Plate Tectonics Theory 2B Flashcards
Theory of Continental Drift
Continental landmasses were “drifting” across the Earth, sometimes plowing through oceans and into each other
Earth’s continents were once part of an enormous, single landmass called Pangea.
240 million years ago
Key Pieces of evidence that support the theory of continental drift
seafloor spreading - As the seafloor grows wider, the continents on opposite sides of the ridge move away from each other.
Mid-Atlantic Ridge
Rift valleys are sites where a continental landmass is ripping itself apart. Africa, for example, will eventually split along the Great Rift Valley system
Short term geological mechanisms for change
Examples: volcanoes, earthquakes, tsunamis, floods, landslides, meteorite impacts
Long term geological mechanisms for change
Examples: weathering, erosion, deposition
Mountain building
Erosion
Rocks break down to smaller pieces, the pieces get moved
How does erosion lead to the creation of mountains?
rocks break down, then get moved and pile up (deposition)
Describe the processes that lead to the creation of mountains
Erosion and weathering of rock, they move and settle somewhere else (deposition
Describe the constructive processes that shape land formations
Volcano eruptions
Mountain formations
Faults
What are the destructive processes that can alter the Earth’s surface?
physical weathering - shaking a sugar cube
Chemical weathering - vinegar vs water
Wind erosion
What causes weathering
wind, rain, rivers,