What are the different types of plate boundaries and their associated geological features?

Plate boundaries are the boundaries where the tectonic plates meet each other. There are three main types of plate boundaries:

• Divergent boundaries: These are the boundaries where two plates are moving away from each other. The geological features associated with divergent boundaries are rift valleys, mid-ocean ridges, and volcanic activity. Mid-Atlantic Ridge is an example of a divergent boundary.
• Convergent boundaries: These are the boundaries where two plates are moving towards each other. The geological features associated with convergent boundaries are subduction zones, mountain ranges, and volcanic activity. The Pacific Ring of Fire is an example of a convergent boundary.
• Transform boundaries: These are the boundaries where two plates are sliding past each other. The geological features associated with transform boundaries are earthquakes and fault lines. The San Andreas Fault in California is an example of a transform boundary.

Plate boundaries and their associated geological features play a significant role in shaping the Earth's surface and its geological history. The study of plate tectonics and the movement of the plates provides valuable insights into how the Earth works and how its features have evolved over time.