File:Gilsonite (uintaite) (Big Bonanza Vein intruded in the Uinta Formation, Middle Eocene; Bonanza, Utah, USA) 4.jpg
![File:Gilsonite (uintaite) (Big Bonanza Vein intruded in the Uinta Formation, Middle Eocene; Bonanza, Utah, USA) 4.jpg](https://upload.wikimedia.org/wikipedia/commons/thumb/e/e9/Gilsonite_%28uintaite%29_%28Big_Bonanza_Vein_intruded_in_the_Uinta_Formation%2C_Middle_Eocene%3B_Bonanza%2C_Utah%2C_USA%29_4.jpg/774px-Gilsonite_%28uintaite%29_%28Big_Bonanza_Vein_intruded_in_the_Uinta_Formation%2C_Middle_Eocene%3B_Bonanza%2C_Utah%2C_USA%29_4.jpg?20201018024259)
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[edit]DescriptionGilsonite (uintaite) (Big Bonanza Vein intruded in the Uinta Formation, Middle Eocene; Bonanza, Utah, USA) 4.jpg |
English: Gilsonite from the Tertiary of Utah, USA. (~7.4 centimetres (2.9 in) across at its widest)
Gilsonite (a.k.a. uintaite) is a variety of asphaltite - it's a solid hydrocarbon - basically solidified oil. Gilsonite usually has the appearance of obsidian or anthracite coal. It is jet black in color, very lightweight, brittle, and has a conchoidal fracture. The largest “deposits” of gilsonite in the world are in the Uinta Basin of northeastern Utah, USA. Gilsonite occurs there as vertical NW-SE trending veins intruded within the Eocene-aged Uinta Formation. The source of the hydrocarbons is organic-rich beds in the underlying Green River Formation (Eocene) and Wasatch Formation (Paleocene). Gilsonite is not readily combustible and is not a fuel, but it does have economic value. Gilsonite is mined in northeastern Utah and processed and is used in numerous products and applications (e.g., see: www.geospectra.net/kite/gilsonite/gilson.htm). Seen here is a gilsonite sample from the Big Bonanza Vein (also known as the Independent Dike or the Independent Vein; other names for the same dike include East Bonanza Vein and Bonanza Vein; the latter designation has been applied to more than 1 gilsonite vein in the area). The dike ranges from about 5 to 14 feet wide and averages over 10 feet wide over a 3 mile stretch. It intrudes the Uinta Formation and was probably emplaced ~10 to 30 million years ago. Locality: unrecorded/undisclosed locality along the Big Bonanza Vein (Independent Dike), near the town of Bonanza, eastern Uintah County, northeastern Utah, USA |
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Source | https://www.flickr.com/photos/47445767@N05/49035142238/ |
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@N05/49035142238. It was reviewed on 18 October 2020 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
18 October 2020
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Camera manufacturer | Canon |
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Camera model | Canon PowerShot D10 |
Exposure time | 1/60 sec (0.016666666666667) |
F-number | f/10 |
ISO speed rating | 80 |
Date and time of data generation | 15:51, 8 November 2019 |
Lens focal length | 9.681 mm |
Width | 4,000 px |
Height | 3,000 px |
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Pixel composition | RGB |
Orientation | Normal |
Number of components | 3 |
Horizontal resolution | 180 dpi |
Vertical resolution | 180 dpi |
Software used | Adobe Photoshop Elements 16.0 (Macintosh) |
File change date and time | 18:15, 8 November 2019 |
Y and C positioning | Co-sited |
Exif version | 2.21 |
Date and time of digitizing | 15:51, 8 November 2019 |
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Image compression mode | 3 |
APEX shutter speed | 5.90625 |
APEX aperture | 6.65625 |
APEX exposure bias | −0.66666666666667 |
Maximum land aperture | 3.625 APEX (f/3.51) |
Metering mode | Pattern |
Flash | Flash fired, compulsory flash firing, red-eye reduction mode |
Supported Flashpix version | 1 |
Color space | sRGB |
Focal plane X resolution | 16,460.905349794 |
Focal plane Y resolution | 16,483.516483516 |
Focal plane resolution unit | inches |
Sensing method | One-chip color area sensor |
File source | Digital still camera |
Custom image processing | Normal process |
Exposure mode | Manual exposure |
White balance | Auto white balance |
Digital zoom ratio | 1 |
Scene capture type | Standard |
Lens used | 6.2-18.6 mm |
Date metadata was last modified | 13:15, 8 November 2019 |
Unique ID of original document | FB88DA2758289C2FE88B94799AA2F9EE |