Auroras are natural light displays in the sky, typically observed at night in polar regions. Charged particles from the solar wind are captured by Earth's magnetosphere and drawn to the magnetic poles, where excited electrons emit energy in the form of light creating the aurora effect. Auroras can take different forms like poleward arcs, theta aurora, and dayside arcs and occur in various colors from flickering to black or subvisual red arcs.

3. Sun emits charged particles Particle form Solar Wind Solar Wind being captured by Earth’s magnetosphere Particles trapped in Van Allen Belts drawn up to the Earth’s magnetic poles The excited electrons emit energy in form of light AURORA

6. October 30, 2003 Aurora February 10, 2008 , Homer, Alaska November 7, 2004, southeastern Minnesota