stratovolcano
- Also called:
- composite volcano
- Related Topics:
- volcano
- andesite
- caldera
- dacite
- subduction zone
stratovolcano, volcanic landform characterized by a conical shape formed by layers of volcanic material deposited during successive volcanic eruptions. Stratovolcanoes tend to slope gently at the base but rise quickly near the summit to form tall mountain peaks. They are typically found above subduction zones, and they are often part of large volcanically active regions, such as the Ring of Fire that frames much of the Pacific Ocean. There are more than 700 known volcanoes classified as stratovolcanoes, many more than any other volcanic formation. Several are among the best-known volcanoes because of their striking appearance and their notoriety for some of the most-spectacular eruptions in history.
Development and features
Stratovolcanoes develop over many thousands of years through repeated eruptions and other volcanic activity. They are among the most-complex volcanic formations, and a single stratovolcano may be composed of mixed layers of ash, mud, solidified lava flows, volcanic domes (large hill-like bulges of solidified magma), and pyroclastic material (fluidized mixtures of hot rock fragments and gases that move rapidly down slopes). Because these layers are deposited in uneven overlapping concentrations rather than in neat strata, many scientists prefer the term composite volcano.
This unevenness of deposition allows for the development of several vents from which gas and magma can escape. Typically, a stratovolcano has one primary vent near its peak. This vent is often located within a crater, where material has been blasted away during one or more previous eruptions. The crater may be filled with water or ice, or it may contain a volcanic dome during a period of relative inactivity. Craters are often unstable features, with the location of the vent changing over time. Other vents associated with the volcano include fumaroles, which emit gas and vapour.
The andesite and dacite rocks common to stratovolcanoes produce cooler and more-viscous lavas than the basalt rocks common to shield volcanoes, which produce faster-moving and less-viscous lavas. Thick extrusions pile up on previous volcanic deposits around the vent of the stratovolcano, and multiple eruptions occurring over thousands of years culminate in tall cone-shaped peaks.
During an eruption, as magma escapes from a chamber within the mountain, a large section of the rock above may give way, and the chamber may collapse. The result is a a large bowl-shaped volcanic depression called a caldera. Calderas are many times larger than the vents that often appear near the top of a stratovolcano, and they are also larger than volcanic craters.
A stratovolcano’s steep slope and composite structure makes its flanks particularly vulnerable to lahars (mudflows of volcanic material), avalanches, and landslides caused by the collapse of large sections of the mountain. Lahars may be the product of an eruption, or they may result from heavy rain on loose ash or from an unusually quick melt of ice. The massive flow of water, ash, rock, and other volcanic debris can travel great distances to impact communities far from the volcano.
Eruption examples
Several of the most-famous volcanic disasters in history resulted from the eruptions of stratovolcanoes. The eruptions of Mount Vesuvius (79 ce), Mount Tambora (1815), Krakatoa (1883), Novarupta (1912), and Mount Pinatubo (1991) caused tremendous damage, loss of life, and climatic disruption. The 1985 eruption of Mount Ruiz, a stratovolcano in Colombia’s Cordillera Central, melted the volcano’s snowcap and sent downslope great mudflows that destroyed the city of Armero and killed more than 25,000 people.
