Convergent boundaries result in

Convergent boundaries occur where two tectonic plates move toward each other. This interaction can lead to several geological features and phenomena, including: 1. **Mountain Ranges**: When two continental plates collide, they can create mountain ranges. An example of this is the Himalayas, formed by the collision of the Indian and Eurasian plates. 2. **Subduction Zones**: When an oceanic plate converges with a continental plate, the denser oceanic plate is forced beneath the continental plate, creating a subduction zone. This can lead to the formation of deep ocean trenches, such as the Mariana Trench. 3. **Volcanic Activity**: Subduction zones often lead to volcanic activity as the subducted plate melts and forms magma, which can rise to the surface. This is seen in the Pacific Ring of Fire, where many active volcanoes are located. 4. **Earthquakes**: The movement of tectonic plates at convergent boundaries can cause significant stress to build up, leading to earthquakes. These can be very powerful, especially in subduction zones. 5. **Metamorphic Rocks**: The intense pressure and heat generated by the collision of tectonic plates can lead to the formation of metamorphic rocks. In summary, convergent boundaries are associated with mountain building, subduction zones, volcanic activity, earthquakes, and the formation of metamorphic rocks.