About: Arnold Lava Tube System

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The Arnold Lava Tube System (or Arnold system) is series of lava tubes in Deschutes County, Oregon, in the United States. It is located several miles southeast of the city of Bend. The system starts in the Deschutes National Forest on the northern flank of Newberry Volcano, heads northeast onto BLM land before finally terminating on private property near Horse Ridge. The system acted as a conduit for the lavas from Lava Top Butte that later fed the Badlands rootless shield. The lava flow that created the Arnold system is also referred to as the basalt of Lava Top Butte and is related to the Horse Cave lobe which is a lava flow that created the Horse Lava Tube System. The lava flows of Lava Top Butte, the Badlands, the Horse system, and the Arnold system all have a geologic age around 80,00

Attributes	Values
rdf:type	Thing place dbo:Location schema:Place natural place Cave cave yago:WikicatCavesOfOregon yago:WikicatLavaTubes geo:SpatialThing yago:Artifact100021939 yago:Cave109238926 yago:Conduit103089014 yago:GeologicalFormation109287968 yago:Object100002684 yago:Passage103895293 yago:PhysicalEntity100001930 yago:YagoGeoEntity yago:YagoPermanentlyLocatedEntity television show yago:Tube104493505 yago:Way104564698 yago:Whole100003553 umbel-rc:Cave
rdfs:label	Arnold Lava Tube System (en)
rdfs:comment	The Arnold Lava Tube System (or Arnold system) is series of lava tubes in Deschutes County, Oregon, in the United States. It is located several miles southeast of the city of Bend. The system starts in the Deschutes National Forest on the northern flank of Newberry Volcano, heads northeast onto BLM land before finally terminating on private property near Horse Ridge. The system acted as a conduit for the lavas from Lava Top Butte that later fed the Badlands rootless shield. The lava flow that created the Arnold system is also referred to as the basalt of Lava Top Butte and is related to the Horse Cave lobe which is a lava flow that created the Horse Lava Tube System. The lava flows of Lava Top Butte, the Badlands, the Horse system, and the Arnold system all have a geologic age around 80,00 (en)
foaf:name	Arnold Lava Tube System (en)
name	Arnold Lava Tube System (en)
geo:lat	43.820000 (xsd:float)
geo:long	-121.120003 (xsd:float)
foaf:depiction
location	Deschutes County, Oregon
dcterms:subject	Lava tubes Caves of Oregon Landforms of Deschutes County, Oregon
Wikipage page ID	23927024 (xsd:integer)
Wikipage revision ID	1021911742 (xsd:integer)
Link from a Wikipage to another Wikipage	Ronald Greeley Environmental degradation Bat Bend, Oregon Deschutes County, Oregon Deschutes National Forest Lava tubes Horse Ridge United States United States Forest Service Townsend's big-eared bat Conservation (ethic) Crook County, Oregon Gemstone NASA Oregon High Desert Grotto Caves of Oregon Landforms of Deschutes County, Oregon Stalagmites Horse Lava Tube System Bureau of Land Management Lava cave AD Cave gate Rock climbing Private property Recreation Lava tubes Hibernation Artifact (archaeology) Indigenous peoples of the Americas Mineral National Speleological Society Indigenous peoples of the Americas Newberry Volcano Oregon Oregon Badlands Wilderness Oregon Department of Geology and Mineral Industries Oregon Field Guide Radiocarbon dating Vandalism Rock art NASA Ames Research Center Redmond Caves Restoration ecology
Link from a Wikipage to an external page	http://ohdgrotto.caves.org/caves/cave-access http://www.opb.org/television/programs/ofg/segment/ice-caves/
sameAs	Arnold Lava Tube System Arnold Lava Tube System Arnold Lava Tube System Arnold Lava Tube System Arnold Lava Tube System
dbp:wikiPageUsesTemplate	dbt:Coord dbt:Reflist dbt:Infobox_cave
thumbnail	wiki-commons:Special:FilePath/Backbone_Cave.jpg?width=300
survey	Mostly complete (en)
location	Deschutes County, Oregon, United States (en)
photo	Backbone Cave.jpg (en)
photo caption	Entrance to Backbone Cave (en)
georss:point	43.82 -121.12
has abstract	The Arnold Lava Tube System (or Arnold system) is series of lava tubes in Deschutes County, Oregon, in the United States. It is located several miles southeast of the city of Bend. The system starts in the Deschutes National Forest on the northern flank of Newberry Volcano, heads northeast onto BLM land before finally terminating on private property near Horse Ridge. The system acted as a conduit for the lavas from Lava Top Butte that later fed the Badlands rootless shield. The lava flow that created the Arnold system is also referred to as the basalt of Lava Top Butte and is related to the Horse Cave lobe which is a lava flow that created the Horse Lava Tube System. The lava flows of Lava Top Butte, the Badlands, the Horse system, and the Arnold system all have a geologic age around 80,000 years old. (en)
access	Varied (en)

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