noun a flat expanse of the deep ocean floor, usually found at depths greater than 2000 meters
Abyssal plains are formed by the accumulation of sediment over millions of years, creating a smooth, flat surface on the ocean floor.
Abyssal plains are important habitats for deep-sea organisms, providing a stable environment for a variety of marine life.
Abyssal plains are part of the broader topography of the ocean floor, and their study helps scientists understand the geological processes shaping the Earth's surface.
Abyssal plains are flat areas on the ocean floor that are covered in sediment and are typically found at depths of 3,000 to 6,000 meters.
Abyssal plains are often mentioned in scientific articles or books written by geologists, oceanographers, or environmental scientists discussing the ocean floor topography.
Geologists study abyssal plains as part of their research on plate tectonics, seafloor spreading, and the formation of ocean basins.
Oceanographers frequently study abyssal plains to understand deep-sea ecosystems, sedimentation processes, and the geological history of the ocean floor.
Marine biologists may explore abyssal plains to study the unique life forms that inhabit these deep-sea environments and to investigate adaptations to extreme conditions.