Sedimentation is the natural process by which sediments, such as sand, silt, and clay, accumulate over time.
It occurs in various environments, including rivers, lakes, and oceans, and can be driven by factors like water flow, wind, and ice.
Important points about sedimentation:
- It helps form sedimentary rocks over extended periods.
- Rate of sedimentation can vary based on environmental conditions and geological events.
- It plays a significant role in shaping landscapes and can provide critical information about Earth's history through sediment layers.
Understanding sedimentation rates, like in the given problem where sediments accumulate at 1 mm per year, is crucial in estimating geological timelines and changes.