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About: Boring Lava Field     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : umbel-rc:Mountain, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: yago:WikicatCascadeVolcanoesyago:WikicatLavaFieldsyago:WikicatVolcanicFieldsOfTheWesternUnitedStatesyago:WikicatVolcanoesOfOregonyago:WikicatVolcanoesOfWashington(state)geo:SpatialThingyago:WikicatSubductionVolcanoesyago:Abstraction100002137yago:AmorphousShape113867492yago:Attribute100024264yago:Crack109258715yago:Field108569998yago:GeographicalArea108574314yago:Location100027167yago:Object100002684yago:Opening109379111yago:PhysicalEntity100001930yago:Region108630985yago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntitysettlementyago:Shape100027807yago:Space113910384yago:Tract108673395yago:Vent109470550yago:WikicatExtinctVolcanoesmountain rangeumbel-rc:Mountain New Facet based on Instances of this Class

The Boring Lava Field (also known as the Boring Volcanic Field) is a Plio-Pleistocene volcanic field with cinder cones, small shield volcanoes, and lava flows in the northern Willamette Valley of the U.S. state of Oregon and adjacent southwest Washington state. The field got its name from the town of Boring, Oregon, located 12 miles (19 km) southeast of downtown Portland. Boring lies southeast of the most dense cluster of lava vents. The zone became volcanically active about 2.7 million years ago, with long periods of eruptive activity interspersed with quiescence. Its last eruptions took place about 57,000 years ago at the Beacon Rock cinder cone volcano; the individual volcanic vents of the field are considered extinct, but the field itself is not.