MRGID |
http://marineregions.org/mrgid/33754 |
Status |
Proposed standard  |
Name |
Language |
Name |
Name source |
English | Faroe-Shetland Channel Drift 1 | M.C. Akhurst, D.A.V. Stow, M.S. Stoker (2002). Late Quaternary glacigenic contourite, debris flow and turbidite process interaction in the Faroe–Shetland Channel, NW Europe continental margin. ,in: D.A.V. Stow, C.J. Pudsey, J.A. Howe, J.-C. Faugères, A.R. Viana (Eds.), Deep-water Contourite Systems: Modern Drifts and Ancient Series, Seismic and Sedimentary Characteristics, Geological Society, London, Memoirs, 22 (2002), pp. 73–84 (look up in IMIS) |
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PlaceType |
Drift |
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Latitude |
60° 45' 36.5" N (60.7601305°) |
Longitude |
4° 31' 42.5" W (-4.52846°) |
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Source |
M.C. Akhurst, D.A.V. Stow, M.S. Stoker (2002). Late Quaternary glacigenic contourite, debris flow and turbidite process interaction in the Faroe–Shetland Channel, NW Europe continental margin. ,in: D.A.V. Stow, C.J. Pudsey, J.A. Howe, J.-C. Faugères, A.R. Viana (Eds.), Deep-water Contourite Systems: Modern Drifts and Ancient Series, Seismic and Sedimentary Characteristics, Geological Society, London, Memoirs, 22 (2002), pp. 73–84 (look up in IMIS) |
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Notes |
Maximum age (en): Plio-Pleistocene |
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Drift type (en): Elongated Mounded |
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Prevailing contourite type (en): Sandy-muddy |
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Relations |
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Map |
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Edit history |
Last edited on 2014-08-06 13:50:51 by Velleman Jules
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