Boring Lava Field
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The Boring Lava Field is an extinct Plio-Pleistocene volcanic zone with at least 32 cinder cones and small shield volcanoes lying within a radius of 13 miles (21 km2) of Kelly Butte, which is approximately 4 miles east of downtown Portland, Oregon, in the United States. The name is derived from the town of Boring, Oregon which lies just to the southeast of the most dense cluster of lava vents. The zone became active 2.7 million years ago, and has been extinct for about 300,000 years.[[Citing sources citation needed]]
The Portland metropolitan area, including suburbs, is one of the few places in the continental US to have extinct volcanoes within a cities limits; Bend, Oregon is another.
Oregon Vents
- Chamberlain Hill - Elevation 980 feet
- Cook's Butte - Elevation 718 feet
- Kelly Butte - Elevation 590 feet
- Mount Scott - Elevation 1,050 feet
- Mount Tabor, Oregon - Elevation 641 feet (center of a large multi-use Portland city park)
- Powell Butte - Elevation 620 feet
- Rocky Butte - Elevation 612 feet (stone tower with outstanding view of Portland)
- Ross Mountain - Elevation 1,380 feet
- Swede Hill - Elevation 995 feet
- TV Hill - Elevation 1,275 feet
- Walker Peak - Elevation 2,450 feet
Washington Vents
- Battleground Lake - Elevation 750 feet (miniature crater lake)
- Bob's Mountain - Elevation 2,110 feet (contains intact summit crater)
- Brunner Hill - Elevation 680 feet
- Green Mountain - Elevation 804 feet (logged off during the First World War)
- Mount Norway - Elevation 1,111 feet
- Mount Pleasant - Elevation 1,010 feet
- Mount Zion - Elevation 1465 feet
- Nichol's Hill - Elevation 1,113 feet
- Pohl's Hill - Elevation 1,395 feet
- Prune Hill - Elevation 610 feet (overlooks Camas, Washington)
Map
[USGS Map of Boring Lava Field]External links
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