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Chapter 3Marine Provinces
Essentials of Oceanography
7th Edition
Bathymetry
Bathymetry is the measurement of ocean depths and the charting of the shape or topography of the ocean floor The ocean floor is a highly varied terrain that contains many interesting features Early methods of determining ocean depths involved using a long weighted line (called a sounding line)
Bathymetric techniques
Echosounders send sound through water to determine water depth and sea floor features Figure 3-1
Bathymetric techniques
Side-scan sonar uses a “fish” towed behind a ship to give a more detailed picture of the sea floor
Figure 3-2
Bathymetric techniques
Low frequency sound is used to determine structure beneath the sea floor
Figure 3-3
Bathymetric techniques
Satellites measure sea surface elevation, which mimics sea floor bathymetry
Figure 3D
The hypsographic curve
The hypsographic curve shows the relationship between the height of the land and the depth of the oceans Figure 3-4
Major regions of the North Atlantic Ocean floor
Continental margin
Ocean basin floor
Mid-ocean ridge
Figure 3-5
Passive versus active continental margins
Passive marginNo plate boundary
Shelf
Slope
Rise
Figure 3-6
Passive versus active continental margins
Active marginPlate boundary
ConvergentShelfSlope (steep)Trench
TransformContinental
borderland
Figure 3-6
Submarine canyons and deep-sea fans
Turbidity currents carve submarine canyons into the slope and shelf
Debris from turbidity currents creates graded bedding deposits and deep-sea fans
Figure 3-8a
Diver in the La Jolla Submarine Canyon
Figure 3-8b
Abyssal plains
Deep flat areas formed by suspension settlingVolcanic peaks poke through the sediment
Abyssal hills (seaknolls)SeamountsTablemounts (guyots)
Figure 3-9
Ocean trenchesDeepest parts of the oceanFormed by plate convergenceMost trenches are in the Pacific OceanAssociated with volcanic arcs
Island arcContinental arc
Figure 3-10
The mid-ocean ridge
Circles the globe like the seam of a baseballMostly traverses the middle of ocean basins A topographically high mountain rangeEntirely volcanic in originAssociated with plate divergenceIn the Pacific Ocean, called the East Pacific RiseIn the Atlantic Ocean, called the Mid-Atlantic RidgeInternet flybys of portions of the mid-ocean ridge
The Mid-Atlantic Ridge
Traverses the center of the Atlantic OceanContains a central down-dropped rift valleyComes above sea level in Iceland
Figure 3-12
Features of the mid-ocean ridge
Rift valleysForm when plates split apartDown-dropped areas associated with faults and earthquakes
Figure 3-13
Features of the mid-ocean ridge
Pillow lavaForms when hot lava comes into contact with cold seawater and quickly cools
Basalt composition
Figure 3-14
Features of the mid-ocean ridge
Hydrothermal ventsForm when seawater is heated by magmaBlack smokers emit hot water through chimneysAssociated with metal sulfide deposits and unusual lifeforms
Figure 3-15
Transform faults and fracture zones
Transform FaultsOccur between segments of the mid-ocean ridge
Transform plate boundaries
Movement in opposite directions
Figure 3-16
Transform faults and fracture zones
Fracture ZonesOccur beyond segments of the mid-ocean ridge
Not plate boundaries
Movement in the same direction
Figure 3-16
End of Chapter 3
Essentials of Oceanography
7th Edition