STS099-749-63
| NASA Photo ID | STS099-749-63 |
| Focal Length | 100mm |
| Date taken | 2000.02.__ |
| Time taken | GMT |
Resolutions offered for this image:
1031 x 1024 pixels 2063 x 2048 pixels 4127 x 4096 pixels 515 x 512 pixels
1031 x 1024 pixels 2063 x 2048 pixels 4127 x 4096 pixels 515 x 512 pixels
Cloud masks available for this image:
Spacecraft nadir point:
Photo center point: 51.5° N, 68.5° W
Photo center point by machine learning:
Photo center point: 51.5° N, 68.5° W
Photo center point by machine learning:
Nadir to Photo Center:
Spacecraft Altitude: nautical miles (0km)
Country or Geographic Name: | CANADA-Q |
Features: | MANICOUAGAN RESERVOIR |
| Features Found Using Machine Learning: | |
Cloud Cover Percentage: | 10 (1-10)% |
Sun Elevation Angle: | ° |
Sun Azimuth: | ° |
Camera: | Hasselblad |
Focal Length: | 100mm |
Camera Tilt: | |
Format: | 5069: Kodak Elite 100S, E6 Reversal, Replaces Lumiere, Warmer in tone vs. Lumiere |
Film Exposure: | |
| Additional Information | |
| Width | Height | Annotated | Cropped | Purpose | Links |
|---|---|---|---|---|---|
| 1031 pixels | 1024 pixels | No | No | Download Image | |
| 2063 pixels | 2048 pixels | No | No | Download Image | |
| 4127 pixels | 4096 pixels | No | No | Download Image | |
| 515 pixels | 512 pixels | No | No | Download Image |
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Image Caption: Manicouagan Impact Crater, Quebec, Canada
One of the largest and most famous craters in Canada is Manicouagan.
Lake Manicouagan and Lake Mushalagan, frozen in this image, surround the
central uplift of the crater. The original crater diameter was 100
kilometers and the age has been dated at 214 million years.
Shattercones, striated features found in rocks deformed by the passage
of shock waves, and shattered and brecciated rocks found in the central
uplift confirm the crater's impact origin.
One of the largest and most famous craters in Canada is Manicouagan.
Lake Manicouagan and Lake Mushalagan, frozen in this image, surround the
central uplift of the crater. The original crater diameter was 100
kilometers and the age has been dated at 214 million years.
Shattercones, striated features found in rocks deformed by the passage
of shock waves, and shattered and brecciated rocks found in the central
uplift confirm the crater's impact origin.
