No Udyo! Bhu{Kh '-a)Laohu'r07r2049 - ta.e.l"*

Pr'a-

R/ovlllag.Abhaypur P o Btudrak ri

rehsnAmb oisfi una. H P

App@.r ot wolkinsrun€nvlonn.nl tl.n.g.n..l Pl.n ol.r.: .pplLd l(rhc ghnr ot Mlnor Ml..nl Ld.. lor .nr.crbn/coll*$o. ot..nd,.lon.b.lfi lmm xh. {o,- l/1 & 7r1 n..4nng 1,l.24.93 Hel!. falllng h rs.u!M.h.r xoodRanoh ot T.rBrr J.!w.n, ol€ri. K.ng.., tl. P, (Govl. Lrnd, Rlvrb.d)16r,r.h Lrn .of lnl.nth.. b*n Isu.d on l9-11-2013.

rn ex6@$ ot po@rs conreired by sub Rure 4 ( D ot rule 21 ol Him&hal P€de:

Mro, M'neBE (concessDn) Rev ot H P iolircalon No Udyoe r(F)'

61?004 daled 1dh Fob 2OO4 I he.eby apflde lhe .bore *id wsk'ngtum-Envnonmenl Maiaseme

P ri lor ir. DuDose of obLinhg Envnonmenr clea€n@ lbm ft ffp€lenl .ulhorilies ol be a(

sppr ed for g€ nr of min iiq rea* The wortidq plai b apDr@d ior . pedod of ltue !€.8 tom lh. dale

.r€cur on ot m .ing l€€se d*d Tnis sprBd is subje.t b $e roLtuing @nddons:

r lh6l rhe woian! @m-€nvto.m€d iranaqemenl PLan ie .pp.ored wilhout pqudice lo any orh

raws appli€ble io lhe m ne/..ea lrom lme lo lme whe$e. m.de by lhe ce.lEuslaE qovl or a'

Thal0is appo€l of the Wodang-cud'Eivnomed Management Plsn dod rcl in anv vav 'mI

the .pproval or 6ovt 'i Ems or ?ny orher prdl.iorc o{ rh. H. F Minq MineEE (Conese.

R.vised Ruree. 1071 o. ant olher lM mcludhq Fo€.t (comenalion) A.L 1930, Envbnmr

Pmb.rion act 1936 a.d the tules nl sHuies oldeB a

suiderines as may b€ appli€b.a lo le$e .re lrcm time lo lime

3 Thal rhe wodng{um-E.vLrcrrenr Managemeit Pran 's

apprred wlhoul pejud.e t0 any otd(

or d €criom lbm any coun or @mpetent juisnidM.4 Thar rn caee sr.t€ Georogisr Geologi.t ..y other nsP.clrns ofierr'official of Gslogsl wi

oepa.t ent ot lndGlries alter feld hspettm .ol@s lhal poposa s madq . nd rclking s shtun

ltre min'io re$E by Ih€ RoP need ed.in corietuns/ amendhe|ts due lo chanqe n @ndlc

eiiher nanna or man rod3, lh€ nspeding olfer can r*ommend ..c*ry ahddmeiG d I

wo*ing-@mEnvnonm.ntManagefredPlandanyp.ido1hmeinth

5 That the hase hoder shar p-rcurc Envnone cea€ne trm 6e mp€leil aumoily as

Cnvtron rcnlar ,npacr &3ees{er r rc! le lor, 2006

6 Thst n e* add'lional oonditrons aG impo$d by ho Mi^'$ry or Envnonmnt a Fd*ts Govt

rndia sh're .ccoding crea€nce undq E a noliletion datod 14 9 2006 and any cond lion impo!

by u6 sra!. Govr. *h{e qEnted Gnryar of mhiiq lea* the sare shalL have to b€ rnetpoEted

makins necessary amendmenrs nrheWol(n9 cum Envtonmenr Managemenr Ptan byllle €sse'

susDended b€lorc lhe exo r

dr rhe e.se p€nod due ro any reason lhe approval or Wo*rs{um-Envno.menl Managemer

Plan sh.n slaid automalcarry canc6led

Thar rhe rease horder sh. cary out produohon or mine.atstlc y n aMrdarde ro rhe produ.t'o

Thar no peen sharrundedake m'nLns opeGlois n any mnmg

anagemenl PLan appbveMmo. M ne.ars (con@ssroi) revrsed Ru€s.197r

Thar the rease horder shar carry olt wod(ng in the h'insEnvnoinent Manag.menr P an onry afrer obbn'ng pemisson

l'omthecddpelentaUlho.ly

10

En.ro*d: coPY or aPpoved Wol( ns{umEnviEnment Management Plan

under.6us 21 (4) ('D or H t

Lease area as per Work'ng{un

ro m* n lhe minnq rease arc

(NnRlsH DHTMANt

Conact No 0l?7 265?:1119

That r rhe m nrns operar r's are n he apprcved woftig cun

srare Geotog 5r ceor.sisl A$ slant Georogrsr.nd rhe M fuiL or:nyor ihe mining opeEsons a

suchopeGions as m?y be nMssaryto resloc rhe condftons n lhe mne as eneeged under rsaid Wort ng-cum.Envnoimeni Man.gemenrPlan

ules a.d suidellnes pena nir

b min ig 'i rhe context of rhe wo

ave b€en withdGwn w

r The Mm'nq orrics Kans a at DhaEmshara, Dsr X:iora,Envircnment M.naqem€nr Pran rq tunher neces$ry &rbi

2 Sh K C Karmh ceolr8is(Rcrd ). Bl.ck-F Ser No 3, Knollos$ood HousinE sMrt colo,

ONDRESI I DTI]M N)

ConuctN. 0l?7265?1:19

\\rCIRK[NGe[mdm[\rnR0NhdH]uF

PLAN

RIVER BED

]{A[E OF APPLICAI{TAPPLICA]IT ADDRESAAREA TEATURETETITNOHALLEASE LOCATIOII

tTT. AIIITA KUTARIvrLL ABHHTPU& PO BHADRAKALT1+i2/hga HectarrsRAlrOltTEIIEIL JAEWAI{DI$TRIGT KAilGNA

PFopa;ud B!/:KC.l(rbctr (nQP)eGobtht (nGff.)BhGL# S"t nh Qlftolbruod {Orsir{ BoadGolony $hlng ([.P.) tzt002

. No.ll.P./R.Q.P./t8/tl2oto

FEBRUARY,2014

$!e

1 .2 status orlhaEiii;;i1.3 Minerab whicn ihe Appti6nt inljends bmine1.4 Peiod fo. which tne mining tease is gra.t€d1.s Nam€ and address of lhs H.p.R.e.p. prcpa n9 the wo*ing pten.1.6 RegistrEtion No ofR e.p1.7 Nams of Prolp€cting Aoency .

t-"catonanamomFcrororiiEi]GcetoiTiii

1.1 c.neral NanE and add€ss of Applicant

2.1 Topcicet numb.r2.2 L@ation of th6 Ared

2.3 DElance frcm jmpoient pts@s in Kitomeiers

llllroduction: -

2.4 ADomach of the AF;2.6 D€l5ilofthe rH

Floi tid Fi'm. or d; ^Jea-

3.1 Land L€as€ patt€m

3.2 Agricuhjle

3.3 Hoiicuttub

3.4 AnimatHusbandry

5.2 Altiludo

5 3 Any tmportanl toature

5.4 Clim.t€

5.5 Raintull

0.2 Slop€ rngle

;\r1\t;/€

3

3

3

3

3

3

12-13'13 - 14

14

14

15

15-18

!!DEX

6.3

66

6.7 Wdth of th€ dwr at the

20

20

20

20

7 Geolodv in c!.. riv.r b.d7.1 The Egional cootogy orthe area

7.2 G€ology ot arca

7.3 The natuE ol rocks and their aflituds

7.4 MineabL Reserves

7.5 MineableResetues;bubtion

7.6 (a) Replenishment & Roterion Wo*ins ftogEmme7.6(b) Y.aftise Pruduclion Prcg€mme

20-2727

27

27

2S

30

30

7.7(a) Develop'n€nt and

7.7(b) Developm6nt and

7.7(c) D€volopmsnt and

7 7(d) D€v.lopm.nt and

7 7(c) OeveloDmenl and

30

32

34

35

I w'siE disposl amng.m€nt it sny 36

s

10

.E3fmated @a6r of R.clamatidn

siE!8gy ior pruduclion or pornt of public utilry 37

12 Main Pd€r dsvelopment 3713 ,\fi x7

11

i5Ii.i/ {,,.: .11 \Envlronmenl menagsm€nt plsn I 37

:-aJFll{li rAny olhff rulova.t infomation 3S

161 /,t:,//Successtue Mine closure Pl6n 40

14.2 \- 41

163 PFgl€65irc Mine Clolule Pian 43

16.4

Tabt6 tn.t€x

Table showinq O.taik Cn The Area

Tab. ShNing Land 0* Panern Around Lea6e acarn rr.cta€6 ( Census-2001 )

Table Show ng Lafd Ur tation In D stict Kangra 6

Table showhq Nd k gated Area From 2oo4 To 2oo3 I-lab

e S h ow ng Lrvcstock C.nsu6 Of The Oisirict 1 ITable Showi.g ForeslArea rn Hrma.ha pTablB showing Ratntat Oata Ot Una And Amb For The ye.r 201 a 17

Tdble Shw nq Rsi.f5ll Data Ot Una And Amb For The year 2OOs 17

Table Showino Rainlarr Dara or Una A.d Amb For The year 2OOg raTabe shor /inq Llho96phy cnTh€ sh. icroup 22

Tab € Showi.g Lilhosl6llgEphy Ol The Siwalik coug 23

Table th owinq Lithostrat g raphy Ot S walik System rn Kafgra Oisrrict 24

Tabl. ShMing Cal€ones Or River Borne Mate.lalAnd E.d Use 2A

Table Showng Mat€nalHandlno YeaNBe 29

labe shovdng OevelopmenrAnd Produclion n Ihe Fi6i year (p ar6 No -5) 30

Idbl€shdwing ErevelopmentAnd Prodlction ln The Se@nd Year (P ate No.-s) 3lTabl€Showino Deve opmern And Producton ln The Third Year (Ptale No -5) 33

Table Shwing Dev€lopm€nl And Productron rn rhe Fourth Y6ar (Pt.te No. 5) 34

Trble Sh@ng OovelopmentAnd Prcduclion l. Th€ Fifih Year (P ate No.-5) 35

I .ble Showng Y.atulso WEst6 Oispoeal Plan 36

Tab e ShowinO Yeafrise Area For Planlal on 36

Iabls Showing Crtsgon66 Or R vd Bome Materia And End Use 41

Table Sh@ing Minesbre Reseryss or The L6as6 Ar.a 42

labl. SCP-3 Scnematicscheme Ofsu@ssive Closue Ol Mine 45

T.ble No Sce4 Rehabrlita on Schem. For Fiv6 Y€a6 16

Tabre Showins Year W se Production Of Waste Ou.inq FNe Ye

,

!tt)

t,

tII

I

Gnph lnd.x

GEph showins L.frr u6e pan€m sumunding To Mining r-€as6 ArcaOraph Showtru Land Us. patt&n o' Oidnd KangEPi. DLEramfie ShoN/ing land Us6 pan m Of Dbtricr X.nsEGr.ph Sho&E Ner Intsat€d Area tn lhe sl5r.GraPh Sh in! lrvestoct Cen.u. Otne O6rndcEph Showing For..t AEa tn Himt.rl,tGr6ph Sho{i.O Monthty R.tf, For The y6r 2OOs

Gdpn Shordng rronthty Ratntsl For Th. year 2OO9

GEph Showhg Mono y Rahfa[ For Th6 y.ar 2O1O

Graph Sho$ng Rainf.l D€t! Oi Una And Amb For lhe yesr 2o1oG..fi Sho$no Ftaintal D.r. ct un. and Amb Fo Th. y6sr 2oo9GEph Showiig R.jdsn Oaia Of Un. And Ahb For The yar 2oooG6ph shorfiE MaGd.t H.ndting Mlneratrise tn Fiw yeeBGdph ShowirE pbducdon o, E.ch Mrtu€t tn Th. 1' y€.Gnlh sno{iing Pbduction Ot Eaoh MjneBt L Th6 2d y*rGEpn Shehg Producnon o' Each Mtn€,.t tn Th. 3d y6ar

Graph shoM.g Produ<tim or Eadr MineEt tn The a6 ydrG..ph Shovrlng Pbdudion Of Each Min6El ln TIE 5h ye.rGnph sho$ing Mine.U. Rd. !s propeed Ftr MintnE Ouring Th. Frve y.aFGEph No scp{ Sh hg yoarwi!. pbdud.lon Otwst€ & SoitduinC Fiw Y€s P.dod tn tonn..

6

9

11

t316

16,I6

1'18

13

30

32

33

u35

42

-'.*=."!sF?E.*

PLATE

NO.

Regional G€olosicai M;;

Pn Position i-rtoBTEi

1-'yll1'S

f6:" )3

'1!ffi'cln.dDiId..FlLd

WORKING CUM ENVIRONMENTMANAGEMENT PLAN FOR MININGLEASE GRANTED IN FAVOUR OF

SMT. AITITA KUMARID/O SHRI PARKASH CHAND,

VILL ABHEYPUR P. O.BHADARKALITEIISIL. FATEMUR DISTT UNA,

HIMACHAL PRADESH.

PREPARED BY

Kc. k ro.n oshsbr (R.rq {RaP)mP No llo. H.PJRQ,P.i66,2O10

K.olLr@tl HoGlng Bod colony

SUAMTTED BY

m Ah.dn*r[, Lh F.t hpur

nF l!![sni'l hrFlllt

ATPROVED

nit+Bltlq !,/i!c

' .jcr No.IJ.dpl -f*?n+-,M-

A h.r L Kr.o; - {) u!"u ' U"u1 "1

i

WORKING -CUM -ENVIRONMENT MANAGEMNN'I'PLAN OF MINING LEASE IN FAVOI]R OF

SMT. ANITA KUMARID/O SIIRI PARKASH CHAND,

\TLL ABHEYPUR P. O.BIIADARKAT,ITEHSIL. FATEHPUR DISTT UNA,

HIMACHAL PRADESH,

shr ania Kumari D/o shl parksh. vileoe Abhaypur p o Bhadarkat . Tehs Amb o6tr ct

Una HifrachalPr.desh has b€sn ssu€d a e(er ot inted by the Deparrment vde leter No Udyog

Bhu- ( Khan/) Lagh!-407l200s0024 daied 19-112013 tor the g@nt ot mining tease ior tlee(raclon of slonB, bajn.nd sand overan a€a sltuaied in Khalra Nos 1/1 a.d 7111 mmeasurine 1,1.

?4-93 H.ctares in Mauia Kota MohatRanoh, Tehs Jaswan. Oistict KangE H.pfora perod ot t5yeac The conditof hss been rmposed lhat the apptrcani 6haltobtrifed EtA cleeraic n advance so

lhal proper gEntoder s Esued

The comm liee has reconmended rhe are.lor gEnt Th6 6@a has been recommended by lhe

Joint lnspecl on Commnee lor gEnr ol mining rease to eslabtsh stone crusher on lhe basis ot raw'1rle allo b€ orocL.Fd fron -'< 1Fr r-a r.iertoto-J app.oac.eo lhe rnde,!r ed ha!-o ROp

rlF.do,A ,ra cpo(d tte^ehotae "p..**d"{.'iy9* . "%\ **v.rr cu+ F.f,o-me-r olrn l-'1 /

.";\j

rae n n,"n resse sre. s ro-a.cd r -e so-a. x-rd rrso roG, v '"*; ^ *- *#;7.-.r.ouerr or rh. c.d .rse. ro o.Apa.6 rF wo*ins-cum Envnonne\.*.t *"'9r -"raop.c or $e nnns lease aec sa> Lc' ed oJr on 2o0o sca'e xr 'Xeg,t*i: *r.€ncompassng Topographical Llhologcal and other tealures The Work ng,clm-Envnonmenl

Mansg€m6nl Plan ncrldes rhe 3Fremanc and scenrifd exploitatoi ol sion6 irom wlhn lhe ease

a€a encompassino a phased progr.mme for afoEstaiion and po nt ot pub ic utit tv

lntoduction::

!ttItt

Itt)

)

I

II

t.3

!!! kdFh4f,iur*i

L G.n.ral1.1 N.m. and .ddr$s ofth. appticant1.1,. Naft6 ot lhe Appti€nrl.l.b Add6. ot lhe alpti@nt

Vill. ,6haypur, p.O. Eh.daft.tiTch.il Amb,Di$tt una (HP)

1.2 St tu. otth. Am @nt

Th6 Apptic!'n inbnd6 to mine sloE, baJn and..nd nomshall be us.d an the p.opo3.d ston. crushor, for menufadu€ orm..t.n d po. the d€ma.d

l.€ Ret.rEdo. Nd or R.o.p.

1.7 N.m. dr P6edind Aq..cv.The area h.. b*n di.@wred by th.

. vasi e&edene in mineFt €J9toEtion

lhe le.se a6E. The €nEd.d slor/egdr and 6and to b€ sotd in tbe op.n

1.1

Knolrswwd Housing Aoard Cotony,

i:,i;,;ilix'f" (('n-.

let@ .nd tunna iMstqdled by rhe R e p as he hss

Loc.0on and Asrerch ot th. r@ lleati.. I.!rL@lion n.p (M.p No.-t)

.$i \i,.' l b,I

nz7'.F'T6 7".' 4 14iLt13

2.1

57

51

57'

Iorh*l-0!DDt4!!!3750

5f

57

2At

876"

7t320'

aor864"

rl5r

.).i-

r6rtb!ffiLldhdrd'F-whhlli.{le

2,2 l! .lion ort'rr 46.

PaM€r Circr.

Po$ Oin6

Suts Oivbion€t Oftier (Clvit)

Divbionet Fo@t OticersutsotvEton (PH)

Sub-Oivi.ion (FM/D)

2,3 pl3t E.lrom lh@rt nrd.@. tn Klm.eF1.

2.

3.

6

24 ArEri$gg4E!Th. pbpoa€d mining 3ite b t@t.d n th6 Sohan lswa.n) Khed. The highest point is at €1 M

R L {ille to\fe$ b sr 418 .nd e66E. width is 220 Mts, to 320 ias. and is apprc.chabte by s€asonat.pFqdr rod rrom th. haln mad on Tatw66- D.ut.tpoFun, Road ar a dist..e of sbolr 12 (m6.lrom TdMB and ls abo approachsbb by OehE.ChintpomlKo a Jaswan- KutE€_ Rafoh Road,rppb,rm.tdly 40 Km8. lrom Dehn. A. p€r Bwnu. 6cord ot the .€a the mining r€a@ area is .Govt land and re@rd€d ss q.n mumkin .'dr

2,5 D€tril. of f, AdrTabb Ahowlnd D.r.ib ol rh. AE.

G.hMtin Kh.d &mntt4t-2303-23-75

t1-2a-sA. pd Mn!.6.dq th. a€a i6 a Govi dassitied.! Gaimomkin KrEt:

3 !a!!LsE-p4@-:!!1s99!4!4e4djt44s3.i L.nd ue Prlt d

Keng€ Disrricl is spred over deep sm.ll €ll.ys snd nd9€3 CuhivarDn 6 96ible only in

sdl ier@€ ot holdings alo.g the hill slote as @ntour enlie fam'ng in rhs b.sins ot

3l6amr^had5. Slopy a,€s ae mGl suilabl€ lor culti€tids. ln the Stali6lic€l Ou{r@ ol Hituchd

P€d6n 2007-m04, oublished by lhe Deg.drnst ol E@nomi6 and SiaGf6, lh€ lollo*inq

@leg.res of land u liat n i. are aou.d l€e and Dbldct kngts b giwn

T.bL Shoslng L.nd U!. P.tt n & L.nd Cowr rcund L€.3o Ar€a

In H3ct E! { C.n.u.-2001 )

0

t-61 3 23

261 12

0

84

645

16

3o

6

Lro*

$f

ill

knd 6e p.tt .umundhg l. mlnlng ha..@

.t 66

c

ria;;h-

Tabl. Showlrg Lrnd Ulilit.rion in Dktrlct Kang.a

Nol available lor dltivation. baren

Land put lo Non AEdcultural u*s 752

876

a2

15 26

142Land under mBellaneous tree crops etc.

1576

5739I

G.aph Showins Land u3e Pattern or Dbttlct K.ngra

I ll

Pio Diaoramme Shding Llnd U$ P.tt m ot Distnct Kang.a

1310 Il

q\,

The d strid ensus hand b@k 1991cla$ified The land.vairabla in suroundi.g virrages r oro towins

1 Aresnot.v.ilrblelorcllivalion32 unjiiEeted

3 CurwabtEwasie

3.2 AarlcurudAgnahlE is the main @upation ot the people in the Dist ict. hali.g dltterent iypes ot so I

and agoJimaie conditions which a€ quile slitable for the growing or v.nous types or ce.6.ls

vsg€tsbles, t€mpersts snd stons fru s and oth€r cops Ths mspr sop€ gr@n in the d sticl a@

eh6 t, Paddy, Maiz6, Ban y, Mill6t Bssid6s th6s pot.to .nd . vad6ty ot regeiable ike geen-pear

GulifloM.. €bb.ge, 6pi.ach. tomai@s alc aB abo gwn in the di6tricl The e@nomy is m@ty

.grai.n 3nd n.jody ot popu.tion is dependenl on agdculiuE and a<lMties allied io il ior earni.g

then lvely hood. Most of the land un inigaled and depend6 upon tie Einy @aen The pad or the

lan& aE inqal6d and lh. irigation faolili* a€ provided by liitng mter from strems, shallow Dlg

@116 and h.diuh to d&p tubs w.lls in lhe valloy aGa The .ou@ of waler type ol idgation sn b€

classiled in to tol oMng fve cla$es

1 Lilt itr galion scheme

2 Well used lor nigalion

Wsll u$ for domeshc purpo*3

5,

a

tIttttIIIttt

The net irrioared area of tho slato durins 2004 to to 200748 ir

Trbl. sh ino Ner hig.Gd Arca Frcn 2oo'l to 2008

45571

1,04027

2006-2007

tn?-2cf814r11 1,47519

43S0 14752 93550

Gaph Shdhg rkr hig.t d.E in ttr St ti*-

t.3 lled&lllEre-rhe bpogEphy snd 6gr@rimatic @.dnior3 ot tbe distiEt src quite suitabte ror r}l€

podlcl6s of Eious fruils Th. topo96lhy oi the district can be touped into three €t qoi*nmdy Hish hirl a6* rGted at rne hbher elevatbn hkj hi0 areas and lrw tying vrley a€as Ftutts

ot vsnou! klnds depending upq the tecin ctinalic @ndit*r md $it e OoM in th€ disticl The

r.nrs werb * orhs ror,r aea

Mdn honbubJe produ@ ol the ere €n bo cra$ined into tou. €t€gd€6

Th. foll hg Eble shM $. a6a rnder akvatons of each hu'l r dr.

AEE-c!@-eacLlqiLedheir-eloCcdic!A. Ciru3

12460

2597

2514

3043

113

B ssb t. pl..t Ftuht

15515

f-f*"\4i ,'r

r cdrus r,u,rs Zr-1S". - ,\.2 SuFrropr@'rtuis t ,: . '^,, \

J rluls and dry truits ": , \?\\/r otn.r

'.hp6*r6 rrud' ,: I l-oli

3/j

!

!3

!

I!5

tI!!I

sI

!t!

!

2302

655 ,(t5

a6 503

l6 21

45 52

175

108

D. oth.rT.nmnt liult!r055

209

70

2125

I 11

13 Allmrl Hu.b.ndryLiw.lo.k . lh. main v€elih nart o ag cultu€ of the pcdomin.nt poputation ot ih6 disfr.{.

Th. .nt6 t min in th. diGdcl G mournainoG wi6 high 6lop4 and dep Etley.. T1E devetopm€nt or

60hcultu6, th.r6ior6, bEdly d.p.nds upon rh. developmern of anim.t husbandry. Animat

huGbandry ha6 6everal dll€d and indiFcl u*s for a fam* and 30 it is an .rmost integdt part ot

3gicu[ur., To lmPrcw ihe fenility ol lhe soil and lo plough lh€ ii6ld!, they r€€d anim.ls. Besides this

mllk and md ls elso lhe n€€d of lhe p€opl€. Th6 p€ople tep rhe follo*ing kind oi 6nimelE:

4 H6e.ndPonies

5

6

T

I9 Do93

t0

T.bL shdinc livcto.fi c.tu ofrfi. olaliicl

.iso7

l '*l

tIi!2

I

t

)

!

!t!

II

!t

II5

216503,1

,bolBia

3-5 Fi!h.ri..XrngB Dislnd is bles$d s h vast and vonegaled f6heies eeulc in the wst netwo* ol

,6..hni.r nveB, 3rrerhs Khuds snd iast iowing .old wale6, harbonng wde vaiely of lr.pi€lsp.ci* of fsh Rivd sFrtm in the DBlrrct @nsti1ul6 t€r Be4 and n6 bbutaies nadly Gaj Neugal,

M.nih asnd and msny o$s peBFn€ sm.4 Khrds fhe lonowdr !.onin6nl varefies or rs. lanilv- -/^\-abiond.rrhe re..n.i.rr4m3 or K8no€ Dlrrr ,r'","'.":,.,NMsha$.r !/ 6' ./ \'drI," -N'

Mnor€rp \\"o,". ,, 1

Ih. Fain sourc. ol lBhery cullNslEn ii in ihe Potg Oam rcs

ff"" 6""(. I';€qllated by 6she!i6s iagislation und{ tha Himscial P€desn Fisheis AcI. 1976 Firheties

&wlopmenl in Pong rese@ir has h€lped ifl ehaUliltlio. of lhe familis displa@d due to inundaton.

snEll nshes arc spotred on 6e 8€16 irer wtere the Ei$ i. dsp and slagnanl

thdi^g Llv6toc* c.n.ua ot th. Diltrict

4 Eh&-a$lfa!!3-9ft!.rir9r4.1 Elgri

Thelopography climate and nalure of soi s mainy respofsibe lor lho growlh olvarouslype

or tees .nd ehrubs wltch .c imponant lor daking the envionmern of lhe area most 5! lable for lhe

sufrivs of livirg bei.gs The lree and 3hrubs grow a@ordiig to the heiqhts The chlis coneidered

th6 p€v5ling conif€r!pto about 1950 met€ heighl when I gives place to the Deodar and lhe blue

pin66 ln KangE Distncl, th€ forosl r.nge betreen shurbs salsnd bamb@ fo.est of lhe lw h ls lolhe

tur and alpne lorest of lhe hgher elevarion LMsl poini oflhe sollhem boundary of lhe disi cl s

ess Ihan 300 meke above mean sea leveland highe.l range i! al an elewiion or s500 melre in the

north Ths forssts gr@n belwen lhese two enremes vary as the elevalon. The robwng mo5t

prominentvadetiei of t66s arelound ln lhe dineEnl elevation

)

tt

Thc loG3t.6r ln Hlmrchd PEd$h lor the th@ yeaB m.a.ur.d dufhg 2005'2006 2006'2007

and 2007 2008 i5 giv.n ln th. lollowing table:

Trbl. Showinr Foe.t Arc. in Himachal

139613

07 08

33 A4 277 36.949

t!S

5

33,01,277

3305973 36 9.19

97 657 36,949I a9,613

I,89 736

97.657

36 23 496

35,30376

t1

97663

6Epn Sh inc Fo€l Aa ir Him*lll

Th. wrrdlf. h a. a@ is dnecrt r.lgf.d to chaEcledrliB ot ip h.bibr i.e Mihbility ol the

tood 6nd w.t6r, natlE 3nd dEn.iry oi n@ pBvElent !n the o@ alo.g wnn orh€r L.$E like slope,

Clinale pGval€ni anthopog.nic aclivila6s 6lc. V.ndion oI allrrlde end slope in lhe llldy €rs has

esqlted in lhe polileraiion ol rauna *hich adods wnh the rulgedn€6 and h.d clirotic @.dilioF.

Due to div€ce no6. clinate and alllluda, th. ,E pc$s*s *ll unrque Ed€ty ol Hinalayan wjldlile

Dle to wide varhiions in rhe altilude, a large vadev ol tatna js aEilable in th€ loGst of the

di6lrid. Th. black b.r6 .e @mmon in tie hiqher v.ll6y Th6 l€oFrds a€ iolnd thougn od me

d6ln.l ba*ng d€r .nd GdEl ae lound .t medium elevado lhe hGt dsr o. keslu6 ae found in

6.t ln ,6.s Th€ lirck foFt snd climale ol lhe distdd E th. best ior 5uwival ol tmy animals and

bids ln od.r to aGt the extinclion oi many sp€is which ued lo suRive in lhe pest, lhe

G@mhonl haB dmlop.d willlif. 3.nctuans, ihe lolbwirc @mmn anirols 5nd biJ& aE round

8 F ing squir€l

iselenarcl6 lhebaianus)

lVaul€DE b€natbn*is)

1S Nima ayan fly catche.

6. Erc!99!ep!j!3la49E!.q!j!!.s!!a

lhe Kan!6 dstnd i.s b6nr€en siwalk a.d esser Hmalaya. Th€ lesser Hmalaya s ocai€d

in nodh restem lndia in the Stal6s of H machslP€desh and Utar PEdesh, in north ceita ndia in

th5 st6t€ of sikk m range from 1500 mercs to 5000 metE n heighl The Ka.gra dBtricl cover as area

ol 53oo sq Kms in ih6 @si nonh weslem psn ol Himacha Himalaya. border€d bv Punjab and

Chamba Kulu MandiHam lpur and Una in nonh east, soulh r6spoctively The elevalion ol lhe d str ct

.b.ve m s L var€siom looo metre lo morelhan 6000 metre n lhe districtwheelheswalik rocks

ae exposed. the topogEphy represenls a senes of parallel hil6nges separated bv lonq udna

va l€ys Thsss vslley are very teriile The high p€aks where allrlde rs more than 4000 melre above

h.S.L Emains coveEd wrih snow Many sireams exist in lhe districl ae s.d fed and many gei

The Dh.ul.dhar mouniains d.nnes lhe nonhern limit of dist cl separated lom chamba

dbhcl. The peBks of tnis mountai.s exp€n6nc. very heavy snow fall and exh b1l5 precip tatbn and

russ€d toposr.phy. The siwa ik Bnges arc mode6l€lv l€ss steep and rorm smalhilocks Beas and

Neuarlsre lhe main river which are Gaj NeugalManJh aaner elc asftenfibulades

tt)

t

tIIII

l-e tu mg ease aEa.i€s n so.a. r loc.iy lnos- s*an ) tet whc,RNer. lt il@s trom soL,ih lo Noih d Eclion andjom Be.s rive. nearTaitar

5.2. Altitude oi rhe Area

Th€ h ghosl po nl ot lhe lease aea is at431 M R Lwh le lowest

$e dGr ne.rlhe lease srea 6 220 Mls lo 320 Mls

s 3 Aiv lm.orilnt fr.tlFTh. pG.d sile foms the @lchm.ni aEa of Beas river' The.rea falls in Sohan (Swan) rver

*,!ric nsar lh. D.ulstpur cnovi( in Una

The rcgion has four disrinct seasons.

March followed by 6erue6 6umm6r s6ason

undd lho innu.no of south -re31 monsoon

season lashns up to Nowmber

The a€a €xD€ .nes 66v6€ winler irofr De@nber io

lasling tom Ap l lo June. The aFa cceNes €in lall

from July to mid Seplembe. td@d by post -mon&on

ThG lerain n gene.al hss profou.d innuen@ on the lemperalures of a.€gon The

temperat!rc g6n66lly d$s trofi lhe beoinn nq ol MErch t ll June, whic$ is ihe hotest nonih oi lhe

ye6r wilh mean mlnimum and Baximum tempeBluc o125.6'cto44',C Erecliveiy vMlh the onset ol

onsoons by lhe end ol lhe June lemF6tu6 bogiB lo Lll Ths drop n day tenpeEt!@ is much

more lhsn th€ drop n nighl temperalure The night l6mp€Elu6 falb rapidly attsr lhe withdrawal of

mon3@m by mid$eplemb.r. The month ol January ls cooler month with the mean maimum and

mi.imum lBmp6ratu6 b.ins 24'C and 1.7'C Espectively. Under lhe influen@s ot wesleh

dislurban@.lhe tempeEtuE lalls appEiab y durlnq winte6 and il may qoewn bolow 0" C

Huffidliv ls o6neElly low lhroughoL{ the yea.. Dudnq sunmer season humid lv is lorest 36

.d. Durins mon6@n honlhs I qoe. as hrsh as 30-900,6. The h ghesl l€vels of humidilv .€ obseryed

in hemonlholAlgu6t Th6 av56g. hlm d{y dunns synoplichouF is53% and 62q,6 espectivelv

5,5 Ralnfall

Rainfall vsries signifi@nlly with allhude ol ths srea The @tchment arca re@iv6 Einr.ll dle

lo wsstsm distudanes lhal pass o@r th6 norlh _weslen pal( ol the colntry dunng winter monlhs

sionilEnt pr€cFlstion i. fom of snos ls @@iv€d at hisher ailiirJde and Finla I in vallevs is .e€ived

dudng lhe wnter monrh. REiny season qeneGlly sbns trom mid July and extends up lo mid

S6Di6mb.r Dunng winler lhe Vains ae tdi@ and exlends in belween l5s December to 15b

February. Th6loll&ing Tsble shos lhe qlanlum of ELnlall dunng lhe ve.r 2008 2009 and 2010

odjoi.inq ro th. dining 16a.6 5ca.

I

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Gdeh Sh*ins r@rit R.iBhll ior lho yar 2OO8

5

Ll,L I II

J

Gnrh Shorlng Xo hly Rrnrt ll for tt. y..r 20Og

LLu ,1,,.

LLL' !

I

Gnph shdi.q xontftly R.i.f.ll lor

I

E:

I JLr,

illEn ,/,/.;{^},

li

It.fr

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ttII

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,

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.to i13.0

55I

Sih@ ih6 €tchddrt ol in. Sohan knad b hilb of li€ Una dislrEt, th. thad Mler is attribuled

to Ih6 Ein5 shah cur in lJn. dbldi a.d Frlly in lh. .16. ol Kd96 diGtricl lt is th6r.tore.

nd3lery lo steak .boul iie rsn lall i. lhe €rchrunl of khad ln the unt dhlncl

lrbL Stwlng RAINFALL DATA OF Ul{A AllD ALB FOR tHE YEAR 2010

& p.. D.t nllni.ln.d br DiEtoEte ot l. nd R6otl Himch.l P6!L.hi6"tt' -li,.i

110 93.rt 2217 2aa 2 256 50.0

1 1 2 13 9', 1

1950 136.0 a2a

I T 10 1l 9 2

Gnpt tho$ng RAINFALL OAla OF UNA ANo affB FOR IHE YEAR 20lO

Lbb Ahnine RAll,lFAlL DATA oF UNA ANO At B FoRtHE YE

A. t r D.r. n.inr.hed by olMloaL of trnd R@rd Hh..h.l PEd6h

tuon Tro TrruTr,t*Tarn usvL_rilRlmlr'r'n 180 24.0 j 340 i 162 s43401lmm l!n.l I I

iAi,iao-iuiw lr f1 ft f7302l2s0 133

D

Jun I Jur lria I Sep

3321506 l4{3.0

t1

Gnph Anodns RAINFALL DATA OF UllA AllD AtB FOR INE YEAR 2009

.L rL r, J..l-Lhr tct Mar Ar May rui

r- [.tITrbl. Sh lng MI{FAI! OATA OF Ul{ AND AtlB FOF TltE YEAR 2l,Oo

A. poro.iam.i .in€d by OieloEt olt nd R.c6nl Him.ch.l Pddah

Nit 20

2 2 1f,

340 23.2 18.8 36.4 18.0 633.0 62.0 NII MI

3 2 2 3 IGEFh shditrg RATIFALL DATA Ol t M AND AtB FOR THE YEAR 2OOa

.n*h I

IA

3;'e*4

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tttttttItItJtttItIat!ttIsI

tttt

t

6, Dscrlpdon or ft. AE ln whbn th. t.& i. rhqt d6,1 G.mhl

The minint l...e.re. k du.r.d in th. Soh$ r\h.d The Sohan Khad (9/.n) b. tet bank

ldbulary ol lho Beft Riwr onginating lrcm Uru dietrict ne.. Dautatpur Chowk at &€ h€ioht or 666

M6i.r6 MSL and ..GE K.ngra dls,tricr d 484 Mebr aboE Me.n s€a Lelet .nd join a6a3 Riwr near

k'n)

Th. S.han kh.d {locally kn@n as Smn) ortglmte near

Oaulatsur Ch@k in UM Disrrict st a h€rght ol €66 Mts, MSL

and 6nter KangF dHnct Al 488 M€l€r .bove Mean s€a

L.Er (,14 M/13) .nd joh B€a3 ne$ 3an6a.pu..

lmpodant tdhll6'i€3 of the Roli Xh.d (Riqht baik libltary ol Sohan N.di),

khad (Right bank tribul.ry of Soh.n Nedl), Kolla

benk lribulsry ol Sohan Nedi).

rmp.ned vlleg66 naar lhe From Orrgrn !o 6nn!.nc€r Samarput Bhambhot r, R€n,

Kulhe6, Ouhlal, Mahala, Gummi, P6sp!r, Mai6, Cnak

dv.r Th. g.ndd now ot lhi! Khad in nininq leae€ erea

The dwr bed b @upied witn €cenl d€po6lb ol mlnor mln.rals comribhg sand, .llt, g€vel

and pebb€s ol Netrer Allwium belonging b quabmary aEs. ThE66 8€dimenb a€ dspo€ll€d in tha

ih.pe ot ch.nnel b€F, pi.rdmoi baF, flood pl.irc and alluvial tan rl.p6its. The allwilm @nsisl6 of

loose ssnd, sih, cley, pebble, gravel and boulde6. lt un@.fomady ftnis difiercnl tom.lion. in

diffeEnt @.s. Ourho momoon *6on lhe .irsam c€dre. h€avy E€dimeri load 5nd dop$[ I.nnlally on the rer H. The Sohan Khad crn ib @uM all nsih thrcush lhe rcck or

Th. m'nrn! r6aB6 aB! E srruEr€d m lh6 tuer K';,..iL*a" s-wd

/ED

6.2. Nrm. ollh€ Riv.r/Slieam B3d on$nich ft. mlnlnd lo..e b 3itu:1ed

The mn ng lease is situaled in Sohrn Khad ( Smn), E i.bllary ol rver Eeas -rhe

hrqhest ponl ol$e lease a6a i3 al431 M R L while loresl . a1413 and average width olthe rv€r

rcarrhe e.se a€als 220 Mls lo32o Mls

6.3. Drainane Svstem

!tio.ms part ot Beas Ddinage svstem

6.a. tvp. oldr.in.d€Th6 prmary iibutaiee above 450 M R L .xhibils dendritLc lype ol ddinage pahsm and then

to its downstEam sid.. sh@ suMendrite tvpe ot d€i.ag€ patt.m

6,5, Oridin ol river/sl@nsohsn ( lo€lly known as Swan) Khad o.isinate nea. Daulalpur Chowk ti a he ght or 666 Mls'

MSL Dlacc known as Chhararban ln U.3 Distncl wherc lhere sawalerdvdeolSMnandSohan

Khad swan 6lhe hbulary salllj cal.hmenl *t e sohan is lhe catchme.t of B$s Rver Both

skeahs I N in opposrte di.eclions

6.6. Allitud..tth.o.i!in,Abolr 666 Mts. MSL near Dallatpur ch@k in una disticl

6.7. widlh otrlv.r the olac6 ol mlnlno

Th6 width of r vd vanes ftom 220 net€s lo 320 metres

7, Oelodv7.1 li!.!9Ab!4slelertltllcll9a

,

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ln Hima.h6l Pradesh Geologcal hstory g@s ba.k to the archaean pbterozoic tEnsition

aliholgh thc aclu.lNimalayan Mounlan bujldn! look pb@ onlv dunng Cenozoic era The Himalava

ls a clasec example ol contin6nt and contnenl colieon due lo @nvergent movemenl of lndian plale

rowad Lhe Eu€san olale ttcomprisesnto @nlEsnng leclogens wilh ih€ir own disllnctive g€ologica

hElory The divdlnq line bctueen these lwo tectog6ns represent a major l6c1on c dis@nunullv and is

d6s gn.led by several local name Horever' il ca. b. 'ollectively

reler to at a Main centraltrust and

on eith.r .rde of this lhrusi lh€ teclosens d splay conl'asling stEtgEphic and teclon cs features

indicat ng convelgen@ of lwo arien blocks These are the le$'r H malavan leclog€ns and the tethve

3

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I,

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5I!

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!9!!q E!4iirEq!9!!9s!!The shal!, the Laa and lhe Deoban rep@3enl the lhree princpaL lecton c slraligraphc

dodains which dom natB ih6 geology of lhe Lesser NimaLavan Tectoge. these domans have

characlBdsiiG which provlde an un mistakable co padson w(h g€ooqicalbels ol lndian peninsula

wilhwhchlheyhaveastructu€lcoineton ln Ih€ Lesser Himalayan Teclogen crystaline nle6.re

n lenersLabsenl. However ihegranlrcgneissesolwsngl!andgandewlhremoblizedlSGaand

2OGa sranlolds is lai Ra pu. Wndorc zore seem lo be $e ep€sentatv€s ot ionh ndians

P€nnsular Huna Nala limestone exposed in lhe aEa is of cement g.ade A ls out crop3 o{ purple

@nglomerat.wlh olcaEous matrr are seen wiih in the dolomile Quarlzarenne-carbonate sequence

presence of oscillalion nppL€.nd stomatolites poinl to a stable shelfplat€ fom condlion of deposil on

Shsli6tructuralBell

The Shai Slruclural B.lt @mpr365lhe Sundemag.r Group and the Shali Group( Sikanta

and sham. 1976) lt occu6 in tr. strucllEl bells viz, the Main shalr struclura Bell and the shali

srbs dEry bel ol Bandla Ranqe(Fig 53)

Tho Mam s hali Si.uclu lal be[ efends over lenglh ol 260 km s in a s]gm oida sh ape bet*ee n

lh6nv6rRsviinlotheN\/andNaglkarrdge nthesE Beyond R.viit exlends n lo the Kashmir

l.ss.r llimal.ye whe.e it was earier Ef6 .d as the Allochthonous lolded bell by wadia (1931)

Th€ Marn shalistrucl!6 beft bilurcates in to two sub beLls respectively The nodhern Asindh'Nag

Tik.r sub-belt and l.Iapanisub b6lt m.rei.g along the @u6e ol BhaEriKhad ard the Sallul in lhe

srapp.r aEa. The Main shal sn.tu€ bell is nearlv 23 kms broad aqoss lhe sarlui valev and lhe

Shali .ana€ (F& 5 3) wheress in the As nd seclor rt ls onlv 2.81 kn. broad alons its NW enension

towards Mandi in to Jsmm! and Kashmir ii becomes enremely narN and constricted wth lhe

development ol lhr6l mbncates

The shal subs diary b€lt ol Band a rano6 rs resticled to a 2one between lhe siwa ik be I and

palaeoge.e p.ELrochlhon bell I enends iiod B.hnd-fibba in the nonh to Khadli in lhe south and

beyond it odG as dLscontnuous sldp as al Tundapathar' Mala Salaun, and otherteas Ths belt is

appa.enlly ind6pand€nl ol lhe Ma n Shalisttuclu.alB€lt and compise

the shariGbup The shali struclural belt conprses the ogl'/,\$ry9hjE!3r9r!{p ro lowed bvid,t-Ell

,ou-ee,sh,r's ouo. //;' .'''. ).

shdlrlelE i\C : :;'he sh.l L'redone was i'cr ut"" uv p"'.* ,

'gz r ' N 'r"h lm*ro'qr%y'ch @ve\ ih"

qo,rh€h nsnk or rhe sFal roo. no rF or sh n'd r "e c as' rcd[oN!$eshau'lt's anerpred bv

wEs(193s)who divided n to Khara ouanzrc. snka ia a"a sh'--"fu16/6 p*t"nt"o "

to'"

detal6d lfth6lralErsphic classilicaton ot lhe Shal Group dividing t n lo eghl iomaions0able 5 5)

2l

€lMlikGreuo

Table Shdinq Lhh@aphv oi the shali Group

G.een-and puDle col@ed sha e, ston€

siltsto.e spoddic eanhy imestone; thin

bedded odhoquazib nter beds gcen

bBccrated rcck and fa dy pe6i{enr band of

wh i6 qusrtzaenie at lhe base

ahcdy dolomlo grey imeslone and white

Grev-qGsn bla.k and pulpl€ shale and

ston.s thin b€dded limestone,lhln bedded

quanzarcnile w lh or wilhout dolomil€

140

dierry oorom e-sey and pmk ncotouu$

-mk and g'ey (€am lerlured meslon€ dlh

with spo€dic quanzaenile

Bnck .ed shale and sillstone

dolomite n ihe lorer ho.izon

developmenl or sah, sall qil

Th. SiMlik Group in the H macha HmalaF loms a paEllel loot -Hima ayan zon€ exlending along lh€ southern maan ol the Palaeogene Snmlr Goupb'[trcmlhe

Rav lo th€ Yamlna and loms psrl ol the aaer sutsHLmalayan mega belt extending irom Pottar

basn n NW 10 lhs Arun.chal looth Ll n sE ln lhe Nimachal Hima ava ithas daxioumwidlh betweei

Hoshiarpur and Jogmdemagar

,

ttt

The Siwalik 6sdimenls . ihoLgh occufting a5 ' independenl slrlctural bell arc aLto s@n lo

overe the Murs in lhe Jamm! sector oI the Kashmn Hmalav' and lhe Kasauli n the Himacha

Hmab;a Pigilm (1910) recodod a aEdual tra'6ition lrom Mur* beds lo Lower siwalk in rhe

Rsmlpindl and Jheluo d sldcb ol PakFlan and rrom K'sauli io L@er siwalik (Nahan) ln the

12

A( Ha taly.ngar n€ar Blaspur. tho L@er

unconforhly. which is descnhed as lhe most

ifeshwat6r deposls and elidentlv representing

lh3 facl assumes inponan@

rhe siwalik and s mu GrcuPs

b@suse the€ is alend€ncy lo gnore this noma

atDh.ransala Sa aghal and Na agalh

swaik s seen €sllnq on the Dagshar wilh an

slrknq discordane in the whole seqlence of

. peiod of conslderabla earlh movements (

I

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The swalik Group B divEble nto three subqroups €spect lely ihe Lorer Middle and UpP€r

on $6 ba6is.l llhostratigraphv (TabrFKarunaka6n and Rsnsa Rao 1979)

Lower Siwalll( Subrroup

the L@er slwa rk subgroup consisls essentia ly ot 3andstone<lav altenalion The !@r

boundsry olthe LN6rsrwalik does nol crop oul at surface inthe Jawslamukhiseclor l' adeep*l

dr led n the oler lhrust block ol ihe J.w'lsmukhi Thrusl however' the Lo@r Siw'hk s lou'd

conlodaby is aiso ma*ed by a.d inc6ase n the percenlag€ of heavy minerals gviig a dark

apDe.Bnce to fte rock and ncoming of less rounded hea!'v mnerals like staurclile and uistable

tyF6B lko zosite and epdrne

Tabl. Showrno LhhGL.li!r.phy ol lhe Siw'lik Group

Lithaboy

6tiiiiimanrry-romns omerar€ wrh red "dorang. clay es maht and mnorsandstone and eanh

bull and brcwn claY slone

a) sandslone clay andconslomerale tkemation'

L-mr smlik

a roassiv-nosrore witFmi6r congLomerale ano

lo@l !arief, ated clay slon€

A) PBdonnaiily edium lo coaEe{6i'ed sand

slon. and ed claF alternaion soft pebblv with

slbordinale cl6y stone, l@lly lhlck pnsm ol

eJAr-ienernalion-i-;;Grealum3r.nedsPo€di€llvp6bbly end$on6 calcareols @menl and p@minent

chocolste and ma6on clavs lone in the middle pad'

A) R.d and mauve c av stone with lhln inlercalalions

6r medrm lo li.e{d ned sandsloneII

I

.y'. va;i

s

€

5ii<t, sitt sra*t ana Febbtes

sa.dsrone. cray and conqlomeraie akmal o.

P€dom nanty massle @nOlomerai. wilh red

and orange clay as mal. x and m no. s.ndstone

and eadhy bufiand brown craY stone

Mas.ive Sandstone wth

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P€domrnanlly medium to co.B6- grained

3andslone aid Ed clay altemation. soft p€bbly

with subordinate cay stone localy lhick pnsm

ALrBnation ol life to medium- q€ined

sporad€lly p€bbly sandstone, @lcaeous

em6nt and oromnent chocolate and medum

maroon clay slone in lhe middle Pan

Red and m.uve cay stone wilh thLn

ntercalation. ol medium lo fne grain€d

fitloMi6ffirrk;i:MEmukhi t re6o m iilFGliiss-seviEt suoavrios are possro e

on the basis ol sndstom-shaie ralio. c a$s are pEs6nl onlv loca lv especia ly towards lhe lop ot the

lomaiion Guallv co.35tins ol we Lrou.ded g6y coLolred quartzite Kasaulisandstone and Shali

dolodlieinlor2hsize.Clselsarepe*ntocalvinthesa.dsloneespecallytowa'dslhetopandthes6 usua ly c.mBl ol g€y and pink.oloured qlarlzsrenlte posslblv beonging to elher lhe

SundernlgarGbup or the Kharn Foma on of the shaliGroup

Fudher easl of Jawalanukh st the inner edg€ of the fool_h lls the LNer siMlik shows a

ditfe€nl lacE3 lmmedialely ov. yi.g lh€ Kausaul lhe€ ls an unLl ol cGBe leLdspalhic sandslone

an.t oBnge co olred clats Hgher up anqllar classts ol q!'rtzare'ite 'nd

cne't a'€ folnd in lhe

6and6ione. The main Lc@r Siwalk *quene conssis ol co.glomerate endng with bouder bed

Table Sftowinq Lirhchtlg6phy otSiw.li* SFtem ln Kang6 Di.trict

I

5nd €d sandv cave. The ovedyi.g unl consisls mainlv ol lhick sofl to

coa's€ ro red,-m sra'ned sardsron€s fr rh lh n nrer *lrl'ons or red ad #5811' I ';\€t /

n the Pa.otsSa aghala@s,lyrng betwen the inner edge oliheloolhils and Jawalamukhi

the lilho ogy of lhe Siwalik s inl6mod.l6 in cha6cter The lorer pan of the sequence co.sisls oi

medum oEined sub greylvacke rnter bedded with thLc.k €d clays. bul hgher !p in the seqlence,

sandstones are @a6er and clasts become mor6 fr€qu.nl wtrile clays a@ ess developed The

uppermost honzo. consisls of @nAlomerate wiih rel rounded casts of grey quanzi€ possiblv

derved lro the sh.rGroup The rolallhckness ol the Lower sMaik in the wesleh llank olthe

sa*aghat anticliie s 19oo m

t'liddle swslik Suborouo

Ths mddle SNslik Subgrcup cmpises ol a.qe thickn*s of 6a6e mi€ecous sandslon€.

6ofr6 ntd b6ds ot e.nhy.l.y. ll.o.mally succeeds the LowsuaLik consisls ol sub gr€vrEcke to

.*ose nler bedded wlh cl.y sto.€ and €l€reous maner occudng in segregations €ther than

d scemmaEd lhrolghod the s.ndslones lhe sandstones a€ less rel€oned $en lhose.ln Lorer

siwslik. Cays are dullcoloured.nd s[y clasls arc common in @a6er claslics especally lowads

top snd @nsisl oi lraghe.ls of mElamorphic rocks occurng Ln the Dhauladhar ranqe and Mafdi

volcan cs. The lhckness ol Middle Swalk 1390 meteG n the gorce of Banganqa nver SW of

Kangra Petrolog cally ihe Lorer boundary otlhe Mddle si@lik co ncides with lhe intlux ol kvan l€ n

thehe.vymned assemblage (Karunaka6n andRansa Rao 1979).

Laters faces changes arc mmmon ln lhe J.walamlkhi a.ea. a lhick prism of conglomerate

ocurs n Ihe Middle swalik, which within 15 km on e lher side ch.nges lo lypica Middle swalk sandv

laces The lhckness nearthe Beas nv.r s lS9O m ln the Jawaamlkhl seclor' lhe middle swalks

whrch r€ of nslure olchanneland flood plain depos13 ln bolh NW Al lhe outer ma@ins lhes€ areas

M idd l. slwalrk rs lRnsiio na I lo flood plai. lacies especia Lly in the lower pa.l of lhe seqlence ll ig he[

up maB6ivs s osic sandslones o@ur in th. Bhaka gorge seclion Middle Siwalik s'quen@ is aboLl

laon n.bd in lhickness. divisible inio lwo iithostratEraphic lnils The l@er lllhdassoctton s 750

m.JeB rh .k wirh a retrrarions ot nodeElely had w€Ll_bedded medium to coa.:?ELlqd-sandslone

q4t'lYLiE-n\a$ive

=

:t

!

t\

.ck of roundne6s of lhe clrsls slgoe$s a shon disiance transpolt The

very lhck (2000 m6l6rs h Mandi area) Slch .onglomerates. rcpesenting

found at BilasDur. Sa .f,hat Pa!.mpu Bakloh and olhe. a€as, and thev ndicate lhat lhe

upmhad-alGady bcgln ulh .nte€denl erosion

along the nonhern edg6 of the

conglom.ralic wlh pebb €s derYed frcm

ioot h rs rhe MiddLe s$iE lo€*ds p,4"i"ii:itv.-.* o.,o -o "" "-iL9."n",

-"nr' nffi

75

It)

)

ttttttItt

h the SE Simour 6reas, on the oth.r hand, th€ middte SiEti|( which is n.Edy 2@O m thick,consBl3 ol git.mrrionB of .lay and sandston6 in the t@. p€rt and fra6si@ sa.dstone. in the upp6rpad. ll cont.inr . modont€ly rich .s.mbtag€ ot opaqus,gs.n.t, toumatitu, epidote, staurotit€,2obn€, zi@n, rulite, chbrne 6nd ky.nir. ma.*er an.nd€d by Lithotosi€t chang€ in th€ Stwatikpolnb lo a major chEnse rn depoeition.l pafl.m, aconpanied by carth mwemenrs Esulins n rhea66 nonh or lhe Siwalik basin

UoEr giw.lil 8lbcreloIh. upp€r Si@lik Subgbup can be easity *p..ai6d nom ihe unds tying Mddte SiMtik on

th. ba6i6 or di6tinct Lnhobgicat chaige. tn tho KansE aEa sh.F the middte Slsltik, tho6nEron6rale3 @nlalns cla3ts ot basic vote.ic rockB ot the Mandi - Dan, Votenic qith . wry thin(10 neleE) lraFition.l ione b.twg€n ihem whici may d.n suggest a to6t b€.k between Middte

and Upper Siwalrk. Th€ lpp€r Siwalik @ngtome.ai.s co.ation Ed and orsnge @touEd ctey as

fiat: NE ofJeelamukhi in th. rambaq.on syncttn. ony 600 to 000 m.ters of upp* SiMtik are

expced as lhe uppe. p3n F ovedapp€d by th6 po6t-Upp.r Siwatlk, N€ogat congtomeEles and cdclay6 ln $€9€ rhe d8B ae smalts snd mll bu^dod ftan lnc6 ot the upper srMtrk li6vFrcbably belong io lh€ li..l i.telgl.cial p.,od ol th. Pt6iskr@ne and ifEreto€, the top ot the Uppergiwalik extend3 inro rh€ Lo@r Pr.istocene

The rim€ i.r.B.r b.r$.n th. lwo epEents ttE tast phase oi tne Himatay.n obgeny. Th6

conglom.r.tic ldijd or th. Uppar Siwalik is iound ln th€ main Mandi Renr€nr hainty in lheLambrgaon.ynclin6 and in lh€ aBa lmm.dialely lo ihe SE ol the main t€ctonic divide between the

Siw.lik b.lt .nd th. Slmaur b6[ Sodh ward6, ihe conglomer.iic Lciee com6 prcge$ivo1y high6r

rn rh€ s6qu.n6. und* rain by gdls and an<Ges san&ton6 sw of J4atamukhi tore$mpt., 1s00

md4 uppor siw.lik aE. .xp6.d cons sthg ol 10.40 m r@r pebbly sand ston€ sequ€nc€, ofr€.

s'lh gr.y .nd bbM cl,y ba.& and 460 m ol @ngiomerat. ov€rlying them. This lituatio @nunues

along tho Nadaun don At Bhak6 Eorg€ ih€ Upp€r Siwalik is 2350 mete6 thick, dMsibte in to a tMrm.mb.r ot 1730 h.t.E thickn66, and an Upper M.mbd 620 hete6 thic* The LMr Member

ms'nly consists of 8ofr. m8ew, pebbly sand slo.6 wnh 6in irt elaton of c0

..ndy cray3 becomb pomin€nr lnowh at rh€ top or tha rooarior ro g6-4nrei,Fplqery rus asub-M6mb€r, 215 m€t68. thick d ahakE. Nodh wsiwards, th" o"v;fft.-0,"*o W iJ.\" *t3rom and congronerater whkn pa6s ole roE in ro a cray. s..d sr{6e$cr6s." Ba ldr'hkor

h rhe ourfl foor h'rls beh. i. Ja",,". ,n" ,o*, "'*'* '"

.l\ . -* ".bHA**w t s'lrs ClnelomeEres occur orly sr rhe I\o+ wesr€m pan or

'n" "Vr- rr'" uiOi4*"rir i"23oo n rhi.r Funhd sornh*3wads m rhe pran$, rne sandy tac'es o lli upper svalii e,renos arr

lhe way up to the oerhi- LahoF .rdr $hich sep.r.les rho Punjab plattom trom rhe Rajalthan

Pletlon Th6 lhid*n€66 ol rhe Upp€r Si@lik d€cEa$6 6teadily f.om 1610 md6 ar H6hlalplr to

ttttttII

k*r-tuF.it!.bq

4t5 ml€r3 at ara mar th€ top ot tn€ .Eh h punFb. ln the ptenss lhec ! io be m di@(bneb€rw4r lf, pcr ahrsti* sttuviuh ,nd th. upt6. siRlir.

7.2 GctwotttbaqTh€ sludy ot (Ek6 h s|d .bnd lh. bas.d d,r e. dw tEt it k tutt ot ,,€r bon€

*difr€nll $ltch h.6 bM gwEt€d by rh€ €@toirt plo6s ot Upper si*atik toin.tioB. The dvsbome n.r. .l6n.ict ot boukbB , Fbbr. @bbt.. b6jd ,*nd and sln Th..@ h6 g€nfl€ sbpe.nole.nd b @clpied wnh r.id!.t.o[ $nit js torEd du. b l@th.dng ot upp€r hi sbpes. The(nrctGB or tht6 rB bom. matstal i6 3-4 mets doprh aB gaiBei in d.cusEion winl pWD.Authoritl66 as lh€r hs .o @d h die past *hite digqhg t { bidge ehrrheobr. The .@ g€nt€n&bmeEes du ng mtls thoebE no Fmn n v6get td 6 tBtbb in ,r. dwr bed hME,swd sh$ glft in lhs .r.bb tsndr or th. khad. For ercuhan ot qHnriy o, min€rat one ner6rdeplh tu! bsn laken inro @nsi.t .arion.

vr* of f,lning L{D Ad!.,,us>

t,l flE MtlE of ett r.d $.tr .ttttd.The aM is p,n or lh. Sohan (to@tt knM Sms) khad b6d rhi.6 ontains boddd, bajn

and send miet cby Th. bouidets ae br@ght rrM si*riik o.t by e@!bi eid .t4m sFrao

7,4 irsbL RervmAte. loMng the no hining alea whin is 10% ot rhe spen trm e6dr bsn* as ps H.p. Micrat

Polic] Gci.l€lireB. th6 :@ aound 128400 SqwE .net* ib w.t€bt€ .E*ll ye& leund 632005q{€@ mlaB.tu dE! b. d.ihbte tor mdijng Th€ eitdbte ar@ shal b€ dnabd ir o tvo bt cti6

2l

lo be woded inihe rdafionalma.ner each bto.k n one ye.r.

conponenls of th€ ssdn€nt8 shal vary tom year lo year

dfierent @moonent is as under but it shal not be avalable

sfra ler sed ment Ehal 90 on nc€ase m companson to leGsr

The averaqe peicenlac€ ofthe various

Presedly ihe cdlcu ated percedage of

rn lhe nerl year as the percentage of

siz€ male a The 6u ls of rhe rest p (

3A%

T.blo ShNinq Categoies Or Raver Borne MaterialAnd End Us.

9r.

I Gil in lhe slone crusher (Jaw)

Gdr n ihe slone dusher(Roller)

3 To be soid n the market atter

separating cray/sli es perdemand

To be used lor back li lino

To be used tor €ha bi ilalio n work

The pllF6c of lease is lo use lhe mater al in the p.opo*d stone .rusher as . sourc ol raw

materia tor manufacture of grit As such. lhe pnmary Bw matenal equned ror slone ctusher is

bou ders and bati (pebbles). The nver bome tuatera @nla ns boolde6, batn {pebb es), sand minure

ol ssnd mixed sih a.d clsy. The lessee can also *l lhe olhs m nor mineElconslluents in the open

madrer if lhere is a demand ol sand and sand mxed sh. The sand mixed slt does not have any

mad€i va ue and this matedal wi I be used for €habiital on work or sha I be slacked ar alpbp.alepa@ lo be idenlifed in consullalion wilh Mining ofii@r Kangra

i order Io calcuiale lhe m neable .eseryes, lhe following pomts are l.ken in lo conside€lion.

r A Geo og calmap on 1.2000 scsles E prepared lo find oul lhe wo*able a€a and other imponant

l6atur.s ofth. a6a li 3 nol possibre ro bifurc.le ditrerenr ilho unrc as all the constitlents are

heie6geneous minu6 and cannoi be marked separale y

2 The dife@ht @n6liluenl6 ot nv6 r bohs doposiis such as boulder, baj. (pebblee), sand mlxed slt

and crai bas6d on 3izc class fielion reE cons der€d ror Bsefre ca culaiion. Although il is not

n.ssblelom.tkrheseunirss€paGt€lyontheoeoloqicalmaDassuchaplotlrlxlhElerMs

sot duF ii th6 fiinino l6as. .rea .nd matenalso erca€ted M3 sepaEled into dilleent sizes afd

lh6n per€ntsge was worked out and lhis p€rdnlaqe was laken in to eount dunng ebllalion ol

Th. a€a sharLb€ divid€d mb lwo equalhalllor rolatbna wo ing The d.mst€am Block shallb€

M*ed in the l't 3d and 5'" year whrle lhe Upsi€am glo.( shall b€ rcfted in the 2"d and 4r )€ar

io prov'de a xre tor rcplenlshnent ol ihe aEa ln a olalDnal $hem€ $e @r1€d out area shall

b€ conplelely reiaigcd lo. tresh wo*ing

The av6€q€ sp€ciEc gdvny oi boulde6 has b€€n taken for €lculalion ol Gstoes has beet

taken as 2 25 rnd on. meter deDlh s take^ for €lculaton ot resNe

Thc Mlnenble re*Ne. €lculsled as pcr Ihe producloN €qliEmenl has been €lculaiei as

s€ilablc wilhin lhe hineabl€ ar6a

.r-r-*" ir-,"1 19"". 11".".111220 ]r1r30 7ll0 I 142200

il4rm trr3ro f7r:rc f i4ri--'i L___t lL-', A22A 21330 71 l0Ir+L-1472A 2tJ30 ;7110 11220f"r, ffitr;;;;; ft:; ."; --;-

t

T.bla Sh@ing lt€ri.l Ha.dling YRdises d M"ed Tsandm l soir,;

4?660

42660 56340

: x@oo

i

I)

)

)

tt?

!,tttt

7.5 R.!l.ni.hh.ntThc mining l6as ar€a being p.d ot lhe Sohan nve. bed is reharged every yea. dunnq

monsoon and sore amounr of edmenls .lso brcught during winter Ems The level ol $e stEam

€,se by on. mcter dling monsmn The whole ot the wo*ed out are shall pbv de 6ndu.ive

ondilEns for deposlion and the dig out aEa is tilled up t]lh ne, bom maler6l. lhe wo.king has

b*n plrnnod m lhe olalioml mann€r by qiving one halt ol the area a chan@ ior €pLenishmenl for

@md.t o^. yer, ol oie tull tuneon tim6 and on€ wnl€. Eins for Hhaainq

7.7 PRODUCTIONPROGRAMHE

7.7{a} Oeveropmenr and Productron ai rh. ond of rhs l6t ysar (Phte No.-s)

Durins l'r Year or development and pbducton Prcg€hme, mhing 6 propo@d in the 63200

Squar. m.t B onlv Thc production of each frineral Constitued willbe as unde. -

I

I .bl. shdinl o€volopmenr .nd Prcdu.r'on In rh. FiEt Yer (Pl.re No.-5)

lsr No Nano of lrir

*searo2

5

11220

Graeh Ahqinc Prcdlction

I

E

IT I

!

ttt

!

I

!I!ISI

7.7(b) D6v.lopment and Production at

Duing 2nd Year ord.velopment and

squa6 m€t€B only. The produclion ol esch

AttoBbtion -Whoe ol lhe area is within the high nood level thereio€thee rs no possibilly of anv

planlation wilhin lhe ease area Lease holder shalimake an aftngem€ntwith land owneF alono lhe

lease aea forconsenlLne to raise p anlation in lh€ sdjoining .nd and ll il l! a govemme't land shal

do p antal on in 6nsu lalion wlh Gram Pa.chav.l and ra se planlalion ol lo€lspecies as dafted Pl

Pretection ot bank6 - A wire crsle glide bundh wi I be conslrucled al c _ 1 ocalion as fr aded in

t

soat dump'Th6whol. ol lhe sca is wiihin hlgh fl@d leve lhereioe. ll is nol pos s ble to pro pose

dumpLng pta@ within th6 lease a€a a.d the w.stage shall be dump€d at oulside place in conslLtation

wiihMnlng olfrcer Dha€nshala pEl€rablv the wastage shou d be 6€d to raise Lowlving ar€as

along baik6which c.n b€lsedlo raseplanlation Possibiliiytouseihe m'le a in ihe road .

consrruction a6 abase layershouldalso be 6xplo@d Topsolshallb€ Kepl separalelv al soildump

and spread over the lznd for plantal on.

Trhl. shoring Developn.nr.nd Poductlon ln the Second Yeat{Plale No's)

the end or the 2"d y.ar (Plata No-'s)

prcduclion PrcaEmne, minng ls p@posed in the 63200

mineEr co.stilenl will be a3 lnder

li'

56330

:ll

cEnh Shnirs Prcducli4 Ot E cn l|lrdl tI dt ?r Y..r

E

I

ot b.nt! - A *ire cEle suld. blndh vll b€ clrelruded at c i2 ldlld * na!|edr_rt

soll d!frF- Th. riole ol lhe 614 is wi$in high f@d l€v61, tl4fore, it b rc

duoDinq ple@ wnhin $e le* ar€a and $6 m3tago sh.ll be dump€d at ouFid€

*lln Mininc Otljc€r, Dhe€msnab p€Labt th6 M3tag. shouh b. us.d io El6e lo* lving a!6along bs}l which on tE u€€d to ai* Pl.nLlion. P@srbihry to use the naled.l in lhe @d

6n trucrion .. a bse lays should de be Bxplorod Top S.il sh.ll be K€9t segaFtslv at &il dump

end.p.6d det 0F l€nd Id plantatlin.

7.t(c) O.v.lopmdt .nd Produc(on :rt lho .nd ol tho !d v..r (Pl.i. No.'6)

Dunns 3d Ydr ot d*lopMnl and ptoduclbn Pro96mtu, mlning i6 prop6.d in lh. 6320It

Sqoab ru!.B o.ly ThE prcduction of €s.h mineEl Con.tilu.nt $ll be 6 unde.

' snis.urd.6 IP.bbt6

)

iauan.nv 41660 t6aao

II

Afio@i.tion - wibl. ot lh6 .@ is wnhn the high iood level, therefffi thBG

ghnlatld wthin lne be .6a L.ese tolder shai make an ar6nq€Mt w r

leae ar€ i.r @neniing lo Eiso prtnl9tion in rhe sdjoining land .nd il rt 16 e

de plenralbn in oonGult tron wltn GEF PandFyal and Eis. pLntalion of loc€r

ii pl€rB lcs

tSr xo----]Efri? xii*:-i I E.arntv i' r""nrtttl tFbutd.B I 42660

F 1u;nimu t =ari3 lsand I 21310

R;nd Mis 3ilt

Gnprr ShwinO Ptirducdon Ol Elch lneEl h Th. 3d Yor

Afi.dt rion - l/Vhole ol th. a@ i! within lhe high fied b€l lhgBfoc ti€F is no po$ibihy of aoy

plant li.n wilhin lh€ lea6e aG L€* holder .hall mako an Emng€rent Ufi land M* alono lh€

L.s .rs lor ds€nling lo 6i.. pl.nialbn in lh. .djoining lend and n is a g@€hm€nt land 'hall

do pl.ni.t@n m @nslltallon wlh GBm P.!.naya! a.d €i.6 pbnlslion ol bel speciee 's

ma'k€d P_3

PELctiq ol b.nlr. - A wne cE€ guide bundh will bc @nEtrucied ar C 3 loers aB ma 'd

in

Soll duhp. The wholo of th. .Ga B within jigh nood lwsl lheEfoF, il js nol posible to prcp@

dunpinlt pl.c6 wi6ti. lhe las aM dnd the rslag€ 6hall be dump'd al outrilo p1a6 in comuhation

wiitt Mhho of@r. ohamshda pBf.dbly the wa61E€t 'h'uld b' u*d io €is low lvinq ar€Es

.bng banh which en be u6€d io 6d. plsntadon Po*ibilrtv io ue tho haletjar.in the o'd

6nsh6lion * a b.* laver should abo b. €tplocd lop Soil shall be K€pl eP'Etely d eil dump

snd 6pi.ad og the land for Pl.nta on

D.rlophot.rd Frcducdd ln th€ Thlrd Yot {Pl.t Io-5}

t

E

€

sodd.c lPobbls

7-7(d) D.v.ropm6nt .nd Productton at the end or the 46 y.sr (pt.re o.-5)

During 4lh Year of dsv.lopm€nr and p@du.tion ProgramFe, mining is popGed n the 63200

Squgte mele6 only. The producipn ot €ach mineEl Consr uent will be as under

v.ropnehland Prodwtion in the Fourth Y*r (Pl*. No.-51

I oc.ndty in ronn6 l

2

5

OFph Sfiwinc Prcduction Ot E.ch ltined in rh6 46 Ye.r

21330

Ie:3

t

Aliob5latlon - Whole of the area is withln lh6 high nood level. tneefoe lhere s no p6sibjli9 ot any

pl5 ntatjon with in lhe lea6e a rea lease holder shall male an a rangenenl with la nd ome6 a long lh6

l€a66 area ior @nsenting to Ei* planlalion in lhe adjoiniig land and if rl is a qoEmment land shan

dd plant.tion in @nslllation wilh O6m Panch.ya! and €ise plantalrd ot l@l specrF as mafted P-4

Pret ctio. ot b.nti - A wire cdle suide bu.dh will be @Flrucled al C - ,l lo€lion as ma*ed in

Plalc No -5

aoil dump. The wnol€ ol lhe ar€a E wth'n h'gh iood level, lheretor€ il s not poseble to poDo6e

dlnrpnliplaewdhmlhelerseaeaandthewsslsqeshallb€dumpedatollsdepb@in.onsuhatonwith Mining olfi@r, Dhersmshals prcfeBbly the wasiage should be usd to €ie low lying a@salonq baiks which €n be u.ed to ai* planlaron. P6sibility ro us the marenal n the oad

golrdcr lPcub.r)

I

l1

mrruction as a b@ lay6r should al5. be a'aloed. Top Soil sh.ll b6 Kept sepabt€lv et $ir dump

and spEd dd th. hnd for pr.ntaton.

7.7(€) D€velopnont and Pmducdon rlth..nd otlh€ 5b vsar (Pl.t l{0.-6)

Dudng lllr Yor ol d€vdopmnt and pEduclion Prcghdm' mining b prop6sd in lh€ 63200

Sq@6 rELE only. Th. prcduclion ot each min.El CoBliluant wilr be as lnd€r

T!bi. sh lng D.v.l6pn.nt tnd Prcdudron h th. Fifr! Y..t (Phr. No.6)

rL;-dMhta-

s63ao

I

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)

tI)

)

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)

t

!tI!I

tuni

21330

Prcductlon of E&h f,llrml ir ttt. 5n Yar

I

Afodl.tlon - Whole oI 0c a@ 15 wilhi. lh. hEh nood level, lhgreloE lhee is no p6sibililv oi 5nv

planlali@ dhtn lh. l6so a@. Lee* holdei 6hall mak6 .n amngerenl {nh hnd owne€ elong th6

bse s.€a ior @n6entng to 6ise planldion in $e adloining bnd and it il b a g@mrent Lnd shall

do pbnt lion h corsuhalion wilh GBm P€*h.val and 6lse phntalion ol lo€l 3Fci6 a3 mark'd P-5

h plsre NF5

Prd.clion ol brnt - A wir. cBl6 gude bundh willbe @n6lruct d alc - 5l@lion * dalled in

soil dqDp- The whol6 ot th. aE. is wilhin high f@d l€v€l lh66lo€ it is nc'l p6!ibl' to pbpG€

duinping r{d tri|nin ,E l€.* area and the w8tag6 .hall b. dumped at oubid' pl* in @nsllitton

wth Mn ng ofic€r, oharsmshala prsferab y thewastaqe should be used lo ralse low lyinq areas

along bank6whdh can b€ us€dloEs€ planlstioi. Possibi yto use the mateial in the road

co^6trucli.n adabasa ayErshouldalso b€ 6xplor€d TopSoi shallb6 Kopt sepddtely at soi!dump

.nd 3pc.do!6rlhe La nd ror pla nrslion

8, Wa3lage Disp.el anangomo.t ifrny:As slready explaii wasle gener:led conla ns Slt mixed sa.d and lop soilwhlch do no( have

any market vslue shal be stacked/ dumpcd somewhere oul ollhe lease area and lhe iver bed in

comu lrtof wnh Mrnmq Ofiicer, Dharamshala and possiblily lo use lh s maleria inlheroadfllnO

mayalso be etploed Topso sha lbe Etackedandsprcadoverlhe land belore raisi.g plailatio..

Trbl. showinq Yeatube Wasle DispG:t Plan

1110

e. 8ecl34!!9!l13!-{eb!e-!.q!)9.t Pl$t tion

Th. .fioEststion Pr€ramme is the most impoda programme lo imprcve the environment

a nd e@logica bala nc6 ol th€ Erea. Grasses End bush€6 sti.h have tibro us r@l3 a re al the firsl

nstance groM wh ch giv€ th6 binding propeny to lhe soi . After gr@ing g€sses and bushes olhe.

lree spec es in con.lllaiion with thB €rp€rts wi b€ raised, based on cha.aclerist 6 of soi.

rooos apr/ sno crnalc co, d rons rhe a'-a proooseo 'or oranr atan E 6 rd{ /r':#=',.T2br.shM'nd Ye. 15.aba lorPlrnbrion 4 , " -

Ptantadon Aea in Squm m.r€E I +-

500 ll

\

T.ble shqrng Yea 15. Aba lor Pltnbrion

s,2 wre cate Guide Bund

FNs No s of wne cEle Guide bund6 wi lb6 raised al localonslo protect lhe banks The

ocal on of chsck dams is shown in Pl.ie No 5 The average lenglh of eacn guide bandh shai be

het.s in l€ngthwth a heLghtof 125 meie6 EstimalE@stoleachwrecraieGudeblndhshal

wil' claleculd. Bundh con.truciion

For @nstruclion of w re CEle Gu d. Bundh,

consrtucl on, on€ mason and one labo€wil

one checkdam sha I be about Rs 30.000/'

E.tlm.t d cocl of Reclamdlon rToerv reclamator Prosramme agadeneronBgllarbasiswillbeempoyed Thegardener

sll wo* 1O dar€ p.r monlh. The btal reclamation c6l aniv€d lor one year shall be lotal coli = 1 0

dayst 12 monrh6 x Rs.2OO- R3 24OOOO/ perAnnum a.d 120000forapeiod ol5vea6

the local maleialwill be used H@ver, lor

b€ employed as andwhen GqulEd Theconslruclonol

11, g$ategy for prot cllon of poinl ol public ulilitv :Thereisnopoinlolpubliculllitvsitualedinfteaea Thor€ is seasonalroad acro$ ihe ease

aEa n lhs str€sm bed which washes awav durnq monsoo. and s construcled each vearfor access

12. Man P orDw.lopmont:

ln order to carry mining op€r.lion 3-10 numberoflabore6 shallbe

on lh6 machin€ry & equipfrenl dnv66 and keeperwllalso be employed'

tlb !q.d for lhe manLi.clunno oJ anl inliE

l

-/',i/ThB Environment Manag6nonl Pkn envilages visualizing lhe

13. lE9-9!-!i!er4!The cnracted ston6 w

emplo4!!..gl*p a watch

1t. Envnonment Manao.m..t Pl.n

Envrcnmeniandslspstobetakentoonlrollhe llefieclsifanyonlheSolArandwaterrcgLme lt

also incudes r6camation ol area or ils best Poss ble ul lialion by way of atfo€staton or olher

P.ogrsmme The pos6ibl.ofiects of mninq and conlro meas!rcs lo be adopled tre discGsed

1

B

i

soil Erosion and Ldd Envlronn.nt

The mining l6a6e ar€s E lolally b.ren a3lh6wholeofthe aca subme.ge in thewaterduing

The slopeofthcrlerbedrsvery gen eandth€speedotlheive.shaInotb€veryhighwhich

may creale any adv€6e 3ilustion €lher work ng in lh€ €ntE pan abng now ol the fiver shal

channellze lhe nvd and shall be he plul in prot€clion of banks and 6hall redue anv

apprehension ol owr fding the banks

Ihe mining would nol make sny adverce chang6 in the prolile ol the nver il the enraclion is

nol beyon'l ihe pemi6s ble lmrt of 1 M depth and is reshcled in lhe cenlEl parl of lhe iver

parallel to th. fl@ of ths water

Waler Rdln.grdEer4delijN. R.urce of w.ter elist3 within

durinq th. monBoon HMve., duing

exc6vabd aea addins slspend€d load

lhe lesse area a.d lhe walerinthe nv$ bed s avaiLable onlv

6iny se.son the waler tom upper levele would flos over th'

2 sub.urft@ wal.r:Th.mining wil nol maks.ny nolrcesble change n

in one y6ar shall be recherged in the nen vear as lhe

msnner. The mlning will nol cause anvchange nlhe sub

no Bffscl on qround wat6r q!.liv. il

and no blastng sha I be canied oul As slch fte

There €n b€ little sound of pLving t6cto6 which

and p.oper ubicat on al regllar intedale

Th6r€ wouLd be no long leh er€d on the Air Envircnment due It6m Eff€cl .e. d edain poinl ol time when lhe @ndiuone are windt

in the 6t6am b.d and this can be minimEed bv spraying waier o' the seasonal oad

The mining wilnot add any toxlc subslance lo the air Envibnment Tle in@ae€ m the

qusnlity ofdud dunng hqhwi.dsls a nallElprocess Butllwillnol €use any adleGe 'ffecl

o !9E4!!!!e!The mining !h.llbe cadied out franualv

no se evel shall b. k6pt under pemi6sible lmLls

can bc Bdled by proper mdrten.n@ of veh cles

l3

The mming sh.llbe €nied oll in

pd.ltin! didatic @ndilions such as on

No fo...l or lorcslland is inlolwd whe€ mining B €nvbaq€d Hene thec rculd be no en€cl

ot mlning on forosl. lhe afoEsraton so.k @ri.d oul 6long lhe l€se€ a€a shall inccase lhe

!!g.r.don cdd s+i.h sh.ll helP in rstalnlng moistu€ conlenb and shdl add to lhe b€.utv of th.

G Es!q!!g!The€ ic no v.g.tation in lh. r.$.d od 4€a €xoepl s€ng gra*.. Hen@ lherc wolld b6 m

r@. ol vegststion. Moeslalion P.ogEmm. will help in incr€as€ ln wgetalion @6r'

.hall nol be theB .3 3udr no

. *dond road acE$ ttE lc.*gnd is rc- aliOn.<I butd an r the

Cllm.t Clr.r6a rery 3n.n .Ba. H.ne

't fill nol eG. .ny efecl on $e

€l ali dat and lampdatuB which aF gi6 in the Table

H E$!ir-!rilCiu!-dr&93!gE9$4qql p6.t or mining on Public building pla@ or nonunents

srruoluc.xid6 in ,nd rtolnd tlE mining leate eEa Th* b onlv

aFa in th. b.d which i. M3hed s.v each v€ar du.ing md&on

I PoliL of Plblic lj0lltv

The sldt gy ld p.oleclion ol Poinb ol Public oliltty haa

J B!!bO49$-e!-6!94!Sge!Ths ecLmatron Plan i6 dlad$.d in dei.il in Para 9 1 and

6nd on P6l @lamllion Plan (Plat . 5) sttacrEd wilh lh€ .eport

K sdlcEconoFic beneflt6 arblno out or mlnl.d

b€en di.cE..d in Parall of lheII

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Minhg e.rsly sh.lls€ne€le etrFoymenl opDonunilie5 to l@l p€tu

bnng .boul upllnnont ln lhoi. €conmv and lh.v could .lso p!tsuit lh€ir on0in'l prof€'lion lik€

aoncu[uc elc.

i6. Anv olh.r Fld.m lniom.don

dt or 6nd clion gcdvily ii p.lvate & Govmment s.dor ls goi'g on Sl@ i3 lh' basic

requi.em6nt ld @n.truclion mat6dal and tE6 B ne€ssilv ot luch tclivilv to flounth in lhe a€a 3o

that lh. EquiM.nt ot lhe nale.ial coold b. m.t lodlly

i6.t,2 Locllion of llineThe lcase aea E located on Ta wara- Dau alpur chowk- lJna Road 'l

a dislan@ oi aboul 12

Khs irom T5[rara m the Sohgn (Swan) nver bed on the eastem s de a.d is also approachable bv

D6hra-Ch ntpuntsKolla Jaswan_ KutheE- Ranoh Road, approximalev 40 Km"rom Oehra The

Sohan rver nows n lhe soulh_ Nodh d Gd'on

l6.l lnhoduction

16l I N'n. ofTh€ Lessee

rE r r Deil DBcribrion Ol Tha Ar..-fh6 minino i€sse is situated n Khasr. No Khasd Nos 1/1 and 7111 measur ng 14_24_93

Nectarcs n Mauj. Kolla MohalRanoh Tehsi Jaw.. D siricl Kangra

SUCCESSIVE MINE CLOSURE PLAN

Discussed in rh6l.li,t eoinl2 5

u.. p.nern ruroihllinq

Ditcu.sed in the !e at pol.( 2,,r .i! ?l!9-!La!!!j! 3howind loetion of lh. l€se are.

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Di&us..d in rhe tert ai polnl3l in dslail {Land

10.1.S M.thodOlMinina

t6.r.4 L.nd llse PalGrn Ol Th. Algi

( i I The mininq/ colLect on or minerals shal inlolve shovelins bv si6pl€ hand-ti*€g{1ealFg inlo

kuck/ kactors Laile6 tor tBfspoding then lo crusher slte' Horev€r, more efficient mining with

sci€nlilc canalizalion ol khld would be possibl€ f pemisson is oblained from the authontes lor

!s€ of mechan €l 6hov. s and loadeF such aB JcB

(2) No blastms shall be esortcd lo lhe leasc area hav ns genlle 3lope lilh g€dient ol 1 40 t6cks for

ih. movement of lrlcks and lractoB can be made and msinla ned in any pan ol the Lease area

(3) TEnch;3,nd pls ror the nin ng purpose ehallbe made in 6uch a wav so that lh€v a€ nol more

$an on6 n6le..nd follow the genBrau nomd channel dnedbn ol the khud'

(4)Wilhthe@p6nishmentolihepitsandlrench€dudnglhehshfloodslheprccessorthe

contrc led inlng can c.nrinue vear ane. v€ar The erosion andweath'nng ol siwalik bouldeF

b6d3 h ths €lchment heve inethsuslible supply ol €quned mineEls

(5) lhough ths frqd mi.ing acllvities wil be underraken durinq $e dry seasons bd restEined

mininq @n b€ under taken dudng lh€ dry davs ol6inv season

(6) Along th6 blnks, gude bunds shalrbe 6ised lo suide th6 fld olwster at approprlats da@ as per

physi€l Equn6ment However wh€nthe bed level al @ntEl pont b broughl doM bvonemeler

theG wil b6 automanc checl in over flow ot waier du'ing nonsoon

16.!.6 lneral Proce$lnq opeallonTh€ basic .equnemenl of the ease Ls to gel supply of stone ol dilfeent sizes lor the

manulaclurng ol grit which €n b6 f6d nto jaw rcld The nver bome sediment! 6hallbe brou€htlo

$e crush.r .l€ snd sh.l be seplrated lo bilu.caie lhe sma I size ol the maleria which cannol be

used for the purpose ol making grl slch ss sand and sard mxed slt The medum size of maGnal

sl'ral be f6d in lhe roller dusher wiil6 siz€ lErger iha. 64 mm shal b€ fed n the law to make gnt

16.1.7 Name & Addrcls Of The Recooni.od Pe6on

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16.2 MINE DESCRIPTION

16.2,1 GEOLOGY

ThB l€ase are. fom Pad orlhe skeam

down durno th6 flood in the streah Thearea

pebbe5, $nd Bsnd mLved silt and cay

Disc6.od ln th.t rt.rpoinlT2lndet il.

(ompnted prcdommanlly the

RIVER BORiIE MATERIAL AND €ND I.'SETABLE SHOW|NG CATEGORIES OR

a;G;;t Mincral/ in,t dar I sizeait in rhe ston e crusher (J aw)

To be sold i. lhe maftel alter

sceening. se paralin 9 clay/silt as

16.2.2 RESEiVE9

Th6 lcase h3s been g.anl6d for lhe procuement ol

slone oru6h6r The €sse a€a falls n lhe ver bed and

pebbles,.sand mx.d clav are alailable in lhe rvar bed

s'w.lk lomatlons Ths bouldeB aB oi quadzite Mini'g is

€wmaleiaLlor m.nulaclurng of srit Ln the

rller borne matera! .s boulders cobbles

which b ge.erale trom lhe ebs o. of the

allowed only up to one meld deplh Asper

ti'i1

\r

KnolErcod Housing B@.d

Ph.n. Noor77-2621053

policy 1/1Orh oi the span lrom th€ banks is ro be left as no mini.g ane ar€ and by t€aying. no mining

arer. the remaining a6. has b€€n raken ior rhe €tcutslion ot potenliatby keping one meter depth

SCP.2 TABLE SHOWING MINEABLE RESERVES OF THE LEASE AREA

i7110121130

12660

56340

56860

I 56330 | 14224 i21330 14220F;a;:lr;;"; h;r;;i v22a ' 21330

17110.i17110 t ,,,, ),

]-ji.-r,42660 I 56830

213300 i28&00

Showins tlin..bl. R.r.ff.. P.oF!.d

i 35550

L ?13t0

L- L' L- l"-

1 5.2-3 lbsqlEclEg4i9!The primary requirement ol the slone crusher is slon€ ol lhe size ol nor more than 60 ms.

sia boulders. The laruer blocls.re hend boken $ rhar rhe same @urd be fed in the primarytaw of

rhe slone cfushe.. The spe otlhe materarbeng led h lhe law 6 franually seperalod to 6ns!€ that

lhe eze ol ihe boulder ol more than 60 cms ae .ol giwn fed tor b€tr€r results and edu.inochanc€s of breakng down oi mach n€ry a.d also enargy Bavinq ope€tion of the machinery The sire

ot bouldeB is tudhe. redudd ln lhe B€condary js to obl.ln.d equiFd 5@ ot ft€ matsial bv Ging

gEnulald, lh6 cqutlEd si4 ol the qdl a3 Fr 6nket demand en b€ pEdued'

16.3 PROGRESSIVE TIIINE CLOSURE PLAN

Th. .rss lies in ihe r€gul* @u@ ol Soh.n (Svan) khud shich Ecl6 nood h moc@n and

al6o oc€lion.l Eins dudng wnL. D!in9 mon&on the miFd od 9it 5G epl€nlshed lo € lal!'

err.nt i. ..6ib.ue 10 ero6l6 ol th. siwalik lom.tion. du. lo heew Eiitall and comequ'nr fasl

nosin! Ml€r tn highq regioh ol th. €lchmenl.

The r€quirened ol lh. applicanl. will b. borltt a of mo€ then sand sla and not mors lhan 60

cm.. 3iE {hi.h can bo Ld inro jd crusher .nd bllor cMhe, No mlning i' dored rilhi' 5 mel€ls ol

€itiler bank or 06 0l lhe sPsn ol th6 khud snichwd is hlghei Th' widlb or lh€ khud of lhe l€ass

.Ba vedes fom 220 io 320 mere6 Henc. no mining ha3 b€€n plann'd i' thb aEa and h6 be€n

6.ft€d es no mlnlnE &n6 h lhe Pl.n Thi6 hes b.€n d$igned lo proitd rhe b€nk3

IHE ININO OPERATION HAS

IHE MEANDERING OF KHAD

BEEN PLANI{ED KEEPING INVIE$T lEPO

!itTh. .8. l@ m lt€ llgul.r coue ol Sohan {Sw.n) khud and O€d Bh dunn! nffi@n and

.bo dunns wlnLr Eins. The depc compns or quartdi"'nd dd t€ai9t or sid ston6r#i

hm$ione and beiaB t€grerns. Th6 bolldeF .e whll"potud whil€' Ei'Fit! wlil€t

rnd dnk green in 6lour 'Ouatt ltc tragrn.nB are Eunded, lub @nd€d ana'i'€

heirg 3moolh surlad Tho si.e veri6 lrcm osel lo bould66 The thickn6s ol deto'it il up lo 3

Donno mo$on lh. min.d orn pits a6 €pl€nlEhed lo tho laE r exl€nt iom lhe e@sion of

.iwallk rom.tiod dle to hdvv Einlell . The 9Ed6t in lhe lea" a@ b very g6ntle as such Budden

dec...s i; lh. e.rying captcilv .nd @mpeloncv ot tF dw at sudt s€dlmetn bed b 3rEd in this

ar6a. llE annuer dePGhion or lhe nwr as 6uch i' th@ io Jout o3 but dl)' lo @nd!6iv6 condition

generat d .luo io mining, th. whol. of the rotlcd od t@ b fuuy Epl'nEhed

Tne baeic ruquiBmenl of gErning le*; is lhe et'btithmert ol dffi cmn€r snd to n€l oul

lh. lupply.of raw ma{.nd wlrich i! th. lizs of horc lhan lht ti4 of $nd and up to lhe 3iz' ol 60

cme rr,.touraers slze ol l.qer lhan 60 dt ennol be f€€d tn lh€ slo€ crushor d@ lo law 3n' of

lhe cn]3'8 rnd betef l@ll of €l€ctrdv @nsundion end abo th' long€r lrt ol tht mdthlnery' as

Fr polcy 1/1On ol th. .pan ol lh€ khsd i5 to hfr nom lhe bsnk6 as m oinin! zon' for th' ptoloclion

of bank , lho t@ ion 22 ml. lo 32 nt . has b4n left es no mining ar€€ 's

€hom ln pl'l. No 5

Th. tad thn minjno on tE con€le bEnk L moD silablo and conwx b l*3 slnabb ior Pdper

"srylsw:"

.,n.l,zanon ol khad bed has been k€Dt nmined so lhat water do nolcha.ge ittchanneldurng heavv

rains and wie.rale glde bundh has aso b€6n planned, keeping in view th€ thrust ot lhe waler

dunng fLood situation Ths nining operalion Ls slggesled to lhe ll@ of the nverwhich shal reduce the

chanes of llooding surcunding area .nd overiowinq ihe banks ll has ben also obseBed in lhe

lpetream area trhee min no lB.ses have been g@nted and beinq wofted that whol€ ol the a€a is

r€plenished dlnng monsoon Hencemnedouia€aofthepre_nonsoonwillbecompl€lelyliledwilh

mircra dudng mon6oon Ho@ver .s an ablndanl p€caulion a qap of o'e year is aLlored for

Ep en shment The a€a on rotat on basis b suqgested in such a wav that pii of previous year mining

w lacl as deposlory lor ths posl monsoon season The wolk3b litv is suggested by keep ng in mind

possibLe etf.ct ol meandenng behavior ol khad if min ng s done on both lhe banks The prc@drnq

y6ar p( wn €du@lhe velocily olwalerflowlnlhe khad, reduci.g iis carryi.g capacitv t'lithe pls are

Elil€dur rnrotarlylheprincipalollhePacerDepo3itisadopted

H6nc., .o rehabilit.tion i6 Gquned h lhe rver bed and

which i6 obta n.d by rolslional melhod HMevsr lor proleciion

bundhs aE pbpos€d al w nereble po n1s es shown n plate No_s

I8.4 CLOSURE PLAN

16.'.1 INEDOIIT LAND

Ths srea lies in ihe r6sulsr@uBe ot Sohan (Swan)khld and oets rain

iko dunng wnter rains. The d€posit compnse ot quad2ile s'nd and t€clon olsad slo'e gBnite

I meslone a nd brcccia s ir.q n enls The bou de rs a € whiie spotled white g'een ish white pr nk puQle

and da* g@n in colour ,Ouartsil6 fragnenls are rolnded, sub rclnded and dis@idal n shape

having smoolh 3udace. As per polcv l/10$ ol the span ofihc khad ls lo left tom fie banks as no

mn no zone tor lh. prolectDn oI banks tha .rsa fiom 22 mls lo 32 mls has been leil as no mining

srea !s shown in plat6 No. 5. The facl lhalmining o.lhe co'€!e bank is no€ suitable aid convex

E rees su abLe for prop€r 6nali4lion olkhad be! has been kepl in m nd 5o lhatwaterdo noi change

l. channelduring healy Einsand wire c€le guide bundh hss also been plann€d keeong in vewthe

thruslollhewalerdldnglloodsllalon-lhemningopeBlionissuggestedloihellowoftheiverwhich Ehel red!@ lhe chan@s of flooding surcunding lhe area snd overflowing lhe banks Hence

no re habilitat on 6 .ec ! ied in iho nver bed a nd only the re plenr shmenl s req u rcd which is obtained

by roiation.lm6thod However lor prot6clion of lhe banks live w rc crate qulde bundhs aE proposed

al vu nerable polnlsas shom in plale No_s

The delailed sy6t6matic proposa s shown n pLate No 5 The mninq is propo*d in the

Dwi3tresm Block in 1'' 3d and 5u vear while uFiream Block

T.bl. SCP'3 sch.fratlc Scheme of su.c6s3ivo cto.ure ofmine

I sucEssrvE cLosuRE

To lre brck fl ed or lo be To

dumped olts de lhe lease in

d@a al appropiale plac€

n consulaton wih m.klnggrl

Mining on.er. ohaEmshala

b€ only nver bom€ tralenal

AFTER I'iTING CHANNELISED RIVER BED

16,rr.2 Water Ou.litY Mrn4enent

The area i€s n th€ reguar coure€ ot Sohan (Swan) khtd which qels flood in lhe rainv

se.3.n othedse lhl6 Pad of the khad remains dry in ihe resl ol ihe vear' Ths is a seasonal khed

The f,h n0 s sugqesled bydigqhglcnches paall€l to the flow ol the waler m the bed Ln such a wav

lh.t mn.d oul pl wilacl as dBposilory lorlheldurc vear Dling monsoon and winbr 'ans

the

mrned oul ar.a is.ep enished io a laae enent is ascribable to erosion ol lhe siwalk lomaton due to

heavy 6nlalland conseque last ftoMns loler n higher region ofthe catchfrent ln the l€ase area

thc gtr di6nl b.rng very genll€ there s sudden dec'ease in ihe enng capacitv snd compelencv oi lhe

ive; Th€ m nrns F suggested in such a wav lh'l mined oul rrenches wil help ii checking lhe rood

TIE sohan kh.d 3 s season.l khad whch rsnams dry lor mosl ol lhe vear bLn Mler ony dunng

monsoon. The wald i6 hesvily loaded wlh se'iimenls du ng llood Mining shall not dislud oler alL

$d m.nls oad or ihe sohan Khad becausE minng is to be lnder laken onlv in a small paich as

compare lo the length of lhc khad There wi l nol be 'nv

chemica contaminafon in lhe water The dug

oul PLi will also help m gblnd water chargnq becalse pil wiladt as adllicialObund waler charge

:-l ,/ .'l'

REI']ABILITATION SCHEME OF FIVE YEARS

TABLE No sCP-,r REHABILITAION SCHEME FOR FIVEYEARS

REHABILITATION SCHEME FOR FIVE YEARS

REFERENCE

5)

N 3001o 900 E 300

c.5

610 E 170

N130 to 210 -E290

Mining Off@r Dharamsha a

oul ol lhe lease a€a as whole

.frhe *se area is wiihin l-lFL

N

N

sand red srlu(bi 6tobe

-oo

ro 950:E

O!n.q 2 " Year dumpedrn.onsurrarionwilh

omq 5b Year

Neoo61250 E 300 io 500

N 7no b 90o -E 300 lo 400

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16.4.3 AtQu.llty Man.s.nenl I: t I

he dee '9

wr''. ll'e '€g-ld' (ou "e of lhc so'd' Khad *h ctlsds'lood r raFv 6'no'

dlsl wll be by the mov6fi.nl .f vehicles lor lhe transporlau'n ol m ne6

orop€.sprav of water w ll be don. oi lhe hsulage @ad

16,4.4, Wasle M.nagBm.nt

The basic EquiBm€.| ol the eate w be spofied white qla'lzite boulde6 for lhe

da.dsclunng of gnt Sinc6 th€ olher components ae not sepadbe from each olher within the bed

b6ing an associaled mincr.l, th€ msteral s lied.s Lump and soned oul dechanicalv in lh€ sione

crlshef lor getino ditfe€.I size ot maleral The s2€ ol less lhan 12mm Mniot be lsed lor the

Dnmg 46 Yd

b"mg r. v"ai

purFs ol g.n na*ino lh6 sdin.nl6 of snd 6i4 and sh.ll€f lnln $nd aE nol epaEbre lnl€srh6!€ !r€ spaBiEd by $nd cl6ifs, Ihe Mslage 3hall nol b. dump€d btcr dthln the lea$ arc.

ss,lFle ofthe las€.€e i. wfthin High no.d Ldd.nd shcllb.m3hed ay dutjnE iood siuerbn.

Mining Ofr6r 3h@rd fnd our rh. My to b.st utli4 lnis MBt g€ to f[ rne ld lying aFa6 n6.r $€

L.s .iL or find oul p63ibilily [o !e lhB natetul in lh. rcad o*sltuclion lo lay dM ba6. lav€r

which 6h.ll b. ln th. intamt ol min€El @n*tdbn lnd al6o shall be sour of addnional Ewnue

elminO b ih. Srat P@ibiw lo spgrste end @nl€nt6lrcs lho sin 3no!U al.o b. nade in lhe

inGcal of min6ralE comaMllon by n@!no nethod

LbL No Scp{YdrWn PRiluclion Ol W-le ourlng Fi6 Yer P.rio<l ln Tonn .

'11220

7110

FV;; 7110

11220

tttm 35550

cnph o AeF! Ahorin! Y@r lM.. Prcdocdon Ot Wat. A SqlDuritrg Fiw Y4r P..iod I. ronB

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tttIJItIb

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LLLIL

r6.a.! oirF..l Of inino ehlnoryTh. mehinery will b€ new and min6 5h.ll be in op€dlion for qolte long lire' th.6bte m

dhn6.l of m.chin.ry B Equned.

41

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t6.1,6 Srlhty ard a.4rilyThenhino.n b. erin on th€ dvq b.d bv diQging uP lo t dadn ol l tFLr -d m bl"trng

i6 hvolsd in it. ltenca, lh.F i. no d.n!€r md no lFclal plgulion is rcqdnd if g!rcEl publb mr:

!E l€ase aF.. ll@v€r, .bnd.d Fec€ufdB .G 'lsay3

to b€ klPt ln min€ iot tF 3€Hv of \rc*eB

and f.nc. th. t€nohes 60 lhat no .nim.l fall ln $. nln'h

lLa.t DLt d.r .naotrln.it And Rbt X'nttd'nlo bl.rling ls in6lv.d and m.lnum dt th d 0E 9il

'hatl not b€ moe lhn d€ meGr'

rh.ELr no 3@9s ol land.lid., fires, lub6ld6no t'iling dam raltuE Htn@ lh'e b no 3c@s ior

di.s6ter elstno to mhhg .dtilv 8.cs. mining aE lr ssnd ti€' b'd and lhm i! m cnem

of sudd€r ru6hhg wai.r .. 3uch no .rlr. Yigil for 0!. 6'l€t 6r stic6 tlm llood wEt€r-F llquiEd

4E

CERTIf'ICATE

Cadfied that provisions of the Himaohal Pradesh Minor

Minerals (Concessio.) ReYised Rules, 1971 and River/Stream Bed Mining

Policy/Guide Lines for the state of Himachal Pradesh have beeD observed

in the Working-cum-EnvironmenFManagement Plan of Sand' Stone &

Bajri Minc ol Smt. Anits Kumar, D/o Sh. Parkash Chan4 on area situated

in Kha$a Nos. lll 2 d1l I I measuring measuring 14-24-98 Hactares ilt

Mohal Ranoh, Tehsil Jaswal Distict Kangra. Himachal Pradesh The

inibrmation Fovidcd ard data fumishcd in fte working Plan is cofiec! to

(KC.K(Retd G los'F0Place

Dele Block R, SStrarvb€rry Hills Shimla-1 71 002

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This is to declare that the Mining_ Cum- Environmenl Management

Plal aod Mine closure Plan ofRiver M Mining comprised Khasra Nos

Kha3ra Nos ltl ud 71/l mm€lsuring 14-2d-98 llectares in M{uj&

Kotlr, Mohtl Rrtroh, Tehsii Jaswrd ' Dlstrict Kttrgrt graDted under

Himacha! Pradesh MiDor Mineral (Concession Rul€s)' l97l in favour of

Anita Kumali D/O ShIi Parkash chand Village Abheypur, Post OIfrce

Bhaddkali, Tehsil Amb, District Un4 has been prepar€d with my consent

anil appmval and that I shall abide by all commitment thereunder' ln case

of any default on my part, the approval of Mining- Cum- Environment

Plan may be with&awn.

DECtfi. TTCIN

Ma*gemmtPlan T-.Yffi*'41*q^-'

(anltr Ku'|lrn)D/O Shn Parkash cha.d

Vilt Abheypu , Po BhaG*ali

Teb ArD Distici Una (HP)Oatdr-

2"

lo1', .ric3o