seafloor sedimentation

Seafloor sedimentation is the process by which particles settle to the ocean floor over time. Tiny bits of organic matter, minerals, and other materials from rivers, wind, and ocean currents accumulate on the sea bed. This sediment can come from land, like soil erosion, or from marine life, such as shells. As layers build up, they can form rocks and provide a record of Earth’s history, including past climates and environments. Understanding sedimentation helps scientists study ocean ecosystems, geological processes, and even the potential for natural resources like oil and gas on the seafloor.