Post-glacial uplift

Digital Resource Commons Repository

dc.date.accessioned	2012-10-04T15:39:45Z
dc.date.available	2012-10-04T15:39:45Z
dc.date.created	1997-08	en_US
dc.date.issued	2012-10-04
dc.identifier.uri	http://hdl.handle.net/2374.OBE/4564
dc.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.	en_US
dc.relation.isformatof	35 mm Kodachrome slide	en_US
dc.rights	For research and educational use only. For all other uses please contact the Oberlin College Department of Geology.	en_US
dc.title	Post-glacial uplift	en_US
dc.publisher.digital	Oberlin College. Library	en_US
dc.contributor.photographer	Wojtal, Steven F.	en_US
dc.description.notes	PhotoCD scan of original	en_US
dc.coverage.latitude	64.04104	en_US
dc.coverage.longitude	-17.00245	en_US
dc.coverage.UTM	Zone: 28, Easting: 402212, Northing: 7103124	en_US
dc.subject.GeoRef	Surficial Geology, Quaternary Geology	en_US
dc.subject.GeoRef	cleavage, crenulation cleavage	en_US
dc.publisher.OLrepository	Oberlin College. Department of Geology	en_US
dc.coverage.spatialstate	Iceland	en_US
dc.coverage.spatialcity	Skaftafell National Park	en_US