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About This GigaPan
Toggle- Taken by
-
Robin Rohrback-Schiavone
- Explore score
- 1
- Size
- 1.01 Gigapixels
- Views
- 387
- Date added
- December 01, 2012
- Date taken
- December 01, 2012
- Categories
- Galleries
- Competitions
- Tags
- m.a.g.i.c., geology, quartzite, metabasalt, Weverton, Catoctin, boulder, cobble, milky quartz, vein, blockfield, boulder field, gelifluction, Devil's Racecourse, South Mountain, lichen
- Description
-
Devil's Racecourse in Ft. Ritchie, MD is a 700-meter-long blockfield created when the area experienced a periglacial climate during the Pleistocene. It is thought that boulders of Weverton quartzite from South Mountain on the west and Catoctin metabasalt from the east weathered out of their respective mountains and were gradually transported and deposited here by gelifluction. In non-dry periods, visitors to Devil's Racecourse can hear a stream running beneath the blockfield, and can even see it if they peer down the right holes.
This was shot on a foggy December morning. During the half hour or so it took to shoot, the fog burned off and the sun came out.
View is to the north.
Stitcher Notes
ToggleMinimizeGigaPan Stitch.Efx version 2.1.0161 (Windows)
Panorama size: 1012 megapixels (66072 x 15328 pixels)
Input images: 350 (35 columns by 10 rows)
Field of view: 68.7 degrees wide by 15.9 degrees high (top=-14.9, bottom=-30.9)
Settings:
Vignette correction on: c1=-0.0199 c2=-0.0392
All default settings
Original image properties:
Camera make: Canon
Camera model: Canon PowerShot SX260 HS
Image size: 4000x3000 (12.0 megapixels)
Capture time: 2012-12-01 11:07:35 - 2012-12-01 11:30:42
Aperture: f/6.8
Exposure time: 0.00125 - 0.008
ISO: 100 - 800
Focal length (35mm equiv.): 502.6 mm
Digital zoom: off
White balance: Automatic
Exposure mode: Automatic
Horizontal overlap: 53.5 to 63.6 percent
Vertical overlap: 49.7 to 58.2 percent
Computer stats: 3996.82 MB RAM, 2 CPUs
Total time 1:27:22 (15 seconds per picture)
Alignment: 45:27, Projection: 10:28, Blending: 31:26
(Preview finished in 1:02:41)

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