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Natural bitumen, on the other hand, is formed as a result of crude oil migrating from oil reservoirs to the earth’s surface layers. The crude oil within these reservoirs is constantly subjected to hydrostatic pressures, which compel it to seek an outlet. Consequently, it migrates towards the earth’s surface through seams, cracks, and faults in the reservoir rock.

Gilsonite is a substance that can be dissolved in oily solutions like 2CS or TCE (trichloroethylene). It is a crucial component of carbon gilsonite. Additionally, it contains nitrogen, sulfur, and various volatile compounds. Asphaltite, on the other hand, is a solid and hard mineral composed of natural bitumen. Its primary compounds, known as asphaltenes, consist of large molecules. The color of asphaltite ranges from dark brown to black. Unlike Natural Bitumen , it cannot be dissolved in naphtha solution, a derivative of petroleum.

Instead, heat is required to extract the petroleum content. Although Natural Asphalt and asphaltite are related, they differ chemically and physically. Asphaltites typically lack minerals, while asphalts may contain higher percentages of these materials. Furthermore, asphaltites do not easily boil, unlike asphalt. Gilsonite is typically found in underground mines, appearing as a black and hard substance with a shiny surface. Due to its fragile nature, it is often used in powder form, which has a dark brown to black color.

By utilizing Natural Bitumen , various industries can benefit from its versatile properties and contribute to the improvement of their respective products and processes.