Matches in DBpedia 2016-04 for { <http://wikidata.dbpedia.org/resource/Q7161909> ?p ?o }
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- Q7161909 subject Q8421852.
- Q7161909 subject Q8421856.
- Q7161909 subject Q8581799.
- Q7161909 subject Q8581879.
- Q7161909 subject Q8582043.
- Q7161909 abstract "The Pembina Escarpment (known in Canada as the Manitoba Escarpment) is a scarp that marks the boundary of glacial Lake Agassiz. It rises up to 300–400 feet (91–122 m) and occurs in South Dakota, North Dakota, and Manitoba.The escarpment was originally formed by the undercutting of Cretaceous sandstones (the Dakota Formation) by the ancestral Red River. The escarpment was later steepened by glacial scouring. The escarpment is preserved due to a layer of erosion-resistant shale (the Pierre Formation) on top of the sandstone. The vista today, of wooded hills with small farms tucked into valleys (such as the Pembina Valley), is reminiscent of pastoral sections of New England. Streams flowing off the escarpment have high gradients and a cobble substrate.Native plants to the escarpment include burr oak, beaked hazel, high bush cranberry, serviceberry, and red osier dogwood.In Manitoba, the scarp forms the eastern edge of Riding Mountain National Park, home of a large bison herd, and Duck Mountain Provincial Park. Turtle Mountain Provincial Park and the Porcupine Hills are also part of the Manitoba Escarpment.The Pembina Escarpment is a distinct ecoregion, as defined by the U.S. Environmental Protection Agency. The ecoregion covers 274 square miles (710 km2), and is part of the larger Northern Glaciated Plains ecoregion.".
- Q7161909 thumbnail 13,000_YBP_Lockhart_Phase.jpg?width=300.
- Q7161909 wikiPageWikiLink Q1082365.
- Q7161909 wikiPageWikiLink Q1174791.
- Q7161909 wikiPageWikiLink Q1207.
- Q7161909 wikiPageWikiLink Q1211.
- Q7161909 wikiPageWikiLink Q13085.
- Q7161909 wikiPageWikiLink Q156006.
- Q7161909 wikiPageWikiLink Q156957.
- Q7161909 wikiPageWikiLink Q16.
- Q7161909 wikiPageWikiLink Q164130.
- Q7161909 wikiPageWikiLink Q18158085.
- Q7161909 wikiPageWikiLink Q18389.
- Q7161909 wikiPageWikiLink Q1948.
- Q7161909 wikiPageWikiLink Q210971.
- Q7161909 wikiPageWikiLink Q2424906.
- Q7161909 wikiPageWikiLink Q295469.
- Q7161909 wikiPageWikiLink Q35666.
- Q7161909 wikiPageWikiLink Q390804.
- Q7161909 wikiPageWikiLink Q44626.
- Q7161909 wikiPageWikiLink Q460173.
- Q7161909 wikiPageWikiLink Q5311463.
- Q7161909 wikiPageWikiLink Q7161921.
- Q7161909 wikiPageWikiLink Q7192447.
- Q7161909 wikiPageWikiLink Q7230026.
- Q7161909 wikiPageWikiLink Q751300.
- Q7161909 wikiPageWikiLink Q7856436.
- Q7161909 wikiPageWikiLink Q795190.
- Q7161909 wikiPageWikiLink Q8421852.
- Q7161909 wikiPageWikiLink Q8421856.
- Q7161909 wikiPageWikiLink Q8581799.
- Q7161909 wikiPageWikiLink Q8581879.
- Q7161909 wikiPageWikiLink Q8582043.
- Q7161909 wikiPageWikiLink Q972950.
- Q7161909 point "50.617232 -99.52652".
- Q7161909 type SpatialThing.
- Q7161909 comment "The Pembina Escarpment (known in Canada as the Manitoba Escarpment) is a scarp that marks the boundary of glacial Lake Agassiz. It rises up to 300–400 feet (91–122 m) and occurs in South Dakota, North Dakota, and Manitoba.The escarpment was originally formed by the undercutting of Cretaceous sandstones (the Dakota Formation) by the ancestral Red River. The escarpment was later steepened by glacial scouring.".
- Q7161909 label "Pembina Escarpment".
- Q7161909 lat "50.617232".
- Q7161909 long "-99.52652".
- Q7161909 depiction 13,000_YBP_Lockhart_Phase.jpg.