Post-glacial uplift
View downstream from the Skogafoss. Skogafoss occurs at a scarp along the southern edge of a glaciated plateau; the base of the waterfall is a wave cut terrace extending to the ocean. The scarp resulted from erosion by waves along the ocean shore. This scarp is currently found several miles from the...
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| Language: | unknown |
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Oberlin College Library
1997
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| Online Access: | http://server15963.contentdm.oclc.org/u?/p15963coll1,2001 |
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ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/2001 |
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| record_format |
openpolar |
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ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/2001 2023-05-15T16:38:10+02:00 Post-glacial uplift Wojtal, Steven F. Zone: 27, Easting: 573576, Northing: 7045113 63.52659 -19.52064 Near Skogafoss Iceland Skogar 1997-08 jpeg2000 http://server15963.contentdm.oclc.org/u?/p15963coll1,2001 unknown Oberlin College Library wojtals_pcd_409 http://server15963.contentdm.oclc.org/u?/p15963coll1,2001 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 View downstream from the Skogafoss. Skogafoss occurs at a scarp along the southern edge of a glaciated plateau; the base of the waterfall is a wave cut terrace extending to the ocean. The scarp resulted from erosion by waves along the ocean shore. This scarp 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. Compare with image 410. Other/Unknown Material Ice cap Iceland Five Colleges of Ohio Digital Collections Skogar ENVELOPE(-19.374,-19.374,63.629,63.629) |
| 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 |
View downstream from the Skogafoss. Skogafoss occurs at a scarp along the southern edge of a glaciated plateau; the base of the waterfall is a wave cut terrace extending to the ocean. The scarp resulted from erosion by waves along the ocean shore. This scarp 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. Compare with image 410. |
| 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?/p15963coll1,2001 |
| op_coverage |
Zone: 27, Easting: 573576, Northing: 7045113 63.52659 -19.52064 Near Skogafoss Iceland Skogar |
| long_lat |
ENVELOPE(-19.374,-19.374,63.629,63.629) |
| geographic |
Skogar |
| geographic_facet |
Skogar |
| genre |
Ice cap Iceland |
| genre_facet |
Ice cap Iceland |
| op_source |
35 mm Kodachrome slide. Oberlin College. Geology Department. |
| op_relation |
wojtals_pcd_409 http://server15963.contentdm.oclc.org/u?/p15963coll1,2001 |
| op_rights |
For research and educational use only. For all other uses please contact the Oberlin College. Geology Department |
| _version_ |
1766028458747494400 |