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Chapter 14:  The Ocean Floor
Starter #10   ,[object Object],[object Object],[object Object],[object Object]
Starter #10   ,[object Object],[object Object]
Lecture Notes Outline (Cornell) 14.1 The Vast World Ocean (p. 394-400) I. Introduction 1. 2.  II. Geography of the Oceans A. Four Main Ocean Basins (sink)  B. Mapping the Ocean Floor 1.Intro.  (2) 2.  3. 4.  What is? What are the 4... How?
14.1   The Vast World Ocean     Nearly 71 percent of Earth’s surface is covered by the global ocean.    Oceanography  is a science that draws on the methods and knowledge of geology, chemistry, physics, and biology to study all aspects of the world ocean. The Blue Planet
The World Ocean
14.1   The Vast World Ocean     The world ocean can be divided into four main ocean basins—the Pacific Ocean, the Atlantic Ocean, the Indian Ocean, and the Arctic Ocean. ,[object Object],[object Object],[object Object],[object Object],Geography of the Oceans
14.1  The Vast World Ocean     The topography of the ocean floor is as diverse as that of the continents.    Bathymetry  is the measurement of ocean depths and the charting of the shape or topography of the ocean floor.    Today’s technology—particularly  sonar, satellites, and submersibles—allows  scientists to study the ocean floor in a more efficient and precise manner than ever before. Mapping the Ocean Floor
The Topography of the Ocean
14.1   The Vast World Ocean     Sonar ,[object Object],[object Object],Mapping the Ocean Floor
Sonar Methods
14.1   The Vast World Ocean     Satellites ,[object Object],[object Object],[object Object],Mapping the Ocean Floor
Satellite Methods
Starter #11 ,[object Object],[object Object]
Mapping the ocean floor
14.1   The Vast World Ocean     Submersibles ,[object Object],[object Object],Mapping the Ocean Floor
14.2   Ocean Floor Features  ,[object Object],Mapping the Ocean Floor
14.2  Ocean Floor Features     In the Atlantic Ocean, thick layers of undisturbed sediment cover the continental margin. This region has very little volcanic or earthquake activity.    A   continental margin  is the zone of transition between a continent and the adjacent ocean basin floor. Continental Margins
Atlantic Continental Margin
14.2  Ocean Floor Features     In the Pacific Ocean, oceanic crust plunges beneath continental crust. This force results in a narrow continental margin that experiences both volcanic activity and earthquakes. Continental Margins
14.2   Ocean Floor Features     Continental Shelf ,[object Object],[object Object],Continental Margins
14.2   Ocean Floor Features     Continental Slope ,[object Object],[object Object],[object Object],Continental Margins
Submarine Canyons
14.2  Ocean Floor Features     Continental Rise ,[object Object],Continental Margins
14.2  Ocean Floor Features     The  ocean basin floor   is the area of the deep-ocean floor between the continental margin and the oceanic ridge. ,[object Object],[object Object],   Deep-Ocean Trenches Ocean Basin Floor
14.2  Ocean Floor Features     Abyssal Plains ,[object Object],[object Object],   Seamounts and Guyots ,[object Object],Ocean Basin Floor
Abyssal Plain Cross Section
14.2   Ocean Floor Features     A  mid-ocean ridge   is found near the center of most ocean basins. It is an interconnected system of underwater mountains that have developed on newly formed ocean crust.    Seafloor Spreading ,[object Object],[object Object],Mid-Ocean Ridges
14.2  Ocean Floor Features     Hydrothermal Vents ,[object Object],Mid-Ocean Ridges
Hydrothermal Vents ,[object Object],[object Object],[object Object],[object Object],[object Object]
14.3   Seafloor Sediments     Ocean-floor sediments can be classified according to their origin into three broad categories: terrigenous sediment, biogenous sediment, and hydrogenous sediment.    Terrigenous Sediment ,[object Object],Types of Seafloor Sediments
14.3   Seafloor Sediments     Biogenous Sediment ,[object Object],-  Calcareous ooze  is thick, common biogenous sediment produced by dissolving calcium carbonate shells. -  Siliceous ooze  is biogenous sediment composed of silica-based shells of single-celled animals and algae. Types of Seafloor Sediments
14.3   Seafloor Sediments     Hydrogenous Sediment ,[object Object],Types of Seafloor Sediments
Biogenous Sediments Radiolaria Foraminifera
14.4   Resources from the Seafloor    Oil and natural gas  are the main energy products currently being obtained from the ocean floor. ,[object Object],   Gas Hydrates ,[object Object],Energy Resources
Gas Hydrates
14.4  Resources from the Seafloor    Other major resources from the ocean floor include sand and gravel, evaporative salts, and manganese nodules.    Sand and Gravel ,[object Object],Other Resources
14.4   Resources from the Seafloor    Manganese Nodules    Evaporative Salts ,[object Object],[object Object],[object Object],Other Resources
Manganese Nodules

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Ch. 14 the ocean floor

  • 1. Chapter 14: The Ocean Floor
  • 2.
  • 3.
  • 4. Lecture Notes Outline (Cornell) 14.1 The Vast World Ocean (p. 394-400) I. Introduction 1. 2. II. Geography of the Oceans A. Four Main Ocean Basins (sink) B. Mapping the Ocean Floor 1.Intro. (2) 2. 3. 4. What is? What are the 4... How?
  • 5. 14.1 The Vast World Ocean  Nearly 71 percent of Earth’s surface is covered by the global ocean.  Oceanography is a science that draws on the methods and knowledge of geology, chemistry, physics, and biology to study all aspects of the world ocean. The Blue Planet
  • 7.
  • 8. 14.1 The Vast World Ocean  The topography of the ocean floor is as diverse as that of the continents.  Bathymetry is the measurement of ocean depths and the charting of the shape or topography of the ocean floor.  Today’s technology—particularly sonar, satellites, and submersibles—allows scientists to study the ocean floor in a more efficient and precise manner than ever before. Mapping the Ocean Floor
  • 9. The Topography of the Ocean
  • 10.
  • 12.
  • 14.
  • 16.
  • 17.
  • 18. 14.2 Ocean Floor Features  In the Atlantic Ocean, thick layers of undisturbed sediment cover the continental margin. This region has very little volcanic or earthquake activity.  A continental margin is the zone of transition between a continent and the adjacent ocean basin floor. Continental Margins
  • 20. 14.2 Ocean Floor Features  In the Pacific Ocean, oceanic crust plunges beneath continental crust. This force results in a narrow continental margin that experiences both volcanic activity and earthquakes. Continental Margins
  • 21.
  • 22.
  • 24.
  • 25.
  • 26.
  • 28.
  • 29.
  • 30.
  • 31.
  • 32.
  • 33.
  • 35.
  • 37.
  • 38.

Notes de l'éditeur

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