An afterglow is a broad arch of whitish or pinkish sunlight in the sky that is scattered by fine particulates like dust suspended in the atmosphere. An afterglow may appear above the highest clouds in the hour of fading twilight, or be reflected off high snowfields in mountain regions long after sunset. The particles produce a scattering effect upon the component parts of white light. True alpenglow, which occurs long after sunset or long before sunrise, is caused by the backscattering of red sunlight by aerosols and fine dust particles low in the atmosphere. After sunset, alpenglow is an afterglow caused by the illumination of atmospheric particles by sunlight as it gets refracted and scattered through the Earth's atmosphere. The high-energy and high-frequency light is scattered out the most, while the remaining low-energy and -frequency light reaches the observer on the horizon at twilight. The backscattering of this light further turns it pinkish to reddish. This period of time is referred to as blue hour and is widely treasured by photographers and painters, as it offers breathtaking views. The afterglow persists until the Earth's shadow (terminator line) overtakes the sky above the observer as night falls and the stars appear, with Venus (the second-brightest celestial object after the Moon in the night sky) visible above the horizon opposite of the Belt of Venus around the antisolar point. After the 1883 eruption of the volcano Krakatoa, a remarkable series of red sunsets appeared worldwide.
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