PLATE TECTONICS
PRESENTED BY GROUP 4
CONTINENTAL DRIFT
• In the 1900’s, German meteorologist by the name of Alfred
Wegener was the first to present an argument supporting
continental drift. He proposed that the continents were not
stationary, but actually moving or drifting away from one
another. His primary sources of evidence included the fit of the
continents, glacial till deposits, and the apparent shifting of
climatic belts over time. His colleagues at the time argued for
polar wandering as an explanation of his data. These ideas were
not well accepted until later scientists in the 1940’s and 50’s
expanded on this ideas adding to them paleomagnetism,
convection currents and seafloor spreading. With all these new
evidence, plate tectonic theory become an accepted theory in
the 1970’s.
• Continental drift was a theory that explained how continents
shift position on Earth's surface.
• Continental drift was a theory that explained how continents shift position on Earth's surface.
EVIDENCE THAT SUPPORT THE CONTINENTAL
DRIFT THEORY
1. Wegener notice that the continents seemed to fit together, not
at the continuously changing shoreline, but at the edge to their
continental shelves. He derived the hypothesis from the
observation that the continents in the southern hemisphere
exhibit an identical pattern at rock and fossils know as the
“Gondwana sequence”. The most logical explanation was that
the continents themselves were once part of a mush larger
“super-continent” which was named Pangaea
• 2.
SEAFLOOR SPREADING
HOW THE SEAFLOOR SPREADS
STRUCTURE AND EVOLUTION OF OCEAN BASINS
HOW THE MOVE LEADS TO THE FORMATION OF FOLDS,
FAULTS, TRENCHES, VOLCANOES, RIFT VALLEYS, AND
MOUNTAIN RANGES