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Answer:
the outside layer, mantle, inner core and core.
Explanation:
the outside rock layer is a hard outer crust that is relatively thin compared to the rest of the layers. When this layer cracks it can cause volcanic eruptions because the hot magma has built up a lot of pressure so it can force itself through the gap/crack. The mantle is the layers just under the crust. A lot of pressure is built up here as it has a thinner cooler layer above it and a hotter liquid/ hotter rocks just below it. The inner core. This is very hot as it can reach a temperature of around 6,000°c. this is a liquid layer just before the solid inner core of the earth. The core. This is the very centre of the earth and therefor the hottest. This solid centre has a rough minimum of 15,000°F and can roughly get as hot as the sun, scientists have proven that fact. <u>I</u><u> </u><u>hope</u><u> </u><u>this</u><u> </u><u>helped</u><u> </u><u>a</u><u> </u><u>little</u><u> </u><u>with</u><u> </u><u>your</u><u> </u><u>issue</u><u> </u><u>:</u><u>)</u>
Answer:
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Answer:
Teotihuacan.
Explanation:
The Classic period was considered a trade mark of the cities of Mayan culture.
This period took place in 250 AD to 900 AD, and all the achievements of arts were achieved by the Mayan civilizations in this period.
Here's a timeline:
400 AD -- Teotihuacan became the dominant city that had power over Mayan's mountains.
560 AD -- Tikal city was conquered by the union of other city-states.
600 AD -- Teotihuacan stopped being the center of cultural events.
900 AD -- Teotihuacan gets abandoned. The end of Maya Classic period.
Archeologists and other people still know very little about those events and why this period was ruined and over, it all still remains a mystery.
