A continent to continent convergent boundary does not have a subduction zone.
No, the Cascadia Subduction Zone is not a transform boundary; it is a convergent boundary where the Juan de Fuca Plate is subducting beneath the North American Plate. This process leads to significant geological activity, including earthquakes and volcanic eruptions. Transform boundaries, in contrast, involve plates sliding past one another horizontally, such as the San Andreas Fault in California.
Mount St. Helens sits on the Cascadia Subduction Zone, which is a convergent plate boundary where the Juan de Fuca Plate is subducting beneath the North American Plate. This subduction zone is responsible for the volcanic activity in the region.
I’m not sure
Krakatoa is located at a convergent boundary, where the Indo-Australian Plate is being subducted beneath the Eurasian Plate. This subduction zone can lead to intense volcanic activity due to the melting and rising of magma from the subducted plate.
A continent to continent convergent boundary does not have a subduction zone.
Yes, a subduction zone is a type of convergent boundary where one tectonic plate is forced beneath another plate.
No, the Cascadia Subduction Zone is not a transform boundary; it is a convergent boundary where the Juan de Fuca Plate is subducting beneath the North American Plate. This process leads to significant geological activity, including earthquakes and volcanic eruptions. Transform boundaries, in contrast, involve plates sliding past one another horizontally, such as the San Andreas Fault in California.
a subduction zone forms
Mount St. Helens sits on the Cascadia Subduction Zone, which is a convergent plate boundary where the Juan de Fuca Plate is subducting beneath the North American Plate. This subduction zone is responsible for the volcanic activity in the region.
A subduction zone is a convergent boundary where two tectonic plates collide.
At a convergent boundary.
It is a subduction zone and can create earthquakes and volcanoes
I’m not sure
Krakatoa is located at a convergent boundary, where the Indo-Australian Plate is being subducted beneath the Eurasian Plate. This subduction zone can lead to intense volcanic activity due to the melting and rising of magma from the subducted plate.
Mount St. Helens is located on the Cascadia Subduction Zone, which is a convergent plate boundary where the Juan de Fuca Plate is being subducted beneath the North American Plate. This subduction zone is a primary source of volcanic activity in the region.
Convergent Boundaries