Based on the description of the plate boundary where one plate dives underneath another, the following statements are TRUE:
- Convection currents within the mantle are moving the plates.
- Subduction is occurring at this plate boundary.
- This type of boundary can form an oceanic trench.
The first two statements you listed (about rift valleys and it being a divergent boundary) are NOT true in this context. Instead, the scenario described indicates a convergent boundary, specifically one where subduction is occurring.