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- During convection in the mantle, hot lower mantle material rises upward1. As it rises, it cools and moves horizontally at the top of the mantle. Over time, it becomes cool and dense enough that it sinks and travels horizontally at the bottom of the mantle. Eventually, the material gets to the location where warm mantle material is rising1. Cool rock material sinks during convection in the mantle because it no longer possesses the heat energy that thrust it upwards away from the intense heat of the outer core2. As hot rock rises up from the deep Earth, it carries heat with it. That heat comes through the crust through volcanoes and rocks in the crust. Then when the mantle rock cools off, it falls back down towards the center3.
Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.Hot lower mantle material rises upward (Figure above). As it rises, it cools. At the top of the mantle it moves horizontally. Over time it becomes cool and dense enough that it sinks. Back at the bottom of the mantle, it travels horizontally. Eventually the material gets to the location where warm mantle material is rising.k12.libretexts.org/Bookshelves/Science_and_Tech…Cool rock material sinks during convection in the mantle because it no longer possesses the heat energy that thrust it upwards away from the intense heat of the outer core. convection currents in the mantle are the result of the upward motion of molten rock heated deep within the earth.socratic.org/questions/5a0b9e0a7c01494364d1a68dAs hot rock rises up from the deep Earth, it carries heat with it. That heat comes through the crust through volcanoes and rocks in the crust. Then when the mantle rock cools off, it falls back down towards the center.scienceline.ucsb.edu/getkey.php?key=6612 - People also ask
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When the warm material reaches the surface, it spreads horizontally. The material cools because it is no longer near the core. It eventually becomes cool and dense enough to sink back down into the mantle. At the bottom of the mantle, the material travels horizontally and is heated by the …
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May 24, 2022 · When the warm material reaches the surface, it spreads horizontally. The material cools because it is no longer near the core. It eventually becomes cool and dense enough to …
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Nov 15, 2017 · Cool rock material sinks during convection in the mantle because it no longer possesses the heat energy that thrust it upwards away from the intense heat of the outer core. …
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5 days ago · Hot lower mantle material rises upward. As it rises, it cools. At the top of the mantle, it moves horizontally. Over time it becomes cool and dense enough that it sinks. Back at the …
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Jun 18, 2024 · Cool rock material is denser than warm rock material, so it tends to sink towards the base of the mantle. As it heats up, the warm rock material becomes less dense and …
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