It's a quarts.
This isn't much info but maybe this will help
A six-sided mineral crystal that is very hard is typically referred to as a hexagonal crystal. One common example of a hard mineral with this crystal structure is quartz, which has a hardness of 7 on the Mohs scale. Another example is beryl, which includes varieties like emerald and aquamarine. These minerals are characterized by their distinct six-sided (hexagonal) symmetry and exceptional durability.
garnets
..bonds made by the chemicals it is composed of. For example, diamonds are so hard and have a very cool natural shape because the chemical that makes up diamonds (Carbon) has formed into a particular pattern. All chemicals, because of their polarity caused by the number of electrons they have, form a different shape when they bond with each other.
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.
A mineral's shape is determined by its internal atomic arrangement and the conditions under which it formed. The atomic structure of a mineral dictates how its crystals will grow, resulting in various shapes such as cubes, prisms, or pyramids. Factors like temperature, pressure, and the presence of impurities can also influence a mineral's final shape.
A six-sided mineral crystal that is very hard is typically referred to as a hexagonal crystal. One common example of a hard mineral with this crystal structure is quartz, which has a hardness of 7 on the Mohs scale. Another example is beryl, which includes varieties like emerald and aquamarine. These minerals are characterized by their distinct six-sided (hexagonal) symmetry and exceptional durability.
A six-sided mineral crystal may be a naturally occurring form of quartz, which is a very hard mineral. Quartz is widely known for its six-sided crystal structure and its hardness, which ranks 7 on the Mohs scale of hardness. It is commonly used in jewelry and as a component in various industrial applications.
Diamond is a very hard white mineral.
Very soft mineral
No, the crystals of a mineral can vary in size depending on factors such as growth conditions and the speed at which the mineral forms. Crystals can range from microscopic to very large sizes, even within the same mineral species.
Granite is very resistant to fracture because of its interlocking mineral crystal structure.
Large crystal formation in mineral specimens typically occurs when the mineral is allowed to grow slowly under ideal conditions, such as low temperature, high pressure, and limited space for crystal growth. These conditions promote the orderly arrangement of atoms within the mineral structure, leading to the development of large crystals. Factors like the presence of impurities, the mineral's chemical composition, and the length of time the mineral has had to grow can also influence crystal size.
garnets
Yes. Quartz can have very well-formed crystals but lacks cleavage.
The color, luster, and crystal shape of a mineral may be observed just by looking at the mineral. Some minerals have very distinctive colors that help identify them. Although the color of a mineral can give away its identity, color is the least useful property for mineral identification.
You unlock "hard" after you finish "normal" and you unlock "very hard" after you finish "hard"
Corundum is a very hard mineral used as an abrasive in industry.