The internal arrangement of atoms.
of crystals.
No, each type of mineral can have its own unique crystal structure determined by its chemical composition and the conditions under which it formed. Different minerals can exhibit a wide variety of crystal structures, leading to the diversity seen in the mineral world.
The visible shape of a mineral's atomic pattern is called its crystal form. This refers to the geometric arrangement of atoms in a mineral, which can vary depending on the type of mineral and its crystal structure.
Cleavage is the mineral property that depends on bond type and the spacing of atoms within the crystal. Cleavage is the tendency of a mineral to break along specific planes of weakness due to the arrangement of atoms and the type of chemical bonds holding them together.
The rate of cooling of the magma determines the type of mineral formed by the magma or lava..
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.
During mineral growth, atoms accumulate on existing surfaces or boundaries within the mineral structure. This process contributes to the enlargement of mineral crystals and the formation of new mineral layers.
No. A crystal is the solid form of a mineral. Mineral crystals are present in nearly every rock, regardless of type.
No, stalactites are not a type of crystal. They are formations that hang from the ceiling of caves, formed by mineral deposits dripping down over time. Crystals, on the other hand, have a more defined geometric structure and can form in a variety of environments.
A crystal is a solid substance in which the atoms are arranged in a repeating pattern, giving it a distinct shape and structure. Crystals are a type of mineral, which is a naturally occurring inorganic solid with a specific chemical composition and structure. Rocks, on the other hand, are made up of minerals or mineraloids.
No one knows my namestake like I do (except Crystallography majors) and in reality obsidian is not quite classified as a type of crystal at all, as its composition is too complex to comprise a single mineral, it's usually just considered a mineraloid.
The type of visible light reflected off a mineral depends on its specific crystal structure and chemical composition. Different minerals will reflect different colors of light, giving them their unique appearance and color. This phenomenon is known as mineral coloration.