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Chota bheem for colouring. Asbestos refers to six unique minerals chrysotile amosite anthophyllite tremolite crocidolite and actinolite belonging to the serpentine and amphibole families. Of the amphibole silicate minerals amosite and crocidolite occur only in the asbestiform habit while tremolite actinolite and anthophyl lite occur in both asbestiform and non asbesti. Chrysotile or white asbestos is the most commonly encountered form of asbestos accounting for approximately 95 of the asbestos in the united states and a similar proportion in other countries.
Amosite crocidolite tremolite actinolite and anthophyllite. In its natural state amosite is known as grunerite and it was mainly mined in south africa. Chrysotile or white asbestos is formed of several scrolls and could be said to have a curly silky nature.
As such it is distinct from other asbestiform minerals in the amphibole group. Chrysotile lizardite and antigorite are the three principal serpentine silicate minerals. The amphibole group has 5 types of asbestos.
Cement sheets fire protection gaskets insulation. Chrysotile is the only asbestos mineral in the serpentine group and has historically accounted for. Serpentine minerals have a sheet or layered structure with curly fibres.
Chrysotile is more easily woven into cloth than other types of asbestos. It is a soft fibrous silicate mineral in the serpentine subgroup of phyllosilicates. According to the american cancer society exposure to amosite asbestos creates a higher risk of cancer in comparison with common chrysotile asbestos.
There is increasing evidence that the curly nature helps the human body to remove chrysotile fibres from the lung.
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