ISS032-E-16579
| NASA Photo ID | ISS032-E-16579 |
| Focal Length | 180mm |
| Date taken | 2012.08.11 |
| Time taken | 21:22:13 GMT |
Resolutions offered for this image:
1000 x 664 pixels 540 x 359 pixels 720 x 480 pixels 4288 x 2848 pixels 640 x 425 pixels
1000 x 664 pixels 540 x 359 pixels 720 x 480 pixels 4288 x 2848 pixels 640 x 425 pixels
Cloud masks available for this image:
Spacecraft nadir point: 5.5° S, 81.5° W
Photo center point: 4.8° S, 81.2° W
Photo center point by machine learning:
Photo center point: 4.8° S, 81.2° W
Photo center point by machine learning:
Nadir to Photo Center: North
Spacecraft Altitude: 217 nautical miles (402km)
Country or Geographic Name: | PERU |
Features: | STRAND PLAIN, CHIRA R. AGR., BALCONES PT. |
| Features Found Using Machine Learning: | |
Cloud Cover Percentage: | 10 (1-10)% |
Sun Elevation Angle: | 29° |
Sun Azimuth: | 291° |
Camera: | Nikon D2Xs Electronic Still Camera |
Focal Length: | 180mm |
Camera Tilt: | 12 degrees |
Format: | 4288E: 4288 x 2848 pixel CMOS sensor, RGBG imager color filter |
Film Exposure: | |
| Additional Information | |
| Width | Height | Annotated | Cropped | Purpose | Links |
|---|---|---|---|---|---|
| 1000 pixels | 664 pixels | No | Yes | Earth From Space collection | Download Image |
| 540 pixels | 359 pixels | Yes | Yes | Earth From Space collection | Download Image |
| 720 pixels | 480 pixels | Yes | Yes | NASA's Earth Observatory web site | Download Image |
| 4288 pixels | 2848 pixels | No | No | Download Image | |
| 640 pixels | 425 pixels | No | No | Download Image |
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Image Caption: Strandplain, coastal Peru
Note: This caption refers to the image versions labeled "NASA's Earth Observatory web site".
The scale and orientation of landscape features that are difficult to see on the ground often become readily visible from orbit. Numerous subparallel lines (image center) along the arid, northern coast of Peru (about 5 degrees south of the Equator) are close-packed beach ridges, known collectively as a strandplain (for scale, the strandplain is 30 km long). Each ridge shows the position of a prior shoreline. The Chira River delta appears at image right, with dark green agricultural fields occupying the delta of the river. A smaller river reaches the sea, without forming a delta, at image extreme left. The prominent cape at lower left is Punta Balcones, a region with many oil wells.
Strandplains are built by successive additions of beach sand usually from some nearby source. Currents on this coast of South America come from the south, suggesting that the Chira River delta (image right) is the source of the sand. The newest beach is being formed today by the waves--which appear as the thin ragged white line along the strandplain--supplied by the north-flowing current. The regularity of the spacing of the beaches suggests that some episodic influx of sediment controls beach formation. This influx may be determined by floods coming down the Chira River, possibly controlled by the heavy rains of El Nino events which occur irregularly every few years.
Two other sets of faint parallel lines can be seen on higher ground inland (between arrows, image center and image top right), the upper set stretching all the way from the Chira river floodplain. Seen in many places along the coast of Peru, these may also be strandplains (i.e. formed at sea level) generated when the land surface was at a lower altitude; both also may have been produced by sand from the Chira River. The land surface is known to be rising along this coast with the rise of the Andes Mts. (outside the top of the image), explaining why the upper shorelines now lie 120 meters above sea level.
Note: This caption refers to the image versions labeled "NASA's Earth Observatory web site".
The scale and orientation of landscape features that are difficult to see on the ground often become readily visible from orbit. Numerous subparallel lines (image center) along the arid, northern coast of Peru (about 5 degrees south of the Equator) are close-packed beach ridges, known collectively as a strandplain (for scale, the strandplain is 30 km long). Each ridge shows the position of a prior shoreline. The Chira River delta appears at image right, with dark green agricultural fields occupying the delta of the river. A smaller river reaches the sea, without forming a delta, at image extreme left. The prominent cape at lower left is Punta Balcones, a region with many oil wells.
Strandplains are built by successive additions of beach sand usually from some nearby source. Currents on this coast of South America come from the south, suggesting that the Chira River delta (image right) is the source of the sand. The newest beach is being formed today by the waves--which appear as the thin ragged white line along the strandplain--supplied by the north-flowing current. The regularity of the spacing of the beaches suggests that some episodic influx of sediment controls beach formation. This influx may be determined by floods coming down the Chira River, possibly controlled by the heavy rains of El Nino events which occur irregularly every few years.
Two other sets of faint parallel lines can be seen on higher ground inland (between arrows, image center and image top right), the upper set stretching all the way from the Chira river floodplain. Seen in many places along the coast of Peru, these may also be strandplains (i.e. formed at sea level) generated when the land surface was at a lower altitude; both also may have been produced by sand from the Chira River. The land surface is known to be rising along this coast with the rise of the Andes Mts. (outside the top of the image), explaining why the upper shorelines now lie 120 meters above sea level.
