An oceanic plateau is a large, flat area of the ocean floor that rises significantly above the surrounding seabed. These plateaus are typically formed by volcanic activity or the accumulation of sediments over time. They are often found near mid-ocean ridges or continental margins and can extend for thousands of kilometers. Oceanic plateaus are important for marine ecosystems, as they provide unique habitats for various species. They can also influence ocean currents and climate patterns. Notable examples of oceanic plateaus include the Shatsky Rise in the North Pacific Ocean and the Kerguelen Plateau in the Southern Ocean.