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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Answer: Ram Nath Kovind
Explanation:
is an Indian politician currently serving as the 14th President of India, in office since 25 July 2017
The majority of species require <u>oxygen</u> to survive
a <u>continental convergent boundry</u> is when a continental and oceanic plates collide, the <em>thinner and more dense oceanic plate is overridden by the thicker and less dense continental plate</em>. The oceanic plate is forced down into the mantle in a process known as "subduction."
hope this helps! ❤ from peachimin (aka kayla)
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