Crystal habit: Difference between revisions
From Glossary of Meteorology
No edit summary |
m (Rewrite with Template:Term and clean up) |
||
Line 1: | Line 1: | ||
{{Term | |||
|Display title=crystal habit | |||
{{ | |Definitions={{Definition | ||
|Num=1 | |||
|Meaning=Any characteristic external crystalline form. | |||
|Explanation=For an [[ice crystal]], may refer just to the ratio of the lengths of the [[crystal]] parallel to its c and a axes (at 90° to or parallel to the hexagonal basal plane), but usually it simply means the crystal shape, including dendritic, skeletal, prismatic, sectors, etc. The term is not applied to the internal [[crystal lattice]]. Slight variations in the growth rates of different crystal planes in a given crystal structure lead to quite different crystal habits. Such growth rate variations may result from variations in [[temperature]] and [[water vapor]] supersaturation of the [[environment]] in which the crystal grows. | |||
}} | |||
= | }} | ||
Latest revision as of 11:50, 26 March 2024
Any characteristic external crystalline form.
For an ice crystal, may refer just to the ratio of the lengths of the crystal parallel to its c and a axes (at 90° to or parallel to the hexagonal basal plane), but usually it simply means the crystal shape, including dendritic, skeletal, prismatic, sectors, etc. The term is not applied to the internal crystal lattice. Slight variations in the growth rates of different crystal planes in a given crystal structure lead to quite different crystal habits. Such growth rate variations may result from variations in temperature and water vapor supersaturation of the environment in which the crystal grows.