GROUND WATER PROSPECTS MAP L E G E N D RECHARGE RECHARGE MAP UNIT GEOLOGICAL SEQUENCE / GEOMORPHIC DEPTH TO G R O U N D W A T E R P R O S P E C T S ( PREPARED FROM SATELLITE IMAGE INTERPRETATION WITH LIMITED FIELD CHECKS ) CONDITIONS STRUCTURES ROCK TYPE UNIT / LANDFORM WATER LEVEL ( HYDROGEOMORPHIC BASED ON SUITABLE & UNIT ) TYPE OF WELLS HOMOGENEITY PRE / POST- MONSOON AVAILABILITY AQUIFER MATERIAL DEPTH RANGE YIELD RANGE QUALITY OF PRIORITY IN THE UNIT GROUND REPRESENTED IN (AVERAGE IN METERS) OF WATER SUITABLE OF WELLS WATER OF WELLS WATER PT = PERCOLATION TANK THE MAP WITH & SUCCESS R E M A R K S ( SUGGESTED ) POTABLE (P) IRRIGATED CD = CHECK DAM ALPHANUMERIC CODE ( EXPECTED ) RATE OF WELLS ( RAINFALL & OTHER NON - POTABLE (NP) AREA NB = NALA BUND ( PROBLEMS / LIMITATIONS ) NO. OF WELLS LS = LOOSE SEDIMENTS DW = DUG WELL 3 ( PROBABILITY ) RW = RECHARGE WELL ( REPRESENTED IN SOURCES ) MIN - MAX ( in LPM or m / day) ( REPRESENTED IN OBSERVED PR = PERMEABLE ROCK RW = RING WELL DT = DESILTING OF TANK FIR ( INDICATE REASONS IF ( APPROX . RANGE Kilometers ( COLOUR INDICATES THE MAP WITH THE MAP WITH = FISSURED ROCK BW = BORE WELL NON POTABLE ) RP = RECHARGE PIT ( IN METERS ) IN PERCENTAGE ) YIELD RANGE AND NUMERIC CODE ) FR = FRACTURED ROCK TW = TUBE WELL VERY HIGH SD = SUBSURFACE DYKE ALPHABETIC CODE ) 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 SCALE - 1 : 50,000 s o p MAP SHEET NO. 73N/15 HOWRAH, PURBA MEDINIPUR & PASCHIM MEDINIPUR DISTRICTS, WEST BENGAL e D Meander Scar RW Groundwater prospects very high MS111 ) Gomakpata y No well observed "Sitapur " Ulanpara Good 10-15 m 200-250 LPM High P Nil Uttar "Bamangram " LS Not Required with high recharge potential. a Dipamalita y (MS) TW Jagannathpur Purba " 11/210 " " d Recharge structures not required. Siuria a Manika !" " "Bangalpur Gauranga " Bangolipara "Nashibpur D Adra " t Kalyanpur 1 D " Khas Chak 4/140 Jagat " n 8/158 ! D " Chak Amrajol D t Chak " 18/152 ! " Bagor a e D" m n " 10/240 s Kanoi Gopalnagar 12/1"15 Birampur Narayan 12/121 FP111 " o APY113 e Rai Chak ! FP111 e " Chak " ! Kaphold d ª r " !" D Sapsit FP111 Chak Pashchim Sulani " a "Shirpur D "Khadinan Faridpur 1 Khajuti s r E10 Kashinathpur " " P " Manika Jhuka Kanai e " , Nagoda R i FB12 Chak " r " Padima i Murgabari " v 12/106 Monaharpur h " Upadkul P Alluvium Ananda Rain e 13 / 8 Chak " t ! ! " " Mesera Kalikapur Flood Plain TW Potable water available at shallow r P 11/1D21 " ( APY113 D "Pakura FP111 Very Good LS 25-30 m Very High 72 " H3 a " "Chak Barabar (Sand Dominant) 250-350 LPM ! 11/115 Kasai Marberia " ) (FP) Not Required depth. Sadaram D " " FP111 r 2 Bhagaboti " i (111) Chak " Patinan g Changageri " Gobindapur FP111 a l " 7/150 "Teorpara Kulia 1 K h a ! " N a i n FP111 10/180 D h "Baksitala b Gopalpur "Sandal Hijlok ! " " " B "Khukhurdaha Beladanga ª Golamutha ) " Khanedihi Sajnagachhia Panitras " 10/183 Chandpur 14/173 Kansabati N " " Khadinan " ! " D! )" 6 D "Mukdanga NH Kansabati Nadi Kaji Bathanberia " "Chak Manua " " "Muralibar Brindaban " "Arar Mamurchi Purbapara " Nabason Chak " 14 / 7 FB12 Bara"nda 10/220 Flood Plain Areas of low groundwater potential. FP111 n 10/195 !APY113 !!12/180 Very Good LS TW 150-200 m 400-500 LPM High P 12 Not Required 10/186 D Bagnan"ªD " o (FP) Better potential at greater depths. Pashchimpara "Bardangi 11/23"0 3 " ! Tapur Mahadebpur i D"Jadupur Kulia "Asharia " " ! Malluk t ª Chhatinga " 8/230 Iswaripur " A Y ! W a S 12/146 D I L Shitalpur Ramchandrapur " A " H ! Matimala R 12/210 m Purba "Bagtia " R N Hatempur "Markundapur D Paikpari E " 4 T ª! Saorberia E A S r " " H Ramnagar " U T Durlabhpur Khalur o 14/137 Hospital S O " Ramchandrapur " F ! " "Madari " D "Jogiber "Paramanandapur Chapda Tamultala 10/220 " " a "Patharia " Brindabanpur "Jagannathpur ! Deulti Rana " 10/187 "Sohapur ª Alluvium 16 / 9 " " w Flood Basin Poor Areas of low groundwater potential. ) Rasti ) " " ! Kanchrul Khari Khaji " "Paikpara LS D " Chak Barul FB12 t (Clay Dominant) TW >100 m 150-200 LPM Low P 68 Not Required Kshetra Payag " Chak 12/152 Bhularo "Antilla e (FB) 20 Better potential at greater depths. Nankar Pulshit ! " a " Nana " Komola " Heiedwip (12) Uttar Hat Kunar D " n Bankadanga " Teghari ! Banshberia Santoshpur " Chak D " " K Chak e "Panchberia 13/137 Najarpur / " 10/237 Kamardaha " Nandanpur Krishnanagar " " c " ! a "Naupala D o Panshila PC13 r Kayadangi F17 l " " "Kantapukur 12/103 Darish Bakurdaha "Chaitanyapur u ! Amir " " o D! Jianda Mihitikri Kolaghat Kultipara s D " Chak Pairit APY11"3 " Orphuli Amberia " " " " " H 14/155 Khaji n Kaya " " Bantuj Kantabani "Uttar 1 " Kharisa ) " " Jiandapara i Ayema " " " Shridharbasan e 14/152 Mosama h Babua "Palara Nunthia NP Chak t Keshapat Tiarpara ! " Areas with high Arsenic and Iron " D Deotabar C Alluvial Plain " a (As&Fe) RW / 14 / 8 8/190 " " Good LS 40 concentration.Potable water available Meshra " Chandbhag " L Younger TW 100-120 m 400-500 LPM High " Dainan APY113 h [At shallow !" Gobinda Rasha Birkul Low D H4 " 66 at depth range above 100 m. Recharge Bishnubar Chak g (APY) Chak o depth] Gurehaki " MS111 " of shallow aquifer recomended. a Kanaipur t " Sangambasan Manishgot Baidyanathpur " Dehati " "Baradabar " " 10/230 " b Gopalnagar "Padampur Bagur Harinarayanpur " Dungama y " " ! Faridpur Deuibar ) " l " ª ) Purba m "Bhujata Mechada r Bahala " FP111 a Alluvium Chak Parbatipur " r Jianda FP111 " a 8/189 ) Sundar 12/121 (Sand and Silt) Jianda Sagobor "Mugkalya " E ! Uttar " ! A D " Nahala " "D ( Dakshin " 11/137 / (113) " Gopalpur "Siuria Panchani a l Kakadihi ! "Beltala Khajurnal Balisar a n Bargachhia " " gujrat a " 12/128 D! l C Kumar " D! r e " " ! 12/115 "Diglabar e v D ) D L Chak " Keon 16/137 FP111 Akubhag Kaliswar i g h " Pashchim Amalhara " u " H Banpur Alluvial Plain r Bahala k ! APO13 i p u Nandai " Chandigarh Potable water available at shallow D i n " " TW d s Younger Not Required 12/121 M e Gajan Mecheda Srikrishnapur APY113 No well observed Good LS 25-30 m 200-300 LPM P 25 APO13 " Khus " Chandanapara Mirpara High depth. " n Siddha "Gobra (APY) " Kadalia Brindaban Chak )" " " a "Halyan C"hak "Hakala P Santipur Jamitta " Duliara " Brindabanpur " Bar " Bansda Kharui 12/146 13/115 14/140 " " ! Halyan 13/134 ! D 6/144 ! " ! ! Barnan " DD D " Pranballobpur D) W A Y Alua " Hariharpur Salukpara L ) H E A S T E R N R A I " " S O U T Ramchandrapur Chak Benapur " e "Bagichia " Bangalpur1 Gathig Kisharpur Katagachi " " " " n " Narayan Darlala Kamalbar e 12/159 Bhogpur " n Pakuria c "! " )Ï" Shrikumar Kishor Uttar o D o Mahammadpur Dubjara Chitra Mosha " Samto Chak " " Kanpur " i " " Sahara R l "Chak " ) )" t Paleo-Channel Areas of very high groundwater 12/176 Mirzapur " No well observed Hurinan Purushottampur " Malpur o Very Good RW 10-15 m 200-250 LPM Nil ! " " PC13 a LS Very High P Not Required D " Murari Bagicha (PC) potential at shallow depth.Most H " Ja"phali )" Uttar 10/170 Khasrekha U Damodarpur TW Bangalpur Kumar Betberia Barasat " m suitable for extraction of groundwater. " " ! " Chanchlara r " Chak y Raghubir J o y g o p a l K h a l " ) D Barari l Khajnabahaia " Jagadishpur o Chak Sahira P " " Putulsaha r " " Dakshin " APY113 Pratappur F " " Rengora " a ) " Dakshin 8/189 FP111 ) " Gopinathpur 9/212 t Chanciara !" Ramtyarak N E Alluvium - D " ! a Deria D " 8/280 (Sand,Silt & Clay) Hirapur Soyadighi e " Naul h Dhuliapur Kamlia Chak " "Balarampur ! " " Agar "Chatara "Chaulia D r " A n (13) 11/170 Palkpari u " D! e c Domura Suttikri p "Panchberia 1 " " " Baikunthapur "Chanpabar "Kalandipur R " Darlara 1 o " m "Hogalberia t Atbeluria Pipulnan a N Khasharbon Balluk F22 " s " " 12/168 A H Nakulyan i Sundarnagar " R " ! " Moderate groundwater potential Gopalbar Hogla Belpukur / Chakdaha " D " e RW 4 Kanktya 12/182 Alluvial Plain Older 15 / 8 Gumal " "Alinan ! Moderate to " 1 l " Atberia a at intermediate depths. " ) " D APO13 Moderate to Good TW 150-200 LPM P 46 Bar Y "Adulepara LS 40-60 m Moderate to Low (APO) P APO13 Salra Nandanpur u 18 High 14/115 Cheinpur 13/146 14/98 Rani " " Harashankar " j ! ! ! Chak " 12/146 e D! 12/146 D D " Sabal Kali "Kultikri i D ! A t " Kharpal Uttar D " Ara Jasamantapur Chak S " Janubasan " Henria a Raghunathbari 10/190 " Baharpata " " " Bar " "Oushadhpur Siuri Deora Rautara ! " " L D" Nunnan " " N Baharpata ( Purba Prasad Bar Gonjola 8/126 Mohanpur Ukharpara Kankharda Kaorapara " " " Itara " "Chak " Suiri " ! " 10/220 Purba DOsmanpur Kontaldaha Amragoal " " ! Shuktia 14/137 ª " " " Ahmadpur "! Harashankar Panchberia Shamaspur D " Gathkilla Uday " Gaurangapur F16 Jagannathpur Khandakhola Harashnkar " Biswas Mukundapur F F "Chandipur " FB12" Chak "Belum " " 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. Purushotta"mpur 1 R " " Baman Krishnanagar Kunar " Ara Chandpur Bhagabatipur) Ara 12/146 Kismat " H11 " I ) ! " Rani Chak " Telipara Shas"hati 10/212 APY113 Radhakrishnapur Maheshwar D Mahishda " Palgeria D D Q Q P P " Beraberia 1 " " ! " Shoyadighi V ª Q Q P P These are dykes, quartz reefs and pegmatite veins, which generally act as barriers for ground water movement. " "Gobindapur " Manoharpur " D D 14/143 " Jhakar "Keshab " ! Sadi Rani Ard Bar E " D 14/121" Harashankar 11/170 Gaurangapur "Nilkanthia Manik Kheyatala Mathuri Bardaspur Dauli Chhaugiri Chak Chak Karanga! Khoskhana " Khorod " " Gogras " 13/140 Kh"aman Chak " D " ! Oushadhpur Kundra "Biswas D Chak Lohanda ! " " " " D 12/137 R Udhabpur " N.B.-The depth range and yield range of wells may vary within the unit because of certain inhomogeneities.