Surface Subsidence at the Henderson Mine

The American Institute of Mining, Metallurgical, and Petroleum Engineers
Daniel Stewart Richard Rein David Firewick
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
10
File Size:
484 KB
Publication Date:
Jan 1, 1984

Abstract

Panel caving of the Henderson orebody began in August, 1976. Fifty months later, on September 10, 1980, the cave zone appeared on surface as a steep-walled cavity positioned directly above the initial cave area. Although surface survey data revealed the development of a slight depression over the production area, surface inspection by geologists, three days prior to breach- ing, resulted in no evidence of impending glory-hole development. Geologic factors such as rock contacts and alteration-zone boundaries had little influence on the location of the initial glory hole. Since initial breakthrough, the glory-hole shape and growth have not directionally followed caveline advance because of topography and faulting. Based on periodic data, mine production has resulted in immediate growth of the Henderson glory hole.
Citation

APA: Daniel Stewart Richard Rein David Firewick  (1984)  Surface Subsidence at the Henderson Mine

MLA: Daniel Stewart Richard Rein David Firewick Surface Subsidence at the Henderson Mine. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1984.

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