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- c06e70c0-616c-44f2-a884-ad0252e29e37 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.
- c06e70c0-616c-44f2-a884-ad0252e29e37 id "1662259" @default.
- c06e70c0-616c-44f2-a884-ad0252e29e37 path_id 1eb0ea0a-312c-4d74-8d42-6f1ad758f999 @default.
- c06e70c0-616c-44f2-a884-ad0252e29e37 path_id 2b9ad978-d986-4d63-b477-0f5efc8ace72 @default.
- c06e70c0-616c-44f2-a884-ad0252e29e37 path_id b5cb1fab-7281-478f-bb3b-ff04f900b3fc @default.
- c06e70c0-616c-44f2-a884-ad0252e29e37 path_id d7b62912-5970-46b1-be45-6a603c9a6979 @default.
- c06e70c0-616c-44f2-a884-ad0252e29e37 path_id e9f67a66-e9fc-435c-b720-ae32a2c3d8f5 @default.
- c06e70c0-616c-44f2-a884-ad0252e29e37 path_label "EARTH SCIENCE" @default.
- c06e70c0-616c-44f2-a884-ad0252e29e37 path_label "GEOMORPHIC LANDFORMS/PROCESSES" @default.
- c06e70c0-616c-44f2-a884-ad0252e29e37 path_label "GLACIAL PROCESSES" @default.
- c06e70c0-616c-44f2-a884-ad0252e29e37 path_label "SOLID EARTH" @default.
- c06e70c0-616c-44f2-a884-ad0252e29e37 path_label "Science Keywords" @default.
- c06e70c0-616c-44f2-a884-ad0252e29e37 prefLabel "CRUST REBOUND" @default.
- c06e70c0-616c-44f2-a884-ad0252e29e37 reference "PhysicalGeography.net" @default.
- c06e70c0-616c-44f2-a884-ad0252e29e37 tag "Science Keywords" @default.