| Reference Type | Journal (article/letter/editorial) |
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| Title | Linear sole markings in Pleistocene till |
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| Journal | Geological Magazine |
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| Authors | Westgate, J. A. | Author |
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| Year | 1968 (December) | Volume | 105 |
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| Issue | 6 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800055849Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 250000 | Long-form Identifier | mindat:1:5:250000:7 |
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| GUID | 0 |
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| Full Reference | Westgate, J. A. (1968) Linear sole markings in Pleistocene till. Geological Magazine, 105 (6) 501-505 doi:10.1017/s0016756800055849 |
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| Plain Text | Westgate, J. A. (1968) Linear sole markings in Pleistocene till. Geological Magazine, 105 (6) 501-505 doi:10.1017/s0016756800055849 |
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| In | (1968, December) Geological Magazine Vol. 105 (6) Cambridge University Press (CUP) |
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| Abstract/Notes | SUMMARYCurrent-produced sole markings are not uncommon in the Pleistocene continental till deposits of Alberta, Canada. Groove, striation and prod moulds have all been recognized, characteristically occurring in close association on the undersurface of the till beds. These sedimentary structures provide a rapid means by which local ice-flow directions may be determined. |
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These are possibly similar items as determined by title/reference text matching only.
