In: Physics
What evidence makes the theory of plate tectonics plausible?
Plate tectonics, theory dealing with the dynamic of Earth’s
outer shell—the lithosphere—that revolutionized Earth sciences by
providing a uniform context for understanding mountain-building
processes, volcanoes, and earthquakes as well as the evolution of
Earth’s surface and reconstructing its past continents and
oceans.
The theory of plate tectonics is based on a broad synthesis of
geologic and geophysical data. It is now almost universally
accepted, and its adoption represents a true scientific revolution,
analogues in its consequences to quantum mechanics in physics or
the discovery of the genetic code in biology. Incorporating the
much older idea of continental drift, as well as the concept of
seafloor spreading, the theory of plate tectonics has provided an
overarching framework in which to describe the past geography of
continents and oceans, the processes controlling creation and
destruction of landforms, and the evolution of Earth’s crust,
atmosphere, biosphere, hydrosphere, and climates. During the late
20th and early 21st centuries, it became apparent that
plate-tectonic processes profoundly influence the composition of
Earth’s atmosphere and oceans, serve as a prime cause of long-term
climate change, and make significant contributions to the chemical
and physical environment in which life evolves.