For large stretches the deep ocean basin is flat. But seamounts, guyots, island arcs and trenches, all of which result at least in part from tectonic
Subject: guyot
Transcript: continental volcanoes, With slopes of maybe about 30 degrees or so, But several thousand feet tall. A guyot in contrast To a seamount is a flat-topped seamount
Seamounts, guyots and island arcs form on the ocean floor as a result of a hot spot or mantle plume. While seamounts do not extend above the ocean
Subject: guyot
Transcript: material, That forms those large volcanoes there. [narrator:] a variation on the same theme is the guyot, which is tall enough to be eroded by wave activity