Aufeis
(#13839047)
Level 1 Imperial
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Energy: 48/50
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Personal Style
Apparel
Skin
Scene
Measurements
Length
30.16 m
Wingspan
20.26 m
Weight
7307.96 kg
Genetics
Ice
Crystal
Crystal
Ice
Facet
Facet
Ice
Gembond
Gembond
Hatchday
Breed
Eye Type
Level 1 Imperial
EXP: 0 / 245
STR
6
AGI
6
DEF
6
QCK
5
INT
8
VIT
8
MND
6
Biography
About
Aufeis (German for "ice on top") is a sheet-like mass of layered ice that forms from successive flows of ground water during freezing temperatures. This form of ice is also called overflow, icings, or the Russian term, naled. According to E. de K. Leffingwell the term was first used in 1859 by A. T. von Middendorff following his observations of the phenomenon in northern Siberia.
Aufeis accumulates during winter along stream and river valleys in arctic and subarctic environments. It forms by upwelling of river water behind ice dams, or by ground-water discharge. The latter mechanism prevails in high-gradient alpine streams as they freeze solid. Ground-water discharge is blocked by ice, perturbing the steady-state condition and causing a small incremental rise in the local water table until discharge occurs along the bank and over the top of the previously formed ice. Successive ice layers can lead to aufeis accumulations that are several meters thick. Aufeis typically melts out during summer and will often form in the same place year after year.
Source: Wikipedia
Aufeis (German for "ice on top") is a sheet-like mass of layered ice that forms from successive flows of ground water during freezing temperatures. This form of ice is also called overflow, icings, or the Russian term, naled. According to E. de K. Leffingwell the term was first used in 1859 by A. T. von Middendorff following his observations of the phenomenon in northern Siberia.
Aufeis accumulates during winter along stream and river valleys in arctic and subarctic environments. It forms by upwelling of river water behind ice dams, or by ground-water discharge. The latter mechanism prevails in high-gradient alpine streams as they freeze solid. Ground-water discharge is blocked by ice, perturbing the steady-state condition and causing a small incremental rise in the local water table until discharge occurs along the bank and over the top of the previously formed ice. Successive ice layers can lead to aufeis accumulations that are several meters thick. Aufeis typically melts out during summer and will often form in the same place year after year.
Source: Wikipedia
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