The Dynamic Interior of the Earth Plate Tectonics The Dynamic Interior of the Earth

Review of Earth’s Interior: Name, in order going from the center of the Earth to where we live, the four major layers of the Earth. What composes the lithosphere? How do the two layers closest to the center of the Earth differ in their composition? Describe how scientists determine the composition of the different layers of the Earth.

If you look at a map of the world, you may notice that some of the continents could fit together like pieces of a puzzle.

Plate Tectonics The Earth’s crust is divided into 12 major plates which are moved in various directions. This plate motion causes them to collide, pull apart, or scrape against each other. Each type of interaction causes a characteristic set of Earth structures or “tectonic” features. The word, tectonic, refers to the deformation of the crust as a consequence of plate interaction.

The World’s Plates

What are tectonic plates made of? Plates are made of rigid lithosphere. Remember - The lithosphere is made up of the crust and the upper part of the mantle.

Theory of Continental Drift Proposed by Alfred Wegener in early 1900’s. He hypothesized that the continents were once joined together in a single large land mass he called Pangea Pangea split apart and the continents moved gradually to their present positions Process is known as Continental Drift

Pangaea, about 200 million years ago, before it began breaking up Pangaea, about 200 million years ago, before it began breaking up. Wegener named the southern portion of Pangaea Gondwana, and the northern portion Laurasia.

The continents about 70 million years ago The continents about 70 million years ago. Notice that the breakup of Pangea formed the Atlantic Ocean. India’s eventual collision with Eurasia would form the Himalayan Mountains.

Learning Check What layer of the Earth composes the tectonic plates? How many “major” plates make up the Earth? Who develop the theory of plate tectonics? Describe Pangea.

Evidence of Continental Drift Continents fit together like a puzzle. Ex. - The Atlantic coastlines of Africa and South America.

More Evidence… Fossils of several plants and animals of the same species found on different continents.

Some More Evidence Rock sequences (the order of rock layers) in South America, Africa, India, Antarctica, and Australia show remarkable similarities. Wegener showed that the same three layers occur at each of these places.

Cont’ The same three layers are in the same order in areas now separated by oceans. Wegener proposed that the rock layers were made when all the continents were part of Pangaea. He proposed that they formed in a smaller small joined land mass that was later broken and drifted apart.

Another Learning Check… Explain 3 pieces of evidence used to support Wegener’s theory of continental drift.

Sea Floor Spreading Everyone agreed that Wegener’s evidence was compelling. But wouldn’t we feel the movement? Also, wouldn’t there be evidence to show that the continents were still moving today? Wegener was a meteorologist and his theory was not well accepted. (He died on an expedition in Greenland collecting ice samples)

Sea Floor Spreading One reason scientists had a hard time with Wegener’s theory is that there was no mechanism for the continents motion.

Sea Floor Spreading Henry Hess 1960’s Using new technology, radar, he discovered that the seafloor has both trenches and mid-ocean ridges. Proposed the sea-floor spreading theory.

Sea Floor Spreading Hess proposed that hot, less dense material below Earth’s crust rises toward the surface at the mid-ocean ridges. Then, it flows sideways, carrying the seafloor away from the ridge in both directions.

Sea Floor Spreading As the seafloor spreads apart at a mid-ocean ridge, new seafloor is created. The older seafloor moves away from the ridge in opposite directions. This helped explain how the crust could move—something that the continental drift hypothesis could not do.

Evidence of Seafloor Spreading In 1968, scientists aboard the research ship Glomar Challenger began gathering information about the rocks on the seafloor. Scientists found that the youngest rocks are located at the mid-ocean ridges.