| Reference Type | Journal (article/letter/editorial) |
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| Title | Alluvial channel bank-collapse phenomena in the Old Red Sandstone Hitra Group, Western Central Norway |
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| Journal | Geological Magazine |
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| Authors | Bøe, R. | Author |
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| Year | 1988 (January) | Volume | 125 |
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| Issue | 1 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800009365Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 253760 | Long-form Identifier | mindat:1:5:253760:7 |
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| GUID | 0 |
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| Full Reference | Bøe, R. (1988) Alluvial channel bank-collapse phenomena in the Old Red Sandstone Hitra Group, Western Central Norway. Geological Magazine, 125 (1) 51-56 doi:10.1017/s0016756800009365 |
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| Plain Text | Bøe, R. (1988) Alluvial channel bank-collapse phenomena in the Old Red Sandstone Hitra Group, Western Central Norway. Geological Magazine, 125 (1) 51-56 doi:10.1017/s0016756800009365 |
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| In | (1988, January) Geological Magazine Vol. 125 (1) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractThe Old Red Sandstone (ORS) on the island of Hitra forms an approximately 1350 m thick succession of alternating continental mudstones, sandstones and conglomerates of possibly latest Silurian to Devonian age. Within the middle part of this succession, just above a major, scoured surface, a spectacular slump feature was observed. The phenomenon is interpreted as a unit of overbank/channel bank mudstones which, because of undercutting and liquidization, caved into a low sinuosity river channel. The Hitra sequence is the only one in the Norwegian ORS where such phenomena have as yet been identified. |
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