description Cruiser Guyot Overview
Cruiser Guyot is a flat-topped submarine volcano, or guyot, in the Mid-Pacific Mountains of the central Pacific Ocean. Like other guyots, it has a broad summit that lies below sea level, a form generally associated with volcanic construction followed by erosion and later subsidence. The feature is of interest to marine geologists and oceanographic surveyors studying seamounts, oceanic crust, and the geological history of the Pacific basin.
help Cruiser Guyot FAQ
What is Cruiser Guyot?
Cruiser Guyot is a flat-topped submarine volcano, also called a guyot or tablemount. It lies in the Mid-Pacific Mountains of the central Pacific, so it is a seafloor feature rather than an island.
Why is Cruiser Guyot flat on top?
A guyot generally formed as a volcanic mountain that was eroded or built near sea level and then subsided as the oceanic crust cooled. Its broad summit is now below sea level, which is the defining contrast with a pointed seamount.
Is Cruiser Guyot part of the Mid-Pacific Mountains?
Yes. Cruiser Guyot is listed within the Mid-Pacific Mountains, a broad chain of submarine volcanic features in the central Pacific.
Could Cruiser Guyot ever have been an island?
The flat summit of a guyot is consistent with a volcanic edifice that once approached or rose above sea level before subsiding. For Cruiser Guyot, the safe description is the present geological one: a flat-topped underwater volcano, not a currently exposed island.
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