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What type of rocks are in bedding planes?

Sedimentary rocks are common in bedding planes due to their layering structure created by the accumulation of sediments. These rocks are often easily eroded, which can result in the formation of bedding planes. Stratification and sedimentary structures are typical in rocks found in bedding planes.


Why FCC crystal structure has more slip plans thenHCP?

FCC crystal structure has 12 slip planes because of its cubic symmetry, which allows slip to occur in many directions. HCP crystal structure, on the other hand, has 3 slip planes due to its hexagonal close-packed arrangement, which restricts the slip to fewer directions.


What is the breakage of a mineral not along planes of weakness in the crystal structure called?

The breakage of a mineral not along planes of weakness in the crystal structure is called conchoidal fracture. This type of fracture results in smooth, curved surfaces resembling the inside of a seashell. It is common in minerals with strong atomic bonding like quartz.


Why cleavage of the crystals is itself anisotropic behavior?

Cleavage of crystals is anisotropic because the structure of crystals consists of planes of atoms where the bonds are weaker or stronger in different directions. When a crystal cleaves, it breaks along planes of weaker bonds, resulting in different cleavage planes having different strengths. This anisotropy arises from the crystalline structure and the arrangement of atoms in the crystal lattice.


What is the clevage of uranium?

The cleavage of uranium refers to its tendency to break along specific planes within its crystal structure. Uranium typically exhibits imperfect cleavage, meaning that while it has some planes along which it can break more easily, these planes are not well-defined or prominent. Instead, uranium tends to fracture in an irregular manner. This characteristic can vary depending on the specific uranium mineral being examined, such as uraninite or other uranium-bearing ores.