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
PLATE 11.--_OCEAN-BOTTOM PHOTOGRAPHS ON THE CONTINENTAL MARGIN AND
OCEAN-BASIN FLOOR_
FIGURE 1. (Station T1-3, photo 27) Depth 260 fathoms, location 47°
42´N., 07° 34´W., just below shelf break west of St. Nazaire, France.
Note small ripples which appear to be superimposed on larger ripples.
FIGURE 2. (Station T1-3, photo 7) Depth 285 fathoms, location several
hundred feet from photograph in Figure 1. Note holothurians and
solitary coral attached to rocks. Ripple marks are less prominent than
in Figure 1.
FIGURE 3. (Stations T1-16, photo 28) Depth 2600 fathoms, location 46°
50´N., 11° 25´W., northern part of Biscay Abyssal Plain. Note tracks of
bottom crawlers, and the prominent conical mounds, each with a central
hole.
FIGURE 4. (Station T1-18, photo 29) Depth 2650 fathoms, location
43° 56´N., 11° 12´W., southern part of Biscay Abyssal Plain. Note
meandering ridge made by subsurface burrower. Note also starfish, upper
left, and quantity of fecal pellets and holes in the bottom.
FIGURE 5. (Station T1-20, photo 53) Depth 2850 fathoms, location 42°
18´N., 14° 47´W., northeastern part of Iberia Abyssal Plain. Note holes
with converging tracks and large mound in upper right.
FIGURE 6. (Station T1-58, photo 14) Depth 3072 fathoms, location 29°
17´N., 57° 23´W., Abyssal Hills southeast of Bermuda Rise. The round
objects are manganese nodules. Note shark's tooth in lower right. Note
also small holes indicating bottom dwellers, and meandering raised
ridge of sub-bottom burrower. Of particular interest are the small
moats surrounding many of the nodules; they are probably scour marks
caused by bottom currents. These currents must be very gentle since
none of the nodules seems to show evidence of recent rolling.
Positions of stations shown on Plate 30.]
Profile E-12 passes from the African coast between Fuerteventura and
Gran Canary toward the northeast. Here the continental slope extends
only to 1000 fathoms. The Canary Islands rise abruptly from the
continental rise. Except for gradients of the order of 1:15 on the
steep slopes of these volcanic islands the gradients of the continental
rise are 1:300-1:1000.
Profiles E-13 and E-14 end on the east near Gran Canary and thus do not
show most of the upper continental rise. They do show the remarkably
wide and nearly level lower continental rise which reaches a width of
more than 500 miles.
Profiles E-15 and E-16 lie off Spanish Sahara. In both profiles the
gradient is 1:10 to 1:20 between the 50-fathom shelf break and a bench
at 300-500 fathoms. In both profiles the gradient drops below 1:40 at
about 1200 fathoms. Both profiles show numerous prominent benches on
the continental slope. The upper continental rise with gradients of
1:350-1:1200 extends to the western limit of the profiles.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account