What do you see at an ocean-continent convergent boundary?
We continue our field trip up the West Coast. Just offshore from Washington, Oregon, and Northern California is a subduction zone, where the Juan de Fuca Plate is sinking into the mantle. The Juan de Fuca Plate is being created at a spreading center, the Juan de Fuca Ridge. Let’s see the results of subduction of the Juan de Fuca Plate.
Convergent Plate Boundaries
When two plates converge, what happens depends on the types of lithosphere that meet. The three possibilities are oceanic crust to oceanic crust, oceanic crust to continental crust, or continental crust to continental crust. If at least one of the slabs of lithosphere is oceanic, that oceanic plate will plunge into the trench and back into the mantle. The meeting of two enormous slabs of lithosphere and subduction of one results in magma generation and earthquakes. If both plates meet with continental crust, there will be mountain building. Each of the three possibilities is discussed in a different lesson.
In this lesson we look at subduction of an oceanic plate beneath a continental plate in the Pacific Northwest.
When oceanic crust converges with continental crust, the denser oceanic plate plunges beneath the continental plate. This process, called
, occurs at the oceanic trenches. The entire region is known as a
. Subduction zones have a lot of intense earthquakes and volcanic eruptions. The subducting plate causes melting in the mantle. The magma rises and erupts, creating volcanoes. These coastal volcanic mountains are found in a line above the subducting plate (
). The volcanoes are known as a
Subduction of an oceanic plate beneath a continental plate causes earthquakes and forms a line of volcanoes known as a continental arc.
The movement of crust and magma causes earthquakes. A map of earthquake epicenters at subduction zones is found here:
This animation shows the relationship between subduction of the lithosphere and creation of a volcanic arc:
Remember that the mid-ocean ridge is where hot mantle material upwells in a convection cell. The upwelling mantle melts due to pressure release to form lava. Lava flows at the surface cool rapidly to become basalt, but deeper in the crust, magma cools more slowly to form gabbro. The entire ridge system is made up of igneous rock that is either extrusive or intrusive. The seafloor is also igneous rock with some sediment that has fallen onto it.
The volcanoes of northeastern California — Lassen Peak, Mount Shasta, and Medicine Lake volcano — along with the rest of the Cascade Mountains of the Pacific Northwest, are the result of subduction of the Juan de Fuca plate beneath the North American plate (
). The Juan de Fuca plate is created by seafloor spreading just offshore at the Juan de Fuca ridge.
The Cascade Mountains of the Pacific Northwest are a continental arc.
Intrusions at a Convergent Boundary
If the magma at a continental arc is felsic, it may be too viscous (thick) to rise through the crust. The magma will cool slowly to form granite or granodiorite. These large bodies of intrusive igneous rocks are called
, which may someday be uplifted to form a mountain range. California has an ancient set of batholiths that make up the Sierra Nevada mountains (
The Sierra Nevada batholith cooled beneath a volcanic arc roughly 200 million years ago. The rock is well exposed here at Mount Whitney. Similar batholiths are likely forming beneath the Andes and Cascades today.
An animation of an ocean continent plate boundary is seen here:
When two plates come towards each other they create a convergent plate boundary.
The plates can meet where both have oceanic crust or both have continental crust, or they can meet where one has oceanic and one has continental.
Dense oceanic crust will subduct beneath continental crust or a less dense slab of oceanic crust.
The oceanic plate subducts into a trench, resulting in earthquakes. Melting of mantle material creates volcanoes at the subduction zone.
If the magma is too viscous to rise to the surface it will become stuck in the crust to create intrusive igneous rocks.
Use these resources to answer the questions that follow.
1. Describe a subduction zone.
2. What forms this subduction zone?
3. How far does the subducting oceanic plate descend?
4. What is formed on the continental plate?
5. Where can an example of this plate boundary be found?
6. What is a locked zone?
7. What is produced when the locked zone is released?
1. What is the direction of plate motion at a convergent plate boundary?
2. Describe the relationship between the convection cell and subduction at a trench.
3. Subduction is sometimes called crustal recycling. Why do you think this is the case?
4. What happens if magma is too viscous to rise through the crust to erupt at the surface?