CCTV footage has emerged from Morocco since the earthquake, showing light emanating from the horizon shortly before the quake.
It's been nearly seven days since a devastating 6.8 magnitude quake struck Morocco, killing more than 2,900 people and injuring more than 3,000 others, as heroes continue to peer through the rubble to find any hope of life trapped beneath the debris alluvium. and jetsam.
A strong earthquake struck southwest of Marrakesh last Friday and the French master warned of aftershocks despite the country not being in the "most dynamic seismological location".
Several CCTV recordings have emerged via web entertainment from Morocco of the seismic tremor, showing a light emanating from the horizon shortly before the tremor. Specialists have identified these brilliant oddities as real, yet they are still scratching their heads as to what causes them in any case.
According to reports, these lights have authentic roots.
John Derr, a retired geophysicist who worked at the US Topographical Review, let CNN know that these different shades of lights are most definitely real.
"EQL's vision depends on obscurity and other positive factors," Derr, breaking away from these shocks, made sense.
He said a new "video from Morocco shared online appeared to be a tremor caught on security cameras during the 2007 earthquake in Pisco, Peru."
Juan Antonio Lira Cacho, a physical sciences teacher at the Universidad Nacional City Hall de San Marcos in Peru and the Ecclesiastical College of Peru who focused on the peculiarity, said video and surveillance cameras made it easier to focus on the lights of the seismic tremors.
Different types of seismic shock lights
There are several kinds of lights referenced in an article co-authored by Derr and distributed in the 2019 edition of the Strong Earth Geophysics reference book.
the lights show the expected illumination or at times it may appear to be the same band as the aurora borealis. They can also appear to be floating in the air. One of these species also includes fire-like radiation from the beginning.
To figure it out, Derr and his partners collected all the relevant data from earthquake lights dating back to the 1600s.
Their work was distributed in 2014 in a paper in the journal Seismological Exploration Letters.
Their findings revealed that about 80% of the earthquake lights were observed in tremors with a magnitude greater than 5.0. As the discoveries suggest, the event was seen virtually immediately before or during the tremor, apparent up to 600 kilometers (372.8 mi) from the focus.
More often, earthquakes occur in nearby unified areas of structural plates. However, the investigation found that in the vast majority of cases the iridescent peculiarities took place within the structural plates, as opposed to their limits.
According to reports, these lights are likely to be seen near rift valleys where the Earth's outer layer has been limited apart.
What can be the reasons for seismic tremors?
Friedemann Freund, a colleague of Derr's, an assistant professor at San Jose College and a previous NASA specialist, proposed the hypothesis.
Freund told CNN that when certain imperfections or impurities in gems in rocks are subjected to mechanical pressure — such as when moving between structural plates — they break into pieces in a flash, creating force.
He noticed that the rock is a shell that turns into a semiconductor when focused precisely.
He added: "In front of earthquakes, huge volumes of rock are concentrated - countless cubic kilometers of rock on the outside of the world - and the loads incite the movement of grains, mineral grains comparable to each other."
"It's reminiscent of turning on a battery, creating electric charges that can flow out of concentrated rocks into and through unstressed rocks. The charges travel fast, up to about 200 meters per second," he opined in a 2014 article for Discussion.
Several different explanations have also stated that friction-based electricity is produced by rock cracking and radon radiation, among other things.
There is no agreement about this peculiarity, and researchers are focused on this mystery.
Freund anticipated that there might be a situation where seismic tremors, or the electrical charge that triggers them, could be used to help estimate the methodology of a significant earthquake.




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