dbo:abstract |
The Doherty Slide is a prominent dissected rim of volcanic origin located in southeastern Oregon in the United States. It is located in rural Lake County, just north of the Nevada border. The ridge sits at the eastern end of the , approximately 20 miles (32 km) east of the town of Adel. The ridge was formed by lava extrusions and has been subsequently eroded to produce the present rim. The term "slide" likely refers to the large amount of eroded material along the base of the ridge, which rises approximately 1000 ft (300 m) from the valley floor on the western side. The eastern side is a plateau that stretches eastward through southeastern Oregon. Oregon Route 140 climbs the face of the slide. (en) |
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wiki-commons:Special:FilePath/DSCN7274_dohertyslide_e_300.jpg?width=300 |
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http://www.blm.gov/or/resources/recreation/site_info.php%3Fsiteid=104 |
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dbr:United_States dbr:Bureau_of_Land_Management dbr:Lava dbr:Adel,_Oregon dbc:Bureau_of_Land_Management_areas_in_Oregon dbc:Landforms_of_Lake_County,_Oregon dbr:Lake_County,_Oregon dbc:Volcanoes_of_Oregon dbr:Nevada dbr:Oregon dbr:Oregon_Route_140 dbc:Protected_areas_of_Lake_County,_Oregon dbr:Volcano dbr:File:DSCN7274_dohertyslide_e_300.jpg dbr:Guano_Valley |
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dbc:Bureau_of_Land_Management_areas_in_Oregon dbc:Landforms_of_Lake_County,_Oregon dbc:Volcanoes_of_Oregon dbc:Protected_areas_of_Lake_County,_Oregon |
gold:hypernym |
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42.036836 -119.483265 |
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rdfs:comment |
The Doherty Slide is a prominent dissected rim of volcanic origin located in southeastern Oregon in the United States. It is located in rural Lake County, just north of the Nevada border. The ridge sits at the eastern end of the , approximately 20 miles (32 km) east of the town of Adel. (en) |
rdfs:label |
Doherty Slide (en) |
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freebase:Doherty Slide yago-res:Doherty Slide wikidata:Doherty Slide https://global.dbpedia.org/id/4iUjb |
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42.036835 (xsd:float) |
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wikipedia-en:Doherty_Slide?oldid=1053658655&ns=0 |
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