The answer is "igneous." Igneous rocks are formed from the solidification of molten material, such as magma or lava.
The two kinds of weathering are mechanical weathering, which breaks down rocks into smaller pieces without changing their chemical composition, and chemical weathering, which alters the chemical composition of rocks through processes like oxidation or dissolution.
Sedimentary rocks are primarily formed through the process of weathering, erosion, and deposition of sediments. These rocks include sandstone, limestone, shale, and conglomerate. Weathering breaks down existing rocks into smaller particles that are then compacted and cemented together to form sedimentary rocks.
The building up of Earth, known as rock deposition, contributes to sedimentary rock formation as sediments are compacted and cemented over time. The wearing down of Earth, through processes like erosion and weathering, breaks down rocks into smaller pieces that can contribute to the formation of sedimentary rocks. Igneous rocks may also be weathered down into sediments, which can undergo lithification to become sedimentary rocks.
Magnetic force does not break down rocks in nature. Rocks are typically broken down by mechanical weathering (e.g. frost wedging, root growth) and chemical weathering (e.g. oxidation, dissolution).
When rainwater soaks into the ground and moves down to rocks, it can contribute to the weathering process where the rocks break down over time. This can lead to the formation of soil and nutrients being released into the ecosystem. Additionally, the water may interact with the minerals in the rocks, potentially changing the chemistry of both the water and the rocks.
Clastic sedimentary rocks.
Clastic sedimentary rocks.
Sediments are produced
Clastic sedimentary rocks.
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The two kinds of weathering are mechanical weathering, which breaks down rocks into smaller pieces without changing their chemical composition, and chemical weathering, which alters the chemical composition of rocks through processes like oxidation or dissolution.
Sediments are produced
Sedimentary rocks are primarily formed through the process of weathering, erosion, and deposition of sediments. These rocks include sandstone, limestone, shale, and conglomerate. Weathering breaks down existing rocks into smaller particles that are then compacted and cemented together to form sedimentary rocks.
Rocks are naturally broken down into smaller pieces through a process called weathering. This includes physical weathering, where rocks are broken apart by factors like ice, wind, and water, as well as chemical weathering, where rocks are broken down by reactions with substances in the environment. Over time, these processes cause rocks to fracture and crumble into smaller particles.
The building up of Earth, known as rock deposition, contributes to sedimentary rock formation as sediments are compacted and cemented over time. The wearing down of Earth, through processes like erosion and weathering, breaks down rocks into smaller pieces that can contribute to the formation of sedimentary rocks. Igneous rocks may also be weathered down into sediments, which can undergo lithification to become sedimentary rocks.
Rocks that are commonly formed through weathering include sedimentary rocks such as sandstone, limestone, and shale. Weathering breaks down existing rocks into smaller fragments that can then be transported and deposited to create sedimentary rocks. These rocks often exhibit features like layers or cemented grains due to the deposition process.
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