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the sideways and downward movement of the edge of a plate of the earth's crust into the mantle beneath another plate.

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Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice, and/or by the force of gravity acting on the particles.

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Deposition is the geological process in which sediments, soil and rocks are added to a landform or land mass.

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In earth science, erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transport it away to another location (not to be confused with weathering which involves no movement).

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Weathering is the breaking down of rocks, soil, and minerals as well as wood and artificial materials through contact with the Earth's atmosphere, water, and biological organisms.

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The freezing process, also called crystallization, involves cooling salt water to form crystals of pure ice. The ice crystals are separated from the unfrozen brine, rinsed to remove residual salt, and then melted to produce fresh water

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Volcanism is the phenomenon of eruption of molten rock (magma) onto the surface of the Earth or a solid-surface planet or moon, where lava, pyroclastics and volcanic gases erupt through a break in the surface called a vent

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hot fluid or semifluid material below or within the earth's crust from which lava and other igneous rock is formed by cooling.

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Metamorphism is the change of minerals or geologic texture distinct arrangement of minerals in pre-existing rocks protoliths, without the protolith melting into liquid magma a solid-state change.

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At the same time the particles of sediment begin to stick to each other - they are cemented together by clay, or by minerals like silica or calcite.

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Lithification is the process that turns loose, unconsolidated sediment into solid sedimentary rock.

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Sedimentary Rocks are types of rock that are formed by the deposition and subsequent cementation of that material at the Earth's surface and within bodies of water.