Final answer:
The Cocos Plate is being subducted beneath the North American Plate at their convergent boundary, which can be identified on an interactive globe by the presence of an oceanic trench.
Step-by-step explanation:
The boundary between the Cocos Plate (CO) and the North American Plate (NA) is a convergent boundary where subduction is taking place. While using an interactive globe or map, this boundary can be identified by the presence of an oceanic trench off the western coast of Central America. In this case, the Cocos Plate is being subducted under the North American Plate.
A convergent boundary is characterized by the coming together of two tectonic plates. It is common for the denser oceanic plate, in this case, the Cocos Plate, to be forced underneath the lighter continental plate, which is the North American Plate. This process of subduction leads to high-pressure and high-temperature conditions that can result in earthquakes and volcanic activity as the subducted material is eventually melted and recycled in the Earth's mantle.