The rock cycle is the natural process in which rocks transform from one rock type into another rock type over time, a type of natural recycling.
Igneous rocks, which are formed from magma cooling underground, or lava above ground are formed from previous igneous, metamorphic, or sedimentary rocks which have become melted, usually as a result of plate collision and subduction.------->
When these igneous rocks are exposed to weathering and erosion, they break down into smaller particles that are transported by wind and water to a place of deposition, where they can form into sedimentary rock strata, through a process of lithification, where excess water is squeezed out by overburden pressures and the particles are cemented together by various minerals precipitating out of solution. Igneous and metamorphic rocks can both be turned into sedimentary rocks in this way.------->
Igneous and sedimentary rocks can also be changed by heat and/or pressure into metamorphic rocks, by transforming their existing mineral structures into new minerals or realigning the existing minerals. There are different degrees of metamorphism, so even an existing metamorphic rock can become a different metamorphic rock. -------->
If these metamorphic rocks are melted, then solidify, they become igneous rocks, and the cycle starts all over again.
The rock cycle is largely driven by lithospheric plate movements which cause subduction and uplift, also by climatic conditions and the associated erosional elements.
The carbon cycle is a natural process that moves carbon between the atmosphere, oceans, soil, and organisms. This cycle plays a crucial role in regulating Earth's climate and supporting life.
The phosphorus cycle does not pass through the atmosphere, as phosphorus mainly cycles through the lithosphere, hydrosphere, and biosphere. It moves through soil and rocks, then into plants and animals, and eventually back to the soil and water bodies.
Water moves through Earth's hydrosphere in a continuous cycle, known as the water cycle. This cycle includes processes such as evaporation, condensation, precipitation, and runoff, as water moves between the atmosphere, oceans, rivers, and groundwater. The movement of water is driven by energy from the sun and gravitational forces, making it a dynamic and essential part of Earth's ecosystems.
The process that repeatedly moves matter between different forms on Earth is the biogeochemical cycle. Examples include the carbon cycle, water cycle, and nitrogen cycle. These cycles involve the movement of elements and compounds through organisms, the atmosphere, water bodies, and the Earth's crust.
Water moves into the atmosphere through evaporation from bodies of water, such as oceans, lakes, and rivers, as well as transpiration from plants. Once in the atmosphere, the water vapor can condense to form clouds and eventually fall back to earth as precipitation, such as rain, snow, or hail. This cycle of evaporation, condensation, and precipitation is known as the water cycle.
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the water cycle
it moves uphill and towards the surface of earth
it fluctuates
Hydrologists study the water cycle. They research and monitor the movement, distribution, and quality of water on Earth, including how water changes state, moves through the atmosphere, and flows in various forms on the planet's surface.
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Water moves through biosphere. It travels through land, water and air.
It's called the Water Cycle (Hydrologic Cycle).
Into the atmosphere. Then it is basically recycled again through the CO2 cycle.
Solid, liquid, or gas.
Into the atmosphere. Then it is basically recycled again through the CO2 cycle.
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