no divergent boundary
Yes, Mount Katmai is located in Alaska, which is on the boundary where the Pacific tectonic plate is converging with the North American plate. This tectonic activity has contributed to the formation of the volcanic arc that includes Mount Katmai.
Mount Erebus did not erupt in 2011. The last known eruption of Mount Erebus in Antarctica occurred in 2018.
It is a lava flow, and has an AA (ah-ah) lava flow
Mount Hood is formed by a convergent boundary where the Juan de Fuca tectonic plate is being subducted beneath the North American plate. This subduction causes magma to rise and create the volcanic activity that forms Mount Hood.
Mount Pinatubo is located at the convergent boundary of the Eurasian Plate and the Philippine Sea Plate.
The Antarctic Plate.
Mt. Erubus has tectonic plates made up of parts of the lithosphere. These plates grind together or pull apart and this causes volcanoes to erupt.
Yes, Mount Katmai is located in Alaska, which is on the boundary where the Pacific tectonic plate is converging with the North American plate. This tectonic activity has contributed to the formation of the volcanic arc that includes Mount Katmai.
Mount Erebus did not erupt in 2011. The last known eruption of Mount Erebus in Antarctica occurred in 2018.
It is a lava flow, and has an AA (ah-ah) lava flow
Because it is on a plat boundary :)
Mount Hood is formed by a convergent boundary where the Juan de Fuca tectonic plate is being subducted beneath the North American plate. This subduction causes magma to rise and create the volcanic activity that forms Mount Hood.
Mount Erebus is a Antarctic volcano.
Mount Erebus is a Antarctic volcano. There are no countries on the Antarctic continent..
plants flora on mount erebus are lichens, bryophytes, algae, and fungiAnother AnswerMt Erebus is an active volcano in a polar climate. There is no flora on Mt Erebus.
Mount Erebus is located in Antarctica.
Mt. Fuji is located in Japan. It is near a continental convergent boundary, a continental transform boundary, and an oceanic transform boundary.