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dbr:Toroweap_Formation
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rdfs:label
Toroweap-Formation Toroweap Formation
rdfs:comment
The Middle Permian Toroweap Formation is a thin, darker geologic unit, between the brighter colored units of the Kaibab Limestone above, and Coconino Sandstone below. It is a prominent unit in Grand Canyon, Arizona, USA, found through sections of the South Rim, Grand Canyon, and the North Rim, of the Kaibab Plateau; also the Kaibab's southeast extension to Cape Royal, the . The Colorado River of the Grand Canyon makes its excursion from due-south to due-west around the Walhalla Plateau, as it enters the east end of the Grand Canyon's interior, . The formation is also found in southeast Utah. Die Toroweap-Formation ist eine permische Formation, die in den US-Bundesstaaten Arizona, Nevada und Utah aufgeschlossen ist.
foaf:depiction
n6:WalnutCanyonNorthWall.jpg n6:Toroweap_Sunrise.jpg n6:Grand_Canyon_National_Park-_Toroweap_Formation.jpg n6:Grand_Canyon_National_Park-Arizona1575.jpg
dct:subject
dbc:Geologic_formations_of_Nevada dbc:Permian_Arizona dbc:Cisuralian_Series_of_North_America dbc:Shale_formations_of_the_United_States dbc:Permian_geology_of_Utah dbc:Geologic_formations_of_Arizona dbc:Permian_geology_of_Nevada dbc:Colorado_Plateau dbc:Natural_history_of_the_Grand_Canyon dbc:Geologic_formations_of_Utah
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and elsewhere in Arizona, Utah, Nevada also South Rim, Kaibab Limestone-, Grand Canyon, North Rim, ,
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dbo:thumbnail
n6:Grand_Canyon_National_Park-_Toroweap_Formation.jpg?width=300
dbp:age
Early Permian,
dbp:caption
Toroweap formation in Grand Canyon National Park
dbp:imagesize
200
dbp:period
Permian
dbp:region
-Colorado Plateau Northern Arizona, southeast Utah
dbp:thickness
approximate maximum
dbp:type
dbr:Geological_formation
dbo:abstract
The Middle Permian Toroweap Formation is a thin, darker geologic unit, between the brighter colored units of the Kaibab Limestone above, and Coconino Sandstone below. It is a prominent unit in Grand Canyon, Arizona, USA, found through sections of the South Rim, Grand Canyon, and the North Rim, of the Kaibab Plateau; also the Kaibab's southeast extension to Cape Royal, the . The Colorado River of the Grand Canyon makes its excursion from due-south to due-west around the Walhalla Plateau, as it enters the east end of the Grand Canyon's interior, . The formation is also found in southeast Utah. The Toroweap Formation is a darker unit of gypsum and shale; also sandstone. In photos the cliff-forming Kaibab and Coconino units, show the more erodable Toroweap Formation slope-forming accumulations upon the underlying Coconino Sandstone; likewise below the Coconino, the softer Hermit Formation is shown forming slopes, above the slope forming 'redbeds' of the Supai Group. Close-up views of the Toroweap will show the resistant sandstone sub-units as erosion resistant sections. Cliffs of the Toroweap Formation can be found in Walnut Canyon National Monument, about 70 mi southeast of the Grand Canyon, and east of Flagstaff, Arizona. Marine transgression, and continental wind-blown sand, laid down the three units of Kaibab, Toroweap, and Coconino. The oceanic sea came from the west, and receded and re-transgressed. The Coconino Sandstone being made of sand dunes, continental, means that near-shore Toroweap deposits, and off-shore Kaibab Limestone, can all have the same actual ages in different regions where they were deposited, (continental, near-shore, open sea). In Arizona, the Toroweap formation is found in two transgressions eastwards, with easternmost 'strand-lines' locating the shoreline, Toroweap west, and Coconino sand dunes or beach deposits, east. Die Toroweap-Formation ist eine permische Formation, die in den US-Bundesstaaten Arizona, Nevada und Utah aufgeschlossen ist.
dbp:extent
Grand Canyon, North & South Rims, northeast Arizona, southeast Utah
dbp:overlies
dbr:Coconino_Sandstone
dbp:prilithology
gypsum & shale, also sandstone
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