Graphite has a layered structure in which carbon atoms are arranged in a hexagonal lattice. These layers are held together by weak van der Waals forces, allowing the layers to slide over each other easily. This property gives graphite its characteristic slippery feel and makes it a good lubricant.
Graphite has several important applications:
Graphite is formed under high-pressure and high-temperature conditions. It is often found in metamorphic rocks such as marble, schist, and gneiss. Graphite is also commonly found in igneous rocks and as a result of organic material metamorphism.
When studying graphite, it is important to understand its structure and how it relates to its physical properties. Be sure to review its uses in various industries and its occurrence in nature. Additionally, consider the significance of graphite in the context of carbon allotropes and its unique electrical and thermal properties.
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