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daryoush talati
The summit of South America’s Llullaillaco Volcano has an elevation
of 22,110 feet above sea level, making it the highest historically
active volcano in the world. The current stratovolcano--a cone-shaped
volcano built from successive layers of thick lava flows and eruption
products like ash and rock fragments--is built on top of an older
stratovolcano. The last explosive eruption of the volcano, based on
historical records, occurred in 1877.
This photograph of
Llullaillaco, taken from aboard the International Space Station,
illustrates an interesting volcanic feature known as a coulée. Coulées
are formed from highly viscous, thick lavas that flow onto a steep
surface. As they flow slowly downwards, the top of the flow cools and
forms a series of parallel ridges oriented at 90 degrees to the
direction of flow (somewhat similar in appearance to the pleats of an
accordion). The sides of the flow can also cool faster than the center,
leading to the formation of wall-like structures known as flow levees.
Llullaillaco is also a well-known archaeological site; the mummified
remains of three Inca children, ritually sacrificed 500 years ago, were
discovered on the summit in 1999.
Image Credit: NASA