Which of the following is characteristic of oceanic-continental convergent plate boundaries?

Oceanic-continental convergent plate boundaries are characterized by several key features:

1. Subduction: This is the process where the denser oceanic plate is forced under the lighter continental plate. This is a key characteristic of oceanic-continental convergent boundaries.

2. Deep Ocean Trenches: These are formed at the point of subduction where the oceanic plate is forced under the continental plate.

3. Volcanic Activity: The subducted oceanic plate melts as it moves into the hotter asthenosphere, leading to the formation of magma. This magma rises through the crust to form volcanoes on the continental plate.

4. Earthquakes: These are common at these boundaries due to the movement of the plates.

5. Mountain Ranges: The collision and compression of the two plates can lead to the formation of mountain ranges on the continental plate.

6. Accretionary Wedge: This is a pile of sediment scraped off the subducting oceanic plate and accumulated at the edge of the continental plate.

These are the main characteristics of oceanic-continental convergent plate boundaries.