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.
| Other Authors: | |
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| Language: | unknown |
| Published: |
Oberlin College Library
1997
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| Subjects: | |
| Online Access: | http://server15963.contentdm.oclc.org/u?/p15963coll1,2000 |
| _version_ | 1829953910571270144 |
|---|---|
| author2 | Wojtal, Steven F. |
| collection | Five Colleges of Ohio Digital Collections |
| 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. |
| genre | Ice cap Iceland |
| genre_facet | Ice cap Iceland |
| geographic | Skaftafell |
| geographic_facet | Skaftafell |
| id | ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/2000 |
| institution | Open Polar |
| language | unknown |
| long_lat | ENVELOPE(-16.940,-16.940,63.999,63.999) |
| op_collection_id | ftohiocolleges |
| op_coverage | Zone: 28, Easting: 402212, Northing: 7103124 64.04104 -17.00245 Iceland Skaftafell National Park |
| 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 |
| op_source | 35 mm Kodachrome slide. Oberlin College. Geology Department. |
| publishDate | 1997 |
| publisher | Oberlin College Library |
| record_format | openpolar |
| spelling | ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/2000 2025-04-20T14:38:32+00:00 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 2025-03-26T04:24:37Z 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) |
| spellingShingle | Surficial Geology Quaternary Geology Cleavage Slip cleavage Post-glacial uplift |
| title | Post-glacial uplift |
| title_full | Post-glacial uplift |
| title_fullStr | Post-glacial uplift |
| title_full_unstemmed | Post-glacial uplift |
| title_short | Post-glacial uplift |
| title_sort | post-glacial uplift |
| topic | Surficial Geology Quaternary Geology Cleavage Slip cleavage |
| topic_facet | Surficial Geology Quaternary Geology Cleavage Slip cleavage |
| url | http://server15963.contentdm.oclc.org/u?/p15963coll1,2000 |