Dendrite (crystal)

Manganese dendrites on a limestone bedding plane from Solnhofen, Germany. Scale in mm.
Simulation of dendritic solidification in a supercooled pure liquid using the phase-field model developed by Kobayashi.[1]

A crystal dendrite is a crystal that develops with a typical multi-branching form, resembling a fractal. The name comes from the Ancient Greek word δένδρον (déndron), which means "tree"[citation needed], since the crystal's structure resembles that of a tree. These crystals can be synthesised by using a supercooled pure liquid, however they are also quite common in nature. The most common crystals in nature exhibit dendritic growth are snowflakes and frost on windows, but many minerals and metals can also be found in dendritic structures.

  1. ^ Kobayashi, R. (1993). "Modeling and numerical simulations of dendritic crystal growth". Physica. 63: 410–423. doi:10.1016/0167-2789(93)90120-P.

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