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Macro photography of a natural snowflake. 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.
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Accretion is defined as the gradual collection of something over time. [1] In meteorology or atmospheric science it is the process of accumulation of frozen water as precipitation over time as it descends through the atmosphere, in particular when an ice crystal or snowflake hits a supercooled liquid droplet, which then freeze together, increasing the size of the water particle.
The hexagonal snowflake, a crystalline formation of ice, has intrigued people throughout history.This is a chronology of interest and research into snowflakes. Artists, philosophers, and scientists have wondered at their shape, recorded them by hand or in photographs, and attempted to recreate hexagonal snowflakes.
Leucojum vernum, commonly called the spring snowflake, [2] [3] St. Agnes' flower (for the patron saint of virgins), [4] and rarely snowbell [5] among others, [a] is a species of flowering plant in the family Amaryllidaceae. [1] It is native to central and southern Europe from Belgium to Ukraine.
Both genera are known as snowflakes. [5] Leucojum is a compound of Greek λευκος, leukos "white" and ἰόν, ion "violet". [5] The spelling Leucoium is also used. In addition to the common name snowflakes, the two Leucojum species are also known as St. Agnes' flower, [5] for patron saint of virgins and gardeners, [5] [6] and snowbells. [7 ...
Sampling the surface of a glacier. There is increasingly dense firn between surface snow and blue glacier ice. Firn field on the top of Säuleck, Hohe Tauern. Firn (/ f ɪər n /; from Swiss German firn "last year's", cognate with before) is partially compacted névé, a type of snow that has been left over from past seasons and has been recrystallized into a substance denser than névé.