Convergent plate boundaries may have _____.
strike slip zones
divergent zones
mid ocean ridges
sebduction zones
From Google:
If two tectonic plates collide, they form a convergent plate boundary. Usually, one of the converging plates will move beneath the other, which is known as subduction. ... While the process is volcanic, volcanoes and earthquakes along oceanic spreading ridges are not as violent as they are at convergent plate boundaries.
Convergent plate boundaries are areas where two tectonic plates come together. They can have several features, including:
1. Strike-slip zones: While strike-slip faults are more commonly associated with transform plate boundaries, they can also occur in some cases along convergent boundaries. These zones occur when two plates slide past each other horizontally, causing significant earthquakes. Examples include the San Andreas Fault in California.
2. Divergent zones: Divergent boundaries occur when two plates move away from each other. However, convergent boundaries are characterized by plates moving towards each other, so divergent zones are not typically found along convergent boundaries. Examples of divergent boundaries include the Mid-Atlantic Ridge and the East African Rift.
3. Mid-ocean ridges: Mid-ocean ridges are underwater mountain ranges that form at divergent boundaries where new oceanic crust is created as two plates move apart. These features are not typically found at convergent boundaries.
4. Subduction zones: Subduction zones are a common feature of convergent plate boundaries. They occur when one tectonic plate is forced beneath another into the Earth's mantle. Subduction zones are characterized by intense geological activity, including the formation of deep-sea trenches, volcanic activity, and powerful earthquakes. Examples of subduction zones include the Cascadia Subduction Zone in the Pacific Northwest and the Andean subduction zone in South America.
Therefore, strike-slip zones and subduction zones are features commonly associated with convergent plate boundaries, while divergent zones and mid-ocean ridges are not typically found in these regions.