< ISS029-E-20003 >

Browse image
Resolutions offered for this image:
1000 x 682 pixels 540 x 368 pixels 720 x 540 pixels 4288 x 2848 pixels 640 x 425 pixels
Cloud masks available for this image:
Binary Heatmap

Spacecraft nadir point: 13.4° S, 71.9° W

Photo center point: 18.1° S, 69.2° W

Photo center point by machine learning:

Nadir to Photo Center: Southeast

Spacecraft Altitude: 211 nautical miles (391km)
Click for a map
Width Height Annotated Cropped Purpose Links
1000 pixels 682 pixels No Yes Earth From Space collection Download Image
540 pixels 368 pixels Yes Yes Earth From Space collection Download Image
720 pixels 540 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
Other options available:
Download Packaged File
Download a Google Earth KML for this Image
View photo footprint information
No GeoTIFF is available for this photo.
Image Caption: Parinacota Volcano, Chile-Bolivia Border Region, South America

Note: This caption refers to the image versions labeled "NASA's Earth Observatory web site".

Volcan Parinacota ("flamingo lake" in the regional Aymara language) is a potentially active stratovolcano located on the Altiplano, a high plateau situated within the Andes mountains of west-central South America. While no direct observations of eruptive activity are recorded, surface exposure age-dating of lava flows suggests that activity occurred as recently as 290 AD +- 300 years. Local Aymara stories also suggest that the volcano has erupted during the past 1000 years.

This detailed astronaut photograph from the International Space Station highlights the symmetrical cone of Parinacota, with its well-developed summit crater (elevation 6348 meters above sea level) at image center. Dark brown to dark gray surfaces to the east and west of the summit include lava flows, pyroclastic deposits, and ash. A companion volcano, Pomerape, is located across a low saddle to the north - this volcano last erupted during the Pleistocene Epoch (extending from approximately 3 million to 12,000 years ago). The summits of both volcanoes are covered by white permanent snowpack and small glaciers. Together, the two volcanoes form the Nevados de Payachata volcanic area.

Eruptive activity at Parinacota has directly influenced development of the local landscape beyond the emplacement of volcanic deposits - approximately 8,000 years ago the western flank of the volcano collapsed, creating a debris avalanche that traveled 22 km to the west. This debris avalanche blocked drainages, leading to the formation of Lake Chungara to the south (just visible at the lower left of this view). The uneven, hummocky surface of the debris avalanche deposit provides ample catchments for water, as evidenced by the numerous small ponds and Cotacotani Lake to the west.