silicates- silicon and oxygen
carbonates- carbon, oxygen, and 1 or more other elements
oxides- oxygen and 1 or more other elements( usually metal)
sufates/sulfides- contain sulfur
halides- halogen ion and 1 or more other elements
native elements- group of minerals that exists in relatively pure form( ex: gold, silver, copper, sulfer, carbon...)
Mineral groups differ in composition based on the elements they contain and their crystalline structures. For example, silicate minerals contain silicon and oxygen, while sulfide minerals contain sulfur and metal ions. The ratio of elements and the way they are arranged in the crystal lattice determine the unique properties of each mineral group.
Nonsilicate minerals are mineral compounds that do not contain silicon and oxygen elements as their primary building blocks. These minerals typically have a different chemical composition than silicate minerals and include groups such as carbonates, sulfates, halides, and oxides. Examples of nonsilicate minerals include calcite, gypsum, halite, and hematite.
Mineral groups are defined by their chemical composition and crystal structure. They are organized based on the elements or compounds that make up the mineral, as well as the way their atoms are arranged in a repeating pattern to form crystals. This classification system helps to identify and categorize the wide variety of minerals found in nature.
The property used to classify minerals into groups like silicates is their chemical composition. Silicates are minerals composed of silicon and oxygen, and they make up the largest group of minerals found in the Earth's crust. Minerals are categorized by their chemical composition, crystal structure, and physical properties.
The main classification criterion is the chemical composition. Minerals are classified as oxides, sulfides, halides, sulfates, silicates, or carbonates. Some elements are also classified as minerals. There's also a metallic and non-metallic mineral classification.
Mineral groups differ in composition based on the elements they contain and their crystalline structures. For example, silicate minerals contain silicon and oxygen, while sulfide minerals contain sulfur and metal ions. The ratio of elements and the way they are arranged in the crystal lattice determine the unique properties of each mineral group.
Minerals are classified according to their composition
Minerals are grouped by their chemical composition. There are more than 3 groups of minerals including. Silicates, oxides, sulfates, sulfides, carbonates, native elements, and halides are all major mineral groups. Silicates are definitely at the top of the list.
The major mineral groups are silicates, carbonates, sulfates, halides, oxides, sulfides, native elements, and phosphates. These groups are classified based on the chemical composition and structure of the minerals.
A mineral structural group refers to minerals that have similar crystal structures due to their chemical composition and arrangement of atoms. These groups help classify and categorize minerals based on their internal structure and bonding characteristics. Examples of mineral structural groups include silicates, carbonates, sulfides, and oxides.
Minerals are classified based on their chemical composition and crystal structure. Chemical composition refers to the elements that make up the mineral, while crystal structure refers to the arrangement of atoms in the mineral's crystal lattice.
Nonsilicate minerals are mineral compounds that do not contain silicon and oxygen elements as their primary building blocks. These minerals typically have a different chemical composition than silicate minerals and include groups such as carbonates, sulfates, halides, and oxides. Examples of nonsilicate minerals include calcite, gypsum, halite, and hematite.
There are roughly 3,000 different types of minerals, which can be categorized into around eight main mineral groups. Some of these groups include silicates, carbonates, sulfides, and oxides. Each group has its own distinct chemical composition and physical properties.
Mineral groups are defined by their chemical composition and crystal structure. They are organized based on the elements or compounds that make up the mineral, as well as the way their atoms are arranged in a repeating pattern to form crystals. This classification system helps to identify and categorize the wide variety of minerals found in nature.
mineral is a naturally occurring solid chemical substance formed through biogeochemical processes, having characteristic chemical composition, highly ordered atomic structure, and specific physical properties. By comparison, a rock is an aggregate of minerals and/or mineraloids and does not have a specific chemical composition. Minerals range in composition from pure elements and simple salts to very complex silicates with thousands of known forms.[1] The study of minerals is called mineralogy.Contents[hide] 1 Mineral definition and classification2 Crystal structure 2.1 Mineral groups and solid solution3 Differences between minerals and rocks 3.1 Mineral composition of rocks4 Physical properties of minerals5 Chemical properties of minerals 5.1 Silicate class5.2 Carbonate class5.3 Sulfate class5.4 Halide class5.5 Oxide class5.6 Sulfide class5.7 Phosphate class5.8 Element class5.9 Organic class6 See also7 References8 External links
Silicates Minerals. Eg. Quartz (SiO2).
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.