The document summarizes Alfred Wegener's theory of continental drift from 1912. It proposed that the continents were once joined together in a supercontinent called Pangea, which later broke apart and drifted to their current positions. Wegener noted evidence like matching coastlines, fossil and rock formations, but did not know the mechanisms that caused the movement. The theory of plate tectonics was later developed to explain how convection currents in the mantle cause the movement of rigid tectonic plates across Earth's surface, opening oceans at mid-ocean ridges and closing them during subduction.
2. Proposed by Alfred
Wegener in 1912; the
hypothesis that state that
the continents once formed
a single landmass
(Pangea), broke up, and
drifted to their current
location
3.
4. a) Shape of the continents
b) Fossil evidence on both
sides of the Atlantic
c) Rock formations on both
sides of the Atlantic
d) Climatic evidence (i.e.
evidence of glaciers in
Southern Africa)
5.
6. He could not come up with
the mechanisms or process
that caused the continents
to move
7. a) Mid-Ocean Ridges – a
long undersea mountain
chain that has a
steep, narrow valley at its
center, that forms as
magma rises from the
mantle, and that creates
new ocean floor as the
tectonic plates move apart
8. b) Sea Floor Spreading –
the process by which new
oceanic crust forms as
magma rises to Earth’s
surface and solidifies at a
mid-ocean ridge, symmetry
of rock layers show oldest
layers are farther from the
ridge
9. c) Paleomagnetism –
• As magma solidifies, iron
particles line up with the
Earth’s magnetic field
• Rocks show reversals in
the Earth’s Magnetism
• Rocks show symmetrical
patterns on both side of the
ridges, thus both plates
formed at the same time
10.
11. The theory that explains
how large pieces of the
crust, called plates, move
and change shape
12. Lithosphere – solid, outer
layer of the Earth that
consists of the crust and the
rigid upper part of the
mantle
Asthenosphere – the
solid, plastic layer of the
mantle that flows slowly
14. Convection – the movement
of hot, less dense material
up and cold, more dense
material down
15. • Interior of the Earth heats
the mantle which rises to
the surface at the Mid-
Ocean Ridges
• Cools into rock and
eventually sinks back
into the mantle where it
is melted and sinks
• This movement of the
mantle drags the plates
with it
16.
17. The boundary between
tectonic plates that are
moving away from each
other.
Results in: magma rises to
surface, forms mid-ocean
ridges and rift valleys
25. An area around the Pacific
Ocean characterized by
volcanoes and seismic
activity
26. Areas where magma
reaches the surface, the
source is under the plates
so the hot spot does not
move, but the plates
do, creates island arcs like
Hawaii
