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A close-up of growing ice crystals displaying typical hexagonal symmetry.
A close-up of growing ice crystals displaying typical hexagonal symmetry.
Further freezing of water on an ice crystal produces snowflakes.
Further freezing of water on an ice crystal produces snowflakes.
A halo created by light reflecting off of ice crystals in cirrus clouds. This specific halo is called a 46° halo.
A halo created by light reflecting off of ice crystals in cirrus clouds. This specific halo is called a 46° halo.
Dendritic ice crystals imaged with a scanning electron microscope. The colors are computer generated.
Dendritic ice crystals imaged with a scanning electron microscope. The colors are computer generated.
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An ice block, photographed at the Duluth Canal Park in Minnesota
An ice block, photographed at the Duluth Canal Park in Minnesota
This iceberg can stay afloat in spite of its size because it is less dense than water
This iceberg can stay afloat in spite of its size because it is less dense than water
So-called feather ice on the plateau near Alta, Norway. The crystals form at temperatures below −30 °C (−22 °F) and contain a lot of trapped air, maki
So-called feather ice on the plateau near Alta, Norway. The crystals form at temperatures below −30 °C (−22 °F) and contain a lot of trapped air, making them light enough to be supported by the thin branch
Frozen waterfall in southeast New York
Frozen waterfall in southeast New York