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Continental Drift
Alfred Wegener
• In 1910, Alfred
Wegener became
curious about the
continents. He
formed a hypothesis
that the continents
had moved.
• Wegener’s hypothesis was that
all continents had been joined
together in a single landmass
and have since moved apart.
• He named this
super continent
Pangaea. This
idea was known
as Continental
• 1. Landforms
– Mountain ranges and other features
on continents provided evidence.
South America and Africa fit
together like puzzle pieces. A
mountain range in South America
lined up with a mountain range in
Africa. European coal fields
matched up with ones in North
• 2. Fossils
–A fossil is a trace of an organism
preserved in rock. Fossils of the
reptiles Mesosaurus and
Lystrosaurus had been found in
places now separated by oceans.
Another example was the fernlike plant Glossopteris found in
Antarctica, Africa, South
America, Australia and India.
-included most of the landmasses
that make up today’s northern
- Southernmost supercontinent
that was once part of Pangaea
• 3. Climate
–Fossils of tropical plants
were found in Antarctica.
–Glaciers once covered South
Africa. Deep scratches from
the glaciers were found on
Rejection of Wegener’s
• Wegener could not provide
evidence for the forces that push or
pull the continents. Many
geologists in the 1900’s thought the
earth was slowly shrinking and
cooling. Wegener disagreed with
this proposal because mountains
usually appear in narrow bands
along the edge of continents
New evidence today:
• The Ring of Fire; showing that the
plates once were connected and
seismic activity in the mantle has
caused the movement and the
eruption of volcanoes and
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