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 km) of Kelly Butte, which is approximately 4 miles (6 km) 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 at least 2.7 million years ago, and has been extinct for about 300,000 years.[1]
The Portland metropolitan area, including suburbs, is one of the few places in the continental US to have extinct volcanoes within a city's limits; Bend, Oregon is another.[citation needed]
| Volcanoes of Oregon | |
|---|---|
| High Cascades | Mt. Hood · Olallie Butte · Mt. Jefferson · Three Fingered Jack · Hogg Rock · Hoodoo Butte · Hayrick Butte · Black Butte · Mt. Washington · Belknap Crater · Black Crater · Three Sisters · Broken Top · Tumalo Mtn. · Mt. Bachelor · Maiden Peak · Diamond Peak · Howlock Mtn. · Mt. Thielsen · Mt. Bailey · Mt. Mazama / Crater Lake · Mt. Scott · Union Peak · Pelican Butte · Mt. McLoughlin · Aspen Butte |
| Western Cascades | Boring Lava Field (Mt. Sylvania · Mt. Tabor · Rocky Butte · Powell Butte · |
| Eastern Cascades | Pilot Butte · Lava Butte · Newberry Volcano · Yamsay Mtn. |
| Basin and Range | Big Hole · Hole-in-the-Ground · Fort Rock · Diamond Craters |
| Columbia Plateau | Columbia River Basalt Group |
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