Discover the Andes

Excursion guide Movies Photos Presentations


by Martin Mergili

General information

When an oceanic plate of the Earth's crust steeply dives beneath another - oceanic or continental - plate, melting of some parts of the upper mantle is often the consequence. The resulting magma rises and, when reaching the Earth surface, appars as lava or pyroclastic material in a more or less explosive way. The molten rock is usually quite viscous, whereas different types of vocanic material can form slopes within a broad range of inclination angles. This si the principle of the formation of stratovolcanoes. Through the subduction of the Nazca Plate beneath the South America Plate along almost the entire Andes, stratovolanos are very common here. Many of them are extinct or dormant, whereas others erupt from time to time, challenging the society to cope with the consequences in the most appropriate way.

Click into the title image to visit a number of traovolcanoes in the Andes. Do you know the one or the other of them? But be careful: two of the photos are not from the Ades, and one of them even does not show a stratovolcano. Track down the cuckoo's eggs!

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Mt. Ngauruhoe is a classic example of a stratovolcano - but it is located on New Zealand's North Island. The Mauna Loa on Hawaii Big Island represents a nice example of a shield volcano.

Layers and more layers

As Eva-Maria shows us ere on the example of the Villarrica volcano in Southern Chile, stratovolcanoes have got their name from the sequence of layers (or strata) of different origin, colour, thickness, and resistance against weathering and erosion. In contrast to shield vocanoes, which are usually dominated by solidified lava flows, pyroclastic deposits are more common on the slopes of stratovolcanoes, as it can be seen in this photograph.

Visit the contribution on the Cordillera de la Sal to see another nice example of pyroclastic deposits. In the following exercise, you can drive a small part of the story of a stratovolcano by yourself and learn more about the origin of individual layers.


A short episode from the history of a volcano

This stratovolcano can already tell you a long story. Over time, eruptions of different types led to the deposition of one layer after the other - partly of lava, ánd partly of pyroclastic material. Just right now, the magma chamber beneath the volcano fills up again with andesitic magma: this type of magma is quite common in the Andes and has an intermediate content of silica, and intermediate viscosity.

Click into the magma chamber to activate the volcano.

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References and links