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District Survey Report Dhamtari AS PER NOTIFICATION NO

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District Survey Report Dhamtari AS PER NOTIFICATION NO 2016 District Survey Report Dhamtari 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 [Type the company name] 27/05/2016 LOCATION AND COMMUNICATION MAP – DHAMTARI DISTRICT 1 1.Introduction With reference to the gazette notification dated 15th January 2016, ministry of Environment, Forest and Climate Change, the district- environment Impact Assessment Authority (DEIAA) and District - Environment Assessment Committee (DEAC) are to be constituted by the divisional commissioner for prior environmental clearance of quarry for minor minerals. The DEIAA and DEAC will scrutinize and recommend the prior environmental clearance of ministry of minor minerals on the basis of district survey report. The main purpose of preparation of District Survey Report is to identify the mineral resources and mining activities along with other relevant data of district. This report contains details of Lease, Sand mining and Revenue which comes from minerals in the district. This report is prepared on the basis of data collected from different concern departments. Dhamtari district is situated in the southeaster part of the Chhattisgarh. It is fertile plains. It falls in the servey of India degree sheet No. 64/H,L and G between Lattitude 20°02"42' : 21°01"33' N and Longtitudes 81°24'41" : 82°10'45" E. The district's total area is 4080 sq. km. and it is about 317 meters (1,040 feet) above sea level. It is bordered by the Raipur and Durg District to the north, the Kanker and Bastar Districts to the Orrisa state of the south. The Gariyaband to the east and the Kanker and Balod Districts to the west. The fertility of the land in the Dhamtari District is due to the Mahanadi River and its tributaries (Sendur, Pairy, Sondur, Joan, Kharun, and Shivnath).dhamtari is situated 79 km from capital Raipur. The Dhamtari including 4 tehsil namely Dhamtari, Nagri,Magarload and Kurud. Population of the district is 7, 99,781 of which 397897 male and 401884 female respectively. The Mahanadi is the main river which originated from sihawa pahadh of the district and runs through Nagari to south of Dhamtari town to Rajim to Raipur. 2 2. Overview of Mining Activity in the District There are no major economic mineral deposits of any significance except limestone at Sonadihi, Nari, Goji, Gotra and Amlidihi and clay at Kosagonda. Laterite cappings of Cainozoic age occuring over the Bundeli granitoids are seen in the southeastern part of the district. Existence of granite in the district as denudational/Structural at Nagri, Sihawa where quarry lease are given in the name of ordinary stone for road and building material. 6 quarry leases are given above granite at village Deopur, Kokdi, Dhaurabhata. Beside these 23 leases to the village panchayat for Sand mining in different rivers and nala. Sand mining are mostly at and around bank of Mahanadi, Sondhur, Pairi. There for in Dhamtari district mining activities are mainly for sand, laterite ordinary stone and clay for brick making. 3 3. List of Mining Leases and Sand in the District with location, area and period of validity ¼d½ ftys esa Lohd`r mR[kfuiV~Vks dh lwph %& foRRkh; o"kZ 2013&14 dzekad iV~Vsnkj dk uke o irk [knku xzke dk uke mRiknu fczdh ¼?keh@Vu½ ¼?keh@Vu½ 1 vkf'k"k VkfV;k xksth 2286 1504 2 xxu ukgVk nsoiqj 1653 1631 3 ;ksxs’k dalkjh dksdMh 1967 4904 3 uhjt xaxoky Xksth 4224 4524 4 iwtk HkksFkjk /kkSjkHkkBk 0 0 5 jktsUnz ikgkfM;k xksth 0 0 6 ukxsUnz 'kqDyk vNksyh 1210 1127 7 iwtk ikj[k dksdMh 5261 3234 8 vCnwy XkQ~Qkj /kkSjkHkkBk 321 321 9 v;qc fjtoh dksdMh 3691 9984 10 foey es?kokuh /kkSjkHkkBk 0 0 (ii) List of Quary lease in the district with location area and period of validity ¼[k½ ftys essa Lohd`r jsr [knkuks dh lwph %& dzekad xzke iapk;r dk jsr [knku xzke Ik-g-u- [kljk dza- jdck uke dk uke ¼gs-½ 1 2 3 4 5 6 1 vNksVk rsUnwdksuk 26 501 2-40 2 vNksVk rsUnwdksuk 26 2@1 5-50 3 tojxkao tojxkao 35 117 8-00 4 yhyj yhyj 35 02 8-00 5 [kjsaxk [kjsaxk 34 920 6-00 6 njhZ njhZ 34 759 16-00 7 f<ejfVdqj f<ejfVdqj 9 1292 2-00 8 lkjaxiqjh lkjaxiqjh 34 757 6-00 9 nsoiqj nsoiqj 16 1392 6-00 10 nksuj nksuj 15 3170 6-00 11 es?kk es?kk 10 959 8-00 12 uokxkao ¼cq-½ uokxkao ¼cq<suh½ 42 1283 9-50 ,- 13 fxjkSn fxjkSn 6@40 319 4-00 14 djsyhcMh djsyhcMh 41@6 01 6-00 15 cq<suh cq<suh 8 1344 5-10 1 2 3 4 5 6 16 Hks.Mjh Hks.Mjh 7 651 5-10 17 uohu tksjkrjkbZ uohu tksjkrjkbZ 40 1018 16-05 18 tuin dq:n xkMkMhg 36 2061 8-00 19 tuin dq:n ij[kank 36 2290 8-00 20 eanjkSn eanjkSn 37 1711 8-00 21 lsejk¼ch½ lsejk¼ch-½ 15 778 6-00 22 veyhMhg veyhMhg 13 1653 8-50 23 ijsokMhg ijsokMhg 09 145 10-00 ¼x½ ftys essa fpeuh HkB~Vh [knkuks dh lwph %& 1 2 4. Details of Royalty or Revenue Received in Last Three Year (i) Major Minerals In Dhamtari district there have no any mining lease. (ii) Details of Royalty or Revenue Received in Last Three Year Minor Minerals o"kZ 2013&14 o"kZ 2014&15 o"kZ 2015&16 dzekad mRiknu ¼?ku jkf'k mRiknu jkf'k mRiknu jkf'k eh- esa½ ¼?ku eh- esa½ ¼?ku eh- esa½ 1 7 8 9 10 11 12 2 & & 50000 1000000 40600 812000 3 70511 1410220 95989 1919780 & & 4 6171 123420 73434 1468680 & & 5 & & 102149 2042980 39477 789540 6 & & & & 50000 1000000 7 & & 40000 800000 & & 8 & & 50000 1000000 50000 1000000 9 10413 208260 44012 880240 16350 3270000 10 540 10800 & & & & 11 11855 237100 & & & & 12 & & 142304 2846080 131557 2631140 13 6000 12000 25000 500000 25000 500000 14 & & 25000 500000 25000 500000 15 & & 35323 706460 25380 507600 16 & & 51400 102800 & & 17 & & & & 51000 1020000 18 900 18000 53040 1060800 48566 971320 19 & & 55207 11041140 & & 20 & & 60000 1200000 & *& 21 6472 129440 & & & & 22 6307 126140 & & & & 23 28400 568000 & & & & 24 2699 72660 & & & & 25 716900 10000 2522500 26000 408500 24000 26 1344550 20000 653600 20000 1361400 26800 dqy 2211718 2946040 16177700 27114960 2272830 13052400 5.Details of Production & Royalty of Sand in last Three years foRRkh; o"kZ 2013&14 foRrh; o"kZ 2014&15 foRRkh; o"kZ 2015&16 dzekad mRiknu fczdh tek mRiknu fczdh tek mRiknu fczdh tek ¼?keh@Vu½ ¼?keh@Vu½ jkf’k ¼?keh@Vu½ ¼?keh@Vu½ jkf’k ¼?keh@Vu½ ¼?keh@Vu½ jkf’k 1 2286 1504 3]81]000 2721 2432 1]80]000 1263 1259 1]60]00 2 1653 1631 1]07893 1455 801 84148 2552 2947 2]50]000 3 1967 4904 2]34]372 5210 5079 2]17]157 1641 1484 1]77]520 4 4224 4524 3]35]767 3976 3632 4]02]000 10950 10851 6]00]000 5 0 0 30]000 325 206 1795 155 35 35]000 6 0 0 15950 1105 224 70]950 4860 2187 1]74]960 7 1210 1127 1]11]431 480 557 61]800 1020 696 35]450 8 5261 3234 5]99]600 1485 1771 0 1950 286 0 9 321 321 32]900 318 304 0 15 0 0 10 3691 9984 4]30]000 771 630 1]76]100 1649 854 2]00]000 11 0 0 0 0 0 0 0 0 0 dqy 20613 27229 15950 17846 15636 85943 26055 20599 1288930 1 6. PROCESS OF DEPOSITION OF SEDIMENTS IN THE RIVERS The district forms a part of the Mahanadi basin. The general slope on the eastern part of the area is towards south –east, in the central part of the area is towards north and on the western part is towards north western direction. The western boundary of the district is running along the Mahanadi River . The Jonk River passes through the central part of the district and is running in northern direction. The Kurar nala, Nami nala, Keswa nala and sukha nadi forms part of the drainage system for Mahanadi River basin. the Mechka nala, Bagh nala, Racme nala Lath nala forms part of the Jonk River basin. The Kunti nala, Surangi nala and Chinar nala forms part of the Ong River basin. The obvious things rivers 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.
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