STS106-707-51
| NASA Photo ID | STS106-707-51 |
| Focal Length | 40mm |
| Date taken | 2000.09.__ |
| Time taken | GMT |
Resolutions offered for this image:
1031 x 1024 pixels 2063 x 2048 pixels 4127 x 4096 pixels 515 x 512 pixels 1296 x 1284 pixels 400 x 396 pixels
1031 x 1024 pixels 2063 x 2048 pixels 4127 x 4096 pixels 515 x 512 pixels 1296 x 1284 pixels 400 x 396 pixels
Cloud masks available for this image:
Spacecraft nadir point:
Photo center point: 37.5° N, 22.5° E
Photo center point by machine learning:
Photo center point: 37.5° N, 22.5° E
Photo center point by machine learning:
Nadir to Photo Center:
Spacecraft Altitude: nautical miles (0km)
Country or Geographic Name: | GREECE |
Features: | PAN-PELOPONNISOS, ISLANDS |
| Features Found Using Machine Learning: | |
Cloud Cover Percentage: | 25 (11-25)% |
Sun Elevation Angle: | ° |
Sun Azimuth: | ° |
Camera: | Hasselblad |
Focal Length: | 40mm |
Camera Tilt: | High Oblique |
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 | |
| 1296 pixels | 1284 pixels | No | No | Download Image | |
| 400 pixels | 396 pixels | Download Image |
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Image Caption: Source: Patricia W. Dickerson
Aegean Sea
Crete (foreground), the Cyclades Islands, Greece and Turkey lie along
the margin of the Eurasian and African tectonic plates; Africa is moving
northward and being driven down beneath Eurasia. As a result volcanic
islands, such as Santorini, develop and fault-bounded basisn such, as
the Gulf of Corinth, are formed. In addition, lavas and sediments that
were originally deposited on the Mediterranean seafloor are uplifted and
deformed. The light-colored masses that extend along a NW-trending line
from the Peloponnesos into the Balkans consist of such uplifted marine
sediments.
Aegean Sea
Crete (foreground), the Cyclades Islands, Greece and Turkey lie along
the margin of the Eurasian and African tectonic plates; Africa is moving
northward and being driven down beneath Eurasia. As a result volcanic
islands, such as Santorini, develop and fault-bounded basisn such, as
the Gulf of Corinth, are formed. In addition, lavas and sediments that
were originally deposited on the Mediterranean seafloor are uplifted and
deformed. The light-colored masses that extend along a NW-trending line
from the Peloponnesos into the Balkans consist of such uplifted marine
sediments.
