Ash and poised magma that will turn into Metal!
Mount Bird is in Antarctica. It has basalt magma.
There are many communities located near Mount Ranier. Most notably, the city of Tacoma is potentially threatened by the volcano.
There is no Mount St. Ranier. This question confuses two different volcanoes: Mount Ranier and Mount St. Helens. Mount Ranier is estimated to be 500,000 years old while Mount St. Helens is estimated at 40,000 years old.
No, Mount St. Helens is not an intrusive volcano. It is a stratovolcano, which is formed from explosive eruptions of viscous lava, ash, and other volcanic materials. An intrusive volcano forms when magma solidifies below the Earth's surface.
Mount ranier is a stratovolcano.
A mountain built from magma is called a volcanic mountain. It forms when magma from beneath the Earth's surface erupts through a vent or fissure, cools, and solidifies to create layers of volcanic rock and ash over time. Examples include Mount St. Helens in the United States and Mount Fuji in Japan.
Mount Katmai is a strato volcano, also known as a composite volcano. It is characterized by its steep slopes, large size, and explosive eruptions caused by the buildup of magma beneath the surface.
Mount Ranier is a stratovolcano. These volcanoes generaly have very viscous magma stored beneath them. It is difficult to get this magma moving. Because of this, many stratovolcanoes go long periods without erupting.
Mount to rhyme with count. Ranier to rhyme with veneer..
No, Mount Nyiragongo is a stratovolcano, also known as a composite volcano. It is characterized by its steep-sided cone shape and explosive eruptions due to the presence of viscous magma.
Volcanoes are known land forms that can release ashes and lava. It actually depends on how big is the magma chamber of a volcano has but according to some scientist and volcanologist that the capacity of magma that a volcano can hold depends on its Volcanic Explosivity Index.
A volcano is a mount (or mountain) that has magma in it. A volcano also is like an earthquake releasing pressure from the inner core of the earth. If there is a lot of pressure to be released this will cause the eruption to be bigger and more destructive, like the volcano Mount Tambora that erupted in 1815.