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Statements

Subject Item
dbr:Moenave_Formation
rdf:type
yago:Abstraction100002137 yago:WikicatHettangianGeologicFormations yago:Formation108426461 dbo:MilitaryUnit yago:Arrangement107938773 yago:Group100031264
rdfs:label
Moenave Formation
rdfs:comment
The Moenave Formation is a Mesozoic geologic formation, in the Glen Canyon Group. It is found in Utah and Arizona. The Moenave was deposited on an erosion surface on the Chinle Formation following an early Jurassic uplift and unconformity that represents about ten million years of missing sedimentation. Periodic incursions of shallow seas from the north during the Jurassic flooded parts of Wyoming, Montana, and a northeast–southwest trending trough on the Utah/Idaho border. The Moenave was deposited in a variety of river, lake, and flood-plain environments, near the ancient .
dbp:name
Moenave Formation
foaf:depiction
n18:Eubrontes01.jpg n18:Moenave_Formation.jpeg
dcterms:subject
dbc:Geologic_formations_of_Arizona dbc:Hettangian_Stage dbc:Early_Jurassic_North_America dbc:Jurassic_Arizona dbc:Ichnofossiliferous_formations dbc:Jurassic_geology_of_Utah
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25157216
dbo:wikiPageRevisionID
1084998150
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dbc:Geologic_formations_of_Arizona dbr:Shale dbr:Formation_(geology) dbr:Neotheropoda dbr:Dipnoi dbr:Dinosaur dbr:Teeth dbr:Wingate_Sandstone dbr:Coelacanthiformes dbr:Utah n9:Eubrontes01.JPG dbr:Early_Jurassic dbr:Grallator dbr:Body_fossil dbr:Protosuchus dbr:Mesozoic dbr:Protosuchus_richardsoni dbc:Early_Jurassic_North_America dbc:Hettangian_Stage dbr:Batrachopus_(reptile) dbr:Zion_National_Park dbr:Navajo_Sandstone dbr:Anomoepus dbr:Kayenta_Formation dbr:Arizona dbr:Geological_formation dbr:Pterosauria dbr:Chinle_Formation dbr:Lake_Dixie dbr:Unconformity dbr:Pteraichnus dbr:Semionotidae dbr:Megapnosaurus dbr:Gigandipus dbr:Sphenodontia dbc:Jurassic_Arizona dbc:Ichnofossiliferous_formations dbr:Jurassic dbr:Sturgeon dbr:Genus dbr:Palaeoniscidae dbr:Siltstone dbr:List_of_dinosaur-bearing_rock_formations dbr:Erosion_surface dbr:Cf. dbr:Fish dbr:Vertebra dbr:Characichnos dbr:Glen_Canyon_Group dbr:Trace_fossil dbr:Crocodylia dbr:Eucynodontia dbr:Sandstone dbc:Jurassic_geology_of_Utah dbr:Theropoda dbr:St._George_Dinosaur_Discovery_Site dbr:Eubrontes dbr:List_of_stratigraphic_units_with_indeterminate_dinosaur_fossils
owl:sameAs
freebase:m.09gj1xh wikidata:Q6890219 yago-res:Moenave_Formation n16:4rwYt
dbp:unitof
dbr:Glen_Canyon_Group
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dbt:Chronostratigraphy_of_Nevada dbt:Convert dbt:Portal dbt:USA dbt:ISBN dbt:Commons_category dbt:Fossilrange dbt:Reflist dbt:Infobox_rockunit dbt:Flag
dbo:thumbnail
n18:Moenave_Formation.jpeg?width=300
dbp:age
dbr:Early_Jurassic ca.
dbp:caption
Moenave Formation outcrop in Zion National Park
dbp:period
Hettangian
dbp:type
dbr:Geological_formation
dbo:abstract
The Moenave Formation is a Mesozoic geologic formation, in the Glen Canyon Group. It is found in Utah and Arizona. The Moenave was deposited on an erosion surface on the Chinle Formation following an early Jurassic uplift and unconformity that represents about ten million years of missing sedimentation. Periodic incursions of shallow seas from the north during the Jurassic flooded parts of Wyoming, Montana, and a northeast–southwest trending trough on the Utah/Idaho border. The Moenave was deposited in a variety of river, lake, and flood-plain environments, near the ancient . The oldest beds of this formation belong to the Dinosaur Canyon Member, a reddish, slope-forming rock layer with thin beds of siltstone that are interbedded with mudstone and fine sandstone. The Dinosaur Canyon, with a local thickness of 140 to 375 feet (43 to 114 m), was probably laid down in slow-moving streams, ponds and large lakes. Evidence for this is in cross-bedding of the sediments and large numbers of fish fossils. The upper member of the Moenave is the pale reddish-brown with a thickness of 75 to 150 feet (23 to 46 m) and cliff-forming Springdale Sandstone. It was deposited in swifter, larger, and more voluminous streams than the older Dinosaur Canyon Member. Fossils of large sturgeon-like freshwater fish have been found in the beds of the Springdale Sandstone. The next member in the Moenave Formation is the thin-bedded Whitmore Point, which is made of mudstone and shale. The lower red cliffs visible from the Zion Human History Museum (until 2000 the Zion Canyon Visitor Center) and the St. George Dinosaur Discovery Site, discovered on February 26, 2000, are accessible examples of this formation.
dbp:extent
, and
dbp:prilithology
siltstone and sandstone
gold:hypernym
dbr:Formation
prov:wasDerivedFrom
wikipedia-en:Moenave_Formation?oldid=1084998150&ns=0
dbo:wikiPageLength
8526
foaf:isPrimaryTopicOf
wikipedia-en:Moenave_Formation