When one plate slides beneath another it carries volatiles such as water with it. These substances get into the mantle rock and lower the temperature needed for it to melt. This molten material then rises as it is less dense and forms volcanoes as it reaches the surface.
Volcanoes are often found near subduction zones because the descending tectonic plate plunges deep into the Earth's mantle, causing melting due to high temperature and pressure. This molten rock, or magma, then rises to the surface, resulting in volcanic activity.
Volcanoes tend to form at convergent subduction boundaries and divergent plate boundaries. One good example would be the broad ring of volcanoes that have formed around the boundary of the Pacific plate. This is why this region is known as the ring of fire. There is also a very long chain of undersea volcanoes that occur at the mid ocean ridges. In some places these have formed islands such as Iceland. Where subduction occurs (along the west coast of South America, and the west coast of the USA for example) volcanoes form, e.g. Subduction zones also form volcanic island arcs such as the Aleutian island chain in Alaska.
The most active volcanoes in the US are in Alaska, particularly in the Aleutian Islands and along the Alaska Peninsula. These volcanic regions have frequent eruptions due to the subduction of the Pacific Plate beneath the North American Plate. Notable active volcanoes in Alaska include Mount Redoubt, Pavlof Volcano, and Mount Shishaldin.
Some of the deepest earthquakes on Earth occur in subduction zones, where one tectonic plate is forced beneath another. These earthquakes can happen as deep as 700 kilometers (430 miles) below the surface. Examples of subduction zones where deep earthquakes occur include the Japan Trench and the Peru-Chile Trench.
Scientists usually find the age of volcanoes through radiometric dating of their rocks.
usually you find most of the zones of earthquakes and volcanoes at a plate boundary.
Volcanoes are often found near subduction zones because the descending tectonic plate plunges deep into the Earth's mantle, causing melting due to high temperature and pressure. This molten rock, or magma, then rises to the surface, resulting in volcanic activity.
There are no active volcanoes in Montana. You have to go further west to the Cascade Range to find volcanoes. The volcanoes in the Cascades are caused by the subduction of the oceanic crust under the continental crust.
Volcanoes are typically found at tectonic plate boundaries, such as the Ring of Fire in the Pacific Ocean, where plates collide or separate. They can also occur in hot spots like Hawaii. Submarine volcanoes can be found along mid-ocean ridges where underwater tectonic plates spread apart.
at the very bottom of the ocean, usally
Volcanoes tend to form at convergent subduction boundaries and divergent plate boundaries. One good example would be the broad ring of volcanoes that have formed around the boundary of the Pacific plate. This is why this region is known as the ring of fire. There is also a very long chain of undersea volcanoes that occur at the mid ocean ridges. In some places these have formed islands such as Iceland. Where subduction occurs (along the west coast of South America, and the west coast of the USA for example) volcanoes form, e.g. Subduction zones also form volcanic island arcs such as the Aleutian island chain in Alaska.
At Fault lines, or places of crustal activity :) Volcanoes usually form near plate boundaries where subduction is occurring. This causes magma from the mantle to rise up onto Earth's surface and form volcanoes. Most volcanoes are formed in this way. Volcanoes can also be formed by hotspots. Magma from the mantle rises through these hotspots and find their way to Earth's surface, forming volcanoes in a chain like Hawaii. Well, volcanoes are usually the land that creates islands like Hawaii. I'm doing homework right now and i'd say an island? If not that, i'd go with the first two answers. :)
One structure you would find at an active continental margin that you would not find at a passive margin is a subduction zone. Subduction zones occur at active margins where tectonic plates collide, resulting in one plate being forced beneath the other. This process can lead to the formation of volcanic arcs, deep ocean trenches, and earthquakes.
You could find subduction zones in the depths of the oceans, at some plate boundaries. At this location, you would observe one tectonic plate (a plate of lower density then the other) being slipped under another plate into magma. These are also known as destructive boundaries, because crust is being destroyed, (as opposed to diverent boundaries where leaking magma creates new crust.)
The most active volcanoes in the US are in Alaska, particularly in the Aleutian Islands and along the Alaska Peninsula. These volcanic regions have frequent eruptions due to the subduction of the Pacific Plate beneath the North American Plate. Notable active volcanoes in Alaska include Mount Redoubt, Pavlof Volcano, and Mount Shishaldin.
Some of the deepest earthquakes on Earth occur in subduction zones, where one tectonic plate is forced beneath another. These earthquakes can happen as deep as 700 kilometers (430 miles) below the surface. Examples of subduction zones where deep earthquakes occur include the Japan Trench and the Peru-Chile Trench.
They usually show up in desert zones.