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∙ 11y agoRocks are broken down by physical or chemical weathering.
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∙ 16y agoWiki User
∙ 7y agoIf a rock contains iron, air and water can react with iron through
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The leftover material from rocks that have been broken down is called sediment. Sediment can include smaller rock fragments, minerals, and organic particles that have weathered and eroded from the original rock. Over time, sediment can accumulate and form sedimentary rocks through processes like compaction and cementation.
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.
All rocks can be broken down into smaller particles known as minerals. These minerals are the basic building blocks of rocks and can be classified based on their chemical composition and crystal structure.
This process is an example of mechanical weathering, where rocks are physically broken down into smaller pieces by forces like water movement and abrasion.
Yes, big rocks can be broken into smaller rocks through natural processes like weathering and erosion, where factors like wind, water, and temperature changes cause the rock to break down into smaller pieces over time. Additionally, human activities such as mining and quarrying also break big rocks into smaller rocks for various purposes.
weathering
Weathering.
Rocks can be broken down into small fragments through physical weathering processes such as frost wedging, thermal expansion, and abrasion. These processes exert stress on the rocks, causing them to break into smaller pieces. Chemical weathering can also contribute by breaking down the minerals in rocks through reactions with water, oxygen, and acids.
Mechanical weathering occurs when rocks are broken apart by physical processes such as frost wedging, root wedging, or abrasion. These processes break down rocks into smaller fragments without altering their chemical composition.
Yes, weathering is the process that breaks down rocks into smaller fragments, while erosion is the transportation of these fragments. Together, they work to disintegrate rocks.
The leftover material from rocks that have been broken down is called sediment. Sediment can include smaller rock fragments, minerals, and organic particles that have weathered and eroded from the original rock. Over time, sediment can accumulate and form sedimentary rocks through processes like compaction and cementation.
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.
Weathering is the alteration of rocks to more stable material from their exposure to the agents of air, water, and organic fluids. ... Mechanical weathering includes processes that fragment and disintegrate rocks into smaller pieces without changing the rock's mineral composition.
One example of weathering is when rocks are broken down into smaller pieces by the process of frost action. Water seeps into cracks in rocks, freezes, expands, and eventually breaks the rock apart into smaller fragments.
The term that describes the breakdown of rocks is "weathering." It refers to the process in which rocks are broken down into smaller pieces through a combination of physical, chemical, and biological processes.
Weathering is the process where rocks and minerals are broken down into smaller fragments by natural elements such as water, wind, and temperature changes. It can lead to the physical disintegration and chemical decomposition of rocks over time, ultimately shaping the Earth's surface.
The process of weathering breaks down big rocks into smaller rocks and then into sand particles. This can happen through physical weathering, where rocks are broken down by forces like wind, water, and temperature changes, or through chemical weathering, where rocks are chemically altered over time.