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Chapter-1 General QUARRY PLAN OF KUKURDIKALA (A) SAND MINE CHAPTER-1 GENERAL (a) Name of Applicant : Sarpanch, Gram Panchayat Kukurdikala Address : Gram Panchayat Kukurdikala Tehsil: Masturi, District :- Bilaspur Tehsil : Masturi District : Bilaspur State : Chhattisgarh PIN code : 495551 Phone : +91-8959101111 (b) Status of the Applicant : Gram Panchayat Kukurdikala (c) Mineral(s) which are : Sand (ordinary) occurring in area and which the applicant intends to Mine (d) Period of which mining lease : As per the sand policy of Chhattisgarh state is granted the area is notified for sand mining by collector Bilaspur notification. (e) Name of RQP preparing the : Mining Inspector, Bilaspur mining plan Khanij Shakha, Collectorate Bilaspur, CG * * * * * 1 | P a g e QUARRY PLAN OF KUKURDIKALA (A) SAND MINE CHAPTER-2 LOCATION AND ACCESSIBILITY (a) Details of area(with location map): Shivnath River Sand Quarry. State : Chhattisgarh District : Bilaspur Taluka : Masturi Village : Kukurdikala Khasra No. : Khasra No- 678/1 (part) Forest Range : NA Forest Division/Circle : NA Lease area (hectares) : 4.99 Hectare Whether the area is recorded to be : NA in forest (please specify whether protected, reserve etc.) Ownership/Occupancy : Gram Panchayat, Kukurdikala Existence of public Road/ railway : Kukurdikala village is located in Masturi Tehsil line, if any, nearby and of Bilaspur district in Chhattisgarh, India. It is approximate distance situated 44km away from sub-district headquarter Masturi and 61km away from district headquarter Bilaspur. As per 2009 stats, Kukudikala is the gram panchayat of Kukurdi Kalan village. Toposheet No with Latitude / : 64K/6 Longitude Point Latitude Longitude A 21°42'59.78"N 82°24'1.04"E B 21°43'3.02"N 82°24'12.80"E C 21°42'58.41"N 82°24'14.78"E D 21°42'55.67"N 82°24'4.30"E Land Use Pattern : Government Revenue Land (Forest, agricultural, grading, barren, etc.) 2 | P a g e QUARRY PLAN OF KUKURDIKALA (A) SAND MINE (b) Attach a general location and vicinity map showing area boundaries and existing and proposed access routes. It is preferred that the area to be marked on a survey of India topographical map or a cadastral map or forest map as the case may be. However if none of these are available the area should be shown on an accurate sketch map on scale of 1:5,000. Key plan attached (Scale 1:50,000) Khasra plan attached (Scale 1: 4,000) Surface Plan attached (Scale 1: 2000) Environment Plan attached (Scale 1:10000) Infrastructure Facilities: Available Facilities Village Distance from the Area 1 Police Station Jodhara About 04 Km. 2 Post Office Jodhara About 04 Km. 3 Electricity Kukurdikala About 1.0km. 4 Nearest habitation Kukurdikala About 1.0km. 5 Rest House Masturi About 38 Km. 6 Medical Jodhara About 04 Km. 7 Telephone Kukurdikala About 01 Km. 8 Education School- Kukurdikala About 1.5 Km High School- Masturi About 38 Km. 9 Nearest Railway Jairamnagar Railway About 42 Km. Station Station 10 Nearest Airport Chakarbhata 47 Km. 11 Nearest River / Nala Shivnath River 0Km. 15 Climate Type Tropical to Subtropical Temperature Maximum 46 0 C in Summer Minimum 08 0 C in Winter Rainfall 1000mm to 1500mm 16 Vegetation Neem, Teak etc. Not found * * * * * 3 | P a g e QUARRY PLAN OF KUKURDIKALA (A) SAND MINE CHAPTER-3 TOPOGRAPHY AND GEOLOGY Topography The Notified sand mine area is geographically situated in the bed of Shivnath River, in khasra no- 678/1(part) of village- Kukurdikala, Gram panchayat- Kukurdikala, Tehsil: Masturi, District- Bilaspur. Shivnath River originates from Panabaras Hill, 624 metres (2,047 ft) above sea level in the Ambagarh Chowki division of Rajnandgaon district of Chhhattisgarh. The river flows in the north-east direction for 300 km. from its source and joins the Mahanadi River near the town Shivrinarayan. The Shivnath River is the longest tributary of Mahanadi River, which it joins in Khargahni in Bilaspur district in Chhattisgarh. The maximum and minimum RL with the lease area is 223m in west direction and 217m in east direction. The average width of the notified area of the quarry area is 150m and length is about 332m. The Khasra plan (Plate-3) and Key plan (Plate 1) of the area showing the location of the mine in Google earth is enclosed as plate no 6 and photographs of the area in Plate no 7 respectively. Geology of the area Regional Geology:- Bilaspur district is situated in the north northwestern part of Chhattisgarh state and is covered in Survey of India Degree sheet nos. 64 E, 64F, 64 J and 64 K between Latitude 21 0 35’ : 21 0 23’ and Longitude 81 0 27’ : 82 0 29’ 58”. The district is bounded by Shahdol and Koriya districts in the north, Korba and Janjgir districts in east, Raipur and Durg district in the south Kawardha and Mandla district in the west. Bilaspur is the district headquarter and Mungeli, Takhatpur, Pendra, Sakola, Kota, Ratanpur are some of the major towns. The katni banch of South Eastern Railway passes from North to south to connect Bilaspur and Raipur in the south and Anuppur in the north. It connects Champa in the east. All the important places within the district are well connected by a network of state highways and all weathered roads. Seonath River flows easterly in the southern most part of the district, Arpa, Kurung, Rahon, Ghongha, Son, Tesua etc., are important tributaries of Seonath draining from west and north to it. The drainage pattern in general is subparallel with medium density. Physiographically the district can be divided into vally fill denudational plateau, denudational pediment/ pediplain and high level plateaux. The vally fills occur in the southern most part. They range in elevation from 260m to 275m. High level plateaux are exposed in the eastern and western parts, ranging in elevation from 539m to 730m in the east and attain a maximum elevation of 1006m in the west. 4 | P a g e QUARRY PLAN OF KUKURDIKALA (A) SAND MINE AGE SUPERGROUP GROUP STRATIGRAPHIC LITHOLOGY STATUS Cainozoic Alluvium Laterite Sandy loam, silty sand, coarse medium laterite Upper Deccan Trap Basalt Flow Cretaceous to Eocene Cretaceous Lameta Arkosic Sandstone, Limestone, Clay. Lower Gondwana Barakar Formarion Sand stone, Shale Permian Supergroup and Coal seams Talchir Formation Boulder bed, Sandstone and shale Meso- Neo Chhattisgarh Raipur Kodwa Formation Argillaceous Proterozoic Supergroup Group Dolomite Terenga Formation Calc- aggillite, dolomite Chandi Formation Clay- chert shale Pink Dolomite & Shale Shale with limestone intercalations Stromatolitic limestone Dolomite Gunderdehi Shale with flaggy Formation limestone Grey shale Raipur Group Unclassified shale, (Unclassified) Limestone Meso Chandrapur Sandstone and Proterozoic conglomerate Quartz and Pegmatite Veins Dolerite andbasic intrusion Archaean to Chhota- Nagpur Gneissic- Complex Unclassified Proterozoic Granite and Gneiss Unclassified metamorphics 5 | P a g e QUARRY PLAN OF KUKURDIKALA (A) SAND MINE Rock formations ranging in age from Archaean to recent times are exposed in the area. They include granites, gneissesand older metamorphic of precambarian age, rocks and Chhattisgarh supergroup of upper Proterozoic age, Gondwanas of Permian age, Lametas of Upper Cretaceous age. Deccan trap of upper Creataceous to Eocene age and laterite (with bauxite) of cainozoic age comprises of unclassified granites and granite gneisses, with enclaves of older metamorphic- phyllites, quartzites, schists and dolomitic marble. This group is exposed in northern part of the area. The Chhattisgarh Supergroup of rocks occurring in the south unconformably overlie the Precambarian basement. The Chhattisgarh Supergroup is divisible into Chandarpur and Raipur groups. The Chandrapur group comprises sandstone and conglomerate. Unclassified Raipur Group comprising of shale and limestone occurs in the central and south central part, whereas in the south- eastern part this Group is represented by the rocks of Gunderdehi Formation, Chandi Formation is represented by grey shale, and limestone with intrafromational conglomerate. Chandi formation is comprised of grey, hardand compact 6 | P a g e QUARRY PLAN OF KUKURDIKALA (A) SAND MINE shale and pick Limestone. Tarenga formation comprises of clay, chert, shale, red calc- aggillaceous Limestone. Mohtara Formation is represented by grey argillaceous Limestone. Gondwana Supergroup is represented by the rocks of Talchir formation and Barakar Formation of Lower Permian age. Talchir Formation occupies the northern most part of the district and is composed of buff and khaki green shale with splintery fragments, Grayish white, fine to medium grained sandstone and boulder bed that comprises of subangular clasts of quartzite and gneiss in grayish, fine to medium grained matrix. Barakar formation consist of grayis white, fine to coarse grained, cross bedded massive sandstone, grey shale, blackish grey carbonaceous shale, light yellow to creamy white clay with coal seams it occurs in the northern most part of the district. Lameta Formation is exposed in the NW part of the district at the foothill of Amarkantak Plateau. It comprises ash grey coloured cherty/ siliceous limestone and greenish feldspathic (arkosic) sandstone with very thin bands of red clay- variegated in nature. Deccan trap of upper cretaceous to Eocene age is exposed in west and nort western parts of the district overlying the Lametas. The Basalt flows are dark grey, fine to medium grained, hard and compact. Laterite and Bauxitic Laterite of Cainozoic age are observed on basalts in the west and north western part of the district. The development of the reddish brown, hard and compact lateritic profile is due to weathering of the trap rocks which subsequently has resulted in the formation of bauxite zones. The Chhattisgarh and Gondwana Supergroup of rocks show bedding trending in the NNE- SSw to NNW-SSE direction with occasional variation to E-W. these have low to moderate southerly and northerly dips varying from 3 0 to 40 0 . The foliation planes in the gnissic rocks also show trend of E-W, NE-SW, NW- SE, dipping northerly or southerly, with the dip varying from 35 0 to 83 0.
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