An Entity of Type: place, from Named Graph: http://dbpedia.org, within Data Space: dbpedia.org

The Big Hollow is a wind eroded deflation basin located to the west of Laramie, Wyoming in the United States. It is the second largest wind eroded depression in the world. The Big Hollow is the largest deflation basin in North America. The Big Hollow is younger than the alluvial valley floors which now form its boundaries and is therefore of Late Pleistocene age (less than 250,000 years). During most of the Pleistocene the Big Hollow was actually a hill composed of soft sedimentary bedrock. The material making up this former hill was much more easily eroded than the alluvial valley floors which bounded it to both the north and south. Eventually, the hill was washed and blown away and then the wind continued to erode a deflation basin into the soft bedrock. Eventually the former hill became

Property Value
dbo:abstract
  • The Big Hollow is a wind eroded deflation basin located to the west of Laramie, Wyoming in the United States. It is the second largest wind eroded depression in the world. The Big Hollow is the largest deflation basin in North America. The Big Hollow is younger than the alluvial valley floors which now form its boundaries and is therefore of Late Pleistocene age (less than 250,000 years). During most of the Pleistocene the Big Hollow was actually a hill composed of soft sedimentary bedrock. The material making up this former hill was much more easily eroded than the alluvial valley floors which bounded it to both the north and south. Eventually, the hill was washed and blown away and then the wind continued to erode a deflation basin into the soft bedrock. Eventually the former hill became lower than the river channels which once flowed around it. The geologists call this "topographic reversal". The Qattara Depression near Cairo, Egypt is the largest. The Big Hollow is an undrained basin and is 11 miles (18 km) long, 4 miles (6.4 km) wide, and up to 200 feet (61 m) deep. Oil was discovered in 1917 and the basin has been productive since. The basin is listed on the National Natural Landmark list. (en)
dbo:location
dbo:wikiPageExternalLink
dbo:wikiPageID
  • 20700106 (xsd:integer)
dbo:wikiPageLength
  • 3374 (xsd:nonNegativeInteger)
dbo:wikiPageRevisionID
  • 1121976836 (xsd:integer)
dbo:wikiPageWikiLink
dbp:designated
  • 1980 (xsd:integer)
dbp:location
  • South-east Wyoming (en)
dbp:mapCaption
  • Map of Wyoming (en)
dbp:name
  • The Big Hollow (en)
dbp:nearestCity
dbp:wikiPageUsesTemplate
dcterms:subject
gold:hypernym
georss:point
  • 41.31321 -105.72131
rdf:type
rdfs:comment
  • The Big Hollow is a wind eroded deflation basin located to the west of Laramie, Wyoming in the United States. It is the second largest wind eroded depression in the world. The Big Hollow is the largest deflation basin in North America. The Big Hollow is younger than the alluvial valley floors which now form its boundaries and is therefore of Late Pleistocene age (less than 250,000 years). During most of the Pleistocene the Big Hollow was actually a hill composed of soft sedimentary bedrock. The material making up this former hill was much more easily eroded than the alluvial valley floors which bounded it to both the north and south. Eventually, the hill was washed and blown away and then the wind continued to erode a deflation basin into the soft bedrock. Eventually the former hill became (en)
rdfs:label
  • The Big Hollow (Wyoming) (en)
owl:sameAs
geo:geometry
  • POINT(-105.72131347656 41.313209533691)
geo:lat
  • 41.313210 (xsd:float)
geo:long
  • -105.721313 (xsd:float)
prov:wasDerivedFrom
foaf:isPrimaryTopicOf
is dbo:wikiPageDisambiguates of
is dbo:wikiPageWikiLink of
is foaf:primaryTopic of
Powered by OpenLink Virtuoso    This material is Open Knowledge     W3C Semantic Web Technology     This material is Open Knowledge    Valid XHTML + RDFa
This content was extracted from Wikipedia and is licensed under the Creative Commons Attribution-ShareAlike 3.0 Unported License