Problems Associated with Soils Stabilization. in the Vicinity of Point Barrow, Alaska

Point Barrow is located in the northernmost extremity of the Arctic Coastal Plain (Figure 1). The coastal plain is an undulating surface of low relief, the major relief being in the vicinity of the major northflowing rivers. The general lack of relief is largely due to the fact that the area is a re...

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Main Authors: O'Sullivan, J. B., Hussey, K. M.
Format: Text
Language:English
Published: UNI ScholarWorks 1957
Subjects:
Online Access:https://scholarworks.uni.edu/pias/vol64/iss1/45
https://scholarworks.uni.edu/context/pias/article/2818/viewcontent/45_Problems_Associated_with_Soils_Stabilization.pdf
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spelling ftunortherniowa:oai:scholarworks.uni.edu:pias-2818 2023-08-20T04:04:15+02:00 Problems Associated with Soils Stabilization. in the Vicinity of Point Barrow, Alaska O'Sullivan, J. B. Hussey, K. M. 1957-01-01T08:00:00Z application/pdf https://scholarworks.uni.edu/pias/vol64/iss1/45 https://scholarworks.uni.edu/context/pias/article/2818/viewcontent/45_Problems_Associated_with_Soils_Stabilization.pdf en eng UNI ScholarWorks https://scholarworks.uni.edu/pias/vol64/iss1/45 https://scholarworks.uni.edu/context/pias/article/2818/viewcontent/45_Problems_Associated_with_Soils_Stabilization.pdf ©1957 Iowa Academy of Science, Inc. Proceedings of the Iowa Academy of Science text 1957 ftunortherniowa 2023-07-29T22:46:58Z Point Barrow is located in the northernmost extremity of the Arctic Coastal Plain (Figure 1). The coastal plain is an undulating surface of low relief, the major relief being in the vicinity of the major northflowing rivers. The general lack of relief is largely due to the fact that the area is a recently elevated segment of the continental shelf, and thus, it has the low relief characteristics of most recently emerged coastal plains. Text Arctic Barrow Point Barrow Alaska University of Northern Iowa: UNI ScholarWorks Arctic
institution Open Polar
collection University of Northern Iowa: UNI ScholarWorks
op_collection_id ftunortherniowa
language English
description Point Barrow is located in the northernmost extremity of the Arctic Coastal Plain (Figure 1). The coastal plain is an undulating surface of low relief, the major relief being in the vicinity of the major northflowing rivers. The general lack of relief is largely due to the fact that the area is a recently elevated segment of the continental shelf, and thus, it has the low relief characteristics of most recently emerged coastal plains.
format Text
author O'Sullivan, J. B.
Hussey, K. M.
spellingShingle O'Sullivan, J. B.
Hussey, K. M.
Problems Associated with Soils Stabilization. in the Vicinity of Point Barrow, Alaska
author_facet O'Sullivan, J. B.
Hussey, K. M.
author_sort O'Sullivan, J. B.
title Problems Associated with Soils Stabilization. in the Vicinity of Point Barrow, Alaska
title_short Problems Associated with Soils Stabilization. in the Vicinity of Point Barrow, Alaska
title_full Problems Associated with Soils Stabilization. in the Vicinity of Point Barrow, Alaska
title_fullStr Problems Associated with Soils Stabilization. in the Vicinity of Point Barrow, Alaska
title_full_unstemmed Problems Associated with Soils Stabilization. in the Vicinity of Point Barrow, Alaska
title_sort problems associated with soils stabilization. in the vicinity of point barrow, alaska
publisher UNI ScholarWorks
publishDate 1957
url https://scholarworks.uni.edu/pias/vol64/iss1/45
https://scholarworks.uni.edu/context/pias/article/2818/viewcontent/45_Problems_Associated_with_Soils_Stabilization.pdf
geographic Arctic
geographic_facet Arctic
genre Arctic
Barrow
Point Barrow
Alaska
genre_facet Arctic
Barrow
Point Barrow
Alaska
op_source Proceedings of the Iowa Academy of Science
op_relation https://scholarworks.uni.edu/pias/vol64/iss1/45
https://scholarworks.uni.edu/context/pias/article/2818/viewcontent/45_Problems_Associated_with_Soils_Stabilization.pdf
op_rights ©1957 Iowa Academy of Science, Inc.
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