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:
542.5 km
Explanation:
average thickness of granitic continental crust = 35 km
Average density of crust ( from section C1 ) (pc) = 3.3 g/cm^3
Average density of mantle (Pd) = 3.1 g/cm^3
applying the concept of Isostay
attached below is the missing part of the question and solution
Answer:
C) more moist broadleaf forests.
Explanation:
Answer: Libyan Desert<span> and the Nubian </span><span>Desert .
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Answer:
C Countour scale
Explanation:
The contour scale is not one of the scales that represent map scale.
A map scale is one that shows the relationship between the ground distance and the one on paper or a model.
Some scale usually associates the real distance to that one shown on a map.
- Map scales can take any of the following forms:
- ratio scale or representative fraction
- word scale or statement scale
- Linear scale or bar scale
There is no such thing as contour scale.
