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earths internal structure
plate tectonics and plate boundaries
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, German geophysicist
Alfred
Wegener
found that the continents fir together as pieces of a jigsaw puzzle do
Alfred Wegener theorized in the past that the continents were once joined as a single supercontinental he called
Pangaea
Wegener's theory would be later be improved upon, leading to a new theory -
the
theory
of
plate
tectonics
the theory of
plate
tectonics
explains the formulation, the movement, and the changes of the outer, rigid layers of Earth
one of the theories used to develop the plate tectonics theory is the
seafloor
spreading
theory
the seafloor spreading theory was theorized by American geologist
Harry
Hammond
Hess
according to the seafloor spreading theory, the
seafloor
splits
and
moves
apart
new oceanic crusts/floor is formed from the
magma
underneath the seafloors as it rises and fills the gap
new oceanic crust forms continuously at the crust of the
mid-ocean
ridge.
oceanic
ridges
are long, high, and continuous chains of mountains that seem to run around Earth
the
Mid-Atlantic
Ridge
is one such oceanic ridges that is located at the center of the Atlantic Ocean basin
to test the theory, samples of
volcanic
rocks
were taken from the ocean floor
the age of the sample rocks was determined and found that the rocks
near
the
mid-ocean
ridge
are
younger
than those farther from the ocean ridge
petrologists
study the origin, composition, distribution, and structure of rocks.
a
divergent
boundary
exists between two plates that move apart
a
convergent
boundary
lies between two tectonic plates moving towards each other
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