DiSTRiCr SURVEY REPORT{sAND M:N:NG)′PAL:

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DiSttRiCT suRVEY REPoR丁

{PALI DistHct Minera!survey RepOrt 2018〕

D!STR:CT PAL!PAL:

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，DtsrRlcr SURVEY REPORT (SAND MINING), PALI

(Under Ministry of Environment, Forest & climate chan3c, New Delhi, Notification Date 2g'7'2018')

PREFACE

Sustainable Development is built on three pillars - environmental,-social and

economic. sustainable development can not be achieved if the environment is

protected but poverty is prevalent in a significant part of the population. Similarly,

sustainable development cannot be achieved through inappropriate economic

growth, if it undermines the environment in which people and businesses exists. So

equilibrium is maintained between environment, society and economics. sand/gravel

has long been used as aggregate for construction of roads and building. Today, the

demand for these materials continues to rise. ln Rajasthan, the main sources of sand

are river flood plain, paleo channel sand, and sand from agricultural fields.

Ministry of Environment, Forest and Climate Change (MoEFCC) had time to

time made provisions for obtaining environmental clearance, such as, wide

Environmental lmpact Notification, SO 1533 (E), dated 14th September 2005, made

mandatory to obtain environmental clearance for different kinds of development

projects as listed in Schedule-1.

Further, Hon'ble Supreme Court wide order dated the 27th February, 2012 in

l.A. No.12- 13 of 2011 in Special Leave Petition (C) No.19628-19529 of 2009, in the

matter of Deepak Kumar etc. Vs. State of Haryana and Others etc., ordered that

" leoses of minor minerols including their renewol t'or on oreo of less thon fivehectores be gronted by the StoteslJnion Territories only ot'ter getting environmentol

clearonce from MoEF"; And Hon'ble National Green Tribunal. order dated the 13th

January,2015 in the matter regarding sand mining has directed for making a policy

on environmental clearance for mining leases in cluster for minor Minerals,

The MoEF&CC in compliance of above Hon'ble Supreme Court's and NGT'S

order has prepared "sustainable sand Mining Guidelines, 2016" in consultation withState governments, detailing the provisions on environmental clearance (EC) for

cluster, creation of District Environment lmpact Assessment Authority, preparation

of District survey report and proper monitoring of minor mineral. There by issued

Notification dated 15.01.2016 for making certain amendments in the EIA

Notification, 2006, and made mandatory to obtain EC for all minoi minerals.

Provisions have been made for the preparation of District survey report (DSR) ofRiver bed mining and other minor minerals.

Every effort has been made to cover all matter/issues mentioned in thenotification for district survey report for Jaipur district, The main objective of thepreparation of DSR (as per the Sustainable Sand Mining Guideline) is to ensure thefollowing -

(i) ldentification of areas of aggradations or deposition where mining can be

allowed;(ii) ldentification of areas of erosion and proximity to

and installations where mining should be prohibitedinfrastructural structures

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DiSTRiCI SURVEY REPORT{SAND MIN:NG)′ PALi〔under Mh`try of En」「Onment,Forest&dimate Change′ NewDJhL Notlflcatton Date2507‐ 20181

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rate of reprenishment and aflowing time for reprenishment after mining in thata rea.

(iii) ldentification of mineral wealth in the district.The DE|M and DEAC wifl scrutinize and recommend for EC of mining of minor

minerals on the basis of DSR. This wifi a moder and guiding document *hi.h i*compendium of avairabre minerar resources, geographicar set up, environmentar andecological set up of the district and reprenishment of minerars and is based on dataof various departments, published reports, journals and websites.

The district has substantial resources of euartz feldspar, Asbestos. Lime Stone,Marble, Granite, Limestone, Marble, Rhyolite, Granite, Masonry stone, Bajari (riversand), China clay, Soap stone, Wollastonte, Gypsum, Magnesite, Calcite,Sandsone/Pattikatla.

District Survey Report (DSR) of pali District

Need of DSR:-

As per Gazette notification of 15th January 2016 of MoEF & cc a survey shabe carried out by the District Environment rmpact Assessment Authority (DETAA) withassistance of irrigation department, Forest department, Mining department, Groundwater Boards, Remote sensing Department and Revenue department in the districtat regular interval to for preparation of District survey Report as per the sustainabresand mining guiderines, 2016 to ensure identification of areas of aggradations ordeposition where mining can be allowed; and identification of areas oi erosion andproximity to infrastructurar structures and instalations where mining iirouta-ieprohibited and carcuration of annuar rate of reprenishment and aIowing time forreplenishment after mining in that area.

As per notification it is essentiar to prepqre a survey document mapping thestatus of sand sources and other minerars in a district. This survey shourd beconducted and report be prepared for each district. Though it is an acceptabre factthat rivers cut across districts and states and every river is an ecosystem in itserf. But,keeping in view the fact that the district is the most estabrished unit ofadministration at which this kind of survey, pranning and monitoring can be ensuredeffectively. so, every district wiI prepare this document taking the river stretch inthat district as an ecorogicar unit and inventorising other sources of sand in thedistrict.

The natural resources must be utirized in environment friendry manner inscientific and systematic way and with the objective of sustainabre deveropment thepolicy on the subject shourd have provisions for protection of environment &ecology. These factors can be accounted for in a most efficient manner at districtlevel. The sustainable mining plan needs to be dynamic.DSR of PALI

report of Pali was prepared based on direct and indirect

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DiSTRICT SURVEY REPORT(SAND MiN:NG),PALl

〔under Min:sttt of Enuronment.ForeSt&Climate Change,New De:hら Notttcation Date 25・ 07‐2018.〕

benefits of mining and identification of the potential threats to the river / streambeds in the district. Besides, the production of aggregate in a particular district is afunction of availability of natural resources, the size of the population, the economyof the area and various developmental and infrastructural works being undertaken inthe d istrict.

Every effort have been made to cover sand mining locations, areas & overyiewof Mining actlvity in the Jaipur district with all its relevant features pertaining toGeology & Mineral wealth in Replenish-able Areas of Rivers, stream and gther sandSources. The mineral potential is calculated based on field investigation & geology ofthe catchment area of the river or streams. The area for removal of the mineral in ariver or stream is decided depending on geo-morphology & other factors, it can be50o/o to 60yo of the area of a particular river or stream. other constituents like clayand silt are excluded as waste while calculating the mineral potential of particularriver or stream.

This DSR shall form the basis for apprication for environment crearance,preparation of reports and appraisal of projects.

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AKNOWLEDGEMENT

The authOris indebted to DirectOtt Mines`L Geology Deptt AdditiOnal DirecLor

(MineS and ceology〕 ,Odhpur zOne for pro宙 ding guide lines for preparing

this District Survey Repo■ for Minor Minerals and Bajari Sand〔 Pali District〕

as perthe MOEF guidelines

we express our most sincere appreciation &deep sense of gratitude to Sh. G.S

Inda Suptdg.Mining Engineer,Jodhpur and Sh.Anil Kumar VermaSuptdg'GeologislJodhpur for suggestion and technicar guidance forfinalization of this report as per the MOEF guide lines.

we are also extend our thanks to supporting technicar staffs and Geologist

for preparing and collection data from the field and from literature and finallythey complied as per the MOEF guide lines .

qa+(Dr.Bhanwara Ram.)

Sr.Geologist

Jodhpur

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Mining Engineer

Sojat city

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D:STRICT suRVEY REPORT{SAND M:N:NG)′PALI

(under Min`trv Of Env"onment,Forest 8t c‖ mate change,New DelhL Notincatlon Date 25‐07‐2018)）

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CIIAPTER II. INTRODUCTION

Pali is a city in Rajasthan state of western lndia. tt is

headquarters of pali District and comes in the Marwar region. ltbank of the river Bandi and is 70 km south east ofJodhpur. ltIndustrial City".

the administrative

is situated on the

is known as "The

Pa‖ District has an area Of 12387 km2 The district lies between 24°451 and

26° 291 north iatitudes and 72° 471 and 74° 181 east iOngitudes The Great Aravali hills

link Pali dも tHct wth Almer′ Raisamand′ udaipur and ttrohi DLtncts westem

Rajasthanゝ famous‖ ver Luni and ts t百 butanes JawaL MthadL sukadら Bandi andGuhiabala flows through Pali district The Largest dams Of this area Jawai Dam and

Sardar samand Dam are alsO Iocated in Pali district wh‖e plains Of this district are

180t0500 meters abOve sea level, Pali city the district headquarter′is situated at

212 meters above sea level While the highest pOint of Aravali hills in the district

measures lo99 meters,the famOus Ranakpur temples are situated in the f00tsteps

Of Arava:も Parashuram Mahadev temple,a place Of wOrship f。「milliOns tt devotees

of Lord Shiva′ is alsO 10cated in the Pali district On the hights Of aravali range

District is we‖ cOnnected by rail i e,Delhi Ahemdabad sectiOn Of North―

Western Railway and JOdhpur― Marwar sectiOn of North‐ Vvestern Railway /、 net‐wOrkOf roads is spread Over the district connecting many villages and important cities of

Raiasthan“ ke JOdhpur′ Jaipur Almer,SirohL udaipur etc

l.1.Location and Extent

Pali district is located in the central part Of Rajasthan lt is bOunded by eight

distncts,Nagaur DistncttO the nOrth,Almer DistncttO the northeast,Raisamand

District tO the east′ udaipur District tO the southeast,sirohi Distictto the

southwest′ Jalore District and Barmer DistricttO the west,and Jodhpur District tO the

northwest lt stretches between 24° 44.3560″ to 26° 2714454″ north latitude and

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DtsTRtcT suRVEY REPORT (SAND MINING), pALt(under Ministry of Environment, torest & climate chante, Nen/ Delhi, Notlfication Date z5{t7-2018.)

district is part of 'Luni River Basin' and occupies the western slopes of Aravali range.

The Aravalli Range forms the eastern boundary of the district; the southern boundary

ends at Bamnera village in Sumerpur Tehsil. A zone of foothills lies to the west,

through which run the many tributaries of the Luni River. The western portion of the

district includes the alluvial plain of the Luni. The major part of the district has

elevations ranging from 200 to 300 m above mean sea level, but in the east-toward

the Aravalli Range-the elevation increases and the average is nearer 600 m and at

some places the elevations exceed 1000 m.

Location Map of the Pali District

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DISTRICT SuRVEY REPOR丁 {SAND MiN:NG)′ PAL:{under Ministry Of Environment,Forest&C:imate Change,New Delhi,Notincation Date 25‐

07‐ 2018)

Fig.1.2 Pali District Administration Map

DiSTRICT:PAL:Administrative Map

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II. GENERAL PROFLE OF THE DISTRICT

2.l BRIEF HISToRY OF TⅡ E DISTRICTln 120 AD′ during the Kushana Age′ King Kanishka conquered the Rohat and

Jaitaran areas′ part5 0f tOday's Pali district Untilthe end Of seventh century AD this

area was ruled by the Chalukya King Harshavardhana along with Other parts Of the

present state of Ralasthan

During the periOd from the loth to the 15th century,the boundaries of Pali

extended to adiOining Mewar,Godwad and Mamar Nado!was the capkal ofthe Chauhan clan All Raiput rulers resisted the foreign invaders but individua‖

yfought for each Otherls land and leadership AFter the defeat Of Prithviraj Chauhan,

against MOhammed Gauri, the Rajput pOwer of the area was disintegrated

The Godwad area of Pali became subieCt tO the then ruler of Mewar,Maharana

Kumbha;hOwever Pali city― which was ruled by Brahminrulers with the patrOnage of

neighbOunng Ralput rulers― remained peace施 l and prOgress市 e

The L6th and 17th centuries saw a number of battles h判

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of Pari' shershah Suri was defeated by Rajput rurers in the battre of Giri nearJaitaran, Mughar emperor Akbar's army had constant battres with MaharanaPratap in the Godwad area. After the Mughals had conquered .trort ,ltof Rajputana, Veer Durga Das Rathore of Marwai made organised efforts to redeemthe Marwar area from Aurangzeb, the rast Mughar emperor. By then pari had becomesubservient to the Rathore cran of Marwar state. pari was rehabiritated ry vratrara;aVijaySinghandsoonitbecameanimportantcommercialcentre.

During the British era in rndia in 1857, various Thakurs of pari under thestewardship of the Thakur of Auwa fought against British rure. nuw, to.t *assurrounded by the British army and the conflict lasted many days.

Georogists trace the settrement at pari back to prehistory and maintain thatPali emerged from the ,.rt. *::t:ln sea, which was spread over a large part ofpresent day Rajasthan. rn the Vedic age, Maharshi Javari stayed in this area formeditation and interpretation of Vedas. rn the Mahabharata age, the pandavas arsomade this area (near Bari) thcir resting prace auring exire. ns a part of ancient ArbudaProvince, this area was known as Balla_Desh.

2.2 ADMINISTRATIVESETUP

The pali district in Nine subdivisions viz. pali, Bali, Sojat, Desuri,5umerpur,Rohat, M'Jn'Raipur and Jaitaran. Each Sub-Division is rooked after by the sub-divisional officer/Magistrate under the collector and District Magistrate, pali. oneAdditional District Magistrate is arso present to execute a[ the work. The Districtcomprises of 10 tehsils as follows:

Sub Divls10n

Pa:i

Rohat

Bali

Sumerpur

Saat

Man″ar Junction

Jaitaran

Raipur

Desuri

Desur!

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Pali

Rohat

Bali

Sumerpur

Sojat

MarwarJunctiOn

Jaitaran

Raipur

Desuri

Rani

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No. Of

V‖ lages

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113

70

125

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118

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I驚llil旗灘1葛11捕「‖『雪i冊席1『 [層T』麗標1)as a BDO(BloCk Development Officer)to

serve as the representative of the district administration in the rurai areas

D:SttR:CT SuRVEY REPORT(SAND MiN:NG}′ PALI{under Min`trv Of Envレ Onment,Forest&C‖ mate change,New Dethら Notin(a“ 。n Date 25‐ 07‐ 2018)

Panchayat Samiti No. of No.Grampanchayat Villages

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Rohat

Bali

Sumerpur

Desur

Jaitaran

Raipur

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23

39

29

24

33

35

38

47

29

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109

69

78

114

141

125

148

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DISTR:(I SURVEY REPORT〔 SAND MiNING)′ PALitunder Min:strv of Environment,Forest&c"mate change,New De:hi,Notncation Date 25Ю

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pali District, with population of about 20.4 lakh is Rajasthan,s the L4thmost popurous district, rocated in the state Rajasthan in rndia. Totar geographicararea of Pari district is about L2 thousand km2 and it is the 7th biggest district by areain the state. popuration density of the district is 164 persons per km2. There are 9sub districts in the district, among them pari is the most popurous sub district withpopulation of about 3.7 rakh andRohatis the reast popurous sub district withpopulation of about 1.2 lakh.

*,^^-^ 'n"" are g cities in the district which comes under the district administratron,rnose are

Council; Sojat, Sumerpur, Sadri, Falna and Jaitaran Municipalities (,,r,;:;'iyI'l::lpopulous).

The district is home to about 20.4 lakh people, among them about 10.3 lakh(5070) are male and about 10.1 lakh (50%) are female. ?3% ;;; ;;;;;;;r;;;;are from generar caste, 20yo are frorn schedure caste and 7% are schedure tribes.child (aged under 6 years) population of pali district is 15%, among them 53% areboys and 47% arc girrs. There are about 4.2 rakh househords in the district and anaverage 5 persons live in every family.

The majority of the popuration, nearry 770/o rabout 15.8 rakh) rive in pariDistrict rural part and 23/o (about 4.6 lakh) population live in the pali District urbanpart. Rurar popuration density of pari district is 132 and urban popuration density is1049 persons per km2.

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2.4 cLIMATE AND RAINFALL

l‖pttilliifilil:lill:1[]:il:|;lifi11‖‖:ler:::1lmlょ :lplil

(May‐June}months′ a large vLnaJon intemperature is fOund due tO ad,Oining green and hi‖

y areas Winters are mOderatelycool during December」 anuary when the mercury dips t0 4-5° C range MonsOOnbrings respite from long drawn summers′

11‖|li(:Tllll:IngthemOnth50fJuly―October resultintO average rainfa‖ Of 450

The rainfa‖ is very fairly goOd but erratic The general distributiOn Of rainfa‖

across can be visualized from isOhyets presented in the Plate―l‖ where mOst Ofthe

d st‖ dに∝市ed ttnfal h he mnge d r留

[肌 !nfЪl:T:1::[蓮写::rainfa‖ was 653.4 mm based On the data

nghest ttnfall o"mml wheぃ bw鵡1∬脱ツT‖ftt mml

Ⅲ帥6taverage annual rainfa‖ was received in 3a‖

DiSTRICr SURVEY REPORT{SAND M:N:NG)′PAL:

〔under Ministrv Of Environment,Forest&chmate change,NewDelt NotincationDate和フ‐2018.)

Table: Block wise annual rainfall statistics

Block Name

MinimumAnnual

Rainfall (mm)

MaximumAnnual

Rainfall (mm)

Average

Annual

Rainfall (mm)Ｂａ

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一7017 1,01370 8797

Desuri 645 1,0691o 7762,aitaran 4276 8061 5777Marwar Junction 5529 7472 6957

4659 6368 5382Raipur 358 9586 6892Rani 5828 7379 6484Rohat 4557 5416 4986Solat 3978 8097 5934〉umerpur 5516 7855 637

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PAL| ptsTrycT 5 YEARS RA|NFA| L DAlYear JAN FEB MARCH APRIL MAY JUNE JULY AUG SEPT OCT NOV DEC2012 04 00 77 866 2710 12■ 4 03 002013 120 40 00 10 02 1484 1フ89 1126 199 00 002014

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00 43 77 1723 1992 1310 00 00 0040 924 3739 50 00 00 00

2016 00 02 ■9 00 00 431 2248 5589 224 309 00 00

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DiSttRiCr SURVEY REPORT{SAND M:NING〕′PALi

(Under Ministry of Envヤ Onment,Forest&chmate Change,NewDeli,Notncation Date 25‐K17‐ 2018.)

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Tehsil wise statu5 0f Rainfa!:data Of Pali District〔2017)

S.No District Name of Station Normal

mml Pali Desuri 446 70

2 Pali Marwar JunctiOn 446 70

3 Pali sumerpur 446 70

4 Pali Bali 446 70

5 Paii Rani 446 70

6 Pali Pali 446 70

7 Pali Rohat 446 70

8 Pali Raipur 446 70

9 Pali sOiat 446 70

10 Pali Jaitaran 446 70

Pa‖ Average 446.70

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2.5 TRANSPORT AND COMMuNICAT10NThe only two mOdes of travei available in the district are roadways and

railways

Alrnost a‖ ofthe vittages are cOnnected by rOads There are twO depots

of government_Owned state transport:Pali and Falna

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07‐2018.)

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connected with Jodhpur, Ajmer, Ahmedabad and Udaipur. pali railway stationis on the Jodhpur route whire the second highest earning rairway station in theAjmer division, Falna is on the Ahmedabad route. other important rairwaystations in the district are Rani, Jawai Bandh, Sojat Road and Falna.

The district got the rairway in the earry age of rndian Rairway in 1g81,when the Ahmedabad_Ajmer line opened at Rajputana State Railway. pali gotconnected to Marwar Junction on 24 June 18g2 and to Luni on tz June 1gi4.Jodhpur was connected to the district via Luni in 1gg5 by the Rajputana-Malwa Rairway network and the first train started on this route on g March1885. This line later becomes part of the Jodhpur-Bikaner Railway.

phulera-Marwar Junction line was converted from Meier. Gauge toBroad Gauge in 1995, whire the Ahmedabad-Ajmer rine was converted in1997. During 1997-99, the 72 km Jalore_Falna route was also surveyed bythe lndian Railway, however, the line has still not been laid.

PALI BYAIR

The nearest Domestic Airport is Jodhpur Airport, roughly oneand half hours, drive from pali. Jodhpur Airport is well connecied to aspectrum of cities rike Derhi, Mumbai, and udaipur through Air rndia and JetAirways.

PALI BY MITWAYSpali has its own Railway Station namcd as pali Railway Station

which is connected to the major cities of Rajasthan. rt is rinked with the citiesIike Guwahati, Jaipur, Ajmer, Bangalore, Ranakpur, yeshwantpur, Bikaner,Jodhpur and Mysore.

Pali by road-pali is 5G Km from Luni, 72 Km from Jodhpur, g7 Km from Samdari, j.11

Km from Beawar, 163 Km from Ajmer, 1g5 Km from Udaipur, 294 Km fromJaipur, 322 Km from Bikaner, 355 Km from Kota and is rinked throughRajasthan State Road Transport corporation (RSRTC) and some private trairservices.

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UdaipurJodhpurAimer

BeawarJaipur

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Time

3 hours 6 minst hour 18 mins

2 hours 44 minst hour 57 mins4 hour 33 mins

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L PROFILE OF TⅡ E DISTRICT

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DiSTRiCI suRVEY REPORT(SAND MiNING〕′PALI

(Under MinistryOf Envlonment Forest&climate Change,NewDettLNotinca●。n Date 25-07‐2018)

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S.No Particular Year Unit Statisticsじeographica1 11a tures

(A) pcggraphlcal Data

i)Latitude

螂転

24' 45'to 260 7 5;North

ほ)I On」 tudc720 48' to 7 40 20,

East123870) AdmiisL“ve U」ts 2011

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1052対) Reve{rue villagesX) ASSCmbly Area 6 MLAs&lMP

2. Population(A) Sex-wise 2011 Nos

D Malc1025895ii) Female1012638

〔B) Rural P望型lat10n1578682

3.抑 C

A Land utilizatiOn 2010_11 Hectarei)TOtal Arca

1233079il)Forcst cOvcr

86536

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Cdttrc Land.58485

iv) cultivable Barren land43760

4. Forest(i) Forest 2010-ll Hectare 86536

5. Livestock&POultryA Cattlc 2007 NOs

1)CoWs354698ii) Buffaloes315125B Other livestock

i)Goats700183

真 6505

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BitChes41372

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h Ofr」l lnc 2010-11 Kms 1232

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DlsTRICI SuRVEY REPORT{sAND M:NING)′PALl

(Und"i Mini"try of Er "r,

D"lhi, Notification Date 25{7-2018.)

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(a) National Highway 2010-11 Kms 25870(b)State Higttway 201o_11 Kms 60800(C)Main Distnct Highway 201o_11 Kms 30000(d)OtheF distnct&RuralRoads 201o_11 Kms 310202

蹴:結悧服毀輸

(o Kacha Road

2010_11

201o_11

Kms 40855Kms

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FLAURA & FLATINA OF THE DISTRICT:The extent of naturar forests in Rajasthan is not onry one of the rowestin the country but also the lowest in terms of proJr.tirity of forest. On thecontrary the state is endowed with the rargest chunk of wasterand which isabout 2Oo/o of the total wastelands of tn" .ornif. iotal forests area ofRajasthan is 32639 km2 forests, which is g.S4 % of the total state,sgeographical area. Reserve Forests constitute 3g.16%, protected Forests53.36% and Unclassified Forests g.4g% of the forest area. AcLording to

!ht1n1o-n and seth (1968), a, the forests or this aisirict come under thetropicalforest.

S.No.

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Name of

District

Pali

Reserved

Forest

81945

Protected

Forest

14162

Unc:assified TOta:

Forest

251 96358

The forests of Rajasthan can be divided into four broad forest types.1. Tropical Thorn Forests,2. Tropical Dry Deciduous Forests,3. Bamboo-Forests4. Central lndia Sub_tropical hill forests.5. Mixed Miscellaneous Forests

Tropical thorn forests are found in arid and semi-arid regions ofwestern Rajasthan in pari District. These extend fro, *"rt"rn rndo -park border andgradua'y merge with the dry deciduous mixed r**irlr the Aravari hirs and thesouth-eastern prateau' The moin species found in ii, xna or .orests ore Acocio

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DiSTR:CrSURVEY REPORT{SAND MiNING)′ PALl〔Under Ministry of Environment,Forest&climate Change,New De!hL NOtttcation Date 25 117‐

2018)

2.9 SEISMICITY: As per seismic zoning map of tndia lS 1893 (part_t): 2002,Figure 3.9, the major part of Rajasthan ries in Zone - [ and western parts ofthe districts of Barmer and sirohi as well as northern sections of Alwardistrict lie in Zone rV, where the maximum intensity courd reach vIr (MSK).The remaining areas of Barmer and Sirohi districts, as we[ as the districts ofBikaner, Jaiselmer and sirohi lie in Zone It. The north-eastern districts ofJhunjhunu, Sikar, Bharatpur and the rest of Arwar arso rie in Zone H. The restof the state, including the capital, Jaipur, lie in Zone ll, where the maximumintensity expected would be around MSK Vl, as is evident from the Seismiczone Map of Rajasthan (Figure 1.4) that some portion of district Barmer,Jalore, Alwar and Bharatpur lie under Zone - lV.

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DiSTRiCr SURVEY REPORT{SAND M:N:NG〕′PAL:

{under Mhistry of Enuronment,Forest&climate change,New De:hL NotttcatiOn Date2J島7‐2018.)

FIG: 1.4 MAp OF SEISMIC ZONES OF INDIA & RAJASTHAN

III LAND UTITIZATION PATTERN IN THE DISTRI T

The pre-dominant randuse in the district is agricurture rand 607511 ha

148.27%), followed by fallow land 204610 ha (t6.25%1, barren andunculturable land 14391g (lL.4lyo), permanent pasture 90g62 ha 17.22%1,

Forest land 82010 ha (6.51r%1, Land under non_agricultural use 582g1 ha(4.63%)' curturabre waste rand 45g04 ha (3.63%) and Mining rand 25355 ha(2.07%l

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IV GEOMoRPHoLOGY&soIL TYPES oF TIIE DISTRICr:

The district has undu!ating plains,scattered hills and a cOntinuOus hil:

range passing across sw― NE of the district. Area may be ca‖ ed submountnaeous.The sOuth eastern and nOrth eastern part is traversed by the

Arava‖ i ranges which is the most st「 iking physiographic features oF thedistrict The highest peak Of these h‖ !sis abOut lloomts t0 500mts and slopeis from easttO west.

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Table : land use pattern of pali districtClassification

Forest

Land under NonAgriculture Use

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lunder Ministry Of Enuronment,Forest&climate Change′ New Delhi,Notincation Date 2507‐ 2018)

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tAL WEALTH 5,lGEOLOGY‐

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The geOb」酬brmttOn d the dtiま葛ξl慕[I籠[FI,~葛悪蔀再[R[£ξsedirnentary and met sedirnent rocks The Delhi Super Group rocks represented by

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";;ilil;:'::;:L:,::Ischists' phy,ite, marbre and- basic vorcanic. ,t "r' *" antruded by granites andrhyolites. The predominant of which is the Errnpu-ra g-.r-an ite whicn cover the southand southeastern parts of the district. The ,rr"r" rrpl or cranites is exposed south ofPali. town and is generally pink in colour. The n/ll.*rr super Group occurs in thenorthern part of the district and is represented by rimestone, doromite, sandstoneand share' Georogicar configuration of pari district i, qrit" .orpr"x. rt is comprised ofheterogeneous assembrage of different ritho units oi igneous, sedimentary andmetamorphic origin.

The oldest & prominent rock exposed along district belongscomprising southern, eastern and north ea-stern ,"rgin otferruginous and massive clastics.

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PALI∫under MI雨詢 dttFOヽ me“,Forest&c‖ mate Change,New De生

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with subordinate chemogenic sediments and associated intrusive and extrusivephases' Rocks of this supergroup have been further classified in Kumbhalgarh,Siroh i & punagarh Groups.The Delhi's are succeeded by a sequence of unmetamorphosed sedimentary rockscomprised of sandstone, lim,estone, siltstone, gypsum beds, This Supergroup isfurther divided into Jodhpur Group, Bilara eroria Nrgrur. erorp.The Delhi's are Intruded by granites .na ,.f,yollt.. The predominant is theErinpura Granite.

5.2ECONOMIC IMPACT OF MININGThe mining wi' generate direct and indirect emproyment during mininSoperations and most of the unskired rabour wi, be used for mining purposes andthey will be paid more thanminimum *rg", pl"r*ii.d by State Govt. ln general,there wi'be no adverse effect on t'rrr'n t"rtti ., no brasting or handring oftoxic materiar is invorved. A, the safety measures wi, be strictry forowed toprevent occupationar risk during excavation, roading and transportation. This wi,b":-{frysource of revenue generation for the go-vernment as after getting theqRE,,F;:rilf, ., ," ffifu-=- ,,

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Phyllite, mica schist, nio@migmatite& gneisses epidiorite, Hornablende

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創 c“h史′marЫ %ra雨腱 h■/amphbdに Ыo■eschist′ quartzite′ mica schist and migmatite

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Environment clearance; the minor minerar concessioner wilr have to pay theRoyalty Price, DMFT and GST which will enhance the revenue of the state andCentral Government.

5.3 Mineral WealthPali district is one ofthe few districts of Rajasthan possessing wide variety of bothmetallic and non-metallic minerals. However ,commercial exploitation formetallic mineral has given encouraging results.

Among non-metallic minerals,limestone, magnesite, calcite, quartz, felsper,china clay , ball clay asbestos etc. are the minerar which being exproited for rast somany years. cement grade limestone of Ras belt has attracted manyentrepreneurs for setting up of major cement plants recent discoveries in thedistrict include blockable granite , wolastonite ,scheerite , worframite and

DISTRICr SURVEY REPORT{SAND MiNING}′ PALi(under Minにtry of Enuronment,Forest&c‖ mate Change,New De:hi,No面 catiOn Date 2507‐ 2018)

indication of gold mineralization. A brief description of each occunence Is givenbelow.

Major MineralsrBase metals:- occurrences of base metals haveNayakhera, Kalabar, Birantiya, Kantaliya, Jaitpura,Sandela etc.

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been reported - in chitar,Bar, Sandarada, Punagarh,

Chittar:- Department of mines & geology has investigated copper deposit nearchittar 10 Km from sendra. A wefl deveroped gossan zone extends for about 2kms stricke length with average width of 1.5 to 2.0 mts .it shows variegatedshades of yellow brown ,maroon ,red and vermillion colours . Department hasproved 0.26 million tones of average 1% copper reserves in this areaNaya Khera :- A "L" shaped gossan body extends for about g00 mts . strike rengthwith variable width 1to 15 mts. rn derhi super group of rocks near naya kheraabout 18 kms from sendra - drifling was carried out by the department in the year1973-76 and proved .i.8 million tones reserves having 2g% sulpher ,0.5% copperand 1.76% zinc. The minerarization mainry consist of pyrite with subordinateamound of pyrrhotite , chalcopyrite, and sphalerite . the prppect may -be workedfor sulpher and base metals like copper, zinc can be recovered as by prtducts.Biranthiya khurd:- on the basis of geological investinggation taken up by G.S.l.massive sulphide minerarization hosted by fersic vorcanic unit (quartz mica schist )has been reported in this area .A 250 mts. Long rensoid ore zone has beenestablished in the north brock having smarr reserves of 44906 tonnes with anaverage grade of 4.6y" cu ,5.!5% pb and 10.6% zn. rn south brock ore bodies aresmall and impersistant both in stricke and dip. rndications of gord have arso beennoticed in north block. Samples have shown 150 to 1000 ppb of au.Kalabar:- massive and stringer surphide minerarization is found in karabar area.The rock type are assemblage of differentiated intermediate meta basic (amphiborites )chrorite scnist, carc granurite etc. ancient mining is evidenced bygold working slags and mine dumps occurring in echelon pattern over

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〔underMinistry21EWironment,Foreil&,‖mate change,New DelhL No●

■catbn Date 25‐ 07‐20181

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cumulative strike lengths of 335 mts. Test drilling done by G.S.l. Lelow theoxidized zone has proved the presence "f orrii"'l p]rrrhotite , sphelarite andchalcopyrite .besides.n rnd,:1 ,]c_1ifi.rnt r.tru oingii_a, oornt, se (1_50 ppm )Hg (2as-4000 ppm )and eu gttlt pp, tr,rr";ir;;;", obtained. 1.25 miiliontonnes reserves of massive sulphide zore having i.irri r^and 0.39% Cu and 0.19million tonnes of stringer surphide ,on. hrring'o-.;; cu and 28% Zn have beenestimated between 400_285 M.R_L G.S.t ,, *ra,.riry jrrestigation

in this area.sandarada punagarh etc :- sma, occurrences or teai mlneratization are observednear sandarda, punagarh ,bijaji ka guda areas . ,in"r"iiration is of disseminatedand vein type and shows erratic nature . air born" ,i^"r"f survey division of G.S.l.hasreported indications of base metar ,ir"rJ;;i;;; kantariya area near sojat

Tuntsten:-occu rrences of scheelite have been reported from Bar-Babra area andthese.areas have been explored by G.S.l. ,","rrOi.ri mineralization has beentraced for 10 kms strike rengths in bar area ."d ; k;;;; babra area ,width variesfrom 2 to 10 mts scheerite mrnerarization in the rt.rnr.no*, wide variation ingrade ' exproratorv dri'ing bv G.S.r. h.r pro;ul-;;;rl,"n." of minerarizationdown to 5 mtr. lt has average grade of O.2% Wo, .scheelite mineralization hasalso been reported by department near bar,runora ,-nrna,bera areas . the nanaareas have been explored by drilling .nd purrirt"n."'oi-sctreetite up to depth 132mtr. Have been observing.Occurrence of wolframite has been observed by G.S.l. near motiya_pipliya areanear kurki Minerarization occurs as dissemination in quartz veins at the contactof sewariya granites with mica schist of Delhi Srp", e ,Jrp.Beryl :- lt is an important source of beryllium metal and arso finds extensive usein atomic reactors. lt occurs in many pegmatite U"ai*

"f Raipur tehsil . Recentlydepartment has arso discovered beryt minerarizati"; ;;; Nador in Desuri tehsir .It occurs as large crystals (15_30 cmi I .nO .on1.in ,pto- 1.3% .rate elernent havealso been discovered during chemical analysis_

rhe major deposits., "".-#il,[:1H,5'"Hexproited in pari district arelimestone, Clay, quartz-feldspar, dimensional stone"s Gr"",* & marble), masonrystone & rhyolite. Details of these minerals are as follois:_

Limestone :- limestone is one of the important ,in"rrt, because of its use incement' chemicar, meturargicar, industries. pati drstrict has extensive rimestonebelonging to Delhi Super Group and Marwar Super Group of rocks. Cement gradeas werr as chemicar grade rimestone are found in the district. Major rime stonedeposits are described below :

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occurs as thin veins with an averageextensively prospected and 130 tonnes

associated with Marani igneous suite near Kharda, Kharda Ki Dhani,Dharamidhari, Jitra, Jawariya. The important potentiar areas have beeninvestigated by the department and granite prots have been delineated forleasing. Keeping in view the overwhelming response from the entrepreneurs,search and delineation of granites is in progress in different parts of pali district.Marble :- Search for marbre in pari district. Began during 1960 when first deposit

was explored at Bheru ka Bariya near Bar. The marble of this district has veriedcolours and is figurative at praces . regionar scanning for marbre was done indifferent parts of the district which herped in rocating deposits near Nandana,Ramgarh, Hemadai, Bhirda, Barwantgarh, Gurha rn Raipur and jaitaran tehsirs andnear jedri,sindru,Diyana,Banki,Khiwandi,Siriya ri,Anna, Kantaliya,Vin pura,Sarangwas etc. inBali, Desuri, and kharchi (Marwar Junction )

Most of the marble deposits of pali district are siliceous in nature . thevariegated corour is important due to presence of ferruginous contents, thinbanda of the district. Corours is attractive but the presence of irregurar croseryspaced fractures are creating probrem in extracting big brock and accordingrymarble industries in pari district has been severry affected .Except two,thrlelocalities i.e Hemardai, siriyari, Bhirda, in the most of the areas minirlg is beingdone for sending the materiars to cement industries. The crystafline rimestone issuitable for cement manufacture. Recentry carcsiricate rocks which are hard,compact & occur as shaets have attracted few entrepreneurs for its extraction asblocks as marble near viflage Asan and samer in the district . economic exproitionof such rocks is yet to begain.Rhyolite:- Rhyolite of pari district is mostry reddish brown,grayish brack in corourand is aphantic as well as porphyritic. lt is being worked near Medi Bhaker,Singhari ,Rohat and kharda ki Dhani , where g reases are in oprection. Besides,Rhyolite ,occurrences are reported from punagarh, Manihari, Bamborai, GuraPartap singh, Bhakariwala Gaon etc. in pali tehsil. These can only be utillised asroad ballast or for chip making-

The minor occurrences of non metallic minerals are as followsrAsbestos :- This mineral mainly finds application in making cement pipes, sheet,fireproof clothing etc. the asbestos deposits in pali diftrict .;; iffi; ;;;;sendra, mala ka guda, chhagri ki bhagal , patariya ,goriya , kanotiya, ramgarh,dhanbarli ,ballupura ,ranakpur ,shyampura ,alipura ,elc. rru_rst of the asbestos istermolite veriety but at place thin veins of chrysotile asbestos are also found .mining of asbestos is known for many years in pali district. these days newmining leases for asbestos are banded as per center government directivesbecause it has been considred hazardous minerar for mine & factory workers . theimportant occurrences are described below:-

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reserves have been estimated upto depth of L mtr.

. chariya ki bhaga patriya :- asbestos of tremorite veriety occurs in srip fibersveins . the vein are short, irregular and discontinuous . the reserves have beenestimated to be 6550 tonnes upto a depth of 20 mtr.Goriya :- Tremolite asbestos occurring here is generally a cross fiber type 2G5

tonnes of reserves have been estimated upto 9 mtr. Depth.Dhan Barli :- asbestos occurs as thin cross fiber veins having 2-3 cmsthickness. The reserves are 1,15,440 tonnes a few thin criss_cross veins ofchrysolite have also been observed.

ln addition to these occurrences of asbestos have been reported from aripura,shyampura,patan,sendra,ballupura,patriya and phulad etc.Calcite i calcite occurrences are located at bara guda,Budha Lalwa, Kalab,Kapilki Bhagel , Khemal ,Alipura,kharol ,patan,Dayalpura ,ltimal ,Kurki ,Sardhana,Patariya,sumel etc.These areas mainry fafl in Raipur,iaitaran and Bari tehsir.Most of these occurrences are pocket type deposit.Garnet :- The minerar has been exproited in the past near devkhedi andkaranpura villages of Raipur tehsil .it is found in garnet -r,., ,.i,ri.ni ,. ,,r" i.skarns associated with wollastonite, epidote, quartz and calcite. lt is found atnumber of praces in Raipur and Kharachi tehsir . it is mainry of abrasive quarity.Graphite :- Small occurrences of graphite are rocated near Bar rairway station &desuri. Preliminary investigation by the department have shown that it has verylow carbon content (6-8%)Gypsum:- it has been worked in part near khutani villages. Gypsum occurs inabout 1 sq'km area with an average thickness of about r mtr. rt has been workedearlier by RSMM and few private mines owner.Magnesite :-the minerar is carbonate of magnesium occurring as hard whiteearthy lumps in urtrabasic rock. When free from sirica & iron it is highry varued forit's refractory properties. small g Magnesite occurrences are found near Koyalvav, Bhimana ,talao ,Charria ki bhagel ,bhilan ,phulad ,Siriyari . it occurs as thin veins& stringers in ultrabasic rocks like peridotites , pyroximate etc. A.few smalloccurrences have also been noticed in Desuri tehsil.Mica :- occurrences of muscovite mica are found in pegmatites along with quartz,felsper,and tourmarine in many parts of Raipur and Bari tehsirs. But no workabredeposits has been established.Barytes:- small occurrences of barites are found in punagarh hiI in the forrn ofsmall veins. lt has off white to cream colour and grade is also low. Barytes havealso been reported from Biranthia khurd by G.s.l. it overlies the lenses of massivesulphides along the contect of quartz-mica schist having intermittentry exposedoutcrops of about 280 mts. strike lengts and 1to 3 mL. Thickness it is of lowgrade.

Soap Stone:- small occurrences of soapstone are reported from kanuja,halwat,shyampu-ra ,khormar ,manpura ,kotri ,nandana ,kanoiiya ,asan etc, these are six,{Pt "6r__;;

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D:SttRICT SuRVEY REPORT〔SAND M:N:NG)′ PALi(rna"r r,n*t ot rnr

"rr", ""* Delhi, otificatlon Date 25.ro7_201g.)

mining leases of shop stone in the district.Red ocher/ Red oxide :- it is observed near botha ki dhani in Raipur tehsir whereit was being exploited by private parties . red oxide and clays.r. ilro being founJaround jaitpura and shyampura and have also been worked in past.Wollastonite: - this mineral is mainly used in ceramics. lt is also used in polymers,rubber, paints, plastics, mineral wood etc. it has become important substitute ofasbestos. Good quarities of wofiastonite are found in berka pahar ,kheravparraareas of sirohi and Udaipur districts. These arso extend in pari district. rt is beingworked by M/s wolkern lndia pw.ltd. it is associated with calcite. Both themineral are being mined out.

Recentry department has rocated row grade wo[astonite arong the border ofAjmer and Pali districts. woilastonite bearing skarns containing 20% woilastonitealong with epidote, garnet, quartz, calcite occur as detached bodies. Theseextend from pisangam-gola in ajmer district to alipura ,rawaniy;.,;.r;;;;,gopalpura, karanpura, sodpura, ramawas etc. for more than g0 kms strikelength beneficiation studies conducted by rBM raboratory,ajmer have indicatedencouraging resurts. Driling conducted in three area of pari district nameryRawaniyo , Rampura ,soupura and Gopalpura has proved 79596 metric tonnes ofWollastonite.

sand(8ajri)The district consists of a polycyclic sequence of large alluvial fans comprisingclastic materiar' Consequentry, considerabre raterar and verticar variations arewitnessed in size and shape of clastics and sand grains depending upon theprovenance and size and shape of clastics and sand grains depending upon theprovenance and size of the river. The newer alluvium is restricted io riverchannels. Texture is medium to coarse grain. Minerals mostly constituted ofquartz and ferdspar minerar with rit e micaceous minerarsand heavies, it containsvery little amount of clayey minerals. The sand (Bajri) was extensively qr"r.i"Jfrom Rover Masi, Dhund etc.

5.4 OVER VIEW Of MIIYING ACTIVITY IN THE DISTRICTPari district is one ofthe few districts of Rajasthanlossessing wide variety of bothmetallic and non-metaric minerars. However, commerciar exproitation formetallic mineral has given encouraging results.

Among non-metallic minerals, limestone, magnesite, calcite, quartz, felsper,china cray, ba, cray asbestos etc. are the mineraiwhich being exproited for rast somany years. Cement grade limestone of Ras belt has 'attracted

;;;;entrepreneurs for setting up of major cement plants recent discoveries in thedistrict include blockable granite, wollastoniie, scheelite, wolframite andindication of gold mineralization.

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DrsTRtcT suRVEy REPORT (SAND MtNtNG), pAtr -

(Under Mininry of En limate Chante, New Delhi, Notification Date 2S{r7_2O18.}

The mining activity in the district is administrated by twO mining engineer

offices viz Mining Engineer― SOlat under the cOntrO1 0f supenntending MiningEngineer― Jodhpur circle and AdditiOnai Director―

Mines′ Jodhpur zOne and MiningEngineer Beawar(Raipur tehsiり

under the contド Ol oF Superintending MiningEngineer―Almer Circ!e and AddtiOna!DirectOr― Mines,Jaipur zOne

The Geo!ogica! Survey and PrOspecting Activitv are COnducted by the

Geologists and seniOr Geologist Of the office of superintending Geologist JOdhpur

under the administrative cOntro1 0f AdditiOnai DirectOr―Geo:ogy′ JOdhpur ZOne.ln

dlstnct ll va面 eJes Of majOr minerals and 8 vanejes of minor minerals are 6eing

exp10ited As on 31 10 2018, 10 nos Of major mineral!eases,500 nos Of minor

mineral:eases and 84 QL were under Operation in the district,the statistics of

which are tabulated in fO‖ Owing tables.

Table‐ No of Malo「 Minera!Leases vvith Area,PrOductiOn,Sale Value′Revenue and

Table ―No. Of Minor Mineral Leases with Area, Production, Sale Value, Revenueand

Table‐ No.of

Employment in Pali district SOiat&Raipur office){Year 2016‐ 18S no Mineral Leases Area Production Sale

Value

Revenue Employment

(Hectare) (Tons) (Lac Rs.) (Lac Rs.) (Nos.)1 Limestone

(cement

Grade)

6 2576 81213501 Leases

holderown

Cementplant

974562 750

2 Megnesite 1 4 Nil N‖ N‖ N‖3 Wollestonite 3 3487 N‖ Nil 099 Ｃ

Ｊ

Total 10 261487 81213501 97457・ 19 765

in Pa!i distr:ct Office) (Year 20t6-18S no Mineral Leases Area Production Sale Value Revenue Employmen

t

(Hecta re ) (Tons) (tac Rs.) (Lac Rs.) (Nos)1 Limestone 46 3072 7670760 400-500 545692 750

Granite 21696 1365702 150■3000 20825 ０ＣＪ

ｎフ

3 Mesonarystone

201 Ｌ̈ツ

０２

4031576 220-26022355 1550

4 Rahylite 28 3735 118128 200-250 805 200ＥＪ Quartz

Feldspar13 112

79948250-300 458 220

6 Chaina

clay/Ballclay25 551

3092340350500 1838 500

7 Marbie 1 1 Nil Nil Nll NilTotal Ｅ

●■ι

４ 419531 16358454 1173922 4170

Value,

,

Minor Mineral Leases with Area, production, Sale Revenue

¨

D:STR:Cr SURVEY REPORT{SAND M:NING),PAL:(under Minifiy of Environment, Forest & climate change, New oelhi, Notiflcatlon Date 25-07-2018.)

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CHAPTER V:

6 RIVER OR STREAM AND OTH[R SAND SOURCES

・

111:11とイ争LT,d gravei are one Of the most important

4

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Udesikuwa/

Sttat/

pali

KHUSHAVIR SiNGH 3997

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SAIJAN SINGH 186

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SHOBHARAM

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Duda ram 24055

Details of Revenue and production from sand/ Bajari received in rast five

Production(in tonnes)

Revenue from bajri/sand(Rs in Lacs)

2013-20■ 4 1410441

2121145

19663116.46

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construction materia:s

赫 44

YEAR

2441999

2014-2015 2179920 1738972

2015‐2016 2511005

2016-2017 2418343 21637.8

2017‐ 18 2096160

2018-19 N‖ Nil

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〔under Minttry of Environment,Forest a climate alange,New DeihL NOtttatbn Date 2●720181

lnternal drainage in ocurring south eastern and north eastern part formed byseasonal nala coming out from rocar hifly region. The deposition of sand/Bajri in naraocuurs locally during rainy season.(6) Marwarln Marwar Panchayat samiti area is having Bandi, sukri Khari and Mithri rivertributries. lnternar drainage in ocurring south eastern and north eastern part formedby seasonal nala coming out from rocar hiily region. The deposition of sand/Bajri innala ocuurs locally during rainy season.(7) Rohat

ln Rohat Panchayat samiti area is having Bandi, Guriya, Rediya, sukri and phuphariariver tributries. rnternar drainage in ocurring south eastern and north eastern partformed by seasonal nara coming out from rocar hifly region. The deposition ofsand/Bajri in nala ocuurs locally during rainy season.(8) Sojatln sojat Panchayat samiti area is having Gurhiya, Rediya, sukri and phuawariya rivertributries. lnternal drainage rn ocurring south eastern and north eastern part formedby seasonal nala coming out from rocar hi[y region. The deposition of sand/Bajri innala ocuurs locally during rainy season.(9) Sumerpurln sumerpure Panchayat Samiti area is having sukri, Mithri and Jawal river tributries.lnternal drainage in ocurring south eastern and north eastern part formed byseasonal nara coming out from rocar hily region. The deposition of sand/Bijri in naraocuurs locally during rainy season.

Drainage system with description of main rivers

The district has a poor drainage system which too is internar. pari district fa[s inthe Luni & Barmer Basins. Major River of the district is Luni, which flows in ENE _wsw direction. rt enters pari district near viflage Ras in Raipur tehsir and reaves thedistrict Eari near vilage Amli. channer pattern of Luni is dendritic to sub-paraIer.However, in major part of the district, the drainage is essentially ephemeral andinternal' Tributaries to the Luni river are sukri, Lirri, Jawar, Bandi. other streams inthe district are Guhiya, Mithari, Kherwa and Khari which are all ephemeral.

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一一

S.No. Name of the River Area drained

lSq.Km)

%Area dralned in the

Distnct1 Raipur Luni 20.44 01652 Sukri Nadi‐ | 1725 0.1393 Lilari Nadi 450 00394 Gudiya 4.80 0038一ｂ Bandi 21 0_1696 Sukri― ll 645 0_520

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PALl〔Under Ministry of Env"onment,Forest&c‖ mate Change,NewDettι No■ ,ca● ●n Date 2507‐2018)

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DescriptiOn ofimpOrtant rivers is as under:_ ‐

い〕Lu面

Rang[:i:IC[|(1:ll。 lr暮 l]::itn:::11Fil」 Itl』51lSII:rll:el。 :;‖ll :`:Ii‖lwestern of Ralasthan,■ disappears in the marshy!and OfRann Of Kutch The totalcatchment area of the Luni River 8asin in Ralasthan is 37,363 km2,coverlng parts of

thiliStricFil富

∬ill:l‖:dhpur′

Nagaur,Barmer′ Ja10re and Gularat in Ralasthan

(b}Guhiva

m:n.rIIttFT訥鵠1器匙「‖誌願引l戦犠i窯

I思躍1距3,835 km2,which is situated in Pali district lts tributaries are Raipur Luni′

Radia Nadi′

lclKh」riHel露attL Suk‖

and Phunpha"a Baぬ

River Khari is fOrmed by the cOnfluence of sma‖ streams namei' sOnnesarけu面…計sOmew酬

…囃腱ISm耀訛榔l蹂!讐鷺II:::淋

all:i志

iミ:liil:‖:la‖ :i::lilir Reserved Forest Bhakar′ after flow OfabOut 30 km)After joining Of a‖ these smali streams,the nver is called Kha‖

AFterlowing fOr about 25 km′ lt,Oins Bandi River downstream of Hemawas reservOir ttscatchment area is l,232 km2

(d}Bandi(Hemawas}Near BOmbadra pickup weir Khan and Mthan Hvers ioin and fOrm the Bandi River

Later Bandi nveriOins the Luni near the Lakhar viliage′after 10wing for about 45 km

The catchment area is about l,685 km2 and Situated in Pali District

{e)M■hari

Mithari river originates by cOnfluence of:Ocal nalas in the sOuth_western siOpes of

聾漁詭塾輔曲上J膿11囃灘riS l,644 km2

「 ドuk‖

Sukri river is fOrmed by the conf!uence of several sma‖ nalas _ Ghanerav NadL

M‖翼]ド f甜′ポ請1‖札:ょ ど1:点

ng tt° m meAmv訓もh Ptt and udJpurl―west directiOns for abOut llo km and

feeds Bankli Dam on the wav NearSamdanin 3armer Dlstnct,it iOins Luni“ver

The Ja10re′ Pali and Barmer Districts are cOvered in this sub_3asin lts catchment area嶋Ψ給 ‐

:静芹ン _

壕 トー

(g)Jawai

Jawai river originate in Udaipur district with its main tributary sukri in the westernslopes of the Aravalris. rt joins Khari river in Jarore district near say.r.. ii. ,ir"r'rr"*,in a north-west direction for about 96 km before that. rts catchment area is2,976 km'z. Report

DiSttR:CI SURVEY REPORT{SAND MINING)′ PAL:(Under Minlstry of En imate Chante, New Delhi, Noflflcatlon Date 25-07-2OtE.)

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{under Ministry of Environment Forest&aimate change,New De:hL Notncatton Date 25 07‐2018.)

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。n Date 25‐ t17-2018)

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6 3 SALIENT FEATURES OFIMPoRTANT RIVERS AND STREAMS

Salient Features Ofimportant Riv nd S

6.4Availab‖ity Of sand Or grave:or aggregate resources in Pali:_

This has already been briefed in the preceeding paras The resOurces are on the

banks Of Luni river are sukri′Lilri′ JawaI′ Bandi other streams in the distri(■

areGuhiya′ MitharL Kherwa alld Khari etc

nt Rtvers a trearnsS.No. Name of the River

or StreamTotal Length

in the District

(in Km)

Place of origin Altitude at Origin

1 Bandi 12495 Bhupat Ka GurhaSingpura

4602 Cuiriya 1221

3228334３

一４

Rediya Lonera 224Sukri 21938 Giri 339

5 Phtlnphariya 3419 Surayata

Sumel2366 107553957 ａ

Ｌ”

νヽ 3560 Perva 302８

　

９

Somesar

Khardi5707 Somesar 5002603

7457Khariya Swaniva

Motagura26910 Mlh●370■

■ Khot Ki Nadi 2544

…

42012 Magai 2996 Jaton ki Doran 37013 iawali 5156 Khaubban ka Gura 37614 Raipur Luni 5516 Lalvacha 37815

16

Tatawari

Jawai

1112

4972

Mahaveer ji templen ear Kundai

434

Dharcial 41117 7552 Oariyara 235

R.K.CONSULTANTS tCHEMiCALANALYSiS D:VIS:ON〕17げ″ ,C.H.町 J●dhpur i贅1.〕

Telefax.0291‐ 270 6098 ha‖ ―歯consu:tant珈劇hpurOMal.COm

R‐,●●lta02

NABLTC1 5788

RepOrt No.:RKC/2019・ 20/130 Date:20.05.2019

TEST REpORT

Day Tlme(600● m.to 10.00P.m.)`Nightttme〔 1000p.m to600a m)Th"reporttnottobereproducedwhOllyorinpartandcannotbcusedaseЙ dence:nthecomoFL喘SubleCttO'Odhpurrurlsdldon o■ ,

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NaDe & Address of CustomerShd3ogttnghSrOShHG●e Sltth

Ⅵ‖age-3● la,Khasra No.-197

Tehs‖ &Distnct― Pa‖ 〔Ral.)

ProleCt

Reference No.

Nolse Sample Code RKC′N/130

Type of Nolse Monltorlng Amb:ent Noぶ e

Date OfNoise Monitorlng 1505.2019

Monltorl● g Stan Date 15052019

Monltorltrg Ead Date 16.052019

EnvlmnmetrtalCondldons :

A Temperatsrre,oC :

& Rdaive Humtdltv,96 :

25■ 2●C4896

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Ｎ。

LOCAT10N UNr SPL LeqDay Time 山

血Ｎ

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1 Mineま te dB(A〕 64.3 33.6