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
CARYN SEAMOUNT: A small conical peak, 1000 fathoms high, whose base is
8 miles in diameter, lies in the abyssal plain west of the Bermuda Rise
(36° 45´N.). A magnetic survey of the peak has been published by Miller
and Ewing (1956). They found an exceptionally large anomaly associated
with the peak, which clearly showed its volcanic origin. Cores from the
peak contained manganese nodules, altered volcanic rocks, and Upper
Cretaceous to Recent fossils, which shows that it is at least as old
as Upper Cretaceous. The base of the peak rises from the abyssal plain
which extends out from the Hudson Submarine Delta.
HORSESHOE SEAMOUNT GROUP: About 300 miles due west from the Straits of
Gibraltar an impressive group of seamounts lies in a horseshoe-shaped
arc. Several of these, most notably Ampere and Josephine seamounts,
rise to less than 100 fathoms. Josephine Seamount is the largest
of the group and lies along an east-west topographic trend (the
Azores-Gibraltar Ridge). In the southern half of the Horseshoe Group
the individual seamounts appear to be coalescing cones similar to the
seamounts of the Kelvin Group. Seamounts of the northern half, although
imperfectly known, seem to be elongated east-west. The southern half
of the group appears to resemble volcanic cones, while in the northern
half tectonic deformation seems to have played a larger part. The
seamounts have been cored, dredged, and photographed by a Lamont
Observatory expedition. The sediments obtained from the seamounts are
middle Tertiary to Recent (Sutton _et al._, 1957).
[Illustration:
Heezen _et al._, PL. 16
FIGURE 1. WESTERN BERMUDA RISE
FIGURE 2. CENTRAL BERMUDA RISE
FIGURE 3. EAST-CENTRAL BERMUDA RISE
FIGURE 4. EASTERN BERMUDA RISE
REPRESENTATIVE PDR RECORDS FROM BERMUDA RISE
Depth in fathoms.]
[Illustration:
Heezen _et al._, PL. 17
PDR RECORD, BERMUDA SCARP ZONE
Depth in fathoms.]
[Illustration:
Heezen _et al._, PL. 18
FIGURE 1. HIGH FRACTURED PLATEAU
FIGURE 2. UPPER STEP
PDR RECORDS MID-ATLANTIC RIDGE
Depth in fathoms.]
[Illustration:
Heezen _et al._, PL. 19
Area of each photograph is about 6 by 8 feet.
PLATE 19.--OCEAN-BOTTOM PHOTOGRAPHS; MID-ATLANTIC RIDGE
FIGURE 1. (Station T1-9, photo 42) Depth 1410 fathoms, location 48°
38´N., 28° 48´W., on Western Rift Mountains, Mid-Atlantic Ridge. In
this plate Figures 1, 2, and 3 are closely spaced photographs less than
100 feet apart.
Note the coarse-grained light and dark gravel in winnow row in the
foreground and the light-colored clay or ooze bottom in background. Of
the sixty photographs taken at this location three resembled Figures 2
and 3, several resembled Figure 1, and in the remainder the ocean floor
was composed entirely of the light and dark gravel.
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