plate tectonics 10.1 08 09
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Ch 10 Plate Tectonics
• Section 10.1
Continental Drift
continental drift - a hypothesis proposed in 1912 by German meteorologist,
Alfred Wegener
Continental Drift
one landmass called Pangaeaone ocean called Panthalassa
Continental Drift
Based on: rock clues fossil clues climate clues
Pangaea
Pangaea
Pangaea
Rock clues
Rock clues
Fossil clues
Fossil clues
Glossopteris
Climate clues
Continental Drift Theory
Evidence:Puzzle-like fit of continentsIdentical fossils & rock structure on various
continentsGlacial deposits in present-day tropical climatesCoal deposits in present-day temperate climates
Wegener’s idea was rejected in early 1900’s –
because he could not answer:
“What caused the continents to move?”
“How, when, or why did continents move?”
Sea Floor Spreading
1947 – rocks on ocean floor found to be younger than continental rocks
1960 – Princeton U. – Harry Hess – proposed theory of Seafloor Spreading – if seafloor is moving, continents may also be moving
mid-1960’s – paleomagnetic reversal time scale developed for continental rock matches that of rocks found on sea floor
The Geomagnetic Reversal Time Scale
Discovery of Sea-Floor Spreading
Sea-Floor Spreading