Glacial erosional landscape - plateau and trough topography

View to the NNE across the glaciated plateau that is the crest of the Long Range Mountains in western Newfoundland. The rock rubble at the surface, called a tor, does not show consistent striations but is thought to develop by rock fracture beneath a slow-moving glacier. The valley in the middle of...

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Bibliographic Details
Other Authors: Wojtal, Steven F.
Language:unknown
Published: Oberlin College Library 1983
Subjects:
Surficial Geology
Quaternary Geology
Glacial erosion
Plateaus
Newfoundland
Ten Mile
Ten Mile Pond
Online Access:http://server15963.contentdm.oclc.org/u?/p15963coll1,1965
id ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/1965
record_format openpolar
spelling ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/1965 2023-05-15T17:16:54+02:00 Glacial erosional landscape - plateau and trough topography Wojtal, Steven F. Zone: 21, Easting: 443334, Northing: 5494352 49.59909 -57.78419 Gros Morne (peak) Newfoundland and Labrador Newfoundland 1983-08 jpeg2000 http://server15963.contentdm.oclc.org/u?/p15963coll1,1965 unknown Oberlin College Library wojtals_pcd_373 http://server15963.contentdm.oclc.org/u?/p15963coll1,1965 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 Glacial erosion Plateaus 1983 ftohiocolleges 2022-05-18T11:55:50Z View to the NNE across the glaciated plateau that is the crest of the Long Range Mountains in western Newfoundland. The rock rubble at the surface, called a tor, does not show consistent striations but is thought to develop by rock fracture beneath a slow-moving glacier. The valley in the middle of the image is Ten Mile Pond, an Icelandic trough carved by an outlet glacier. Other/Unknown Material Newfoundland Five Colleges of Ohio Digital Collections Newfoundland Ten Mile ENVELOPE(-134.370,-134.370,60.166,60.166) Ten Mile Pond ENVELOPE(-57.798,-57.798,49.617,49.617)
institution Open Polar
collection Five Colleges of Ohio Digital Collections
op_collection_id ftohiocolleges
language unknown
topic Surficial Geology
Quaternary Geology
Glacial erosion
Plateaus
spellingShingle Surficial Geology
Quaternary Geology
Glacial erosion
Plateaus
Glacial erosional landscape - plateau and trough topography
topic_facet Surficial Geology
Quaternary Geology
Glacial erosion
Plateaus
description View to the NNE across the glaciated plateau that is the crest of the Long Range Mountains in western Newfoundland. The rock rubble at the surface, called a tor, does not show consistent striations but is thought to develop by rock fracture beneath a slow-moving glacier. The valley in the middle of the image is Ten Mile Pond, an Icelandic trough carved by an outlet glacier.
author2 Wojtal, Steven F.
title Glacial erosional landscape - plateau and trough topography
title_short Glacial erosional landscape - plateau and trough topography
title_full Glacial erosional landscape - plateau and trough topography
title_fullStr Glacial erosional landscape - plateau and trough topography
title_full_unstemmed Glacial erosional landscape - plateau and trough topography
title_sort glacial erosional landscape - plateau and trough topography
publisher Oberlin College Library
publishDate 1983
url http://server15963.contentdm.oclc.org/u?/p15963coll1,1965
op_coverage Zone: 21, Easting: 443334, Northing: 5494352
49.59909
-57.78419
Gros Morne (peak)
Newfoundland and Labrador
Newfoundland
long_lat ENVELOPE(-134.370,-134.370,60.166,60.166)
ENVELOPE(-57.798,-57.798,49.617,49.617)
geographic Newfoundland
Ten Mile
Ten Mile Pond
geographic_facet Newfoundland
Ten Mile
Ten Mile Pond
genre Newfoundland
genre_facet Newfoundland
op_source 35 mm Kodachrome slide. Oberlin College. Geology Department.
op_relation wojtals_pcd_373
http://server15963.contentdm.oclc.org/u?/p15963coll1,1965
op_rights For research and educational use only. For all other uses please contact the Oberlin College. Geology Department
_version_ 1766082277940396032

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