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し DiSTRiCr SURVEY REPORT{sAND M:N:NG)′ し PAL: 輌 mmat“ ヽ 眈 ・ 晩W田 軋恥tLLお ・“ 塾 "changら n Date 2"″∝鋤 ヽ DiSttRiCT suRVEY REPoR丁 し
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し YEAR 2018‐ 19
し :n comp!iance of Ministry Of EnvirOnmel ヽ
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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 five hectores 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 with State governments, detailing the provisions on environmental clearance (EC) for ヽ cluster, creation of District Environment lmpact Assessment Authority, preparation 民 issued of District survey report and proper monitoring of minor mineral. There by Ц Notification dated 15.01.2016 for making certain amendments in the EIA Notification, 2006, and made mandatory to obtain EC for all minoi minerals. Ｉ Ｆ Provisions have been made for the preparation of District survey report (DSR) of River bed mining and other minor minerals. ミ Every effort has been made to cover all matter/issues mentioned in the ー ア notification for district survey report for Jaipur district, The main objective of the preparation of DSR (as per the Sustainable Sand Mining Guideline) is to ensure the ヽ following - (i) ldentification of areas of aggradations or deposition where mining can be allowed; (ii) ldentification of areas of erosion and proximity to infrastructural structures and installations where mining should be prohibited
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＾ DiSTRiCI SURVEY REPORT{SAND MIN:NG)′ PALi 〔under Mh`try of En」 Onment,Forest&dimate Change′ 「 NewDJhL Notlflcatton Date2507‐ 20181 ヽ
rate of reprenishment and aflowing time for reprenishment し after mining in that a 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 and ecological set up of the district and reprenishment of minerars and is based on data of 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 (river sand), 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 sha be carried out by the District Environment rmpact Assessment Authority (DETAA) with assistance of irrigation department, Forest department, Mining department, Ground water Boards, Remote sensing Department and Revenue department in the district at regular interval to preparation for of District survey Report as per the sustainabre sand mining guiderines, 2016 to ensure identification of areas of aggradations or deposition where mining can be allowed; and identification of areas oi erosion and proximity to infrastructurar structures and instalations where mining iirouta-ie prohibited and carcuration of annuar rate of reprenishment and aIowing time for replenishment after mining in that area. As per notification it is essentiar to prepqre a survey document mapping the status of sand sources and other minerars in a district. This survey shourd be conducted and report be prepared for each district. Though it is an acceptabre fact that 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 of administration at which this kind of survey, pranning and monitoring can be ensured effectively. so, every district prepare wiI this document taking the river stretch in that district as an ecorogicar unit and inventorising other sources of sand in the district. The natural resources must be utirized in environment friendry manner in scientific and systematic way and with the objective of sustainabre deveropment the policy on the subject shourd provisions have for protection of environment & ecology. These factors can be accounted for in a most efficient manner at district level. The sustainable mining plan needs to be dynamic. DSR of PALI District survey report of Pali was prepared based on direct and indirect ・ 3 ― 曼 奎 屋 ヽ
ヽ DiSTRICT SURVEY REPORT(SAND MiN:NG),PALl ヽ
〔under Min:sttt of Enuronment.ForeSt&Climate Change,New De:hら Notttcation Date 25・ 07‐2018.〕 ヘ benefits of mining and identification of the potential threats to the river / stream ヘ beds in the district. Besides, the production of aggregate in a particular district is a ヘ function of availability of natural resources, the size of the population, the economy of the area and various developmental and infrastructural works being undertaken in ヘ the d istrict. Every effort have been made to cover sand mining locations, areas & overyiew of Mining actlvity in the Jaipur district with all its relevant features pertaining to Geology & Mineral wealth in Replenish-able Areas of Rivers, stream and gther sand Sources. The mineral potential is calculated based on field investigation & geology of the catchment area of the river or streams. The area for removal of the mineral in a river or stream is decided depending on geo-morphology & other factors, it can be 50o/o to 60yo of the area of a particular river or stream. other constituents like clay and silt are excluded as waste while calculating the mineral potential of particular river or stream. 」 This DSR shall form the basis for apprication for environment crearance, 諷 preparation of reports and appraisal of projects. 」 Ｒ Ｆ ｋ ｌ ｋ 」 ヽ F, ●fミ ヽ3 1ギ ヤ子」 Pヤ 」 口1.w■ ‐Fン嗣帥 ′ 翁.覇粋 ヽ 雨 漏RFa ビ 爺qヽ ・) ヽ ， ヽ ヒ ヽ 口 ヽ 日 へ ‥ ヘ ーミ Ｆ へ ‐ ヽ
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し AKNOWLEDGEMENT ヽ
し The authOris indebted to DirectOtt Mines`L Geology Deptt AdditiOnal DirecLor
ヽ (MineS and ceology〕 ,Odhpur zOne for pro宙 ding guide lines for preparing this District Survey Repo■ し for Minor Minerals and Bajari Sand〔 Pali District〕
ヽ as perthe MOEF guidelines
ヽ we express our most sincere appreciation &deep sense of gratitude to Sh. G.S し Inda Suptdg.Mining Engineer,Jodhpur and Sh.Anil Kumar Verma し Suptdg'GeologislJodhpur for suggestion and technicar guidance for ヽ finalization of this report as per the MOEF guide lines. し we are also ヽ extend our thanks to supporting technicar staffs and Geologist for preparing and し collection data from the field and from literature and finally they し complied as per the MOEF guide lines .
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し qa+ (Dr.Bhanwara Ram.) ヽ R VishnOi〕卜 η
し Sr.Geologist Mining Engineer
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CIIAPTER I し I. INTRODUCTION
Pali is a city in Rajasthan state of western lndia. tt is the administrative headquarters pali of District and comes in the Marwar region. lt is situated on the bank of the river Bandi and is 70 km south east ofJodhpur. lt is known as "The Industrial City".
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 and ） Guhiabala 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 し measures lo99 meters,the famOus Ranakpur temples are situated in the f00tsteps し 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 ヽ
District is we‖ し cOnnected by rail i e,Delhi Ahemdabad sectiOn Of North― Western Railway and JOdhpur― し Marwar sectiOn of North‐ Vvestern Railway /、 net‐ wOrk Of roads is spread Over the district connecting many villages and important cities of ヽ Raiasthan“ し ke JOdhpur′ Jaipur Almer,SirohL udaipur etc
ヽ l.1.Location and Extent
ヽ Pali district is located in the central part Of Rajasthan lt is bOunded by eight
し distncts,Nagaur DistncttO the nOrth,Almer DistncttO the northeast,Raisamand
ヽ District tO the east′ udaipur District tO the southeast,sirohi Distictto the
ヽ southwest′ Jalore District and Barmer DistricttO the west,and Jodhpur District tO the
ヽ northwest lt stretches between 24° 44.3560″ to 26° 2714454″ north latitude and ヽ ‐ “ …… ） 」 茸
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DtsTRtcT suRVEY REPORT (SAND MINING), pALt ヽ
(under Ministry of Environment, torest & climate chante, Nen/ Delhi, Notlfication Date z5{t7-2018.) ヽ
へ district is part of 'Luni River Basin' and occupies the western slopes of Aravali range.
ヽ 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
¨ 匡 ― DiSTRICT:PAL: Administrative Map
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II. GENERAL PROFLE OF THE DISTRICT
2.l BRIEF HISToRY OF TⅡ E DISTRICT ln 120 AD′ during the Kushana Age′ King Kanishka conquered the Rohat and ヽ 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 of the Chauhan clan All Raiput rulers resisted the foreign invaders but individua‖ y fought 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 1磐 ヽ 盪 , し __ =:蒻
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DiSTR:CI SuRVEY REPORT(SAND MiN:NG)′ PAL: ヽ 〔under Ministry of Environment,Forest a climate change,New De:hi,NotttcatiOn Date 25‐ 07‐2018.) ヘ of Pari' shershah Suri was defeated by Rajput rurers in the battre of Giri near ヘ Jaitaran, Mughar emperor Akbar's army had constant battres with Maharana Pratap in the Godwad area. After the Mughals had conquered of .trort ,lt Rajputana, Veer Durga Das Rathore of Marwai made organised efforts to redeem |ヘ the Marwar area from Aurangzeb, the rast Mughar emperor. By then pari had become subservient to the Rathore cran pari of Marwar state. was rehabiritated ry vratrara;a VijaySinghandsoonitbecameanimportantcommercialcentre. ト L During the British era in rndia in 1857, various Thakurs of pari under the stewardship of the Thakur of Auwa fought against British rure. nuw, to.t *as L surrounded by the British army and the conflict lasted many days. L Georogists trace the settrement pari at back to prehistory and maintain that L Pali emerged from the ,.rt. *::t:ln sea, which was spread over a large part present day Rajasthan. of L rn the Vedic age, Maharshi Javari stayed meditation in this area for and interpretation of Vedas. rn the L Mahabharata age, the pandavas arso made this area (near Bari) thcir resting prace auring exire. ns a part of ancient Arbuda L Province, this area was known as Balla_Desh. L 2.2 ADMINISTRATIVESETUP L The pali district in Nine pali, subdivisions viz. Bali, Sojat, Desuri,5umerpur, L Rohat, M'Jn'Raipur and Jaitaran. Each Sub-Division is rooked after by the sub- divisional officer/Magistrate under the L collector and District Magistrate, pali. one Additional District Magistrate is arso present to execute a[ the work. The District L comprises of 10 tehsils as follows: k Sub Divls10n Tehs‖ s Nagar/Township No. Of ミ V‖ lages Pa:i Pali ヽ 1 88 Rohat Rohat 0 80 民 Bali Bali 2 113 Sumerpur Ц Sumerpur 2 70 Saat Sojat 1 125 Ц Man″ar Junction Marwar 1 157 . ミ JunctiOn Jaitaran Jaitaran k 1 118 Raipur Raipur 0 141 （ Desuri Desuri 1 81 ヘ Desur! Rani 1 77 「
ntains a number Of Pa ヽ
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「『‖雪i冊 席1『 [層T』麗標1 I驚llil旗灘1葛11捕)as a BDO(BloCk Development Officer)to serve as the representative of the district administration in the rurai areas
Panchayat Samiti No. of No. Grampanchayat Villages し Pali 23 82 ヽ） Rohat 23 81 Bali 39 109 Sumerpur 29 69 Desur 24 78 Jaitaran 33 114 Raipur 35 141 Solat 38 125 MarwarJunctiOn 47 148 Rani 29 77 ） ＰＡ Ｌ ＝ ） Ｄ ¨ ム 一 し ゴ
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ヽ 2.3 PHIC PROFILE
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pali District, with population of about 20.4 lakh is Rajasthan,s the L4th most popurous district, rocated in the state Rajasthan in rndia. Totar geographicar area of Pari district is about L2 thousand km2 and it is the 7th biggest district by area in the state. popuration density of the district is 164 persons per km2. There are 9 sub districts in the district, pari among them is the most popurous sub district with population of about 3.7 rakh andRohatis the reast popurous sub district with population of about 1.2 lakh.
are g cities in the district which *,^^-^ comes under the district administratron, rnose'n"" are Council; Sojat, Sumerpur, Sadri, Falna and Jaitaran Municipalities (,,r,;:;'iyI'l::l populous).
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 pali of district is 15%, among them 53% are boys and 47% arc girrs. There are about 4.2 rakh househords in the district and an average 5 persons live in every family.
The majority of the popuration, nearry 770/o rabout 15.8 rakh) rive in pari District rural part and 23/o (about 4.6 lakh) population live in the pali part. District urban Rurar popuration density of pari district is 132 and urban popuration density is 1049 persons per km2.
Caste wlse Male ttmale pOpulatわ ¨ n2011‐ Pa‖ 』 ¨ ｋ 』 ¨ Ｌ ¨ 』 聖 ¨ ヽ ＾３ ● ¨ ｂ α ヽ Ｌ ０ ¨ ０ ヽ ｚ ¨ Ｈ ¨ ヽ ‥ ¨ Ｌ ¨ ヽ 。 ヽ
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） ） DiSTRICr SURVEY REPORT{SAND M:N:NG)′ PAL: ） 〔under Ministrv Of Environment,Forest&chmate change,NewDelt NotincationDate和 フ‐2018.) ） 2.4 cLIMATE AND RAINFALL ） Ｌ ‖:ler:::1lmlょ :lplil l‖ pttilliifilil:lill:1[]:il:|;lifi11‖ (May‐ June}months′ a large vLnaJon in ヽ temperature is fOund due tO ad,Oining green and hi‖ y areas Winters are mOderately cool during December」 ） anuary when the mercury dips t0 4-5° C range MonsOOn brings respite from long drawn summers′ 」 October resultintO average rainfa‖ Of 450 11‖|li(:Tllll:IngthemOnth50fJuly― ） 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 rainfa‖ was 653.4 mm based On the data [肌 !nfЪl:T:1::[蓮 写:: ） nghest ttnfall o"mml wheぃ bw鵡 6t average annual rainfa‖ Ⅲ帥 ） was received in 3a‖ 1∬脱ツT‖ ftt mml ）
ptsTrycT ） PAL| 5 YEARS RA|NFA| L DAl Year JAN FEB MARCH APRIL MAY JUNE JULY ） AUG SEPT OCT NOV DEC 2012 04 00 77 866 2710 12■ 4 03 00 2013 ） 120 40 00 10 02 1484 1フ 89 1126 199 00 00 2014 00 00 00 43 77 」 1723 1992 1310 00 00 00 2015 11 00 40 924 3739 50 00 00 00 2016 ） 00 02 ■9 00 00 431 2248 5589 224 309 00 00 ） Table: Block wise annual rainfall statistics ） Minimum Maximum Average 」 Annual Annual Annual Block Name ） Rainfall (mm) ‐ Rainfall (mm) Rainfall Ｂ ａ ｉ (mm) ） 一 7017 1,01370 8797 Desuri 645 1,0691o 7762 」 ,aitaran 4276 8061 5777 Marwar Junction 5529 7472 し 6957 4659 6368 5382 ヽ Raipur 358 9586 6892 Rani 5828 7379 6484 ） Rohat 4557 5416 4986 Solat 3978 ） 8097 5934 〉umerpur 5516 7855 637 ヽ ） い ） ヽ珈 輔 ） ・ ・ ） ヽ 』 一 ヽ
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） Tehsil wise statu5 0f Rainfa!:data Of Pali District〔 2017) し S.No District Name of Station Normal ヽ Actual DeviatiOn mm mm % し l Pali Desuri 446 70 l17200 16237% ） 2 Pali Marwar JunctiOn 446 70 95800 11446% 3 Pali sumerpur 446 70 ） 90500 10260% 4 Pali Bali 446 70 84400 8894% ヽ 5 Paii Rani 446 70 83700 8737% 6 Pali Pali 446 70 Ｌ 77800 7417% 7 Pali Rohat 446 70 67200 5044% ） 8 Pali Raipur 446 70 623.00 3947% 」 9 Pali sOiat 446 70 5410o 2111% 10 Pali Jaitaran 446 70 し 477_00 678% Pa‖ Average 446.70 し 780.70 74.77%
ヽ 2.5 TRANSPORT AND COMMuNICAT10N し The 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 し of government_Owned state transport:Pali and Falna
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ヽ ヘ D!STRiCI SuRVEY REPORT(SAND M:NING)′ PALi ヘ {under Mhistry of Environment,Forest&Gimate Change,New De:hi,NOtncaJon Date 25・ 07‐ 2018.) ヘ connected with Jodhpur, Ajmer, Ahmedabad and Udaipur. pali railway station ヽ is on the Jodhpur route whire the second highest earning rairway station in the Ajmer division, Falna ヘ is on the Ahmedabad route. other important rairway stations in the district are Rani, Jawai Bandh, Sojat Road and Falna. ヽ 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 got connected to Marwar Junction on 24 June 18g2 and to Luni on tz June 1gi4. |ミ Jodhpur was connected to the district via Luni in 1gg5 by the Rajputana- Malwa Rairway network は and the first train started on this route on g March 1885. This line later becomes part of the Jodhpur-Bikaner Railway. phulera-Marwar Junction line was converted from Meier. Gauge to [ Broad Gauge in 1995, whire the Ahmedabad-Ajmer rine was converted in 1997. During 1997-99, 72 the km Jalore_Falna route was also surveyed by L the lndian Railway, however, the line has still not been laid. Ц PALI BYAIR L The nearest Domestic Airport is Jodhpur Airport, roughly one Ц and half hours, drive from pali. Jodhpur Airport is well connecied to a spectrum of cities rike Derhi, Mumbai, L and udaipur through Air rndia and Jet Airways. L
PALI BY MITWAYS k pali has its own Railway Station namcd as pali Railway Station L which is connected to the major cities of Rajasthan. rt is rinked with the cities Iike Guwahati, Jaipur, Ц Ajmer, Bangalore, Ranakpur, yeshwantpur, Bikaner, Jodhpur and Mysore. Ц Pali by road- L pali is 5G Km from Luni, 72 Km from Jodhpur, g7 Km from Samdari, j.11 Ц Km from Beawar, 163 Km from Ajmer, 1g5 Km from Udaipur, 294 Km from Jaipur, 322 Km from Bikaner, Ц 355 Km from Kota and is rinked through Rajasthan State Road Transport corporation (RSRTC) and some private L services. trair ヽ ｂ From Time ミ Udaipur Ｐａｌｉ 3 hours ‐８５ k Jodhpur Ｐａｌｉ 6 mins ．７９ 闘 t hour 18 mins ． Aimer ‐６３ ヽ 2 hours 44 mins Beawar Ｐａ‐‐ 「 t hour 57 Jaipur 画 mins ２９４ ヽ 4 hour 33 mins ヽ
L PROFILE OF TⅡ E DISTRICT へ
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し DiSTRiCI suRVEY REPORT(SAND MiNING〕 . ′PALI :蜻 (Under MinistryOf Envlonment Forest&climate Change,NewDettLNotinca● ヽ 。n Date 25-07‐2018)
ヽ S.No Particular Year Unit Statistics じeographica1 11a ヽ tures (A) pcggraphlcal Data
ヽ i)Latitude 24' 45'to 260 7 5; し North 720 48' to 7 40 20, ほ)I On」 tudc ヽ 螂 East 12387 し AdmiisL“ve U」 転 0) ts 2011
i) Sub divisiOns ９
し 一 Tchsils ９ iii)Sub_Tehsil し 8 iVI Pa● Va circlc 357 し V) Panchayat Simitis 10 ¨ し vli)Nagar PJika 1 7 viii) Gram Panchayats ヽ 320 対) Reve{rue villages 1052 し X) ASSCmbly Area 6 MLAs&lMP 2. し Population (A) Sex-wise 2011 Nos し D Malc 1025895 ii) Female 1012638 し 〔B) Rural P望 lat10n 型 1578682 3. ■ 抑 C A Land utilizatiOn 2010_11 Hectare i)TOtal Arca し 1233079 il)Forcst cOvcr 86536 ヽ Cdttrc Land .58485 し … iv) cultivable Barren land 43760 ヽ 4. Forest し (i) Forest 2010-ll Hectare 86536 ヽ 5. Livestock&POultry A し Cattlc 2007 NOs 1)CoWs ヽ 354698 ii) Buffaloes B 315125 ヽ Other livestock i)Goats し 700183 真 6505 し BitChes 41372 … 」 yS
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DlsTRICI SuRVEY REPORT{sAND M:NING)′ PALl ヘ (Und"i Mini"try of Er D"lhi, Notification "r, Date 25{7-2018.)
ヘ … 7 (a) National ヽ Highway 2010-11 Kms 25870 (b)State Higttway 201o_11 Kms 60800 (C)Main Distnct Highway 201o_11 Kms 30000 (d)OtheF distnct&Rural Roads 輸 201o_11 Kms 310202 蹴:結 悧服毀 2010_11 Kms 40855 (o Kacha Road 201o_11 Kms
FLAURA & FLATINA OF THE DISTRICT: The extent of naturar forests in Rajasthan is not onry one of the rowest in the country but also the lowest in terms of proJr.tirity of forest. contrary On the the state is endowed with the rargest chunk of wasterand which is about 2Oo/o of the total wastelands of tn" .ornif. iotal forests area of Rajasthan is 32639 胃 km2 forests, which is g.S4 % of the total geographical state,s Ｒ area. Reserve Forests constitute 3g.16%, protected 53.36% Forests 」 and Unclassified Forests g.4g% Ｒ of the forest area. AcLording to and seth (1968), 」 !ht1n1o-n a, the forests or this aisirict come under tropicalforest. the ヽ 』 』 S.No. Name of Reserved Protected Unc:assified TOta: 卜 District ヽ Forest Forest Forest 卜 1 Pali 81945 14162 251 96358 ヽ し ヽ
い The forests of Rajasthan can be divided into four broad forest types. ヽ 1. Tropical Thorn Forests, 日 2. Tropical Dry Deciduous Forests, ヽ 饉 3. Bamboo-Forests Ｌ 4. Central 「 lndia Sub_tropical hill forests. に ヘ 5. Mixed Miscellaneous Forests Tropical thorn ‐ forests are found in arid and semi-arid ヽ western Rajasthan pari regions of in District. These extend ‘ gradua'y fro, *"rt"rn rndo -park border and ― merge with the dry deciduous mixed ヘ r**irlr the Aravari hirs and the south-eastern prateau' The moin species found in ヽ ii, xna or .orests ore Acocio e u c o p - h t oe o' P ro s o pi s c i n e ra ri o, co ii,, i, a pi t t o, n, ?llll,ii;,liiii i i; ;, ;;;., ヽ "t
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‐ iJuiilrl\ o, IrU l\t .v.,t(r tn ltxli ilt\rflr r t! FIurr|t,ft rirl tvat.-t\ iu( r(cn .iqnitr.;rllr irrtir,.rtccd Jamt-,nrl in .tlltnr\t Jll th{_. h) ,:lirur,, .rrJ Ilmution\ vit . :rll \ lnni. gr n ltr. gtlcl\\c\ ヽ l'\11r,; i,la:.ic:rl ilr(rrr:r .tllr:l\. .tdi..ti.inJ clr. \!hrfh Iiilvr,t( t:o,itlttutr [lqoa p(Ienttil ilqllllerr- J|r (hc rhitriat. Jr(..llt' ttrirj4r i.r;lLrr= ,rlle.jro,, Iltr gr.rrrn,l ..r:,k,1 'lLr. llurrritL.L.I\t1N1io1 ヽ qrrrlirv lrxn \hr,q\ tno\t,,r lllq. (il.t(m.arl(l n{,ithtrt pxtt} ot thc (li\tfl lIr gt hci,U . )irlltit) !r\rurlrl untrr v,uic\ [rgm lr(,51t o(!'tlltcJ hv Frnlrnrl !\.: c. llivillU flurrrih conccnuflioi ヽ (o lrf,IlY uline t.muiol: lrotrl l-10 lts/,jnl (RilntljtD, hr$rc thiro l.l ntEl.. .\t G'(l:,lrr ofl(l \t lnn rd ltill t)cl rr t,locliJ t,r (cltMod: .JajJr :l(Jl{I) ltstot .srurr.rlur lrl.'rl, Ictcr rur, rvrts xnd Lntdi in .lcrrrran tlorLl the rl,Jlct poclctt lrlock, ヽ lic\h drc mrirrl! utr{nul Bithun Xh0i(1, ;Uxn\rr Jrr. in Khuchr blcr[, Bh:rL.ho. ttt Blli, Drsurr R:t,ti in(l trloctr oI rlrc iisrriit ln llIufitd:rtir, Khor\ril. Vlir ヽ 橘?ri? ヽ 口1■ 9■ fお前 飾 , ィギ魚 〓 ヽ ― ― ヽ し , DiSTR:CrSURVEY REPORT{SAND MiNING)′ PALl こ◎〔Under Ministry of Environment,Forest&climate Change,New De!hL NOtttcation Date 25 117‐ 2018) ヽ 2.9 SEISMICITY: As per seismic zoning map of tndia lS 1893 (part_t): 2002, ヽ Figure 3.9, the major part of Rajasthan ries in Zone - [ and western parts of the districts ヽ of Barmer and sirohi as well as northern sections of Alwar district lie in Zone rV, where the maximum intensity courd reach vIr (MSK). し The remaining areas of Barmer and Sirohi districts, as we[ as the districts of Bikaner, ヽ Jaiselmer and sirohi lie in Zone It. The north-eastern districts of Jhunjhunu, Sikar, Bharatpur and the rest of Arwar arso rie in Zone H. The rest し of the state, including the capital, Jaipur, lie in Zone ll, where the maximum し intensity expected would be around MSK Vl, as is evident from the Seismic zone Map of Rajasthan (Figure 1.4) that some portion of district Barmer, ヽ Jalore, Alwar and Bharatpur lie under Zone - lV. し ::.:!,r;i3:i:, jr: , rl::.;- ‐ S. No- seirmir Zone tnrenii(y (M5K) tu.gniruCe Di!rri.r Ⅳいい ‐ !1-i p,l':i rf B;r.r.r iai.hir:r ? ca\1. t:icre し l さ0-`つ 器… … :;,'iair': -qli(i., : ir;: ii:rfj t',raiil.;rC lfi-ei5!i'jr;ai i,i...r .r -.h;' 1 し /鷺 maSe JⅢ !r:r! r.ii! oi Ld;rour, tJ.t.]rlur. Srrc,.tr_ 2 "I・ :rr,-:r. 11:選 i I :! ie.!rt-r_ air;r.._ jhu.rh.r.lu. prrrj or し i [;r 13 pur Cair:t,;:a8,,-rdiL]u,. r,:: n_,... ..,r;a.r r_rir.. し a: ii:i ._-:iu-r a.,r, . ... ■ ● .: ;j ,.- t,.,., ij u 3 :LcI`]● 1■ =| Y rr L-.. . t.!.. t,'.r,.-ii.i. (.rJ.].., :,huij.. し 1:,:4j;:. :!fir. "ra.]:.; Siij,;"r UCr:)lji irit.r,l,,r !.,:r. il,,j i !ri ‐ ‐ し ‐ し ‐ し ヽ ヽ ヽ .― ´ ‐・_― ―‐‐●ヽ ‐ “ ‐ ヽ (%. ヽ -=,"; -ifr, i.. rK;! +; 1i, Es; ,:it,ifq, ヽ -..*q5: (i,--;. ' 27 し ヽ （ ヽ よ 〓 （ 〓 DiSTRiCr SURVEY REPORT{SAND M:N:NG〕 へ PAL: ′ {under Mhistry of Enuronment,Forest&climate change,New De:hL NotttcatiOn Date2J島 ヽ 7‐2018.) （ FIG: 1.4 MAp OF SEISMIC ZONES OF INDIA & RAJASTHAN ヘ III LAND UTITIZATION PATTERN IN THE DISTRI T Ｆ The pre-dominant randuse Ｆ in the district is agricurture rand 607511 ha 148.27%), followed Ｐ by fallow land 204610 ha (t6.25%1, barren and unculturable land 14391g (lL.4lyo), permanent pasture 静 90g62 ha 17.22%1, Forest land 82010 ha (6.51r%1, Ｆ Land under non_agricultural use 582g1 ha (4.63%)' curturabre waste rand Ｆ 45g04 ha (3.63%) and Mining rand 25355 ha (2.07%l 酔 卜 Table : land use pattern of pali district Ｒ Classification Area (Hectares) Percentage(%) Ｌ Forest 82010 651 Land under NonAgriculture Use 58281 463 Ｌ 143918 11436 Ｌ ― 90862 7.22 Ｌ Land under Misce‖ aneous trees and 103 0008 grooves Ｌ tulturable waste land 45804 3.63 ｋ TotJね ‖∞′hnd ~ 204610 1625 Ц Acti:alsOwn area 607511 48_27 Mining Ｌ 25355 2.01 1258454 Ц IV GEOMoRPHoLOGY&soIL TYPES oF TIIE DISTRICr: Ｌ The district has undu!ating plains,scattered hills and a cOntinuOus hil: ｋ range passing across sw― NE of the district. Area may be ca‖ ed sub ヽ mountnaeous.The sOuth eastern and nOrth eastern part is traversed by the Ｌ Arava‖ i ranges which is the most st「 iking physiographic features oF the district The highest peak Of these h‖ !sis abOut lloomts t0 500mts and slope ｋ is from easttO west. The sOi1 0f the district is sandy and water tabie i5 0CCurring at sha‖ ow ヽ ヽ lよ ‖:|1滉11::『:111‖ |[:羊:t』 :よ i:|!!:Ileii:illli計 も駕 l:サ!|[lllよthrough the area.There is nO natural!ake ヽ but theFe are number of big and s: ヽ ミ （ ヽ し DiSTRICT SuRVEY REPOR丁 (SAND MiNING)′ PALl lunder Ministry Of Enuronment,Forest&climate Change′ こり New Delhi,Notincation Date 2507‐ 2018) ‐ ヽ ヽ し じ し １ ０ し ｔ ヽ し ‐ し ‐ し し し し し ヽ ヽ し ヽ し ‐″●‐ ‐´.、 _ハ _● ヽ ヽ ヽ ヽ ‐ ‐ rマ ゃぎ■. ql● ‐ ヽ 甲■F:雨 諭 ′ :喘 爺■マ(ヽ ) ヽ 29 ヽ ヽ ） し DISTR:CrSURVEY REPORT{SAND MINING)′ PALi {under Ministry Of Environment Forest&c:imate Change,New Delhi,Notincation Date 25 07‐ ヽ 2018) ‐ し ヽ し ‐ し Old釣 樹eロ 0「 し Stt C■ ●r“ntion “ じ翼 さ し し し し 屋ヨSWE●ltH¨ Y ‐ 國●●商 .a mpFf 田。ctal,。 1 ‐ ぬt 目鰍I「… Eヨ し 、り 、 `[。 “ 目 襲 ,。 こ,s し 日 ヽ t。りЩ IImL sa= し ■ S‐ L〔 St"I[ ●C,R``螂 s ‐ し し し ヽ し し ヽ ‐ ） _ a. i! _.4__.:,-sq:.: t,,- - .::: q5 ].'! - : ia'{rq, ） 9. ;.i;; --:---.- ,--- -. \ ） 1I!tl! !: i.Y:'.i-r ） ヽ こき 31 」 ヽ 状 ヘ ´ DISTRICT ・ SURVEY REPORT (SAND MINtNG), pAtt ヘ (und", Miniory of Er c", N"* Derhi, Notification Date 2s_{r7_2018.) ヽ ヘ tAL WEALTH 5,lGEOLOGY‐ ヘ ‐ :.).,: Ｆ ,Y- Ｆ rr$ H er nrera enEt Dt3rircr n€SaxricE p rD lr Dtstnlc , illastfillt Ｆ Ｆ Ｆ Ｆ Ｆ い Ｆ Ｄ ト ■≡二F― ―l=:■ _:lF : ‐ ｀｀ ■:■ __ヽ ::‐ ト Ｌ Ｌ Ｌ Ц Ｌ The geOb」 酬brmttOn d the dtiま 葛ξl慕[I籠[FI,~葛 sedirnentary and met sedirnent rocks The Delhi Super Group rocks represented悪蔀再[R[£ by ξ ミ the AinhoArhAjabgarh rrハ n ^´ ´..´ _^^― Group“ occur near ^:―the eastern border Ц schists' phy,ite, marbre and- basic vorcanic. ,t *"";;ilil;:'::;:L:,::I antruded by granites Ｌ rhyolites. The predominant and of which is the "r' g-.r-an Errnpu-ra ite whicn cover the south and southeastern parts of the district. Ц The ,rr"r" rrpl or cranites is exposed south of Pali. town and is generally pink in colour. The n/ll.*rr super Group occurs in the Ｌ northern part of the district and is represented by rimestone, doromite, sandstone and share' Georogicar configuration of pari Ｌ district i, qrit" .orpr"x. rt is comprised of heterogeneous assembrage of different ritho units oi igneous, sedimentary and metamorphic origin. ヽ The oldest & prominent rock exposed along district belongs to Delhi supergroup 「 comprising southern, eastern and north ea-stern ,"rgin ot the metamorphosed ferruginous and massive clastics. ヽ "*l.mmt へ 爺■fttf■′ "'' 5"e s ヽ u日 Ⅲ■ね゛由n円口 32 ヽ ヽ し し ヽ DiSttRICI suRVEY REPORT(sAND MiNING)′ PALI under MI雨 S. ∫ 詢 dttFOヽ me“,Forest&c‖ mate Change,New De生 し しNot,■ca● On Date 25‐07‐ 20181 ） し ヽ Alluvium & wind blown ） ） Sandstone, shale, boulders and chert. Grante(J。 10r type)′ R「 yOnte&pyrOdasucs wLh dykes Of し ） ） Baslc vd∞ 面c nh plllow b"′ mda mt qu誡 ゴぃhJQ ） ¨ !‖ te′ bedded chert し Phyllite, mica schist, nio@ migmatite& gneisses epidiorite, Hornablende ） ） ） PhuladophiOI Hornblends ） schist, amphibolite, pyroxene granulite, ite Suite し 創c“h史 marЫ ′ %ra雨腱h■/amphbdに Ыo■e ） schist′ quartzite′ mica schist and migmatite ） with subordinate chemogenic sediments and associated phases' intrusive and extrusive Rocks of this supergroup have し been further classified in Kumbhalgarh, Siroh i & punagarh Groups. The Delhi's ヽ are succeeded by a sequence of unmetamorphosed comprised sedimentary rocks of sandstone, lim,estone, siltstone, gypsum し beds, This Supergroup is further divided into Jodhpur Group, Bilara eroria Nrgrur. erorp. し The Delhi's are Intruded by granites .na ,.f,yollt.. The predominant Erinpura Granite. is the ヽ 5.2ECONOMIC IMPACT OF MINING し The mining generate wi' direct and indirect emproyment operations during mininS and most of the unskired rabour ヽ wi, be used for mining purposes and they 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 toxic materiar or handring of is invorved. A, the safety measures ） prevent wi, be strictry forowed to occupationar risk during excavation, roading and transportation. This wi, ヽ b":-{frysource of revenue generation for the go-vernment as after getting the し qRE,,F;:rilf, ., ," ヽ ri -".rrm fu{FI' . ffifu-=- ,, eFr=t Ei ヽ 一 : へ ヽ 一 ・ ヘ ｔ DISTRICr SURVEY REPORT{SAND MiNING}′ PALi ヘ try of Enuronment,Forest&c‖ (under Minに mate Change,New De:hi,No面 catiOn Date 2507‐ 2018) ヽ Environment へ clearance; the minor minerar concessioner wilr have to pay the Royalty Price, DMFT and GST which will enhance the revenue of the state and ヽ Central Government. 5.3 Mineral Wealth Pali district is one ofthe few districts of Rajasthan possessing wide variety of both metallic and non-metallic minerals. However ,commercial exploitation for metallic 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 so many years. cement grade limestone of Ras belt has attracted many entrepreneurs for setting up of major cement plants recent discoveries in the district include blockable granite , wolastonite ,scheerite , worframite and indication gold of mineralization. A brief description of each occunence Is given below. Major Mineralsr Base - metals:- occurrences of base metals have been reported in chitar, Nayakhera, Kalabar, Birantiya, Kantaliya, Jaitpura, Bar, Sandarada, Punagarh, Sandela etc. Chittar:- Department of mines & geology has investigated copper deposit near chittar 10 Km from sendra. A wefl deveroped gossan zone extends for about 2 kms stricke length with average width of 1.5 to 2.0 mts .it shows variegated 」 shades of yellow brown ,maroon ,red and vermillion colours . Department has Ｒ proved 0.26 million tones of average 1% copper reserves in this area 」 ヽ Naya Khera :- A "L" shaped gossan body extends for about g00 mts . strike rength ヽ Ｌ with variable width 1to 15 mts. rn derhi super group rocks of near naya khera Ｆ about 18 kms from sendra - drifling was carried out by the department in the year Ｌ 1973-76 and proved .i.8 million Ｆ tones reserves having 2g% sulpher ,0.5% copper and 1.76% zinc. The minerarization mainry Ｌ consist of pyrite with subordinate Ｆ amound of pyrrhotite , chalcopyrite, and sphalerite . the prppect may Ｌ -be worked for sulpher Ｆ and base metals like copper, zinc can be recovered as by prtducts. Biranthiya khurd:- on the basis of geological Ｌ investinggation taken up by G.S.l. Ｆ massive sulphide minerarization hosted by fersic vorcanic Ｌ unit (quartz mica schist ) has been reported Ｆ in this area .A 250 mts. Long rensoid ore zone has been Ｌ established in the north brock having smarr reserves of 44906 tonnes with an Ｆ average grade of 4.6y" cu ,5.!5% pb and 10.6% zn. rn south brock ore bodies are Ｉ small and impersistant ヽ both in stricke and dip. rndications of gord have arso been noticed in north block. Samples have shown 150 to 1000 ppb of au. ヽ Kalabar:- massive and stringer surphide minerarization is found in karabar area. The rock type are assemblage ヽ of differentiated intermediate meta basic ( amphiborites )chrorite scnist, carc granurite etc. ancient mining is evidenced by 「 gold working slags and mine dumps occurring in echelon pattern over ヽ でレ ヽ ζえ宅 i■ 1てや , ミ 「 沐 ヘ 謙甲 (雨 う ― ― ― ―― ――‐、 し ヽ ① し DiSTRiCT suRVEY REPORT isAND MIN:NG〕 PALi underMinistry21EWironment,Foreil&,‖ ′ ヽ 〔 mate change,New DelhL No● ■catbn Date 25‐ 07‐ 20181 し cumulative strike lengths of 335 mts. Test drilling done by G.S.l. Lelow ） oxidized zone has proved the the presence p]rrrhotite chalcopyrite orrii"'l , sphelarite and .besides.n rnd,:1 ,]c_1ifi.rnt "f ） r.tru oingii_a, oornt, se (1_50 ppm Hg (2as-4000 ppm )and eu gttlt pp, ) tr,rr";ir;;;", obtained. 1.25 miilion tonnes reserves of massive sulphide zore having i.irri r^and 0.39% million tonnes of stringer Cu and 0.19 ） surphide ,on. hrring'o-.;; estimated cu and 28% Zn have been between 400_285 M.R_L G.S.t ,, jrrestigation *ra,.riry in this area. 」） sandarada punagarh etc :- sma, occurrences or teai mlneratization near are observed ・ sandarda, punagarh ,bijaji ka guda ） areas . ,in"r"iiration is of disseminated and vein type and shows erratic nature . air born" hasreported ,i^"r"f survey division of G.S.l. indications of base metar ,ir"rJ;;i;;; kantariya area near sojat ） Tuntsten:-occu rrences of scheelite have been reported from Bar-Babra area 」 these.areas have been and explored by G.S.l. ,","rrOi.ri traced mineralization has been し for 10 kms strike rengths in bar area ."d ; k;;;; babra area from 2 to 10 ,width varies mts scheerite mrnerarization in the grade rt.rnr.no*, wide variation in ' exproratorv dri'ing bv G.S.r. h.r pro;ul-;;;rl,"n." down to 5 mtr. of minerarization し lt has average grade of O.2% Wo, also .scheelite mineralization has been reported by department near bar,runora ヽ ,-nrna,bera areas . the nana areas have been explored by drilling .nd purrirt"n."'oi-sctreetite up to depth 132 ） mtr. Have been observing. Occurrence of wolframite has been observed by G.S.l. near ） near motiya_pipliya area kurki Minerarization occurs as dissemination in quartz veins at the contact of sewariya granites with mica schist of ‐ Delhi Srp", e ,Jrp. Beryl :- lt is an important source of beryllium metal and arso in atomic finds extensive use ヽ reactors. lt occurs in many pegmatite U"ai* department Raipur tehsil . Recently has arso discovered beryt "f ヽ minerarizati"; ;;; Nador in It occurs Desuri tehsir . as large crystals (15_30 cmi .nO I .on1.in ,pto- 1.3% .rate elernent have し also been discovered during chemical analysis_ ヽ rhe major deposits., pari limestone, "".-#il,[:1H,5'"Hexproited in district are し Clay, quartz-feldspar, dimensional stone"s Gr"",* & marble), masonry stone & rhyolite. Details of ヽ these minerals are as follois:_ Limestone :- limestone is one of the important ,in"rrt, because し cement' of its use in chemicar, meturargicar, industries. pati drstrict has extensive rimestone belonging to Delhi Super Group and ヽ Marwar Super Group of rocks. Cement grade as werr as chemicar grade rimestone are found in the district. Major ヽ deposits rime stone are described below : 譜:|::11°::llelu::11:|:i::S:alillCitta:):1::s穐 :nl:″ FI:‖ extends from kurklin the NE tO tunkra‐ 11」 』ょ1linl mOriya in south_west it Occursin fOrm Of ヽ nnral10r hOぃ ●´ ^__^´ ^J : _ :::高 |・ Iiよ l:[[1 し ,′′]!]:lindSexpOSed inanareaofabOui′ :'i:li!!lili丁 ヽ ,,trHF ,' --rl=):..,:: ir:; \ 」 Ｌ | 一 ― ヘ ヘ ヽ ， DISTRiCT SURVEY REPORT{SAND M:NING〕 ′PALi (under Ministry of Environment, Forest & oimate change, New Derhi, Notification Date 2907-201g.) associated with Marani igneous suite near Kharda, Kharda Ki Dhani, Dharamidhari, Jitra, Jawariya. The important potentiar areas have been investigated by the department and granite prots have been delineated for leasing. 「 Keeping in view the overwhelming response from the entrepreneurs, search ト 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 ト was explored at Bheru ka Bariya near Bar. The marble of this district has veried colours and is figurative ト at praces . regionar scanning for marbre was done in different parts of the district which herped in rocating deposits near Nandana, ト Ramgarh, Hemadai, Bhirda, Barwantgarh, Gurha jaitaran rn Raipur and tehsirs and ト near jedri, sindru,Diyana,Banki,Khiwandi,Siriya ri,Anna, Kantaliya,Vin pura,Sarangwas etc. in ト Bali, Desuri, and kharchi (Marwar Junction ) ｋ Most of the marble deposits pali of district are siliceous in nature . the Ｌ variegated corour is important due to presence of ferruginous contents, thin banda of the district. ｋ Corours is attractive but the presence of irregurar crosery spaced fractures are creating probrem in extracting big brock and accordingry Ｌ marble industries in pari district has been severry affected .Except two,thrle localities i.e Hemardai, Ｌ siriyari, Bhirda, in the most of the areas minirlg is being done for sending the materiars to cement industries. The crystafline rimestone is Ｌ suitable for cement manufacture. Recentry carcsiricate rocks which are hard, compact & occur as shaets have attracted few entrepreneurs for its extraction as Ｌ blocks as marble near viflage Asan and samer in the district . economic exproition Ｌ of such rocks is yet to begain. Rhyolite:- Rhyolite of pari district is mostry reddish brown,grayish brack in corour Ц and is aphantic as well as porphyritic. lt is being worked near Medi Bhaker, Singhari and Ц ,Rohat kharda ki Dhani , where g reases are in oprection. Besides, Rhyolite are punagarh, ,occurrences reported from Manihari, Bamborai, Gura Ц Partap singh, Bhakariwala Gaon etc. in pali tehsil. These can only be utillised as 民 road ballast or for chip making- The minor occurrences of non metallic minerals are as followsr Ц Asbestos :- This mineral mainly finds application in making cement pipes, sheet, Ц fireproof clothing etc. the asbestos deposits in pali diftrict .;; iffi; ;;;; sendra, mala ka guda, chhagri ki bhagal , patariya ,goriya , kanotiya, ramgarh ヽ ,dhanbarli ,ballupura ,ranakpur ,shyampura ,alipura ,elc. rru_rst of the asbestos is 民 termolite 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 new mining leases for asbestos （ are banded as per center government directives because it has been considred hazardous ― minerar for mine & factory workers . the 、 important occurrences are described below:- Dhe: Maiali Ka Cuda:‐ asbestOs occurs th夏 as thin veins with an average extensively prospected ヽ and 130 tonnes ヽ i:`´:!i:ill the area has been 幸 `箭 “ ヽ １ ・＾ DtsTRtcT SURVEY REPORT (SAND MtNtNG), pArl ヽ ⑨(u^d", Mini*ry of E. h"ng", *"* Derhi, Notification Date 25.07_2018.) 」 reserves have been estimated upto depth of L mtr. ） chariya ki bhaga patriya :- asbestos of tremorite . veriety occurs in srip fibers ） veins . the vein are short, irregular and discontinuous . the reserves have been estimated 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 cms thickness. The reserves are 1,15,440 tonnes a few thin criss_cross veins of chrysolite 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,Kapil ki 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 and karanpura 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 at number 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 very low carbon ） content (6-8%) Gypsum:- it has been worked in part near khutani villages. Gypsum occurs in し about 1 sq'km area with an average thickness of about r mtr. rt has been worked earlier by RSMM ） and few private mines owner. Magnesite :-the minerar is carbonate of magnesium occurring as hard white Ｌ earthy lumps in urtrabasic rock. When free from sirica & iron it is highry varued for it's refractory properties. g し small Magnesite occurrences are found near Koyalvav , Bhimana ,talao ki bhagel ,Charria ,bhilan ,phulad ,Siriyari . it occurs as thin veins ヽ & stringers in ultrabasic rocks like peridotites , pyroximate etc. A.few small occurrences 」 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 workabre Ｌ deposits has been established. Barytes:- small occurrences of barites are found in punagarh hiI in the forrn of ） small veins. lt has off white to cream colour and grade is also low. Barytes have ヽ also been reported from Biranthia khurd by G.s.l. it overlies the lenses of massive sulphides along the contect of quartz-mica schist having 」 intermittentry exposed outcrops of about 280 mts. strike lengts and 1to 3 mL. Thickness it is of low し grade. Soap Stone:- small occurrences of soapstone ヽ are reported from kanuja,halwat ,shyampu-ra ,khormar ,manpura ,kotri ,nandana ,kanoiiya ,asan etc, these are six し ,{Pt 」 輛"6r__;;」 ・ 薔 i. - ヽ ハ へ D:SttRICT SuRVEY REPORT〔 ・ SAND M:N:NG)′ PALi ヽ (rna"r r,n*t ot rnr Delhi, "rr", ""* otificatlon Date 25.ro7_201g.) ヽ へ mining leases of shop stone in the district. Red ocher/ Red oxide :- it is observed near botha ki dhani in Raipur tehsir where （ it was being exploited by private parties . red oxide and clays.r. ilro being founJ around jaitpura and shyampura and have also been worked in past. |~~ヽ 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 of asbestos. Good quarities of wofiastonite are found in berka pahar ,kheravparra areas of sirohi and Udaipur districts. These arso extend in pari district. rt is being worked by M/s wolkern lndia pw.ltd. it is associated with calcite. Both the mineral are being mined out. Recentry department has rocated row grade wo[astonite arong the border of Ajmer and Pali districts. woilastonite bearing skarns containing 20% woilastonite along with epidote, garnet, quartz, calcite occur as detached bodies. These extend from pisangam-gola in ajmer district to alipura ,rawaniy;.,;.r;;;; ,gopalpura, karanpura, sodpura, ramawas etc. for more than g0 kms strike length beneficiation studies conducted by rBM raboratory,ajmer have indicated encouraging resurts. Driling conducted in three area of pari district namery Rawaniyo , Rampura ,soupura and Gopalpura has proved 79596 metric tonnes Wollastonite. of 』 sand(8ajri) ｋ The district consists polycyclic ｉ of a sequence of large alluvial fans comprising clastic materiar' Consequentry, Ｆ considerabre raterar and verticar variations are witnessed in size and shape ヽ of clastics and sand grains depending upon the provenance and size and shape Ｉ of clastics and sand grains depending upon the provenance and size of the Ｆ river. The newer alluvium is restricted io river channels. Texture is medium ヽ to coarse grain. Minerals mostly constituted of quartz and ferdspar minerar with 卜 rit e micaceous minerarsand heavies, it contains very little amount of clayey ヽ minerals. The sand (Bajri) was extensively qr"r.i"J 」 from Rover Masi, Dhund etc. ヽ 」 Ｆ 5.4 OVER VIEW Of MIIYING ACTIVITY IN THE DISTRICT Щ Pari district is one ofthe few districts of Rajasthanlossessing wide variety of both Ｌ metallic and non-metaric minerars. However, commerciar exproitation for Ｆ metallic mineral has given encouraging results. ヽ Among non-metallic minerals, limestone, magnesite, calcite, quartz, felsper, china cray, ba, cray asbestos etc. are the mineraiwhich へ being exproited'attracted for rast so many years. Cement grade limestone of Ras belt has ;;;; ヽ entrepreneurs for setting up of major cement plants recent discoveries in the district include blockable granite, ヽ wollastoniie, scheelite, wolframite and indication of gold mineralization. ヘ ヘ ヘ ヽ Ｌ し ） - DrsTRtcT suRVEy REPORT (SAND MtNtNG), pAtr し 呻(Under Mininry of En limate Chante, New Delhi, Notification Date 2S{r7_2O18.} ヽ The mining activity in the district is administrated by twO mining engineer し offices viz Mining Engineer― SOlat under the cOntrO1 0f supenntending Mining Engineer― Jodhpur circle and AdditiOnai Director― ヽ Mines′ Jodhpur zOne and Mining Engineer Beawar(Raipur tehsiり under the contド Ol oF Superintending Mining ） Engineer― 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 Employment in Pali district SOiat&Raipur office){Year 2016‐ 18 し S no Mineral Leases Area Production Sale Revenue Employment ） Value (Hectare) (Tons) (Lac Rs.) (Lac Rs.) (Nos.) 1 Limestone ） 6 2576 81213501 Leases 974562 750 (cement ） holder Grade) own ） Cement plant ） 2 Megnesite 1 4 Nil N‖ N‖ N‖ 3 Wollestonite 3 3487 Ｃ 」 N‖ Nil 099 Ｊ Total 10 261487 81213501 97457・ 19 765 ） Table ―No. Of Minor Mineral Leases with Area, Production, Sale Value, Revenue and ） in Pa!i distr:ct Office) (Year 20t6-18 S no Mineral Leases Area Production Sale Value Revenue Employmen 」 t (Hecta re ) (Tons) し (tac Rs.) (Lac Rs.) (Nos) 1 Limestone 46 3072 7670760 400-500 545692 750 ヽ ｎ Ｃ ０ Granite 21696 フ 1365702 150■3000 20825 Ｊ ２ ０ Ｌ¨ 3 Mesonary 201 ツ し 22355 1550 stone 4031576 220-260 し 4 Rahylite 28 3735 118128 Ｅ 200-250 805 Ｊ 200 Quartz 13 112 250-300 ヽ 458 220 Feldspar 79948 6 Chaina 」 25 551 350500 1838 500 clay/Ballclay 3092340 」 7 Marbie 1 1 Nil Nil ４ ■ Ｅ Nll Nil Total ι ● Ｌ 419531 16358454 1173922 4170 ヽ Table‐ No.of Minor Mineral production, Leases with Area, Sale Value, Revenue 」 Ｌ , ¨ ヽ こ ヘ ヽ D:STR:Cr SURVEY REPORT{SAND M:NING),PAL: ヽ (under Minifiy of Environment, Forest & climate change, New oelhi, Notiflcatlon Date 25-07-2018.) ヘ 4 Udesikuwa/ ヘ 2019100005061 Sttat/ KHUSHAVIR SiNGH 3997 ヽ pali ヽ 5 Hirankhuri/ ヘ 2019100005279 rani/ SAIJAN SINGH 186 ヘ pali 6 Dhundali/ 20191CXICD5421 rohat/ SHOBHARAM pali 7 Lototi/ 2019100003940 jaitaran/ Duda ram 24055 pa!i へ ¨ヘ Details of Revenue and production from sand/ Bajari received in rast five ヘ YEAR Production Revenue from bajri/sand (in tonnes) (Rs in Lacs) Ｌ 卜 2013-20■ 4 2441999 1410441 → Ｌ Ｉ 2014-2015 2179920 1738972 Ｆ ｋ 2015‐ 2016 2511005 2121145 卜 Ｆ Ｌ 2016-2017 2418343 21637.8 Ｌ ヽ レ ， ¨ 2017‐ 18 2096160 19663116.46 へ 2018-19 （ N‖ Nil （ CHAPTER V: ＾ 6 RIVER OR STREAM AND OTH[R SAND SOURCES （ ・ construction materia:s へ 争 イ LT,d gravei are one Of the most important （ 111:11と 赫 44 （ 爺叩 価研う ・ へ ｒ ぶt DiSTRiCr SuRVEY REPORT{SAND MIN:NG〕 ′PALl 、 under Minttry of Environment,Forest a climate alange,New DeihL NOtttatbn Date 2● 〔 720181 へ lnternal drainage in ocurring Ｆ south eastern and north eastern part formed by seasonal nala coming out from rocar hifly region. The deposition of sand/Bajri in nara い ocuurs locally during rainy season. い (6) Marwar ln Marwar Panchayat い samiti area is having Bandi, sukri Khari and Mithri river tributries. lnternar drainage in ocurring south eastern and north eastern part formed い by seasonal nala coming out from rocar hiily region. The deposition of sand/Bajri in ト nala ocuurs locally during rainy season. (7) Rohat ト ln Rohat Panchayat samiti area is having Bandi, Guriya, Rediya, sukri and phupharia ト river tributries. rnternar drainage in ocurring south eastern and north eastern part formed by seasonal nara Ｌ coming out from rocar hifly region. The deposition of sand/Bajri in nala ocuurs locally during rainy season. Ｌ (8) Sojat Ｌ ln sojat Panchayat samiti area is having Gurhiya, Rediya, sukri and phuawariya river tributries. lnternal drainage rn ocurring south eastern and north eastern part formed Ｌ by seasonal nala coming out from rocar hi[y region. The deposition of sand/Bajri in Ｌ nala ocuurs locally during rainy season. (9) Sumerpur Ｌ ln sumerpure Panchayat Samiti area is having sukri, Mithri and Jawal river tributries. Ｌ lnternal drainage in ocurring south eastern and north eastern part formed by seasonal nara coming out rocar from hily region. The deposition of sand/Bijri in nara Ｌ ocuurs locally during rainy season. Ｌ Drainage system with description of main rivers Ｌ The district has a poor drainage Ц system which too is internar. pari district fa[s in the Luni & Barmer Basins. Major River of the district is Luni, which flows in ENE _ ｋ wsw direction. rt enters pari district near viflage Ras in Raipur tehsir and reaves the district Eari near vilage Ｌ Amli. channer pattern of Luni is dendritic to sub-paraIer. However, in major part of the district, the drainage is essentially ephemeral and Ｌ internal' Tributaries to the Luni river are sukri, Lirri, Jawar, Bandi. other streams in the district Ｌ are Guhiya, Mithari, Kherwa and Khari which are all ephemeral. Ｌ S.No. Name of the River Area drained %Area dralned in the Ｌ lSq.Km) Distnct 1 Raipur Luni 20.44 0165 2 Sukri Nadi‐ | （ 1725 0.139 3 Lilari Nadi 450 0039 ヽ 4 Gudiya 4.80 一ｂ 0038 Bandi ヘ 21 0_169 6 Sukri― ll 645 0_520 （ ノ ， （ ′ ヽ ― 一 一 ‐｀ ） ヽ D:STR:(I suRVEY REPORT{SAND MIN:NG}′ PALl Under Ministry of Env"onment,Forest&c‖ 〔 mate Change,NewDettι No■ ,ca● ●n Date 2507‐ 2018) ） ヽ DescriptiOn ofimpOrtant rivers is as under:_ ‐ い〕Lu面 Rang[:i:IC[|(1:ll。 lr暮 l]::itn:::11Fil」 Itl』51lSII:rll:el。 :;‖ l western of Ralasthan,■ ll｀::Ii‖ ） disappears in the marshy!and OfRann Of Kutch The total catchment area of the Luni River 8asin in Ralasthan is 37,363 km2,coverlng parts of ） thiliStricFil富 Nagaur,Barmer′ Ja10re and Gularat in Ralasthan ∬ill:l‖:dhpur′ (b}Guhiva ） i窯 m:n.rIIttFT訥 「 」 鵠1器匙‖誌願引l戦犠 I思 3,835 km2,which is situated in Pali district lts tributaries are Raipur Luni′ 躍1距 Radia Nadi′ and Phunpha"a Baぬ ） lclKh」 riHel露attL Suk‖ River Khari is fOrmed by the cOnfluence of sma‖ streams namei' sOnnesar ） けu面 計sOmew酬 囃腱 ） all:i志… … ISm耀訛榔l蹂!讐鷺 II:::淋 iミ:liil:‖ :i::lilir Reserved Forest Bhakar′ し :la‖ after flow Of abOut 30 km)After joining Of a‖ these smali streams,the nver is called Kha‖ AFter lowing fOr about 25 km′ lt,Oins Bandi River downstream of Hemawas reservOir tts catchment 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′ ヽ 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 ） し ヽ 上J膿11囃灘 聾漁詭塾輔曲riS l,644 km2 ヽ uk‖ 「ド Sukri river is fOrmed by the conf!uence of several sma‖ Ｌ nalas _ Ghanerav NadL ′ ng tt° m meAmv訓 ） もh Ptt and udJpur M‖翼]ド f甜 1‖ :ょ ポ請札ど1:点l― west directiOns for abOut llo km and feeds Bankli Dam on the wav NearSamdanin 3armer Dlstnct,it iOins Luni“ ヽ ver The Ja10re′ Pali and Barmer Districts are cOvered in this sub_3asin lts catchment area ヽ 嶋 」 Ψ給 ‐ 芹 ヽ :静 ‥ ン _ ー 壕 ト DiSttR:CI SURVEY REPORT{SAND MINING)′ PAL: (Under Minlstry of En imate Chante, New Delhi, Noflflcatlon Date 25-07-2OtE.) (g)Jawai Jawai river originate in Udaipur district with its main tributary sukri in the western slopes of the joins Aravalris. rt 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 is 2,976 km'z. Report （ 」Ｌ こ Ｌ 」 卜 ‐ （ ヽ ・ ゛< （ ヘ へ ´ ヘ 滞 ｋ Ｌ 式 Ｌ Ｌ 纂 Ｌ ゞ いい uNO uSE Ｌ ）、 PS Ш ｌ ヽ ●sTRrr ecl,NEVUW ） PmAYAr mlll∞ いい ヽ」 CATE60meS PcR CEW や IEeCO Шェ旺 一 00い “ 一 Ct■TⅣA¬ m tAN0 450 100n― ED mGE旺 い □ FOneST さい¨MIEmED Ю 〕 日 υ中。 196 l¨ 鵬¨ 崚 PASuCい o lυ 107AL GECRA― 一 ― 一NON ARハ ヨにε鰤 166 0TIERS s6 榊P雀1サr i 鳴紫F, ヽ 品鷺lil丼 炉 52 へ ‥ ヽ へ （ へ DISTRICT SuRVEY REPORT{SAND MINING)′ J、 _ PAL: ヽ {under Ministry of Environment Forest&aimate change,New De:hL Notncatton Date 25 07‐ 2018.) ヘ ヘ 三 ― ‥ ― ― ‥ ‥ ‥ ― い， ― ‥ ヘ ‥ ― Ｓ ― ‥ ― ― ¨ リ を リ 費 コ コ 菫: ８ ６ ２ Ｈ ６ 箋 彙 ８ ２ ● こ ヨ ， ヽ ｎ 讐言 を ０ 艶 壼 Ｅ Ｗ り ， ２ 縁 〓 ‘ ● ● Ｐ ８ “』 ８¨ ● ≦ 肇 ● な ≦ ８ ６ ス 礫 こ り ス あ χ ご 〓 ｇ） 】 萎 ● ２ ■ ρ ー 一 詢 ー ー 一 ー Ｌ ー 一 Ｉ く ・ ● ﹈ も Ｃ ０ ９ ‘ り Ｄ 聖 』 ■ ヽ く マ ５ 一 ¨ Ｌ 」 ｒ 築 ■ 〕 〇 ０ 一 く ■ ０ ６ こ ト 雛 一 く 〓 コ一 く Ｏ 」 ‥ ｕ ・ コ一 「 工 卜一 く ” ∽ 一 ａ １ 〓 Ｉ ∝ ・ く 卜 ＝ Ш ∽ ０ υ 卜 卜 ２ ｌ く ‘ 「 ＞ 卜 ■ を く ∽ １ ´ 一 一〇 ■ ０ ０ ・ 〓 ∝ く ０ 一 ミ一 ０ ０ ２ そ ５ ０ ｏ 目 〓 そ こ 雪 目 口 言 口 【 ， ヨ 臣 ∽ 」 ロ 一 く ‘ ヨ Ｅ 〓 」 ロ Ｅ ３ ｏ２ エ ロ ３ ２ ２ ０」 卜 １ ロ 日 口 一“ ヽ ロ ■ 一 日 ロ Ｒ Ｆ ヨ Ｒ ｒ 日 」 だ 電 」ヘ 轟膊 ′ ‐ 勧輛 口:・ ●■R師 ′ ヘ →雫 (") （ liヽ へ へ ヽ 56 ヽ ‐ ―ヽ じ し DiSTR:CT SURVEY REPORT{SAND MiNING)′ PALi (under Ministry t⑩ of Environment, Forest & climate change, New Delhi, Notification Date 2s-o7-2018.) ヽ し ヽ ， ０ 〓 」 雪: 一 ” ■ ， コ 0贅 ロ ｃ ｏ ‘ ¨ 山 ツ ， 一 5= ¨ご ” コ に Ｃ 叫 く ヽ 一 ｉ Ｌ い し Ｃ い 」 ● 〕 三 ヽ ， ¨ 』 ， 〓 二 ゛ で ボ ¨ ｃ こ ０ 」 ０ 」 ■ ０ ′ ） 0‐ ロ 一 Ｅ 日 一 一 一 一 一 １ ｒ １ 2 ロ 日 一 一 １ （ 一 ロ １ ¨ ― １ り り ● ´ ‥ こヽ 一 ＾ １ ｒ ● ´ ３ く ） １ ● υ ¨ Ｉ ■ ＝ ″ ， ■ 】 ） 一 ｒ ● ｐ ０ κ ′ α ﹈ ２ コ ＾ ・． コ ゝ ‘ “ 一 て く ヒ Ｏ ａ ， ” ヽ ０ ｖ り ０ じ ６ 二 〕 ｝ 〕 工 ） ‘ ゆ 一 ι Ｚ こ ” γ ′ ” ´ う イ 一 コ 〓 ０ Ｗ ｚ Ｌ ‥ Ｊ ず イ ● ´ 市 ∝ ● κ ● こ ４ ０ 」 Ｌ り 【 コ ¨ ケ ■ Ｒ ■ ０ ” ６ に の ″ ‘ ２ 々 一 ¨， ■ メ ´ ” ） 二 ０ リ ‘ ０ 一 ヽ ン ヨ ０ ０ ０ ９ ， ０ ０ 一 コ ピ Λ ６ こ マコ イ ■ “ 』 〓 “ ０ ６ ０ ９ Ｏ 一 臣 ， ‘ ９ ‘ ¨０ こ ｒ ， ニ ） α ∽ ０ ¨ ´ ＾ 】 ） ） ） ミl ドヾl, ） ■ Ｌ トミ く ¨ ミ ） 〓 ｒ 〓 Ｏ く ｕ 〓 一 〓 一 一 Ｆ く ） ∽ 〓 こ Ｌ ´ く 【 ｕ ０ ０ 卜 一 卜 α ） く く 卜 ヽ ヽ ０ ゝ く 〇一 ０ 〓 ‥ ０ ） ∝ ２ こ ０ く ， 一 ヽ Ｅ 」 ！ ． ″ ・ ） 一４ 一 ・い ） ， Z・ ‐ ト く 〓 く ヽ ） 、 し ヽ し ヽ ∠ ヽ ´ し ■:タ ヽ れ、ど職rT, ） 口H■ ■餞嗣斜呵′ 爺 マ 喝 (マ 詞.) ） 」 ・ 」 へ ヽ ・＾ へ ´ ヽ DiSTRICT SURVEY REPORT{SAND MiNING)′ PAL: （ ・ (Under MinisEy of Environment, Forest & Oimate Change, New Delhi, Notificatlm Date 25.(t7-2018,) ヽ ヽ ■ ■ ０ ９ ０ ８ 一 一 ¨ ０ ヘ 一 ０ Ｏ い ２ ζ ≦ 〇 ― 〇 ２ 讐 ０ ５２ コ‘ を０ ｕ 霞 へ 一 ｒ に の ‘ ３ Ｄ Ш 妻 Ｌ ビ 一 ２ 工 ３ ８ ａ ９ Ｆ 一く Ｏ ユ ■一 〔 一 ■ ■ Ｌ く Ｈ 口 ■ 一 ― ■ 日 一 ■ ● 〓 Ｚ 「 一 く ０ ピ ＝ ユ 日 Ｌ ロ 一 １ エ ト ヨ 〓一 く 一 ∽ ユ ＝ “ く ・ の 卜 ｕ ロ ０ ｌ ｋ 卜 一 ト く Ｅ ｌ く， 卜 「 〓 く ０ ＝ 工 〇一 ｕ Ｏ Ｏ ｌ ｋ Ｚ Ｊ Ｌ ‘ Ｏ ユ 〓一 ｋ Ｌ 抵 ｋ Ｌ Ｌ Ｌ Ｌ ｋ ‐ ゴ ― ‥ ぬ “ Ｌ ‥ ν 風 ― ‐ ” ｚ 讐 Ｌ コ コ 目 リ Ш ８ ％ 』 屁 監 お Ｌ ｎ 暇 ヌ 要 “ だ 臨 曜 畔 鋼 ｋ 〓 要 一 ９ 醍 館 ０ 壁 聟 ミ ３ 一 ヽ Ц ヽ 儡 ヽ 爺 マ(雨・) 嘔 ヽ ヽ ヘ 58 ミ ヽ し ヽ D:STRICI suRVEY REPORTiSAND MiNING〕 ′PALi (暑2) (under Min、 try of Environment,Forest&c:imate change,New De:hi,Notncauon Date 25‐ こ 07‐2013.) し ヽ ヽ ） ::=:=ミ ） こ ヨヨ ２ ， く 一 ＾ 藝 ∽ こ 〓 ） 三 r 聖 〕 ヽ Ｌ 【 一 Ｏ く 』 Ｃ ゝ ¢ 一 ¨一 〕 卜 コ 」 く ３ ０ ） ０ ０ 」 幣 口 一 口 ロ ‐ ‐ ヽ ロ Ｕ ） ・一一 中 し 一ヽ■ 「す ¨一 式 ，ｒ 一 ） ャ）・ 」 ヽ :… ・ 】 I ） ） 」 ） ） ） ‐ Ｌ ′ く 卜 じ ― Ｅ く ７ １ ） 「 Ｏ ０ ∽ Ш コ一 工 く ０ 卜一 κ 日 ） の 一 望 Ｅ一 ・ ∝ し ロ く 卜 由 ト ０ ０ ヽ ‘一 ９ 」 く 卜 硼 ０ く ” 〓 ヽ め Zく こ く 一 ０ 工 〇 督 ‥ ０ ヽ “ ２ ― ０ く ― 」 ・ ， 〓一 ― ） ９ 人 ′ 」 ヽ ヽ ．ｏ 」 ぼ ヽ ヽ ′ 」 ） 歳 ト舅」 Fヽ市, 」 、ビ uH哺 キで調 ｀ . ） ヨ →琴 (ヽ「 う 膏 ） 」 59 し ヽ ヽ¨ Ｏ DiSTRiCT SURVEY REPORT(sAND MINING),PALl , ｋ い {undor Minlstw Of Envttonment,Forest 8t c‖ mate Change,New DethL Notrlca“ ｌ 。n Date 25‐ t17-2018) 6 3 SALIENT FEATURES OFIMPoRTANT RIVERS AND STREAMS Ｌ ム Salient Features Ofimportant Riv nt Rtvers and S trearns Ｌ S.No. Name of the River Total Length Place of origin Altitude at Origin Ｌ or Stream in the District (in Km) Ｌ 1 Bandi 12495 Bhupat Ka Gurha 460 2 Cuiriya 1221 Ｌ ３ Singpura 334 一 Rediya 3228 ４ Lonera 224 Ｌ Sukri 21938 Giri 339 5 Phtlnphariya 3419 Ｌ Surayata 236 6 10755 ν Ｌ Sumel ヽ ” ａ 395 Ｌ 7 3560 ８ Perva 302 Somesar 5707 Ц ９ Somesar 500 Khardi 2603 Khariya Swaniva 269 10 Mlh● 7457 ｋ ■ Motagura ■ 370 Khot Ki Nadi 2544 420 Ц 12 Magai 2996 Jaton ki Doran 370 13 iawali 5156 … ｋ Khaubban ka Gura 376 14 Raipur Luni 5516 Lalvacha 378 ｋ 15 Tatawari 1112 Mahaveer ji temple 434 n ear Kundai ｋ 16 Jawai 4972 Dharcial 411 17 7552 ｋ Oariyara 235 Ц 6.4Availab‖ity Of sand Or grave:or aggregate resources in Pali:_ ｋ This has already been briefed in the preceeding paras The resOurces are on the ｋ banks Of Luni river are sukri′ Lilri′ JawaI′ Bandi other streams in the distri(■ are Ц Guhiya′ MitharL Kherwa alld Khari etc ｋ ｋ ｋ ム ム ヘ 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 NABL TC1 5788 RepOrt No.:RKC/2019・ 20/130 Date:20.05.2019 TEST REpORT Shd3ogttnghSrOShHG● e Sltth NaDe & Address of Customer 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 : 25■ 2●C & Rdaive Humtdltv,96 : 4896 Ｓ ． LOCAT10N UNr SPL Leq Ｎ 。 Ｎ 山 Day Time Ｔ 血 1 Mineま te dB(A〕 64.3 33.6 Ｎ ¨ ■ Day Tlme(600● m.to 10.00P.m.)`Nightttme〔 1000p.m to600a m) ２ dence:nthecomoFL喘 ■ Th"reporttnottobereproducedwhOllyorinpartandcannotbcusedaseЙ SubleCttO'Odhpurrurlsdldon o■ , PaBe 1 of 1