Fractal analysis of Laurentide glacial boundaries in the conterminous United States : an honors thesis (HONRS 499)

The Wisconsinan event of the Laurentide Ice Sheet covered a wide fetch of land from New Jersey to Montana in the conterminous United States. The contact it created between new tills and older units formed a boundary that exhibits irregular curves with many scales of wandering. This boundary crosses...

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Main Author: Adams, Byron A.
Other Authors: Rice-Snow, Robin S.
Format: Other/Unknown Material
Language:unknown
Published: 2005
Subjects:
Online Access:http://cardinalscholar.bsu.edu/handle/handle/189234
http://liblink.bsu.edu/catkey/1338443
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spelling ftballstcs:oai:cardinalscholar.bsu.edu:handle/189234 2023-05-15T16:41:21+02:00 Fractal analysis of Laurentide glacial boundaries in the conterminous United States : an honors thesis (HONRS 499) Adams, Byron A. Rice-Snow, Robin S. 2005 iii, 45 p. : ill. 30 cm. http://cardinalscholar.bsu.edu/handle/handle/189234 http://liblink.bsu.edu/catkey/1338443 unknown A-306 http://cardinalscholar.bsu.edu/handle/handle/189234 http://liblink.bsu.edu/catkey/1338443 Virtual Press Geology Undergraduate senior honors thesis 2005 ftballstcs 2022-05-30T13:35:17Z The Wisconsinan event of the Laurentide Ice Sheet covered a wide fetch of land from New Jersey to Montana in the conterminous United States. The contact it created between new tills and older units formed a boundary that exhibits irregular curves with many scales of wandering. This boundary crosses five physiographic provinces: the Piedmont, Valley and Ridge, Appalachian Plateau, Central Lowlands and Great Plains Provinces. We have performed divider analyses on the Wisconsinan maximum advance to correlate plan-view geometry of the boundary with local geomorphology. In addition to dividing the boundary into sections according to province, large provinces were also split up into smaller segments to reduce the issue of scale discrepancy. A total of 37 line segments were created including: five of the whole province sections and 32 subsequent divisions.All sections of this boundary of maximum advance were found to have fractal character. Richardson plots showed at least one area of linearity and in some cases two. These linear areas led to calculated fractal dimension (D) values. The ranges of these D values are quite broad. The fine scales showed values of 1.01-1.17 and the coarse scales had values of 1.01-1.32. The Appalachian Plateau Province shows a fractal character pattern that is different from that of most other plots, where the amount of wandering decreases in the coarse scales. The subsections of this area also show D values that occur over similar ranges of step lengths. These studies are significant, as they may imply an active scale-specific process in the formation of these boundary segments. Honors College Thesis (B.?.) Other/Unknown Material Ice Sheet Ball State University: Cardinal Scholar Plateau Central ENVELOPE(69.577,69.577,-49.389,-49.389)
institution Open Polar
collection Ball State University: Cardinal Scholar
op_collection_id ftballstcs
language unknown
topic Geology
spellingShingle Geology
Adams, Byron A.
Fractal analysis of Laurentide glacial boundaries in the conterminous United States : an honors thesis (HONRS 499)
topic_facet Geology
description The Wisconsinan event of the Laurentide Ice Sheet covered a wide fetch of land from New Jersey to Montana in the conterminous United States. The contact it created between new tills and older units formed a boundary that exhibits irregular curves with many scales of wandering. This boundary crosses five physiographic provinces: the Piedmont, Valley and Ridge, Appalachian Plateau, Central Lowlands and Great Plains Provinces. We have performed divider analyses on the Wisconsinan maximum advance to correlate plan-view geometry of the boundary with local geomorphology. In addition to dividing the boundary into sections according to province, large provinces were also split up into smaller segments to reduce the issue of scale discrepancy. A total of 37 line segments were created including: five of the whole province sections and 32 subsequent divisions.All sections of this boundary of maximum advance were found to have fractal character. Richardson plots showed at least one area of linearity and in some cases two. These linear areas led to calculated fractal dimension (D) values. The ranges of these D values are quite broad. The fine scales showed values of 1.01-1.17 and the coarse scales had values of 1.01-1.32. The Appalachian Plateau Province shows a fractal character pattern that is different from that of most other plots, where the amount of wandering decreases in the coarse scales. The subsections of this area also show D values that occur over similar ranges of step lengths. These studies are significant, as they may imply an active scale-specific process in the formation of these boundary segments. Honors College Thesis (B.?.)
author2 Rice-Snow, Robin S.
format Other/Unknown Material
author Adams, Byron A.
author_facet Adams, Byron A.
author_sort Adams, Byron A.
title Fractal analysis of Laurentide glacial boundaries in the conterminous United States : an honors thesis (HONRS 499)
title_short Fractal analysis of Laurentide glacial boundaries in the conterminous United States : an honors thesis (HONRS 499)
title_full Fractal analysis of Laurentide glacial boundaries in the conterminous United States : an honors thesis (HONRS 499)
title_fullStr Fractal analysis of Laurentide glacial boundaries in the conterminous United States : an honors thesis (HONRS 499)
title_full_unstemmed Fractal analysis of Laurentide glacial boundaries in the conterminous United States : an honors thesis (HONRS 499)
title_sort fractal analysis of laurentide glacial boundaries in the conterminous united states : an honors thesis (honrs 499)
publishDate 2005
url http://cardinalscholar.bsu.edu/handle/handle/189234
http://liblink.bsu.edu/catkey/1338443
long_lat ENVELOPE(69.577,69.577,-49.389,-49.389)
geographic Plateau Central
geographic_facet Plateau Central
genre Ice Sheet
genre_facet Ice Sheet
op_source Virtual Press
op_relation A-306
http://cardinalscholar.bsu.edu/handle/handle/189234
http://liblink.bsu.edu/catkey/1338443
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