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About This GigaPanToggle
- Taken by
- Jen Piatek
- Explore score
- 0.22 Gigapixels
- Date added
- November 03, 2010
- Date taken
- August 06, 2009
Now a ski slope, this pile of rock formed as a mass of ice and rock that flowed downhill. The surface topography is partly due to compression of the debris as it flowed (plus later human modification).
This type of glacial/periglacial feature is thought to be an analog for features called debris aprons found at the base of massifs on Mars.
GigaPan Stitcher version 0.4.3865 (Macintosh)
Panorama size: 220 megapixels (29123 x 7565 pixels)
Input images: 80 (16 columns by 5 rows)
Field of view: 124.1 degrees wide by 32.2 degrees high (top=29.9, bottom=-2.3)
Use larger blending region
Original image properties:
Camera make: Canon
Camera model: Canon PowerShot SD850 IS
Image size: 3264x2448 (8.0 megapixels)
Capture time: 2009-08-06 13:40:30 - 2009-08-06 13:46:57
Exposure time: 0.000625 - 0.01
Focal length (35mm equiv.): 140.4 mm
Digital zoom: off
White balance: Fixed
Exposure mode: Automatic
Horizontal overlap: 46.8 to 53.8 percent
Vertical overlap: 47.3 to 50.7 percent
Computer stats: 2560 MB RAM, 2 CPUs
Total time 1:07:22 (0:50 per picture)
Alignment: 6:24, Projection: 4:26, Blending: 56:31