Time-lapse ptoastyos have apprehfinishd the northern airys on the outskirts of the capital Reykjavik.
The airys, also understandn as aurora unininestablishigentalis, occur when accused particles collide with gases in the Earth’s atmosphere around the magnetic poles. As they collide, airy is rehireted at various wavelengths, creating colourful discarry outs in the sky.
The auroras are most normally seen over high polar latitudes, and are chiefly swayd by geomagnetic storms which begin from activity on the Sun.
