Erosion is a key external process in the rock cycle where rocks are broken down and transported by wind, water, or ice. Deposition is another external process where eroded materials settle and accumulate in new locations, eventually forming sedimentary rocks.
The two processes of the water cycle are responsible for creating a lake are:EvaporationCondensationThese processes are involved.
The two processes that cycle water from land to the atmosphere are:1. Evaporation2. Condensation
The two types of energy that drive the Earth's rock cycle are solar energy and geothermal energy. Solar energy powers processes such as weathering and erosion by driving atmospheric and hydrological cycles, while geothermal energy comes from the Earth's interior, facilitating processes like melting and metamorphism. Together, these energies contribute to the continuous transformation of rocks through various geological processes.
Igneous rock can undergo weathering and erosion, breaking down into sediments that may eventually compact and cement into sedimentary rock. Alternatively, it can be subjected to intense heat and pressure, transforming it into metamorphic rock. Both pathways illustrate the dynamic processes of the rock cycle, showcasing how rocks can change forms over geological time.
respiration is the reverse of photosynthesis and are the important processes of carbon cycle and water cycle.
Denudation and Volcanism.
External processes affect the surface of the Earth and include flooding.
The two processes in the rock cycle that must occur in order to change any rock into an igneous rock are melting (to form magma) and solidification (to form igneous rock). Melting of existing rocks due to high temperatures or pressure creates molten magma, which can then cool and solidify to form new igneous rocks.
The two processes of the water cycle are responsible for creating a lake are:EvaporationCondensationThese processes are involved.
The two processes that cycle water from land to the atmosphere are:1. Evaporation2. Condensation
The two processes resulting from sedimentary into metamorphic rock are known as contact metamorphism and regional metamorphism. Regional metamorphism most notably involves two tectonic plates colliding, while contact metamorphism occurs due to the intrusion of magma.
The heat from the centre of the Earth (fueled by nuclear fission and therefore the energy of an ancient supernova explosion) which drives tectonic convection processes.The heat from the Sun which drives the erosion processes.
The two types of energy that drive the Earth's rock cycle are solar energy and geothermal energy. Solar energy powers processes such as weathering and erosion by driving atmospheric and hydrological cycles, while geothermal energy comes from the Earth's interior, facilitating processes like melting and metamorphism. Together, these energies contribute to the continuous transformation of rocks through various geological processes.
Igneous rock can undergo weathering and erosion, breaking down into sediments that may eventually compact and cement into sedimentary rock. Alternatively, it can be subjected to intense heat and pressure, transforming it into metamorphic rock. Both pathways illustrate the dynamic processes of the rock cycle, showcasing how rocks can change forms over geological time.
respiration is the reverse of photosynthesis and are the important processes of carbon cycle and water cycle.
In the term "rock cycle," the word "rock" is acting as an adjective to describe the second word, "cycle." This term describes the process by which rocks are transformed and recycled through various geological processes over time.
Miller Cycle and Boxer. Internal and External.