Continental-volcanic IS NOT a convergent boundary (Option D).
A convergent plate boundary occurs where two plates push against each other.
The three types of convergent boundaries include:
- Oceanic-Continental convergent boundaries, which occur when a continental plate and oceanic plate collide (e.g., the Nazca Plate under South America).
- Oceanic-Oceanic convergent boundaries, which occur when two oceanic plates collide (e.g., the Tonga Islands).
- Continental-Continental convergent boundaries, which occur when two continental plates collide (e.g., the Himalayas Mountains created by the collision of the India plate with the Eurasian plate).
In conclusion, continental-volcanic IS NOT a convergent boundary (Option D).
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