This is a photo of Mount Fuiji, an active volcano in Japan. This image relates to the PowerPoint that we looked at in class since it talked about earthquakes and the different types of volcanoes: composite volcanoes, shield volcanoes, and rift eruptions.
We also learned that the type of volcano that forms depends on type of tectonic plate boundaries involved. Mount Fuji is an example of a composite volcano. Mount Fuji is a composite volcano due to the cone like shape it maintains. The cone like shape is caused by previous eruptions that had resulted in a buildup of ash and lava layers.
Eruptions from composite volcanoes occur when magma reaches the surface and gas gest trapped below, causing a buildup of pressure. Once the pressure is great enough the volcano will erupt. Mount Fuji hasn’t erupted since 1707; after part of Japan had been struck by an 8.6 magnitude earthquake it had caused Mount Fuji to erupt 2 moths later in December, its ash had reached as far as Tokyo. Mount Fuji hadn’t stopped erupting until the start of 1708. People fear that if another large earthquake occurs that it will cause Mount Fuji to erupt and cause a big catastrophe like it had in 1707.
Works cited:
Klemetti, Erik. “Mt. Fuji: Japan’s Sacred Volcano.” Big Think. N.p., 17 Mar. 2011. Web. 24 May 2017.