This document discusses coastal landforms and sediment transport along coastlines. It explains that sediments move parallel to the shoreline through processes like longshore currents and longshore drift. Sediments are deposited when waves lose energy, with larger sediments deposited first in sheltered areas. Coastal landforms like cliffs, shore platforms, headlands, and bays form through erosion processes acting on rocks of varying resistance over time. Cliff retreat leads to the formation of shore platforms, while differential erosion of resistant and less resistant rock bands creates alternating headlands and bays along indented coastlines.