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Marine Science Chapter 2 – The Sea Floor. FOCUS QUESTIONS I.What are the major physical features of the Earth’s surface? II.What explanation have scientists.

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Presentation on theme: "Marine Science Chapter 2 – The Sea Floor. FOCUS QUESTIONS I.What are the major physical features of the Earth’s surface? II.What explanation have scientists."— Presentation transcript:

1 Marine Science Chapter 2 – The Sea Floor

2 FOCUS QUESTIONS I.What are the major physical features of the Earth’s surface? II.What explanation have scientists developed for the existence and distribution of these features? III.How do these features affect the Earth’s oceans?

3 The Water Planet 71% of earth covered in ocean Oceans regulate climate and atmosphere Four large basins: –Pacific – largest and deepest –Atlantic –Indian –Arctic – smallest and shallowest –(Southern ocean – continuous body of water surrounding Antarctica) Large basins connected by smaller, shallow seas

4 Our Fledgling Planet Earth – approximately 4.5 billion years old Formed from an aggregation of dust clouds and gas particles that condensed into solid matter. Intense heating melted many of these heavier elements in the core and mantle of the planet. The uppermost of layers cooled and formed the Earth’s crust.

5 The Structure of the Earth Materials have settled in the planet according to their density. Lithosphere (crust – very thin) Asthenosphere (upper mantle – fluid) Core (mixtures of iron – inner is solid, outer is molten) Mesosphere (mid to lower mantle – solid but very hot) d = m/V

6 All Crust is not the Same Continental crust is composed of granite. Oceanic crust is composed of basalt. Continental crust is: –lighter –thicker (20-50 km vs. 5 km for ocean) –less dense –geologically older … than Oceanic crust. See Table 2.2 on page 24

7 Hypothesis of Continental Drift Developed by Alfred Wegener in 1915. Proposed that present continents had drifted apart after the breakup of a single supercontinent, Pangaea. Hypothesis not widely accepted (How?)

8 480533/animations/ch13_animations/animat ion3.html 480533/animations/ch13_animations/animat ion3.html gea_4.htm gea_4.htm

9 Theory of Plate Tectonics Plate tectonics – the study of the processes by which the lithosphere moves laterally across the asthenosphere. This hypothesis is supported by: presence of the mid-ocean ridge comparative fossil data from different continents apparent puzzle-piece shape of different continents magnetic reversal and sediment patterns on the sea floor distribution of geological features on the Earth

10 Plate Tectonics in Action Plates “float” on the asthenosphere. There are areas where plates spread apart… …and areas where plates collide. Mid-ocean Ridges/ RiftsSubduction zones/ Trenches

11 Types of Plate Boundaries Video

12 Types of Boundaries Convergence – plates collide –Oceanic-continental convergence –Continental-continental convergence –Oceanic-oceanic convergence Shear Boundary – plates slide past each other Divergence – plates separate –Mid-ocean ridge –Transforms faults –Rift valleys

13 Oceanic-Continental Boundaries Heavy oceanic crust slides under continent. Called subduction. Trench forms. Causes explosive earthquakes. Molten lithosphere seeps up through continental crust and forms volcanoes.

14 Oceanic-Oceanic Boundaries One plate will slide under the other. Trench forms. Slow-flowing volcanoes form –sometimes break the ocean surface (island arcs). –Examples: Aleutian Islands, AK Mariana Islands

15 Continental-Continental Boundaries Two continents smash against one another with force and become “welded” together. Crust buckles forming mountain ranges. No trenches or volcanoes. India Collision (Animation)Animation (

16 Californians Get Closer Together In addition the Pacific Plate (which contains the city of Los Angeles) and the North American Plate (which contains San Francisco) share a shear boundary. These two plates slide past each other such that these cities get 4 inches closer each year.

17 The Mid-Ocean Ridge and Transform Faults A continuous chain of submarine volcanic mountains that circles the globe Caused by rising of hot mantle and pushes apart oceanic plates Results in sea floor spreading

18 The Mid-Ocean Ridge and Transform Faults Displaced at regular intervals by transform faults. Occasionally breaks the surface at places like Iceland and the Azores. Examples: –Mid-Atlantic Ridge –East Pacific Rise Above: Mid-Atlantic Ridge Left: Iceland – showing ridge

19 Rift Valleys A gap or depression resulting in the center of a mid-ocean ridge or on land. –African Rift Valley

20 Features of Mid-Ocean Rifts Hydrothermal vents – deep water hot-springs that dissolve minerals in the Earth’s crust (mainly sulfides) ( –Black smokers – chimney-like structures that build up deposits of minerals and “smoke” a cloud of mineral particles. Hot Spots – sporadic areas where molten magma forces its way through the lithosphere; creates volcanic activity (Hawaiian Islands) (

21 Geological “Hot Spots” Occur in over 100 places on the globe Areas where hot magma sporadically forces its way through the lithosphere to erupt in volcanic activity. Examples: –Hawaiian Islands –Yellowstone National Park

22 Hot Spot Formation Although this model has been contested, it describes a stationary magma source over which plates slide.

23 Major Features of the Sea Floor

24 World Distribution of Volcanoes & Earthquakes



27 Geological Provinces of the Ocean Floor Based on previous knowledge and logic, label the following parts of the map: –Abyssal plain –Continental rise –Continental shelf –Continental slope –Guyot –Seamount –Shelf break –Trench

28 Seafloor Topography Continental shelf Continental edge / Shelf break Continental slope Abyssal plain Ocean ridge and rise systems Trenches Seamount

29 Seafloor Topography

30 Geological Provinces of the Ocean Floor A. Continental shelf – The shallow gently sloping section of the continental margin that extends from the shore to the point where the slope gets steeper. B. Shelf break – The section of the continental shelf where the slope abruptly becomes steeper, usually at a depth of 120 to 200 m (400 to 600 ft). C. Continental Slope – The steeper, seaward section of the continental margin. D. Continental Rise –The gently sloping area at the base of the continental slope. E.Abyssal Plain – The nearly flat region of the deep-sea floor. F.Guyot – A flat topped- seamount G.Trench – A narrow deep depression in the sea floor. H.Seamount – A submarine volcano in the abyssal plain

31 Global Seafloor Topography

32 Continental Margins Active Margin – a continental margin that is colliding with another plate and as a result is geologically active Passive Margin – a continental margin that is located at the trailing edge of a continent and as a result shows little geological activity

33 Continental Shelf – passive margin

34 Continental Margin – active margin

35 Comparative Fossil/Sediment Data Geologists noted the similarities between the fossils and sediment deposits found on opposite sides of the Atlantic Ocean.

36 Magnetic Reversals Rocks contain magnetic particles that align with the Earth’s magnetic field. During periods called magnetic reversals, the Earth’s north pole switches to the opposite side of the globe as it is now. Believed to be related to movements in the Earth’s molten core.

37 Magnetic Anomalies When molten rock comes to the surface, the magnetic particles are free to align with the Earth’s magnetic pole. When the rock cools, the particles are fixed in the magnetic orientation at the time.

38 Magnetic Anomalies Geologists have thus discovered a pattern of magnetic banding parallel to the mid-ocean ridge.


40 References Castro, P. & J. Huber (2005) Marine Biology, 5 th ed. McGraw-Hill Higher Education, Boston, MA. Watson, J.M. (1999) “Understanding plate motions.” USGS. Retrieved on September 27, 2004 from Watson, J.M. (1999) “Understanding plate motions.” USGS. Retrieved on September 27, 2004 from


42 Global projection of Earth showing tectonic boundaries and areas of active seismic and vulcan activity.

43 2002-2003 Annual Seismic Activity at Mt. St. Helens, WA

44 Above: The Glomar Challenger was the first research vessel specifically designed in the late 1960s for the purpose of drilling into and taking core samples from the deep ocean floor.

45 Further Evidence of Earth’s Changing Nature Sediments Sea Level Changes Greenhouse Effect

46 Origin of the Atmosphere Originally free oxygen not present in the atmosphere. 600 mya – O 2 produced by single- celled photosynthetic organisms (cyanobacteria) Stromatolites Photo credit images/l741b.jpg

47 Stromatolites – Shark Bay, WA Photo credits

48 Results of an O 2 Rich Atmosphere Aerobic organisms began to out-compete anaerobes. Excess oxygen begins to react in the high atmosphere with ultraviolet radiation. This creates ozone (O 3 ) –prevents harmful UV rays from penetrating to the earth. –Allows organisms to colonize the land. Also, Earth ideally settled in an orbit where molecular water can exist in all three states –particularly the liquid state!

49 Sediments Lithogenous sediment – results from the physical and chemical weathering of rocks on land. –Carried by run-off and rivers to the ocean. Biogenous sediment – skeletons and shells of marine organisms that have fallen to the ocean floor. –Diatoms, radiolarians, foraminiferans, and coccolithophorids

50 Biogenous sediments Calcareous ooze – skeletons composed of calcium carbonate (CaCO 3 ) Siliceous ooze – skeletons composed of silica (SiO 2 ).

51 Sea Level Change Interglacials – warm periods during which freshwater melts and sea level rises. Ice ages – cold periods when large amounts of water are stored in ice caps and glaciers and sea level drops.

52 Greenhouse Effect Global temperatures and the rate of glacial melting are rapidly increasing. –Still uncertainty as to whether this is a natural phenomenon or whether it has been accelerated by humans.

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