Post-Last Glacial Maximum Thickness
The thickness maps of the Post-LGM deposits can be used to identify areas where i) pre-Holocene submerged landscapes are exposed at or close to the seabed, or, ii) where there is high potential for preservation of early Holocene landscape features such as submerged river valleys or coasts. Contours are presented as depth (metres) below the present seafloor or the base of the post-LGM sedimentary cover. In glaciated regions, the thickness of the Holocene is used.
Data and resources
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A general description of EMODnet Geology and the accessible data.HTML Open
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Web map service for Post-Last Glacial Maximum ThicknessHTML Open
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wmsWMS Open
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HTML Open
Additional information
| Date (publication) | 2024-10-29 |
|---|---|
| Status | onGoing |
| Update frequency | asNeeded |
| Metadata language | en |
| License | Creative Commons Attribution 4.0 |
| Source metadata | ISO 19115 XML |
| Last updated | 2026-11-04 |
| Created | 2026-11-04 |
| API | package_show |