The early hypothesis of continental drift proposed by Alfred Wegener has
given way to the Theory of Plate Tectonics. This theory is (as described in
Chapter 19 of your textbook) the unifying theory of Geology, and provides
Earth scientists with a context for understanding the geological history of
our planet. Plate Tectonic theory has been confirmed by many observations
during the last 40 years or so.
Among the unique capabilities that the understanding of Plate Tectonics has
given geologists is the ability to reconstruct past positions of continental
landmasses showing the evolution of those continents from
the supercontinent of Pangea to the present day. Maps of continental positions
are made possible by studies of Earth's magnetism and the geological record
of Earth's magnetic field preserved in igneous and (some) sedimentary rocks.
Pangea 150 Million Years Ago (84.0K)Pangea 150 Million Years Ago
The image above is an reconstruction of Pangea and the arrangment of continental
landmasses as they appeared 150 million years ago, shortly after the Atlantic
Ocean basin began to open between North America and Africa. The outlines of
the modern continents are indicated with a black border so that you might
recognize this strange planet. Click on the link below to view a Virtual Vista
showing the breakup of Pangea and movement of the continents during the last
150 million years of Earth's history.