none is really sure
the composition of luster is limstone
Before metamorphism, serpentinite is a type of ultramafic rock primarily composed of the mineral olivine, which undergoes alteration due to hydrothermal processes. It typically forms from the alteration of peridotite, a rock rich in magnesium and iron. This alteration leads to the formation of serpentinite, characterized by its greenish color and smooth, waxy texture, resulting from the hydration of olivine into serpentine minerals. The process often occurs in environments such as mid-ocean ridges or subduction zones.
Oxygen.
The Earth's upper mantle has a composition similar to the green mineral olivine. Olivine is a common mineral found in the upper mantle, making up a significant portion of its composition.
Igneous rocks are classified based on mineral composition and texture, metamorphic rocks are classified by texture and mineral composition, and sedimentary rocks are primarily classified by their grain size and composition. These classifications help scientists understand the origin and characteristics of each type of rock.
Serpentinite can contain the mineral Chrysotile, also known as white asbestos. Asbestos is carcinogenic (cancer causing) and can also if inhaled cause serious lung problems and is best avoided!
Each known mineral has a specific chemical composition.
The color of a mineral sample is determined by its chemical composition
the composition of luster is limstone
The chemical composition of a mineral is important because it helps identify the mineral and provides information on its physical and chemical properties. Understanding the composition can help determine how the mineral formed, where it is found, and how it can be used in various applications.
Before metamorphism, serpentinite is a type of ultramafic rock primarily composed of the mineral olivine, which undergoes alteration due to hydrothermal processes. It typically forms from the alteration of peridotite, a rock rich in magnesium and iron. This alteration leads to the formation of serpentinite, characterized by its greenish color and smooth, waxy texture, resulting from the hydration of olivine into serpentine minerals. The process often occurs in environments such as mid-ocean ridges or subduction zones.
The Precambrian is a geological age, not a mineral.
Talc is a mineral and is not classified as metamorphic, sedimentary, or igneous as are rocks.
It is a mineral or a number of minerals which are part of the composition of rock.
elemen
Magma is not a mineral becauseIt is liquid.It does not have a definite chemical composition.
Calcium