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

Magma and Volcanoes

In this section, we will explore the properties of magma and how their mineral composition and physical properties may impact their behavior during volcanic eruptions. Magma can have different amounts of silica (SiO4) and dissolved gases (like CO2, SO2, and H2O). These factors affect how magma erupts and the type of volcano it will form when it solidifies. Note that the amount of silica in magma and its viscosity are positively correlated. Magma can contain 1% to 10% dissolved gases, much like a soda contains dissolved CO2.

 

Exercise 1: Properties of Magma

Let’s examine the physical and chemical properties of magma, which controls the type and impact of volcanic eruptions.  Use the resources below and answer the following questions.

Watch the video above for

  1. What is magma and where does it come from?
  2. What is lava?
  3. Magma does not rise to the surface to form volcanoes everywhere. Where do most volcanoes form?

Let’s explore how the silica (SiO4) and dissolved gas (like CO2, SO2, and H2O) composition affect the eruption style.

  1. Define viscosity.
  2. What is more viscous: Water or Maple syrup?
  3. Lava with low viscosity will be able to flow a long distance before it cools and hardens into rock, or to cool and harden close to the vent?
  4. The lava in the above question has low silica or high silica?
  5. Lava with high viscosity will be able to flow a long distance before it cools and hardens into rock or cool and harden close to the vent?
  6. The lava in the above question has low silica or high silica?
  7. Contents from one of the two sealed bottles will erupt when vigorously shaken: Plain water or Soda?
  8. Compared to magma with lower gas content magma with a higher gas content will erupt: More explosively or Less explosively
  9. Define an effusive eruption.
  10. Define an explosive eruption.
  11. Silica and gas content in effusive eruptions are high or low?

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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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