Location of Investigated Area Applicant

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Location of Investigated Area Applicant IN LOCATION OF INVESTIGATED AREA EXTENT : 1.51.5 Ha, S.F.Nos. : 1322/1A2,1B2,2, 1407/1A,3A, 1408/2B, 1410/1A2,1B and 2B VILLAGE : MALLANKUZHI, TALUK : THALAVADI, DISTRICT : ERODE, STATE : TAMILNADU. FOR APPLICANT No. 120, HOODI APARTMENTS, CUNNINGHAM ROAD, BENGALURU, KARNATAKA - 560 052. PREPARED BY Recognized Qualified Person RQP/MAS/253/2013/A New No.17, Advaitha Ashram Road, Alagapuram, Salem District, Tamilnadu – 636 004. Cell: 94422 78601, 94433 56539 E-mail: [email protected], [email protected] LIST OF CONTENTS Page S. No. Description No. 1. Preamble 1 2. Infrastructure 2 3. Location and Physiography 3 4. Details of the area 4 5. Geology 6 6. Contour Mapping and Preparation of the Base Plan 8 7. Method of Estimation of Reserves 8 8. Summary and Conclusion 11 LIST OF PLATES Plate S. No. Description Scale No. 1. GEOLOGICAL PLAN AND SECTIONS I 1:1,000 2 KEY PLAN II 1:1,00,000 Geological Report Mallankuzhi Black Granite A BRIEF GEOLOGICAL REPORT FOR THE OCCURRENCE AND DISTRIBUTION OF BLACK GRANITE (DOLERITE) DEPOSIT OVER AN EXTENT OF 1.51.5Ha OF MALLANKUZHI VILLAGE, THALAVADI TALUK, ERODE DISTRICT. 1.0 PREAMBLE: This Geological report is prepared for evaluation of Black Granite belongs to M/s. Deccan Trading Company Pvt. Ltd., having an office at No. 120, Hoodi Apartments, Cunningham Road, Bengaluru, Karnataka - 560 052. The applicant intends to carry out a Geotechnical study to estimate the Resources and Reserves of Black Granite in the prospecting area, hence the proponent approach me S. Ilavarasan, M.Sc., to carry out a detailed Geological investigation. S. Ilavarasan, M.Sc., has decided to carry out the Geological evaluation and validation of the Black granite deposit. The primary objective of this study is to make a Geological and geophysical investigation of the Black granite, which is available in the study area moreover analyzing the physical properties like structure, Texture, Colour, Hardness, etc., to suitable for the Commercial exploitation in the Present Market position. The principle aim of this Reconnaissance Survey is to delineate Granite deposits to evaluate the resource and estimate the reserves of the granite in the area, over an extent of 1.51.5Ha of Patta lands in S.F.Nos. 1322/1A2, 1322/1B2, 1322/2, 1407/1A, 1407/3A, 1408/2B, 1410/1A2, 1410/1B and 1410/2B of Mallankuzhi Village, Thalavadi Taluk, Erode District, Tamil Nadu State along with Global Positioning System (in W.G.S datum-1984). The scope of the work is to assess the nature of the Black Granite deposit and its occurrence and distribution within the study area. Accordingly, the consultant undertook the various Geological studies, and this report is prepared based on the investigation conducted, field observation and its inference along with recommendations. 1 Geological Report Mallankuzhi Black Granite The study area has under consideration in quarrying operations earlier. The first lease has granted in favour of M/s. Pacific Enterprises, for quarrying black granite over an extent of 1.73.5 hectares in S.F.Nos. 1322/1A2, 1322/1B2, 1322/2, 1407/1A, 1407/3A, 1408/2B, 1410/1A2, 1410/1B, 1410/2B and 1411/2A of Mallankuzhi Village, Sathiyamangalam Taluk, Erode District for a period of 5 years from 1996 – 2001. The study area is containing two existing quarry pits situated in S.F.Nos. and an existing waste dump, due to quarry operations carried out during earlier quarry lease period. The maximum dimension of the existing quarry pits and waste dump is given table below (Please refer Geological Plan Plate No. I). Table - 1 Existing pit dimension in meters PIT No. (Maximum) Location in S.F.Nos. Length Width Depth 1410/1A2, 1410/1B and Pit – 1 49 15 4 1410/2B (additional pit covered in S.F.No. 1411/2A) Pit – 2 30 30 3 1407/1A Table - 2 Existing Waste dump dimension in meters Location in (Maximum) S.F.Nos. Length Width Height 48 41 6 1322/1A2 2.0 INFRASTRUCTURE: The study Area is located about 4km northeast of Mallankuzhi hamlet and 100m north of Dhoddakhajanur to Aralvadi village road. The nearest town is Thalavadi, which is about 5km on the Northeastern side where all basic facilities like Hospital, Communication centre, Schools, Police Station, and Bus terminus are available. The District Administrative Office and the District headquarters are available in the Erode town located at a distance of 95km on the southeastern side. 2 Geological Report Mallankuzhi Black Granite There is good approachable metal road is already existence on the southwestern side of the area, there is no other patta land encountered for the haulage and approach of Black Granite. Table – 3 Approximate aerial distance Particulars Location from lease applied area. Nearest School Soosaiyapuram 2km – SE Nearest Post Office Aralvadi 4km – West Nearest Town Thalavadi 5km – NE Nearest Police Station Thalavadi 5km – NE Nearest govt. Hospital Thalavadi 5km – NE Nearest D.S.P. Office Sathiyamangalam 42km – SE Nearest Railway Station Samrajnagar 18km – North Nearest Airport Coimbatore 82km – South Nearest Seaport Kochi 215km – SW There is no habitation/village located within the radius of 300m and few villages are located within the 5km radius, approximate distance with direction & population are furnished below. Table – 4 Name of the Approximate Approximate S. No. Direction Village Distance population 1. Soosaiyapuram SE 2km 2,750 2. Dhoddakhajanur East 4km 5,300 3. Bisalavadi NW 4km 4,600 4. Karulavadi South 3km 1,900 5. Arulavadi West 4km 2,900 6. Mallankuzhi SW 4km 5,050 There is no historical/National Monuments, Reserved forest, Wild life sanctuaries, Places of Worship, Public Buildings, Places of Public Interest and Permanent structures situated within 500m radius of the area. 3.0 LOCATION AND PHYSIOGRAPHY: The area is situated in an undulated surface on the hilly terrain. The gradient is gentle towards southeast and altitude of the area is about 790m to 795m above from MSL. The Black granite is clearly visible right from the existing quarry pit with physical weathering. The ground water occurrence in this area is about 52mts in summer and 47mts in rainy season. The average annual rainfall is about 575mm – 833mm. The climate is dry and the temperature rises up to 40oC in summer and falls down to 21oC in winter seasons. 3 Geological Report Mallankuzhi Black Granite The study area is a barren land and the area has been carried out quarry operation in earlier hence, this area does not fit for any agricultural activities. The surrounding lands are barren land and seasonal cultivation practiced in some places by lift irrigation method. The main crops are Paddy, Ragi, Maize, Beens, Groundnut and trees like Neem, Cocos nucifera, Cactus and thorny bushes are seen around the area. Fig.1.0 Satellite Imagery of the study area 4.0 DETAILS OF THE AREA a. The area is marked in the Survey of India, Topo sheet No. 58-A/13. b. The details of the land covered by the area is given below. TABLE - 5 Area in Patta Occupancy District Taluk Village S.F.Nos. Hectares No. 1322/1A2 0.24.5 1322/1B2 0.05.5 It is a Patta land 1322/2 0.23.0 registered in the name 1407/1A 0.37.5 of M/s. Pacific Enterprises. The Erode Thalavadi Mallankuzhi 1407/3A 0.03.0 1783 company has obtained 1408/2B 0.20.0 consent from the 1410/1A2 0.06.5 pattadar for the period 1410/1B 0.07.0 of 25 years from 1410/2B 0.24.5 23.10.2018. Total Extent 1.51.5 4 Geological Report Mallankuzhi Black Granite The investigated area lies between the North Latitudes of 11°46'09.42"N to 11°46'16.35"N and East Longitudes of 76°57'19.22"E to 76°57'28.22"E (in W.G.S datum-84). Fig 2.0 Photographs of the Study area 5 Geological Report Mallankuzhi Black Granite 5.0 GEOLOGY: i) REGIONAL GEOLOGY The hard rock terrain of Archaean to Late proterozoic comprises of predominantly Granite, Gneiss, Charnockite, Khondalite group of rocks and their magmatic derivatives, supracrustual sequences intruded by ultramafic complexes, basic dykes, granites. The northern part of Tamilnadu, north of Noyil – Cauvery River is characterized by the occurrences of a number of Dolerite dykes in contrast to the areas south of Noyil – Cauvery River where the dykes are absent. The dolerite dykes in general trending is in WNW- ESE and NNE – SSE directions and rarely in N-S and NNW – SSE directions. In central part of Tamilnadu, ENE – WNW to NE- SW trending dolerite dykes (Black granite) are seen transecting the Charnockite in Kalrayan & Kolli Hills. Palaeo magnetic studies of some of these dykes indicate Mid-Proterozoic age. Due to emplacement of Dolerite Dykes along narrower plains of weakness, the rock on solidification develops cracks and fractures mostly along the contacts with the country rocks. The dolerite dykes are mostly emplaced as ‘swarms” in an area. Granites were formed from molten rock referred to as “Magma” formed at great depths within the crust of the earth. During the cooling process, some of the minerals grow into larger crystals of colours peculiar to those minerals or get aligned along certain preferred directions giving rise to beautiful colors and patterns. Such rocks that were formed at great depths during the Archaean age are now exposed at the surface of the earth as a result of the combined actions of wind, air, sunlight and water and weathering and denudation over the past several million years. The granitic group ranges in composition from granite, through granodiorities to adamellite, augite-diorite, monzonite, etc., and contains inclusions of hornblendic rocks.
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