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The Continental Drift

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The Continental Drift
Shawna Taylor
SCI 101-1404A
November 3, 2014

The Continental Drift was a theory in the early 20th century of Alfred Wegener, a German scientist. Wegener believed that the continental landmasses were drifting across the earth. Wegener noticed the coasts of South America and western Africa looked like a jigsaw puzzle with interlocking pieces. Both continents had some of the same biological and geological similarities. The fossil of the ancient reptile mesosaurus was only found in South America and southern Africa. The mesosaurus is a freshwater reptile roughly one meter long and couldn’t have swum in the ocean due to it being a freshwater reptile. Wegener also believed that all the continents were once joined in a super continent also known as Pangaea meaning all lands in Greek.
Many scientists didn’t believe Wegener’s theory of the continental drift back then. Today’s scientists know now that continents sit on massive slabs called tectonic plates. Tectonic plates are constantly interacting and moving called plate tectonics. After a period of time the tectonic activity changes the surface of the earth and reshapes and rearranging the landmasses.
The scientific method attempts to explain the phenomena of the universe using a consistent, logical, systematic method of investigation, using data collection, hypothesis, experiment, and a theory. Establishing a new theory must be introduced to the scientific community, be well written, documented and submitted to a scientific journal for publication.
Qualative science generates a hypothesis, focuses on studying ideas, and captures rich, contextual, and detailed information from a small number of participants. Qualative science is generally inductive and answers why and what does it mean questions. Quantitive science tests a hypothesis, answers how much, how many and what questions and is generally

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