name 2 ways mnerals can be classified put into groups
Minerals are divided into groups based on their chemical composition and crystalline structure. The two main groups are silicate minerals, which are made of silicon and oxygen, and non-silicate minerals, which are composed of other elements. Within these groups, minerals are further classified based on their specific properties and characteristics.
In general, minerals can form in two ways: through the crystallization of melted materials, and through the crystallization of materials dissolved in water.
Minerals are classified by chemical formula, composition, physical properties, optical properties, and special properties. The Dana Classification System is a chemical classification for minerals, and the Strunz Classification System (chemical-structural) are two systems designed for mineral classification.
Clay and Quartz!
They are divided into puddingstone and somipone. Puddingstone is made of tiny minerals but somipone is made up of HUGE minerals.
The two main minerals in cheese are calcium and phosphorus.
The two ways are: Heterogeneous Homogeneous
A solid mixture of two or more minerals is typically called a rock. Rocks can be classified into three main categories: igneous, sedimentary, and metamorphic, based on their origin and formation process.
Two ways are by temperature and brightness
Minerals are divided into groups based on their chemical composition and crystalline structure. The two main groups are silicate minerals, which are made of silicon and oxygen, and non-silicate minerals, which are composed of other elements. Within these groups, minerals are further classified based on their specific properties and characteristics.
Two examples are quartz and mica. Minerals are also classified as metallic or non-metallic.
In general, minerals can form in two ways: through the crystallization of melted materials, and through the crystallization of materials dissolved in water.
Rocks are classified into two main groups based on how they are formed: igneous rocks, which are formed from cooling and solidifying magma or lava, and sedimentary rocks, which are formed from the accumulation and compression of sediments.
Minerals are classified by chemical formula, composition, physical properties, optical properties, and special properties. The Dana Classification System is a chemical classification for minerals, and the Strunz Classification System (chemical-structural) are two systems designed for mineral classification.
elevation and shape
Public and Private
The two main ways minerals are put together in rock are crystalline and clastic. The crystalline process gives rocks the characteristic and structure of crystals. Clastic rocks are composed of fragments, or clasts, of pre-existing minerals and rock.