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Explore the fascinating theories of Continental Drift and Plate Tectonics. Originally proposed by Alfred Wegener, the Continental Drift theory suggests that Earth's continents were once joined as a single landmass, Pangaea, before drifting apart over time. Evidence from matching coastlines and geological structures supports this idea. Furthermore, the Sea Floor Spreading Theory explains how new crust forms due to plate movements. Dive into the behavior of tectonic plates, their boundaries, and the geological features they create, including ocean ridges, volcanoes, and earthquake zones.
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Crust Mantle Outer Core Inner Core
Abraham Ortelius Eduard Suess
Alfred Wegener Continental Drift
Continental Drift Theory In the distant past, the Earth’s continents were all joined as a single landmass and broke into pieces and eventually drifted away from each other.
Evidence for His Theory South America and Africa would fit remarkably well, shoreline to shoreline.
Evidence for His Theory If the N. and S. Americas were moved next to Africa and Europe, there would be a match of ancient continental rocks and tectonic (fold and fault) structures.
Evidence for His Theory When Wegener placed all the continents together like a puzzle, they formed a large landmass which he called ...
What made Alfred Wegener different from the other scientists that conceived the idea of drifting continents?
The scientific community during Wegener’s time did not accept his proposition. What was the reason behind this?
Continental Drift Theory + In the distant past, the Earth’s continents were all joined as a single landmass and broke into pieces and eventually drifted away from each other. Sea Floor Spreading Theory
Continental Drift Theory + It states that new crust are formed as a result of continuous plate movement. Sea Floor Spreading Theory
? PLATE TECTONICS Theory
We know what PLATES are, but what do we mean by TECTONICS?
“TO BUILD” “FORMATION” “DEFORMATION”
Behavior of the Plates
Plate Boundaries • Divergent • Convergent • Transform
Geologic Features Ocean Ridges Volcanoes Rift Valleys Trenches Subduction Zones Volcanic Island Arcs Mountain Ranges Faults Shallow Earthquakes
What happens in DIVERGENT boundaries?
MID-OCEAN RIDGE OCEAN CRUST MAGMA MANTLE
CONSEQUENCE? DIVERGENT Boundaries
Spreading Ridges As plates move apart new material is erupted to fill the gap