File:Multiple Igneous Intrusion Phases Kosterhavet Sweden.jpg
Original file (2,112 × 2,816 pixels, file size: 2.49 MB, MIME type: image/jpeg)
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Summary
[edit]DescriptionMultiple Igneous Intrusion Phases Kosterhavet Sweden.jpg |
English: An igneous intrusion cut by a pegmatite dyke, which in turn is cut by a dolerite dyke. These rocks are of Precambrian (Proterozoic) age and they are located in Kosterhavet National Park on Yttre Ursholmen island in the Koster Islands in Sweden. The oldest igneous rocks in this photo show features caused by magma mingling or magma mixing. |
Date | |
Source | https://www.flickr.com/photos/geologicalsurveyofsweden/5128430135/in/set-72157625147499901 |
Author | Thomas Eliasson of Geological Survey of Sweden https://www.flickr.com/people/geologicalsurveyofsweden/ |
Camera location | 58° 53′ 42.89″ N, 10° 59′ 00.27″ E | View this and other nearby images on: OpenStreetMap | 58.895246; 10.983409 |
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Licensing
[edit]This image was originally posted to Flickr by Geological Survey of Sweden at https://www.flickr.com/photos/55118510@N03/5128430135. It was reviewed on 1 December 2013 by FlickreviewR and was confirmed to be licensed under the terms of the cc-by-2.0. |
1 December 2013
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Annotations InfoField | This image is annotated: View the annotations at Commons |
These are the oldest rocks in this photo. They are an igneous intrusion that formed by magma mixing or magma mingling.
These are the oldest rocks in this photo. They are an igneous intrusion that formed by magma mixing or magma mingling.
Pegmatite dyke
Dolerite dyke, the youngest rock in this photo.
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current | 16:06, 1 December 2013 | 2,112 × 2,816 (2.49 MB) | GeoWriter (talk | contribs) | User created page with UploadWizard |
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Metadata
This file contains additional information such as Exif metadata which may have been added by the digital camera, scanner, or software program used to create or digitize it. If the file has been modified from its original state, some details such as the timestamp may not fully reflect those of the original file. The timestamp is only as accurate as the clock in the camera, and it may be completely wrong.
Camera manufacturer | NIKON |
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Camera model | COOLPIX S10 |
Exposure time | 2/1,111 sec (0.0018001800180018) |
F-number | f/4 |
ISO speed rating | 50 |
Date and time of data generation | 09:33, 23 August 2008 |
Lens focal length | 6.3 mm |
Orientation | Normal |
Horizontal resolution | 300 dpi |
Vertical resolution | 300 dpi |
Software used | COOLPIX S10V1.0 |
File change date and time | 09:33, 23 August 2008 |
Y and C positioning | Co-sited |
Exposure Program | Normal program |
Exif version | 2.2 |
Date and time of digitizing | 09:33, 23 August 2008 |
Meaning of each component |
|
Image compression mode | 2 |
APEX exposure bias | 0 |
Maximum land aperture | 3.6 APEX (f/3.48) |
Metering mode | Pattern |
Light source | Unknown |
Flash | Flash did not fire, compulsory flash suppression |
Supported Flashpix version | 1 |
Color space | sRGB |
File source | Digital still camera |
Scene type | A directly photographed image |
Custom image processing | Normal process |
Exposure mode | Auto exposure |
White balance | Auto white balance |
Digital zoom ratio | 0 |
Focal length in 35 mm film | 38 mm |
Scene capture type | Standard |
Scene control | None |
Contrast | Normal |
Saturation | Normal |
Sharpness | Normal |
Subject distance range | Unknown |