Essentials of OceanographyRevised for increased readability and streamlined for clarity, this text is designed to accompany an introductory college-level course in oceanography. This insightful, ecologically sensitive presentation of the relationship of scientific principles to ocean phenomena is made even more relevant to a new generation of teachers and students by pairing new co-author Alan Trujillo with renowned author Harold V. Thurman. *NEW - A new coauthor: - With Thurman's retirement from teaching, Alan Trujillo of Palomar College has been added as co-author for this edition. Alan's ideas and approach will help make this edition as relevant to a new generation of teachers and students as previous editions were to Thurman's contemporaries. *NEW - Changes in chapter organization: - A new Chapter 1, Introduction to Planet Earth, replaces the old Chapter 1 (History of Oceanography). The historical perspective is now included as chapter-opening feature boxes which highlight important events in oceanographic history relevant to chapter-specific material. - New placement of the chapter on plate tectonics (switched with the chapter on sea floor features) ensures that the processes of plate tectonics can be |
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Page 80
... slope Continental rise Abyssal plain Sea level Continental slope 4 km 4 km Ocean basin floor Ocean trench 50 kilometers VE = 10x 50 kilometers VE = 10x Shelf Slope Rise Abyssal plain Sea level Shelf Slope Seamounts 4 kilometers Trench ...
... slope Continental rise Abyssal plain Sea level Continental slope 4 km 4 km Ocean basin floor Ocean trench 50 kilometers VE = 10x 50 kilometers VE = 10x Shelf Slope Rise Abyssal plain Sea level Shelf Slope Seamounts 4 kilometers Trench ...
Page 86
... Slope The continental slope , which lies beyond the shelf break , is where the deep - ocean basins begin . Total relief in this region is similar to that found in mountain ranges on the continents . The break at the top of the slope may ...
... Slope The continental slope , which lies beyond the shelf break , is where the deep - ocean basins begin . Total relief in this region is similar to that found in mountain ranges on the continents . The break at the top of the slope may ...
Page 88
... slope and deeper ocean floor at greater dis- tances from the earthquake were broken progressively later in time . It seemed unusual that certain cables were affected by the failure of the slope due to ground shaking , but others were ...
... slope and deeper ocean floor at greater dis- tances from the earthquake were broken progressively later in time . It seemed unusual that certain cables were affected by the failure of the slope due to ground shaking , but others were ...
Contents
Rational Use of Technology? | 3 |
Some Historical Notes | 9 |
Origins | 17 |
Copyright | |
47 other sections not shown
Common terms and phrases
abyssal abyssal plains algae animals Antarctic areas Atlantic Ocean atmosphere beach benthic boundary called carbon caused cells centimeters coast coastal continental continents coral reefs Coriolis effect crust currents deep degrees centigrade density deposits depth diatoms dissolved Earth energy ENSO environment Equator equatorial estuary feet Figure fish flow Gulf gyres heat high tide hydrogen hydrothermal vents increase islands kilometers land latitude layer lithogenous lithosphere longshore magnetic marine mass meters mid-ocean ridge miles million moon move Northern Hemisphere nutrients occur ocean basins ocean floor ocean surface ocean water Oceanography ooze open ocean organisms oxygen Pacific Ocean particles percent Photo photosynthesis phytoplankton plankton plate tectonics polar produce pycnocline regions rock salinity sand sea floor sea level seawater sediment ship shore shoreline slope solar South species surface water temperature thermocline tidal tion transform faults tropical tsunami upwelling vapor volcanic warm water molecules wavelength waves whales wind zone