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Head of Wind River Canyon, Wyoming by Callan Bentley

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About This Gigapan

Taken by
Callan Bentley Callan Bentley
Explore score
Print Pricing
$8.23 to $577.00
1.55 Gigapixels
Date added
Jul 31, 2013
Date taken
Jul 26, 2013

This is the south (upstream) end of Wind River Canyon, Wyoming, as viewed from the Lower Campground at Boysen State Park. The rocks here are Archean aged metamorphics.

A hand sample of schist from near this site may be viewed at this macro GigaPan:
A few granite dikes cross-cutting the metamorphics may also be picked out. Further downstream (north), these rocks are overlain by Paleozoic and Mesozoic sedimentary strata. The canyon formed during the Laramide Orogeny, as the Owl Creek Range was uplifted, and the Wind River cut downward. The Owl Creek mountains trend east-west, and the Wind River runs south-to-north at this location, providing a near-perfect cross-section through the local stratigraphy.

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Stitcher Notes


GigaPan Stitch version 2.1.0161 (Windows)
Panorama size: 1550 megapixels (48068 x 32252 pixels)
Input images: 323 (17 columns by 19 rows)
Field of view: 90.5 degrees wide by 60.7 degrees high (top=45.3, bottom=-15.4)
Vignette correction on: c1=0.00143 c2=-0.000941
All default settings
Original image properties:
Camera make: Canon
Camera model: Canon EOS 60D
Image size: 5184x3456 (17.9 megapixels)
Capture time: 2013-07-26 21:50:36 - 2013-07-26 22:12:13
Aperture: f/7.1
Exposure time: 0.0333333
ISO: 250
Focal length (35mm equiv.): 212.3 mm
White balance: Automatic
Exposure mode: Manual
Horizontal overlap: 49.1 to 63.0 percent
Vertical overlap: 52.4 to 54.5 percent
Computer stats: 3317.82 MB RAM, 4 CPUs
Total time 57:14 (11 seconds per picture)
Alignment: 9:05, Projection: 12:50, Blending: 35:19
(Preview finished in 31:14)

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