the continental shelf, slope, and trenches of course!
Mountains
Submerged underwater volcanoes are referred to as submarine volcanoes or seamounts. These volcanic structures can be found on the ocean floor and may rise from the seabed to create underwater mountains.
Isolated volcanic peaks on the ocean floor are known as seamounts. The deepest parts of the ocean are long, narrow features known as deep ocean trenches.
Yes, the ocean floor can have mountain ridges, valleys, and plains. Mountain ridges are formed by tectonic activity, valleys may be created by the movement of tectonic plates, and plains can result from sedimentation and volcanic activity. These features are important in shaping the ocean floor's topography.
Yes, seamounts are underwater mountains that rise from the ocean floor but do not reach the water's surface. The tops of seamounts are typically submerged beneath the surface of the ocean.
Yes the ocean floor has mountains and deep trenches.
Derr! there called sea mount's.
Seamounts are isolated volcanic mountains scatteredacross the ocean floor
Yes, there are underwater mountains called seamounts that rise from the ocean floor. These volcanic structures can be as large as terrestrial mountains and provide unique habitats for marine life. It is estimated that there are thousands of seamounts across the world's oceans.
The ocean floor does have underwater mountains called seamounts and undersea valleys known as trenches. These features are created by tectonic plate movements and volcanic activity on the ocean floor.
volcanic mountains not formed on mid-ocean ridge
Mountains
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.
Sea Floor Spreading and the way the volcanoes erupt make the mountains erode into the ocean.
The mid-ocean ridge. The longest in the world, in the sea and on land.
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