Is Mount Vesuvius a cone or shield volcano?
Italy’s Mt. Vesuvius is a famous cinder cone volcano. In contrast, shield volcanoes are characterized by a large, broad cone with sides sloping gently away from the center. Composite cone volcanoes are also called stratovolcanoes.
What kind of volcanoes are Mt Vesuvius and Mt Fuji?
Stratovolcano: Stratovolcanoes (also called composite volcanoes) are classic cone-shaped volcanoes formed of alternating ash and lava layers. Famous stratovolcanoes include Mt Fuji (Japan), Mt Pinatubo (Philippines), Mt Taranaki (New Zealand), Mt Vesuvius (Italy), Mt St Helens (USA) and Mt Merapi (Indonesia).
Is Vesuvius an active volcano?
Vesuvius, also called Mount Vesuvius or Italian Vesuvio, active volcano that rises above the Bay of Naples on the plain of Campania in southern Italy. Its western base rests almost upon the bay. The height of the cone in 2013 was 4,203 feet (1,281 metres), but it varies considerably after each major eruption.
What type of volcano is Mount St Helens?
stratovolcano
Mount St. Helens is a stratovolcano, a steep-sided volcano located in the Pacific Northwest region of the United States in the state of Washington. Sitting about 97 miles south of Seattle and 52 miles northeast of Portland, Oregon, Mt.
How did Vesuvius erupt?
It’s creation and eruption was caused by the African and Eurasian plates colliding: more specifically, the African plate sunk below the Eurasian plate, causing the Eurasian plate to scrape over the African plate and generate what is called a “Convergent boundary” (see Figure 8) which refers to the event of two tectonic …
Can Mount Vesuvius erupt again?
Yes, Mount Vesuvius is considered an active volcano. It very well could erupt again. Mount Vesuvius sits on top of an extremely deep layer of magma that goes 154 miles into the earth.
Is Mt St Helens divergent or convergent?
Mt. St. Helens is a volcano in Washington, near the Oregon border, in the Cascade Range. The Cascade Volcanoes, which stretch all from British Columbia through Northern California, are stratovolcanoes that have formed inland from a convergent plate boundary, where ocean crust is subducting below the continent.