Answer 1:
This is a great question. Alfred Wegener was a
German scientist who suggested the theory of
continental drift. His theory suggested that
Earth was a one big supercontinent called
Pangaea. The Pangaea broke up and drifted
to form all those continents you see today. He
backed up his theory by many observations and
similarities of fossils in different parts of the
continents. However, his theory was rejected
because of two reasons:
The first reason was that his theory of
continental drift was just too weak for most
geologists to accept. Even though he believed
the supercontinent that broke up into different
continents moved, he did not have a clear
explanation to how the continents moved. The
other reason is that some of his explanation
clashed with ideas that were widely accepted in
the science communities. He used similar
fossils from different continents to back up his
theory of continental drift. However, at that
time, many scientists that had observed
similarities in fossils in places like South
America and Africa believed there were similar
fossils in different continents because of a land
bridge that were formed by two continents.
Many science communities believe that land
bridges allowed migration of many different
species and even people to one place to another by
large bodies of water frozen by low temperature
known as ice age.
Though many scientists today continue to reject
Wegener’s explanation for continental drift,
his statement of drifting continents has gained
wide acceptance in the science community. This
is because throughout many years, new
information was found. For instance, in the
1950, evidence for sea floor spreading was
discovered by the US Navy scientists. This led to
the formation of plate tectonics, and part of its
evidence suggests that continents do move,
which supports Wegener’s statement about
continents drifting apart from each other. Even
though Wegener’s theory was rejected, his
contribution led a base for future scientists to
support or reject his theory of continental drift.
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