The West Victorian Uplands of Southeastern Australia: Origin and history
The West Victorian Uplands is a region of low relief, gentle gradients, young volcanicity and local domal uplift. These characteristics distinguish it from the rest of the Eastern Highlands of Australia. The origin of the West Victorian Uplands dates back to uplift in the Cretaceous, but elevation a...
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Veröffentlicht in: | Earth surface processes and landforms 1992-06, Vol.17 (4), p.407-418 |
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description | The West Victorian Uplands is a region of low relief, gentle gradients, young volcanicity and local domal uplift. These characteristics distinguish it from the rest of the Eastern Highlands of Australia. The origin of the West Victorian Uplands dates back to uplift in the Cretaceous, but elevation and relief have always remained low. Further uplift, extending westwards from central Victoria, may have begun raising the West Victorian Uplands in Middle Tertiary times. Doming, fault activity, earthquakes and volcanism are extending progressively westwards. Not only may the Eastern Highlands of Victoria have grown in this way in the past, but the area may also provide a view of the early evolution of the Eastern Highlands of Australia. |
doi_str_mv | 10.1002/esp.3290170410 |
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Not only may the Eastern Highlands of Victoria have grown in this way in the past, but the area may also provide a view of the early evolution of the Eastern Highlands of Australia.</description><subject>Australia</subject><subject>Bgi / Prodig</subject><subject>Doming</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Faulting</subject><subject>Geomorphology, landform evolution</subject><subject>Oceania</subject><subject>Physical geography</subject><subject>Regolith</subject><subject>Southeastern Australia</subject><subject>Surficial geology</subject><subject>Uplift</subject><subject>Volcanism</subject><subject>West Victorian Uplands</subject><issn>0197-9337</issn><issn>1096-9837</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1992</creationdate><recordtype>article</recordtype><recordid>eNqFkEFPwjAUgBujiYhePffgdfi6duvqjSCChggJIMem21qpzm1pR5R_78wMxhOnd_m-914-hK4JDAhAeKt9PaChAMKBEThBPQIiDkRC-SnqARE8EJTyc3Th_RsAISwRPTRdbTXeaN_gF5s1lbOqxOu6UGXucWXwsto1W618o12JhzvfOFVYdYfnzr7aErcY3lrfevtLdGZU4fXV7-yj9cN4NZoGs_nkcTScBYpBDIHmQEKmgSaaM5oCV8ANS_IoNaBTiGIdGc6zXBAa0zw11DASAclZAiYLTU77aNDtzVzlvdNG1s5-KLeXBORPB9l2kH8dWuGmE2rlM1UYp8rM-oMVRzThcBxrexFgLSY67NMWen_kthwvF_8-CTq3Laa_Dq5y7zLmlEdy8zyR9zETixlfySf6Db3IiXo</recordid><startdate>199206</startdate><enddate>199206</enddate><creator>Joyce, E. 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B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a4060-e70124e038e743b07a07f48d5bf0eb056e5f77cd91363dbf3f41501d480fc2fd3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1992</creationdate><topic>Australia</topic><topic>Bgi / Prodig</topic><topic>Doming</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Faulting</topic><topic>Geomorphology, landform evolution</topic><topic>Oceania</topic><topic>Physical geography</topic><topic>Regolith</topic><topic>Southeastern Australia</topic><topic>Surficial geology</topic><topic>Uplift</topic><topic>Volcanism</topic><topic>West Victorian Uplands</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Joyce, E. B.</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><jtitle>Earth surface processes and landforms</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Joyce, E. B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The West Victorian Uplands of Southeastern Australia: Origin and history</atitle><jtitle>Earth surface processes and landforms</jtitle><addtitle>Earth Surf. Process. Landforms</addtitle><date>1992-06</date><risdate>1992</risdate><volume>17</volume><issue>4</issue><spage>407</spage><epage>418</epage><pages>407-418</pages><issn>0197-9337</issn><eissn>1096-9837</eissn><coden>ESPLDB</coden><abstract>The West Victorian Uplands is a region of low relief, gentle gradients, young volcanicity and local domal uplift. These characteristics distinguish it from the rest of the Eastern Highlands of Australia. The origin of the West Victorian Uplands dates back to uplift in the Cretaceous, but elevation and relief have always remained low. Further uplift, extending westwards from central Victoria, may have begun raising the West Victorian Uplands in Middle Tertiary times. Doming, fault activity, earthquakes and volcanism are extending progressively westwards. Not only may the Eastern Highlands of Victoria have grown in this way in the past, but the area may also provide a view of the early evolution of the Eastern Highlands of Australia.</abstract><cop>Sussex</cop><pub>John Wiley & Sons, Ltd</pub><doi>10.1002/esp.3290170410</doi><tpages>12</tpages></addata></record> |
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source | Wiley-Blackwell Journals |
subjects | Australia Bgi / Prodig Doming Earth sciences Earth, ocean, space Exact sciences and technology Faulting Geomorphology, landform evolution Oceania Physical geography Regolith Southeastern Australia Surficial geology Uplift Volcanism West Victorian Uplands |
title | The West Victorian Uplands of Southeastern Australia: Origin and history |
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