salt
Yes, a crystal structure is an essential characteristic of any mineral. Minerals are defined as naturally occurring inorganic solids with a specific chemical composition and a crystalline structure, which gives them unique physical properties. The arrangement of atoms in a crystal lattice influences the mineral's hardness, cleavage, and other characteristics. Without a defined crystal structure, a substance would not be classified as a mineral.
That type of substance is called a crystal.
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.
Fluorite belongs to the same crystal system as salt - the cubic (also known as the isometric) crystal system.
A substance made entirely of one type of molecule and crystal structure. Sugar, common salt, and sulphur would all be good examples.
No. It is a carbohydrate. Salt would be an example of a mineral.
I believe the answer would be the crystal system, but the crystal system is based on the angles and length of the axis of the crystal. The axis length and the angle at which they meet would affact the number and angle of the crystal faces.
A mineral is a naturally occurring inorganic substance with a specific chemical composition and orderly internal structure. Minerals are the building blocks of rocks and are defined by their unique physical and chemical properties.
The opposite of a mineral would be a non-mineral or a substance that is not classified as a mineral, such as organic matter or man-made materials.
mineral is any chemical substance occuring naturally in earth crust
There are many types of sugar but, if you are describing one type of sugar and not a mixture of many sugars it would be a pure substance.
If you could examine a mineral with a powerful microscope that reveals atoms and ions, you would see the arrangement of individual atoms within the crystal lattice structure of the mineral. This would give you insight into the bonding between atoms, the types of elements present, and the overall crystal morphology of the mineral at a microscopic level.