Answer: General Sherman
Explanation: Hope it helps :)
Hey there!!
Scientists are able to understand Earth's interior by studying seismic waves<span>. These are waves of energy that travel through Earth, and they move similarly to other types of waves, like sound waves, light waves, and water waves.</span>
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Answer:
Upwelling is<u> a process in which deep, cold water rises toward the surface</u>. How displaced surface waters are replaced by cold, nutrient-rich water that “wells up” from below. Conditions are optimal for upwelling along the coast when winds blow along the shore. Winds blowing across the ocean surface push water away.
Explanation:
Upwelling is an oceanographic phenomenon that involves wind-driven motion of dense, cooler, and usually nutrient-rich water towards the ocean surface, replacing the warmer, usually nutrient-depleted surface water. The nutrient-rich upwelled water stimulates the growth and reproduction of primary producers such as phytoplankton.
Tectonic plates are parts (pieces) of the outermost layer of Earth: the Crust. (the outermost part of the mantle is also often included in the plates). This means that the land in the middle of the plates is relatively stable while the borders of the plates can be in movement - after all this is where two pieces meet. Plate borders are where the vocanoes and Earthquakes often take place.
Answer:Espero te sirva
Explanation:La subducción es el proceso de hundimiento de una placa litosférica bajo el borde de otra placa, formándose los llamados límites convergentes entre placas. La placa subducida, la que se hunde, suele estar formada por corteza oceánica, más delgada y densa que la continental. La subducción ocurre a lo largo de amplias zonas de subducción que en el presente se concentran especialmente en el entorno del océano Pacífico, en el llamado cinturón de fuego del Pacífico, pero también hay zonas de subducción en partes del mar Mediterráneo, las Antillas, las Antillas del Sur y la costa índica de Indonesia.
