File:Upper Terraces of Mammoth Hot Springs.jpg
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Summary
[edit]DescriptionUpper Terraces of Mammoth Hot Springs.jpg |
English: Hot water is the creative force of the terraces. Even though Mammoth Hot Springs lie north of the caldera ring-fracture system, a fault trending north from Norris Geyser Basin, 21 miles (34 km) away, may connect Mammoth Hot Springs to the hot water of that system. A system of small fissures carries water upward to create approximately 50 hot springs in the Mammoth Hot Springs area. Another necessary ingredient for terrace growth is the mineral calcium carbonate. Thick layers of sedimentary limestone, deposited millions of years ago by vast seas, lie beneath the Mammoth area. As ground water seeps slowly downward and laterally, it comes in contact with hot gases charged with carbon dioxide rising from the magma chamber. Some carbon dioxide is readily dissolved in the hot water to form a weak carbonic acid solution. This hot, acidic solution dissolves great quantities of limestone as it works up through the rock layers to the surface hot springs. Once exposed to the open air, some of the carbon dioxide escapes from solution. As this happens, limestone can no longer remain in solution. A solid mineral reforms and is deposited as the travertine that forms the terraces. (The image caption was taken from here.)
Français : Hautes terrasses de Mammoth Hot Springs (Litt. « Les sources chaudes taille mammouth ». Les terrasses (ou plutôt les gours) de Mammoth hot springs ont une origine géologique assez complexe: Le site de Mammoth hot springs ne se trouve pas dans la Caldeira de Yellowstone, mais sur un substrat sédimentaire Calcaire. De l'eau chaude provenant du bassin de Norris situé à 34 km de là circule vers cette zone via un système de failles orientées nord-sud. Cette eau est chargée en Acide carbonique, ce qui lui confère la propriété de dissoudre le calcaire. Lorsque l'eau chaude chargée en calcaire émerge, une partie de l'acide carbonique s'évapore sous forme de dioxyde de carbone, et une partie du calcaire précipite, formant de gigantesques gours. |
Source | Own work |
Author | Brocken Inaglory |
Camera location | 44° 58′ 22″ N, 110° 42′ 17″ W | View this and other nearby images on: OpenStreetMap | 44.972778; -110.704722 |
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current | 02:08, 5 April 2009 | 2,100 × 1,493 (2.17 MB) | Mbz1 (talk | contribs) | improved quality | |
01:55, 5 April 2009 | 2,100 × 1,493 (2.3 MB) | Mbz1 (talk | contribs) | improved quality | ||
00:22, 29 March 2009 | 2,100 × 1,493 (2.31 MB) | Mbz1 (talk | contribs) | Improved quality | ||
14:54, 8 July 2008 | 2,100 × 1,493 (2.09 MB) | Mbz1 (talk | contribs) | {{Information |Description={{en|1=u}} |Source=Own work by uploader |Author=Mbz1 |Date= |Permission= |other_versions= }} {{ImageUpload|full}} |
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Camera manufacturer | Canon |
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Camera model | Canon EOS DIGITAL REBEL XTi |
Exposure time | 1/800 sec (0.00125) |
F-number | f/9 |
ISO speed rating | 100 |
Date and time of data generation | 15:17, 22 June 2008 |
Lens focal length | 30 mm |
Orientation | Normal |
Horizontal resolution | 72 dpi |
Vertical resolution | 72 dpi |
Software used | Adobe Photoshop CS3 Windows |
File change date and time | 19:06, 4 April 2009 |
Y and C positioning | Co-sited |
Exposure Program | Manual |
Exif version | 2.21 |
Date and time of digitizing | 15:17, 22 June 2008 |
Meaning of each component |
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APEX shutter speed | 9.6438598632812 |
APEX aperture | 6.33984375 |
APEX exposure bias | 0 |
Metering mode | Pattern |
Flash | Flash did not fire, compulsory flash suppression |
Supported Flashpix version | 1 |
Color space | sRGB |
Focal plane X resolution | 4,433.2953249715 |
Focal plane Y resolution | 4,453.6082474227 |
Focal plane resolution unit | inches |
Custom image processing | Normal process |
Exposure mode | Manual exposure |
White balance | Auto white balance |
Scene capture type | Standard |
Supported Flashpix version | 1 |
Image width | 2,100 px |
Image height | 1,493 px |
Date metadata was last modified | 12:06, 4 April 2009 |
IIM version | 2 |
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44°58'22.001"N, 110°42'16.999"W
0.00125 second
30 millimetre
100
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