yes
Quartz is a mineral that commonly forms six-sided crystals due to its hexagonal crystal structure. The most well-known form of quartz with this characteristic is the clear variety known as rock crystal.
Beneficial to euhedral crystal shapes would be the proper temperature and length of time spent in ideal conditions for crystal formation for the particular mineral. Ideal conditions would include: space available for mineral crystal growth and availability or supply of mineral rich solutions bearing mineral components.
The mineral that commonly forms 12-sided crystals is called dodecahedrite, which is a form of garnet. However, one of the most well-known minerals with a dodecahedral crystal habit is quartz, specifically in its dodecahedral variety known as dodecahedral quartz. These 12-sided crystals are characterized by their geometric symmetry and distinct faces.
Dunite has a coarse-grained texture with visible mineral grains that are usually large and well-defined. It is composed mainly of the mineral olivine, giving it a greenish color and a granular appearance.
Intrusive rock crystal size refers to the dimensions of crystals that form within igneous rocks as they cool slowly beneath the Earth's surface. These crystals tend to be larger than those found in extrusive rocks, which cool quickly on the surface. The size can vary significantly depending on factors such as the cooling rate, mineral composition, and the environment of crystallization. Typically, intrusive rocks like granite exhibit larger, well-formed crystals compared to their extrusive counterparts.
Large crystals with well-formed crystal faces tend to form when the mineral is given enough time to grow undisturbed in a stable environment with plenty of space and nutrients. The slower the cooling or solidification process, the larger and more well-formed the crystals can grow.
Mineral crystal formation is a naturally occurring process of inorganic material. Crystal formation can occur in organic material as well, but would not be considered mineralogical crystal formation.
Symmetrical crystal shapes indicate that the mineral has a well-defined crystal structure with uniform internal arrangement of atoms or molecules. This suggests that the mineral formed under conditions that allowed for ordered growth, resulting in distinct geometric shapes.
True. A mineral can exhibit a distinct crystal form while lacking cleavage, which is the tendency to break along specific planes of weakness. For example, quartz has a well-defined crystal structure but does not exhibit cleavage; instead, it fractures conchoidally. This distinction highlights the complexities of mineral characteristics beyond just crystal form and cleavage.
Yes. Quartz can have very well-formed crystals but lacks cleavage.
Quartz is a mineral that commonly forms six-sided crystals due to its hexagonal crystal structure. The most well-known form of quartz with this characteristic is the clear variety known as rock crystal.
A crystal shape refers to the geometric form or structure that a mineral naturally takes on when it solidifies. This can include shapes like cubes, hexagons, prisms, or even more complex forms depending on the mineral's atomic structure and growth conditions.
Beneficial to euhedral crystal shapes would be the proper temperature and length of time spent in ideal conditions for crystal formation for the particular mineral. Ideal conditions would include: space available for mineral crystal growth and availability or supply of mineral rich solutions bearing mineral components.
Well, I think a mineral that is crystalline reflects the light only by total internal reflection in air medium. Hence, even if it is a black mineral, it can still appear shiny. So, the mineral should still appear lustrous but may appear that it is being seen in a low light..
Mineral crystals can exhibit a variety of shapes depending on their atomic structure and growth conditions. While some minerals do form common shapes like cubes, octahedrons, and hexagonal prisms, many others can have irregular or unique shapes due to factors such as impurities, growth environment, and crystallographic features.
The crystalline structure of a mineral significantly influences its cleavage, which is the tendency of a mineral to break along specific planes of weakness. Minerals with well-defined atomic arrangements, such as those with layered or planar structures, tend to exhibit clear and predictable cleavage patterns. Conversely, minerals with more complex or irregular structures may have less distinct cleavage or none at all. Thus, the symmetry and bonding within the crystal lattice dictate the direction and quality of cleavage.
The mineral that commonly forms 12-sided crystals is called dodecahedrite, which is a form of garnet. However, one of the most well-known minerals with a dodecahedral crystal habit is quartz, specifically in its dodecahedral variety known as dodecahedral quartz. These 12-sided crystals are characterized by their geometric symmetry and distinct faces.