Terrigenous sediments are likely find on the landward side of a bar trough.
Terrigenous sediments in oceanography are those that result from the erosion of land-based rocks; they are thus sourced from terrestrial (as opposed to marine) environments.
Rivers carry sand, mud, and silt, and these sediments are mainly deposited on the continental shelf. Their composition is typically related to the source rocks.
Terrigenous sediments are produced by a variety of processes, such as volcanic eruptions, rock weathering, wind-blown dust, glacial churning, and sediment transport by rivers or icebergs.
A large portion of the salt in today's oceans is the result of terrible sediments. Minerals are still carried by rivers to the ocean throughout time, but when water evaporates, the minerals are left behind.
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