John Day Formation (original) (raw)

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dbo:abstract The John Day Formation is a series of rock strata exposed in the Picture Gorge district of the John Day River basin and elsewhere in north-central Oregon in the United States. The Picture Gorge exposure lies east of the Blue Mountain uplift, which cuts southwest–northeast through the Horse Heaven mining district northeast of Madras. Aside from the Picture Gorge district, which defines the type, the formation is visible on the surface in two other areas: another exposure is in the Warm Springs district west of the uplift, between it and the Cascade Range, and the third is along the south side of the Ochoco Mountains. All three exposures, consisting mainly of tuffaceous sediments and pyroclastic rock rich in silica, lie unconformably between the older rocks of the Clarno Formation below and Columbia River basalts above. (en) De John Day-formatie (Engels: John Day Formation) is een geologische formatie in de Amerikaanse staat Oregon, die een ouderdom heeft van Laat-Eoceen tot Vroeg-Mioceen (37 tot 20 miljoen jaar oud). De formatie bestaat voornamelijk uit vulkanisch gesteente als tufsteen, scoria en lava. De vulkanische gesteenten zijn meestal ryolitisch tot andesitisch van samenstelling. (nl)
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dbo:wikiPageWikiLink dbr:Cascade_Range dbc:Neogene_geology_of_Oregon dbr:Horse_Heaven,_Oregon dbr:Pyroclastic_rock dbr:Genus dbr:Eocene dbr:Miocene dbr:Madras,_Oregon dbr:Silicon_dioxide dbr:Columbia_River_Basalt_Group dbr:Tuff dbr:Central_Oregon dbc:Sandstone_formations_of_the_United_States dbr:Daeodon dbr:Unconformity dbc:Eocene_United_States dbc:Tuff_formations dbr:John_Day_Fossil_Beds_National_Monument dbr:John_Day_River dbc:John_Day_Fossil_Beds_National_Monument dbc:Geologic_formations_of_Oregon dbr:Clarno_Formation dbr:Metasequoia dbc:Miocene_United_States dbr:Ochoco_Mountains dbr:Oregon dbc:Oligocene_North_America dbr:Sandstone dbr:Type_site dbr:Turtle_Cove_Formation dbr:Oreodont dbr:Blue_Mountains_(Oregon) dbr:Big_Basin_Formation dbr:File:NPS_john-day-fossil-beds-geologic-map.jpg dbr:Haystack_Formation dbr:Kimberly_Formation dbr:Picture_Gorge_Ignimbrite
dbp:age dbr:Eocene dbr:Miocene
dbp:caption Exposures of the Turtle Cove Formation along a hiking trail in the Sheep Rock Unit of the John Day Fossil Beds National Monument (en)
dbp:name John Day Strata (en)
dbp:namedfor dbr:John_Day_River
dbp:otherlithology dbr:Pyroclastic_rock
dbp:overlies dbr:Clarno_Formation
dbp:period Miocene (en)
dbp:prilithology dbr:Tuff dbr:Sandstone
dbp:region dbr:Central_Oregon
dbp:type Sedimentary , igneous (en)
dbp:underlies dbr:Columbia_River_Basalt_Group
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dcterms:subject dbc:Neogene_geology_of_Oregon dbc:Sandstone_formations_of_the_United_States dbc:Eocene_United_States dbc:Tuff_formations dbc:John_Day_Fossil_Beds_National_Monument dbc:Geologic_formations_of_Oregon dbc:Miocene_United_States dbc:Oligocene_North_America
gold:hypernym dbr:Series
schema:sameAs http://viaf.org/viaf/244763808
rdf:type yago:Abstraction100002137 yago:Arrangement107938773 yago:Formation108426461 yago:Group100031264 yago:WikicatGeologicFormationsOfTheUnitedStates dbo:TelevisionShow
rdfs:comment De John Day-formatie (Engels: John Day Formation) is een geologische formatie in de Amerikaanse staat Oregon, die een ouderdom heeft van Laat-Eoceen tot Vroeg-Mioceen (37 tot 20 miljoen jaar oud). De formatie bestaat voornamelijk uit vulkanisch gesteente als tufsteen, scoria en lava. De vulkanische gesteenten zijn meestal ryolitisch tot andesitisch van samenstelling. (nl) The John Day Formation is a series of rock strata exposed in the Picture Gorge district of the John Day River basin and elsewhere in north-central Oregon in the United States. The Picture Gorge exposure lies east of the Blue Mountain uplift, which cuts southwest–northeast through the Horse Heaven mining district northeast of Madras. Aside from the Picture Gorge district, which defines the type, the formation is visible on the surface in two other areas: another exposure is in the Warm Springs district west of the uplift, between it and the Cascade Range, and the third is along the south side of the Ochoco Mountains. All three exposures, consisting mainly of tuffaceous sediments and pyroclastic rock rich in silica, lie unconformably between the older rocks of the Clarno Formation below and (en)
rdfs:label John Day Formation (en) John Day-formatie (nl)
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foaf:depiction wiki-commons:Special:FilePath/East_face_painted_hills_panorama.jpg wiki-commons:Special:FilePath/Blue_basin_lower_trail.jpg wiki-commons:Special:FilePath/NPS_john-day-fossil-beds-geologic-map.jpg
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