What Lightning Flash at Marion Rosenthal blog

What Lightning Flash. While lightning's effects have been measured among the clouds of venus and. Discover the different types of. Lightning is a large spark of electrical current in a planet's atmosphere. Most of these originate in negatively charged regions of the cloud. There are two main types of lighting: The extremely high temperatures generated heat the air molecules to a state of incandescence (white hot) such that they emit a vivid white light. Lightning can occur between opposite charges within the. The flash of lightning temporarily equalizes the charged regions in the atmosphere until the opposite charges build up again.

thunder, Storn, Flash, Lightning, Sky, Night, Eclair, Nuit, Foudre
from wallup.net

The extremely high temperatures generated heat the air molecules to a state of incandescence (white hot) such that they emit a vivid white light. While lightning's effects have been measured among the clouds of venus and. Discover the different types of. Lightning can occur between opposite charges within the. There are two main types of lighting: Lightning is a large spark of electrical current in a planet's atmosphere. The flash of lightning temporarily equalizes the charged regions in the atmosphere until the opposite charges build up again. Most of these originate in negatively charged regions of the cloud.

thunder, Storn, Flash, Lightning, Sky, Night, Eclair, Nuit, Foudre

What Lightning Flash While lightning's effects have been measured among the clouds of venus and. Lightning is a large spark of electrical current in a planet's atmosphere. There are two main types of lighting: The extremely high temperatures generated heat the air molecules to a state of incandescence (white hot) such that they emit a vivid white light. While lightning's effects have been measured among the clouds of venus and. Most of these originate in negatively charged regions of the cloud. Lightning can occur between opposite charges within the. Discover the different types of. The flash of lightning temporarily equalizes the charged regions in the atmosphere until the opposite charges build up again.

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