File:Columnar-jointed basalt (Columbia River Flood Basalt, Miocene, ~15-17 Ma; Mud Hollow, Oregon, USA) 1.jpg
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[edit]DescriptionColumnar-jointed basalt (Columbia River Flood Basalt, Miocene, ~15-17 Ma; Mud Hollow, Oregon, USA) 1.jpg |
English: Columnar-jointed basalt in the Miocene of Oregon, USA.
The vertical fractures seen here are columnar jointing. With cooling, many lava flows contract slightly after they solidify. Contraction results in the formation of polygonal columns - columnar jointing. As seen from above, the columns often have a hexagonal or pentagonal shape, but other shapes are known. Some famous examples include Devils Tower in Wyoming, Devil's Postpile in California, and Giant's Causeway in Ireland. The basalt lava flow seen here is part of the Columbia River Flood Basalt of Miocene age. Flood basalts are vast outpourings of lava from one or more large fractures in the crust. This rare type of volcanism is not occurring on Earth at present, but there are ancient flood basalt provinces that can be examined - for example, the latest Cretaceous-aged Deccan Traps of India and the latest Permian Siberian Traps of Russia. Flood lavas are also known on Mercury, Venus, and the Moon. Most of the Columbia River Flood Basalt erupted over a time span of a little over one million years, between 15 and 17 million years ago, during the Miocene. The deposit has been partially eroded, but covers much of Washington State and Oregon, plus parts of Idaho. Some lava reached the Pacific Ocean. The cause of the Columbia River Flood Basalt volcanism is not entirely settled, but is probably related to the initial emergence of the Yellowstone Hotspot mantle plume in the late Tertiary. Since it first appeared, the Yellowstone Hotspot has been moving ~eastward from the Oregon-California-Nevada area and is currently in northwestern Wyoming. In reality, the North American Plate is moving over the Yellowstone Hotspot. Locality: roadcut along Mud Hollow Road, south-southeast of the town of Biggs Junction, far-northern Oregon, USA Info. at: www.usgs.gov/observatories/cvo/columbia-river-basalt-grou... and en.wikipedia.org/wiki/Columbia_River_Basalt_Group |
Date | |
Source | https://www.flickr.com/photos/47445767@N05/53214835601/ |
Author | James St. John |
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/53214835601. It was reviewed on 11 October 2023 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
11 October 2023
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current | 15:47, 11 October 2023 | 4,288 × 2,848 (8.66 MB) | Ser Amantio di Nicolao (talk | contribs) | Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/53214835601/ with UploadWizard |
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File change date and time | 21:48, 25 September 2023 |
Y and C positioning | Co-sited |
Exposure Program | Not defined |
Exif version | 2.21 |
Date and time of digitizing | 13:45, 1 August 2012 |
Meaning of each component |
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File source | Digital still camera |
Scene type | A directly photographed image |
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White balance | Auto white balance |
Digital zoom ratio | 1 |
Focal length in 35 mm film | 27 mm |
Scene capture type | Standard |
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Date metadata was last modified | 17:48, 25 September 2023 |
Unique ID of original document | 5453DC4CD49BD70A0BD7071840403F60 |