Mountain Formation and Tectonic Plate Interactions
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The Formation of Mountains
The thickening of the crust, caused by the collision of continents, results in mountain ranges. The relief is formed by the collision of lithospheric plates, by volcanic activity, or hot spots in the crust. Both mechanisms are related to upstream and downstream flows that exist in the mantle.
- Oceanic Ridges: Present intense volcanic activity.
- Oceanic Trenches: Deep areas of the oceans.
- Abyssal Plains: Flat underwater areas, are the most extensive.
- Submarine Volcanoes: Isolated reliefs, which in some cases emerge from the ocean and cause volcanic archipelagos.
Interaction of Internal and External Processes
Isostatic movements are vertical movements of the lithosphere, which tends to sink in some places and rise in others.... Continue reading "Mountain Formation and Tectonic Plate Interactions" »