Mega-geomorphology and sedimentation history of parts of the Ganga–Yamuna plains
Mega-geomorphological units in parts of the Ganga–Yamuna plains have been mapped using IRS-LISS III remote sensing data. The study highlights the differences in geomorphic setting of this part of the Gangetic plains with that in more eastern parts, and this is manifested in fluvial landforms. A 20 m...
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Veröffentlicht in: | Current science (Bangalore) 2002-03, Vol.82 (5), p.562-566 |
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creator | Sinha, R. Khanna, Madhur Jain, V. Tandon, S. K. |
description | Mega-geomorphological units in parts of the Ganga–Yamuna plains have been mapped using IRS-LISS III remote sensing data. The study highlights the differences in geomorphic setting of this part of the Gangetic plains with that in more eastern parts, and this is manifested in fluvial landforms. A 20 m incised bank section at Kalpi in the Yamuna plains has also been examined and preliminary interpretations about the general stratigraphy are presented. The fluvial sequence manifests several hiatuses in the sedimentation record represented by palaeosol units. |
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K.</creator><creatorcontrib>Sinha, R. ; Khanna, Madhur ; Jain, V. ; Tandon, S. K.</creatorcontrib><description>Mega-geomorphological units in parts of the Ganga–Yamuna plains have been mapped using IRS-LISS III remote sensing data. The study highlights the differences in geomorphic setting of this part of the Gangetic plains with that in more eastern parts, and this is manifested in fluvial landforms. A 20 m incised bank section at Kalpi in the Yamuna plains has also been examined and preliminary interpretations about the general stratigraphy are presented. 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K.</creatorcontrib><title>Mega-geomorphology and sedimentation history of parts of the Ganga–Yamuna plains</title><title>Current science (Bangalore)</title><description>Mega-geomorphological units in parts of the Ganga–Yamuna plains have been mapped using IRS-LISS III remote sensing data. The study highlights the differences in geomorphic setting of this part of the Gangetic plains with that in more eastern parts, and this is manifested in fluvial landforms. A 20 m incised bank section at Kalpi in the Yamuna plains has also been examined and preliminary interpretations about the general stratigraphy are presented. The fluvial sequence manifests several hiatuses in the sedimentation record represented by palaeosol units.</description><subject>Braiding</subject><subject>Floodplains</subject><subject>Groundwater</subject><subject>Mud</subject><subject>Natural channels</subject><subject>Nodules</subject><subject>Plains</subject><subject>RESEARCH COMMUNICATIONS</subject><subject>River meanders</subject><subject>Riverbanks</subject><subject>Rivers</subject><issn>0011-3891</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><sourceid/><recordid>eNotjk9KxDAcRrNQcBw9gpALFPJnkiZLGXQURgZEF66GX5qkTWmT0sRFd97BG3oSZ9DV-xaPj3eBVoRQWnGl6RW6zrknhHFG9Aq9vrgWqtalMc1Tl4bULhiixdnZMLpYoIQUcRdySfOCk8cTzCWfR-kc3kFs4efr-wPGzwh4GiDEfIMuPQzZ3f5zjd4fH962T9X-sHve3u-rntaiVM4oIZW0_gRhGuZM7Z1TllsuN7XU2nBmhWRUE3WSjKJG-1oRB16qxjR8je7-fvtz3HGawwjzcmQbSoSWgv8CTnJKpA</recordid><startdate>20020310</startdate><enddate>20020310</enddate><creator>Sinha, R.</creator><creator>Khanna, Madhur</creator><creator>Jain, V.</creator><creator>Tandon, S. K.</creator><general>Current Science Association</general><scope/></search><sort><creationdate>20020310</creationdate><title>Mega-geomorphology and sedimentation history of parts of the Ganga–Yamuna plains</title><author>Sinha, R. ; Khanna, Madhur ; Jain, V. ; Tandon, S. 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K.</creatorcontrib><jtitle>Current science (Bangalore)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sinha, R.</au><au>Khanna, Madhur</au><au>Jain, V.</au><au>Tandon, S. K.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Mega-geomorphology and sedimentation history of parts of the Ganga–Yamuna plains</atitle><jtitle>Current science (Bangalore)</jtitle><date>2002-03-10</date><risdate>2002</risdate><volume>82</volume><issue>5</issue><spage>562</spage><epage>566</epage><pages>562-566</pages><issn>0011-3891</issn><abstract>Mega-geomorphological units in parts of the Ganga–Yamuna plains have been mapped using IRS-LISS III remote sensing data. The study highlights the differences in geomorphic setting of this part of the Gangetic plains with that in more eastern parts, and this is manifested in fluvial landforms. A 20 m incised bank section at Kalpi in the Yamuna plains has also been examined and preliminary interpretations about the general stratigraphy are presented. The fluvial sequence manifests several hiatuses in the sedimentation record represented by palaeosol units.</abstract><pub>Current Science Association</pub><tpages>5</tpages></addata></record> |
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language | eng |
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source | JSTOR Archive Collection A-Z Listing; EZB-FREE-00999 freely available EZB journals |
subjects | Braiding Floodplains Groundwater Mud Natural channels Nodules Plains RESEARCH COMMUNICATIONS River meanders Riverbanks Rivers |
title | Mega-geomorphology and sedimentation history of parts of the Ganga–Yamuna plains |
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