Essentials of OceanographyRevised for increased readability, this full-colour text offers an insightful, ecologically-sensitive presentation of the relationship of scientific principles to ocean phenomena. Now better suited for non-major oceanography courses, this edition offers a broader study with a marked reduction in concentrated topic coverage, with a continued emphasis on how we must take more precautions in activities that can modify the environment and learn how to keep these modifications to a minimum. |
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Page 67
... kilometers in width typically overlies the plate boundary above a magma chamber that may be about 4 kilometers wide and 1 kilometer thick . An axial valley less than 1 kilometer wide and up to 100 meters deep may run along the axis of ...
... kilometers in width typically overlies the plate boundary above a magma chamber that may be about 4 kilometers wide and 1 kilometer thick . An axial valley less than 1 kilometer wide and up to 100 meters deep may run along the axis of ...
Page 138
... kilometers / hour at the poles to over 1600 kilometers / hour ( nearly 1000 miles / hour ) at the equator . The trade winds blow from the northeast because , as the air mass moves southward from the subtropical region near 30 ° N ...
... kilometers / hour at the poles to over 1600 kilometers / hour ( nearly 1000 miles / hour ) at the equator . The trade winds blow from the northeast because , as the air mass moves southward from the subtropical region near 30 ° N ...
Page 139
... kilometers ( about 25,000 miles ) around the equator , dividing that distance by 24 ( hours in a day ) means that Earth's equator is traveling at more than 1600 kilometers / hour . Moving poleward , the velocity dimin- ishes to 0 kilometers ...
... kilometers ( about 25,000 miles ) around the equator , dividing that distance by 24 ( hours in a day ) means that Earth's equator is traveling at more than 1600 kilometers / hour . Moving poleward , the velocity dimin- ishes to 0 kilometers ...
Contents
CHAPTER | 5 |
The RossesSounders of the Deep | 11 |
Law of the | 22 |
Copyright | |
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Common terms and phrases
air mass algae animals Antarctic areas Atlantic Ocean atmosphere bacteria barrier beach benthic biological bottom carbon cells centimeters chemosynthesis circulation coast coastal concentration continental shelf continental slope continents coral Coriolis effect currents deep deep-ocean density deposits depth developed Earth environment equator equatorial erosion estuary feeding feet Figure fish flow Gulf gyres heat energy Hemisphere high tide hydrogen hydrothermal vents increases islands kilometers latitudes layer lithosphere marine meters miles million moon move North Atlantic nutrients occur ocean basins ocean floor ocean surface ocean water oceanic crust oceanic ridges Oceanography open ocean organisms oxygen Pacific Ocean particles percent Photo photosynthesis phytoplankton plankton plants plate plate tectonics polar produce radiation reef regions rise rocks salinity sand sea level seafloor seawater sediment shore shoreline slope solar South species subtropical surface water tectonics temperature thermocline tide zone tion trenches tropical vapor volcanic warm water molecules wavelength waves whales wind