Borealis
(#21162543)
Level 1 Skydancer
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Energy: 0/50
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Personal Style
Apparel
Skin
Scene
Measurements
Length
3.79 m
Wingspan
5.4 m
Weight
683.83 kg
Genetics
White
Ripple
Ripple
Royal
Shimmer
Shimmer
White
Gembond
Gembond
Hatchday
Breed
Eye Type
Level 1 Skydancer
EXP: 0 / 245
STR
4
AGI
5
DEF
4
QCK
9
INT
9
VIT
4
MND
9
Lineage
Parents
Offspring
- Sirvente
- Cia
- LaVieVoleta
- Broderic
- Aria
- Greenfield
- Balsoi
- Yellowfield
- Dixie
- Ion
- Caden
- Watercape
- Rolande
- Dreamstrider
- Eeren
- Eeren
- Eeren
- Odessa
- Eugene
- Unnamed
- Foston
- Chipperfield
- Brylen
- Akakia
- Saa
- Ian
- Lominna
- Lominna
- Berseth
- Riverwalker
- Tofu
- Knight
- Matilal
- Azra
- Pouncer
- Jonathan
- Blair
- Highstorm
- Violin
- Ricneiros
- Haimona
- Ironfrill
- Pluto
- Neptune
- Serenity
- Melisande
- Fishsticks
- Asiedu
- Vessel
- Ringo
- Xanthia
- Lastway
- Shannon
- Lezard
- Emery
- Siella
- Tupelo
Biography
Fact Corner:
An aurora, sometimes referred to as a polar light, is a natural light display in the sky, predominantly seen in the high latitude (Arctic and Antarctic) regions. Auroras are produced when the magnetosphere is sufficiently disturbed by the solar wind that the trajectories of charged particles in both solar wind and magnetospheric plasma, mainly in the form of electrons and protons, precipitate them into the upper atmosphere (thermosphere/exosphere), where their energy is lost. The resulting ionization and excitation of atmospheric constituents emits light of varying colour and complexity. The form of the aurora, occurring within bands around both polar regions, is also dependent on the amount of acceleration imparted to the precipitating particles. Precipitating protons generally produce optical emissions as incident hydrogen atoms after gaining electrons from the atmosphere. Proton auroras are usually observed at lower latitudes.
In northern latitudes, the effect is known as the aurora borealis (or the northern lights), named after the Roman goddess of dawn, Aurora, and the Greek name for the north wind, Boreas, by Galileo in 1619. Auroras seen within the auroral oval may be directly overhead, but from farther away they illuminate the poleward horizon as a greenish glow, or sometimes a faint red, as if the Sun were rising from an unusual direction.
An aurora, sometimes referred to as a polar light, is a natural light display in the sky, predominantly seen in the high latitude (Arctic and Antarctic) regions. Auroras are produced when the magnetosphere is sufficiently disturbed by the solar wind that the trajectories of charged particles in both solar wind and magnetospheric plasma, mainly in the form of electrons and protons, precipitate them into the upper atmosphere (thermosphere/exosphere), where their energy is lost. The resulting ionization and excitation of atmospheric constituents emits light of varying colour and complexity. The form of the aurora, occurring within bands around both polar regions, is also dependent on the amount of acceleration imparted to the precipitating particles. Precipitating protons generally produce optical emissions as incident hydrogen atoms after gaining electrons from the atmosphere. Proton auroras are usually observed at lower latitudes.
In northern latitudes, the effect is known as the aurora borealis (or the northern lights), named after the Roman goddess of dawn, Aurora, and the Greek name for the north wind, Boreas, by Galileo in 1619. Auroras seen within the auroral oval may be directly overhead, but from farther away they illuminate the poleward horizon as a greenish glow, or sometimes a faint red, as if the Sun were rising from an unusual direction.
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