Rock Fracture
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Mirror and Mist

Mirror refers to a smooth morphology on a joint surface and mist refers to the near-smooth frosted zone (Figure 1). Mirror and mist are commonly confined in a small area around the initiation point and interpreted to occur at low propagation velocity. When the propagation velocity becomes high and the local stress is perturbed, hackle marks, rib marks, and fringe joints will occur.

Fracture surface of glass rod broken in tension, showing 'mirror', 'mist', as well as 'hackle' zones spreading outward from fracture origin (lower edge). Viewed in reflected light. Diameter of rod 4.5 mm. From Johnson and Holloway (1966).Figure 1. Fracture surface of glass rod broken in tension, showing 'mirror', 'mist', as well as 'hackle' zones spreading outward from fracture origin (lower edge). Viewed in reflected light. Diameter of rod 4.5 mm. From Johnson and Holloway (1966).
Reference:

Johnson, A.M., Holloway, D.G., 1966. On the shape and size of the fracture zones on glass fracture surfaces. Philosophical Magazine 14 (130): 731 - 743.



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