Ladawan:SP crater NASA.jpg

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Sumaryo

Pagladawan
English: The Advanced Land Imager (ALI) on NASA’s Earth Observing-1 (EO-1) satellite captured this natural-color image on April 17, 2010.

SP Crater is a cinder cone, a conical structure made up of volcanic fragments, often glassy rocks containing bubbles of trapped gas. Cinder cones often form around or downwind from volcanic vents. When lava erupts from these structures, it frequently flows out of breaches on the side, and that appears to be the case at SP Crater. Like most volcanoes in this field, SP Crater is a basalt cinder cone. Basalt has low resistance to flow, so basalt lava flows tend to travel fairly far from the eruption source.

Forming a paisley pattern, the dark volcanic rocks north of SP Crater result from lava flows. (This image has been rotated and north is at right.) The hardened lava extends some 4 miles (6 kilometers) from the cinder cone, and is about 100 feet (30 meters) thick. Different dating techniques have placed the age of this lava between 4,000 and 71,000 years old.
Petsa
Pinagkunan https://earthobservatory.nasa.gov/images/49450/sp-crater-northern-arizona
Kagsurat NASA Earth Observatory image by Jesse Allen and Robert Simmon, using ALI data from the NASA EO-1 team.

Paglisensya

Public domain This file is in the public domain in the United States because it was solely created by NASA. NASA copyright policy states that "NASA material is not protected by copyright unless noted". (See Template:PD-USGov, NASA copyright policy page or JPL Image Use Policy.)
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presente17:21, 7 Disyembre 2019Thumbnail para sa bersyon kaitong 17:21, 7 Disyembre 2019720 × 360 (232 KB)Hike395{{Information |description ={{en|1=The Advanced Land Imager (ALI) on NASA’s Earth Observing-1 (EO-1) satellite captured this natural-color image on April 17, 2010. SP Crater is a cinder cone, a conical structure made up of volcanic fragments, often glassy rocks containing bubbles of trapped gas. Cinder cones often form around or downwind from volcanic vents. When lava erupts from these structures, it frequently flows out of breaches on the side, and that appears to be the case at SP Crater...

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