Reconnaissance for Radioactive Deposits in Southeastern Alaska, 1952
From abstract: Reconnaissance for radioactive deposits in southeastern Alaska in 1952 was centered in three localities: the northern part of Prince of Wales Island and parts of adjacent islands, the Taku Harbor-Point Astley district, and the Hyder area. Significant concentrations of radioactive mine...
Main Authors: | , , , |
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Other Authors: | , |
Format: | Report |
Language: | English |
Published: |
United States. Government Printing Office.
1958
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Subjects: | |
Online Access: | https://digital.library.unt.edu/ark:/67531/metadc304291/ |
_version_ | 1821689945939509248 |
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author | Houston, Joseph R. Bates, Robert Glenn Velikanje, Robert S. Wedow, Helmuth, Jr. |
author2 | Geological Survey (U.S.) U.S. Atomic Energy Commission |
author_facet | Houston, Joseph R. Bates, Robert Glenn Velikanje, Robert S. Wedow, Helmuth, Jr. |
author_sort | Houston, Joseph R. |
collection | University of North Texas: UNT Digital Library |
description | From abstract: Reconnaissance for radioactive deposits in southeastern Alaska in 1952 was centered in three localities: the northern part of Prince of Wales Island and parts of adjacent islands, the Taku Harbor-Point Astley district, and the Hyder area. Significant concentrations of radioactive minerals were found only in the vicinity of Salmon Bay on the northeastern shore of Prince of Wales Island. In this area radioactive carbonate-hematite veins occur along the coast for about 8 miles. The veins are generally short, irregular, and lenticular, but a few can be traced for more than 300 feet between the low-tide line and the forest cover. The width of the veins normally ranges from less than 1 inch to 2.5 feet; several, however, are 5 to 10 feet wide. |
format | Report |
genre | Prince of Wales Island Alaska |
genre_facet | Prince of Wales Island Alaska |
geographic | Harbor Point Prince of Wales Island Salmon Bay Taku |
geographic_facet | Harbor Point Prince of Wales Island Salmon Bay Taku |
id | ftunivnotexas:info:ark/67531/metadc304291 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-36.683,-36.683,-54.150,-54.150) ENVELOPE(-99.001,-99.001,72.668,72.668) ENVELOPE(164.550,164.550,-77.933,-77.933) ENVELOPE(-133.854,-133.854,59.633,59.633) |
op_collection_id | ftunivnotexas |
op_coverage | United States - Alaska |
op_relation | oclc: 885119821 sudoc: I 19.3:1058-A rep-no: USGS Bulletin 1058-A https://digital.library.unt.edu/ark:/67531/metadc304291/ ark: ark:/67531/metadc304291 |
publishDate | 1958 |
publisher | United States. Government Printing Office. |
record_format | openpolar |
spelling | ftunivnotexas:info:ark/67531/metadc304291 2025-01-17T00:24:43+00:00 Reconnaissance for Radioactive Deposits in Southeastern Alaska, 1952 Mineral resources of Alaska Geological Survey bulletin United States Geological Survey Bulletin 1058-A United States Geological Survey Reports Houston, Joseph R. Bates, Robert Glenn Velikanje, Robert S. Wedow, Helmuth, Jr. Geological Survey (U.S.) U.S. Atomic Energy Commission United States - Alaska 1958 [44] p. : ill., maps, charts 23 cm. Text https://digital.library.unt.edu/ark:/67531/metadc304291/ English eng United States. Government Printing Office. oclc: 885119821 sudoc: I 19.3:1058-A rep-no: USGS Bulletin 1058-A https://digital.library.unt.edu/ark:/67531/metadc304291/ ark: ark:/67531/metadc304291 Mines and mineral resources -- Alaska Radioactive substances -- Alaska Mines and mineral resources Radioactive substances Report 1958 ftunivnotexas 2017-06-10T22:07:38Z From abstract: Reconnaissance for radioactive deposits in southeastern Alaska in 1952 was centered in three localities: the northern part of Prince of Wales Island and parts of adjacent islands, the Taku Harbor-Point Astley district, and the Hyder area. Significant concentrations of radioactive minerals were found only in the vicinity of Salmon Bay on the northeastern shore of Prince of Wales Island. In this area radioactive carbonate-hematite veins occur along the coast for about 8 miles. The veins are generally short, irregular, and lenticular, but a few can be traced for more than 300 feet between the low-tide line and the forest cover. The width of the veins normally ranges from less than 1 inch to 2.5 feet; several, however, are 5 to 10 feet wide. Report Prince of Wales Island Alaska University of North Texas: UNT Digital Library Harbor Point ENVELOPE(-36.683,-36.683,-54.150,-54.150) Prince of Wales Island ENVELOPE(-99.001,-99.001,72.668,72.668) Salmon Bay ENVELOPE(164.550,164.550,-77.933,-77.933) Taku ENVELOPE(-133.854,-133.854,59.633,59.633) |
spellingShingle | Mines and mineral resources -- Alaska Radioactive substances -- Alaska Mines and mineral resources Radioactive substances Houston, Joseph R. Bates, Robert Glenn Velikanje, Robert S. Wedow, Helmuth, Jr. Reconnaissance for Radioactive Deposits in Southeastern Alaska, 1952 |
title | Reconnaissance for Radioactive Deposits in Southeastern Alaska, 1952 |
title_full | Reconnaissance for Radioactive Deposits in Southeastern Alaska, 1952 |
title_fullStr | Reconnaissance for Radioactive Deposits in Southeastern Alaska, 1952 |
title_full_unstemmed | Reconnaissance for Radioactive Deposits in Southeastern Alaska, 1952 |
title_short | Reconnaissance for Radioactive Deposits in Southeastern Alaska, 1952 |
title_sort | reconnaissance for radioactive deposits in southeastern alaska, 1952 |
topic | Mines and mineral resources -- Alaska Radioactive substances -- Alaska Mines and mineral resources Radioactive substances |
topic_facet | Mines and mineral resources -- Alaska Radioactive substances -- Alaska Mines and mineral resources Radioactive substances |
url | https://digital.library.unt.edu/ark:/67531/metadc304291/ |