plate tectonics or do the continents move because they don’t like their neighbors?
TRANSCRIPT
Plate TectonicsPlate Tectonics
OrOr
Do the continents move because Do the continents move because they don’t like their neighbors?they don’t like their neighbors?
1919thth century geologists wondered century geologists wondered about the origin of mountains.about the origin of mountains.
• How were they formed?
• What process folded rocks like putty?
• What made the Earth’s surface move?
Contraction TheoryContraction Theory
Edward Suess (1831-1914)
• Thought that the Earth has been cooling since its formation.
• And as the planet contracted its surface wrinkled like a drying apple.
Or maybe prunes.Or maybe prunes.
• Suess believed that:• Continents over time
would collapse and become ocean basins.
• Ocean basins would then be higher and become continents.
• This would explain marine fossils on dry land.
The Theory of Continental DriftThe Theory of Continental Drift
• In 1915, Alfred Wegener, a German meteorologist and geophysicist, published The Origin of Continents and Oceans.
• This book set forth the hypothesis of Continental Drift.
Pangaea - “All Land”Pangaea - “All Land”
• Wegener believed that 200 million years ago all the present-day continents combined to form a single super continent called Pangaea.
The EvidenceThe Evidence
• If the continents were cut out like a jig-saw puzzle, which ones would you match up first?
Since the 16Since the 16thth century, scientists century, scientists have puzzled over the fit of have puzzled over the fit of South America and Africa.South America and Africa.
Evidence: Jigsaw Puzzle MatchEvidence: Jigsaw Puzzle Match
• Wegener also noticed the fit.
• Challenged by other scientists citing coastal erosion.
• In fact at a depth of 900 meters at the edge of the continental shelf, the continents match perfectly.
Evidence: Fossil CorrelationEvidence: Fossil Correlation• Wegener cited several documented cases where
fossils were found on different landmasses but that could not have crossed present day oceans.
• Classic example Mesosaurus.
Evidence: Rock Type and Evidence: Rock Type and Structure MatchStructure Match
• Several mountain belts of similar rock structure terminate at a coastline only to reappear on a land mass across the ocean.
• Example: Appalachians and Caledonian Mts.
Evidence: Ancient ClimatesEvidence: Ancient Climates• Evidence of
glaciation in areas presently in subtropical climates.
Layers of glacial till and scratches found in southern Africa and South America, also in India and Australia.
Wegener’s Theory RejectedWegener’s Theory Rejected
• The theory was widely discussed in the 1920’s and 30’s.
• Hotly rejected, especially by geologists in the U.S. who labeled it bad science.
• Reason: Wegener could not give clear causal mechanism.
Earth’s Internal HeatEarth’s Internal Heat
• As Earth’s internal heat became better understood, new theories arose.
• Arthur Holmes (1890-1965)believed the area under the continents could be plastic and ductile due to heat.
• If it was, then continents could move with it.
Upper Mantle ConvectionUpper Mantle Convection• Holmes believed that continental drift was driven by
mantle convection currents.• At mid-ocean ridges new crust is being made and at
deep ocean trenches old crust pushed back into mantle.• Continents dragged along conveyor belt style.
Sea floor spreading Mid-ocean ridges were not known until about 55 years ago because they are under water. Rift valleys in the middle of long mountain ranges. Upwelling of lava forms the igneous rock basalt
Age of Sea FloorAge of Sea Floor The sea floor (oceanic crust) is younger close to mid-ocean ridges and much older farther away.
Red – young Dark Blue - old
Magnetic ReversalsMagnetic Reversals Atoms of iron in molten lava
arrange themselves in the direction of Earth’s magnetic field.
When the lava hardens the iron atoms are locked in place.
It was found that at times they pointed north and other times pointed south.
The magnetic bands on one side of the mid-ocean ridge are a mirror image of the bands on the other side.