no not at all
retain its chemical composition and crystal structure, but in smaller fragments. The properties of the mineral would remain the same because the chemical composition and crystal lattice are unchanged by the physical breakup.
Cleavage is a physical characteristic determined by the arrangement of atoms within a mineral. Cleavage describes how a mineral breaks along planes of weakness due to its atomic structure, creating smooth, flat surfaces. The number and orientation of these planes are unique to each mineral.
The shape of a mineral depends on the chemical structure that the bonds form between atoms in the mineral. A cubic mineral (such as pyrite) has a chemical structure that, as bonds are made, a cubic shape is formed.
Minerals are classified by their geometry into six different mineral crystal systems. Each crystal system has its own set of parameters based on relationships between length and angles between a crystals axes.
Tungsten has a body-centered cubic (BCC) crystal structure at room temperature and pressure. In this structure, each tungsten atom is located at the center of a cube, with eight neighboring atoms at the corners.
No. Each mineral has its own structure.
no
no not at all
retain its chemical composition and crystal structure, but in smaller fragments. The properties of the mineral would remain the same because the chemical composition and crystal lattice are unchanged by the physical breakup.
of crystals.
Cleavage is a physical characteristic determined by the arrangement of atoms within a mineral. Cleavage describes how a mineral breaks along planes of weakness due to its atomic structure, creating smooth, flat surfaces. The number and orientation of these planes are unique to each mineral.
Arrangement of atoms and ions within the mineral's crystal lattice structure, which is determined by the mineral's chemical composition and bonding properties. This unique arrangement leads to the formation of distinct crystal shapes that can vary depending on external factors like temperature and pressure during the mineral's formation.
Each mineral has its own unique crystal structure, which determines its physical properties such as hardness, cleavage, and color. Additionally, the chemical composition of each mineral varies, leading to differences in properties like density and reactivity. These characteristics are a result of the specific arrangement of atoms within the mineral's structure, giving each mineral its distinct set of properties.
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Each mineral is unique based on its chemical composition and crystal structure. These characteristics determine the mineral's physical properties such as color, hardness, cleavage, and luster. Additionally, each mineral forms under specific conditions, giving it distinct features that differentiate it from other minerals.
A crystal system is a method for categorizing minerals based on their crystal structure and symmetry. This classification is useful because it helps geologists and mineralogists identify and describe minerals more accurately. It also provides insight into the physical properties and formation conditions of minerals within each crystal system.
The shape of a mineral depends on the chemical structure that the bonds form between atoms in the mineral. A cubic mineral (such as pyrite) has a chemical structure that, as bonds are made, a cubic shape is formed.