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Name each member of the silicate family?
Quartz, feldspar, mica, and pyroxene are common members of the silicate mineral family.
How do you contrast the composition of minerals in each mineral group?
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.
What are sheet silicates?
A structural type of silicate mineral in which flat sheets are formed by the sharing of three of the four oxygen atoms in each tetrahedron with neighboring tetrahedrons. Also known as layer silicate; sheet mineral; sheet silicate.
Halides oxides sulfates sulfides carbonates and native elements are what kind of mineral?
Those are categories of minerals known as mineral classes. They group minerals based on their chemical compositions and structures. Each class has unique properties and characteristics that help differentiate one mineral from another.
Which of these is a mineral silicate?
Sheet silicates are known as phyllosilicates or layer silicates. They consist of silicon and oxygen atoms - 2 silicon atoms for each 5 oxygen atoms. Kaolinite and serpentine are examples of sheet silicates. Kaolinite also contains hydrogen and aluminum atoms while serpentine contains hydrogen and magnesium atoms.
Name each member of the silicate family?
Quartz, feldspar, mica, and pyroxene are common members of the silicate mineral family.
Does the ratio of silicon to oxygen remain constant for each silicate mineral?
No, the ratio of silicon to oxygen can vary among different silicate minerals. The overall structure and composition of the mineral will determine the specific ratio of silicon to oxygen present in that mineral.
How do you contrast the composition of minerals in each mineral group?
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.
What are sheet silicates?
A structural type of silicate mineral in which flat sheets are formed by the sharing of three of the four oxygen atoms in each tetrahedron with neighboring tetrahedrons. Also known as layer silicate; sheet mineral; sheet silicate.
Halides oxides sulfates sulfides carbonates and native elements are what kind of mineral?
Those are categories of minerals known as mineral classes. They group minerals based on their chemical compositions and structures. Each class has unique properties and characteristics that help differentiate one mineral from another.
Which of these is a mineral silicate?
Sheet silicates are known as phyllosilicates or layer silicates. They consist of silicon and oxygen atoms - 2 silicon atoms for each 5 oxygen atoms. Kaolinite and serpentine are examples of sheet silicates. Kaolinite also contains hydrogen and aluminum atoms while serpentine contains hydrogen and magnesium atoms.
What mineral is not a silicate mineral?
A silicate mineral comes from silicates, the most dominant mineral class which accounts for over 90 percent of Earth's crust. Silicates form through the combination of oxygen and silicon, and more than 800 species of silicate minerals have been identified. Silicates include feldspars, quartz, olivine, and more. Yet, to identify a mineral that is not a silicate mineral we must identify the nonsilicate class, which encompass the other mineral classes that are far less abundant than the silicates. They are very important economically and they can be further categorized into carbonates, halides, oxides, sulfides, sulfates, and native elements. Minerals of each of these sub-classes represent minerals that are not a silicate mineral; thus, there are numerous answers to this question. Calcite is not a silicate mineral because it is a carbonate, halite is not because it is a halide, galena is not because it is a sulfide, gypsum is not because it is a sulfate, and gold is not because it is a native element.
What mineral group if any contain silicon carbonates halides or sulfides?
Silicates are the mineral group that contain silicon, carbonates are the mineral group that contain carbon, halides are the mineral group that contain halogen elements, and sulfides are the mineral group that contain sulfur. Each of these mineral groups encompasses a variety of minerals with different chemical compositions.
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 the relationship between a silicate and a tetrahedron?
A silicate is a mineral composed of silicon and oxygen atoms arranged in a tetrahedral structure, where each silicon atom is bound to four oxygen atoms in a tetrahedral shape. This tetrahedral structure is the building block of silicate minerals, which make up the majority of Earth's crust.
What a mineral is and give examples of each type of mineral.?
A mineral is a naturally occurring, inorganic solid with a definite chemical composition and a crystalline structure. Minerals are classified into three main types: silicate minerals (like quartz and feldspar), which contain silicon and oxygen; non-silicate minerals (such as calcite and gypsum), which do not have that structure; and ore minerals (like hematite and bauxite), which are economically valuable for extracting metals. Each type of mineral plays a significant role in geology, industry, and various natural processes.
How do silica tetrahedra bond in silicate minerals?
Silica tetrahedra in silicate minerals are linked together by sharing oxygen ions at the corners of the tetrahedra. This creates a strong network structure known as a silicate framework that gives the mineral its physical and chemical properties. The arrangement and bonding of these tetrahedra determine the crystal structure and properties of the silicate mineral.
