Essentials of Oceanography"How do the oceans work?" To help readers find the answers, Trujillo and Thurman present & in-depth and rigorous discussions of oceanographic concepts and demystify the science for the layperson. Highlights the interdisciplinary relationship between oceanographic phenomena and how those phenomena affect other Earth systems. Incorporates scientific information from geology, chemistry, physics, and biology to illustrate how each of these disciplines relates to the ocean. Updates content throughout to include some of the most recent developments in oceanography, such as the recent Indian Ocean tsunamis and Hurricanes Katrina, Rita, and Wilma. A readable, informative reference for anyone interested in learning more about our oceans. |
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Page 22
... layer ( the oil ) and a higher - densi- ty bottom layer ( the vinegar ) , then you've seen how density stratification causes separate layers to form . Earth's Internal Structure As a result of density stratification , Earth became a layered ...
... layer ( the oil ) and a higher - densi- ty bottom layer ( the vinegar ) , then you've seen how density stratification causes separate layers to form . Earth's Internal Structure As a result of density stratification , Earth became a layered ...
Page 82
... layer A Rock layer B Rock layer C 2 : Reflection Depth = V X T 712 FAULT Ocean floor Soft sediment . Firm sediment . Rock layer A- Rock layer B NE 1600 1700 Yusuf Ridge 1800 19000 Yusuf Basin Eastern Alboran Basin Site 977 Site 977 5 km ...
... layer A Rock layer B Rock layer C 2 : Reflection Depth = V X T 712 FAULT Ocean floor Soft sediment . Firm sediment . Rock layer A- Rock layer B NE 1600 1700 Yusuf Ridge 1800 19000 Yusuf Basin Eastern Alboran Basin Site 977 Site 977 5 km ...
Page 216
... layer , and the direction of each arrow indicates the direction it moves . Under ideal conditions , therefore , the surface layer should move at an angle of 45 degrees from the direction of the wind . All the layers combine , howev- er ...
... layer , and the direction of each arrow indicates the direction it moves . Under ideal conditions , therefore , the surface layer should move at an angle of 45 degrees from the direction of the wind . All the layers combine , howev- er ...
Contents
I | 3 |
Introduction to Planet Earth | 6 |
Visiting the Deep Ocean Floor | 11 |
Copyright | |
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Other editions - View all
Essentials of Oceanography, Eighth Edition: Student Lecture Notebook Alan P. Trujillo,Harold V. Thurman No preview available - 2005 |
Common terms and phrases
algae Antarctic Arctic areas asthenosphere Atlantic Ocean atmosphere atoms beach biogenous called caused chemical coast coastal continents coral Coriolis effect crust deep density deposits depth dissolved drift Earth El Niño energy environment equator equatorial feet Figure fish flow Gulf heat hydrogen hydrothermal vents increases Indian Ocean islands kilometers land latitudes layer lithogenous lithosphere magnetic manganese nodules marine meters mid-ocean ridge miles million Moon move Niño North Atlantic Northern Hemisphere nutrients occur ocean basins ocean floor ocean surface Oceanography ooze organisms oxygen Pacific Ocean particles pattern photosynthesis plankton plate boundaries plate tectonics polar pressure produce pycnocline reef regions rocks salinity sand Scientific American sea floor spreading sea ice sea level seawater sediment shore shoreline slope solar South species Students Sometimes Ask subduction subtropical gyres surface currents surface water temperature thermocline tidal tide tion transform faults Trench tropical tsunami upwelling volcanic warm water molecules waves whales zone