There was an earthquake about 500 years ago that caused a tsunami that hit the coast of Japan, according to my Geology professor at Pierce College in Puyallup, WA.
The earthquake was about 9.0 on the richtor scale, and hit in the fall of 1700, as recorded in Japan.
Generally, what happens at that subduction zone is the Juan De Fuca, the last reminent of the Ferallon plate, is subducting under the North American plate due to collision, creating the orogenic belt.
A subductional plate boundary is a boundary where two plates of are colliding, and one plate subducts, or goes underneath, the other. This happens because the plates have different densities, and the denser one subducts when they collide. If two plates that are colliding have the same densities, they will push upward, forming mountain ranges like the Himalayas.
It created mountains on the west coast of Canada which is known today as Rocky mountains in British Columbia
Because the Juan de Fuca plate has dense oceanic crust so it's being subducted beneath the north American plate's continental crust, which is less dense compared to oceanic crust.
Plates are sliding past each other
trenches
It appears to be continuous because it is a cycle. Old plate is subducted, but new plates are formed.
An erosion
residual soil
Paracutin is in the trans-Mexican volcanic belt formed by the riviera and cocos plates subducting under the north American plate
Intrusive igneous rock.
trenches
trenches
The Nazca Plate and the South American Plate are colliding. Because oceanic plates like the Nazca are more dense than continental plates, they are forced below the continental plate and subduct, or flow downward into the mantle at varying degrees of descent from the area of collision!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!
The Aleutian Islands were formed by the collision of the Pacific and North American tectonic plates. The Pacific Plate is subducting beneath the North American Plate, creating volcanic activity and earthquakes in the region. This process has led to the creation of the Aleutian volcanic island arc.
It was formed by the subduction of the Pacific Plate beneath the north American plate.
Mount hoot is formed by the Juan de Fuca Plate subducting under the North American Plate.
The Benioff Zone is formed when a piece of oceanic crust is being subducted into the mantle. This line of earthquakes follow the angle of the subducting plate as it slides beneath the continental crust.
It was formed from the volcanism created by a subducting oceanic plate at a convergent plate boundary.
The Pacific Ring of Fire was formed due to the subduction of the Nazca Plate beneath the South American Plate, the Cocos Plate beneath the Caribbean Plate, the Pacific and Juan de Fuca Plate beneath the North American Plate, the Pacific Plate and Philippines Plate beneath the Eurasian Plate, the Indo-Australian Plate beneath the Eurasian Plate, and the Pacific Plate beneath the Indo-Australian Plate. This all occurs around the Pacific Ocean.
A series of volcanic islands formed by an older oceanic plate subducting under a newer oceanic plate.
This was because part of the northward-moving African Plate is subducting beneath the Eurasian Plate. Trapped lava forms bubbles of gas as it gets near the surface. Pressure is released by coming to the surface. It bursts out as lava. Then layers build up to form the cone shape. There you go!
It appears to be continuous because it is a cycle. Old plate is subducted, but new plates are formed.