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 / CONDITIONS STRUCTURES ( PREPARED FROM SATELLITE IMAGE INTERPRETATION WITH LIMITED FIELD CHECKS ) 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 = DUG WELL 3 RW = RECHARGE WELL ( REPRESENTED IN SOURCES ) DW MIN - MAX ( PROBABILITY ) ( REPRESENTED IN OBSERVED PR = PERMEABLE ROCK RW = RING WELL ( in LPM or m / day) DT = DESILTING OF TANK FIR ( INDICATE REASONS IF ( APPROX . RANGE ( COLOUR INDICATES THE MAP WITH THE MAP WITH = FISSURED ROCK BW = BORE WELL NON POTABLE ) RP = RECHARGE PIT FR ( IN METERS ) IN PERCENTAGE ) Kilometers YIELD RANGE AND NUMERIC CODE ) ALPHABETIC CODE ) = FRACTURED ROCK TW = TUBE WELL VERY HIGH SD = SUBSURFACE DYKE 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 SCALE - 1 : 50,000 s Groundwater prospects very high t Channel Bar RW i No well observed Excellant LS 5-10 m Very High P Nil Not Required with high recharge potential. MAP SHEET NO. 73N/14 HOWRAH, HUGLI, PURBA MEDINIPUR & PASCHIM MEDINIPUR DISTRICTS, WEST BENGAL CB111 s (CB) TW 400-500 LPM " o Recharge structures not required. " Mahipara p Gujrat "Kantapukur " Konakpur Baira " Atgara e Anndol " " Madanpur " " " " Khanpara Madanpur " Kurchi 1 Khempur D Mayal Barbakul Chak Kolmi " " Raibarh " " " " Bhedua y "Bandipur Harali " Kaiba a ) " "Ghol " Sankarpur Patul "Gourangapur " d Bamankhand " Raghunathpur " Radhanagar " Malikpara Satpota " " t Bhelua "Harinagere " Durgapur " Pahar " Senpur Sitapur n Srirampur chak "Daspur " " " e Ishanpur " Harali Nagarpara " " s Isapur "Sultanpur " Gopinathpur e "Ghansa "Pangare Bagri r " "Kurchi ) Arandabazar Chak P " y Alluvium " Piarapur / Point Bar Groundwater prospects very high Krishnanagar Jagannathpur " " Baira a RW Ghoshpur " n (Sand Dominant) Dakshinapara "Kumaripara "Dhuliapara " Very Good 300-500 LPM " Sulut Kurchi Pratap D 5-10 m P Not Required " Chatrasali " PB111 o (PB) No well observed LS TW Very High Nil with high recharge potential. Banahari K10 i (111) Chak t " t Jora "Amarpur Recharge structures not required. Singhpur n " a " "Kulat Gopalnagar e " "Garhberia Gaja m Ramnagar " Takapur " s " Jagri " r "Radhanagar e Dhulekunda o " r "Dhamla Udaynarayanpur" "Pol F " P ( Kolagachia i "Malancha 10/60 "Kotra Jospur Sarda K11 h " " " ! "Ghoshpur D Jangalpara t Benatola Narayanpur " " a "Sahanpur Narendra r "Dakshinpara Arunda " i Khadra "Singli "Chak Birlok Radhaballabhpur 6/120 " " g " terai Iterar " "Dakshinpara Bondhaipur " " ! " Samanthapara " DBelgran a Kachra Malikpara " Sibpur h " Ramnagar Ghagarpur " Nij " ) " Sonatikri B Groundwater prospects very high " / Mansukha i " FP111 Flood Plain No well observed <30 m 250-300 LPM Very High 40 with high recharge potential. "Madhabkundi l Very Good LS TW P Not Required "BoroPara Khanakul " "Kedarpur Datta g (FP) Recharge structures not required. Chak u Abidpur Arunda" " Sibanipur " Nabason " " H " " " Akna Daulat Nakunda Sibpur " " Atrogarh Joyda "Duliapara Naoshar " " Rajapur "Chak " Thakurani Mainan "Ajodhya "Pancharul "Dharasimul Chak "Sankarpur " 13/150 "Harishpur " Udaypur Ramsaran Dhero " Brahmanpara ! n " Dainan " Kabilpur ª Chak Dharmapur " Chak " " Gara o Para Jayram " " i "Jaynandapur Akna t "Gunanandapur Baishnabpara Chak " Rajapur " " Chak PB111 a " Kamdebpur " " " Jonka Thakurani Gangaprasad m " Chakrapur Ketedaha Sodam Dakshin " " Singti " Chak r Flood Basin "Dabandi "Panchtikri " " No well observed Poor Areas of low groundwater potential. "Hirapur Anantanagar "Chak Harishpur TW >100 m 150-200 LPM Low P Nil Singhpur o " (FB) LS Not Required "Chabbishpur FB12 Better potential at greater depths. Sonagachia " F Pati Malancha BAlai ) " " a Sargal Musalmanpara " "Rahulkhana "Chak " 8/60 Gauranga e Kumirmara w " " t Sobsa ! n Badaspur " " D "Ranjitbati Chak Kankroi Santosh Chak H12 " a Kamarhati Subal e " "Singti Anulia Jaynagar " (Sibnarayan " c " Panchghara Chak Nishchintopur K Chak) " " / " o "Balipota " " Garh l Kaknan "Khantara "Tetuleh Nabin Chak " a Naopara r "Pratapnagar " Nabin Jugaldhah o (Nabinpara) AC13 u "Ramchandrapur Charhati "Sitapur Chak H " Chingra " s " " e Balipota Dabandi Dakshin n t Kaknan Purpat i Alluvial Plain Areas with high Arsenic and Iron " " NP Siagti " a Srirampur h Kaknan " Senhati Jayram " " " Ganeshpur " Alluvium Younger 11 / 7 concentration.Potable water L " Baligram C Good LS TW 400-500 LPM High (As&Fe) RW E8 Balarampur Kushali Chak " " Abhirampur / " " Naranarayan APY113 (Sand and Silt) (APY) >150 m 53 available at depth range above Simulia o 21 Panychanda 11/66 " h [At shallow Low "Chingra Uttar_mansri Kalikapur Chak " t (113) 150 m. Recharge of shallow ! " g " D 8/60 )" depth] a Bandar ! Shim " y aquifer recomended. " D Rajhati l " b Madhyarang Chak Rai Chak Kanupat " r " " Dakshin Pratappur m " Teorpara a Panychanda " "Mustaphapur Mansri a " " Mansuko " E r Ghoradana Hariram " ( " 12/189 Chak Baharampur Radhakrishnapur "Mamakpur " Chak " ! Debipur A " Bakanagar D " / "Harisinghpur a "Dhanyaghori Kumar Natibpur r CB111 " Chak 10/66 "Makri " u " ! "Baligarh k Harishpur " D "Sripur Garh s Chand n "Bhabanipur Thakurani Alluvial Plain "Ghoradaha Chak a " Chak 1 " APY113 Good LS P Younger No well observed 25-30 m 200-250 LPM P Potable water available at shallow "Ratneswarbati TW High 25 " Not Required "Ratneswarbati Nandanpur Kumar (APY) depth. " Bar " Sabalsinghpur Bhabanipur Sripur " Harish Chak Nandanpur 6/124 " " Chak ) " APO13 " D"! Shyamsundarpur " Palashpur Sonatala "Bolpai " K12 " Daulat "Monoharpur Chak Kansona " Kuna Chand "Suratban "Chak Chak Gurngarh Chltrasenpur 12/212 "Sabalsinghpur " " " Gopmahal D!" " " Bidhi " Bali Barbati Lalbenagoria ) n Chak e "Chandrapur Shyamsundarpur " o "Narendrapur n Abandoned Dakshinpara " " i Kalagechhia e Palashpai t " Patikhali " Baje Areas of very high groundwater " c Channel RW a No well observed Shudam Pratap AC13 o Very Good 250-300 LPM Very High P Nil potential at shallow depth.Most Khanjapur l (AC) LS 10-15 m Not Required " m "Kotasi TW o Bar Chak " "Champanagar Gholdipa r Banhijli " suitable for extraction of groundwater. H Kismat " Nandanpur " Haitpur Saimana o Kotalpur " " " " Jot F Khanjapur " y " "Nandanpur l Kanuramgarh t Raghunathpur " Pratap 6/130 r a Jagatpur Bhairabpur " a " " Nakubar Narayanpur D!Bagua Alluvium " E Gopalpur "Barabaman h " - (Borda) r Sarpai (Sand,Silt & Clay) "Kamalpur " e "Ranjoybar Kultikri u " n " 8/126 Makhalpur p (13) Kaigeria " e " Hanua " !" Shoshapata c D m "Jhikhira Paikbasa Saoraberia " o Dubrajpur Bhojan a " APY113 " t "Kalgeria s Sriramnagar R " i Alluvial Plain / Chand " Moderate groundwater potential e RW a 13 / 6 150-200 LPM Moderate to Kunda Sundarpur "Rautara Harindhara l Older TW 40-60 m P Khudi " " u LS 69 "Hajraberia Natungram H1 P Moderate to Good Moderate to Low at intermediate depths. Hayatpur j High " Chak " APO13 (APO) "Chak i 5 e t Salika S Ramnagar Rani " Durgapur " Blnala a "Bhagabatipur " Dihi Chak " 14/98 L " " Tealish ( " " ! Kumaria " Ishabpur Kishor Markhana " D "Amragari " Chak " ! Kundulia Kankrol D " Ramnagar Kumar Sibgachia 10/212 Krishtobati "Dholdanga " " Chak Chak " " F F Ramkrishnapur " Chota 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. "Bharatpur Janardan Kalikata" Pansiuli Raspur " " Chak "Nischintopur "Thalia Kaljuri " Chota D D Q Q P P Sheorapara Kalikata " Dari " P These are dykes, quartz reefs and pegmatite veins, which generally act as barriers for ground water movement. Ber " D D Q Q P "Sagarpur Sagarpur Ajodhya Sheorapara Sehagari " 10/201 " " Jot (! ª! "Maniram " " E "Jayput 10/183 9/213 Bhattikiri ! ! 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. Mahabbatpur D " D Santoshnagar " Chak " Satpata Mainan " 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. "Bishnupur "Chainpat 10/197 Dhalpur ! " Nabin Uday " KharDap " "Simulia Chak Nahia " Tajibere (K"hanap) Chainpat Gurdahpara " Ghanashyambati " Jagolgori " Dharapara Ghanashyambati " )" "Naihati Arita " "Kalbansh Betai " "Bhuta Bar"una GROUND WATER PROSPECTS INFORMATION HYDROLOGICAL INFORMATION STRUCTURAL INFORMATION BASE MAP INFORMATION