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During subduction, one tectonic plate moves beneath another into the mantle. This process can cause melting of the descending plate, leading to the formation of magma. This magma can then rise to the surface through volcanic activity, contributing to the formation of new igneous rocks and completing the rock cycle.

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By which process is the earths crust returned to the mantle?

The process by which the Earth's crust is returned to the mantle is known as subduction. In subduction zones, oceanic plates are forced beneath continental plates, carrying crustal material back into the mantle where it is recycled. This process is a key part of the Earth's tectonic cycle.


What does subduction mean in the rock cycle?

Subduction in the rock cycle refers to the process where one tectonic plate moves underneath another at a convergent boundary. As the plates collide, the denser oceanic plate sinks into the mantle, leading to the recycling of crustal material back into the Earth's interior. This process plays a crucial role in the formation of volcanic arcs and mountain ranges.


Evaporation and precipitation are two important parts in the?

water cycle. Evaporation occurs when water from bodies of water or plants turns into vapor due to heat from the sun. Precipitation happens when this vapor condenses and falls back to Earth's surface as rain, snow, sleet, or hail.


What happens during the diurnal cycle?

During the diurnal cycle, which spans roughly a 24-hour period, there are various changes that occur in the environment and living organisms. This includes fluctuations in temperature, light intensity, and atmospheric pressure, as well as corresponding behaviors and physiological adaptations in animals and plants to optimize their survival and reproductive success. For example, some animals are more active during the day while others are more active at night, depending on their feeding and predatory habits.


What cycle is guano an important part of?

Guano is an important part of the phosphorus cycle. It contributes to the cycling of phosphorus from the environment to living organisms and back again.