A mineral is a naturally occurring substance that is solid and stable at room temperature, representable by a chemical formula, usually abiogenic, and has an ordered atomic structure. It is different from a rock, which can be an aggregate of minerals or non-minerals, and does not have a specific chemical composition. The exact definition of a mineral is under debate, especially with respect to the requirement a valid species be abiogenic, and to a lesser extent with regards to it having an ordered atomic structure. The study of minerals is called mineralogy.
There are over 4,900 known mineral species; over 4,660 of these have been approved by the International Mineralogical Association (IMA). The silicate minerals compose over 90% of the Earth's crust. The diversity and abundance of mineral species is controlled by the Earth's chemistry. Silicon and oxygen constitute approximately 75% of the Earth's crust, which translates directly into the predominance of silicate minerals. Minerals are distinguished by various chemical and physical properties. Differences in chemical composition and crystal structure distinguish various species, and these properties in turn are influenced by the mineral's geological environment of formation. Changes in the temperature, pressure, and bulk composition of a rock mass cause changes in its mineralogy; however, a rock can maintain its bulk composition, but as long as temperature and pressure change, its mineralogy can change as well.
Minerals can be described by a variable physical properties, which relate to its chemical structure and composition. Common distinguishing characteristics include crystal structure and habit, hardness, lustre, diaphaneity, colour, streak, tenacity, cleavage, fracture, parting, and specific gravity. More specific tests for minerals include reaction to acid, magnetism, taste or smell, and radioactivity.
Minerals are classified by key chemical constituents; the two dominant systems are the Dana classification and the Strunz classification. The silicate class of minerals is subdivided into six subclasses by the degree of polymerization in the chemical structure. All silicate minerals have a base unit of a [SiO4]4- silica tetrahedra-that is, a silicon cation coordinated by four oxygen anions, which gives the shape of a tetrahedron. These tetrahedra can be polymerized to give the subclasses: orthosilicates (no polymerization, thus single tetrahedra), disilicates (two tetrahedra bonded together), cyclosilicates (rings of tetrahedra), inosilicates (chains of tetrahedra), phyllosilicates (sheets of tetrahedra), and tectosilicates (three-dimensional network of tetrahedra). Other important mineral groups include the native elements, sulfides, oxides, halides, carbonates, sulfates, and phosphates. hope this helps!
The least effective property used to identify most minerals would be the color. The color of a mineral can be altered by impurities.
The property of cleavage.
Hardness measures a mineral's resistance to being scratched.
the color is the least reliable source!
It is the streak property. The streak is the color of a mineral in powdered form.
The property that describes a mineral's surface shines is called luster.
If the mineral rights have been severed from the property and the owner of the mineral rights does not own the property then there is no need to notify the property owner. It's possible to own the mineral rights and not own the property. That would be called the "mineral estate". The owner of the property if different than the mineral owner would be the owner of the "property estate". Being the "mineral estate" owner gives you the same rights as being a "property owner". You can do as you wish with your mineral interests. Only time there is a need to notify the property owner is if any leasing will be going on. Hope this helps.
The characteristic property of the mineral pyrite is sand it is very shiny
Fluorescence is a property not a mineral.
Hardness
You are testing the relative hardness of the mineral.
When a mineral spontaneously decays into subatomic particles, it has this property
Diamond is the hardest known mineral, which is a physical property of the mineral.
feldspar
No. Streak color is distinct of mineral hardness. They are separate properties.
No. Streak color is distinct of mineral hardness. They are separate properties.
The property that describes a mineral's surface shines is called luster.