Fulgurites (from the Latin fulgur meaning thunderbolt) are natural hollow glass tubes formed in quartzose sand, or silica, or soil by lightning strikes.[1] They are formed when lightning with a temperature of at least 1,800 °C (3,270 °F) instantaneously melts silica on a conductive surface and fuses grains together; the fulgurite tube is the cooled product.[2] This process occurs over a period of around one second,[3] and leaves evidence of the lightning path and its dispersion over the surface.[4] Fulgurites can also be produced when a high voltage electrical distribution network breaks and the lines fall onto a conductive surface with sand beneath. They are sometimes referred to as petrified lightning. The glass formed is called lechatelierite which may also be formed by meteorite impact and volcanic explosions. Because it is amorphous, fulgurite is classified as a mineraloid. Fulgurites can have deep penetrations, sometimes occurring as far as 15 metres (49 ft) below the surface that was struck.[5]

The tubes can be up to several centimeters in diameter, and meters long. The longest fulgurite to have been found is a little over 4.9 meters in length, and was found in northern Florida, USA.[3] Their color varies depending on the composition of the sand they formed in, ranging from black or tan to green or a translucent white. The interior is normally very smooth or lined with fine bubbles; the exterior is generally coated with rough sand particles and is porous. They are rootlike in appearance and often show branching or small holes. Fulgurites occasionally form as glazing on solid rocks (sometimes referred to as an exogenic fulgurite).[6]


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  2. Carl Ege. "What are fulgurites and where can they be found?". geology.utah.gov. http://geology.utah.gov/surveynotes/gladasked/gladfulgurites.htm. Retrieved 2009-03-21.
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  6. Exogenic fulgurites from Elko County, Nevada: a new class of fulgurite associated with large soil-gravel fulgurite tubes (Rocks & Minerals, Sep/Oct 2004, Vol. 79, No. 5.)

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