< STS51A-36-71 >
| NASA Photo ID | STS51A-36-71 |
| Focal Length | 250mm |
| Date taken | 1984.11.11 |
| Time taken | 14:24:50 GMT |
Cloud masks available for this image:
Country or Geographic Name: | CUBA |
Features: | BAY OF CORTES |
| Features Found Using Machine Learning: | |
Cloud Cover Percentage: | 0 (no clouds present) |
Sun Elevation Angle: | 32° |
Sun Azimuth: | 128° |
Camera: | Hasselblad |
Focal Length: | 250mm |
Camera Tilt: | 18 degrees |
Format: | 6017: Kodak Ektachrome 64, 220 Roll Format |
Film Exposure: | Normal |
| Additional Information | |
| Width | Height | Annotated | Cropped | Purpose | Links |
|---|---|---|---|---|---|
| 5700 pixels | 5900 pixels | No | No | Download Image | |
| 483 pixels | 500 pixels | No | No | Download Image | |
| 640 pixels | 480 pixels | No | No | Download Image |
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No GeoTIFF is available for this photo.Image Caption:
Western Cuba
Western end of Cuba is a complex geologic region. The Sierra de
los Organos is a folded sequence of Cretaceous sedimentary rocks
that form a low range of mountains that rise to about 2800 feet
in elevation. Oligocene and Miocene marine sediments extend
south and east of these mountains. Quaternary coastal terrace
and beach deposits line most of the southern shore area around
the Gulf of Batabano. Karst topography, created by limestone
solution weathering is visible (characterized by many natural
lakes) at the southwestern quadrant of this photograph. (51A-
36-071)
Western Cuba
Western end of Cuba is a complex geologic region. The Sierra de
los Organos is a folded sequence of Cretaceous sedimentary rocks
that form a low range of mountains that rise to about 2800 feet
in elevation. Oligocene and Miocene marine sediments extend
south and east of these mountains. Quaternary coastal terrace
and beach deposits line most of the southern shore area around
the Gulf of Batabano. Karst topography, created by limestone
solution weathering is visible (characterized by many natural
lakes) at the southwestern quadrant of this photograph. (51A-
36-071)

