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...

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Main Authors: Houston, Joseph R., Bates, Robert Glenn, Velikanje, Robert S., Wedow, Helmuth, Jr.
Other Authors: Geological Survey (U.S.), U.S. Atomic Energy Commission
Format: Report
Language:English
Published: United States. Government Printing Office. 1958
Subjects:
Online Access:https://digital.library.unt.edu/ark:/67531/metadc304291/
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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
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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/