Glacial Geology and Geomorphology of Terra Nova Bay (Antarctica).
During the two first Italian Antarctic Expeditions (1985/86 and 1986/87) glacial-geological and geomorphological research has been carried out in the area of Terra Nova Bay. In particular the Cenozoic glacial sediments, the Holocene raised beaches and the Holocene glacier fluctuations have been inve...
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ftunivpisairis:oai:arpi.unipi.it:11568/12293 2024-01-28T10:00:59+01:00 Glacial Geology and Geomorphology of Terra Nova Bay (Antarctica). BARONI, CARLO OROMBELLI G. Baroni, Carlo Orombelli, G. 1987 STAMPA http://hdl.handle.net/11568/12293 http://www.socgeol.info/Ricerca/pubblicazioni.asp?act=see&type=Memorie&y=1987&v=33&f= eng eng volume:33 firstpage:171 lastpage:193 numberofpages:23 journal:MEMORIE DELLA SOCIETA' GEOLOGICA ITALIANA http://hdl.handle.net/11568/12293 http://www.socgeol.info/Ricerca/pubblicazioni.asp?act=see&type=Memorie&y=1987&v=33&f= Glacial history Glacial geology Pleistocene Last Glacial Maximum Deglaciation Ornithogenic soil Relict penguin colonie Radiocarbon dating Holocene Terra Nova Bay Antarctica info:eu-repo/semantics/article 1987 ftunivpisairis 2024-01-03T17:42:04Z During the two first Italian Antarctic Expeditions (1985/86 and 1986/87) glacial-geological and geomorphological research has been carried out in the area of Terra Nova Bay. In particular the Cenozoic glacial sediments, the Holocene raised beaches and the Holocene glacier fluctuations have been investigated. Three main glacial drifts have been recognized. The youngest drift consists of a massive matrix-supported diamict extending up to about 350 m a.s.l. on the Northern Foothills, where it contains fragments of Pelecypods and Serpulids; it was deposited by a grounded ice-shelf during the last glaciation. In the interior mountains the upper limit of the drift rises up to about 1000 m a.s.l. The young glacial drift is characterized by frequent ice-cored topography, initial weathering stages, slightly stained granitic boulders without cavernous weathering, exept in the coastal belt. The older drift, very thin and discontinuous, occurs above the previous one, up to about 600 m on the Northern Foothills, and it is characterized by red stained granitic boulders affected by cavernous weathering. A third, oldest drift occurs up to 800 m a.s.l., composed of large and scattered boulders, strongly oxidized and affected by cavernous weathering, locally resting on a strongly developed red paleosol. At higher elevations up to about 1000 m round topped glacialy abraded reliefs, devoid of any glacial cover, can be observed and represent evidence of a still older glacial stage. Holocene beaches raised up to 30 m are well known at Terra Nova Bay (Inexpressible Island and Gerlache Inlet). In addition to the ones described by previous authors, other emerged beaches have been found in several localities on the coast of the Northern Foothills, near Evans Cove and at Edmonson Point. It is possible to distinguish two groups of emerged beaches: the first one consists of the beaches at Inexpressible Island and the Northern Foothills, ranging in altitude up to about 30 m a.s.l.; the second group, not higher than 7 m, is present at the ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Shelf Inexpressible Island ARPI - Archivio della Ricerca dell'Università di Pisa Antarctic Edmonson Point ENVELOPE(165.133,165.133,-74.333,-74.333) Evans Cove ENVELOPE(163.800,163.800,-74.883,-74.883) Gerlache ENVELOPE(99.033,99.033,-66.500,-66.500) Gerlache Inlet ENVELOPE(164.100,164.100,-74.683,-74.683) Inexpressible Island ENVELOPE(163.650,163.650,-74.900,-74.900) Northern Foothills ENVELOPE(163.917,163.917,-74.733,-74.733) Terra Nova Bay The Beaches ENVELOPE(-56.832,-56.832,49.583,49.583) |
institution |
Open Polar |
collection |
ARPI - Archivio della Ricerca dell'Università di Pisa |
op_collection_id |
ftunivpisairis |
language |
English |
topic |
Glacial history Glacial geology Pleistocene Last Glacial Maximum Deglaciation Ornithogenic soil Relict penguin colonie Radiocarbon dating Holocene Terra Nova Bay Antarctica |
spellingShingle |
Glacial history Glacial geology Pleistocene Last Glacial Maximum Deglaciation Ornithogenic soil Relict penguin colonie Radiocarbon dating Holocene Terra Nova Bay Antarctica BARONI, CARLO OROMBELLI G. Glacial Geology and Geomorphology of Terra Nova Bay (Antarctica). |
topic_facet |
Glacial history Glacial geology Pleistocene Last Glacial Maximum Deglaciation Ornithogenic soil Relict penguin colonie Radiocarbon dating Holocene Terra Nova Bay Antarctica |
description |
During the two first Italian Antarctic Expeditions (1985/86 and 1986/87) glacial-geological and geomorphological research has been carried out in the area of Terra Nova Bay. In particular the Cenozoic glacial sediments, the Holocene raised beaches and the Holocene glacier fluctuations have been investigated. Three main glacial drifts have been recognized. The youngest drift consists of a massive matrix-supported diamict extending up to about 350 m a.s.l. on the Northern Foothills, where it contains fragments of Pelecypods and Serpulids; it was deposited by a grounded ice-shelf during the last glaciation. In the interior mountains the upper limit of the drift rises up to about 1000 m a.s.l. The young glacial drift is characterized by frequent ice-cored topography, initial weathering stages, slightly stained granitic boulders without cavernous weathering, exept in the coastal belt. The older drift, very thin and discontinuous, occurs above the previous one, up to about 600 m on the Northern Foothills, and it is characterized by red stained granitic boulders affected by cavernous weathering. A third, oldest drift occurs up to 800 m a.s.l., composed of large and scattered boulders, strongly oxidized and affected by cavernous weathering, locally resting on a strongly developed red paleosol. At higher elevations up to about 1000 m round topped glacialy abraded reliefs, devoid of any glacial cover, can be observed and represent evidence of a still older glacial stage. Holocene beaches raised up to 30 m are well known at Terra Nova Bay (Inexpressible Island and Gerlache Inlet). In addition to the ones described by previous authors, other emerged beaches have been found in several localities on the coast of the Northern Foothills, near Evans Cove and at Edmonson Point. It is possible to distinguish two groups of emerged beaches: the first one consists of the beaches at Inexpressible Island and the Northern Foothills, ranging in altitude up to about 30 m a.s.l.; the second group, not higher than 7 m, is present at the ... |
author2 |
Baroni, Carlo Orombelli, G. |
format |
Article in Journal/Newspaper |
author |
BARONI, CARLO OROMBELLI G. |
author_facet |
BARONI, CARLO OROMBELLI G. |
author_sort |
BARONI, CARLO |
title |
Glacial Geology and Geomorphology of Terra Nova Bay (Antarctica). |
title_short |
Glacial Geology and Geomorphology of Terra Nova Bay (Antarctica). |
title_full |
Glacial Geology and Geomorphology of Terra Nova Bay (Antarctica). |
title_fullStr |
Glacial Geology and Geomorphology of Terra Nova Bay (Antarctica). |
title_full_unstemmed |
Glacial Geology and Geomorphology of Terra Nova Bay (Antarctica). |
title_sort |
glacial geology and geomorphology of terra nova bay (antarctica). |
publishDate |
1987 |
url |
http://hdl.handle.net/11568/12293 http://www.socgeol.info/Ricerca/pubblicazioni.asp?act=see&type=Memorie&y=1987&v=33&f= |
long_lat |
ENVELOPE(165.133,165.133,-74.333,-74.333) ENVELOPE(163.800,163.800,-74.883,-74.883) ENVELOPE(99.033,99.033,-66.500,-66.500) ENVELOPE(164.100,164.100,-74.683,-74.683) ENVELOPE(163.650,163.650,-74.900,-74.900) ENVELOPE(163.917,163.917,-74.733,-74.733) ENVELOPE(-56.832,-56.832,49.583,49.583) |
geographic |
Antarctic Edmonson Point Evans Cove Gerlache Gerlache Inlet Inexpressible Island Northern Foothills Terra Nova Bay The Beaches |
geographic_facet |
Antarctic Edmonson Point Evans Cove Gerlache Gerlache Inlet Inexpressible Island Northern Foothills Terra Nova Bay The Beaches |
genre |
Antarc* Antarctic Antarctica Ice Shelf Inexpressible Island |
genre_facet |
Antarc* Antarctic Antarctica Ice Shelf Inexpressible Island |
op_relation |
volume:33 firstpage:171 lastpage:193 numberofpages:23 journal:MEMORIE DELLA SOCIETA' GEOLOGICA ITALIANA http://hdl.handle.net/11568/12293 http://www.socgeol.info/Ricerca/pubblicazioni.asp?act=see&type=Memorie&y=1987&v=33&f= |
_version_ |
1789325634288222208 |