The Juan de Fuca Plate is primarily a convergent tectonic plate. It is located off the northwest coast of North America, beneath the Pacific Ocean and adjacent to the North American tectonic plate.
This plate is involved in a convergent boundary interaction with the North American Plate. At these boundaries, the denser oceanic plate, which in this case is the Juan de Fuca Plate, is forced beneath the lighter continental plate, resulting in subduction. This process leads to the formation of oceanic trenches, volcanic activity, and earthquakes in the region.
To summarize, the Juan de Fuca Plate is indeed convergent as it is being subducted under the North American Plate, leading to significant geological activity in the Pacific Northwest.