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Sector collapse

Adapted from Wikipedia · Discoverer experience

This photo shows the aftermath of the Mount St. Helens eruption in 1980, with mudflow near the Cowlitz River. It illustrates the powerful effects of volcanic activity on the landscape.

A sector collapse is when a big piece of a volcano falls down very quickly. This piece can be as large as one cubic kilometer, which is about the size of a small mountain. When this happens, it can cause dangerous explosions moving sideways, huge landslides, and changes in how the volcano erupts. These collapses can be triggered by earthquakes, volcanic eruptions, or slow changes in the shape of the volcano over time.

Sector collapse during the 1980 eruption of Mount St. Helens

Sector collapses can happen on volcanoes located where Earth's plates come together or move apart. Even though they happen very suddenly, scientists are trying to find ways to predict when they might occur. These events are very dangerous and are one of the most hazardous things that can happen with volcanoes. Understanding them helps scientists keep people safe near active volcanoes.

Causes

Example of sector collapse: cross-section diagram of Tata Sabaya volcano (in Bolivia) (a) pre-collapse volcano, (b) after collapse, (c) new edifice built on top of collapsed old edifice

Sector collapse can happen because of processes inside the volcano. When a volcano erupts, it can weaken parts of the volcano, making them fall down. Even without an eruption, changes inside the volcano, like the movement of magma or the formation of cracks, can make the volcano weaker and lead to collapse. The shape and angle of the volcano also play a role—if the slope gets too steep, it can collapse under its own weight.

External factors can also cause sector collapse. Earthquakes can shake and weaken a volcano, making it more likely to collapse. Heavy rain and intense weather can wear away the rock, making the volcano unstable. When glaciers melt, they can change the shape of a volcano and increase the chance of collapse. Changes in sea level can also affect the stability of volcanoes near the ocean.

Consequences

Mudflow-induced property damage caused by the 1980 Mount St. Helens sector collapse

When a big part of a volcano collapses, it can change how the volcano works. Sometimes, the volcano may erupt more often or in different ways after the collapse. The collapse can also cause explosions of steam and water because the pressure inside the volcano drops suddenly.

These collapses can be very dangerous for people. They have caused many deaths and destroyed homes. One famous collapse created a huge wave in the ocean that flooded coastal areas. Scientists can learn about old collapses by studying the rocks and land left behind after these events. These rocks show clues about when and where the collapse happened.

Examples

Approximation of Mount Rainer's Osceola collapse

Some famous examples of sector collapses include volcanoes like Antuco, Chimborazo, Popocatépetl, Mount Rainier, Mount Shasta, Shiveluch, and Stromboli from long ago. More recent events happened at Anak Krakatoa, Mount Bandai in 1888, Bezymianny in 1956, Oshima-Oshima in 1741, Ritter Island in 1888, and Mount St. Helens in 1980. These events show how powerful volcanic collapses can be.

Images

An artistic print showing the eruption of Mount Bandai in Japan in 1888, illustrating a powerful natural event.
A 3D model showing the shape and features of a landslide area near a volcano in Bolivia.

This article is a child-friendly adaptation of the Wikipedia article on Sector collapse, available under CC BY-SA 4.0.

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