The internal atomic structure of a mineral most likely determines the mineral's hardness, cleavage and crystal shape.
i think crystal habit is the minerals structure, while cleavage is the patter it breaks into.
Cleavage is the way a mineral breaks along planes of weakness in its atomic structure. The number and orientation of cleavage planes are determined by the arrangement of atoms in the mineral's crystal lattice. Minerals with strong atomic bonds tend to have poor or no cleavage, while those with weaker bonds exhibit good cleavage.
The properties of a mineral are primarily the result of its chemical composition and atomic structure. These factors determine characteristics such as color, hardness, cleavage, and crystal form in a mineral.
The chemical properties of a mineral are determined by its chemical composition, specifically the types of elements it contains and how they are bonded together. The physical properties of a mineral are determined by its internal atomic structure, including how atoms are arranged, how they bond, and how they interact with light and other forces.
Luster is a property of minerals that describes their appearance. A crystal is the structure that minerals possess due to the arrangement of their atomic particles.
The internal atomic structure.
The internal atomic structure.
... internal atomic arrangement. The crystal shape forms based on how the mineral's atoms are arranged in a repeating pattern. Cleavage is the tendency of a mineral to break along planes of weakness due to the atomic structure.
Cleavage is related to the minerals atomic structure because minerals are arranged in crystal lattices . It's the shape of these lattices that determine the mineral's cleavage.
Cleavage in minerals can be identified by observing how the mineral breaks along certain planes or directions, resulting in smooth, flat surfaces. This cleavage is a result of the internal atomic structure of the mineral. By examining the shape and pattern of the breakage, one can determine the cleavage of a mineral.
The internal structure of a mineral, including its atomic arrangement and crystal lattice, affects its physical properties like cleavage, color, luster, and transparency. For example, a mineral with a repeating atomic pattern may exhibit a geometric crystal shape, while another mineral with random arrangement may appear massive or granular. The internal structure also determines the mineral's hardness, density, and other characteristics that manifest in its physical appearance.
i think crystal habit is the minerals structure, while cleavage is the patter it breaks into.
Cleavage is the way a mineral breaks along planes of weakness in its atomic structure. The number and orientation of cleavage planes are determined by the arrangement of atoms in the mineral's crystal lattice. Minerals with strong atomic bonds tend to have poor or no cleavage, while those with weaker bonds exhibit good cleavage.
crystal shape
The properties of a mineral are primarily the result of its chemical composition and atomic structure. These factors determine characteristics such as color, hardness, cleavage, and crystal form in a mineral.
The crystal system a mineral belongs to relates most to the mineral's internal atomic structure and arrangement of atoms. This determines the shape and physical properties of the mineral, such as its cleavage, hardness, and color.
A mineral that breaks along a weakly bonded plane is called "cleavage". Cleavage is the tendency of a mineral to break along smooth, flat surfaces determined by its internal atomic structure.