L E G E N D GROUND WATER PROSPECTS MAP DEPTH TO 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 / GEOMORPHIC RECHARGE STRUCTURES ROCK TYPE UNIT / LANDFORM WATER LEVEL CONDITIONS ( PREPARED FROM SATELLITE IMAGE INTERPRETATION WITH LIMITED FIELD CHECKS ) SUITABLE & ( HYDROGEOMORPHIC BASED ON UNIT ) AVAILABILITY AQUIFER MATERIAL TYPE OF WELLS DEPTH RANGE YIELD RANGE HOMOGENEITY QUALITY OF GROUND PRIORITY REPRESENTED IN OF WATER OF WELLS IN THE UNIT WATER WATER PRE / POST- MONSOON SUITABLE OF WELLS PT = PERCOLATION TANK THE MAP WITH & SUCCESS (AVERAGE IN METERS) ( SUGGESTED ) ( EXPECTED ) POTABLE (P) IRRIGATED CD = CHECK DAM R E M A R K S ALPHANUMERIC CODE RATE OF WELLS NON - POTABLE (NP) AREA NB = NALA BUND ( RAINFALL & OTHER LS ( PROBLEMS / LIMITATIONS ) = LOOSE SEDIMENTS DW = DUG WELL 3 RW = RECHARGE WELL ( REPRESENTED IN SOURCES ) MIN - MAX ( PROBABILITY ) ( REPRESENTED IN PR = PERMEABLE ROCK RW = RING WELL ( in LPM or m / day) DT = DESILTING OF TANK NO. OF WELLS FIR ( INDICATE REASONS IF ( APPROX . RANGE ( COLOUR INDICATES THE MAP WITH THE MAP WITH = FISSURED ROCK BW = BORE WELL NON POTABLE ) RP = RECHARGE PIT OBSERVED FR = FRACTURED ROCK ( IN METERS ) VERY HIGH IN PERCENTAGE ) Kilometers YIELD RANGE AND NUMERIC CODE ) ALPHABETIC CODE ) TW = TUBE WELL SD = SUBSURFACE DYKE HATCHING INDICATE WR / = WEATHERED ROCK / DBW / = DUG CUM-BORE WELL / HIGH RS = RECHARGE SHAFT WM MODERATE DEPTH RANGE) WEATHERED MATERIAL DTW DUG CUM-TUBE WELL ST = STORAGE TANK 0 1 2 3 4 5 © IR = IMPERIVIOUS ROCK LOW SCM = SOIL CONSERVATION MEASURES s RW SCALE - 1 : 50,000 t Groundwater prospects very high i Channel Bar No well observed Excellant TW 5-10 m 400-500 LPM Very High P Not Required s LS Nil CB111 (CB) with high recharge potential. BANKURA, BARDDHAMAN & HUGLI DISTRICTS, WEST BENGAL o Recharge structures not required. MAP SHEET NO. 73M/12 p e " " D " " Mishripukur )" Mirapara PB111 Hamirpur Parulia Panchpara Bhasapur " " y Lakshmipur CB111 3/15 APY113 CB111 CB111 a !" Keshabpur d ) ª Khosalpur " 6/13 Dhagaria " ) !" PB111 y ªMamudpur t a Kumirkhola n Dhamsa B21 Nabagram " " " Dharampur e " D "Muktapur Netkhara Alluvium RW " " Rupsa " s Point Bar Groundwater prospects very high "Baikanthapur PB111 t Jankinagar RI111 "Shyamghat e (Sand Dominant) Very Good TW 5-10 m 300-400 LPM P Naricha n (PB) No well observed LS Very High Nil Not Required with high recharge potential. Sundigaren APY113 Majher r " " e "Salkhara "Bhagabatipur " ) (111) Char Keleti " P Recharge structures not required. " s Gola / 8/13 )" Gharkura e ! n ª Bagpara r " Borolbandhi " o i Gola P " Tildanga t ( "Colony Belut a "Gosaingram )" APY113 m 4/15 Beldanga Dudhopukur !" " r " ª Balarampur Samsor o " Amarpur 12/16 "Bhasna " )Ï" ! Bhetia PC13 F ª Bijpur River Island RW Groundwater prospects very high Andra " i Krishnanagar "1/10 " 5/12 Aradanga RI111 l No well observed Excellant 5-10 m 400-500 LPM Very High " 2/10 ! Sainbuni ! " (RI) LS TW P Nil Not Required with high recharge potential. ª Kantaban " Khejurhati g ! ª " " ! " ª u ( 5/11 Barui Recharge structures not required. Banglardanga ! " "Pathanpara Nischintapur E ª H "Chandni Baburgram " Raghunathpur Metiadanga " " §! )" " Deuli " Ujjalpukur Bansdaha Kajirdanga " Metepara " Bagichaban Khandaghosh ! Khaerbani " " ) § "Kumna Hamirpur " " Kantadighi 8/12 e (! Idli " ! ) n Kaktia ª Palasdanga n " " E e "Chak o i c Bijnathgram t " " (! o Mallikpur a " §! ) Lodna E " l Fakir Kalsar o 10/14 m Rasulpur " " ! r D10 Danga ª H Alluvium Alluvial Plain " o 8/ 4 3/10 e Potable water available at shallow F ! Dakshin t (Sand and Silt) Younger Good LS 25 - 30 m 200-250 LPM High P Nil Sekender a TW Not Required ª a Baganpara Pataspur Naldanga" 10 depth. APY113 r " 5/15 L Chak Katora " ! (113) (APY) " u Lalbandh " ! ª o " ª k Shyamsundarpur t 4/12 "Oari s ! y n ª Ratnapur l " r ! Barsali a § a " P Chak "Patrasaer E ( " Patrasaer Alipur 4/12 "Daspukur (!" ª!" Shyamdanga E §! ª! 9/13 " 6/17 3/14 Danna !" ! Biurªi ª" " Bhutura Gopalnagar Areas of good groundwater potential Ulkunda Natural Levee " 9/ 5 TW High Nabason ! 3/11 Belur " NL13 Good LS 20-30 m 200-250 LPM P Nil Not Required at shallow depth.Recharge good, ª" (NL) Bagdi Konnagar Enayetnagar " 9 " recharge structures not required. (P!ara 5/12 Khantikar E )Ï" LP211 ! ) §! ª e n n 6/12 " e !" o Karajbani Rol c " Baladhadaª " Nawhat i o t l a ! o § 17/40 4/16 Abandoned " H ! )! Birugram m Areas of very high groundwater D ªKumrul r 8/ 6 y Channel ! Bamria Bamnari " Gayespur " l (" " " ) AC13 o RW 250-300 LPM Very High Nil )Ï ! r Very Good LS 10-15 m P Not Required potential at shallow depth.Most Jamsola ( F E a (AC) "Thakurhati " 1 TW t suitable for extraction of groundwater. Dakhin E Madhpur E a Para (! Fatika Dubrajhat o " h 4/13 t " E )! B30 r Alluvium e ª u Krishnabati "Ukria n (Sand,Silt & Clay) " p Patit "! 6/50 e c D m (13) Baharagarh o Chichinga " a t " Dumurtala s " ) R i Paleo-channel RW Areas of very high groundwater / No well observed Paschim e Very Good 10-15 m N il Kule PC13 l LS 200-250 LPM Very High P Not Required ! " a TW potential at shallow depth.Most (Para P (PC) u Maukuchi " " 6/15 j )E e ! ! i suitable for extraction of groundwater. ª ªMaheshpur t " a S "Heyatnagar 10/80 L ! Bayda ( D" Birshimul " Kaina §! Khosbag 14/40 " !" Mirzapur 8/41 D " Deogharia D"! " Hasipukur ! 10/13 ª6/10 Shankhurul !" "Dharabari " Alluvial Plain Older 9/ 4 ªBalsi Singiri (! " APO13 Moderate to Good LS 10 RW Moderate groundwater potential (APO) 80 TW 40-60 m 150-200 LPM Moderate to P E Indas at intermediate depths. !" 4/12 High Moderate to Low Bhaluka ª 10/13 Khatra " ª! " Meral 10/80 Sultanpur " ! NL13 " Tarul Srikara 10/90 D " !" Batania ªD ! 10/40 " Dhuma 6/16 5/13 D " " ! Sripur 10/80 !" Samtari !" " "Banberia Narayanpur ª" ªAusnara Arapur n Moural D " "Daiyar o ) Gopalpur i " Amral e NL13 " t n Areas of exposed lithomarge clay. Balkunthapur Sahaspur a Bhagabanbati " 8/80 e " ! Lateritic Plain 10/ 4 Nil Fracture zones form the aquifer, c RW/ DT Sikdari D Road m " " Sadhanpur Limited WM+FR TW/BW Dhamur r 50-60 m Moderate Belgaria " o (LP) 50-100 LPM P " Sibrambati t 9 High recharge structures will enhance " LP211 "Narangi 4/12 ) " o !" !" s i "Bhubut ªªAmrul F groundwater development. Gangabati Abdulpur Dahuka e Laterite " l r " "Shyampukur P ) a "Kapsit "Tilpur Pan (Ferricrete-Hard Dhopa z r e Pushkarini a crust, lateritic nodules CB111 "Pushkarini " Pratapmath p Monoharpur b " " ) Patan " & lithomarge clay) Belbandhi p Chak-kabir " APO13 " "Punsur Narayanpur m Essentially run-off zone where hard U " (211) ) a Thakuranidighi" Charigram" 4/9 Banki l capping is present. Areas of nodular ! 4/9 o Dakhin " Adilpur Beldanga Berghosh " l " ª) ! t ! " 8/90 I Karardanga Haldi " ªª) laterites are recharge zones with deep Abdulpur" !" ) / Chak Kabir 6/13 "Srirampur D e Dissected Lateritic l ! h WM+IR ª ! 9/80 DLU211 No well observed Nil to Moderate TW/BW 80-100 m 30-50 LPM Low P Not Required water table conditions. Primarily forest Nunduri d Colony Bangal " r Nil " DKarisunda Dharampur Upland(DLU) " d (Impervious Material) ) " a areas with sparse settlements.Not APY113 APY113 "Chak i Sahaspur 6/12 g M 7/80 " l Bajitpur" Kenet !! Chhota suitable for large scale development ! " Paharpur " ( ªª a D Gobindapur "Bhurkunda " of groundwater. L " Bihar Panjkona D11 "Pushkarlni " "Gabpur Dharampur" 6/80 "Santara Thakurani ! Dongalan Chandpur 6/11 D Mandra" F F " !" Pushkarini PB111 ª " Fadilpur 10/80 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. Bhitsayer " ! " D)" 6/13 Singerbandh Musarbal Akui Daulatpur ! Simulia " Chandipur " ª" Rasulpur " ! Molkiri " " 6/10 D " Rakta " ! Ashwanpur D D Q Q P P Madanhardanga ª " " Nara Banshi " " Q P P These are dykes, quartz reefs and pegmatite veins, which generally act as barriers for ground water movement. " Bagmari" 6/12 Bara Dasarathbati Jhiknara" 4/10 D D Q Akrasal "Srirampur ! ! " ª ª Tandighi Gobindapur Kushmuri 9/85 Borajpota Kanchanpur " D"! " " " "Srirampur1 8/12 " 4/11 ! Fatehpur 10/90 Baruli ! Pankhal Tentulmuri !" " " ª ª " Belekhali ) N" L13 D " " Bhurbandi Tishanal Shanpura Ballampur " 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. Madhupur " " Babla " Belekhali 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. Chandpukur " Kalagram 7/13 "Palpata Chandpukur !" 9/80 "Pujur ª Sahisnara!" APY113 10/80 "Sursinghapur D! Pantrai Shyampur "! Ha"riharpur " D ª " Shyamsundarpur Jagaldwip 6/12 ) Palashi " 7/12 Gechho" " ! Goalpukur ) ! ª Jashdighi " "Birampur Chhatina ª " " "Bagajal PB111 " PB111 Maheshpur" "Parashe 10/33 Chandgram Dhajamanipur Gaur Khayerbani ! "6/13 " " " " D ! Bhabanipur Daripota ª !Ranahat " 6/13 ª " ! GROUND WATER PROSPECTS INFORMATION HYDROLOGICAL INFORMATION STRUCTURAL INFORMATION BASE MAP INFORMATION LOCATION INFORMATION Shanpura ª Kharsi Baidanga "Khatnagar " " 6/15 6/10 " ! DESCRIPTION