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Statements

Subject Item
dbr:Post-glacial_clay
rdfs:label
Post-glacial clay
rdfs:comment
Post-glacial clay (Swedish: Postglacial lera) is any sedimentary clay layer or deposit that formed after retreating glaciers have abandoned an area. The term is used in Sweden. Compared to glacial clay, post-glacial clay tend to be less rich in calcium carbonate. In some places like around Göta Älv post-glacial clay distinguishes itself by having lower silt content than the glacial clays under it.
dcterms:subject
dbc:Clay dbc:Types_of_soil dbc:Sediments
dbo:wikiPageID
70854396
dbo:wikiPageRevisionID
1097636423
dbo:wikiPageWikiLink
dbc:Types_of_soil dbr:Clay dbr:Swedish_language dbr:Swedish_Geotechnical_Institute dbr:Calcium_carbonate dbc:Clay dbr:Silt dbc:Sediments dbr:Sweden dbr:Göta_Älv
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n9:sgi-r65.pdf
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n14:GPja6 wikidata:Q112261804
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dbo:abstract
Post-glacial clay (Swedish: Postglacial lera) is any sedimentary clay layer or deposit that formed after retreating glaciers have abandoned an area. The term is used in Sweden. Compared to glacial clay, post-glacial clay tend to be less rich in calcium carbonate. In some places like around Göta Älv post-glacial clay distinguishes itself by having lower silt content than the glacial clays under it.
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wikipedia-en:Post-glacial_clay?oldid=1097636423&ns=0
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wikipedia-en:Post-glacial_clay