The mid-oceanic ridge system is formed by oceanic-oceanic divergence. The Himalayas are created by continental-continental convergence. The Mariana Trench and Challenger's Deep are associated with oceanic-oceanic convergence, where an oceanic plate is subducting beneath another oceanic plate.
The mid-oceanic ridge system, the world's longest mountain range, results from oceanic-oceanic divergence. As tectonic plates pull apart, magma rises to create this continuous underwater ridge in all five oceans. In contrast, the majestic Himalayas, among Earth's highest non-volcanic mountains, stem from the collision of two continental plates in continental-continental convergence.
The Mariana Trench, the planet's deepest trench, and Challenger's Deep form at oceanic-oceanic convergence, where one oceanic plate subducts beneath another. These geological formations exemplify the dynamic forces and diverse landscapes shaped by plate tectonics and the interactions between Earth's crustal plates.
The complete question is:
Match each geological formation with the type of boundary Interaction that most likely created it.
continental-continental convergence
oceanic-oceanic convergence
oceanic-oceanic divergence
The mid-occanic ridge system is a continuous oceanic ridge that runs through all five of Earth's oceans. Although it is an underground formation, It is the longest mountain range in the world.
The Himalayas are a non-volcanic mountain range that includes some of the world's highest peaks. The Himalayas lie between the Indo-Gangetic Plain of northern India and the Tibetan Plateau.
The Mariana Trench in the Pacific Ocean is the deepest trench in the world. Along its subduction zone, there's an area called Challenger's Deep, which is known to be the deepest point on Earth.