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This ice waterfall shows some illumination on the bottom (somebody was shining a flashlight) and some of the red lava (or earth) above. The lavender is some sort of artifact of technique because I recall no colors like that in the cave - but it looks nice in the picture.
Dendritic ice crystals imaged with a scanning electron microscope. The colors are computer generated. The aerospace industry is working to design a radar that can detect ice crystal environments to discern hazardous flight conditions. Ice crystals can melt when they touch the surface of warm aircraft, and refreeze due to environmental conditions.
A snowflake is a single ice crystal that is large enough to fall through the Earth's atmosphere as snow. [1] [2] [3] Snow appears white in color despite being made of clear ice. This is because the many small crystal facets of the snowflakes scatter the sunlight between them. [4]
Water vapor plays a role as it deposits ice crystals, known as hoar frost, during cold, still conditions. [54] During this transition, snow "is a highly porous, sintered material made up of a continuous ice structure and a continuously connected pore space, forming together the snow microstructure".
Ice Fog (Also called ice-crystal fog, frozen fog, frost fog, frost flakes, air hoar, rime fog, pogonip.) A type of fog, composed of suspended particles of ice; partly ice crystals 20 to 100 micron in diameter, but chiefly (especially when dense) ice particles about 12–20 micron in diameter, formed by direct freezing of supercooled water ...
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Crystal structure of Ice XI viewed along the c-axis Crystal structure of ice XI (c-axis in the vertical direction) Ice XI is the hydrogen-ordered form of the ordinary form of ice. The total internal energy of ice XI is about one sixth lower than ice I h, so in principle it should naturally form when ice I h is cooled to below 72 K.