Traducción y análisis de palabras por inteligencia artificial ChatGPT
En esta página puede obtener un análisis detallado de una palabra o frase, producido utilizando la mejor tecnología de inteligencia artificial hasta la fecha:
- cómo se usa la palabra
- frecuencia de uso
- se utiliza con más frecuencia en el habla oral o escrita
- opciones de traducción
- ejemplos de uso (varias frases con traducción)
- etimología
avalanche of ice - traducción al ruso
![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.")
![Forest Service]] team using a 105mm [[recoilless rifle]] for avalanche control at [[Mammoth Mountain]] in the [[Inyo National Forest]].](https://commons.wikimedia.org/wiki/Special:FilePath/106mm Recoilless Rifle.jpg?width=200 "Forest Service]] team using a 105mm [[recoilless rifle]] for avalanche control at [[Mammoth Mountain]] in the [[Inyo National Forest]].")
![Trains passing in an avalanche gallery on the [[Wengernalpbahn]] in Switzerland.](https://commons.wikimedia.org/wiki/Special:FilePath/WAB Allmend Lawinengalerie Sommer.jpg?width=200 "Trains passing in an avalanche gallery on the [[Wengernalpbahn]] in Switzerland.")
строительное дело
противообвальная (лавинозащитная) галерея
строительное дело
снегозащитная галерея
Definición
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Wikipedia
An avalanche is a rapid flow of snow down a slope, such as a hill or mountain.
Avalanches can be set off spontaneously, by factors such as increased precipitation or snowpack weakening, or by external means such as humans, animals, and earthquakes. Primarily composed of flowing snow and air, large avalanches have the capability to capture and move ice, rocks, and trees.
Avalanches occur in two general forms, or combinations thereof: slab avalanches made of tightly packed snow, triggered by a collapse of an underlying weak snow layer, and loose snow avalanches made of looser snow. After being set off, avalanches usually accelerate rapidly and grow in mass and volume as they capture more snow. If an avalanche moves fast enough, some of the snow may mix with the air, forming a powder snow avalanche.
Though they appear to share similarities, avalanches are distinct from slush flows, mudslides, rock slides, and serac collapses. They are also different from large scale movements of ice.
Avalanches can happen in any mountain range that has an enduring snowpack. They are most frequent in winter or spring, but may occur at any time of the year. In mountainous areas, avalanches are among the most serious natural hazards to life and property, so great efforts are made in avalanche control.
There are many classification systems for the different forms of avalanches, which vary according to their users' needs. Avalanches can be described by their size, destructive potential, initiation mechanism, composition, and dynamics.
