Most calderas are associated with subduction zones, a kind of convergent plate boundary. However, a few calderas, such as the ones at Yellowstone, are associated with hot spots rather than plate boundaries.
A strato-volcano is typically found at convergent plate boundaries, where one tectonic plate is being forced beneath another in a process known as subduction. The molten rock (magma) produced by the subduction process rises to the surface, resulting in the formation of a strato-volcano.
Calderas don't form from plate tectonics, they occur when a the magma chamber of volcano is partly emptied by a massive eruption and the volcano collapses into the open space. The kind of volcanic activity associated with caldera-forming eruptions is most often found at convergent plate boundaries, but there are some calderas associated with hot spot volcanoes.
Lava domes are usually associated with convergent boundaries.
divergent plate boundaries
At destructive late margins.
The northern boundary of Sumatra is a general tectonic boundary where the Eurasian Plate meets the Sunda Plate. This boundary can experience earthquakes and volcanic activity due to tectonic movements.
Mount Mazama was formed by the collision of two tectonic plates along a convergent boundary. Specifically, it was caused by the subduction of the Juan de Fuca Plate beneath the North American Plate in the Cascadia Subduction Zone.
A divergent plate boundary.
A stratovolcano, also known as a composite volcano, is most likely to erupt with ash and lava for miles at a convergent boundary. These volcanoes are common at subduction zones, where one tectonic plate is forced beneath another, creating extreme pressure and leading to explosive eruptions.
A convergent boundary forms from the collision of two tectonic plates. In this type of boundary, one plate is typically forced beneath the other in a process known as subduction. This collision can lead to the formation of mountain ranges, volcanic arcs, and earthquakes.
a tectonic plate
The type of boundary where one tectonic plate slides under another is called a convergent boundary. This process is known as subduction, where one plate is forced beneath the other due to differences in density.
The asthenosphere is not a plate boundary. It is the layer of Earth's mantle on which tectonic plates float.
it was a convergent of divergent because it is a stratovolcano
A divergent plate boundary.
A stratovolcano, also known as a composite volcano, is most likely to erupt with ash and lava for miles at a convergent boundary. These volcanoes are common at subduction zones, where one tectonic plate is forced beneath another, creating extreme pressure and leading to explosive eruptions.
Convergent boundaries occur at subduction zones, the point where one plate slides under another plate.
Convergent boundaries occur at subduction zones, the point where one plate slides under another plate.
A convergent plate boundary leads to subduction. This occurs when two tectonic plates collide and one plate is forced beneath the other, typically resulting in the formation of deep oceanic trenches and volcanic arcs.
A convergent boundary forms from the collision of two tectonic plates. In this type of boundary, one plate is typically forced beneath the other in a process known as subduction. This collision can lead to the formation of mountain ranges, volcanic arcs, and earthquakes.
A reverse fault is typically formed at a convergent plate boundary where two tectonic plates are colliding. The movement along the fault results in one block of rock moving up and over the other block.
Mount Yasur is on the Indo-Australian Plate and Pacific Plate boundary. This provides the volcano with a constant supply of fresh rock to erupt.