Перевод и анализ слов искусственным интеллектом ChatGPT
На этой странице Вы можете получить подробный анализ слова или словосочетания, произведенный с помощью лучшей на сегодняшний день технологии искусственного интеллекта:
- как употребляется слово
- частота употребления
- используется оно чаще в устной или письменной речи
- варианты перевода слова
- примеры употребления (несколько фраз с переводом)
- этимология
avalanche$6176$ - перевод на голландский
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![Kenai Fjords]].](https://commons.wikimedia.org/wiki/Special:FilePath/AvalancheToe.jpg?width=200 "Kenai Fjords]].")
![Avalanche blasting in French [[ski resort]] [[Tignes]] (3,600 m)](https://commons.wikimedia.org/wiki/Special:FilePath/Avalanche Blasting.jpg?width=200 "Avalanche blasting in French [[ski resort]] [[Tignes]] (3,600 m)")
![A powder snow avalanche in the [[Himalayas]] near [[Mount Everest]].](https://commons.wikimedia.org/wiki/Special:FilePath/Avalanche on Everest.JPG?width=200 "A powder snow avalanche in the [[Himalayas]] near [[Mount Everest]].")
![Washington state]]. Avalanche paths in alpine terrain may be poorly defined because of limited vegetation. Below tree line, avalanche paths are often delineated by vegetative trim lines created by past avalanches. The start zone is visible near the top of the image, the track is in the middle of the image and clearly denoted by vegetative trimlines, and the runout zone is shown at the bottom of the image. One possible timeline is as follows: an avalanche forms in the start zone near the ridge, and then descends the track, until coming to rest in the runout zone.](https://commons.wikimedia.org/wiki/Special:FilePath/Avalanche path 7271.JPG?width=200 "Washington state]]. Avalanche paths in alpine terrain may be poorly defined because of limited vegetation. Below tree line, avalanche paths are often delineated by vegetative trim lines created by past avalanches. The start zone is visible near the top of the image, the track is in the middle of the image and clearly denoted by vegetative trimlines, and the runout zone is shown at the bottom of the image. One possible timeline is as follows: an avalanche forms in the start zone near the ridge, and then descends the track, until coming to rest in the runout zone.")
![Avalanche warning sign near [[Banff, Alberta]]](https://commons.wikimedia.org/wiki/Special:FilePath/Avalanche warning Banff.jpg?width=200 "Avalanche warning sign near [[Banff, Alberta]]")
![[[United States Forest Service]] avalanche danger advisories.](https://commons.wikimedia.org/wiki/Special:FilePath/Avalanche warning in Tuckerman.JPG?width=200 "[[United States Forest Service]] avalanche danger advisories.")
![After surface [[hoarfrost]] becomes buried by later snowfall, the buried hoar layer can be a weak layer upon which upper layers can slide.](https://commons.wikimedia.org/wiki/Special:FilePath/D Hoarfrost 3.jpg?width=200 "After surface [[hoarfrost]] becomes buried by later snowfall, the buried hoar layer can be a weak layer upon which upper layers can slide.")
![Avalanche on [[Simplon Pass]] (2019)](https://commons.wikimedia.org/wiki/Special:FilePath/Lawinenkegel auf dem Simplonpass (2019).jpg?width=200 "Avalanche on [[Simplon Pass]] (2019)")
![Heavy equipment in action after an avalanche has interrupted service on the [[Saint-Gervais–Vallorcine railway]] in [[Haute-Savoie]], France (2006).](https://commons.wikimedia.org/wiki/Special:FilePath/Ligne Saint-Gervais - Vallorcine - avalanche 2006 - 08.jpg?width=200 "Heavy equipment in action after an avalanche has interrupted service on the [[Saint-Gervais–Vallorcine railway]] in [[Haute-Savoie]], France (2006).")
![Loose snow avalanches (far left) and slab avalanches (near center) near [[Mount Shuksan]] in the [[North Cascades]] mountains. Fracture propagation is relatively limited.](https://commons.wikimedia.org/wiki/Special:FilePath/Loose snow and slab avalanches near mt shuksan.jpg?width=200 "Loose snow avalanches (far left) and slab avalanches (near center) near [[Mount Shuksan]] in the [[North Cascades]] mountains. Fracture propagation is relatively limited.")
![cornice]] of snow about to fall. Cracks in the snow are visible in area (1). Area (3) fell soon after this picture was taken, leaving area (2) as the new edge.](https://commons.wikimedia.org/wiki/Special:FilePath/Mount Windsor Cornice2.jpg?width=200 "cornice]] of snow about to fall. Cracks in the snow are visible in area (1). Area (3) fell soon after this picture was taken, leaving area (2) as the new edge.")
![In steep avalanche-prone terrain, traveling on [[ridge]]s is generally safer than traversing the slopes.](https://commons.wikimedia.org/wiki/Special:FilePath/North Ridge of Mount Rohr.jpg?width=200 "In steep avalanche-prone terrain, traveling on [[ridge]]s is generally safer than traversing the slopes.")
![15 cm deep, soft slab avalanche triggered by a snowboarder near Heliotrope Ridge, [[Mount Baker]] in March 2010. Multiple crown fracture lines are visible in the top-middle of the image. Note the granular characteristic of the debris in the foreground that results from the slab breaking up during descent.](https://commons.wikimedia.org/wiki/Special:FilePath/Snowboarder triggered soft slab near mount baker.jpg?width=200 "15 cm deep, soft slab avalanche triggered by a snowboarder near Heliotrope Ridge, [[Mount Baker]] in March 2010. Multiple crown fracture lines are visible in the top-middle of the image. Note the granular characteristic of the debris in the foreground that results from the slab breaking up during descent.")
![[[Snow fence]]s in [[Switzerland]] during summer.](https://commons.wikimedia.org/wiki/Special:FilePath/Verbauung Tanngrindel.JPG?width=200 "[[Snow fence]]s in [[Switzerland]] during summer.")
Определение
Википедия
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The Galtür avalanche occurred on 23 February 1999 in the Alpine village of Galtür, Austria. At 50 m (160 ft) high and traveling at 290 km/h (180 mph), the powder avalanche overturned cars, destroyed buildings and buried 57 people. By the time rescue crews managed to arrive, 31 people had died. It was considered the worst Alpine avalanche in 40 years. Three major weather systems originating from the Atlantic accounted for large snowfalls totaling around four meters in the area. Freeze-thaw conditions created a weak layer on top of an existing snow pack; further snow was then deposited on top. This, coupled with high wind speeds, created large snow drifts and caused roughly 170,000 tons of snow to be deposited.
