Artic and subarctic environmental analyses utilizing ERTS-1 imagery. Discipline 8: Interpretation techniques development. Subdiscipline C: Classfication and pattern recognition

The author has identified the following significant results. Uncontrolled photo mosaics of ERTS-1 imagery using MSS band 5 and 7 at a scale of 1:1,000,000 were used to make a preliminary surficial geology map in northcentral Alaska. Seven distinct geologic units were recognized, defined, and mapped...

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Main Author: Anderson, D. M.
Format: Other/Unknown Material
Language:unknown
Published: 1973
Subjects:
Online Access:http://hdl.handle.net/2060/19730005631
id ftnasantrs:oai:casi.ntrs.nasa.gov:19730005631
record_format openpolar
spelling ftnasantrs:oai:casi.ntrs.nasa.gov:19730005631 2023-05-15T15:46:59+02:00 Artic and subarctic environmental analyses utilizing ERTS-1 imagery. Discipline 8: Interpretation techniques development. Subdiscipline C: Classfication and pattern recognition Anderson, D. M. Unclassified, Unlimited, Publicly available JAN 1, 1973 application/pdf http://hdl.handle.net/2060/19730005631 unknown Document ID: 19730005631 Accession ID: 73N14358 http://hdl.handle.net/2060/19730005631 No Copyright CASI GEOPHYSICS E72-10370 NASA-CR-129826 1973 ftnasantrs 2019-07-21T11:32:52Z The author has identified the following significant results. Uncontrolled photo mosaics of ERTS-1 imagery using MSS band 5 and 7 at a scale of 1:1,000,000 were used to make a preliminary surficial geology map in northcentral Alaska. Seven distinct geologic units were recognized, defined, and mapped directly on a photo mosaic. Results are closely correlated with published surficial geology maps. Eight MSS images were examined to test utility of ERTS data in studies of coastal processes and stream hydrology, and in the identification and interpretation of geomorphic features throughout Alaska. The feasibility of using ERTS-1 data to map structural lineaments is well illustrated on a mosaic of 8, band 5 MSS images. Along the northern edge of the Brooks Range one lineament can be followed the entire width of the mosaic, a distance of 225 miles. Two nearly parallel lineaments can be seen running along the northern and southern edges of the Schwatka Mountains. About 135 miles south of these two lineaments another series located in the Chitanana River region can be followed for 45 miles. These lineaments appear to be faults, and it is interesting to note that the Yukon River parallels these and appears to be structurally controlled. Other/Unknown Material Brooks Range Subarctic Yukon river Alaska Yukon NASA Technical Reports Server (NTRS) Yukon
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic GEOPHYSICS
spellingShingle GEOPHYSICS
Anderson, D. M.
Artic and subarctic environmental analyses utilizing ERTS-1 imagery. Discipline 8: Interpretation techniques development. Subdiscipline C: Classfication and pattern recognition
topic_facet GEOPHYSICS
description The author has identified the following significant results. Uncontrolled photo mosaics of ERTS-1 imagery using MSS band 5 and 7 at a scale of 1:1,000,000 were used to make a preliminary surficial geology map in northcentral Alaska. Seven distinct geologic units were recognized, defined, and mapped directly on a photo mosaic. Results are closely correlated with published surficial geology maps. Eight MSS images were examined to test utility of ERTS data in studies of coastal processes and stream hydrology, and in the identification and interpretation of geomorphic features throughout Alaska. The feasibility of using ERTS-1 data to map structural lineaments is well illustrated on a mosaic of 8, band 5 MSS images. Along the northern edge of the Brooks Range one lineament can be followed the entire width of the mosaic, a distance of 225 miles. Two nearly parallel lineaments can be seen running along the northern and southern edges of the Schwatka Mountains. About 135 miles south of these two lineaments another series located in the Chitanana River region can be followed for 45 miles. These lineaments appear to be faults, and it is interesting to note that the Yukon River parallels these and appears to be structurally controlled.
format Other/Unknown Material
author Anderson, D. M.
author_facet Anderson, D. M.
author_sort Anderson, D. M.
title Artic and subarctic environmental analyses utilizing ERTS-1 imagery. Discipline 8: Interpretation techniques development. Subdiscipline C: Classfication and pattern recognition
title_short Artic and subarctic environmental analyses utilizing ERTS-1 imagery. Discipline 8: Interpretation techniques development. Subdiscipline C: Classfication and pattern recognition
title_full Artic and subarctic environmental analyses utilizing ERTS-1 imagery. Discipline 8: Interpretation techniques development. Subdiscipline C: Classfication and pattern recognition
title_fullStr Artic and subarctic environmental analyses utilizing ERTS-1 imagery. Discipline 8: Interpretation techniques development. Subdiscipline C: Classfication and pattern recognition
title_full_unstemmed Artic and subarctic environmental analyses utilizing ERTS-1 imagery. Discipline 8: Interpretation techniques development. Subdiscipline C: Classfication and pattern recognition
title_sort artic and subarctic environmental analyses utilizing erts-1 imagery. discipline 8: interpretation techniques development. subdiscipline c: classfication and pattern recognition
publishDate 1973
url http://hdl.handle.net/2060/19730005631
op_coverage Unclassified, Unlimited, Publicly available
geographic Yukon
geographic_facet Yukon
genre Brooks Range
Subarctic
Yukon river
Alaska
Yukon
genre_facet Brooks Range
Subarctic
Yukon river
Alaska
Yukon
op_source CASI
op_relation Document ID: 19730005631
Accession ID: 73N14358
http://hdl.handle.net/2060/19730005631
op_rights No Copyright
_version_ 1766381793445937152