guyots are flat topped from erosion by waves; seamounts are point-topped
They are formed usually from extinct volcanoes
A seamount is a mountain rising from the ocean seafloor that does not reach to the water's surface (sea level), and thus is not an island.
Differ.
Use it as a verb. Shelly differs from Mary
I differ with your argument that all fatty foods are bad to eat.Though I do agree with you, I differ with you on some points.
Abyssal plains,seamounts,guyots,and contenintal slopes.
Guyot
Unusual flat-topped seamounts in the ocean are called Guyots. Guyots are submerged volcanic mountains with a flat top that has been eroded by waves and currents over time.
Guyots are seamounts with flat tops that have been eroded by wave action. This erosion typically occurs when seamounts subside and move away from the mid-ocean ridge, entering shallower waters where wave erosion can shape their peaks into flat surfaces.
guyots
Basalt volcanoes are referred to as shield volcanoes. Volcanoes of this type include Mauna Loa and Kilauea, both in Hawaii.
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.
A guyot is a volcano built up from the sea floor, sometimes to sea level or above. The sea floor gradually sinks an flattens guyots are submerged to become undersea flat topped peaks. Guyots are chiefly found in the Pacific ocean. Seamounts (Guyots) are formed by volcanic activity and can be taller than 3,000 meters (10,000 ft.) They can be isolated or large parts of mountain chains. The New England Seamount contains more than thirty peaks that stretch 1,600 kilometers (about 994 miles) from the coast of New England.
guyots
Guyots are underwater volcanic mountains with flat tops that are submerged beneath the ocean's surface. They are formed through the process of volcanic activity followed by erosion and subsidence. Guyots can be found in all the world's oceans.
crabs
Guyots form through volcanic activity on the seafloor. Initially, these underwater volcanoes build up to create islands, but over time as they erode and sink, they flatten out to form guyots. The flat tops of guyots are due to wave action eroding the former islands at sea level.