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© 2009 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors in teaching their courses and assessing student learning. Dissemination or sale of any part of this work (including on the World Wide Web) will destroy the integrity of the work and is not permitted. The work and materials from it should never be made available to students except by instructors using the accompanying text in their classes. All recipients of this work are expected to abide by these restrictions and to honor the intended pedagogical purposes and the needs of other instructors who rely on these materials. Lecture Outlines PowerPoint Chapter 13 Earth Science, 12e Tarbuck/Lutgens

Earth Science, 12e The Ocean Floor Chapter 13

The vast world ocean  Earth is often referred to as the blue planet Seventy-one percent of Earth’s surface is represented by oceans and marginal seas Continents and islands comprise the remaining 29 percent  Northern Hemisphere is called the land hemisphere, and the Southern Hemisphere the water hemisphere

Views of the Northern and Southern Hemispheres Figure 13.1

The vast world ocean  Four main ocean basins Pacific Ocean – the largest and has the greatest depth Atlantic Ocean – about half the size of the Pacific and not quite as deep Indian Ocean – slightly smaller than the Atlantic, largely a Southern Hemisphere body Arctic Ocean – about 7 percent the size of the Pacific

The oceans of Earth Figure 13.2 B

Mapping the ocean floor  Bathymetry – measurement of ocean depths and the charting of the shape or topography of the ocean floor  Echo sounder (also referred to as sonar) Invented in the 1920s Primary instrument for measuring depth Reflects sound from ocean floor

Echo sounder and multibeam sonar Echo sounder and multibeam sonar Figure 13.4

Mapping the ocean floor  Sidescan Sonar (Towfish) Developed after WWII to look for mines Trail behind ship by cable on either side of ship Makes picture of seafloor Does not give Bathymetric (water depth) data

Mapping the ocean floor  Multibeam sonar Employs an array of sound sources and listening devices Obtains a profile of a narrow strip of seafloor

Mapping the ocean floor  Measuring the shape of the ocean surface from space Gravity attracts water to more massive structures like mountains Water tends to pile up Above canyons water levels depressed

Mapping the ocean floor  Three major topographic units of the ocean floor Continental margins Ocean basin floor Mid-ocean ridge

Major topographic divisions of the North Atlantic Ocean Figure 13.8