1. Convergent Boundaries:
- Continental-Continental: These occur when two continental masses collide. An example is the collision of the Indian and Eurasian plates, which formed the Himalayas.
- Oceanic-Continental: Occurs when an oceanic plate subducts beneath a continental plate. An example is the Nazca Plate subducting beneath the South American Plate, creating the Andes Mountains.
- Oceanic-Oceanic: Forms when two oceanic plates collide. An example is the Mariana Trench formed due to the collision and subduction of the Pacific Plate beneath the Philippine Plate.
2. Divergent Boundaries:
- Mid-Oceanic Ridges: These occur where two oceanic plates move away from each other. Examples include the Mid-Atlantic Ridge and the East Pacific Rise, where new oceanic crust is created.
3. Transform Boundaries:
- Fault Lines: These occur when two plates slide past each other horizontally. An example is the San Andreas Fault in California, USA, which marks the boundary between the Pacific and North American plates.
4. Plate Boundaries:
- Plate Margins: These are the boundaries between different tectonic plates. They can be convergent, divergent, or transform boundaries, depending on the nature of the plate movements.
It's important to note that these boundaries can occur in various regions around the world, and the specific locations can be found by studying plate tectonics and the geology of different regions.
