What two types of convergent boundaries do mountains form?
Typically, a convergent plate boundary—such as the one between the Indian Plate and the Eurasian Plate—forms towering mountain ranges, like the Himalaya, as Earth’s crust is crumpled and pushed upward.
What is formed in the convergence of two continental plates?
When two continental crusted plates converge, they eventually collide and end up producing mountains; this was how the Himalayan Mountains were created. … When two oceanic plates converge, the denser plate will end up sinking below the less dense plate, leading to the formation of an oceanic subduction zone.
What are the three types of convergence?
There are three types of convergent boundaries: Oceanic-Continental Convergence. Oceanic-Oceanic Convergence. Continental-Continental Convergence.
Which is the best example of a convergent plate boundary?
Answer: The Washington-Oregon coastline of the United States is an example of this type of convergent plate boundary. Here the Juan de Fuca oceanic plate is subducting beneath the westward-moving North American continental plate. The Cascade Mountain Range is a line of volcanoes above the melting oceanic plate.
What landforms are created by 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.
Do convergent boundaries form mountains?
Mountains are usually formed at what are called convergent plate boundaries, meaning a boundary at which two plates are moving towards one another. … Sometimes, the two tectonic plates press up against each other, causing the land to lift into mountainous forms as the plates continue to collide.