The crystalline structure of a mineral is determined by the way in which its atoms, ions, or molecules are bonded together. There are seven main crystal systems, each characterized by a unique arrangement of atoms, ions, or molecules. The seven crystal systems are:
* Cubic
* Tetragonal
* Orthorhombic
* Monoclinic
* Triclinic
* Hexagonal
* Trigonal
Each of these crystal systems has its own unique properties and characteristics. For example, cubic crystals are characterized by their eight identical sides and angles, while tetragonal crystals have three equal sides and one longer side.
The crystalline structure of a mineral is important because it helps to determine its physical properties, such as hardness, density, and cleavage. It also plays a role in the mineral's chemical reactivity.