PERMAFROST IN THE KNOB LAKE IRON MIMNG REGION
This paper presents in outline the programme of exploration used in mapping permafros t in the Knob Lake (Schefferville, P. Q.) mine region, and the techniques used by the I ron Ore Company of Canada (IOCC) to overcome problems of mining in permafrost a r e a s. Pe rmaf ros t in central Labrador-Ung...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.564.7934 2023-05-15T17:56:55+02:00 PERMAFROST IN THE KNOB LAKE IRON MIMNG REGION B. G. Thom The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.7934 http://pubs.aina.ucalgary.ca/cpc/cpc3-9.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.7934 http://pubs.aina.ucalgary.ca/cpc/cpc3-9.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/cpc/cpc3-9.pdf text ftciteseerx 2016-01-08T12:12:45Z This paper presents in outline the programme of exploration used in mapping permafros t in the Knob Lake (Schefferville, P. Q.) mine region, and the techniques used by the I ron Ore Company of Canada (IOCC) to overcome problems of mining in permafrost a r e a s. Pe rmaf ros t in central Labrador-Ungava occurs a s discontinuous bodies of various shapes and s izes within the upland t e r r a i n above approximately 2200 feet in elevation. In most mine a r e a s of tne Knob Lake dis t r ic t, frozen ground is absent. At two locations shown in F igure 1, F e r r i m a n and Timmins, permafrost presents, however, a problem to mining. The active layer (seasonal f reezing and thawing) va r i e s f r o m 5 to 10 feet i n depth, and i f there i s no permafrost below that layer then the groundwater c irculates f reely in aquifers. Par t icu lar ly under exposed windswept r idges, f r e e of t r e e cover, permafros t o r perennially frozen ground can extend to depths of 253 feet. These perma-f r o s t bodies a r e commonly elliptical in cross-section and a r e elongated Text permafrost Unknown Canada Knob Lake ENVELOPE(-115.168,-115.168,64.317,64.317) The Knob ENVELOPE(-131.721,-131.721,56.850,56.850) |
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Open Polar |
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ftciteseerx |
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English |
description |
This paper presents in outline the programme of exploration used in mapping permafros t in the Knob Lake (Schefferville, P. Q.) mine region, and the techniques used by the I ron Ore Company of Canada (IOCC) to overcome problems of mining in permafrost a r e a s. Pe rmaf ros t in central Labrador-Ungava occurs a s discontinuous bodies of various shapes and s izes within the upland t e r r a i n above approximately 2200 feet in elevation. In most mine a r e a s of tne Knob Lake dis t r ic t, frozen ground is absent. At two locations shown in F igure 1, F e r r i m a n and Timmins, permafrost presents, however, a problem to mining. The active layer (seasonal f reezing and thawing) va r i e s f r o m 5 to 10 feet i n depth, and i f there i s no permafrost below that layer then the groundwater c irculates f reely in aquifers. Par t icu lar ly under exposed windswept r idges, f r e e of t r e e cover, permafros t o r perennially frozen ground can extend to depths of 253 feet. These perma-f r o s t bodies a r e commonly elliptical in cross-section and a r e elongated |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
B. G. Thom |
spellingShingle |
B. G. Thom PERMAFROST IN THE KNOB LAKE IRON MIMNG REGION |
author_facet |
B. G. Thom |
author_sort |
B. G. Thom |
title |
PERMAFROST IN THE KNOB LAKE IRON MIMNG REGION |
title_short |
PERMAFROST IN THE KNOB LAKE IRON MIMNG REGION |
title_full |
PERMAFROST IN THE KNOB LAKE IRON MIMNG REGION |
title_fullStr |
PERMAFROST IN THE KNOB LAKE IRON MIMNG REGION |
title_full_unstemmed |
PERMAFROST IN THE KNOB LAKE IRON MIMNG REGION |
title_sort |
permafrost in the knob lake iron mimng region |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.7934 http://pubs.aina.ucalgary.ca/cpc/cpc3-9.pdf |
long_lat |
ENVELOPE(-115.168,-115.168,64.317,64.317) ENVELOPE(-131.721,-131.721,56.850,56.850) |
geographic |
Canada Knob Lake The Knob |
geographic_facet |
Canada Knob Lake The Knob |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
http://pubs.aina.ucalgary.ca/cpc/cpc3-9.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.7934 http://pubs.aina.ucalgary.ca/cpc/cpc3-9.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766165229556727808 |