The relief of coastal lowlands is typically very low, with elevations rarely exceeding a few meters above sea level. This is due to the fact that these areas are often formed by the deposition of sediment from rivers and streams, which tends to create a flat landscape. In some cases, coastal lowlands may be formed by the erosion of cliffs or headlands, which can create a more rugged landscape.
Coastal lowlands are often found in areas with a high rate of erosion, such as along coastlines that are exposed to strong winds and waves. This erosion can cause the coastline to retreat, and can also lead to the formation of new coastal lowlands. In some cases, coastal lowlands may also be formed by the subsidence of the land, which can occur as a result of natural processes or human activities.