This sediment eventually formed into limestone.

If there is a large angle between the waves and the shoreline, the sediment converges, accumulates, and forms beach ridges.

The sediment has formed a clastic wedge making up most of the coastal plain and continental shelf.

Fine grained sediments and carbonate rocks formed from 1675 to 1590.

During the ensuing Pennsylvanian epoch the same sediments eroded from the mountains had formed an expansive coastal plain.

Layered sediment forms the valley, containing fossils from when the area was once covered by the sea.

The sediments traveled westward and formed a great delta into the sea that was in the area at that time.

Fine sediments formed a level lakebed.

The dark sediments have formed a patch at Euphrates' base.

After death, sediment enters and forms a cast of the central cavity of the stem.