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Statements

Subject Item
dbr:Till_plain
rdf:type
dbo:Place
rdfs:label
Pianoro di till Till plain
rdfs:comment
Till plains are an extensive flat plain of glacial till that forms when a sheet of ice becomes detached from the main body of a glacier and melts in place, depositing the sediments it carried. Ground moraines are formed with melts out of the glacier in irregular heaps, forming rolling hills. Till plains are common in areas such as the Midwestern United States, due to multiple glaciation events that occurred in the Holocene epoch. During this period, the Laurentide Ice Sheet advanced and retreated during the Pleistocene epoch. Till plains created by the Wisconsin glaciation cover much of the Midwest, including North Dakota, South Dakota, Indiana, Minnesota, Wisconsin, Iowa, Illinois, and northern Ohio (see Glacial till plains (Ohio)). Un pianoro di till (in inglese till plain) è una estensione pianeggiante di till glaciale che si forma quando un ammasso di ghiaccio si distacca dal corpo principale di un ghiacciaio e fonde sul luogo depositando i sedimenti che trasportava. Un pianoro di till con topografia irregolare viene riferito come morena terrestre.
foaf:depiction
n9:Ground_moraine_9004.jpg
dct:subject
dbc:Glaciology dbc:Geomorphology
dbo:wikiPageID
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dbo:wikiPageRevisionID
1114529820
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dbr:Advection dbr:Ice dbr:Outwash_plain dbr:Glacier dbr:Pleistocene dbr:Plain dbr:Aquitard dbr:Moraines dbr:Loam dbr:Ablation_till dbr:Drumlins dbr:Laurentide_Ice_Sheet dbr:Ohio dbc:Glaciology dbc:Geomorphology dbr:Till dbr:Holocene dbr:Moraine dbr:Darcy's_law dbr:Glacial_till dbr:Ground_moraine n17:Ground_moraine_9004.jpg dbr:Southeastern_Wisconsin_Till_Plains_(ecoregion) dbr:Flute_(glacial) dbr:Glacial_till_plains_(Ohio) dbr:Wisconsin_glaciation dbr:Sediment
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dbpedia-fa:دشت_یخ‌نهشته‌ای dbpedia-it:Pianoro_di_till n18:3bxie freebase:m.04x4xs wikidata:Q3902058
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n9:Ground_moraine_9004.jpg?width=300
dbo:abstract
Till plains are an extensive flat plain of glacial till that forms when a sheet of ice becomes detached from the main body of a glacier and melts in place, depositing the sediments it carried. Ground moraines are formed with melts out of the glacier in irregular heaps, forming rolling hills. Till plains are common in areas such as the Midwestern United States, due to multiple glaciation events that occurred in the Holocene epoch. During this period, the Laurentide Ice Sheet advanced and retreated during the Pleistocene epoch. Till plains created by the Wisconsin glaciation cover much of the Midwest, including North Dakota, South Dakota, Indiana, Minnesota, Wisconsin, Iowa, Illinois, and northern Ohio (see Glacial till plains (Ohio)). Un pianoro di till (in inglese till plain) è una estensione pianeggiante di till glaciale che si forma quando un ammasso di ghiaccio si distacca dal corpo principale di un ghiacciaio e fonde sul luogo depositando i sedimenti che trasportava. Un pianoro di till con topografia irregolare viene riferito come morena terrestre.
gold:hypernym
dbr:Plain
prov:wasDerivedFrom
wikipedia-en:Till_plain?oldid=1114529820&ns=0
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wikipedia-en:Till_plain