J Indian Soc Remote Sens

2001

DOI: 10.1007/bf02989928

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Hydromorphogeology and Remote Sensing applications for groundwater exploration in agnigundala mineralised belt, Andhra Pradesh, India

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M. Jagannadha Rao

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B. Suryaprakasa Rao

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et al.

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Valley Fills1

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Cited by 6 publications

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“…and Sriwttsava, 1991;Singh et al, 1993;Pal et al, 1997;Pratap et al, 1997). Sankar et al (2001) have carried out hydrogeomorphok)gical and remote sensing investigations in Agnigundala mineralised belt, Andhra Pradesh and identified valley fills sediments over granites and granite gneiss. They have opined that valley fills are excellent (geological) areas for groundwater storage.…”

Section: Valley Fillsmentioning

confidence: 99%

Identification of groundwater prospective zones using irs-id liss iii and pump test methods

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2004

J Indian Soc Remote Sens

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The role of hydrogeomorphological units and lineaments in tile storage of groundwater from the Muvattupuzha river basin has been investigated using IRS ID LISS Ill data. Other than the usual water bodies such as river course, reservoirs and ponds, the major hydrogeomorphologica[ units identified in this basin in the descending order of their groundwater potential are: valley fills, moderately dissected plateau, pediments, residual mounts, residual mount complex, linear ridges, residual hills and structural hills. Majority of the lineaments trends in NW-SE and WNW-ESE directions. Even though the eastern part of the basin is characterised by moderate to high lineament density, the above area is found to be poor to moderate groundwater prospect zone because of high gradient and structural hills. Tile pump test analyses of dug wells from different hydrogeomorphic units also confirm that valley fills are the most promising unit lot groundwater prospecting than the rest.

“…and Sriwttsava, 1991;Singh et al, 1993;Pal et al, 1997;Pratap et al, 1997). Sankar et al (2001) have carried out hydrogeomorphok)gical and remote sensing investigations in Agnigundala mineralised belt, Andhra Pradesh and identified valley fills sediments over granites and granite gneiss. They have opined that valley fills are excellent (geological) areas for groundwater storage.…”

Section: Valley Fillsmentioning

confidence: 99%

Identification of groundwater prospective zones using irs-id liss iii and pump test methods

¹

,

²

2004

J Indian Soc Remote Sens

View full text Add to dashboard Cite

The role of hydrogeomorphological units and lineaments in tile storage of groundwater from the Muvattupuzha river basin has been investigated using IRS ID LISS Ill data. Other than the usual water bodies such as river course, reservoirs and ponds, the major hydrogeomorphologica[ units identified in this basin in the descending order of their groundwater potential are: valley fills, moderately dissected plateau, pediments, residual mounts, residual mount complex, linear ridges, residual hills and structural hills. Majority of the lineaments trends in NW-SE and WNW-ESE directions. Even though the eastern part of the basin is characterised by moderate to high lineament density, the above area is found to be poor to moderate groundwater prospect zone because of high gradient and structural hills. Tile pump test analyses of dug wells from different hydrogeomorphic units also confirm that valley fills are the most promising unit lot groundwater prospecting than the rest.

“…These landforms act as ground water storage reservoirs and some of them can act as recharge and run-off zones (Jai Sankar et al, 2001). Different landforms have been delineated by standard visual interpretation techniques on IRS-IB-LISS-II data (Fig.l).…”

mentioning

confidence: 99%

An integrated study on ground water resource of pedda gedda watershed

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2004

J Indian Soc Remote Sens

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Geomorphology and land use pattern of visakhapatnam urban - industrial area

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et al. 2003

J Indian Soc Remote Sens

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Geomorphology and land use pattern of Visakhapatnam urban -industrial area have been studied using IRS IB and SPOT data. The geomorphie units under structural landforms, fluvial landforms and coastal landforms were identified and appropriate field confirmations were made. The geomorphic units such as inselbergs/residual hills, rolling plains, colluvial plains, fractures, piedmont fans, pediments were identified under structural landforms. The units wind gap, paleo channels, gully land, alluvial plain and natural levee were identified under fluvial landforms. The coastal landforms include sea cave, sea stack, red sediments, beach sands and marshy area. Study of the land use pattern reveals the land use under various categories of residential, planned and un planned, agricultural land, waste land and others. The data will have high relevance and usefulness for urban, industrial and ground water resource evaluations in the context of rapid urbanization and industrialization.

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