The Floors of the Ocean: 1. The North Atlantic: Text to accompany the physiographic diagram of the North AtlanticHeezen, Bruce C.
Science
The Floors of the Ocean: 1. The North Atlantic: Text to accompany the physiographic diagram of the North Atlantic
Heezen, Bruce C.
Ocean bottom
The ocean-basin floor lies between the continental margin and the
Mid-Oceanic Ridge and consists of the deeper abyssal floor and
the elevated oceanic rises. On the abyssal floor adjacent to the
continental margins are found the flattest surfaces of the earth. These
abyssal plains apparently were built by turbidity-current deposits. The
unburied abyssal floor is represented by the abyssal hills. The oceanic
rises are broad uplifts which rise from the abyssal floor through a
series of scarps. Oceanic rises are covered with pelagic sediments
except locally near islands and seamounts. The crustal structure of
oceanic rises differs significantly from the typical abyssal floor in
having lower velocities and generally thicker crustal layers.
The Mid-Oceanic Ridge is a broad fractured arch whose axis follows the
median line of the ocean. It generally covers the center third of the
ocean. The ridge provinces are divided into crest provinces and flank
provinces. The crest provinces include (1) the Rift Valley, a long
axial cleft 15-30 miles wide and 500-1500 fathoms deep; (2) the Rift
Mountains which form the sides of the Rift Valley; and (3) the High
Fractured Plateau, a rugged plateau which borders the Rift Mountains.
The flank provinces consist, on each side, of roughly three steps
separated by large scarps. A seismic belt accurately follows the Rift
Valley. The topography of the Mid-Oceanic Ridge seems best explained by
extensive normal faulting. The mid-oceanic Rift Valley connects with
and is probably of the same origin as the African rift valleys.
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Public-domain text, read in full here on John Shaqi.
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