What geologic features are created at continental oceanic convergent boundaries?

What geologic features are created at continental oceanic convergent boundaries?

Deep ocean trenches, volcanoes, island arcs, submarine mountain ranges, and fault lines are examples of features that can form along plate tectonic boundaries. Volcanoes are one kind of feature that forms along convergent plate boundaries, where two tectonic plates collide and one moves beneath the other.

What geological feature is produced at a continental continental convergent plate boundary?

When two continental plates converge, they smash together and create mountains. The amazing Himalaya Mountains are the result of this type of convergent plate boundary.

What 2 features form at a convergent boundary between an oceanic and continental plate?

Effects of a convergent boundary between an oceanic and continental plate include: a zone of earthquake activity that is shallow along the continent margin but deepens beneath the continent; sometimes an ocean trench immediately off shore of the continent; a line of volcanic eruptions a few hundred miles inland from …

Which is an example of the features formed at oceanic oceanic convergence?

Examples of ocean-ocean convergent zones are subduction of the Pacific Plate south of Alaska (creating the Aleutian Islands) and under the Philippine Plate, where it creates the Marianas Trench, the deepest part of the ocean.

What geologic events are possible with the oceanic oceanic convergence?

When oceanic- oceanic convergence take place, big events like volcanic activities, earthquakes, trenches and valleys forms. Some examples of oceanic convergence are the Aleutian islands, the Mariana’s islands.

Which feature can be produced at an oceanic continental convergence?

Subduction of an oceanic plate beneath a continental plate forms a line of volcanoes known as a continental arc and causes earthquakes. As you would expect, where plates collide there are lots of intense earthquakes and volcanic eruptions. The subducting oceanic plate melts as it reenters the mantle.

What is oceanic continental convergent?

Continental – oceanic convergence When oceanic lithosphere and continental lithosphere collide, the dense oceanic lithosphere subducts beneath the less dense continental lithosphere. An accretionary wedge forms on the continental crust as deep-sea sediments and oceanic crust are scraped from the oceanic plate.

What features are formed at oceanic to continental convergence?

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.

What geologic feature results the convergence of continental and oceanic crusts?

When oceanic crust converges with continental crust, the denser oceanic plate plunges beneath the continental plate. This process, called subduction, occurs at the oceanic trenches (figure 6). The entire region is known as a subduction zone. Subduction zones have a lot of intense earthquakes and volcanic eruptions.

What is a real life example of a convergent boundary?

The Andes Mountain Range of western South America is another example of a convergent boundary between an oceanic and continental plate. Here the Nazca Plate is subducting beneath the South American plate .

What Landforms do convergent plates make?

Landforms that could be created at convergent boundaries would consist of: volcanoes, mountains, trenches, volcanic islands, and even deserts could result from effects of converging boundaries. The landforms are mountains.

What is oceanic continental convergence?

Oceanic-continental convergence occurs where an oceanic plate converges with a continental plate and subducts under it. An oceanic-oceanic convergent plate boundary occurs when one oceanic plate becomes subducted under another, resulting in the creation of a deep oceanic trench.

What happens in a convergent boundary?

Convergent boundaries are highly unstable areas of the lithosphere of the Earth. Some or all of these activities happen at the convergent boundaries: subduction of the denser plate underneath the less dense one, melting of parts of the subducted plates, plate collision, faulting and folding,…