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Gendzwill, D. J., Hajnal, Z. (1971) Seismic Investigation of the Crater Lake Collapse Structure in Southeastern Saskatchewan. Canadian Journal of Earth Sciences, 8 (12) 1514-1524 doi:10.1139/e71-141

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Reference TypeJournal (article/letter/editorial)
TitleSeismic Investigation of the Crater Lake Collapse Structure in Southeastern Saskatchewan
JournalCanadian Journal of Earth Sciences
AuthorsGendzwill, D. J.Author
Hajnal, Z.Author
Year1971 (December 1)Volume8
Issue12
PublisherCanadian Science Publishing
DOIdoi:10.1139/e71-141Search in ResearchGate
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Mindat Ref. ID472922Long-form Identifiermindat:1:5:472922:2
GUID0
Full ReferenceGendzwill, D. J., Hajnal, Z. (1971) Seismic Investigation of the Crater Lake Collapse Structure in Southeastern Saskatchewan. Canadian Journal of Earth Sciences, 8 (12) 1514-1524 doi:10.1139/e71-141
Plain TextGendzwill, D. J., Hajnal, Z. (1971) Seismic Investigation of the Crater Lake Collapse Structure in Southeastern Saskatchewan. Canadian Journal of Earth Sciences, 8 (12) 1514-1524 doi:10.1139/e71-141
In(1971, December) Canadian Journal of Earth Sciences Vol. 8 (12) Canadian Science Publishing
Abstract/Notes A detailed survey was carried out near Crater Lake, an unusual, circular depression 800 ft. (244 m) across, about 20 miles (~32 km) south of Yorkton, Saskatchewan. In-line and offset profiling with threefold subsurface coverage were used to outline this very small structure. The seismograms show a deep, narrow structural disturbance beneath the lake. This is interpreted as a chimney filled with breccia, which had collapsed into a solution cavern in the Prairie Evaporite salt over 3000 ft (914 m) below surface. About 125 ft (38 m) of salt has been removed from an area about 800 ft (244 m) in diameter. The chimney is about 350 ft (107 m) in mini mum diameter. Solution-collapse features are common in Saskatchewan, but previously none has been described that is so small or so well delineated on the surface. In northern Michigan, however, structures that are thought to be similar occur as columns of indurated breccia exposed by differential erosion.Small collapse structures present peculiar hazards to potash mining because they are very difficult to detect. There is also danger to roads and buildings should subsidence or sudden collapse occur in the future.


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