1. Chapter 1 EQ: 1. How did the oceans form? 2. Where are the major ones located?

2. Oceanography Oceanography is the study of all aspects of the marine environment. To do this, we need to use many different sciences. Often times, the knowledge of multiple sciences is needed to see how each aspect works together.

3. Oceanography Biology Marine life, Adaptations, fisheries Chemistry Seawater composition, Pollutants, Density, temperature changes Physics Waves, currents, pressure changes, light, sound Geology Plate tectonics, sediments, coastlines Geography World climates, wind belts, current systems Astronomy Formation of earth, origins of oceans, tidal cycles and forces

4. Formation of Earth and the Solar System Nebular hypothesis – all bodies in the solar system formed from nebula Nebula = cloud of gases and space dust Mainly hydrogen and helium

5. Nebular Hypothesis Gravity concentrates material at center of cloud (Sun) Protoplanets form from smaller concentrations of matter (eddies)

6. Protoearth: Our early earth Larger than Earth today Homogeneous composition Bombarded by meteorites Moon formed from collision with large asteroid

7. Protoearth Radioactive heat Spontaneous breaking apart of atoms Releases heat energy Means protoearth was HOT HOT HOT! Gravity pulls matter towards the center of the earth, contracting the matter Earth is heated from the extra pressure from contraction This makes Protoearth partially melt (lots of lava) Density stratification (layered Earth)

8. Density Stratification High density = heavy for its size Early Earth experienced gravitational separation. High density materials (Iron and Nickel) settled in core. Less dense materials formed concentric spheres around core. Least dense gases left the earth to begin to form the atmosphere

9. Earth’s Internal Structure Layers defined by Chemical composition Physical properties

10. Layers by Chemical Composition Crust Low-density, mainly silicate minerals Mantle Mainly iron (Fe) and magnesium (Mg) silicate minerals Core High-density, mainly iron (Fe) and nickel (Ni)

11. Origin of Earth’s Atmosphere Outgassing – occurred during density stratification Less dense gases drift up into the atmosphere Water vapor Carbon dioxide Hydrogen Other gases Earth’s early atmosphere different from today Lacks oxygen, would be toxic to us now

12. Origin of Earth’s Oceans Outgassed water vapor fell as rain. The first permanent oceans formed 4 billion years ago. Salinity developed from dissolved rock elements. Early acidic rain dissolved more crustal minerals than today.

13. Development of Earth’s Oceans

14. DO NOW #1 We have been and will continue to look at the formation of earth and the oceans, information about each ocean, and where the major oceans and seas are located. From the first day, what areas of science are we using today? (biology, chemistry, physics, geology, geography, astronomy)

15. Life’s Possible Ocean Origins Earth’s earliest known life forms are 3.5-billion-year-old bacteria fossilized in ocean rocks. These are the building blocks for life on early Earth. There is no direct evidence of early Earth’s environment.

16. The Beginning…. The world ocean is the most prominent feature on Earth. Oceans cover 70.8% of Earth’s surface. The origin and development of life on Earth is connected to the ocean. The oceans have a long history on Earth.

17. Earth’s Oceans Earth has one ocean. It is divided into four principle oceans, and one other. Pacific Ocean Atlantic Ocean Indian Ocean Arctic Ocean Southern, or Antarctic Ocean

18. Ocean Info a) oceans cover 70.8% of the earth b) of the major oceans, the Pacific is the biggest c) the Pacific, Atlantic, and Indian are around the same depth. The Arctic is much shallower. d) the oceans are deeper than the land is tall.

19. Comparing Oceans to Continents Average ocean depth is 3729 meters (12,234 feet) Average continental elevation is 840 meters (2756 feet) Deepest ocean trench is the Mariana Trench at 11,022 meters (36,161 feet) Highest continental mountain is Mt. Everest at 8850 meters (29,935 feet)

20. Earth’s Oceans Pacific Ocean World’s largest ocean Accounts for more than half of Earth’s ocean space World’s deepest ocean Earth’s largest geographic feature Named in 1520 by Ferdinand Magellan for his peaceful journey across it.

21. Earth’s Oceans Atlantic Ocean Half the size of the Pacific Ocean Shallower than the Pacific Ocean Named after Atlas, the Greek Titan Indian Ocean Smaller than the Atlantic Ocean Similar depth as the Atlantic Ocean Primarily in the Southern Hemisphere

22. Earth’s Oceans Arctic Ocean Seven percent the size of the Pacific Ocean Shallowest world ocean Permanent layer of sea ice a few meters thick

23. Earth’s Oceans Southern Ocean or Antarctic Ocean Circumnavigates Antarctica Is really the parts of the Pacific, Atlantic, and Indian Oceans that lie south of 50° S latitude

24. The Seven Seas Smaller and shallower than oceans Salt water Usually enclosed by land Sargasso Sea defined by surrounding ocean currents Directly connected to the ocean Before the 15th Century, Europeans considered the seven seas to be the following: 1. Red Sea 2. Mediterranean Sea 3. Persian Gulf 4. Black Sea 5. Adriatic Sea 6. Caspian Sea 7. Indian Ocean

25. Seas Now that the oceans have been explored further (and we know we are not going to fall off the edge of the earth) there are many more than 7 seas. Here are some of the top ones:

26. 1. Mediterranean 2. Red Sea 3. Adriatic Sea 4. Black Sea 5. Caspian Sea 6. Persian Gulf Seas

27. 7. Arabian Sea 8. Bay of Bengal 9. Hudson Bay 10. Labrador Sea 11. Gulf of Mexico 12. Caribbean Sea Seas

28. 13. Bering Sea 14. Sea of Okhotsk 15. Sea of Japan 16. Coral Sea 17. Scotia Sea 18. Weddell Sea Seas

29. Closure: 1. Why is Oceanography called an interdisciplinary science? 2. How did the earth form? 3. How did the oceans form?