Ferrel Seamount is an underwater volcano located in the North Pacific Ocean. It is part of the Aleutian Arc, a volcanic island arc that is situated near the northern edge of the Pacific Plate. Ferrel Seamount is known for its steep underwater slopes and prominent peak, which rises significantly from the ocean floor. The seamount is primarily composed of volcanic rocks, and like many seamounts, it may host a variety of marine life due to the nutrient-rich waters that surround it.
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