Subsidence and Outbursts - Subsidence and Ground Movement in a Limestone Mine and on the Surface Caused by Longwall Mining in a Coal Bed Below (With Discussion)

The American Institute of Mining, Metallurgical, and Petroleum Engineers
R. Laird Auchmuty
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
24
File Size:
851 KB
Publication Date:
Jan 1, 1931

Abstract

The A. I. M. E. Subcommittee on Bituminous Mining has been trying for several years to secure the information that was collected by the Marquette Cement Manufacturing &. on the subsidence of its property caused by mining coal beneath it. The Marquette company was willing to have these data used, but it was impossible to obtain them because the records had been filed away. About two years ago these records became available and the engineering data presented herewith were compiled from them by R. L. Auchmuty, assisted by L. E. Young, who was connected with the collection of the information. On account of the cost, it is impossible to reproduce all of the data here, although the original information is on file with the records of the Committee on Ground Movement and Subsidence. The accompanying charts show representative and average data and give only the engineering information with enough description to tell how it was obtained. It is hoped that all of those connected with the original case will participate in the discussion that this will bring forth. Howard N. Eavenson, Chairman, Subcommittee on Bituminous Coal Mining. PRobably the most complete records of subsidence due to coal mining in the United States are those compiled by the Marquette Cement Manufacturing Co. at LaSalle, 111. These records, covering a period of more than three years, were compiled and used as evidence during the suit of the Marquette Cement Manufacturing Co. vs. the Oglesby Coal Co. at Oglesby, LaSalle County, Ill., in which the cement company successfully endeavored to stop the coal company from mining under its property. Fig. 1 shows a typical section of the geological formation. The cement company was mining the LaSalle limestone which lies about 125 ft. under the surface. The limestone is 30 to 35 ft. thick and underlain by about 15 ft. of shale. The cement company was mining about 20 ft. of the limestone, and in some places 10 to 12 ft. of the underlying shale, by the room and pillar method. The mining of the limestone always preceded the mining of the shale. The coal company was mining by longwall advance methods the NO. 2 seam of coal 42 in. thick underlying the limestone bed by 435 to 470 ft. The coal mine, a very old one, had largely mined out its original property
Citation

APA: R. Laird Auchmuty  (1931)  Subsidence and Outbursts - Subsidence and Ground Movement in a Limestone Mine and on the Surface Caused by Longwall Mining in a Coal Bed Below (With Discussion)

MLA: R. Laird Auchmuty Subsidence and Outbursts - Subsidence and Ground Movement in a Limestone Mine and on the Surface Caused by Longwall Mining in a Coal Bed Below (With Discussion). The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1931.

Export
Purchase this Article for $25.00

Create a Guest account to purchase this file
- or -
Log in to your existing Guest account