In this article we propose a Decision Support System using Case Based Reasoning (CBR) Technique for assessing ground water potential. Ground water is found in bedrock or in thick masses of overburden many feet below the surface. Theoretically ground water is function of various terrain parameters viz. Land Use/ Land Cover, Geology, Soil, Landform and Lineament. Using this theoretical framework ...

Increasing population growth worldwide is putting increasing pressure on water resources. In arid and semi area pressure goes to groundwater. Keeping in view havoc capability of remote sensing and GIS, a study for the integrated groundwater development has been under taken in part of Lalitpur district, Uttar Pradesh. The Satellite data of IRS -IC and ID have been used to prepare the hydrogeomor...

landscape that has escaped erasure by heating from below is imprinted with generation after generation of intersecting Four distinct classes of lineaments can be described on the ridges at various scales and orientations. Relatively recent fracbasis of Galileo’s improved spectral and spatial coverage of tures expose coarse-grained, clean ice in the shallow subsurface, Europa: (1) incipient crac...

We detect, for the first time, a negative free-air gravity anomaly of 23 mGal amplitude over a region in the South Atlantic Ocean centered at 48◦W and 35◦S. To this end, we used the integration of conventional shipborne gravity data and gravity data derived from GEOSAT/ERM satellite altimetry. The north bound of this anomaly coincides with the Chuı́ Lineament and the south bound indicates anothe...

This study aimed to delineate the intrusion body that controls structural setting and formation around river Niger-Benue confluence zone with particular attention its solid mineral potentials, this is achieved in mapping subsurface features through analysis of recent high-resolution aeromagnetic (HRAM) data-sets purpose examining their effects on geological structures characterize zones from ar...

The Sonju Lake intrusion (SLI) is a 1200-m-thick, shallow-dipping, sheet-like intrusion that forms part of the Beaver Bay Complex (RI-58, Chapter 7). Although its exposed strike-length is only about 3 km (Fig. 3-1), the SLI has a distinctive aeromagnetic signature that can be traced for at least 20 km beneath a cover of glacial drift. The nearly constant width of its aeromagnetic anomaly sugges...