wegener-continental drift

34
History of geological science: Continental Drift is not plate tectonics. Jigsaw fit of continents was noted by Alfred Wegener, a german meteorologist he proposed “Continental Drift” in 1915 saying the continents once fit together as one and naming the supercontinent Pangaea the idea was considered absurd ->no mechanism for moving continents

Upload: zorina

Post on 09-Jan-2016

38 views

Category:

Documents


3 download

DESCRIPTION

- PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Wegener-Continental Drift

History of geological science:

Continental Drift is not plate tectonics.

Jigsaw fit of continents was noted by Alfred Wegener, a german meteorologist

he proposed “Continental Drift” in 1915 saying the continents once fit together as one and naming the

supercontinent Pangaea

the idea was considered absurd

->no mechanism for moving continents

Page 2: Wegener-Continental Drift
Page 3: Wegener-Continental Drift

Wegener’s evidence

1. fit of continents2. matching up past glaciations3. distribution of equatorial climate belts4. distribution of fossils/ fauna across continents5. matching up of rocks/geologic units

Criticism: explanation for how it could happen did not make sense---continental crust can’t plow through the ocean crust

Page 4: Wegener-Continental Drift

This animation presents a view of the continents at the level of map precision available to Alfred Wegener, who proposed that the continents once existed as a vast supercontinent, Pangea, that later fragmented. Test the fit of the continents for yourself by clicking and dragging a continent to a new location; then, using the arrow keys on your keyboard, rotate the continent into position.

PC version Mac version

Wegener-Continental Drift

Page 5: Wegener-Continental Drift

03_03a.jpg

2. Matching up of past glaciations

Page 6: Wegener-Continental Drift

03_03b.jpg

Page 7: Wegener-Continental Drift

03_04.jpg

3. Equatorial climate belts

Page 8: Wegener-Continental Drift

03_05.jpg

4. Matching up of fauna

Page 9: Wegener-Continental Drift

03_06.jpg

5. Matching up of rocks,geological units

Page 10: Wegener-Continental Drift

The story unfolds: paleomagnetism

As we talked about earlier, Earth has a magnetic field.It is due to convection of the molten Fe in the outer core

(geodynamo)

magnetic north pole is not the geographic north pole- the difference for a given location is the declination

the Earth’s magnetic field has a component of direction (N-S) and a dip angle (magnetic inclination):

both can be recorded in magnetic minerals

Page 11: Wegener-Continental Drift
Page 12: Wegener-Continental Drift
Page 13: Wegener-Continental Drift

the direction of the field is easily recorded in some minerals, especially magnetite just like a compass needles, tiny grains of magnetite (or a few other Fe bearing minerals) crystallize in rocks at the surface. The little magnetic domains in these minerals align with the magnetic field (once they are below the curie Temperature)

this gives:1) direction to magnetic N pole2) the dip of the field which depends on latitude.

Page 14: Wegener-Continental Drift

03_07.jpg

Page 15: Wegener-Continental Drift

03_10.jpg

Page 16: Wegener-Continental Drift

03_11.jpg

Page 17: Wegener-Continental Drift

More trouble…

Paleomagnetic analysis along with radiometric dating indicated the magnetic N pole was moving all over the place with time-worse yet, different continents gave different polar paths

-> this was called apparent polar wander

Wait! If the same data were interpreted to reflect a fixed pole but wandering continents, everything worked. YIKES!

But still, how do continents drift???

Page 18: Wegener-Continental Drift

03_16.jpg

Page 19: Wegener-Continental Drift

03_17.jpg

Page 20: Wegener-Continental Drift

More info: ocean depth

Seafloor bathymetry showed flat seafloor but big mountain range in middle of the Atlantic...and there was high heatflow in these mountains... and these mountain ranges were locations of particular type of earthquakes....

Hard to know the shape of the ocean floor-not until WWII did sonar develop to measure bathymetry (shape of seafloor surface).

Right in the middle of the Atlantic Ocean, there was a big mountain range!

There was also high heat flow, a particular type of earthquake (reflecting tensional forces) and sediment thickness increased away from the mountain range…

Page 21: Wegener-Continental Drift

03_18.jpg

Page 22: Wegener-Continental Drift

03_19.jpg

Page 23: Wegener-Continental Drift

One last piece of info:

maps of earth quake locations was not random--rather EQ found along distinct belts including the mountain range in the Atlantic

Page 24: Wegener-Continental Drift

03_22.jpg

Page 25: Wegener-Continental Drift

Harry Hess’s hypothesis

Proposed the idea of sea-floor spreading:1) Seafloor spreads and cracks2) Magma ascends and forms new oceanic crust made of

volcanic rock3) Crust must be consumed somewhere--said it descends in

ocean trenches.

Testable as will be shown

-> got the big picture right but in detail more than just crust that is created and destroyed

Page 26: Wegener-Continental Drift

03_23.jpg

Page 27: Wegener-Continental Drift

How to test the hypothesisPaleo magnetics gets used again:

Geologists working on volcanic rocks on land noticed that the magnetic field of the Earth flipped directions on an irregular basis (this has to do with the geodynamo, and yes it could happen today or tomorrow…)

These are called polarity reversals

Magnetometers towed across the Mid-Atlantic Ridge revealed stripes of alternating magnetic direction recorded in the ocean crust--and it was symmetrical across the ridge!

Page 28: Wegener-Continental Drift

This animation shows progressive stages in the opening of the Atlantic Ocean. The youngest rocks (in red) clearly outline the mid-ocean ridge system, complete with transform faults. The oldest ocean crust (in blue), is confined to offshore regions adjacent to the United States, Canada and western Africa. This distribution demonstrates that the North Atlantic began to open before the South Atlantic.

PC version Mac version

Sea Floor Spreading

Page 29: Wegener-Continental Drift

03_24.jpg

Page 30: Wegener-Continental Drift

03_26.jpg

Page 31: Wegener-Continental Drift

The polarity of Earth's magnetic field reverses with time. The main figure demonstrates how sea-floor anomalies, also known as magnetic stripes, develop during sea-floor spreading. The inset image records the reversal of Earth's dipole.

PC version Mac version

Magnetic Reversals

Page 32: Wegener-Continental Drift

03_29.jpg

Page 33: Wegener-Continental Drift

03_Featured_Art.jpgZoomable ArtPC Mac

Page 34: Wegener-Continental Drift

Finally, radiometric dating of the volcanic rock away from the ridge was the final proof

The rocks got older away from the ridge confirming that Hess’s basic idea, that ocean crust was created and destroyed allowing the continents to move, was indeed correct.

Next: How Plate Tectonics works