南アメリカプレート
Along the geologically complex southern boundary, the Caribbean Plate interacts with the South American Plate forming Barbados, Trinidad and Tobago (all on the Caribbean Plate), and islands off the coast of Venezuela (including the Leeward Antilles) and Colombia. This boundary is in part the result of transform faulting along with thrust faulting and some subduction. The rich Venezuelan petroleum fields possibly result from this complex plate interaction. The Caribbean Plate is moving eastward about 22 millimeters per year in relation to the South American plate. In Venezuela much of the movement between the Caribbean Plate and the South American Plate occurs along the faults of Boconó, El Pilar and San Sebastián.