Determine the general wave and longshore sediment transport directions by determiing where the sand is against where it is eroding, is heaping up.
from the top to the bottom
- The direction of beach drift
- Groyne
- The incoming wave direction
-The direction of the longshore current
<h3>What is longshore sediment transport?</h3>
- The collective movement of beach and nearshore sand parallel to the shore caused by the combined action of tides, wind, and waves, as well as the shore-parallel currents produced by them, is referred to as longshore transport.
- Usually, these forces cause sand to move practically continuously, either in bedload flows or suspension.
- This happens in an intricate, three-dimensional pattern that changes quickly over time.
- Sand in the area of interest may occasionally have an upcoast component whereas other sand is often migrating downcoast.
Learn more about longshore sediment here:
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Answer:
Explanation:
Air masses form over large surfaces with uniform temperatures and humidity, called source regions. Low wind speeds let air remain stationary long enough to take on the features of the source region, such as heat or cold.
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The answer is the threat of earthquakes. Earthquakes may happen in territories where there are "skilled deficiencies". These are partitioning limits between two plates of the world's covering which have encountered no less than one noteworthy seismic movement amid the most recent 35,000 years, or a few huge exercises amid the most recent 500,000 years.
The distance between the earth and the sun is 92.96 million miles
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Answer:
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Explanation:
This promise lasted throughout Truman's time in office and continued in the administrations that followed. The policy of containment later informed the “domino theory,” which stated that one country falling to Communism meant the surrounding countries were likely to fall as well.
