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About This GigaPan
Toggle- Taken by
-
Manuel Sintubin
- Explore score
- 1
- Size
- 2.42 Gigapixels
- Views
- 830
- Date added
- May 06, 2011
- Date taken
- May 05, 2011
- Categories
- Galleries
- Geology in Belgium
- Competitions
- Tags
- ninglinspo, Ardenne, belgium, geology, unconformity, rocks
- Description
-
The famous unconformity at the northwestern border of the Lower Palaeozoic Stavelot-Venn basement inlier in the valley of the Ninglinspo (Belgium). The layers are overturned and dip to the south. On the outcrop the basal conglomerate and reddish claystone is exposed; both are of Lochkovian age. The slates below the unconformity are Cambrian in age.
If you want to know more about the Ardennian unconformities, please read our publication: dx.doi.org/10.1016/j.crte.2008.11.012
Stitcher Notes
ToggleMinimizeGigaPan Stitch version 1.0.0805 (Windows)
Panorama size: 2423 megapixels (63680 x 38060 pixels)
Input images: 374 (22 columns by 17 rows)
Field of view: 3.6 degrees wide by 2.2 degrees high (top=2.1, bottom=-0.1)
Settings:
All default settings
Original image properties:
Camera make: Panasonic
Camera model: DMC-FZ28
Image size: 3648x2736 (10.0 megapixels)
Capture time: 2011-05-05 08:27:28 - 2011-05-05 08:49:12
Aperture: f/5
Exposure time: 0.008 - 0.0666667
ISO: 100 - 400
Focal length (35mm equiv.): 486.0 mm
Digital zoom: off
White balance: Fixed
Exposure mode: Automatic
Horizontal overlap: 8.5 to 32.0 percent
Vertical overlap: 15.6 to 45.1 percent
Computer stats: 2038.37 MB RAM, 2 CPUs
Total time 13:36:42 (2:11 per picture)
Alignment: 5:43:51, Projection: 14:15, Blending: 7:38:36
(Preview finished in 6:18:59)
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