District Survey Report of Minor Minerols, tamtaro (Except River Sand) Prepored in accordonce with Pora V (iii) of 5.0.141 (E) Doted 75th Januory 2016 of Ministry ol Environment, Forest ond Climote Change Notification.

GOVERNMENT OF DISTMCT-

JAMTARA DISTRICT JHARKHANO +

PREPARED BY DEIAA UNDER THE GUIDANCE OF DEPUW COMMISSIONER CUM CHAIRMAN DEIAA, JAMTARA e-*,, iErs\,s

G EOLOGIST ASSISTANT MININ6 OFFICER DISTRICT G EOLOG ICAL OFFICE ]AMTARA

)hlr' )11qplR EXECUTIVE ENGINEER, IRRIGATION ]AMTARA n '(ffi* ("q9 EXEXCUTIVE ENCINEER, ,,u,r,o^o, ,oJi OFFICER ROAD CONSTRUCTION DEPARTMENT JAMTARA

^H#-',

Dy. COMMISSIONER / CHAIRMAN, DEIAA, JAMTARA Ch.No Description

Preomble 5

1 lntradudian 7-8

1.1 Locotion ond Geographicol Areo 7

1.2 Administrotive Units 7

1.3 Cannectivity 7

2 OveNiew oI mining dctivity in the disttict 9

3 List of Mining leose in the distrid 70-26

3.1 List ol opeiotive stane mines in the district

i.2 List of non-operdtive stone mines in the district 73

3.i List of Terminated / Cancelled Leose of Stone Mines 18

34 Patential blocks of the District 19-26

4 Detatl ol Bayolty or Revenue received in last 3 yeors 27

; Detoil of ptoduction of minor minerol in last 3 yeors 27 e Genercl prdile ol the Dis'trict 28-35

b.,L River System

6.2 Climote 28-i0

6.3 6eomorphology

6.4 Soil 32

5.5 lrrigation 33

6.5 Physiogrophy 33

6.7 Demography

6.8 Forest (Floro & Fduno ) 35-36 7 Land Utilizotion Pottern of the District 37-iA

8 Ground Water Scendrio 3944

8.1 Hydrogeology 39

8_2 Consol id dted Formation 40

Se m i -Co nsa lid dted F o rmat i on

8.4 2epth to Woter level

I Ground woter mondgemet strotegy 4548

9.1 6rou nd woter d evelopment 45

9.2 GROUND WATER RESOURCES 46

9.3 GROUND WATER REUTED ISSLJES & PROBLEMS 45-47

9.4 RECOMMENDATIANS 48

70 Roinfall: Month Wlse 49

77 Geology & Mineral wedlth of the oreo s0-52

72 Brief Disdster Risk Profile 53-54

12.7 Vulnerability of the state 53

12.2 Mine Disaster 54

13 OVERV'EW OF IMPACT OF MIMNG AN ENIy,RANMENT 55-59

Conclusion & Reference 60 Prior to the formation of rharkhand Minor Minerar concession Rure 2004, the mining operation for minor minerar were carried out in unscientific manner in. rdentifying this fact in exercise of power, conferred by section 15 by Mines and Minerars (Deveropment and Reguration) Act 1957 and a other powers enabring it in that beharf, the industry Mines & .eorogy Department, Govt. of Jharkhand framed the aforementioned rure, and it has been amended with period of times in the year 2OO7,2A7O,2074,2O75 and 2017 .

Keeping in view of experience ga!ned in perioci of one decade, the MoEF&cc came out with Environmental rmpact Assessment Notification s.o.-1533(E) dated 14th sept.2006. rih* n".n made mandatory to obtain environmentar crearance for different kinds of deveropment projects as listed in Scheduled -t^ of notification.

Further, pursuance of the order of petition Hon'bre Supreme court {c) No. 1g62g 1g62g of 2009, dated 27',h Feb.2oL2 rn the matter of Deepak Kumar etc., vs state of Haryana and others etc., prior environmentar ciearance has now become mandatory for Minint of Minor Minerars irrespective ofthe area of Mining Lease.

And also in view of the Hon'bre Nationar Green Tribunar, orcrer dated the 13th Jan.2015 the rnatter regarding sand, Brick earth, & burrowed earth cutting for Road construction has to take prior E C For Mining Lease irrespective of the fact that whether the area invorved is more or less than 5 hectares' They arso suggested to make a poricy on E.c for sand incruding other minor minerals mining lease in cluster. ln pursuance MoEF&cc Notification s.o. 141(E) dated 1s,h ian.2016, District Environment lrnpact Assessment Authority (DETAA) & District revel Expert Appraisar committee (DEAC) has been formed for Category -82 Minor Minerals having area less than or equal to 5 ha. \4oEF&cc in consurtation with state Government has prepared Guiderines on sustainabre sand & other Minor minerals mining detailing the provisions on Environmental Clearance for cluster. creation of District Environmental rmpact Assessment Authority (DETAA,) & proper monitorinB :f Minor Minerals Minint using rnformation Technorogy to track the minerar out materiar from sou rce to destin ation.

DEAC iviil scrutinize and recommend the prior environmentar crearance of Mining of Minor l!4ineral to DErAA on basis of District survey report. This wiI moder and guiding document !\ l'ich is a compendium of avairabre minerar resources, geographicar setup, environmentar and e:o:ogtcal set up of the district and replenishment of minerals and is based on data of various ceoartments, published reports, Journal and websites, The District Survev report will form the 53sis for application for environmental crearance, preparation of reports and appraisar of prcjecs District survey Reports are to be reviewed once in every five years a5 per statue, h o *e,rer this is an interim report, which will be updated at regular intervals. n ne with above guideline Chief Secretary of Government of Jharkhand issued a letter to all leputy Commissioner's Vide letter No. -Ig74/Cs dated 01_0g-2017 & Notification No. Khani(vivid) '67 /2017 /190s dated 16-08-2017 by secretary Government Department of industries, jhari

The Main objective ofthe preparation of District survey Report is to ensure the following:-

1. ldentification of Mineral Resources in the district. 2. Identification of areas of minor minerals having the potential where mining can be allowed. And 3. ldentification of area and proximity to infrastructure and installations where mining shou ld be pr.oh ihited. is situated in the North Eastern part of Jharkhand state. The district is situated in the Northern Plain of lndia and eastern plateau and hill region. Jamtara town is the administrative headquarters of this district. lt is bounded by district in north, Dumka and West Ben8al in the east, and in the south and in the west. The district is situated between 24'9'51" North and 23" 47'55" North latitude and 86" 27'58" East and 87" L7' 26" East longitude, having an area of 1802 km2 (approx). Total population of the district is 79A,2oi , with the population density of 440/krr'? (As per Census 2011).

Jamtara district comprises of only one administrative sub-division (Jamtara) and six development blocks, namely , Nala, Jamtara, Narayanpur, Karmatar and Fatehpur. There are 1175 villates and 118 Gram Panchayats in the district.

Jamtara is on the Main Line of the Eastern Railway from Howrah to Delhi, thus it is well connected with other important cities of the country, such as, (2a2km), Chittaranjan (14 Kms), Ka rmatanr Vidyasagar (18 Kms), Patna (293 Kms), Howrah (245 Kms by railway. Sevaral passenger buses run regularly from Ranchi, Dumka, Deoghar, Giridih, , Chittaranjan and other places in Jhaikhand to Jamtara.

The nearest major airport is Birsa Munda Airport. This airport has domestic flights from Ranchi, lndia and is 243 km from the center of Jamtara, lndia.

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2 87"Co',E *+,N S

UTTAR PRADESH

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N JAMTARA DISTRICT JHARKHAND

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LEGEI{O o 'lo

, nri'40 0'E The district has total 16 operative and 3z non-operative stone mines, which generate on an average royarry ofaround 1 crore rupees, arong with a Dead Rent of a.oura? r.rt r., .rr"". every year, Mineral based industries in the district incur an investment of approximately Lakh rupees. Jamtara is rich iir mi.erais such a. stone, Ferdspar, Presece-185 ofsand euar,, Granite. stone is observed in Karmatanr Vidyasagar and-Fatehpur ui".ti * and is rich in Rajnrahar lrlrt trap Basait. carnet Biotite Gnei.ss is present in Narayanpur Block. Noticibre amount of deposii of Sand stone is observed in tlre southern part of .

Picture showing mining of Stone in Jamtara District Lease ho ld er M./s Keshaw Stone Lokdih I a n'rta ra 37s/P 16.09.2008 23"55',21.28"N Udoyog, (Pa h rudih) to to Pro- Sri Wakil 15.09.20i8 23"55',26.34"N Hembram, 86"49',38.36" S/o Sri Rasik E to Hembram, 86"49',41.0s"8 at-

Lokdih (Pahrudih ), P.o-Bewa, P.s , Dist- lamtara Sri Gan esh Kundahit 72,05.201.1 23"56',45.09"N H ernbram, to to 11.05.2021 23"56'47 .r2"N Harinarayanpur, 87"08',33.36"E F. o- Kun dah it, Dist- to iamtara 87'08',36.15" E -_l Sri Laxman Dubey Digharia Binda pat 2?.17.2008 Si o Sri N ilkanth har to Du bey, 21.12.2018 At & P. o- Ku kraha, Ch rtra, Dist- D eogh ar & Sri Alun Chandra Chcudh a Tapa n kumar jha 03.09.2010 23"56',55.8"N b.Bablu raut to 86"52',s6.3"E V lir Ba u ripasra 02.0s.2020 23"56',46.9"N :'c+Cist:-lamtara 86"52',52.5"E Irp:ress infratech Cha ndradipa Ja mtara 636 to 19.10.2010 23"53',38"N r,i.ltd. Director- 639,64 to 86"49',41.83"E Sr Pa n kal Das, 1/P,r1 18.10.2020 23"51'42.07"N 46/P,1. S : S:; Mani Kant 85"49',43.82"E Das, t4t to 1749,1 ri c.- A.t. C. Bos e 151,11 F.D3i Karnani 52/P,1. Siaie 3rd Flor Seet ,'. 153,11 :39 A Koikata- 54

10 7000L7

6 Sri Asit Kumar Fuljhori lamtara 221.7 /P 7 .50 05.03.2011 23"s6',6.2s"N M andal. to to S/o Sri Malindra 07.o3.707L 23"56'13.16"N

Mandal, 86'41'28.59" E At- Su khjora, P.o- to Gundlipahri, 86"41'39.44"

P.s & DistJamtara E 7 Sri Sadha n Dh obna lamtara 25t3/P 2.00 L7.06.20LL 23"56',46"N to Mandal, to 23"56',40.6"N S/o Sri Magaram 16.06.7021 86"41',28.59" Mandal, Eto At. & P.o- Dhobna, 86"47',39.44"E P.s & Dist-Jamtara Sri Amit Kumar Golpa ha ri Jamta ra 2357 /P 11.0 29.08.2015 23"56'16.58"N Pandey, to 86"40'03.49"E

S/o Sri S.N. 28.08.2025 ; Pan dey, 23"56',16.05"N At-Flat no. 101 86'40',07.80"

Lake View, E Apartment, Bihand lawahar Nagar, Kan ke Road

Ra nch i. J harkh and. q M/s Shiv Durga Teliyadih Karmata 8481P 6.0 07.L0.2015 24"05',38.6"N MininB Project NT to to Pa rtn er- Sri Kishor 06.10.2025 24"05'36.7"N Mandal, 86"44',43.7"E S/o Sri Rajend ra lo 86"44'44"E Prasad Mandal, At- Ka ron Road, Karm atanr,P. o & P.s-Karmatar, Dist- I amtara 1.0 11)Sri N ityan and Mouza - Fatehpur 335 4.05 05.02.2014 24"00'21.0"N Yadav s/o Sa lpatra to 86"57'49.0"E PIot no - 335 H akim chan dra 04.02.2024 24"O0',22.5"t\ - yadav Thana- Anchal 86"57'50.5"E Pa Iajori dist:- 24'00'25.0"N Deoghar 86"57',44.8"8 (2 )Sri Mritunjoy 24"00'26.2"N '/adav s/o a5"57',42.A"8 !axminaTayan 24'00'27.9"N ladav vill-H arinad 86'57',39.0"E Thana- 24"00'27.0"N B'ndapathar Dist- 86"57'38.8"E .ran'ltara 24"00'23.6"N

11 86'57',44.8"E (raa,'o 11 Sri Ananad Jain la mtara u5.ul,lu#t s/o-Sri Ashok to kumar jain Main 04.02.2424 roa d ,mihiiam,lamtara M/s Maa shakti Naya dih Narayan )1.ilD 23"\7',15.5A" co rp o ratio n pur to Nto Pro-Sri Gauri 28.02.2A26 23"57',2r.59"N Shankar mohta 86"37'5't.58" s/o-Sri Late Chand Eto qa"17'6l rattan mohta ,io"F sh astrinagar, Dhan bad

13 N arayan ch. Bandarpaha r Bindapat 4.14 2r.02.2016 24"00'31.52"N Mahato s/o- i har to to ,n ni lil?( N arah a ri rn ahato 24"00'38.71"N Vill+po- 86"56',30.30"E Mohnabank dist- to .lamtara 86"56'4t.26"8 :4 Sri Kamal bhusan Golpahari Ja mta ra 2357lP 11.00 08.03.2016 23"56',17.98"N s,/c-Sri t;isutanath to 86"40'r.7.82"8 b h agat,Shastri 07.03.2026 ; chowk Than a- 23'56'2L.Ol"N Sukhdevnagar, 85"40'19.25"E Ranchi -: e.i n;t-h-c'",=r Digha ria Fateh pu t 2.A6 24'03'07.06"N Pras ad yadav s/o - to 86"53'41,28"E Sr Dulal mahato 1"O.O7.2023 V ill- H aripur po- 24"03',05.90"N Chapuria, 86"53'45.L7"E Thana- ; Bindap athar, lamtara 16 M/s Maa durga Piplata nr Narayan 262,26 4.83 24"00'58.20"N pur 3,264,2 E nterprise 86"41',48.10"E 11 p. Pa!tner- z/-t uu 43.la i\4d.N4 ozahim s/o- N Late 5au kat ali vill- 86"41'53.95"E :"russain nagar, Rani

gu n j,W. B. 24"00'57,50"N 86"41'47.7A"E ; 24"0A'52.57"N 864t'57.57"E Total number of operative stone mines as on March 2018 is 16. 3 nos cf leases {Shaded above) going to end by 2t}20. .i ri:l',.:ril.':r l sl Lease Mouza Circle/Tha Plot Area Period Co-ordinates no holder/Compa na no in ny Acre s to 1 Arvin d Kr. Muchiadih Narayanp 143s/ 4.0 8.11.2010 23"58'14.5"N Bhaiya ur P to 23"58',30.8"N to S/o Sri Vishnu 7.L1..2020 86"40'51.8"E Prasad Bhaiva 86"40',52.6"E Dumka Road, I amtara 2 Ash ok Kr. Sinha Banspa h ar Narayanp 693|P 2.0 16.12.2010 24'00'39.52"N S/o Ram Singh i ur to 86"41'16.32"E ; Cou rt Road, 15.12.2020 24"00'45.70"N Jamtara 86'41',10.06" E to 4 Sarobi Mondal Fu l.iori Jamtara 2217 / 8.10 15.02.2007 23"56'8.54"N C/o Asit Kr. P to 23"56'17.03"N a6"47'3-1 M ond al 14.o7.7017 .6'7"Ero Vil. - Sukhjora, 86"41'45.01"E J a mtara

23"57'10.59"N to 5 Akhtar H ussain Nayadih Narayanp ztolP 12.o 26.07.2007 C/o Haji Abdul UT to 23"s7'10.65"N Gazi 75.07 .?077 86"3S',01.32"E to Mongiamarni, 86"38'03.15" E Narayan pur, I amtara o Seema Siyarkatia Nala 92L 2.96 28.L2.2007 23'55',4.70"N , Bh attacharjee to 87"03',14.91"E ; C/o Damodar 21.72.7047 23'55',13.04"N 87"03',04.18"E Bh attacharjee Searkatia, lamtara to 7 M/s lharkha nd Muchiadih Narayanp 743s/ 1.50 28.12.7007 23"58',14.5"N Stcne Udyog, ur P to 23's8'30.8"N Part- Mci- 77.12.701-7 86"40'51.8"E to Ka m ru ddin 86"40'52.6"E Ansari & others, At- Muchlyadih, P.c- Bankuciih, Naraya n pur, Dlst- lamtara M,/s Bholan ath Bardehi Nala ilP 3.0 25.07.2008 23"5g',02.94"N Ston e Quarry to ,86"56',04.19"E ; Satya narayan 24.07.2018 23"5g',05.53"N 86"56',14.96"E Yad av & Others Godia, Jamtara

13 I Sri lavant la m kana Ii Na la 525, 5.47 24.10.2000 Bhatta ch;i'ya 5 25, 5/o Ana nd Gopal 530 & 23.10.2020 Bhattacharyya 531 vil. - Puratangram, Birbhum, West

Benga I sri Umesh Singh Ba manbhui N3la 77 4.98 18.12.2002 Saga rbhanga to Coloney, 71.12.2022 Durgapur, Eiirdwan, West

Benga I 11 M/s Sagar Sadhu Dadar Na la 113s/ 3 28.05.2010 & p to Sri Damodar 27.05.2020 Bhatta charya, At- Da dar, P.o- Devjor,Dist- la mta ra N 23" 72 Sri Dayamay Dadar Na la 954/P 2 14.09.2006 23" 56' 45" to Bhattacharya & to 56',44.3" N 87" 3'6.18" E to 87' (Renewal Dharmdas f' 6.28" E Bhattacharya, Applicatino At- Siyarkatiya, Submitted) Na la, Dist- ta mtara Tt M/sK C.P.L. Banspaha ri Narayanpu 693 lP ) 28.12.2007 Sr Pashuoati r to I i Pullam Ralu 27.r2.20L7 t__ Pa bta Lamp, Naraya npur,

Na la fl341 2 14-04.2008 24 02',41.88"N,86 i'-) Rameswar I Bamunkana to E YaCav, DebiOur, J li P 54' 27.37" Pattajoria, 13.04.2018 I ramtara I 24 02'41.86"N,86 i2l Anirudh I _,'I 54'7L.34"E irwan, Kuswana, I Ma h =shmunda. I 2402'17.60"N,86 P rrdih I 54'29.44"8 131 Ajrt Kumar Yadav, I I 24 02', 37.64"N, 86 3asr, iirnaih, i )3l, \4' 29.47" E rr ria, I

DeoEarh I 15 14.07.2008 S'r Sanleev I Ba munkana Nala 7L341 N-rnar Mishra, ,, p to I 13.07.2018 ( . S!' Niwas I Cha ndra Mishra,

Kumardih,P.o- Cha puria, Dist-DeoRhar. 16 M/s Shyam Banspa hri Na rayanpu 693/p 2.5 14.07.08 Udyog r to Part- Sri Harsh 13.07.18 Kr. Gutgutiya, & sri saurav Kr, Gutgutiya, Both S/o Sri Prakash Kumar Gutgutiya At & P.o- Ka rmatand, Dist-

.l a mta ra 77 M/s Maa Kusrupu r Kundahit 4/399 2.81 11.10.08 Ana purna Stone, to Pro- sri Ganesh 10.10.18 Hembram, at- Harinarayanpur, P.o-Baragoijor, P.s-Kundahit, Dist-lamta ra 18 M/s Diversified Nawadih Jamtara 223h 7 04.02.09 24 3',28.11"N, 86 Byapar Ltd. o09/p, to 46',28.OO"E Pro- sri Bir s7s/p, 03.02.19 Kumar Agrawal, 224 At- Sriram pur &223 Road Dha ndhra,

J amta ra District- .iamtara- 10 M/s Raj Stone, Manjhaladi Na la 504 1 04.02.09 Pro- Sri Anand h to Ral, 03.02.19 5,/o 5n 5rromant Ya dav,

At- J anumdih, F.o-Chapuria, P. s- Binda pather, Dist-lamta ra 20 Smt. lanki Devi, Uda lbani la mtara los:-.l 5 23 56'08.35"N, 86 Wo Srl Gopal p to 50' 17.3s"E Pa ndit, 04.o7.21 At- Udalba ni, 23 57'08.74"N, 86 P,o- Dha n dhara, 50'16.23"E Ps& Dist-.lamtara 23 57', 22.47"N,86 50'09.25"E

23 57' 23.74"N, 86 50'10.64"E 2t M/s Devendra Lokdih lamta ra 362 to 0.9 05.01.11 Stcne Wo;ks, 366/p to Pro- Sri Wakil 04.o7.2L Hembram, 5/O 5fl Rasrk Hembram, At- Lokdih {Pahrudih ), P.o-Bewa, P.s- Mihi.lam, Dist- .lamtara 22 Smt. Sunita Devi Kelahi la mta ra s288/ 1.5 20.07.11

Bha ndari, rJ to W/o Sri Vijay 19.07 .21 Bhandari, At- Kangoi, P.o & P.s.- Mihijam, Dist-Jamta ra 23 Sri Maheshwar Digharia Na la 694/p 1.5 17.08.11 24 02',s6.90"N, Prasad Yadav, f5 54.J6 t S/o Sri Lakhi 16.08.21 Narayan Yadav, 24 02',59.32"N, 86 At- Ha rinada h, 53',59.03"E F.c- Chapuriy:, P.s- Bindapather, Dist- lamtara S!'i Sa urav Kr. Digharia Nala 694/p, 9 08.08.11 24 03',08.08"N, 86 G,Jtgutiya, 831 to \3',1.41"E S/o Sri Prakash 07.08.21 Kr. Gutgutia, 24 02', 9.73"N,86 At & P.o- 53',9.87"E Ka rmatand, Dist- .lamta ra Dho bna la mtara )5t31 30.08.11 Cha ndrashekha r p 2 9.08.21

S/o Late Ravi Shankar Singh, At & P.o- Ba bha ngawa n, P.s- Sarath, Dist- Deoghar. 76 Sri Mani Lal Gowalpipla I a mtara 5o7 /p 2.17 23.09.11 24 o',55.43"N, 86 Ra wa ni, to 50'52.62"E 5/o Late l(huni 22.A9.2i. Rawani, 23 0 56.93 86 s0 At- Babudih, P.o c,4 n2

Ka rmatand, Dist- iamtara 27 Sri Dinesh Chand Murgatona Ja mtara 2046 1.2 25.17.1L 23 50', 10.29"N, 86 Mandal, & to 50'00.91"E 5/o 5n l-(asral 204.7 24.77.21 Mandal, 23 50', 10.10"N,86 At & P.o- Kelahi, 50' 1.44"E Mihijam, Dist- I amta ra 23 50',09.08"N. 86 50'00.86"E

23 50', 09.44"N, 86 50'00.63"E 28 M/s Laxmi Fofna d Ka rmatand r57 /p, 73.12.77 Enterprises, 158, Pro - Sri Kishor 159, 12.11.10 Mandal, 160 S/o 5ri Rajendra Mandal. Al- Karon Road, Ka rmatand, Dist- lamta ra. 29 I M/s Kewaljuria Na la 70 1.5 21.05.12 23 54', 33.45"N, 87 Mahaprabhu to a4' 33.22" E Stone Mines, 20.o5.22 Part- Sri Nimai 23 54',38.11"N, 87 Chand chosh, 04'37.87"E S/o Sri Vijay Pad G hcsh, At- Da {a bar, P.o-

.la mta ra Sri Binjay Bharti Golpahri la mtara 23s7 / 17 08.03.2016 C/o Rabindra P to Nath Bharti 07.03.2015 Ratu Road, Ranchi, iharkhand 31 M/s Sanjeet Chandrade Jamtara s6e/P 2.3 t8.o7.20L7 23 54',01.1"N, 86 lembram epa art & to 49',42.5'E Vil. Amoi, 62slp 17 .O7 .2027 ivi ih ija m, 23 53',54.8"N, 86 Jamtara 49'36.5"E 32 M/s Alert Sawla pur 429 to 4.47 25.10.20L7 24 11',38.53"N, 86 System Ltd. 435 to 31',40.38"E 5n Saiish V. 74.LO.2027 Ccurt Road, 24 11'36.09"N, 86 37'40.77"E

Totalnumber of non-operative stone mines as on March 2018 is 32. The mines are non operative due to technical reasons/statutory clearences. Shaded portion represents the leases going to end by 2020.

sl. Leasse Details Mouza Circle/Thana Plot no Area in Period N( Acres c., c,,-,i r. N^-L-+^ 1 Ke la h; Mrhrlam 2.5 S/o Mathur Mahato to Kali Mandir, Aam Baga n, 02.72.201,8 PO+PS - Mihijam, Jamta r MC. Atikur Rehman Kelahi Mihijam s288/P 5 23.1).2004 5/o Md. Sataur Rehman to iamtara Road, Mihijam, 22.12.2018 iarntara

3 Sri Robin Singh, P u nsia Bindyapatha r 288lP 1.5 31.10-2008 5,/o Sri Pitambar Singh to Vil - Punsia, PO+PS * 30.10.2018 tsrndyapathar, Jaiutati

Smt. T: runlal Marandi Kela h i Mihijam s288lP 3 11.10.2008 r'r'l o 5fl l.(anglal ludu to \,/ l- Siwliwadi, PO-Kelahi 10.10.2018 PS-Mihiiam. iamtara

5r Arun Kr. McnCal Kelahi ["4 ih ija m 25.05.2008 Clo 5ri Kailash Mandal to . J-Kela hi, PS-Mihijam, 25.05.2018 .la.n ta ra Asgar Ansari Gundalipa hi Narayanpur 639 28.1"2.2007 Sr'o Esak Mia, And to ahand Soren 27 .L2.2017 S,/o liten Soren \"/i j.-Chirudih, Narayan lamtara

.13 wa ha r Soren Gopa lpur lamtara 7r7lP 1.8 10.05.2008 C,'o Llkham Soi-en to '/: . Gcwa lpipla, PO- 09.05.2018 Daiishin Bahai, lamtara Rock type 5l no. Mouza eircle/Ihana Plot no Block Area Limiting Co- as per ordinates Ge orefe re n ce (Hectares) N Dolerite 7 Chandradipa Jamtara 843 & 5.3 3 23"53'14.59" / _10 adjacent 86"48',55.49" E Blackstone plots 23'53'15.72" N 86'48'47.59" E

23"s3'09.88"N 86"48'45.72" E

23"s3'05.71" N 86'48',52-76" E

N Dolerite Chand rad ipa lamtara 3238 5.16 23"52' 4t.24','. / -10 86"48'54.15" E Blackstone

21"52',44.46"N 86'48'50.98" E

23"52' 49.O7" N 85"49'00.59" E

23"52'52.7 8" N 86"48'54.-1L" E 23"56',5.07" N Dolerite /. 3 J u rgudih-13 Jamtara 323 & 6.38 adjacent 85"39'52.07"E Blackstone plots 73"56'!7.77" N 86'39'55.00" E

23"s6'08.6!" N 86" 40'A4.57" E 24"00'49.40"N 86"41'58.22"E

24"00'46.65"N 86'42'03.76"E

Granite Pahargora Fateh p u r 1086 & 24"03'13.s0"N Sneiss adjacent 86"52'13.7 L" E plots 24"03'1"5.18"N 86"52'10.05" E

24"03'77.49"N 86'52',15.54" E

24"03'20.06"N 86"s2'12.51" E

# Some other stone blocks which have good mineral potential from mouzas here namely Amjora langartanr, Karmoi, Budhudih, Chatabad, can not be enlisted as the blocks falls under Forest/Gochar land type'

to the required #* These blocks ore prepared on the bosis of geologicol studies ond subiected cleoronces Ircm the concerned depdrunents.

lt : l::il-:r:. i-d,rA* --kr ;}r,

Mouza- Navadih (Block shown in red outline

Mouza- Laxmiour (Block shown in red outline

23 , ,,, . ,', . .t?i.,r,x:. ..+'' ;. itr ..,, '" , ,I - .t'; li. y. :;i:1,-r.li'.\' ." ;. ,. ,..'. ... . '' . :,.,:.:. 'li1' frt' ,], i . :".\,, " . .+ :./;.. . r' ..:.,' .1 . .",i_. :_t!_",r,. ,,.: . ;,,,,i ','f' ffi:,;;r,, ' . 'iff.'- '

MINING STATUS JAMTARA

I]EVGHAR

DI-iANBAD

Mining Status

66 40 r)"E Year RovaltY Dead Rent ?otl - t8 9,4L0,776 1,085,000 2076 - 17 12,033,876 992,000 zu-tJ - .l.o 8,579,000

Year Production (CFT) 20L7 - !8 1982000 2At6 - 17 2980900 2015 - 16 35E9000 i: i

DRAINAGE MAP JAMTARA DISTRICT. JHARKITAND ,,.,.1'ii". t-:f- i -,

I ]ei....",",". t1"..."","",, i ,ln u"..",.-l ", "-.,"" - L q 1".",, t..l^*

Th€ The district is mainly .lrained by the rivers Brahmani, Ma,'urakshi, Aioy and their trillutaries' soon du rirg the ,list.ict .eceives ;l laige. share of the an itual rainfall nlailrly by ihe sorrth west moll pefiod which originates in rainy season an d front the retreating monsoon during the inter n!onsoon pel'iod the Bay of Bengal. The district receives rnost of the annual raillfall during tlle monsoon

The dimate is tropical in Jamtara. The summers are much rainier than the winters in Jamtara. This dimate is considered to be Aw according to the Koppen-Geiger alimate classification. The tempsrature here averages 26.0 "C. Precipitation here averages 1228 mm

28 jiri,'i;1,iia jiA:tii!r,\i,ti) r:iI:,ilii i siJRt"It.i Ilit9ofi i rji: -:

J3Dusry octobcr Novemlr€r Ir.cember' Av9. T€mperafure ('c)

Mln, Teftper*Jre fc)

Ma( Temperature fc)

Avs. Te$p€ratute ("F)

Min- lemperatur€ rF)

Ma( Toffipvatua fF)

Procipfration / Rainfall(mm)

The precipitation varies 306 mm between the driesi month and the llettest month. The varlation in temperatures throughout the year is 14.2 'C.

CLIMOGRAPH JAMTARA

29 TEMPERATURE GRAPH JAMTARA ., r .;i:..., I :iriN,l.'lir'

Jamtara district is situated in the North Eastern part of Jharkhand state. The district is srtuated in the Northern Plain of lndia and eastern plateau and hill region. Geomorphologica lly, the district can broadly be divided into thr-ee well defined physiographic units (a) Hilly area (b) Rolling velleys anC (c) Pedi plain flat country. The gsieral elevetion of the area renges between 150 m - 640 m above MSL. lhe general slope ofthe district is from North to South East.

86',40'0"E 87'5'0'E

GEOMORPHOLOGY JAMTARA

DEVGHAR

z ? 9

DHANBAD

BIRBHUM BARODHAMAN WES-I AENGAL WFST BENGAL

Geomorphology Pediplain (vasl plain wilh highs and lows. associated z z with sDattered pebbies of different sizes derived afler p ? weathering effect 01 regolith soil) - Ridges and valleys (Denudational hills v!ilh immense weathoring and scrl ercsion and interm4otane valleys)

36'4e',C"E

31 ,I r,ll:

Major soil types are Aifisols amongst which Red sandy soils are common and Ultisols of which red and Vellow soils are common.

86"40',0'E B7'5'0"E SOIL JAMTARA

DEVGHAR

z z tr I

DH AN B.4t]

BIRBIlUI,1 BARDDHAI\,IAN WFST BENGAL !!E3T tsE i\! GAl.

z Soil z -o Red Loamy Soils

Red Earth Scils

Red & Yellow Soils

86'40',0"E 87'5',0"E

t

32 ,.,l 1 r,.r l:r-r! rttii

The planning commission, Govt. of lndia, has divided the whole country into 15- agro climatic zones, Jharkhand State falls under Vll th Agro climatic Zone. This State is aiso divided into three- agro climatic regions i.e. lVth. Vth and Vith. Among the three, Jamtara district comes under the lvth {Central 3nd North East--rn plateau region} Agro climstic irrigaticn and crcpping pattern, Jamtara distrlct has been divided into four Agro Ecological Situation (AESS) for the purpose of SREP preparation. One representative village of each AES was selected for participatory data collection through mu ltidisciplinary AES teams. AII the villages selected are located 15 to 50 km froi'n the district headquarters, larntara.

. tr"I .,, ii I l\. ii" al*rc,;;;;; in hightand. lt consist of ro ing open land surface with tong ridges end intervening depressions. Average eievation of the district ranges betweerr 150 to 3oo metres. Geologically the area is comprised with basaltic trap and sedimentary beds. euartz and gneiss are found at some places. Ajay is the major river flowing through the dlstrict. r: , ,,i:'!t_rrt! lltiiiv' Demographic Dynamics in district when seen from a wider perspective have larger implication on the Sustainable Development. The population groMh has been marked at almost 2O,% over the last decade which means it requires more infrastructure support, more health services and accordingly more resources for the same. lt wilt also have implications on a number of important issues in the area of urbanization, migration and development, and on some important variables which impact on their interrelationships. ln the watershed villages 85 percent of house hold are headed by male members where as 15 percent of family is headed by women members. Mostly women members head family when male guardian is not there. lt some cases it is also because of greater awareness among the women members especially who hsve been mernbers of the SHGS- Aceeptance of women as head of the family has iimited acceptabllity which needs to be seen from the gender perspective- This watershed is dominated by people from other communities. The share of SCs and STs Communities accounts for 39.55 % of total population. The distrlct is dominated by the people from OBC and general category but tribals and scheduled caste people also have sizable population. population of the other communities stands at 60.449l, followed by tribals whose population is at 30.29% and SCs at 9.260A. SC I St Population is close to 55% in Fatehpur and Jamtara, Lowest at 2G% in Karmatanr and is t7% at Mihijam NP. Gender ratio of the district stands at 956. cender ratio is best at Faiehpur which is at 968 ad worst at Mihijam NP standing at 890. Average family size of the cjistrict is close to five with Narayanpur having family size close to six and Kundahit having a fanily size close to four.

JJ Population sc ST 0thers Tdal

Popula Popula BlocMNP Male Fenraie Totai HH tioD HIt Population HH Populatior No. HH tioB

Jamtlrrr 63195 60939 t?3vla 1102 4746 lI0t)6 56563 I tJl6 5866q 2t121 l23qm

F ehpur' J55d6 .t-t099 s96-t5 1{t7 6924 8619 4209C ,1327 896t5

Kurdahit 4J137 II J7O 8J9tr7 2991 13002 5822 25309 10719 l65i)6 19532 8l9t)7

Nala 6A17 t 65{l$) 13.1780 3.!0{) l67ltl mtSl ,186?6 l,ls3? 69436 ?8?!ti 13J780

Kllrmrfanr 589f,7 s5329 l132116 1380 7731 2885 21161 16307 45762 2$5'12 r t 52rs

Narayarpur &3971 ?!91n 161%6 167-l 950t 69?0 3S485 20195 I !,I9!{} 78912 t63966

r-P N{ihijanr 19062 2l{01 {0,t63 t 165 5791 {1r 2012 6563 32630 8 t,19 "t0"163

\P- Jaor13ra !5372 1{{}r3 19dl5 788 l03J 721 ll62 !.179 2J2t9 57$

Block and Gender vvise population details

I I i9 ,I fil **i t -*{.#l $ i I! ,'ffi ffi ffi '#i'#i* $,* ;-"5- *:...t-{{

Figure No. 1: Block and cenderwise population details Sex Ratio at Jamtara

Figura No. 2: S€x ratio in Jailtara distrid

ln lamtara district total area covered under forest is about 18L1 KM'z. There is no significant forest existing in the district as reported by the local Forest Office, Jamtatrd'

Distri{t-wise Forest Cov€r Area in Jharkhand {Area in Km2} 2017 Assessment District Geograph Very Moder- Open Total Percent Change Scrub ical Area Dense ate. Forest of GA xm2 Forest Dense Forest 3E tsoka ro t)l 231 271 57C 79.71 3,77t 241 86t 55: 7,7 6t 47.5t -E 79 10< t2 Deoghar 2,47i c tt 202 8.1( )ot 2 2t Dha nb ad 2,O4( C 4t LbL 10.0( s7c 1) J2 6 44 D umka ,761 c -t 62 Ga rhwa 4.Ogi t2: 4lt 85 L,39t 33.9r 2€ G irid ih 4,962 7', 33! 47t 89( 16 Codda 2,26t 1 27C 13t 421 18.5t 5,36( 55( 7,44',) 26.8€ 11 Haza ribagh q 5s( 21( 341 771 1 CS1 38.0( I 19 l.), 1!. ii 'i. i

(h,Jti , q?r 7i 34i 48t 901 3s.6( 72

Kcderma ) \Ll 81 49t 44\ 1,Ozt 40.31 c -2 4,291 47-, 61( 1 Ait s6.0i 8 Lof,,3 1,50' 17t 2r, 111 sat 33_ 5( 2

35 c 2t Pa kur t,a7i 77' 17, a8', 1s.B: 98 Pa la mu 4.39 51 52 62' I.20C 27.3 52 West Singhbhum 462 L,55' 3,36r 46.59 L,O7(. 34.21 )2 E ast Singhbhum 3,56i 5! 59i Ramgarh 1,341 3l ),7( 18t 321 24.5 22.841 1t 35 R e n.hi 5.09 6: 36t 73 1,16t -4 61 sahebsani 2,06 1 25t 29 57! 27.7d 5 21, Sa ra ike la - 2,65-, zi 27t 33; 57: 21.si Kh arsawan c 21 simdega 3,77' 21 871 L,241) 3 2.8t 669 Grand 79,7rt 2,s9i 9,58( rr,26a 23,55: 29.55 2a Total

(Source: lndia state of forest report 2017Jharkhand)

crops of the lmpo rtant trees in c lud e sal, semal, kaha, ashar, mahua etc' inlportant district are paddy, rnaize and wheat.

36 Landuse is a function of four variables, land, water, air and man, each plays in its own role in composing its life history. Land constitutes its body, water runs through its veins llke blood, air gives it oxygen and man acts as the dynamic actor to reflect its types, pattern and distribution. Land varies in altitudes, forms and expressions. Man has played his part on land to portray the different phases of hls ties with lt. The Homo-sapiens moved from one topography to another where climate, flora and fauna also changed. He used land, flora and fauna to fit his limited wants. Men multiplied, their wants increased and become complex, the uses of land also increased, methods and technology also changed. Man was making his own map on the face of the earth to portray his link, adaptation, creation and destruction. Man has cleared the forest for shifting {Jhum) cultivation. He then used the land for large- scale farming, small-scale farming, intensive farming, mixed farming, dry farming, etc. He has used the land for one crop or another is a minor landuse problem, but to use each plot of land for the right cultivation under optimum conditions to obtain optimum yield is a significant problem. Man has learnt the use of grasslands, semi-arid and arid lands to his own advantage by applying irnproved methodology and utilisation of his accornplishments, Over a period, geographic pattern of agricultural landuse are the outcome of concurrent interaction between the variable combinations of natural condition and human circumstances. Primarily, these are influenced by natural condition and thereafter affected by human circumstances because of their colonizing capability. The human circumstances are rnainly responsible for dynamism in agriculture landuse or changing crcpland occupancy.

Therefore, efficient cropland occupancy, say cropping pattern, implies the most successful use of agriculture land, consequent upon development of irrigation facilities and application of modern methods of farm technology. The key to the most important aspect of landuse lies in the relation of population to land. The crux of the review, there fore, refers to ihe stuC'y of the problems in use of land by man. According to R.H. Best, the term lanC use deals with the spatial aspects of human activities on the Land and with the way in which the land surface is adapted or could be adapted, to serve human needs. This leads one back to the village farm and farmer, to the fields, gardens, pastures, fallow land, forest and to the isclated farmstead (Freeman, 1960). The land use shifts from agricultural uses to residential, industrial, transportation, neighborhood retail and service activlties due to urbanization. A true nature of these dynamic qualities in land use emerges from a historical survey designed to reveal the successive development of inherent characteristics of land because 'some changes are short lived whereas others represent a more constant demand' {Jackson,1963). r,,l

F I E z .l >. cz CE t i;tr ; ra E hrl 'l iB eQ F. ,:b L. E E-ar 6.9 E>s nE c tr3 -lq9: F. ,(, *43 t..5 U'J Er ,*&E q4 Er 'J -.i 63 BLOCIi(s)

102.0

FATF-PI ]R 1246.1 1 1246.1 l 27 t8 87 l1ll66 /q. tJ 12A.87 2231.98 4 200.94

'J..r ') r;.-l "l i) i+, .t l i ir:..it: /.:r'., i.q llr ! l

162 0 KL.INDAHTT 2t967.68 919 86 921 36 346124 378.89 108.08 3400.27 0 833.3 8

30995 76 1716 77 1s5.t.78 246 '15 31l] I5 98 75 1179.86

06.5 NAR.AYANPUR 18993.40 I 169.89 ,1022 14 1249.59 20 36 619 53 1'777 07 6 730 64

5 8.8 vID\'ASAGAR 13131 85 731 90 2?70.16 t21.79 28 56 0 869.42 59.75 137.42

Since the area consist of hilly landscape and receive more rainfall it has considerable vegetative cover. Brt d,Je tc ruthless explcitation, most of the forest have turned into bushes devoid of big trees. lmportant trees include sal, semal, kaha, ashal mahua etc. important crops of the district are paddy, maize and wheat. Only 6.42 percent area of agricultural use is net irrigated and major source of irrigations are well and tanks. 86'40',0"E B7'5',0',E i. GEOHYOROLOGY JAMTARA J I

DFVGHAR

z 1 o DUMKA

V/E€ T AEiiOAL ir'Esr a[ltGAL

Geohydrology z - Wedrhered zone gu.ldble for mJde'ale I . .Jr^ ,ru^olr r.c"'Inirneni Ll/ Jir,r^t',ll

Harci ifesh mas3:ve rock- no slope iof !iaufi J.f,aier dcrelopnrerii

Bfj'40',0'E 37'5',o-E

-he district is underlain by the Precambrian crystalline metamorphic rocks, intrusive, Gondwana sedimentaries and Recent to sub-Recent alluvium occurring as thin and dls.onrinuous patches on a iimited scaie aiong prominent cirainage channeis. The hard crystaliines of the Precambrian age occupy 90% of the total geographical area of the district Ttre semi-consolldated rocks of ihe Gondwana formation occur in pockets.

?o The Precamtlrians are hard and compact and do not possess p.imary porosity, though secondary porosity is produced in these rocks due to weathering, jointing, fracturing etc. Ground water, occurrence and riovement in these rocks are manifested through the secondary porosity and permeability introduced in them due to their weathering and fracturing. Ground water occuTs under unconfined conditions in the weathered mantle and under semi-confined to confined cond itions in the fractured rocks below.

The major hydrogeologic units in the distrlct can be subdivided intc two broad groups: i) Areas underlain by fractured, fissured and consolidated formations ii) Areas underlain bv the semi-consolidated {Gondwana )formation.

Granites and Gneisses are the most predominant rock tyPes among all other rocks falling under the consolidated unit. Weathering in Sranitic rocks is pronounced and fissures and joints etc are aiso rarel! developed. These rocks are traversed by iumerous veins of quartz and pegmatite. Weathered zones of granites and gneisses are the most productive zone for ground water development. The depth of weathering varies from place to place, which influences the aquifer characteristics. The drinking water and sanitation department has drilled a number of tube wells in Jamtara district having a yield of approximatelY 80 liter per minute. The dug wells in this formation has a depth to water range from 4 m to 9 m bgl and the wells can sustain 2 hours of pumpiag with a yleld range of 4000 to 6000 liters per hour. These aquifers are main!y unconfined to semi-confined in nature. Dug wells within the hard, fractured granites cannot sustain long durations of pumping. Fracture porosity plays an important role but with varying degree, in different parts of the area depending upon the pattern and intensity of joints and fractures' The potentiality and yielding property of these aquifers vary considerably. Bore wel!s can be constructed tapping the deep-seated fractures and joints- J lie areas underlain by the semi-consolidated (Gondwana) formation occur in isolared pockets in the noflhern parl ofthe district. The rocks are mainly sandstoles and shales belonging to the Barakar and 'lalchit fr.:r'mation Barakat satrdsllrles ale coatse to nreciiun grained- rveatheled:rr nalure and t-,tay Lre a productive zone tbr ground u,ater development. Exploration r.lork has to be taken up for knor.vine detail aquifer characterisiic olGondvrana formation. The yield of wells in this lbrmation is less than l0 mt/lrr Wells constructed in sandstone yield better than those in shale. Depth ofopen rvells in this ibrmation ranges lrom 5 to 12 m bgl Dug uells can sustarn pumping of I mi ofwater per hour with a moderate recuperation rate

@tf tf E r-.;-'lur EI I E fl

41 ( iies.",:Eetou oi depti: to t{aler le'.'el ci pLlii-lut'rllsc'3ll1x.od rIc';e:r:ber l0l li lbr [$-5 il .Iau:u.r di:$ci rr pre;e:::ed belot' trble-l Tr.ble-) C;rteg,-''n:inon ci depu :o rvater le','el of poet-rrotlsrrot Pelod 5t1';enrber :0: I ) 5o. of Deprh to 0-l .Dli r- 10 iu) 10-i0r u:i n ell-. n:rtel ler tl nea.,ured (m hel) \Iin ]\Irr \o Nc. \o Ic.

I 0 1.6_i r 9l 0 0 _1 ,\ 0

A17

s lr s t lh gf f f oi 9. 6 ;"s r.rir' #'lri"',:l i:er f,rIoco ?'Eeff i 5I 4 4# !' hlrD i.:!]rlj Ft :1. iii'-,r: l.-1:.ir:lllii 11-il.l!rt: !i!rl liii:.tr !-ir! i ln the rural areas the entire water supply is dependent on ground water. Ground water hr development is mainly carried out in the district through dug wells and Hand pumps' Dug wells are in genera! of 2 rn diarneter and between 8 to 15 rn depth, depending on ihe thickness of the weathered zone, tapping the shallow ground water in the weathered zone and uppermost slice of the basement. Large number of dug wells used for drinkirg water is under private ownership for which there is no reliable data. Over the years Mark ll/ Mark lll hand pumps are being drilled in large numbers for ground water development. These hand pumps have the following two major advantages i) are less susceptible to contamination from surface sources and ii) they tap fractures between 20-60m depth which have been found to be iess affected by seasonal water level fiuctuation an.i thus have lesser chances of failure even during extreme summer. ln rural areas of Jamtara district th€ number of hand pumps drilled by PHED is 9561 of which 6815 are under working condition. In ihe urban areas ground water plays a supPlementary role in water supply, the major supply being made through dams, reservoirs or weirs across rivers or stTeams No authentic data is available on the number of ground water structures caterinB the urban water supply. For lamtara urban area the dependence on ground water has been considered as 15% . As per the latest resource estimation carried out following GEC 97 methodology, the overall stage of ground water development in Jamtara district is 22.94 % indicatlng sufficient scope of deveiopment. The ground water resouice of jamtara district is shown in the table-5 below.

.-:. .1,.,r il-:lt !i .\i l,i!:ir.!i ! {r{,_l..it;: Ground water Resources of the district have been evaluated based on the recommendation of the GEC-1997. Resources are carried out on the bloCk wise basis for the year 2009. Total dynamic Resources of the district come out to be 149 03 mcm' Total ground water drafts for all uses are 39.9105 mcm. Stage of ground water development ls 27?6. As per the future ground water development point of view, all blocks of the d istrict come under the safe category. 5 h i.- lb l.r BLOCK WrSE GROUND l lArER RESOURCES OF .IAMTAR.\ OISTRICT (AS ON a009) :r;nir-; l;l):irl r'l !il_le h :.1 A:,9i1:,n iriir! ',:itlra i:r riLn,l ti ',t:. etil .rt i "r,,',,r. '.i;ie :;,:,rteda ,!ite ,l - !li lii ::i;f Eii A,iiii:'+rh, li l ri,li!,:r. A r(-i idr:ri:: fl;'f: i :.-'lJr 1.,:ai;,r il{ I i r-11 iHe-rr i hJrit i' t!'le 'e- ;rl:er i!: ti! .: l.r ['i]1, Fn-r1i lii'ri1 't i.,i l Ij,rt: iil.l +: t+.:: ira,.i: l:l.r.li t 1!.1 i i,:.ri ItI:.ii : -.1.1 9AfE

!:r:]l,ihil +l;r".; ii r.:g r r.:-i .::rE.lr l-r.5'l srf

j.i-i 1.r sart I I'i +11!,1 Jti,1 i :r,1i,5,.1 ] sAft J lJ.t;rtfi 1:1r,!l l:5.:: i+.tn P* I'r sAFT l l!ir 1:' tili.-1: 1:!- 1i r if,:.{..i: :i.rj

ri-.L:,il-l li,---!.,1-l] .]jll{- iti !.}.1,.L!.1 l-5:i-i.:r. :!--1.:i-t!*-!il;"i-L:

Some ofkey ground water reiated issues are

n) I-ow stage of Ground water development b) Locating suitable sites for bore *'ells c) Siritatrle design of dug wells atrd liat'd pump; fl$urerses: ai opii."i O"r"jtp.eni of irrigation inrensrtv bv deveioping ground water a\'"ilable for camps' NGO's and e) Cieating public awareness for conserving ground water through a\ aren€ss nrass medu.

Ar1al.eress & Traini g activity -NIL

\tass Awareness Campaign (l\1A P) & Water Management Training- NIL

Programme (\ MTP) bY CGWB:- NIL

{REA NOTIFIED BY CGWB/SGWA - NONE

46 i r., .- : } i ii i 1r. r j j ',i1:Ili t | ; ar ,l: :r:ir,ir ri: i ::;,rirr i| iir i:it

.oa"rz ,gr,.Ez

.g'l' rn {o^'

-:I 9; aF ebC) l.:- a, t'-Z c) *: -l- c :io i7 ]:T i! 1 t-

L..l E o- :T -J 4 trJ I :a - (') .:; .,E 2Ul (,) Fi -o ; [o r:i,{i) .00..12 ,gr,.tz E i'l

Ground water development in the district should agricultural be stepped up to give boost to sector. Ihe present acreege under irrigation which is just cultivable atea can over 9% of total be increased by development of ground bore wells. water through dug wells and

ln the hard rock areas, pin pointing suitabre sites for considering bore wers is arways a cha,enge. the anisotropv in d:,t1bu,tio.n oi f,".trr* .i-i""p". I"ruf, suitable sites may r€mote sensins techniques ln associaiion ffff:i#jlii: riith geophysicat and hydro-

For deriving optimar benefit from aquifers in areas under fissured formation should be so designed the dug wers that it penetrates the weathered .onu the underlying ., *"tt as top part (1-2 m) of bed rock so as to derive the b"*fit .f and shallow ;;;.;;tilw For hand pumps tube wells the casing provided against,fr" *""it "quitu.. at the bottom zone should be slotted so that the we' can extract sharow ground "r"O water arso. rn urban areas use shallow aquifers should be encouraged. of

The surface run off in urban areas and its peripheral parts augment the ground -t"ri should be harnessed to water resource through approp rir,u roof top n,qu"r. For urban areas rain water harvesting and.artificial r.ctra.ge i, *"r, ,ri .or". Location and design shoutd be suided by i,varo"slophvs;r-;;;rr. ".]^:Trecharge "r.r"y-: sites for artjftc,at shourd be taken up if fractures are avairibre .noii"-i"p,'' should be governed of the recharge we, by the depth ot occurrence of the fractures_ I b

jr,"r- .,. r. r j j r;. r i.i ::r j.'. t','i i ",;.; :-

sets in the middle of lune and The area receives rainfall bY South-West monsoon' RainY season lasts till Sept€mber.

2015 YEAR 2013 2014 2015 Avg Avg Sl.No Month AvB AV8 Avg 17.50 1 lan 10.10 0.40 9.10

41.60 5.70 7 .34 2 Feb 6.1.0 25.70 56.30 s.20 3 March 5.00 0.50 20.80 42.lO 0.80 4 April 30.10 29.90 9.30 31.10 i22 3A 5 h4ay 52.20 L30.80 87.30 234.1C 6 lune 151.00 234.90 165.50

779.10 578.20 360.70 7 July 419.10 742.sO 342.3C 8 August 207.90 316.20 219.50 3 -?4.60

9 29i,80 204.9G

7 .30 39.30 10 Oct 50.00 24L.30 11.30 0.00 0.00 11 Nov 7r.r0 o.0o 0.00 0.o0 0.00 1,2 Dec 6.50 0.00 0.00

No NAGPUR RMc/CS-312' dated The lndian Meteorological Department, Nagpur, vide letter viz' Normal dates of onset and L8th lanuarv, 2016 has provided the perioJof Rainv Season duratlon for the period is Withdrawal of South West Monsoon over as state-wise- The 10ih lune to 15ttr October.

49 The geology of the area mainry comprises of chotanagpur Gneissic comprex i. the southern poftion of the district which covefs r.rosi of tl're district an.l forms the basefileni rock ot Frcterozoic age. chotanagpur Gneissic comprex consists rnainry cf of granitic gneiss, erso patches of amph ibolites can be seen at p,aces in pockets.

The chotanagpur Gneissic comprex is overrain by patches of Gondwana formations in north-central po,"tion oi the district exposed in Lalmatia area . ln the eastern part of the district basic rocks or'Rajmahal Traps iound which gives ihe area an undulatirrg pattern. Ai places Lhese fcrmatic s are traversed b'/ Degmatite and dolerite cykes. rn nor r western ccnicn of the area is covered by quartenay sand and alluviam

The district is underlain by the precambrian crystalrine metarnorphic rocks, inlrusive, Gondwana sedimentaries and Recent to sub-Recent alluvium occurring as thin and ciisconiinuous patches on a iimited scaie along prominent drainage channels. The hard crystallines of the Precambrian age oecupy 9o9d of the total geographical area of th? disti-ict. The semi-consolidated rocks of the Gondwana formation occur in pockets. The precambrians are hard and compact and do n01 possess primary porosity, though secondary porosity is produced in these rocks due to weathering, jointing, fracturing etc.

GROUP FORMATION LITHOLOGY Quartena Sand and Alluvium C retaceous Dslerltes . Dykes and Pegrnatite J u rassic Gondwana Formation Alternating layers of Sandstone Triassic Shale, Coal and Silistone Perm ian

Pre-Cambrian Chotanagpur Gn Granite Gneiss , AmpftiOotite anO Comolex older metarnomhics ti GEOLOGY JAMTARA -l_t'

IIi.\,GHAR

DIIAI.]tsAD

v,ra sl BEl.l-1AL

Geology

Un.-lassifi ed Cuaternary Seilirrenls

Ratnrahal Traii 8a-aall r ii'ter l.6ppean b+ds che(

Barakar fornlation ffiffi Tetch,r fonral,,rn ChhotanaEpur Gisnlte Gnels!: C"'mpiex l-lniiassliied iVetamorPhrc ri: i ij Eastern Gliai Supei Croup 46"40'0'E RESOURCE N JAMTARA ,l 1--

DEVGHAR z

DHANSAD

B RBIIUII EARODHAMAN V{ES T gENGAL .!VEST tsENGAL Resource Unclassrlied Ouaternary SeoinrentS

RajmahalTrap Basall / late. Tr?ppPan heds. cherl

Siltlone. Sandstone and Shale w(h CoalSeam

Shale, Sandstone & Conqlomerate

l-lnclEssrfied Granite Gneiss w h e claves of Inelamorohics z Garnel Brotite Gnelgs

I ill.t cmph;nolie Hchblends Schist. Epioorite 1i,.,':Li r,tetaaorite m Nlrca Schisl lir= Khondolite / 6arnel SLlhmar(e Biohte Gnerss

66'40',0"E 87^50"E iriir i:.'i, t

Almost all the 24 districts are affected by different kind of Disaster. There is great need to strengthen the capacity of State, District, Block and newly formed Panchayat level of departments, institutions and functionaries to respond to ihe Disaster at their own ievel in p:rticip3tion of c-ommuniiy. iharkhand is ,rulnerable to foilowing kind of Hazards-- . Drought, . l\4ining Accidents, . Chemicaland lndustrial Haza rds, . Lightning, . Bird Flu, . Flood, r Earthquake, . Fire / Forest Fire, r Elephant Attacks, . climate change, Biodiversity loss, r Naxalism/Landmine Blasts etc.

Major Hazar Name 0f Hazards No. of distric Name of the distri.t affected affected districts sl Drought All the 24 All districts affected 1. Districts (2010)

l- Iood 01 {Sa h ibgunj ) 2.

Flash Flood 03 (, Saraikela, Ranchi ) 3. Foi'esi Fire 09 (carh wa, Palamau, Lateher, chatra, 4. , E. & W. Singhbhum, Simdeaa,Gumla) Lightening 09 (Palamau, Chatra, Latehar, Kod erma, 5. Ranchi, Glridih, 9 Haza ribagh, Loha rdagga, Dumka) 6. Mining Hazards 09 Latehar, Ramgarh, Dhanbad, Loharriagga. Giridih E & W Singhbhum,& Koderma Earthquake l Flazard .- Zone lV 02 Districls (Codda& Sahibgunj - Partially)

( . Sahrbgun;. 6arhrva. Zone lll l5 Dish icts Palamau- Chatra. Hazari[rag)r. Koderma. Grrrdi h, Bokaro, l)hanbacl. Deoghar, DLunka. Godda. Jamtara- Jiuntara)

Zone 11 7 Dist cts i Lohardagga. Ranchi, Ramgarh, Khur1i, (lumia. E & W. Sinilhbhunr)

Thousands of miners die each year around the globe due to mining accidents, especially from underground coal mining, although hard rock mining is not immune from accidents. A number of coal mines in the state are affected by fires leading to steady destruction of precious energy resource. The reason for mine fires presumabiy invoives the phenonrenon of spontaneous heating thrcugh two interrelated pro.esses viz., the oxyge* ccal interaction or oxidative process and the thermal process. lt is estimated that about L0% of total national coal Tesources are in the fire-affected areas. Although underground mining has considerably less impact than opencast mining on iand, lt causes enough damage through subsidence as observed in Jharia 3nd R3niganj ccalfields. A,Eart from this, leaks of poiscncus gases such as hydrogen sulphide cr explosive natural gases, especially firedamp or methane, dust explosions, collapsing of mine s opes, mining-induced seismlcity, fiooding, or general mechanical errors from improperly used or malfunctioning mining equipments and improper explosives underground can also cause to caiastrophe.

-ihe Chasnaia mining ciisaster happened on 27 December 1975 in a coai mine near Dhanbad caused by 3p explcsion in the mine followed by flocding which killed 372 rniners.

The Dhanbad coal mine disaster occurred on May 28, 1965, in a coal mine near Dhanbad. On the fatefulday, there was an explosion in Ghori Dhori colliery near Dhanbad, which led to fire in :ri *, .ti whi;h k;lled 375 mrnerj Tpact on Environfirent due to mining activities varies based on the quantam of production 'ate proposed. The different activities envolved before & during mining are narrated below, "!hiah helps to asses ihe itrpact on erivironmEilt.

Exploration: #

A mining prqect can only commence with knowledge of the extent and value of the miirei'ai oi'e d€posit- lnfornration about ihe location and value oi the mineral ore deposit is obt3ined during the exploration phase. This phase includes surveys, field studies, and driliing test boreholes and other exploratory excavations.

The exploratory phase may involve clearing of wide areas of vegetation (typically in lines), to allow the entry of heavy vehicles mounted with d!-!lling rigs. Many countries require a separate EIA for the exploratory phase of a mining project because the impacts of this phase can be profound and because further phases of mining may not ensue if exploration fails to find sufficient quantities of high-grade mineral ore deposits of economicalvalues,

Developmeni

if the mineral ore exploration phase proves that there is a iarge enough mineral ore deposit, of sufficient grade, then the project proponent may begin to plan for the development of the mine. This phase of the mining project has several distinct comoonents.

. Site preparation

lf a mine site is lccated in a remote, undeveloped area, the project proponent may need to begln bi/ cleai'ing lanci foi'the consiruction of staging ai'eas ihat r,vould house project personnel and equipment. Even before any land is mined, activities associated with slte preparation and clearing can have significant environmental impacts, especially if they are within or adjacent to ecologically sensitive areas. The EIA must assess, separately, the impacts associated with site preparatioh and clearing.

. Active mining

Once a mining company has constructed access roads and prepared staging areas that would house project personnel and equipment, mining may commence. Alltypes of active i-nining shai'e a common aspect, i.e. the extraciion and conce ntration (or beneficaaticn)of a metal from the earth. Proposed mining projects differ considerably in the proposed method for extracting and concentrating the metallic ore. ln almost every case, metallic ores are buried under a layer of ordinary soil or rock (called 'overburden' or 'waste rock,) that mUSt be morred or excavated to allow access to the ore deposit. The first way in which proposed mining projecls differ is the proposed method of moving or excavating the overburden. What follows are brief descriptions of the most comracn methods.

. Open-pit rnining

Open-pit mining is a tvpe of strip mining in which the cre deposit extends very deep !n the ground, necessitating the removal of layer upon layer of overburden and ore. ln many cases, logging of trees and ciear-cutting or burning of vegetation above the ore deposit may precede removal of the overburden. The use of heavy machinery, usually bulldozers and dump trucks, is the mDst common meas of removing overburden. Open- pit m,ning often involves the removal of natively vegetated areas, and is therefore among the mosl environmentally- destructive types of minlng, especially wlthin tropical forests-

. Underground mining in underground mining, a minimal amount of overburden is removed to gain access to the ore deposit. Access to this ore deposit is gained by tunnels or shafts. Tunnels or shafts lead to a moTe horizontal network of underground tunnels that directly access the ore. ln an underground mining methcd called 'stoping' or'block caving,' secticns cr blccks of rock are removed in vertical strips that leave a connected underground cavity that is usually filled with cemented aggregate and waste rock.

Although underground mining is a iess en vi ron menia lly-d estructive means of gair'riirg access to an ore deposit, it is often more costly and entails greater safety risks than strip mining, including open-pit mining. While most large- scale mining projects invoive open- pit mining, many large underground mines are in operation around the world.

. Disposal ofoverburden and waste rock ln almost every project, metallic ores are buried under a layer of ordinary soil or rod< (called 'overburden'or'wasie rock') that must be moved or excavated to allow access to the metallic ore deposit. For most mining projects, the quantitv of overburden generated by mining is enormous. The ratio of the quantity of overburden to the quantity of mineral ore (called the 'strip ratio') is usually greater tl'l3R one, and can be much higher. For exan:ple, if a proposed mining project involves the extraction of 100 million metric tons of mineral ore, then the p!-oposed mining project could generate more than one billion metric tons of overb urden and waste rock.

These high -volu me wastes, sometimes contain ing sign ificant leveis of toxic substances, are usually deposited on-site, either in piles on the surface or as backfill in open pits, or within underground mines. Therefore, the EIA for a proposed mining project must carefully assess the management options and associated impacts of overburden d isposal. . Site reclamation and closure

When active mining ceases, mine facilities and the site are reclaimed and closed. The goal of mine site reclamation and closure should always be to return the site to a condition that most resembles the pre-mining condition. Mines that are notorious for their immense impact on the environment often made impacts only durinE the closure phase, when active mining operations ceased. These impacts can persist for decades and even centuries. Therefore, the EIA for every proposed mining project must include a detailed discussion of the mine Reciamation and Closure PIan offered by the mining proponent-

Mine reclamation and closure plans must describe in sufficient detail how the mining company will restore the site to a condition that most resembles pre-mining environmental quality; how it \^lill p!'event - in perpetuity - the release of toxic contaminants from various mine facilities (such as abandoned open pits and tailings impoundments); and how funds will be set aside to insure that the costs of reclamation and closure will be paid for.

I Human displacement and resettlement

According to the tnternationa! lnstitute fo!'Environment and Development: The displacement of settled communities is a significant cause of resentment and conflict associated with large-scale mineral development. Entire communities may be uprooted and forced to shift elsewhere, often into purpose-built settlements not necessarily of their cwn chccsing. Besides losing their hcmes, communities may also lose their land, and thus their livelihoods. Community institutions and power relations may also be disrupted. Displaced communities are often settled in areas without adequate resources or are left near the mine, where they may bear the brunt of pollution and contamination. Forced resettlement can be particularly disastrous for indlgenous comrnunities who have ;ti'ong cultural and spirituai ties to the lands of their ancestors and who may find it difficult to survive when these are broken.

!!i.1,.. ',:.'r;:,-i,,ri-,1i iir.j r.. J-.i r.-i 1:f.i rit;!:-: ilr. i:', ti i!:lfuliijt:i The most important environmental impact of mining projects are:-

I Acid mine drainage and contaminant leaching

Acid mine drainage i$ considered one of mining most serious threats to water resources. A mine with acid mine drainage has the potential for long-term devastating impacts on rivers, streams and aquatic Iife.

57 HARM TO FISH & CITHER AQUATIC LiFE:

animals and plants can be severe' If mine waste is acid -gene rating, the impacts to fish' a pH value of 4 or lower - similar to Many streams impacted by acid mine drainage have in streams such asthis' battery acid. Plants, anima!s, and fish are unlikelYto survive

PERPETUAL POLLUTION:

can continue indefinitely causing Acid mine drainage is particularlY harmful because it severitv of water quality impacts from damage long after mining t unauO' Due lo the ", west require water treatment in acid mine drainage, many hardrock mines across the ls virtuailv impossible to stop perpetuitY. Even with existing technology, acid mine drainage once the reactions begin. generations will take responsibility To permit an acid generating mine means that future hundreds of years " for a mine that must be managed for possibly

lmpacts of mining proiects on air qualityr

are: The largest sources of air pollution in mining operations

resuit of excavations' biasting' Particulate matter transported by the wind as a transportationofmaterials,winderosion(morefrequentinopen-pitmining)'fugitivedust haul roads Exhaust emissions from from tailings facilities, stockpilesl *Jt a'*pt' and mobilesources(cars,trucks,heawequipment)raisetheseparticulatelevels;andgas emissionsfromthecombustionof'fuelsin'station"ryandmobilesources'explosions'and they undergo physical and mineral processing. Once poliutants enter the atmosPhere' pollutants can ca use seriou seffects chemicatchanges before reaching a receptor' These to people's health and to the environment'

lmPacts Huma. health, Emissions Atmosphere transported,diluied, Environm enl iw ater, soil, wildii{e), IUobiie and stationarY Pollutal]ts are physical and chemical changes lnfiastfucture, sources, {can be measured undergo and.ontrolledi

significantlyto airpollution' especially Large-scale mining hasthe potential tJ tont'ibutu in the operation phase. All activities during ore extraction' .Ottt:::]19':1OI:::1: processes and materials that generate transport depend on equipment, generators' heavy metsls' carbon monoxide' hazardous air pollutants such as iarticulate matter' su lfu r dioxid e, a nd n itroge n oxides' in excavation pollutants include heavv vehicles used Transportation sources of air mining site' and trucks that transport transport rnining operations, cars that o"Itt""' "itn" depends on the fuel and emissions from these sources materials. The level of pottuting small' individual emissions can be relatively of the equipment a malor conditions ln addition' mobile sources are emissions t"n'"*'iftt"tl Lt oi toncern collectively these 'uui volatile organic compounds that source of particulate 'na '"*"'' ""J*'rno"o*iO"'ground-level ozone' ;;tiiir;" ignificantlY to the formation of stotioD$Iyjgw power generation from combustion of fuels in The main gaseous emissions are of precious *urting operation-s. Many producers and drying, *rrr,ng,lna and installations, iJ off*ite refine'ies, Typically' gold metal on-site, or'-,.'rn'oo"* metals smelt produce elevated levels of is produced in meltingfluxini tuln.."r,r,*.u, silver metals' arsenic, iulfur dioxide' and other ";;;;;J;;;r", Fuoitive emissions of materiars; mine incrude: storage and handring sources of fugitive emissions common and roadwavs associated with fusitiv" au't, urt'tine' ioil;;;;;;;;'"s' orocessins;t,nffi#iir;;;;1.*n p:r"""d ponds; and.w:-

Noise and vibration

engines' Ioading include noise from-vehicle pollution associated with mining may Noise ttt**' O:*':' C:n":t-::^' and other sources and unloading of rock into steel O"rnp?tt' or.'r ng' crushins' srindins' cumulative impacts of shoveting' ilii'n* ?'"toiP'-t^"-l,tlln' '"0 and nearby residents' *.0 t,tj"'t *n slgnificantly affeci' wildlife operations' but of equipment,used mining associated with many types Vibraiions are viu*tion has affected-in the stability of brasting is considered tire maioi mining living- near large-scale open-pit ,nf rastructures, buildings' #;"';;';;ople 2000: ""0 "J"tu by the European Ufiion in operations. According to a stuaylo*'ittion"a lead io noise' O'"tt'"* connection withmining can "shocks and vibraiions as a *'"'"i life' on which i" t"t""Oi* 'n The animal dust and collapse of structures '"nabited.areas' might also be disturbed'" ir'," lo." i popuiu,ion may depend' out of ="qulul-ql identified that are found to be new potential areas have been I nos lrra.i in area as per field Forest or protected ,;;-;; tt"ig"r ?r ?:* Reserved verified by consulting with DFO' lt is recommended i" U",,t.i" observation. opting"r*r for Ec or any other statutory sabhalother oritir"iuror" co, Gram "utt *1"-'f:::t of stone in the it is tn int"''*l"Joilt" rn9"119 clearances, since operatlng mines lease by expiry of-irr;ontv ot existing oresent scenario due to and get the sJcn'p'Ji"nilti at;ertain interval ?020. it is proposed to iaentiiy "'"tt data bank of DSR to be updated'

District Mining Office - Jamtara Distrid Forest Office - lamtara by T' M' Mahadevan oeology ot eil'ar and lharkhand of Disaster Management Report Natioial tnstitute state Unit go;rd' Ministry of water Resources - Report of central Ground Water Office, Ranchi, SePtember 2013' of lndia Maps from 6eological Survey gov'in . htto://www.iharkhandminerals

ttj;-U"' - t t Iogllt fNILANf,AN 6INHA) 'crratp?rst , D u v''lo

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