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Statements

Subject Item
dbr:Coconino_Sandstone
rdf:type
owl:Thing yago:Group100031264 yago:Arrangement107938773 yago:WikicatGeologicFormationsOfTheUnitedStates yago:Formation108426461 yago:Abstraction100002137 dbo:MilitaryUnit
rdfs:label
Coconino Sandstone Coconino Sandstone
rdfs:comment
Der Coconino Sandstone ist eine kontinentale, äolische Formation, die in den US-Bundesstaaten Arizona, Colorado, Kalifornien, Nevada und Utah während des Perms abgelagert worden war. Coconino Sandstone is a geologic formation named after its exposure in Coconino County, Arizona. This formation spreads across the Colorado Plateau province of the United States, including northern Arizona, northwest Colorado, Nevada, and Utah. Lechatelierite (silica glass), as well as coesite and stishovite (high pressure forms of SiO2) were formed during the impact of a meteorite into the Coconino Sandstone at Barringer Crater in Arizona.
dbp:name
Coconino Sandstone
foaf:depiction
n13:Rim_view.jpg n13:Chelichnus-gigas.jpg n13:GrandNP4.jpg
dcterms:subject
dbc:Permian_System_of_North_America dbc:Geologic_formations_of_Colorado dbc:Permian_Arizona dbc:Permian_Colorado dbc:Sandstone_formations_of_the_United_States dbc:Permian_geology_of_Nevada dbc:Geologic_formations_of_Nevada dbc:Natural_history_of_the_Grand_Canyon dbc:Geologic_formations_of_Utah dbc:Geologic_formations_of_Arizona dbc:Permian_geology_of_Utah dbc:Geography_of_Coconino_County,_Arizona
dbo:wikiPageID
5050272
dbo:wikiPageRevisionID
1117263510
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dbr:Nevada dbr:Meteorite dbr:Coconino_County,_Arizona dbr:Formation_(geology) dbr:Lechatelierite dbr:Sand_dune n11:Chelichnus-gigas.jpg dbc:Geologic_formations_of_Colorado dbc:Permian_Arizona dbc:Permian_Colorado dbc:Permian_geology_of_Nevada dbr:Stishovite dbc:Permian_System_of_North_America dbr:Sandstone dbr:Coesite dbc:Geologic_formations_of_Nevada dbc:Natural_history_of_the_Grand_Canyon n11:GrandNP4.jpg dbr:Colorado dbc:Geologic_formations_of_Utah dbc:Geologic_formations_of_Arizona dbc:Sandstone_formations_of_the_United_States dbr:Ripple_marks dbr:Meteor_Crater dbr:Hermit_Formation dbr:Hermit_Shale dbr:Southwestern_United_States dbr:Geology_of_the_Grand_Canyon dbr:Kaibab_Limestone n11:Rim_view.jpg dbr:Utah dbr:Colorado_Plateau dbr:United_States dbr:Arizona dbr:Supai_Group dbr:Toroweap_Formation dbr:Eolian_processes dbr:Grand_Canyon dbc:Permian_geology_of_Utah dbc:Geography_of_Coconino_County,_Arizona
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n4:index.html n14:coconino.htm n20:formations.html n24:coconino.pdf
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dbp:subunits
Cave Spring Sandstone Harding Point Sandstone Member,
dbp:underlies
dbr:Kaibab_Limestone dbr:Toroweap_Formation
dbp:wikiPageUsesTemplate
dbt:Infobox_rockunit dbt:Snd dbt:Convert dbt:Authority_control dbt:Short_description dbt:Commons_category dbt:Chronostratigraphy_of_Nevada dbt:C dbt:Reflist dbt:Flag
dbo:thumbnail
n13:Rim_view.jpg?width=300
dbp:age
Permian
dbp:country
dbp:period
Permian
dbp:region
dbr:Colorado_Plateau
dbp:type
Sedimentary
dbo:abstract
Coconino Sandstone is a geologic formation named after its exposure in Coconino County, Arizona. This formation spreads across the Colorado Plateau province of the United States, including northern Arizona, northwest Colorado, Nevada, and Utah. This rock formation is particularly prominent in the Grand Canyon, where it is visible as a prominent white cliff-forming layer. The thickness of the formation varies due to regional structural features; in the Grand Canyon area it is only 65 feet (20 m) thick in the west, thickens to over 600 feet (180 m) in the middle and then thins to 57 feet (17 m) in the east. Either the Kaibab Limestone or Toroweap Formation overlies the Coconino Sandstone. The Coconino Sandstone is typically buff to white in color. It consists primarily of fine well-sorted quartz grains, with minor amounts of potassium feldspar grains deposited by eolian processes (wind-deposited) approximately 275 million years ago. Several structural features such as ripple marks, sand dune deposits, rain patches, slump marks, and fossil tracks are not only well preserved within the formation, but also contribute evidence of its eolian origin. Lechatelierite (silica glass), as well as coesite and stishovite (high pressure forms of SiO2) were formed during the impact of a meteorite into the Coconino Sandstone at Barringer Crater in Arizona. Der Coconino Sandstone ist eine kontinentale, äolische Formation, die in den US-Bundesstaaten Arizona, Colorado, Kalifornien, Nevada und Utah während des Perms abgelagert worden war.
dbp:extent
-
dbp:namedby
N. H. Darton, 1910
dbp:namedfor
Coconino Plateau
dbp:overlies
dbr:Hermit_Formation
dbp:prilithology
dbr:Sandstone
gold:hypernym
dbr:Formation
prov:wasDerivedFrom
wikipedia-en:Coconino_Sandstone?oldid=1117263510&ns=0
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6174
foaf:isPrimaryTopicOf
wikipedia-en:Coconino_Sandstone