Ground Water Prospects
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L E G E N D GROUND WATER PROSPECTS MAP GEOMORPHIC DEPTH TO RECHARGE G R O U N D W A T E R P R O S P E C T S RECHARGE MAP UNIT GEOLOGICAL SEQUENCE / STRUCTURES ( PREPARED FROM SATELLITE IMAGE INTERPRETATION WITH LIMITED FIELD CHECKS ) ROCK TYPE UNIT / LANDFORM WATER LEVEL CONDITIONS ( HYDROGEOMORPHIC SUITABLE & UNIT ) AQUIFER MATERIAL TYPE OF WELLS DEPTH RANGE YIELD RANGE HOMOGENEITY QUALITY OF GROUND PRIORITY REPRESENTED IN SUITABLE OF WELLS IN THE UNIT WATER BASED ON OF WELLS WATER PT = PERCOLATION TANK THE MAP WITH PRE / POST- MONSOON AVAILABILITY ( SUGGESTED ) & SUCCESS IRRIGATED CD = CHECK DAM R E M A R K S ALPHANUMERIC CODE ( EXPECTED ) POTABLE (P) (AVERAGE IN METERS) RATE OF WELLS NON - POTABLE (NP) NB = NALA BUND OF WATER LS AREA ( PROBLEMS / LIMITATIONS ) = LOOSE SEDIMENTS DW = DUG WELL 3 RW = RECHARGE WELL MIN - MAX ( PROBABILITY ) ( REPRESENTED IN ( REPRESENTED IN PR = PERMEABLE ROCK = RING WELL ( in LPM or m / day) DT = DESILTING OF TANK RW ( INDICATE REASONS IF THE MAP WITH FIR = FISSURED ROCK BW = BORE WELL ( APPROX . RANGE RP = RECHARGE PIT ( COLOUR INDICATES THE MAP WITH NO. OF WELLS ( RAINFALL & OTHER ( IN METERS ) NON POTABLE ) FR = FRACTURED ROCK = TUBE WELL VERY HIGH IN PERCENTAGE ) SD = SUBSURFACE DYKE Kilometers YIELD RANGE AND NUMERIC CODE ) ALPHABETIC CODE ) OBSERVED TW SOURCES ) WR /= WEATHERED ROCK / HIGH HATCHING INDICATE DBW / = DUG CUM-BORE WELL / RS = RECHARGE SHAFT WM WEATHERED MATERIAL DUG CUM-TUBE WELL MODERATE ST = STORAGE TANK DEPTH RANGE) DTW 0 1 2 3 4 5 IR = IMPERIVIOUS ROCK LOW SCM = SOIL CONSERVATION MEASURES s © t i s SCALE - 1 : 50,000 o p e Groundwater prospects very high Channel Bar D 5-10 m 400-500 LPM Very High Not Required MAP SHEET NO. 73N/9 BANKURA, BARDDHAMAN, HUGLI & PASCHIM MEDINIPUR DISTRICTS, WEST BENGAL No well observed Excellant LS RW P Nil with high recharge potential. (CB) CB111 y Recharge structures not required. " " " TW Hedua " Ashura!"li 5/13 Koradanga ) a ª Kuntal " Sias Panna 6/120 D d Bazar "Gopalbati "Shyamdas "! w Shindepat " Mamrur D a r t Kamla k B31 "Balitha Chak e APO13 Madhaganj " Belun " s n " Muidhra w " Eklakhi 5/13 Jamadarpara " ! a e " Brahmadanga 8/107 D r " s !" Lego "Ghichagerla ! 16/125 o ª " D" r Kunrre e Banmukho Salikona Chagla D " "Diachapri " r Lego h Shanko Mahaldanga " a " " Boradanga l P " k / "Bhurkunda i ) Panahar Mashidberia s y Tentulmuri " " n " " Hatigeria " ! o ! " r D a D Shamunt "Pundait o Bhurkhunda 10/107 R Nutangram 10/30 i " i Khanda D v Jhinukairi t Alluvium Groundwater prospects very high "Danna e Ismali a r " " Gachh ) t (Sand Dominant) Point Bar 5-10 m " " PB111 No well observed Very Good 300-400 LPM Very High P Nil Not Required with high recharge potential. Dalal Chak Narattambaria " n LS RW " Gotai m Daulat "Koalpara " (PB) e Chak Radhadamodarpur r (111) Recharge structures not required. "Panua " Kotal Kumarganj TW Kharagpur "Riya " " s Chak "Rambagra " o K e a F n Jatadharpur "Ganjua g Asudhkona r " " Baliarpur s Agai " i " Kadipara a " P Sakimchank " b Sahabad ! h " a ( Adrajai t D Pahari Poalgera " i 10/107 t Chhanua 6/9 "Chak B " r a a Parbaopur " ! n r c ª i " " Kanchannagar Khatul " h 10/95 C Malikata g Arjundanga )" Prasadpukur a Gauripur " ! Dhanjora Jamuna " n D " " a a Parbatipur ! l " D "Narahatibati h 5/45 10/105 "Bijolkona Nachur " "Raghunathpur Ramchandrapur B " " " Bhalukgara " ! Chhana Rahim " D / Sulut i Mathurapur Muro l ! " Chak Cut-off Meander RW D " Aswinkota g ) " " CM111 No well observed Very Good 10-15 m 200-300 LPM Not Required D13 "Saluger Katgram LS Very High P Nil Potable water available at shallow " Gopalganj u (CM) TW depth. "Narainpur Senal H "Gopinathpur " "Saljhar Santoshpur Nandagrarh " Chhana "Idalbati " Dhaja Raghunathpur Chak Gopalganj " Narainpur Chela Dakshinbar " " " (! " ! " ( " E Shekati Madhabpur 6/28 "Palpukur E Ramdiha 20/35 ! Damgosa D " "Saijhar " ! ) D "Deshra B " 18/30 D12 a Badeshwar e ! n D Gopinathpur " Siramanipur Nalbunia h n e " " Goreshwarbati o a S " ! i c Dubrajbati Sundarpur H ( t " " "Deshra r o 2 E a l Krishnanagar "Damgasa K m " o h Lalbazar " r " Barul H Alluvial Plain Chandipur Pirit " a o Alluvium e l F " ! ) Metal Chak " D t Younger 10 / 6 Potable water available at shallow " 8/110 (Sand and Silt) Not Required a Puniajol APY113 a " Shaer Tunga " TW 25-30 m 200-300 LPM High P 28.8 Dhajmanipur " " APO13 Raghubati r (APY) Good LS depth. 2/12 " L Nutangram " Bhadur (113) 6 Chorkola ! u " ª Bangal o "Dhara Durgabati " (! Bejua k Silakon " " t Sihar s " Patpur " E y 2/10 Tajpur "Durgapur n Ismal " " l a " ! Rajgram r P Brahmankonda Chak Lankajol ª Anur 10/115 a " " " " Suliandihi Kumkumi "Pratappur " ! E D "Sitanagar Gobrager "8/125 "Dhanghari " 6/20 8/107 Kalia "Bhelaighata !Madhopur " ! "Belpara ! D ª" 11/65 D" 8/80 Kamarpur 5/12 ! Madina ) "Bankoti D e ! n D Amlasol ! "Jayra Bankati Jheterbardi ª e " " " "Kopshil " " c Lankardihi Ganeshbati n " o Balarampur l o i Jaykilshnapur o " t H Alluvial Plain Randanga Indara "Salingcha 8/107 a RW " r Alluvium Kamarbazar " ! 11 / 6 Moderate to " E Moderate groundwater potential Shunda D m Older 150-200 LPM P Harisabha " " APO13 - (Sand,Silt & Clay) Moderate to Good LS 40-60 m 71.1 Moderate to Low " r Gobindapur e (APO) 70 TW High at intermediate depths. o n (13) "Musenapur Amarpur e " (! 6/98 F Betra " Chargere Pukur 9/107 c "Kantapukur " " E o ! ! a D t D" " Tilari u " s i Golpur Ratanpur j Jibta i "Balibhadrapur " Dasghara e Udaypur l Pukuria " " Fulai " S " P 8/165 t Kantapukur L D! Kokun " ( Tangra " " Charulpata " 10/107 "Badanganj Narainpur Penkale " ! Bhawadighi " Kayapat D" " 8/65 " Kamarpukur "Deraipur LP211 ! " Daurlpara (! D " E "Majdiha Katoli "Khanat Khanat 7/107 " Shyampur 8/107 ! Balarampur" Areas of exposed lithomarge clay. " ! " Shyambazar Satberia DKatali "Nabashona n D " 8/107 " ! Lateritic Plain 11 / 7 Fracture zones form the aquifer, Teurmuri Mahmudpur D!8/65 LP211 o 50-60 m 50-100 LPM Moderate P Nil RW i " " ! D ) Limited WM+FR TW Chakran 7/65 Ba"ladwip 6/107 Madhubati " D" t recharge structures will enhance Beldiha " e (LP) High "Nishchintapur ! ! 9/90 3 a D D n " Sahyid Brahmangram "Goohat groundwater development. " e Tiloti Meharbanpur m Kadra " " "Krishnaganj Chak " c " r 8/13 Chamar Khushiganj 7/107 " o o " ! t ! D Sheoragere " Shaluka ! " s Chak Lalpur F ª 8/55 D" Maheshpur Maodaran i " " 8/107 Bhickdash "Lodra Laterite (Ferricrete- " e ! r "Kadra Ramnagar D l 10/107 a Hard crust, lateritic Amgacha P ! " Adua Pandugram " z D Gudar " " r nodules & lithomerge "Khejurbandhi "Muluk a Chak e b p clay) "Karnapur 7/107 Lagapukur p " ! m (211) U D a Lashkarpukur "Tarahat Methal " l Dharampur l " Sukhanjona o Essentially run-off zone where hard Chak " I " Betbuni Kamcha " t "Barasol 6/107 " Dumura / "Jadabbati Bagalpur " Uluspur capping is present.Areas of " " e h ! l 8/65 r D " "Sushanigeria d nodularlaterites are recharge zones with ! " Chandalpara a Dissected Lateritic D Bhalukgare " Jodhbansi d WM+IR 30-50 LPM i 80-100 m DLU211 g No well observed TW Low P Nil Not Required deep water table conditions. Primarily E4 l Poor to Limited "Kuchidhari Kajla Upland (Impervious Material) " Naldubi M Selimpur a " 9/107 Rangameta " Chak ( forest areas with sparse settlements. "Sabhagar " (DLU) Bhaunta L " ! 7/134 10/65 Hari " D"Manikbandh K7 Not suitable for large scale ! " Ahmadpur Bhaunta Santlpur D K8 ! " " " D development of groundwater. Hatibari " Jharia " Gurulia Kirtibaspur " " Lakurpal "Baburampur "Bhatkhola "Tetulmuri 9/107 7/107 "Kumairsa Raykhan(indrajitpur) " Bandanga ! Sunia " Sundarpur ! Paschimpara D" " " D" Bhagwanpur Sanbandhi Hat 10/1"4 " " ! Jagannathpur Gopaldanga 7/107 (! F F Kayarganj DLU211 ª " " LP211 Ramnandapur ! E These are fault / fracture zones, which generally act as conduits for movement of ground water in hard rocks. Along these zones, the yields are significantly higher and wells are likely to be sustainable for longer duration. However, the inferred fractures need to be confirmed by detailed ground surveys. " Kamal DSingrapur " "Badia "Chak Kolrakhal "Sandhipur "Anupnagar " "Naroka ! Konkure "Silempur ª "Bishnudaspur " 8/13 Kultala D D Q Q P P Laleganj " " 10/80 Solpur " 8/107 " 8/107 These are dykes, quartz reefs and pegmatite veins, which generally act as barriers for ground water movement. Dwarkhola "Chandpur Ut!tar_saita Daiya Q Q P P " ! Uttar D ! D D "Katrabati D Kanda D "Katapukur " " "Salta Kanpur Dianpur Braja Bhagabantapur " A " Sahebganj m "Mohanpur " " Kanta Paikmalita" u d " N.B.-The depth range and yield range of wells may vary within the unit because of certain inhomogeneities. Fractures/Lineaments which are clearly observed / inferred from the satellite image are indicated on the map. There could be some obscured fractures which also influence the ground water prospects. " Ghola Debkhuna Dakshin e DLU211 " " r Mamrez Kharagsuli Saith Dari Locations of the recharge structures shown in the map are tentative. This map is useful for narrowing down the target zones,and exact location on the ground for wells and recharge structures should be identified based on follow-up ground hydrogeological/geophysical surveys. Sasageria Ghola " N Chak " " "Tehora Nakunda a Idpur Phulbani "Bagchar " d " " 8/107 i " ! Dhanyasara Parulia Bahadurpur 9/42 D" " " " Nakunda " RDa!meshwarpur Malipukur Monaharpur " (! (! APY113 11/40 Pandua" (! LP211 ! Dadpur 11/107 E E D " E 8/105 " Tentulmuri ! Hafizganj Balrampur "D " ! " "Hajipur Gauhati D Banpur Ramjibanpur Dariahat GROUND WATER PROSPECTS INFORMATION STRUCTURAL INFORMATION BASE MAP INFORMATION Thakurhati " Pota HYDROLOGICAL INFORMATION