Guided Notes about Continental Drift Chapter 17 Section

Guided Notes about Continental Drift Chapter 17, Section 1

1. Who were the first to consider the idea of moving landmasses? o Early mapmakers were the first to consider moving landmasses. They noticed how continents fit together.

2. Construct a flow map or timeline… o 1. Abraham Ortelius—late 1500’s: - thought that North America and South America were separated from Europe and Africa by floods and earthquakes.

2. Construct a flow map or timeline… o 2. Eduard Suess—late 1800’s: thought that the Southern continents were once joined together as a single landmass, which he called Gondwanaland

2. Construct a flow map or timeline… o 3. Alfred Wegener— 1912: -proposed theory of continental drift, but it was rejected by the scientific community

3. Describe Wegener’s theory of continental drift and Pangaea. o Earth’s continents were once joined as a single landmass. Wegener called it Pangaea, which means “all the Earth”. It broke apart 200 million years ago, and since that time, the continents have been drifting to their current positions.

Evidence for Continental Drift o o FIT OF THE COASTLINES the coasts of South America and Africa fit together like a puzzle in the Atlantic Ocean

Evidence for Continental Drift o o SIMILAR ROCK FORMATIONS Rocks in areas that were once joined have the same age and structure, such as the Appalachian Mountains and mountains in Greenland Europe.

Evidence for Continental Drift o o FOSSILS Fossils of land animals and plants were found in widely separated continents. These fossils are all the same age, which suggests that all land was once joined. Glossopteris (an ancient fern-like plant) Mesosaurus (a small aquatic reptile)

Evidence for Continental Drift o o o CLIMATE EVIDENCE Layers of coal were found in polar regions Glacial deposits were found in tropical and temperate regions

5. Why was Wegener’s hypothesis rejected? o o 1. Wegener could not explain what was causing the continents to move. 2. Wegener could not explain how the continents were able to move through the solid rock of the ocean floor.