Guyot remains sharply etched in my memory.
To technically be considered a guyot or tablemount, they must stand at least 3000 ft (900 m) tall.
Further subsidence causes the volcano to sink below the sea surface, becoming a seamount and/or a guyot.
The limestone cliffs, some 60 metres in height, of the guyot and the rest of the island are covered in dense tropical jungle.
The volcano has a flat-topped summit (thus making it a guyot) rising about 3000mft -3 above the seabed, to 24mft 0 below sea level.
The vines are generally trained in either single or double guyot.
Guyot has recently started to appear in theater productions.
Some of these rise above sea level, but the vast majority are submarine features known as seamounts, or if they are flat-topped, guyots.
