Blue Lake Crater
Maar · United States · 1136 m

- Tipo
- Maar
- Paese
- United States
- Regione
- North America Volcanic Regions / High Cascades Volcanic Arc
- Altitudine
- 1136 m
- Coordinate
- 44.413, -121.769
- Ultima eruzione
- 680
- Contesto tettonico
- Subduction zone / Continental crust (> 25 km)
- Forma vulcanica
- Minor (Basaltic)
- Roccia principale
- Basalt / Picro-Basalt
Sintesi geologica
Blue Lake Crater is a series of at least three overlapping explosion craters along a NE trend slightly east of the crest of the Cascade Range in the state of Oregon. Explosions through pre-existing bedrock about 1,300 years ago deposited basaltic bombs and cinders, and spread tephra to the E and SE during perhaps the youngest eruption in the Santiam and McKenzie Passes region. The eruption created an elongated, steep-walled crater with a low rim that rises about 50 m above adjacent topography. The crater is now filled by the 300 x 800 m Blue Lake, immediately west of the glacial moraine dammed Suttle Lake. A chain of spatter cones, 6 km to the SSW and about 4 km NE of Mount Washington, is aligned with Blue Lake Crater and has ejecta that are petrographically similar and may have been erupted at the same time.
Sintesi da Wikipedia
Riassunto in ingleseBlue Lake Crater is a maar, or a broad, low-relief volcanic crater, in the U.S. state of Oregon. Located in Jefferson County, it consists of three overlapping craters, which hold Blue Lake. The drainage basin for Blue Lake has very steep, forested slopes and is mostly part of the explosion crater left by the volcano's eruption. The volcano lies within the Metolius River basin, which supports a wide array of plant life, large and small mammals, and more than 80 bird species. A 2009 Oregon law designated the Metolius River basin as an area of critical concern, preventing large-scale development and protecting wildlife.
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Storia delle eruzioni
Cronologia dettagliata
- 680 (±200 anni)VEI ?Stima geologica680 – In corso
Link esterni
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