Earth and Space Science: Plate Tectonics, Carbon Cycle, Climate, Stars
Plate Tectonics Evidence
Continental fit, fossil evidence, matching rock layers, paleoclimate indicators, seafloor spreading, and magnetic striping all show that Earth's plates move over time.
- Continental fit (matching coastlines)
- Fossil evidence across now-separated continents
- Matching rock layers and geological sequences
- Paleoclimate indicators (evidence of past climates)
- Seafloor spreading at mid-ocean ridges
- Magnetic striping preserved in oceanic crust
Plate Structures
Different plate boundaries produce characteristic structures and landforms:
- Convergent boundaries: Volcanic mountains form where subduction causes magma to rise (example: Japan).
- Continental collisions: Non-volcanic mountain ranges form when two continental plates collide (example:
English with a size of 4.74 KB