Warm Up 11/4

1. Warm Up 11/4 • Why are subduction zones not commonly found at convergent continental-continental boundaries? a. Oceanic lithosphere is too buoyant to be forced down into the mantle. b. Continental lithosphere is too dense to be forced down into the mantle. c. Continental lithosphere is too buoyant to be forced down into the mantle. d. Subduction zones are never found at convergent boundaries. • Which of the following is a geographic example of a transform fault boundary? a. the Andes Mountains c. the San Andreas Fault b. the East African Rift valley d. the Mid-Atlantic Ridge • The Red Sea is theorized to be the site of a recently formed ____. a. convergent boundary c. divergent boundary b. hot spot d. transform fault boundary Answers: 1) c. 2) c. 3) c.

2. Testing Plate Tectonics Chapter 9, Section 4

3. Paleomagnetism • Paleomagnetism – the study of changes in Earth’s magnetic field, as shown by patterns of magnetism in rocks that have formed over time • Some rocks contain iron-rich minerals that will align with Earth’s magnetic field at the time of their formation, creating a time capsule of the magnetic field at that time in time • When the rock moves, or the magnetic pole changes position, it will still retain its original alignment

4. Apparent Polar Wander

5. Paleomagnetism Cont. • Normal Polarity – the same direction of magnetism as the present day • Reverse Polarity – the reverse direction of the magnetic field today • The discovery of strips of rocks of alternating polarity, which lie as mirror images across the ocean ridges, provided strong evidence of seafloor spreading • Ships towed instruments called magnetometers across the sea floor, revealing alternating high and low magnetism running in parallel bands to the oceanic ridges • As new basalt is added to the ocean floor, it gains the magnetism of the current magnetic field, and when the field changes over time, the basalt records the changes

6. Paleomagnetism

7. Time Scale of Earth’s Polarity

8. Magnetic Reversals in Seafloor Spreading

9. Earthquake Patterns • Scientists found a close link between deep-focus earthquakes and ocean trenches. Also, the absence of deep-focus earthquakes along the oceanic ridge system was shown to be consistent with the new theory • Scientists have found that intermediate and deep focus earthquakes occur within the subducting plate as it goes into the mantle • Shallow-focus earthquakes are produced as the descending slab reacts with the lithosphere around it

10. Earthquake Distribution

11. Distribution of Earthquake Foci in Japan Trench

12. Ocean Drilling • Some of the best evidence has come from deep-sea drilling into the sediments on the ocean floor • The data on the ages of seafloor sediment confirmed what the seafloor spreading hypothesis predicted • The youngest oceanic crust is at the ridge crest and the oldest oceanic crust is at the continental margins • No sediment older than 180 million years has been found in the ocean basins

13. Hot Spots • Mapping revealed that there was a chain of volcanic structures in the middle of the Pacific Ocean ranging from the Hawaiian Islands to Midway Island and then north to the Aleutian trench • Hawaii is the youngest and the islands get older the further from Hawaii you are • Hot Spot – a rising plume of mantle material that melts as it nears the surface, creating a volcanic area • As the Pacific plate moves over this spot, the island chain gets longer • The age of each volcanic island indicates when that part of the Pacific plate was over the hot spot • Hot spot evidence supports the idea that the plates move over Earth’s surface

14. Hot Spots Trace Plate Motion

15. Directions and Rates of Plates