-10 gs0 Q'khZ iRFkj 737@2 08-06-2035 rg0 xq.Mjnsgh fnO;k ekbZUl izks Jh vcth 633 HkkbZ vk0 Jh ykyk th HkkbZ @1]2]3]4]5]6] 02-12-2005 ls 7 dqjnh xq.Mjnsgh 1-31 gs0 Q'khZ iRFkj fu0 dqjnh rg0 xq.Mjnsgh 634 Hkkx] 01-12-2035 ftyk ckyksn 637@1]2]3]4]5 Jh d`".k dqekj lkgw vk0 Jh 302 Hkkx] 303 04-12-2004 ls 8 dqjnh xq.Mjnsgh 0-85 gs0 Q'khZ iRFkj folkSgk jke fu0 dqjnh Hkkx] 404 03-12-2034 312@1]2] 315] 18-01-2007 ls 9 Jh vjfoUn dqekj tSu dqjnh dqjnh xq.Mjnsgh 1-31 gs0 Q'khZ iRFkj 397 17-01-2037

313@1 Hkkx] Jh v'kksd flag jktiwr vk0 313@2 Hkkx] 03-03-2008 ls 10 Lo0 Jh jru jktiwr fu0 iks dqjnh xq.Mjnsgh 0-49 gs0 Q'khZ iRFkj 313@3 Hkkx] 02-03-2038 fQaxs'oj rg0 o ftyk jk;iqj 306 Hkkx Jherh dkUrk pUnzkdj ifr Jh d`".k dqekj pUnzkdj }kjk 16-05-2008 ls 11 dqjnh xq.Mjnsgh 327/2, 330, 376, 1-10 gs0 Q'khZ iRFkj dkUrk LVksu dfVZx ,.M xzke 15-05-2038 386 dqjnh ftyk ckyksn Jh ukuth HkkbZ iVsy vk0 17-02-2009 ls 12 Lo0 Lksketh HkkbZ iVsy U;w dqjnh xq.Mjnsgh 1-174 gs0 Q'khZ iRFkj 336/3 16-02-2039 fVacj ekdsZV QkQkMhg jk;iqj 29-03-2007 ls 13 Jh chjsUnz dqekj nsokaxu dqjnh xq.Mjnsgh 0-50 gs0 Q'khZ iRFkj 660/1 28-03-2037 Jh iq[kjkt tSu] dqjnh] rg- 26-04-2005 ls 14 dqjnh xq.Mjnsgh 395 0-65 gs0 Q'khZ iRFkj xq.Mjnsgh 25-04-2035 Jh ys[kjke lkgw vk0 Jh 10-10-2008 ls 15 cfyjke lkgw ¼vt; LVksu½ dqjnh xq.Mjnsgh 739] 740 0-37 gs0 Q'khZ iRFkj 09-10-2038 Ikqjkuh cLrh dksgdk

Jh ys[kjke lkgw vk0 Jh 681] 27-01-2014 ls 16 cfyjke lkgw Ikqjkuh cLrh dqjnh xq.Mjnsgh 682@1] 2] 3] 1-31 gs0 Q'khZ iRFkj 26-01-2044 dksgdk 683 Jherh uferk lkgw] ifr Jh 348] 364] 365] 27-01-2014 ls 17 [ksepan lkgw] fu0 dqjnh] dqjnh xq.Mjnsgh 0-70 gss0 Q'khZ iRFkj 369 26-01-2044 xq.Mjnsgh 350@1Hkkx] Jh psru iVsy vk0 euksgj 31-12-2011 ls 18 dqjnh xq.Mjnsgh 363@1Hkkx] 366 0-743 gs0 Q'khZ iRFkj fu0 vtqZnk rg0 xq.Mjnsgh 30-12-2041 Hkkx eks0 vfrdqn~nhu [kku vk-eks0 998 ih] 05-06-1997 ls 19 Hk.Msjk MkS0yks0 0-81 gs0 Q'khZ iRFkj ljQqjnhu [kku xq.Mjnsgh 1000] 1001@2] 04-06-2027 29-01-2002 ls 20 Jh dqys'oj izlkn panzkdj Hk.Msjk MkS0yks0 982]991@2]993Hkkx 1-73 gs0 Q'khZ iRFkj 28-01-2032 Jh vkuan dqekj tSu fu0 16-12-2004 ls 21 Hk.Msjk MkS0yks0 872@9 0-33 gs0 Q'khZ iRFkj Hk.Msjk 15-12-2034 Jh vk'kk nsoh lka[kyk ifr 01-02-2005 ls 22 Jh 'khry lka[kyk fu0 'kkarh Hk.Msjk MkS0yks0 947@1 ih 1-22 gs0 Q'khZ iRFkj 31-01-2035 dkyksuh /kerjh Jh xksiky xqIrk vk0 Jh 969@1&2] 26-06-2005 ls 23 jktsUnz xqIrk fu0 dsykckMh Hk.Msjk MkSa0 yks0 1-07 gs0 Q'khZ iRFkj 972@1&2 25-06-2035 nqxZ ckypUn ikj[k vk0 Lo0 16-02-2006 ls 24 jkeyky th fu0 dkeBh Hk.Msjk MkS0 yks0 987 0-69 gs0 Q'khZ iRFkj 15-02-2036 ykbZu jktukanxkao Jherh lhek ikj[k ¼Jh larks"k ikj[k vk0 Lo0 Jh js[k pan 18-08-2006 ls 25 Hk.Msjk MkS0 yks0 967 0-36 gs0 Q'khZ iRFkj ikj[k ½ fu0 dkeBh ykbZu 17-08-2036 jktukanxkao es0 lksuy LVksu b.MLVht izks0 fouhrk 'kekZ ifr Jh 15-10-2007 ls 26 v:.k dqekj 'kekZ fu0 Hk.Msjk MkS0 yks0 951@2] 935- 954 0-93 Q'khZ iRFkj 14-10-2037 2@333 LVsfM;e jksM dksVk jk;iqj Jh fd'kksj lpnso vk0 Jh 960] 962] 963] 15-10-2007 ls 27 eqjyh/kj lpnso fu0 uokikjk Hk.Msjk MkS0 yks0 964] 984] 985] 1-40 gs0 Q'khZ iRFkj 14-10-2037 jkfte ftyk jk;iqj 983@1] 983@4 x.kifr ik"kk.k m?kksx izks0 misUnz Mkdfj;k vk0 Jh 878@2] 27-05-2008 ls 28 Hk.Msjk MkS0 yks0 0-96 gs0 Q'khZ iRFkj izdk'k pUnz Mkdfj;k fu0 xat 874 Hkkx 26-05-2038 pkSd rg0 o ftyk nqxZ vk'kh"k tSu] es- vkjo LVksu] 949@1] 950@1] 21-10-2007 ls 29 fu0 ,e- vkbZ- th- 411 Hk.Msjk MkS0 yks0 0-96 gs0 Q'khZ iRFkj 961@2 20-10-2037 in~eukHkiqj nqxZ Jh ve`ryky tSu vk0 Jh fn0 07-10- 30 jey tSu fu0 ejdkikjk Hk.Msjk MkS0 yks0 875@1] 877 0-53 gs00 Q'khZ iRFkj 2009 ls 06- jktukanxkao 10-2019 N0x0 feujYl izks0 Jh fuys'k 969@5] 28-02-2001 ls 31 egksfc;k vk0 Jh d`".k dqekj Hk.Msjk MkS0 yks0 969@6] 0-693 gs0 Q'khZ iRFkj 27-02-2031 fuoklh iksylk; ikjk nqxZ 969@7] 969@8

Jh y[ku yky frokjh vk0 975] 979] 980] 01-05-2002 ls 32 Jh ,p-ih- frokjh fu0 fouksok Hk.Msjk MkS0 yks0 981] 991@1] 1-42 gs0 Q'khZ iRFkj 30-04-2032 uxj tquokuh ftyk ckyksn 992@2 ]995 fn- 22-02- Jh ftrsUnz dqekj

¼M-½ ftyss dh jsr [knkuksa dh lwph %&

dz0 [knkuksa dk uke xzke iapk;r [kljk dzekad jdck gs0 esa rglhy unh 1 2 3 4 5 6 7 1 is.Mjh is.Mjh 1 MkS.Mh rkanqyk 5.40 2 ipsM+k ipsM+k 1 MkS.Mh rkanqyk 6.33 3 iVsyh iVsyh 159] 160 ds Hkkx MkS.Mh rkanqyk 6.05 BsekcqtqxZ BsekcqtqxZ 392 MkS.Mh rkanqyk 4 6.94 5 /kkscuh ¼c½ /kkscuh ¼c½ 39 MkS.Mh rkanqyk 2.00 6 ?kksfV;k ?kksfV;k 36 MkS.Mh rkanqyk 1.10 7 csyksnk csyksnk 387] 463 ds Hkkx MkS.Mh lw[kk ukyk 4.65 8 eqYysxqM+k 01 eqYysxqM+k 97@3 ckyksn lw[kk ukyk 2.58 9 eqYysxqM+k 02 eqYysxqM+k 143 ckyksn lw[kk ukyk 3.78 10 iksM+ iksM+ 152 xq:j egkunh 8.00 11 ghjkiqj ghjkiqj 01] 765@1 ds Hkkx ckyksn rkanqyk 5.00 12 mejknkg mejknkg 1 ckyksn rkanqyk 5.00 13 rkanqyk c?kejk c?kejk 96 5.00 ckyksn 14 vksjek 01 vksjek 223 ckyksn rkanqyk 5.00 15 vksjek 02 vksjek 223 ckyksn rkanqyk 2.80 16 rkanqyk usokjhdyk 01 usokjhdyk 728 dk Hkkx 5.00 ckyksn 17 rkanqyk usokjhdyk 02 usokjhdyk 1 1.20 ckyksn 18 nsohuokaxkao nsohuokaxkao 1 ckyksn rkanqyk 5.00 19 rkanqyk vjkSn vjkSn 1 4.00 ckyksn 20 dejkSn dejkSn 1186 xq.Mjnsgh rkanqyk 8.00 21 eksgybZ dkasxuh 239 xq.Mjnsgh rkanqyk 5.00 22 iSjh iSjh 1 xq.Mjnsgh rkanqyk 4.00 23 pkSjsy pkSjsy 1002 xq.Mjnsgh rkanqyk 5.00 24 /kuxkao /kuxkao 896 xq.Mjnsgh rkanqyk 5.00 25 dksM+sok dksM+sok 1462 xq.Mjnsgh rkanqyk 5.00 26 eugksjk fldkslk 1 xq.Mjnsgh rkanqyk 5.00 27 [ks:n [ks:n 1466 xq.Mjnsgh rkanqyk 5.00 28 [kqaVsjh [ks:n 1031 xq.Mjnsgh rkanqyk 3.10 29 fyeksjk 1 fyeksjk 1 xq.Mjnsgh rkanqyk 5.00

30 fyeksjk 2 fyeksjk 1 xq.Mjnsgh rkanqyk 5.00 31 pUnufcjgh pUnufcjgh 1339 xq.Mjnsgh rkanqyk 5.00 32 [kqaVsjh jax [kqaVsjh jax 53 xq.Mjnsgh rkanqyk 8.74 33 lukSn lukSn 192 xq.Mjnsgh rkanqyk 6.00 34 jassxkdBsjk jassxkdBsjk 1 o 37 ds Hkkx xq.Mjnsgh rkanqyk 3.00 35 uokxkWao ¼lukSn½ uokxkWao ¼lukSn½ 499 xq.Mjnsgh rkanqyk 3.00 36 fppyxkSanh fppyxkSanh 541 xq.Mjnsgh rkanqyk 5.60 37 xq.Mnsgh xq.Mnsgh 387 xq.Mjnsgh rkanqyk 8.00 38 c?kejk c?kejk 143 xq.Mjnsgh rkanqyk 8.40 39 [kjkZ [kjkZ 971 xq.Mjnsgh rkanqyk 4.90 40 jkSuk jkSuk 582 xq.Mjnsgh rkanqyk 4.90 41 Hkjnk[kqnZ Hkjnk[kqnZ 1 xq.Mjnsgh rkanqyk 5.00 42 fHkykbZ fHkykbZ 328 xq.Mjnsgh rkanqyk 10.00 43 nsojh ¼[k½ nsojh ¼[k½ 200 xq.Mjnsgh rkanqyk 7.41 44 lyksuh fry[kSjh 491 Hkkx xq.Mjnsgh rkanqyk 5.00

¼p½ ftys esa fo|eku juj eksafYMx lsaM ds iV~Vks dh lwph %&

fujad

¼N½ ftys esa fo|eku iwosZ{k.k vuqKfIr dh lwph %&

fujad

4. DETAILS OF ROYALTY OR REVENUE RECEIVED IN LAST THREE YEARS MAJOR AND MINOR MINERALS

Details of Royalty or Revenue Received in Last Three Years of Major Mineral

S.No. Mineral Royalty or Revenue Received 2016-17 2017-18 2018-19 1 Irone Ore 1729727704 2730011400 3392296673

Total - 1729727704 2730011400 3392296673

Details of Royalty or Revenue Received in Last Three Year s of Minor Mineral

S.No. Mineral Royalty or Revenue Received 2016-17 2017-18 2018-19 1 Limestone 3694700 2253800 4686692 2 Flagstone 1720985 2264606 2421350 3 Ordinary Stone 2781740 2042360 1818700 4 Murum 1529000 1566000 1655000 5 Soil 218800 229745 413920

Total - 9945225 8356511 10995662

5. DETAILS OF PRODUCTION OF ORDINARY SAND OR BAJARI IN LAST THREE YEARS

¼aA½ Details of Royalty of Orinary Sand in Last Three Years

S.No. Financial year Royalty Received in Rs. 1 2016-17 3627700 2 2017-18 6519770 3 2018-19 1786575

¼B½ Details of Production of Orinary Sand in Last Three Years

S.No. Financial year Production of Sand (in CuM) 1 2016-17 181385.00 2 2017-18 325988.50 3 2018-19 35731.50

6. PROCESS OF DEPOSITION OF SEDIMENTS IN THE RIVERS

Sendimentation of rivers of District

Process of river sedimentation:- What is erosion? Erosion is natural process, wathering, corrosion, or abrasion can reduce a material into smaller particles. Normally, these smaller units are relocated by water, wing, ice, or man. Erosion removes tosoil, organic material, and other valuable resources.

What is sedimentation? Once a material is broken free of the larger mass, it can be carried away and deposited elsewhere. This process of depositing eroded material is known as sedimentation. Some indications of sedimentation are sand dunes, mud in the street around drains, and decreased water holding capacity of stream, reservoir, or pond.

Why should we be concerned about erosion and sedimentation? Sediment is responsible for more stream and river degardation than any other pollutant. Deposits of sediments in ditches, streams, and rivers reduce their capacity to store water resulting in more frequent and severe flooding and increased property damage. Accumulations of sediment may result in severe damage to storm drain systers. Many millions of dollars are spent each year to dredge our state waterways, to remove sediments from storm drain systerms, reseroirs, and water treatment plants, and to repair flood damage.

Sediment in streams and rivers causes the most damage to aduatic life by severely impacting aquatic animal habitats and degrading water quality. Areas needed for

reproduction and food sources are destroyed when fine silts cover the sand and gravel streambed. Decreased clarity of the water prevents sunlight from reaching plants resulting in loss of aquatic plant communities. The result is a reduction in the number and variety of fish and other aquatic life. This impact ofter can see for many miles downstream.

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 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 corrasion. 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. Cavitation 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 saltation. 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 are several reasons why a river could lose energy. If the river’s discharge is reduced then the river will lose energy because it isn’t flowing as quickly anymore. This could happen because of a lack of precipitation or an increase in evaporation. Increased human use (abstraction) of a river could also reduce its discharge forcing it deposit its load. If the gradient of the river’s course flattens out, the river will deposit its load because it will be travelling a lot slower. When a river meets the sea a river will deposit its load because the gradient is generally reduced at sea level and the sea will absorb a lot of energy. As rivers get nearer to their mouths they flow in increasingly wide, gentle sided valleys. The channel increases in size to hold the extra water which the river has to receive from its tributaries. As the river gets bigger it can carry larger amounts of material. This material will be small in size, as larger rocks will have broken up on their way from the mountains. Much of the material will be carried in suspension and will erode the river banks by abrasion. When rivers flow over flatter land, they develop large bends called meanders. As a river goes around a bend most of the water is pushed towards the outside causing increased erosion. The river is now eroding sideways into its banks rather than downwards into its bed, a process called lateral erosion. On the inside of the bend, in contrast, there is much less water. The river will therefore be shallow and slow-flowing. It cannot carry as much material and so sand and shingle will be deposited. This is called 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

Balod is a town in bank of river Tandula and also nagar palika in Balod district in the state of Chhattisgarh, India. Balod is 44 km from Dhamtari and 58 km from Durg. Balod has one college, one court, one CHC (Community Health Center), and a jail. Medical facilities are good in Balod. There are two Dams nearby Tandula and Aadmabaad built on rivers Sukha and tandula in 1913. On January 1, 2012 it was notified as Civil District though revenue district was declared from January 10, 2012. Balod became the 29th district of Chhattishgarh.There are several religious temples nearby town, particularly Ganga Maiyya temple and Siyadevi temple hold great religious value for the townsfolk. dzekad

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Communication :-

Road :- State highway network from Balod district connects Durg, Dhamtari, Rajnandgaon, Dallirajhara, Doundi, Doundilohara, Pakhanjore, Kanker, Kondagaon & Jagdalpur cities. It is 44 km from Dhamtari and 58 km from Durg & 56 km from Rajnandgaon.

Rail :- South Central East Railway (SCER) Connected with Rail section line from Raipur & Durg cities.

8. LAND UTILITION PATTERN IN THE DISTRICT: FOREST, AGRICULTURE, HORTICULTURE, MINING ETC.

(i) Types of Soil:-

Name of Block Red Soil (Bhata) Sandy loams Dorsa (Alfisols) Black (Kanhar) Total Entisols (Matasi) Inceptisols vertisols Area

Area % Area % Area % Area %

Doundi 4381 12.70 8022 23.26 8925 25.88 13157 38.15 34485 Lohara Gunderdehi 5840 9.98 27143 46.38 14122 24.13 11420 19.51 58525 Balod 7670 14.25 10360 19.24 15626 29.02 20183 37.49 53839 Gurur Doundi 17891 12.30 45525 29.63 38673 26.35 44760 31.72 146849 Total (ii) Types of Forest:-

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(iii) Details of Horticulture:- S. No. Particular Details Area in Hectare 1 Geographical Area of the District 352700 Hect. 2 Forest Area 24851 Hect. 3 Total Kast Land Area 176228 Hect. 4 Land Covered by Gardening Crops 15373 Hect. 5 Land Covered by Fruit Plants 2934 Hect. 6 Land Covered by Vegetables Crop 10602 Hect. 7 Land Covered by Masala 1535 Hect. 8 Land Covered by Flowers 185 Hect. 9 Land Covered by Medicinal & Sented Plants 117 Hect. 10 Percentage of Gardening Crops 8.72%

(iv) Details of Agriculture:- S. No. Particular Details Area in Hectare 1 Geographical Area of the District 352700 Hect. 2 Forest Area 24851 Hect. 3 Non-Agricultural Land 183699 Hect. 4 Duel Crop Area 97824 Hect. 5 Total Kast Land Area 281523 Hect. 6 Kharif Crop Area 178603 Hect. 7 Ravi Crop Area 73008 Hect. 8 Area of Jayad 1200 Hect. 9 Total Crop Area 252811 Hect. 10 Density 138%

(v) Details of Ground Water Survey:-

Climate:- Climate of the district is of tropical type. Summer is a little bit hotter. Rise of temperature begins from the month of March to May. May is hottest amongst other. Balod District's annual average rainfall is 1052 MM. During the year, most rainfall occurs during the monsoon month June to September. July is the month of highest rainfall.

9. PHYSIOGRAPHY OF THE DISTRICT Physiographically the area in Balod District having Southern peripheral undulating terrain of low hills. The general slope of the district is towards the north - east in which direction the major streams of the district flow.

10. YEAR WISE RAINFALL OF DISTRICT BALOD

Rainfall in District Balod - 2017 June – 2017 304 mm July – 2017 653 mm August – 2017 903 mm September – 2017 1118 mm October - 2017 1150 mm Total 4128 mm

Rainfall in District Balod - 2018 June – 2018 149 mm July – 2018 423 mm August – 2018 872 mm September – 2018 954 mm October - 2018 958 mm Total 3356 mm

Rainfall in District Balod – 2019 June – 2019 115 mm July – 2019 360 mm August – 2019 629 mm September – 2019 1048 mm October - 2019 …………. Total 2152 mm

11. GEOLOGY AND MINERAL WEALTH

Geology:- Geologically, the district comprises of rocks of Archaean basement of Meso to neo-Proterozoic ages. The oldest rocks belong to Archaean and mainly comprise the basement granite gneiss with metasedimentary and metaigneous enclaves belonging to the Bengpal Group. The overlying bailadila Group includes banded iron formation, shale and phylite belonging to Archaean-lower Proterozoic age. It is uncomfortably overlain by the rocks of the nandgaon Group belonging to the palaeo- Proterozoic age comprising rhyolite, rhylitic tuffs, basic pyroclastics, basalt, dolerite and gabbro etc. The Meso-to Neo- Proterozoic sequence is represented by the Chhattisgarh Supergroup, Raipur Group comprises Charmuria formation, Gunderdehi formation, Chandi formation, Tarenga formation, Hirri formation and Maniari formation. Charmuria formation mainly comprises grey bedded, limestone with minor phosphatic clay bands. Gunderdehi formation consists of purple to reddish brown calcareous shale. Quatrenary is represented by pebble beds, (Khamaria pebble bed).

The granite gneiss show well developed banding with light colour minerals and dark colour minerals oriented parallelly. The banded iron formation of bailadila group form ridges in the southern part of the district. These show curvilinear pattern with beds trending E-W to NE-SW with northerly and southwesterly dips of 40° to 80°, the rocks of the Chhattisgarh Group show sub-horizontal dips. The Chandrapur group show dips varying from 5° to 15° towards north. The overlying formations are nearly flat dipping.

Stratigraphy Succession of Balod district

Lithology Formation/Bed Group Supergroup Age Nature and Characteristic Purple to grey, fine Stromatolite Limestone Chandi Formation grained, hard and compact, calcareous rock showing stromatilitic structure Purple to white, fine grained, friable Purple calcareous shale Gunderdehi Raipur Group Chhattisgarh Neo to Meso calcareous with Formation Supergroup Proterozoic intercalations of stromalitic limestone Dark grey, hard compact Grey bedded/Flaggy Charmuria Formation flaggy/ we bedded, limestone calcareous rock, pyritiferous at place, with Grey to yellowish, medium grained, Sandstone with shale & compact, glaucreonitic, siltstone, inter- Chandarpur peblly at place (viz, calations and Group conglomerate, arenite). conglomerete Shale is fine grained, Basic pyroclastics Dark grey, medium to basalt, dolorite and course grained, massive, babbro hard, basic rock Nandgaon Group Palaeo Pinkish, light grey, fine (Kotri Group) Proterozoic Ryolite, porphyritic grained, massive add acid pyroclastics, volcanic rock basalt, dolorite and gabbro Hard, compact, Banded Banded hematite Palaeo Iron Formation (BIF). quartzite, Bailadila Group Proterozoic Shale/phylite is fine ferruginouse to Archean grained, soft rock, at place ferruginous Hard, compact, Banded Quartz vein, silified Basement Iron Formation (BIF). zone Gneissic Comlez Shale/phylite is fine (Bengpal Group) grained, soft rock, at place ferruginous Granite gnisses with Basement Archean enclaves of quartzite, Gneissic Comlez quartz-mica schist and (Bengpal Group) amphibolite

Mineral:-

Mineral deposit of Balod district includes Iron Ore, Limestone, Flagstone, Sandstone, Quartzite, Laterite, Sand, Murum and Soil etc.

Low grade limestone occurs as flagstone in Gunderdehi block of Balod district.

Brick Earth (clay for brick making) is also available in village's different part of the district.

Orinary Sand is mostly available in Bank of Tandula River and Sukha nala. Quarry leases for sand mining are given in different village of Balod district.

12. ADDITIONAL INFORMATION OF THE DISTRICT

Drainage System:- Tandula This river originates from hills situated in the north of Bhanupratappur (District- Kanker). After covering a distance of 34 km this river joins Sukha nala. This river joins Sheonath River in the south-west of Durg at a distance of approximately 13 km at gram Changori. The total length of this river is 96.6 km. A dam was constructed during the period 1905 to 1921 at the joining point of Sukhanala and Tandula River.

Kharkhara This river originates from Hils of Dallirajhara (Banjaridih) District Balod. After covering a distance of 55 km this river joins Sheonath River. The total length of this river is 55 km.

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.

Survey Report for Sand Mining of District Balod This survey report is prepared for District Balod to identify the sustainable mining in the area. In District Balod there are three rivers namely Tandula, Kharkhara and Kharun having length of 70 km., 55 km and 60 km. respectively. All possible sand mining area has been surveyed. The river wise area surveyed and identified for sand mining is given in the annexure. The thickness of sand load is considered average 4 meters in depth by observation as well as local enquiry out of which up to depth of 3 meter is considered for calculation of mineral potential. The mining area will be 10 m. away from the river bank and about 10m. Influence as safity barrier from the main streem will be left, where mining operation will be restricted. Hence 10 m. influence area from the main stream has been considered as safity zone or non mining zone. It is considered that replenishment of sand in every monsoon season is a regular process. Based on the last five year observation, it is experienced that average of 3m. Sand is replenished every year.

Area Prohibited for Mining:- The following area will be prohibited for minng. i. Quarrying shall be done excluding space on both banks of a river up to a distance equal to ten percent of the width of the river. ii. Mining is prohibited within 10 m. from the flow of the main stream. iii. Quarrying shall be done only up to a depth of three meters from the surface or up to the bed rock of the river. iv. During mining measures should be taken to guide the flow to the centre of the river to avoide erosion of banks. v. No quarrying activity shall be done within a distance of hundred meters from any natural source of water or dam or reservoir or other structure. vi. No quarrying activity shall be done within a distance of two hundred meters from any bridge or National / State Highway.

vii. Measures should be kept in consideration that the flow of river should not be diverted or obstructed. viii. The distance between two sand mining locations should be minimum 500 meters. Otherwise areas come under cluster zone. ix. Before permission of mining a suitable test of sand for construction purpose like silt percentage, fineness modulus etc. must be obtained from competent laboratory / authority. x. Provision for plantation must be assured on the river bank of concerened sand mining zone to protect erosion of banks and to maintaines ecobalance.

Details are given bellow:-

S. No. Name of River Ara Drained Sq. K.M. % Area in Balod Dist Total Drained in the District 1 2 3 4 5 1 Tandula River 70 Sq. k.m. 22484 Sq. k.m. 50 % 2 Kharun River 60 Sq. k.m. 2880 Sq. k.m. 30 % 3 Kharkhara River 55 Sq. k.m. 55 Sq. k.m. 100 %

Salient Features of Important Rivers and Streams:-

S. No. Name of the Total Length Place of origin Height of River or Stream in the District origin (in k.m.) 1 2 3 4 5 1 Tandula River 32.00 k.m. Hills Near Bhanupratapur 8 m (Dist-Kanker) 2 Kharun River 38.00 k.m. Kankalin (Petachuwa) 1 m (Dist-Balod) 3 Kharkhara River 31.00 k.m. Hils of Dallirajhara 3 m (Banjaridih) (Dist- Balod

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Mineral Potential:-

Boulder (CuM) Bajari (CuM) Sand (CuM) Total Mineable Mineral Potential (CuM) 337320 674640 2361240 3373200

Annual Deposition:- Boulder (MT) Bajari (MT) Sand (MT) Total Mineable Mineral Potential (MT) _ _ _ _

S.No. River or Portion of the Length of Average Area Mineable Stream River of area Width of area recommended mineral Stream recommended Recommended for mineral potential Recommended for mineral for mineral concession (in (in for Mineral concession (in concession (in meter) metric Concession kilometer) meters) tonne) 60% of total mineral potential) 1 ------2 ------Total for the District - - - -