The minerals that are in a rock will influence how quick it weathers. Strong materials will not weather as quickly as loose materials.
the composition of luster is limstone
none is really sure
Oxygen.
The breakdown of rocks and minerals into smaller particles without a change in composition is called mechanical weathering. This process involves physical forces like temperature changes, freeze-thaw cycles, and abrasion, which fragment the material. Unlike chemical weathering, mechanical weathering does not alter the mineral composition of the rocks. Examples include frost wedging and the action of roots growing in cracks.
The Earth's upper mantle has a composition similar to the green mineral olivine. Olivine is a common mineral found in the upper mantle, making up a significant portion of its composition.
Chemical weathering is the type of weathering that causes the mineral composition of rocks to change. This process occurs when minerals in rocks react with elements in the environment, causing a chemical reaction that alters the rock's mineral composition over time.
During mechanical weathering, the physical breakdown of rocks occurs without changing their mineral composition. The rock may break into smaller pieces, but the minerals that make up the rock remain the same.
Each known mineral has a specific chemical composition.
The mineral composition of a rock remains unchanged by mechanical weathering, which only affects the physical structure of the rock by breaking it into smaller pieces or changing its shape.
Mechanical.
The color of a mineral sample is determined by its chemical composition
the composition of luster is limstone
The chemical composition of a mineral is important because it helps identify the mineral and provides information on its physical and chemical properties. Understanding the composition can help determine how the mineral formed, where it is found, and how it can be used in various applications.
The Precambrian is a geological age, not a mineral.
It is a mineral or a number of minerals which are part of the composition of rock.
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Factors that affect the rate of mechanical weathering include temperature fluctuations, presence of water, wind intensity, type of rock or mineral composition, and presence of vegetation or organisms that can contribute to physical breakdown of rocks.