Glacial erosional features - lunate fractures

Lunate fractures have crescent shape in plan view. In cross section, lunate fractures have an asymmetric "V" shape, with shallowly inclined up-glacier side and a steeply-inclined down-glacier side. Glacier flow was, then, from left to right across this surface.

Bibliographic Details
Other Authors: Wojtal, Steven F.
Language:unknown
Published: Oberlin College Library 1993
Subjects:
Surficial geology
Quaternary Geology
Glacial erosion
Fractures
Canada
glacier*
Online Access:http://server15963.contentdm.oclc.org/u?/p15963coll1,1928
id ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/1928
record_format openpolar
spelling ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/1928 2023-05-15T16:22:23+02:00 Glacial erosional features - lunate fractures Wojtal, Steven F. Zone: 17, Easting: 468304, Northing: 5093120 45.99092 -81.40928 Killarney Canada Ontario 1993-07-17 jpeg2000 http://server15963.contentdm.oclc.org/u?/p15963coll1,1928 unknown Oberlin College Library wojtals_pcd_336 http://server15963.contentdm.oclc.org/u?/p15963coll1,1928 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 Fractures 1993 ftohiocolleges 2022-05-18T11:55:50Z Lunate fractures have crescent shape in plan view. In cross section, lunate fractures have an asymmetric "V" shape, with shallowly inclined up-glacier side and a steeply-inclined down-glacier side. Glacier flow was, then, from left to right across this surface. Other/Unknown Material glacier* Five Colleges of Ohio Digital Collections Canada
institution Open Polar
collection Five Colleges of Ohio Digital Collections
op_collection_id ftohiocolleges
language unknown
topic Surficial geology
Quaternary Geology
Glacial erosion
Fractures
spellingShingle Surficial geology
Quaternary Geology
Glacial erosion
Fractures
Glacial erosional features - lunate fractures
topic_facet Surficial geology
Quaternary Geology
Glacial erosion
Fractures
description Lunate fractures have crescent shape in plan view. In cross section, lunate fractures have an asymmetric "V" shape, with shallowly inclined up-glacier side and a steeply-inclined down-glacier side. Glacier flow was, then, from left to right across this surface.
author2 Wojtal, Steven F.
title Glacial erosional features - lunate fractures
title_short Glacial erosional features - lunate fractures
title_full Glacial erosional features - lunate fractures
title_fullStr Glacial erosional features - lunate fractures
title_full_unstemmed Glacial erosional features - lunate fractures
title_sort glacial erosional features - lunate fractures
publisher Oberlin College Library
publishDate 1993
url http://server15963.contentdm.oclc.org/u?/p15963coll1,1928
op_coverage Zone: 17, Easting: 468304, Northing: 5093120
45.99092
-81.40928
Killarney
Canada
Ontario
geographic Canada
geographic_facet Canada
genre glacier*
genre_facet glacier*
op_source 35 mm Kodachrome slide. Oberlin College. Geology Department.
op_relation wojtals_pcd_336
http://server15963.contentdm.oclc.org/u?/p15963coll1,1928
op_rights For research and educational use only. For all other uses please contact the Oberlin College. Geology Department
_version_ 1766010356139819008

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