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Long chains of mountains that rise up from the ocean are primarily formed by tectonic plate movements, particularly at convergent boundaries where plates collide. This process, known as orogeny, can result in the uplift of underwater mountain ranges, such as mid-ocean ridges. Additionally, volcanic activity can contribute to the formation of these mountainous structures, creating islands and underwater peaks as magma rises from the ocean floor.
The ocean floor feature that consist of chains of individual volcanoes is called mid ocean ridges. This ridge can rise from 1 to 3 kilometers above the ocean basin.
No, mountains can also be found on the ocean floor. These underwater mountains are known as seamounts or guyots. They are formed by volcanic activity and can rise thousands of feet from the ocean floor.
Underwater mountains that rise above the surface of the water are called islands. These formations are the result of volcanic activity or tectonic movements that cause them to breach the water's surface.
Underwater mountains, also known as seamounts, are volcanic formations that rise from the seafloor. They provide a unique habitat for a diverse range of marine life due to their topographical complexity. Seamounts can also influence oceanic currents and nutrient cycling in the water column.
The source is Thaba Putsoa in the Drakensburg Mountains in Lesotho. The mouth is Alexander Bay, the Atlantic Ocean
this most common type of mountain is formed when two tectonic plates smash into each other the edges buckle and crumble,giving rise to long mountain chains~bobby from Texas
Not exactly. Sea mountains are underwater topographic features that rise above the ocean floor but are not necessarily volcanic in origin. They can be formed through various geological processes such as tectonic activity or erosion.
Seamounts and underwater volcanoes are structures on the ocean floor that can be equivalent to mountains on land. These features are created by volcanic activity and can rise thousands of feet from the ocean floor, resembling the towering heights of mountains on land.
They rise in the western mountains and flow east across the North China plain to the Pacific Ocean.
The Continental rise is often hundreds of kiometres. But in the pacific ocean it has a greater number.