Claire Chadwick; Lauren Maurizio; Robin Humphreys; and Vijay Vulava

Composite Volcanoes

In this section, we learn about composite volcanoes – also known as stratovolcanoes – which are known to be the most explosive and destructive volcanoes in the world. Their location is associated with specific types of plate boundaries as well as the composition of the magma. We will also study three composite volcanoes from different parts of the world.

Exercise 2 – Composite Volcanoes

Use the resources listed below to answer the following questions.

  1. Click Major Volcanoes of the World (arcgis.com). At which type of plate boundaries are a majority of composite volcanoes found?
  2. Composite volcanoes occur at subduction zones. T/F
  3. Do composite volcanoes occur at convergent boundaries where subduction does not occur?
  4. Explain your above answer. (Hint: Explore the Major Volcanoes of the World (arcgis.com) and examine other convergent boundaries.)
  5. Which parts of the US have composite volcanoes?
  6. Is subduction occurring at these locations?
  7. Click 4.1 Plate Tectonics and Volcanism – Physical Geology – 2nd Edition (opentextbc.ca) and study Fig. 4.1.1. On which type of a plate do the volcanoes form? Overriding Plate or Downgoing Plate

Click on the textbook link below and scroll down to “4.5.2 Volcano Features and Types.” Study the figure that shows the features of a composite volcano and read the description for composite volcanoes.

  1. Why is a composite volcano called by that name?
  2. How would you characterize the profile of a composite volcano? Tall and conical or broad dome-like and wide?
  3. What do the alternating light and dark bands of rock signify in the composite volcano?
  4. What is tephra composed of?
  5. Lava flows on composite volcanoes (and elsewhere) are associated with: high silica content (high viscosity) or low silica content (low viscosity).
  6. Tephra on composite volcanoes (and elsewhere) are associated with: high silica content (high viscosity) or low silica content (low viscosity).
  7. How do alternate layers of lava flows and tephra influence the profile (shape) of composite volcanoes?
  8. What scale is used to measure the magnitude and intensity of a volcanic eruption?
  9. On this scale, what is considered to be a major eruption?

 

Mt. St. Helens, Washington, USA

Mt. St. Helens is a volcano in the Cascade chain of volcanoes in western Washington and Oregon. In 1980, this volcano erupted causing significant damage and loss of life in this area.

Exercise 3 – Mount St. Helens

Let’s examine the recent major eruption history at Mt. St. Helens. Use the resources below to answer the following questions.

  1. What are the names of the tectonic plates are involved at this location?
  2. What kind of blast occurred during this eruption?
  3. What was the area impacted by this blast?
  4. What was the reported VEI for the 1980 eruption?
  5. Which volcanic hazards were recorded during the 1980 eruption?
  6. What were the names of rocks found at this volcano?

 

Krakatau, Indonesia

Krakatau is an active island volcano located in the Sunda Strait between Java and Sumatra islands in southern Indonesia. A massive eruption occurred in 1883 killing more than 36,000 people and this volcano is still highly active today.

 

Exercise 4 – Krakatau

Use the resources below to answer the questions.

  1. What are the names of the tectonic plates are involved at this location?
  2. What kind of blast occurred during the 1883 eruption?
  3. What was the deadliest hazard that was associated with that eruption?
  4. What was the reported VEI for the 1883 eruption?
  5. As you can see from the video, (Anak or new or child of) Krakatau is still erupting. Why is this volcano still active?
  6. According to the above video, what geologic hazards were caused by the recent eruptions?
  7. What types of rocks were reported near this volcano?

Mt. Pelée, Martinique

Mt. Pelée is a composite volcano located in the Caribbean island of Martinique. In 1902 the dome collapse on the top of this volcano resulted in an explosion that killed virtually the entire population of the port city of St. Pierre.  The video below shows the type of hazard that destroyed St. Pierre.

 

Exercise 5 – Mt. Pelée

Use the resources below to answer the following questions.

  1. What are the names of the tectonic plates are involved at this location?
  2. What was the deadliest hazard that was associated with the 1902 eruption?
  3. What was the reported VEI for the 1902 eruption?
  4. Explain what made this hazard so deadly.

 

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Environmental Geology Laboratory Copyright © 2021 by Dr. Vijay M. Vulava and colleagues at the Department of Geology and Environmental Geosciences, College of Charleston is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License, except where otherwise noted.

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