The correct answer is oceanic; subduction
The lithosphere layer is above the asthenosphere, a layer that presents the rocks in a more pasty state, due to the high temperatures present inside the planet. The meeting zone between the lithosphere and the asthenosphere has an isotherm, that is, a constant temperature, which is approximately 1,200ºC. Thus, everything above this point of contact has sufficient temperatures to make the rocks remain rigid.
It should be noted that coastal upwelling occurs when the wind blow surface waters laterally. There is an abundance of marine life in these areas because of the dense nutrient concentrations in upwelled waters.
<h3>How to illustrate the information?</h3>
Strong winds that blow off the coasts of continents and the earth's rotation generate a phenomenon known as coastal upwelling that pushes surface waters offshore. Then, water from the ocean's depths is drawn up, or upwelled, to the surface to replace it.
Along the west coast of continents, upwelling occurs most frequently (eastern sides of ocean basins). Along west coasts in the Northern Hemisphere, upwelling happens.
Coastal upwelling occurs when the wind blow surface waters laterally.
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Answer:
Computers produce maps using data from many sources, including <u>satellites and global positioning system (GPS)</u>. Where instruments are used to determine distance and elevation.
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Answer:
Before the Journey, Hispaniola and Hurricane, Across the Caribbean, and Hurricane
