Mass sediment failure and transport features revealed by acoustic techniques, Beringian Margin, Bering Sea, Alaska
Marine Geotechnology
By: P.R. Carlson, Herman A. Karl, and B. D. Edwards
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Abstract
Some of the largest single slide masses, including huge blocks tens of kilometers wide, occur on the rise of the central margin. Sliding of these blocks may have initiated the incision of some of the world's largest submarine canyons. One mass failure, particularly well defined by GLORIA, is 55 km long. This slide and others along the plateau are associated with diapiric-like structures indicative of relatively recent tectonism. -from Authors
Suggested Citation
Carlson, P., Karl, H.A., and Edwards, B.D., 1991, Mass sediment failure and transport features revealed by acoustic techniques, Beringian Margin, Bering Sea, Alaska: Marine Geotechnology, v. 10, no. 1-2, p. 33-51, https://doi.org/10.1080/10641199109379881.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Mass sediment failure and transport features revealed by acoustic techniques, Beringian Margin, Bering Sea, Alaska |
| Series title | Marine Geotechnology |
| DOI | 10.1080/10641199109379881 |
| Volume | 10 |
| Issue | 1-2 |
| Year Published | 1991 |
| Language | English |
| Publisher | Taylor and Francis |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Marine Geotechnology |
| First page | 33 |
| Last page | 51 |