About: Pembina Escarpment

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The Pembina Escarpment is a scarp that runs from South Dakota to Manitoba, and forms the western wall of the Red River Valley. The height of the escarpment above the river valley is 300–400 feet (91–122 m).

Attributes	Values
rdf:type	Thing place geo:SpatialThing yago:Escarpment109274152 yago:GeologicalFormation109287968 yago:Object100002684 yago:PhysicalEntity100001930 yago:YagoGeoEntity yago:YagoPermanentlyLocatedEntity yago:Slope109437454 yago:WikicatEscarpmentsOfCanada yago:WikicatEscarpmentsOfTheUnitedStates mountain range
rdfs:label	Pembina Escarpment (en) 彭比纳断崖 (zh)
rdfs:comment	The Pembina Escarpment is a scarp that runs from South Dakota to Manitoba, and forms the western wall of the Red River Valley. The height of the escarpment above the river valley is 300–400 feet (91–122 m). (en) 彭比纳断崖（Pembina Escarpment）（在加拿大被称为曼尼托巴断崖（Manitoba Escarpment）) 是一个标志冰川边界的陡峭断崖。断层高度为300-400英尺（约合91-122米），分布在北达科他州，南达科他州和曼尼托巴省。断崖最初是由古红河底部的白垩纪砂岩（）形成的。断崖随后通过冰川冲刷而变得陡峭。由于在砂岩顶部有一层抗侵蚀的页岩（Pierre岩层），悬崖得以被保留下来。今天的景色，树木繁茂的丘陵卷入山谷（如Pembina valley），让人想起新英格兰的牧区。从悬崖流出的溪流坡度较高且具有卵石基质。悬崖的本地植物包括大果栎，榛子，，唐棣树和。在马尼托巴，断崖形成了雷丁山国家公园的东部边缘，一个大野牛群的栖息地，和鸭山省立公园。乌龟山省立公园，彭比纳山谷省立公园和豪猪山也是马尼托巴断崖的一部分。根据美国环境保护局的定义，彭比纳断崖是一个独特的生态区。该生态区涵盖274平方英里（710平方千米）的土地，并且是较大的北方冰河平原生态区的一部分。 (zh)
geo:lat	50.617233 (xsd:float)
geo:long	-99.526520 (xsd:float)
foaf:depiction
dcterms:subject	Escarpments of Canada Landforms of Manitoba Landforms of North Dakota Landforms of South Dakota Escarpments of the United States
Wikipage page ID	9068407 (xsd:integer)
Wikipage revision ID	1022142648 (xsd:integer)
Link from a Wikipage to another Wikipage	Canada Saskatchewan Pembina Valley United States Deciduous Cretaceous Escarpments of Canada Escarpment Mississippi River Red Osier Dogwood Landforms of Manitoba Ice age Ice sheet Burr oak Turtle Mountain (plateau) U.S. Environmental Protection Agency Landforms of North Dakota Glacier Dakota Formation North America Beaked Hazel Viburnum trilobum Red River Valley Gulf of Mexico Landforms of South Dakota Assiniboine River Escarpments of the United States Lake Agassiz Lake Souris Laurentide Ice Sheet Ecoregion Willow Populus sect. Populus Manitoba Souris River South Dakota Green ash New England Red River of the North Sandstone Settler Shale Manitoba Escarpment Manitoba Maple Serviceberry Pin cherry Pierre Formation Northern Glaciated Plains
Link from a Wikipage to an external page	https://www.gov.mb.ca/stem/mrd/geo/exp-sup/files/fig8.pdf%7Carchiveurl=https:/web.archive.org/web/20120722020234/http:/www.manitoba.ca/iem/mrd/geo/exp-sup/files/fig8.pdf%7Carchivedate=2012-07-22%7Ctitle=Map
sameAs	Pembina Escarpment Pembina Escarpment Pembina Escarpment Pembina Escarpment Pembina Escarpment
dbp:wikiPageUsesTemplate	dbt:Authority_control dbt:Cite_web dbt:Clear_right dbt:Convert dbt:Coord dbt:Reflist dbt:Canadian_Prairies
thumbnail	wiki-commons:Special:FilePath/13,000_YBP_Lockhart_Phase.jpg?width=300
georss:point	50.617232 -99.52652
has abstract	The Pembina Escarpment is a scarp that runs from South Dakota to Manitoba, and forms the western wall of the Red River Valley. The height of the escarpment above the river valley is 300–400 feet (91–122 m). (en) 彭比纳断崖（Pembina Escarpment）（在加拿大被称为曼尼托巴断崖（Manitoba Escarpment）) 是一个标志冰川边界的陡峭断崖。断层高度为300-400英尺（约合91-122米），分布在北达科他州，南达科他州和曼尼托巴省。断崖最初是由古红河底部的白垩纪砂岩（）形成的。断崖随后通过冰川冲刷而变得陡峭。由于在砂岩顶部有一层抗侵蚀的页岩（Pierre岩层），悬崖得以被保留下来。今天的景色，树木繁茂的丘陵卷入山谷（如Pembina valley），让人想起新英格兰的牧区。从悬崖流出的溪流坡度较高且具有卵石基质。悬崖的本地植物包括大果栎，榛子，，唐棣树和。在马尼托巴，断崖形成了雷丁山国家公园的东部边缘，一个大野牛群的栖息地，和鸭山省立公园。乌龟山省立公园，彭比纳山谷省立公园和豪猪山也是马尼托巴断崖的一部分。根据美国环境保护局的定义，彭比纳断崖是一个独特的生态区。该生态区涵盖274平方英里（710平方千米）的土地，并且是较大的北方冰河平原生态区的一部分。 (zh)
gold:hypernym	Scarp
prov:wasDerivedFrom	wikipedia-en:Pembina_Escarpment?oldid=1022142648&ns=0
page length (characters) of wiki page	7581 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Pembina_Escarpment
geo:geometry	POINT(-99.526519775391 50.617233276367)
is Link from a Wikipage to another Wikipage of	Boyne River (Manitoba) Pembina River (Manitoba – North Dakota)

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