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Statements

Subject Item
dbr:Sand_Mountain_Volcanic_Field
rdf:type
geo:SpatialThing
rdfs:label
Sand Mountain Volcanic Field
rdfs:comment
The Sand Mountain Volcanic Field (also known as the Sand Mountain Field) is a volcanic field in the upper McKenzie River watershed, located in the United States in Oregon. Part of the Cascade Volcanic Arc, it lies southwest of Mount Jefferson and northwest of Belknap Crater and Mount Washington. Its highest elevation is 5,463 feet (1,665 m).
dbp:name
Sand Mountain Volcanic Field
geo:lat
44.38000106811523
geo:long
-121.9300003051758
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dbo:thumbnail
n10:Sand_Mountain_volcanic_field.jpg?width=300
dbp:age
dbr:Holocene
dbp:location
dbr:Oregon dbr:United_States
dbp:photo
Sand Mountain volcanic field.jpg
dbp:photoCaption
View down the north–northeast alignment of the Sand Mountain Volcanic Field, with Mount Jefferson visible in the distance
dbp:range
dbr:Cascade_Range
dbp:type
dbr:Volcanic_field
georss:point
44.38 -121.93
dbo:abstract
The Sand Mountain Volcanic Field (also known as the Sand Mountain Field) is a volcanic field in the upper McKenzie River watershed, located in the United States in Oregon. Part of the Cascade Volcanic Arc, it lies southwest of Mount Jefferson and northwest of Belknap Crater and Mount Washington. Its highest elevation is 5,463 feet (1,665 m). Active during the Holocene epoch, the Sand Mountain Field began erupting about 4,000 years ago. The field includes 23 basaltic and basaltic andesitic cinder cones and lava flows, for a total of 42 volcanic vents within two roughly north–south trending alignments. Its total dense-rock equivalent eruptive output is 0.22 to 0.29 cubic miles (0.92 to 1.21 km3), with subfeatures including a tephra field and a lava tube system. Future activity is possible, but according to the Volcano Hazards Program of the United States Geological Survey, the threat from the field itself is low. The field lies within the Willamette National Forest near Santiam Pass. It supports some forested areas, which grow well on lava flows with tephra that serves as suitable soil for stands of Douglas fir and western hemlock and less commonly western red cedar. The surroundings represent an area of geological interest, and scoria has been quarried from one of the field's volcanic cones for highway supplies. Nearby tourist destinations include a ski resort, Tamolitch Falls, and Clear Lake.
dbp:lastEruption
6.31152E10
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