Post-glacial uplift

The steep cliff resulted from erosion by waves along the ocean shore. This cliff is currently found several miles from the shoreline. It was eroded immediately following the melting of the ice cap and was later raised significantly above sea level by post-glacial rebound.

Bibliographic Details
Other Authors: Wojtal, Steven F.
Language:unknown
Published: Oberlin College Library 1997
Subjects:
Surficial Geology
Quaternary Geology
Cleavage
Slip cleavage
Skaftafell
Ice cap
Iceland
Online Access:http://server15963.contentdm.oclc.org/u?/p15963coll1,2000
id ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/2000
record_format openpolar
spelling ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/2000 2023-05-15T16:38:08+02:00 Post-glacial uplift Wojtal, Steven F. Zone: 28, Easting: 402212, Northing: 7103124 64.04104 -17.00245 Iceland Skaftafell National Park 1997-08 jpeg2000 http://server15963.contentdm.oclc.org/u?/p15963coll1,2000 unknown Oberlin College Library wojtals_pcd_408 http://server15963.contentdm.oclc.org/u?/p15963coll1,2000 For research and educational use only. For all other uses please contact the Oberlin College. Geology Department 35 mm Kodachrome slide. Oberlin College. Geology Department. Surficial Geology Quaternary Geology Cleavage Slip cleavage 1997 ftohiocolleges 2022-05-18T11:55:50Z The steep cliff resulted from erosion by waves along the ocean shore. This cliff is currently found several miles from the shoreline. It was eroded immediately following the melting of the ice cap and was later raised significantly above sea level by post-glacial rebound. Other/Unknown Material Ice cap Iceland Five Colleges of Ohio Digital Collections Skaftafell ENVELOPE(-16.940,-16.940,63.999,63.999)
institution Open Polar
collection Five Colleges of Ohio Digital Collections
op_collection_id ftohiocolleges
language unknown
topic Surficial Geology
Quaternary Geology
Cleavage
Slip cleavage
spellingShingle Surficial Geology
Quaternary Geology
Cleavage
Slip cleavage
Post-glacial uplift
topic_facet Surficial Geology
Quaternary Geology
Cleavage
Slip cleavage
description The steep cliff resulted from erosion by waves along the ocean shore. This cliff is currently found several miles from the shoreline. It was eroded immediately following the melting of the ice cap and was later raised significantly above sea level by post-glacial rebound.
author2 Wojtal, Steven F.
title Post-glacial uplift
title_short Post-glacial uplift
title_full Post-glacial uplift
title_fullStr Post-glacial uplift
title_full_unstemmed Post-glacial uplift
title_sort post-glacial uplift
publisher Oberlin College Library
publishDate 1997
url http://server15963.contentdm.oclc.org/u?/p15963coll1,2000
op_coverage Zone: 28, Easting: 402212, Northing: 7103124
64.04104
-17.00245
Iceland
Skaftafell National Park
long_lat ENVELOPE(-16.940,-16.940,63.999,63.999)
geographic Skaftafell
geographic_facet Skaftafell
genre Ice cap
Iceland
genre_facet Ice cap
Iceland
op_source 35 mm Kodachrome slide. Oberlin College. Geology Department.
op_relation wojtals_pcd_408
http://server15963.contentdm.oclc.org/u?/p15963coll1,2000
op_rights For research and educational use only. For all other uses please contact the Oberlin College. Geology Department
_version_ 1766028425204596736

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