Most explosive volcanism is located at oceanic to continental subduction zones.
Many are in Europe.
Caldera volcanoes are located around the world, but some well-known examples include Yellowstone in the United States, Santorini in Greece, and Taal in the Philippines. They can be found in volcanic regions with a history of explosive eruptions that have led to the formation of large, collapsed crater structures.
When an overriding plate is continental, a marginal trench forms where the topographic depression seems to follow the outline of the continental margin. It is here where explosive volcanoes can be found.
1. The explosive volcanoes are found at points in the earth's crust that are weak. This means the pressure builds up and ash can burst out easily. Some examples are: - Mt. Vesuvius - Mt. Kilauea - Mt. St. Helens
Some volcanoes similar to Mount Rainier in terms of being stratovolcanoes and having the potential for lahars are Mount Hood in Oregon and Mount Shasta in California. Both of these volcanoes are located in the Cascade Range like Mount Rainier and have a history of producing explosive eruptions.
An oceanic volcano is a volcano located on the ocean floor, often forming underwater mountains or seamounts. These volcanoes can be explosive or non-explosive and contribute to the formation of oceanic islands or mid-ocean ridges.
Volcanoes that always erupt explosively can be located on both water and land. The type of eruption is determined by the composition of the magma within the volcano, not its location. Explosive eruptions are typically caused by the high pressure buildup of gas within the magma.
When an overriding plate is continental, a marginal trench forms where the topographic depression seems to follow the outline of the continental margin. It is here where explosive volcanoes can be found.
Komaga-take Volcano is one of the most active volcanoes in Japan. It is located on the Oshima Peninsula of southern Hokkaido and is known for its violent and explosive explosions.
Which volcanoes are located at hot spots
They will normally be located at the bottom, unless otherwise upset through geologic activity.
Volcanoes are mainly on what is called ring of fire - this area is the edge of the tectonic plates on which the crust is moving. The ring of of is the subduction zones of these plates - where one plate is sliding under another. The volcanoes in this area are explosive. Other volcanoes are located over hot spots and rift zones.