There are three types of convergent plate boundaries Oceanic–Oceanic Japanese Islands Oceanic–Continent Andes Mountains Continent–Continent Himalaya Mountains.

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Presentation transcript:

There are three types of convergent plate boundaries Oceanic–Oceanic Japanese Islands Oceanic–Continent Andes Mountains Continent–Continent Himalaya Mountains We will look at each type Convergent Boundaries

Oceanic - Oceanic Under the ocean, one plate slides underneath another at a subduction zone

Oceanic - Oceanic A deep trench forms along the contact

Oceanic - Oceanic Magma wells up along the subduction zone creating volcanoes, which can form volcanic island arcs such as the Japanese Islands

Oceanic - Continent An oceanic plate slides under a continental plate at a subduction zone

The relative densities of the oceanic crust versus the continental crust are important: The continental crust is lighter and has an average density of 2.8 g/cm 3 The oceanic crust is heavier and has an average density 3.2 g/cm 3 Therefore, the heavier oceanic crust sinks beneath the more buoyant, lighter continental crust Oceanic - Continent

A deep trench forms along the subduction zone

Oceanic - Continent The lighter continental crust is pushed up and forms a mountain range

Oceanic - Continent Magma wells up along the subduction zone creating volcanoes, which adds to the size of the mountains and creates a continental volcanic arc

Andes Mountains The Andes Mountains stretch over 5500 miles along the Pacific side of South America

Pacific Ring of Fire

Both continental plates are lighter than the heavier, underlying asthenosphere So, when two continental plates collide, they are too buoyant to be subducted Instead, the continental crust is deformed and uplifted, creating mountains such as Mount Everest Continent - Continent

Why? Because the continent of India collided with the continent of Asia

Continent - Continent

Transform Plate Boundaries A transform fault plate boundary occurs when two plate slide past each other in opposite directions

Transform Plate Boundaries The most famous example is the San Andreas Fault Zone in California The portion of California in blue is heading northwest to Alaska This is the most studied fault zone in the world

San Andreas Fault Earthquakes Each red dot marks an earthquake Notice how many have occurred in California They are not kidding when they talk about the “BIG ONE”

San Andreas Fault Zone

Transform Plate Boundaries