The appropriate answer is B. Chains of volcanoes along ocean coastlines. The theory of plate tectonics states that the earth's crust is divided into plates that float on the semi-molten mantle below. Plates can converge, diverge or slide past each other. Chains of volcanoes along coastlines are evidence of plates converging with one plate subducting beneath the other. The subducting plate will melt producing magma which is lighter than surrounding rock and so will force its way through cracks and fissures in the surface. Once magma reaches the earth's surface, volcanoes are formed.
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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I believe the correct answer from the choices listed above is option A. Subduction is the collision between two tectonic plates. It is the biggest crash scene here on Earth. It is a geological process where one plate moves under another and is forced down into the mantle.
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