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- Presumpscot_Formation abstract "The Presumpscot formation is a late Pleistocene glacial deposit of predominantly submarine clays, located along the Maine and New Hampshire coast and inland along their major river valleys. It consists of primarily silt- and clay-sized particles formed from the glacial abrasion of the feldspars, quartz, and micas of the region, carried by glacial meltwater and deposited below sea level before subsequent crust rising (isostatic rebound) elevated the deposits up to more than 300 feet (91 m). It is named after the Presumpscot River where large amounts of the characteristic blue-gray clay are found.Fossilized remains of marine organisms are found interspersed among the deposits.It was a historically significant resource for the production of brick, though little of that industry remains.Pollen found in the clays near Portland, Maine, indicate spruce forests, with low proportions of pines, about 11500 BP.".
- Presumpscot_Formation wikiPageExternalLink oct00.htm.
- Presumpscot_Formation wikiPageID "34166649".
- Presumpscot_Formation wikiPageLength "1607".
- Presumpscot_Formation wikiPageOutDegree "14".
- Presumpscot_Formation wikiPageRevisionID "636189022".
- Presumpscot_Formation wikiPageWikiLink Category:Geologic_formations_of_Maine.
- Presumpscot_Formation wikiPageWikiLink Category:Geologic_formations_of_New_Hampshire.
- Presumpscot_Formation wikiPageWikiLink Feldspar.
- Presumpscot_Formation wikiPageWikiLink Fossil.
- Presumpscot_Formation wikiPageWikiLink Glacial_deposit.
- Presumpscot_Formation wikiPageWikiLink Isostatic_rebound.
- Presumpscot_Formation wikiPageWikiLink Maine.
- Presumpscot_Formation wikiPageWikiLink Mica.
- Presumpscot_Formation wikiPageWikiLink New_Hampshire.
- Presumpscot_Formation wikiPageWikiLink Pleistocene.
- Presumpscot_Formation wikiPageWikiLink Pollen.
- Presumpscot_Formation wikiPageWikiLink Portland,_Maine.
- Presumpscot_Formation wikiPageWikiLink Post-glacial_rebound.
- Presumpscot_Formation wikiPageWikiLink Presumpscot_River.
- Presumpscot_Formation wikiPageWikiLink Quartz.
- Presumpscot_Formation wikiPageWikiLink Till.
- Presumpscot_Formation wikiPageWikiLinkText "Presumpscot Formation".
- Presumpscot_Formation hasPhotoCollection Presumpscot_Formation.
- Presumpscot_Formation wikiPageUsesTemplate Template:Convert.
- Presumpscot_Formation wikiPageUsesTemplate Template:Reflist.
- Presumpscot_Formation subject Category:Geologic_formations_of_Maine.
- Presumpscot_Formation subject Category:Geologic_formations_of_New_Hampshire.
- Presumpscot_Formation hypernym Deposit.
- Presumpscot_Formation type Library.
- Presumpscot_Formation type Formation.
- Presumpscot_Formation type Landform.
- Presumpscot_Formation comment "The Presumpscot formation is a late Pleistocene glacial deposit of predominantly submarine clays, located along the Maine and New Hampshire coast and inland along their major river valleys. It consists of primarily silt- and clay-sized particles formed from the glacial abrasion of the feldspars, quartz, and micas of the region, carried by glacial meltwater and deposited below sea level before subsequent crust rising (isostatic rebound) elevated the deposits up to more than 300 feet (91 m).".
- Presumpscot_Formation label "Presumpscot Formation".
- Presumpscot_Formation sameAs m.0hrc0rl.
- Presumpscot_Formation sameAs Q7242094.
- Presumpscot_Formation sameAs Q7242094.
- Presumpscot_Formation wasDerivedFrom Presumpscot_Formation?oldid=636189022.
- Presumpscot_Formation isPrimaryTopicOf Presumpscot_Formation.