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ice field - перевод на русский
![Harding Icefield, [[Kenai National Wildlife Refuge]]](https://commons.wikimedia.org/wiki/Special:FilePath/Harding Ice Field 2.jpg?width=200 "Harding Icefield, [[Kenai National Wildlife Refuge]]")
общая лексика
поля ледяные обширные
['aisfi:ld]
существительное
общая лексика
ледяное поле
ледяной простор
![Rare phenomenon – the formation of ball ice. Stroomi Beach, [[Tallinn]], [[Estonia]].](https://commons.wikimedia.org/wiki/Special:FilePath/Jää on kulmunud pallideks (Looduse veidrused). 05.jpg?width=200 "Rare phenomenon – the formation of ball ice. Stroomi Beach, [[Tallinn]], [[Estonia]].")
![Nilas in [[Baffin Bay]]](https://commons.wikimedia.org/wiki/Special:FilePath/Nilas Sea Ice.JPG?width=200 "Nilas in [[Baffin Bay]]")
![As ice melts, the liquid water collects in depressions on the surface and deepens them, forming these melt ponds in the [[Arctic]]. These fresh water ponds are separated from the salty sea below and around it, until breaks in the ice merge the two.](https://commons.wikimedia.org/wiki/Special:FilePath/Ponds on the Ocean, ICESCAPE.jpg?width=200 "As ice melts, the liquid water collects in depressions on the surface and deepens them, forming these melt ponds in the [[Arctic]]. These fresh water ponds are separated from the salty sea below and around it, until breaks in the ice merge the two.")
![Satellite image of sea ice forming near [[St. Matthew Island]] in the Bering Sea](https://commons.wikimedia.org/wiki/Special:FilePath/Seaice.jpg?width=200 "Satellite image of sea ice forming near [[St. Matthew Island]] in the Bering Sea")
![lead]]s. (Scale not available.)](https://commons.wikimedia.org/wiki/Special:FilePath/Sea ice near coast of Labrador -a.jpg?width=200 "lead]]s. (Scale not available.)")
![lead]] developing in the centre.(Scale not available.)](https://commons.wikimedia.org/wiki/Special:FilePath/Ikaasaartik-strait-icefloes-aerial.jpg?width=200 "lead]] developing in the centre.(Scale not available.)")
![leads]]. Much of the open water inside those leads is already covered by ''new ice'' (indicated by a slightly lighter blue color)(scale not available).](https://commons.wikimedia.org/wiki/Special:FilePath/Chukchi Sea.JPG?width=200 "leads]]. Much of the open water inside those leads is already covered by ''new ice'' (indicated by a slightly lighter blue color)(scale not available).")
![Change in extent of the [[Arctic Sea]] ice between April and August, in 2013](https://commons.wikimedia.org/wiki/Special:FilePath/Sea-ice-2013-en.svg?width=200 "Change in extent of the [[Arctic Sea]] ice between April and August, in 2013")
![Sea ice off [[Baffin Island]]](https://commons.wikimedia.org/wiki/Special:FilePath/Sea Ice off Baffin Island.jpg?width=200 "Sea ice off [[Baffin Island]]")
![Sea ice imitates the shoreline along the [[Kamchatka Peninsula]].](https://commons.wikimedia.org/wiki/Special:FilePath/Sea Ice Imitates the Shoreline along the Kamchatka Peninsula.jpg?width=200 "Sea ice imitates the shoreline along the [[Kamchatka Peninsula]].")
![Clear view of the [[Antarctic Peninsula]], the [[Larsen Ice Shelf]] and the sea ice-covered waters around the region](https://commons.wikimedia.org/wiki/Special:FilePath/Antarctic Peninsula, the Larsen Ice Shelf, and the sea ice covered waters around the region.jpg?width=200 "Clear view of the [[Antarctic Peninsula]], the [[Larsen Ice Shelf]] and the sea ice-covered waters around the region")
['aisdrift]
общая лексика
дрейф льда
плавучие льды
торосы
нагромождение плавучего льда
ледяные поля
география
покров ледовый
строительное дело
слой подземного льда
['aisfləu]
существительное
общая лексика
плавучая льдина
ледяное поле
строительное дело
припай, неподвижный лёд
![Ice road between [[Oulunsalo]] and [[Hailuoto]]. This is the longest ice road in Finland.](https://commons.wikimedia.org/wiki/Special:FilePath/Hailuoto Ice Road 20130113 05.JPG?width=200 "Ice road between [[Oulunsalo]] and [[Hailuoto]]. This is the longest ice road in Finland.")
строительное дело
автозимник
Определение
.
Википедия
An ice field (also spelled icefield) is a mass of interconnected valley glaciers (also called mountain glaciers or alpine glaciers) on a mountain mass with protruding rock ridges or summits. They are often found in the colder climates and higher altitudes of the world where there is sufficient precipitation for them to form. The higher peaks of the underlying mountain rock that protrude through the icefields are known as nunataks. Ice fields are larger than alpine glaciers, but smaller than ice caps and ice sheets. The topography of ice fields is determined by the shape of the surrounding landforms, while ice caps have their own forms overriding underlying shapes.
