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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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 |
dbp:wikiPageUsesTemplate |
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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) |
owl:sameAs |
freebase:John Day Formation yago-res:John Day Formation wikidata:John Day Formation dbpedia-nl:John Day Formation https://global.dbpedia.org/id/3GSQP |
prov:wasDerivedFrom |
wikipedia-en:John_Day_Formation?oldid=1103727660&ns=0 |
foaf:depiction |
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wikipedia-en:John_Day_Formation |
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dbr:Turtle_Cove_Formation |
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dbr:List_of_fossil_sites dbr:1926_in_paleontology dbr:2021_in_paleobotany dbr:2022_in_paleomammalogy dbr:List_of_fossiliferous_stratigraphic_units_in_Oregon dbr:Ulmus_okanaganensis dbr:Comptonia_columbiana dbr:Corumictis dbr:Coyote_Butte_Limestone dbr:Mascall_Formation dbr:1997_in_paleontology dbr:Cline_Buttes dbr:1987_in_paleontology dbr:2011_in_paleomammalogy dbr:List_of_Acer_species dbr:Acer_ashwilli dbr:Acer_clarnoense dbr:Acer_eonegundo dbr:Acer_taurocursum dbr:Daeodon dbr:Dyticonastis dbr:Eucommia_jeffersonensis dbr:Eucommia_montana dbr:Florissantia_(plant) dbr:Novumbra_oregonensis dbr:1999_in_paleontology dbr:2015_in_paleomammalogy dbr:2016_in_paleomammalogy dbr:Taxodium_dubium dbr:2017_in_paleomammalogy dbr:2019_in_paleomammalogy dbr:John_Day_Fossil_Beds_National_Monument dbr:Dipteronia dbr:Dipteronia_brownii dbr:Phlaocyon dbr:Phlaocyon_latidens dbr:Merychyus dbr:Ochoco_Mountains dbr:Rhizocyon dbr:Uranium_mining_in_the_United_States dbr:Turtle_Cove_Formation |
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dbr:Mascall_Formation |
is foaf:primaryTopic of |
wikipedia-en:John_Day_Formation |