Geology Of The Ross-Adams Uranium-Thorium Deposit, Alaska

The American Institute of Mining, Metallurgical, and Petroleum Engineers
E. M. MacKevett
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
5
File Size:
512 KB
Publication Date:
Jan 9, 1959

Abstract

The only source of uranium ore in Alaska that has been mined commercially is the Ross-Adams de- posit, a gently inclined, fusiform orebody in alkali granite in which uranothorite and uranoan thorianlte are the chief ore minerals. In mode of occurrence, apparent genetic association with the granite, and to a lesser extent in mineralogy, this type of deposit is uncommon. The mine is in the southern part of Prince of Wales Island (Fig. 1) at an altitude of about 950 ft on the southeast flank of Bokan Mountain. A steep unpaved road 1 ¾ miles long leads to the dock on the West Arm of Kendrick Bay, which can be reached by boat or seaplane from Ketchikan, some 35 miles to the northeast.
Citation

APA: E. M. MacKevett  (1959)  Geology Of The Ross-Adams Uranium-Thorium Deposit, Alaska

MLA: E. M. MacKevett Geology Of The Ross-Adams Uranium-Thorium Deposit, Alaska. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1959.

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