Brief description
The formation of incised valleys on continental shelves is generally attributed to fluvial erosion under low sea level conditions. However, there are exceptions. A multibeam sonar survey at the northern end of Australia's Great Barrier Reef, adjacent to the southern edge of the Gulf of Papua, mapped a shelf valley system up to 220 m deep that extends for more than 90 km across the continental shelf. Based on observations, we propose a new conceptual model for the formation of tidally incised shelf valleys.Lineage
Maintenance and Update Frequency: unknown
Statement: Unknown
Issued: 2005
text: westlimit=142; southlimit=-11.0; eastlimit=146; northlimit=-7.0
Subjects
AU-QLD |
Earth Sciences |
External Publication |
Published_External |
Scientific Journal Paper |
geoscientificInformation |
marine |
marine survey |
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Other Information
Link to Publication
Identifiers
- DOI : 10.1016/J.MARGEO.2005.06.019
- URI : pid.geoscience.gov.au/dataset/ga/69131
- global : a05f7892-ec08-7506-e044-00144fdd4fa6