WikiVisually
The entire wiki reimagined as a visual magazine with video discovery · Watch your interests come alive
WikiVisually
The entire wiki reimagined as a visual magazine with video discovery · Watch your interests come alive
Nature The World Movies USA Top Art Fine & Rare History Ivy & Inquiry
Dyatlov Pass incident
Videos
The Dyatlov Pass incident was an event in which nine Soviet ski hikers died in the northern part of the Ural Mountains ridge in the Russian SFSR on 1 or 2 February 1959 under undetermined circumstance
The group's tomb at the Mikhailovskoe Cemetery in Yekaterinburg, Russia, in 2012
The group's tomb at the Mikhailovskoe Cemetery in Yekaterinburg, Russia, in 2012
A view of the tent as the rescuers found it 26 February 1959. The tent had been cut open from the inside, and most of the hikers had fled in socks or
A view of the tent as the rescuers found it 26 February 1959. The tent had been cut open from the inside, and most of the hikers had fled in socks or barefoot.
Tomb of the deceased at Mikhailovskoe Cemetery in Yekaterinburg, Russia
Tomb of the deceased at Mikhailovskoe Cemetery in Yekaterinburg, Russia
Katabatic wind
Videos
A katabatic wind is a downslope wind caused by the flow of an elevated, high-density air mass into a lower-density air mass below. The spelling catabatic is also used. Since air density is strongly de
Dyatlov Pass incident
…account for the unexplained deaths, including animal attacks, an avalanche or loud slab avalanche to their tent, appearance of a UFO or ball lightning, katabatic winds, infrasound-induced panic, conflict with local ethnic groups or fugitive criminals, a botched spy meeting with representatives of the Western bloc…
Plateau-cooled air falls into the Makhtesh Ramon, traced by radiation fog, just after dawn. Radiative cooling of the desert highlands chills the air,
Plateau-cooled air falls into the Makhtesh Ramon, traced by radiation fog, just after dawn. Radiative cooling of the desert highlands chills the air, making it more dense than the air over the lowlands. Cooler air can also hold less water vapour; it condenses out as tiny fog droplets, which re-evaporate as the air warms. Here, the falling air is warming adiabatically, and so the fog re-evaporates as it falls.[citation needed]
Katabatic wind in Antarctica
Katabatic wind in Antarctica