
The colours are probably caused by interference. Light enters the ice and is reflected to and fro between the edges of the fissures. So there are differences in the time the light needs to cover the distance between the ice and the eye of the observer. This causes light waves to amplify or extinguish each other. This is what we perceive as colours.
There is no direct sunlight necessary for this effect (1 2), but it can increase it enormeously (3 4).
Author: Reinhard Nitze, Barsinghausen, Germany
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