Which of the following features is prominent at transform boundaries?

What is the most common feature at a transform boundary?

This is known as a transform plate boundary. As the plates rub against each other, huge stresses can cause portions of the rock to break, resulting in earthquakes. Places where these breaks occur are called faults. A well-known example of a transform plate boundary is the San Andreas Fault in California.

What is Brainly transform boundary?

Transform Plate Boundaries are locations where two plates slide past one another. … Most transform faults are found in the ocean basin and connect offsets in the mid-ocean ridges.

What geologic feature is formed in transform fault boundary?

The broad zone of shearing at a transform plate boundary includes masses of rock displaced tens to hundreds of miles, shallow earthquakes, and a landscape consisting of long ridges separated by narrow valleys. U.S. Geological Survey.

Which features are commonly formed at the plate boundaries where continental crust converges with oceanic crust?

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.

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Which two features are commonly found at divergent plate boundaries?

The features most commonly associated with divergent boundaries between tectonic plates are rift valleys, ocean ridges, fissure volcanoes, and…

What are the characteristics convergent divergent and transform plate boundaries?

Divergent boundaries — where new crust is generated as the plates pull away from each other. Convergent boundaries — where crust is destroyed as one plate dives under another. Transform boundaries — where crust is neither produced nor destroyed as the plates slide horizontally past each other.

What process along transform fault plate boundary?

The third type of plate boundary is the transform fault, where plates slide past one another without the production or destruction of crust. Because rocks are cut and displaced by movement in opposite direction, rocks facing each other on two sides of the fault are typically of different type and age.