About: Lake Bassano

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Lake Bassano was a proglacial lake that formed in the Late Pleistocene during the deglaciation of south-central Alberta by the impoundment of a re-established drainage system and addition of glacial meltwater. It is associated with the development of through-flowing drainage within the Red Deer River basin in particular, and the South Saskatchewan drainage network in general. Approximately 7,500 square kilometres (2,900 sq mi) of the is covered with lacustrine sediments. These sediments are bordered by the topographically higher Buffalo Lake Moraine to the west, the Suffield Moraine to the east and the Lethbridge Moraine to the south.

Attributes	Values
rdf:type	yago:BodyOfWater109225146 yago:Lake109328904 yago:PhysicalEntity100001930 yago:WikicatGlacialLakesOfCanada yago:YagoGeoEntity yago:YagoPermanentlyLocatedEntity lake yago:Thing100002452 yago:WikicatFormerLakes
rdfs:label	Lake Bassano (en)
rdfs:comment	Lake Bassano was a proglacial lake that formed in the Late Pleistocene during the deglaciation of south-central Alberta by the impoundment of a re-established drainage system and addition of glacial meltwater. It is associated with the development of through-flowing drainage within the Red Deer River basin in particular, and the South Saskatchewan drainage network in general. Approximately 7,500 square kilometres (2,900 sq mi) of the is covered with lacustrine sediments. These sediments are bordered by the topographically higher Buffalo Lake Moraine to the west, the Suffield Moraine to the east and the Lethbridge Moraine to the south. (en)
dcterms:subject	Former lakes of North America Glacial lakes of Canada
Wikipage page ID	14046313 (xsd:integer)
Wikipage revision ID	1123207279 (xsd:integer)
Link from a Wikipage to another Wikipage	Canadian Journal of Earth Sciences Quaternary Science Reviews Saskatchewan Meltwater Proglacial lake Deglaciation Former lakes of North America Glacial lakes of Canada Geological Survey of Canada Chronological Geological Society of America Wisconsin Drainage system (geomorphology) Glacier Alberta Drumheller Etzikom Coulee Lake Laurentide Ice Sheet Buffalo Lake Moraine Pleistocene Canadian Geotechnical Journal Red Deer River Southern Alberta Sediment dbr:Bassano_basin dbr:Deglacial_landscape dbr:Glacial_Lake_Empress dbr:Missouri_Drainage_System dbr:Strathmore_Channel
Link from a Wikipage to an external page	https://open.alberta.ca/opendata/gda-dig_2007_0012 https://era.library.ualberta.ca/items/db91e56d-9702-43f0-902d-9211ea912f6f/view/3995b013-ebab-40b2-a795-cbee3580f72d/MM18309.pdf https://id.erudit.org/iderudit/032681ar
sameAs	Lake Bassano Lake Bassano Lake Bassano Lake Bassano
dbp:wikiPageUsesTemplate	dbt:Citation_style dbt:Cite_book dbt:Cite_journal dbt:Cite_thesis dbt:Convert dbt:Coord_missing dbt:Multiple_issues dbt:Refimprove dbt:Reflist dbt:Sfnmp dbt:Sfnp dbt:Google_books dbt:Harvp dbt:Pleistocene_Lakes_and_Seas dbt:Cite_map
4a	Shetsen (en) Vreeken (en)
4y	1984 (xsd:integer) 1989 (xsd:integer)
1a	Christiansen (en) Horberg (en) St-Onge (en)
1y	1954 (xsd:integer) 1972 (xsd:integer) 1979 (xsd:integer)
2a	Stalker (en) Moran (en) Clayton (en) Quigley (en) Teller (en)
2y	1973 (xsd:integer) 1980 (xsd:integer)
3a	Moran (en) Clayton (en) Shetsen (en) Vreeken (en)
3y	1982 (xsd:integer) 1987 (xsd:integer) 1989 (xsd:integer)
5a	Prest (en) Dyke (en)
5y	1987 (xsd:integer)
6a	Teller (en)
6y	1987 (xsd:integer)
7a	Klassen (en)
7y	1994 (xsd:integer)
has abstract	Lake Bassano was a proglacial lake that formed in the Late Pleistocene during the deglaciation of south-central Alberta by the impoundment of a re-established drainage system and addition of glacial meltwater. It is associated with the development of through-flowing drainage within the Red Deer River basin in particular, and the South Saskatchewan drainage network in general. Approximately 7,500 square kilometres (2,900 sq mi) of the is covered with lacustrine sediments. These sediments are bordered by the topographically higher Buffalo Lake Moraine to the west, the Suffield Moraine to the east and the Lethbridge Moraine to the south. The transmission of water through the basin was ultimately controlled by the regional topography and the position of the ice front. As the Laurentide Ice Sheet retreated, lower outlet channels were exposed. The lake levels at any given time were constrained by the elevation of the lowest drainage channel. As Glacial Lake Bassano, and the proglacial lake system as a whole developed, throughflow in individual channels waxed, waned, and reversed, depending on the systemic controls. (en)
gold:hypernym	Lake

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