Template:Volcanoes of Oregon

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Volcanoes of Oregon v • d • e
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 | Larch Mtn)
Eastern Cascades		Pilot Butte | Lava Butte | Newberry Volcano | Yamsay Mtn
Basin and Range		Big Hole | Hole-in-the-Ground | Fort Rock	Columbia Plateau		Columbia River Basalt Group

This template should be placed at the bottom of articles about volcanoes in Oregon (see Category:Volcanoes of Oregon), to allow easy one-click navigation between them in some reasonable geographic order. Please add any missing or new volcano articles in the appropriate sections of the template, in north-south order for each of the Cascade sections and west-east order for the Basin and Range section.

[edit] Notes about the sections:

The High Cascades include volcanoes which are members of the main Cascade volcanic arc and located on or near the Cascade Crest, the main hydrologic divide along the length of the Cascade Range.

The Western Cascades include volcanoes on the west side of the range, most of which are very old eroded remnants (examples: Coffin Mtn, Iron Mtn), but there are also some more recent volcanoes such as the Boring Lava Field.

The Eastern Cascades or Cascade Back-Arc includes volcanoes in the back-arc on the east side of the range. This second, somewhat discontinuous, volcanic arc is about 20-30 miles east of the Cascade Crest, and it includes both older volcanoes (several million years old) and more recently active ones such as Newberry Volcano and its numerous associated cinder cones.

The Basin and Range includes volcanoes in eastern Oregon which are primarily the result of crustal extension or other mechanisms, in contrast to the Cascade volcanoes which are the result of subduction along the Cascadia subduction zone.

The Columbia Plateau includes a large igneous province of flood basalt, the Columbia River Basalt Group.