Which of the following locations is NOT an example of convergence between oceanic plates?

The Himalayas serve as an example of continental convergence rather than oceanic plate convergence. The Himalayas were formed as a result of the collision between the Indian Plate and the Eurasian Plate, both of which are continental plates. In this scenario, instead of one plate being subducted beneath the other—common in oceanic-oceanic convergence—both plates push against each other, resulting in the uplift that forms mountain ranges.

In contrast, locations like the Aleutian Islands and the Marianas Trench are where oceanic plates converge. The Aleutian Islands are primarily formed by the subduction of the Pacific Plate beneath the North American Plate. Meanwhile, the Marianas Trench is the deepest oceanic trench in the world, created by the subduction of the Pacific Plate beneath the Mariana Plate. Similarly, Java in Indonesia represents an area where oceanic plates converge, specifically the subduction of the Indo-Australian Plate beneath the Eurasian Plate.

Thus, while other choices involve oceanic plate convergence, the Himalayas are distinctly characterized by continental plate interaction.