Terminal Moraines

Image Description from historic lecture booklet: "The thick drift accumulated beneath the end of a valley glacier, or beneath the edge of an ice sheet, is a terminal moraine. At each halt of the receding ice sheet a terminal moraine was built with lobes extending down the valleys. These moraine...

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Bibliographic Details
Format: Still Image
Language:unknown
Published: 1915
Subjects:
Maps
Ice Sheet
Online Access:http://oregondigital.org/catalog/oregondigital:df70dm722
id ftoregondigital:oai:oregondigital.org:osu-scarc/df70dm722
record_format openpolar
spelling ftoregondigital:oai:oregondigital.org:osu-scarc/df70dm722 2023-05-15T16:39:43+02:00 Terminal Moraines 1915; 2010-11-11 image/tiff http://oregondigital.org/catalog/oregondigital:df70dm722 unknown OSU Special Collections & Archives Research Center; Visual Instruction Department Lantern Slides, 1900-1940 (P 217) http://oregondigital.org/catalog/oregondigital:df70dm722 http://rightsstatements.org/vocab/NoC-US/1.0/; OSU Special Collections & Archives Research Center; default Maps Image 1915 ftoregondigital 2022-11-14T22:22:06Z Image Description from historic lecture booklet: "The thick drift accumulated beneath the end of a valley glacier, or beneath the edge of an ice sheet, is a terminal moraine. At each halt of the receding ice sheet a terminal moraine was built with lobes extending down the valleys. These moraines are low, hummocky hills, with enclosed basins, or kettles often occupied by ponds. We have seen these proofs of the great ice sheet of North America that developed during the glacial period. Let us now look at some of the glaciers of the present time." Still Image Ice Sheet Oregon Digital (University of Oregon/Oregon State University)
institution Open Polar
collection Oregon Digital (University of Oregon/Oregon State University)
op_collection_id ftoregondigital
language unknown
topic Maps
spellingShingle Maps
Terminal Moraines
topic_facet Maps
description Image Description from historic lecture booklet: "The thick drift accumulated beneath the end of a valley glacier, or beneath the edge of an ice sheet, is a terminal moraine. At each halt of the receding ice sheet a terminal moraine was built with lobes extending down the valleys. These moraines are low, hummocky hills, with enclosed basins, or kettles often occupied by ponds. We have seen these proofs of the great ice sheet of North America that developed during the glacial period. Let us now look at some of the glaciers of the present time."
format Still Image
title Terminal Moraines
title_short Terminal Moraines
title_full Terminal Moraines
title_fullStr Terminal Moraines
title_full_unstemmed Terminal Moraines
title_sort terminal moraines
publishDate 1915
url http://oregondigital.org/catalog/oregondigital:df70dm722
genre Ice Sheet
genre_facet Ice Sheet
op_relation OSU Special Collections & Archives Research Center; Visual Instruction Department Lantern Slides, 1900-1940 (P 217)
http://oregondigital.org/catalog/oregondigital:df70dm722
op_rights http://rightsstatements.org/vocab/NoC-US/1.0/; OSU Special Collections & Archives Research Center; default
_version_ 1766030046326161408

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