The specific gravity of garnet schist can vary depending on the composition and density of the minerals present. On average, the specific gravity of garnet schist is around 2.7 to 3.2. However, it is recommended to measure the specific gravity of a specific sample to get an accurate value.
Graphite is a nonsilicate mineral composed primarily of carbon. It does not contain silicate minerals in its chemical composition.
Graphite is a non-foliated metamorphic mineral. It forms from the metamorphism of organic material like coal under high temperature and pressure conditions, but it lacks the layering common in foliated rocks like slate or schist.
Graphite is primarily found in metamorphic rocks such as schist and gneiss. It can also be found in some igneous rocks like granite and pegmatite.
Schist typically begins as a metamorphic rock called shale, which is composed of clay and other fine-grained sedimentary minerals. Through the process of metamorphism, intense heat and pressure cause the minerals in the shale to recrystallize, forming the distinct foliated structure and mineral composition that characterize schist.
It is a medium-grade metamorphic rock with a preponderance of the platy mineral graphite.
it has a metallic luster usually silver and black :)
schist
The color of schist depends on its mineral composition. It can be gray, yellow, light or dark green, brown, or even black.
Graphite and Diamonds are both allotropes of Carbon.
Mica schist typically does not react with hydrochloric acid because the minerals in mica schist, such as mica and quartz, are generally chemically inert or resistant to acid dissolution. However, acid reactions can vary depending on the specific mineral composition of the schist.
Both are foliated metamorphic rocks in which individual minerals can be seen with the naked eye. The difference is that gneiss is generally more coarsely crystalline and has color banding and schist smells bad.
Yes, graphite is commonly found in nature. It is a mineral form of carbon and can be found in rocks and ores, particularly in metamorphic rocks like marble and schist. Graphite is often mined and used for various applications, such as in pencils, lubricants, and batteries.
Yes, schist is typically porous due to its layered composition of minerals. The porosity of schist can vary depending on the specific mineral content and the degree of metamorphism it has undergone.
The specific gravity of garnet schist can vary depending on the composition and density of the minerals present. On average, the specific gravity of garnet schist is around 2.7 to 3.2. However, it is recommended to measure the specific gravity of a specific sample to get an accurate value.
Graphite is a nonsilicate mineral composed primarily of carbon. It does not contain silicate minerals in its chemical composition.
Graphite is a non-foliated metamorphic mineral. It forms from the metamorphism of organic material like coal under high temperature and pressure conditions, but it lacks the layering common in foliated rocks like slate or schist.