Fort Rock Basin
Fort Rock Basin | ||
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Fort Rock , Fort Rock Basin |
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height | 1500 m mean altitude, altitude range 1,320 - 1,716 m | |
location | United States ( Oregon , United States ) | |
Mountains | Cascade Range (Cascade Range) | |
Coordinates | 43 ° 18 ′ 0 ″ N , 121 ° 0 ′ 0 ″ W | |
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Type | Maar area | |
Age of the rock | 50,000 to 100,000 years | |
Last eruption | about 50,000 years ago |
The Fort Rock Basin , also Fort Rock - Christmas Lake Valley Basin , is a former lake basin in the US state of Oregon that existed from the late Pliocene to the late Pleistocene . The Fort Rock Basin maar field comprises more than 30 phreatomagmatic landforms scattered over an area of more than 4,000 square kilometers.
Origin of volcanism
The Fort Rock Basin is part of the volcanic Cascade Range (Cascade Range), which extends from northern California to southern British Columbia extends. The subsurface of the cascade chain consists of fragments of the earth's crust that have been added to the west coast of North America ( accretion ) by the subduction of the Juan de Fuca plate since the Paleogene . For about five million years, the volcanic activity caused by the melting of the subducted earth's crust has been particularly brisk. Due to the composition of the rising magma ( andesite and dacite ), which is influenced by the crust material, volcanism is often explosive.
Moffitt Butte
Moffitt Butte is a basaltic tuff ring that has been cut up by erosion . It has a diameter of 1,400 m and is 122 m high. Moffitt Butte is not associated with a lake basin, as is the case with Fort Rock and Hole-in-the-Ground , but with the rise of magma into a groundwater- bearing layer. A series of tuff rings between Moffitt Butte and the Fort Rock Basin are strung on a line that might correspond to an early drainage line between the Fort Rock Basin and neighboring La Pine Basin. The crater floor of Moffitt Butte is about 80 m above the adjacent plain. A small volcanic vent, 520 m in diameter, surrounded by a tuff ring, sits on the southwest flank of Moffitt Butte. The crater of the small vent is filled with solidified lava that emerged from a volcanic dyke on its northwestern edge.
Table rock
Table Rock is the eroded remnant of a tuff volcano, which today has the shape of a symmetrical cone with a base diameter of 1,530 m and its top at a height of 360 m about 360 m. The cone has a lid made of flat basalt that once filled the crater. The erosion has removed the original volcanic cone, leaving the former lava lake in the crater. Volcanic dykes extend south and north of the former lava lake. On the lower flanks of the cone, the tuffs consist essentially of palagonitic lapilli ; near the summit, these palagonite tuffs are covered by massive layers of ash with volcanic bombs , which testify to the violent ejective volcanic activity that took place before the crater was filled with lava.
Major volcanoes of the Fort Rock Basin
Surname | height | Coordinates | Type | Last eruption | image |
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Big hole | 1,447.8 m | 43 ° 26 ′ N , 121 ° 19 ′ W. | Maar | probably 20,000 years ago | |
Black Hills | 1558 m | 43 ° 10 ′ N , 120 ° 41 ′ W. | Tuff ring / lava lake | ||
Boat-Wright Ranch | 43 ° 18 ′ N , 121 ° 11 ′ W. | Tuff ring | |||
Flat top | Tuff ring / lava lake | ||||
Flatiron | 1,354 m | 43 ° 21 ′ N , 120 ° 52 ′ W. | Tuff ring / lava lake | ||
Fort Rock | 1,431 m | 43 ° 22 ′ N , 121 ° 4 ′ W. | Tuff ring | 50,000 to 100,000 years ago | |
Hole-in-the-Ground | 43 ° 25 ′ N , 121 ° 12 ′ W. | Maar | 50,000 to 100,000 years ago | ||
Horning Bend | 43 ° 18 ′ N , 121 ° 2 ′ W. | Tuff ring | |||
Moffitt Butte | 43 ° 31 ' N , 121 ° 26' W | Tuff ring / lava lake | 50,000 to 100,000 years ago | ||
Reed rock | 43 ° 21 ′ N , 120 ° 44 ′ W. | Tuff ring / lava lake | |||
Ridge 28 | 43 ° 28 ′ N , 121 ° 26 ′ W. | Tuff ring | |||
St. Patrick Mountain | 1,764 m | 43 ° 7 ′ N , 120 ° 35 ′ W. | Tuff ring / lava lake | ||
Sand rock | 1,405 m | 43 ° 22 ′ N , 120 ° 19 ′ W. | Tuff ring | 50,000 to 100,000 years ago | |
Seven-Mile Ridge | 1,324 m | 43 ° 13 ′ N , 120 ° 43 ′ W. | Tuff ring | ||
South Green Mountain | 43 ° 21 ′ N , 120 ° 42 ′ W. | Tuff ring | |||
Table Mountain | 1,387 m | 43 ° 24 ' N , 120 ° 51' W. | Tuff ring / lava lake | ||
Table rock | 43 ° 10 ′ N , 120 ° 53 ′ W. | Tuff ring / tuff cone / lava lake | 50,000 to 100,000 years ago | ||
Wastina | 43 ° 18 ′ N , 121 ° 11 ′ W. | Tuff ring | |||
Wildcat Butte | 43 ° 18 ′ N , 120 ° 20 ′ W. | Tuff ring |
Individual evidence
- ↑ a b c d e f g h i j k l m n o p q Oregon Volcanoes - Fort Rock Basin Maar Field. In: Deschutes & Ochoco National Forests - Crooked River National Grassland. United States Forest Service , January 9, 2004, accessed September 19, 2008 .
- ^ RV Fisher, NV Peterson, GH Heiken: A Field Trip to the Maar Volcanoes of the Fort Rock - Christmas Lake Valley Basin, Oregon. In: Geological Survey Circular 838: Guides to Some Volcanic Terrances in Washington, Idaho, Oregon, and Northern California. United States Geological Survey , March 28, 2006, accessed September 19, 2008 .
- ↑ Jurgen Kienle, Charles A. Wood: Volcanoes of North America . Cambridge University Press, 1993, ISBN 0-521-43811-X , pp. 203-204 .
- ^ Gerhard H. Eisbacher: North America . In: Geology of the Earth . 1st edition. tape 2 . Ferdinand Enke Verlag, Stuttgart 1986, ISBN 3-432-96901-5 .
- ^ A b Oregon Volcanoes - Moffitt Butte Volcano. In: Deschutes & Ochoco National Forests - Crooked River National Grassland. United States Forest Service , January 9, 2004, accessed September 20, 2008 .
- ^ A b Oregon Volcanoes - Table Rock Volcano. In: Deschutes & Ochoco National Forests - Crooked River National Grassland. United States Forest Service , November 26, 2003, accessed September 20, 2008 .
- ↑ Volker Lorenz: Some Aspects of the Eruption Mechanism of the Big Hole Maar, Central Oregon . In: Geological Society of America Bulletin . tape 81 , no. 6 . Geological Society of America , 1970, pp. 1823-1830 , doi : 10.1130 / 0016-7606 (1970) 81 [1823: SAOTEM] 2.0.CO; 2 .
- ^ Oregon Volcanoes - Fort Rock Volcano. In: Deschutes & Ochoco National Forests - Crooked River National Grassland. United States Forest Service , December 24, 2003, accessed September 20, 2008 .
- ^ Oregon Volcanoes - Hole-in-the-Ground Volcano. In: Deschutes & Ochoco National Forests - Crooked River National Grassland. United States Forest Service , December 24, 2003, accessed September 20, 2008 .
- ^ Oregon Volcanoes - Sand Rock Volcano. In: Deschutes & Ochoco National Forests - Crooked River National Grassland. United States Forest Service , January 9, 2004, accessed September 20, 2008 .