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About This GigaPanToggle
- Taken by
- Explore score
- 3.30 Gigapixels
- Date added
- August 05, 2011
- Date taken
- July 28, 2011
Whitney Falls occurs where Whitney Creek flows over a resistant 9,300 year old basaltic andesite lava flow. Melt water from the Whitney Glacier feeds Whitney Creek. The water in Whitney Creek is usually chocolate brown from the sediment eroded by the glacier and the creek as it flows down the northern flank of Mt Shasta.
The north side of Mt Shasta consists of basaltic andesite lava flows and unconsolidated pyroclastic, debris flow, and river (fluvial) deposits. Pyroclasitic material was deposited about 1800 hyears ago. Since this time, Whitney Creek has eroded this material, indicating that the Whitney gorge visible in this image was formed during the last 1800 years.
Across the gorge, the 9300 year-old basaltic andesite flow forms the stout western wall of the gorge.
The information here was extracted from Fuente and Bachmann (1999) and Hirt (1999), both in "Across the Klamath/Cascade Frontier", the NAGT Fall Field Conference guidebook.
GigaPan Stitch version 1.0.0805 (Windows)
Panorama size: 3299 megapixels (100372 x 32872 pixels)
Input images: 774 (43 columns by 18 rows)
Field of view: 158.9 degrees wide by 52.0 degrees high (top=20.2, bottom=-31.8)
All default settings
Original image properties:
Camera make: PENTAX
Camera model: PENTAX K-r
Image size: 4288x2848 (12.2 megapixels)
Capture time: 2011-07-28 14:01:25 - 2011-07-28 14:59:38
Exposure time: 0.004
Focal length (35mm equiv.): 315.0 mm
White balance: Fixed
Exposure mode: Manual
Horizontal overlap: 36.8 to 60.2 percent
Vertical overlap: 36.1 to 42.5 percent
Computer stats: 8098.69 MB RAM, 8 CPUs
Total time 9:05:44 (42 seconds per picture)
Alignment: 1:10:45, Projection: 15:17, Blending: 7:39:42
(Preview finished in 8:48:13)