0
Silicate and nonsilicate minerals are primarily grouped based on their chemical composition. Silicate minerals contain silicon and oxygen in their crystal structure, often combined with other elements, and are the most abundant group in the Earth's crust. Nonsilicate minerals, on the other hand, do not contain silicon-oxygen tetrahedra and include a variety of mineral types such as carbonates, oxides, sulfates, and halides. This classification helps in understanding their properties, occurrences, and uses in various applications.
What else can I help you with?
How do you make a concept map using the following terms of minerals calite silicate minerals gypsum carbonates nonsilicate minerals quartz and sulfates?
To create a concept map using the terms, start by organizing them into categories based on their characteristics. Place "silicate minerals" and "nonsilicate minerals" as the primary categories. Under "nonsilicate minerals," further divide into subcategories such as "carbonates" (which includes calcite) and "sulfates" (which includes gypsum). Finally, place quartz under "silicate minerals," illustrating the relationships and hierarchy among the terms visually.
How are minerals divided?
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.
What must be true of silicate minerals?
Silicate minerals must contain silicon and oxygen as their primary components, forming the silicate tetrahedron (SiO4) as the fundamental building block. They are the most abundant group of minerals in the Earth's crust and can be classified into different types based on their structures, such as isolated tetrahedra, chains, sheets, and frameworks. Additionally, silicate minerals often incorporate various metal ions, influencing their physical properties and chemical behavior.
What is field spar?
Assuming you meant 'Feldspar' - it's a group of rock-forming silicate based minerals.
Is platinum a silicate or a non silicate?
Platinum is a non-silicate mineral. It is classified as a native element, meaning it is composed of only one type of atom and does not contain silicate structures. Unlike silicate minerals, which are based on silicon-oxygen tetrahedra, platinum occurs in its pure metallic form and does not form silicate compounds.
How do you make a concept map using the following terms of minerals calite silicate minerals gypsum carbonates nonsilicate minerals quartz and sulfates?
To create a concept map using the terms, start by organizing them into categories based on their characteristics. Place "silicate minerals" and "nonsilicate minerals" as the primary categories. Under "nonsilicate minerals," further divide into subcategories such as "carbonates" (which includes calcite) and "sulfates" (which includes gypsum). Finally, place quartz under "silicate minerals," illustrating the relationships and hierarchy among the terms visually.
What is the grouping of silicate and non-silicate minerals based on?
The grouping of silicate and non-silicate minerals is based on whether they contain silicon and oxygen. Silicate minerals are divided into smaller groups based on their structure. Non-silicate minerals are didvided into smaller groups based on their composition.
How are silicate minerals different from non silicate minerals?
Silicates are found in just about every variety of rock, including sedimentary, igneous and metamorphic. The thing that differentiates silicates from other minerals is the presence of the element silicon in the matrix. It is silicon that silicate minerals are named for. Use link below to check out this huge family of minerals.
Describe the two major groups of minerals?
Minerals can be classified into 13 groups according to their constituents. The major groups are: (1) native elements; (2) sulfides; (3) sulfosalts; (4) oxides and hydroxides; (5) halides and borates; (6) carbonates; (7) nitrates and iodates; (8) phosphates, vanadates, and arsenates; (9) sulfates; (10) tungstates and molybdates; and (11) silicates.
Why do minerals that have the nonsilicate crystalline structure called closest packing have high density?
Minerals of a nonsilicate crystal have very high densities because their crystal structures are based on the packing of atoms that are as close together as possible. This structure is called this closest packing.
How are minerals divided?
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.
What are the 6 main crystalline structures of silicate minerals?
The six main crystalline structures of silicate minerals are isolated tetrahedra, single chain, double chain, sheet, framework, and ring structures. Each structure is based on how the silicate tetrahedra are arranged and linked together in the mineral's crystal lattice.
What is different silicate minerals produceed from solidifying magma is directly related to?
The temperature, pressure, and chemical composition of the magma are the main factors that determine the specific silicate minerals that form during solidification. Silicate minerals can vary in their chemical composition and crystal structure based on these conditions, leading to the formation of different minerals such as quartz, feldspar, mica, and pyroxene.
What must be true of silicate minerals?
Silicate minerals must contain silicon and oxygen as their primary components, forming the silicate tetrahedron (SiO4) as the fundamental building block. They are the most abundant group of minerals in the Earth's crust and can be classified into different types based on their structures, such as isolated tetrahedra, chains, sheets, and frameworks. Additionally, silicate minerals often incorporate various metal ions, influencing their physical properties and chemical behavior.
Each silicate mineral group has its own particular silicate?
Yes, each silicate mineral group is defined by its unique silicate structure. For example, the structure of feldspar group minerals is based on interconnected silica tetrahedra, while the structure of pyroxene group minerals is made up of single chains of silica tetrahedra.
What is field spar?
Assuming you meant 'Feldspar' - it's a group of rock-forming silicate based minerals.
What 2 groups are minerals divided into based on their chemical compositon?
There are more than 2 groups of minerals. The following groupings exist based on their chemical composition:SilicatesOxidesSulfatesSulfidesCarbonatesNative elementsHalides
