Question

It is a type of convergent plate boundary typically doesn’t generate magma.

Answer 1

Answer: The correct answer is Continent-continent convergent plate boundaries.

Continent-continent convergent plate boundaries is the type of boundary typically not generating magma.

Convergent Boundary: When two or more of Earth's lithosphere's plates come together, the resulting boundary is called a convergent boundary. Subduction is the gradual descent of one tectonic plate beneath another. Oceanic-oceanic, oceanic-continental, and continental-continental lithosphere boundaries all converge.

Explanation:

• The density of the continental crust is far too low for it to descend into the mantle.
• Plate borders that are caused by continents colliding into one another are not subduction zones. Instead, the two continents smash into one other, causing faulting, folding, and the eventual formation of a mountain range that is both high and expansive.
• The Himalayas, which are located in south central Asia, are an example of a convergent plate boundary that separates two continents.
• There are no volcanoes in this region, despite the fact that major earthquakes are often associated with the convergent plate borders that exist between continents.
• Mountain ranges that do not have an oceanic plate subducting beneath them do not have volcanoes.
• Examples of such mountain ranges include the Himalayas.

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