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- df77e4c7-0b22-4f14-afa5-11b1d335a315 definition "Post-glacial rebound (sometimes called continental rebound, glacial isostatic adjustment) is the rise of land masses that were depressed by the huge weight of ice sheets during the last glacial period, through a process known as isostasy. It affects northern Europe (especially Scotland, Fennoscandia and northern Denmark), Siberia, Canada, the Great Lakes of Canada and the United States, parts of Patagonia, and Antarctica." @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 id "1662650" @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 path_id 1eb0ea0a-312c-4d74-8d42-6f1ad758f999 @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 path_id 6a426480-c58f-4b6b-8e35-0975b7f6edb5 @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 path_id b409a30b-0e3f-4592-bec9-7d371797b4a9 @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 path_id d35b9ba5-d018-48a5-8f0d-92b9c55b3279 @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 path_id e9f67a66-e9fc-435c-b720-ae32a2c3d8f5 @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 path_label "EARTH SCIENCE" @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 path_label "GEOMORPHIC LANDFORMS/PROCESSES" @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 path_label "GLACIAL PROCESSES" @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 path_label "LAND SURFACE" @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 path_label "Science Keywords" @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 prefLabel "CRUST REBOUND" @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 reference "PhysicalGeography.net" @default.
- df77e4c7-0b22-4f14-afa5-11b1d335a315 tag "Science Keywords" @default.