kettle hole - definitie. Wat is kettle hole
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Wat (wie) is kettle hole - definitie

SHALLOW, SEDIMENT-FILLED BODY OF WATER FORMED BY RETREATING GLACIERS OR DRAINING FLOODWATERS
Kettle hole; Kettle lake; Kettlehole; Kettlepond; Kettle pond; Kettlelake; Kettle (geology); Kettle holes; Glacial potholes; Kettle bog; Kettle lakes; Glacial kettles
  • A kettle in the [[Isunngua]] highland, central-western Greenland
  • Hossa]] hiking area, Suomussalmi, Finland
  • Numerous kettle lakes border the [[Denali Highway]] in [[Alaska]]
  • Satellite image of kettle lakes in [[Yamal Peninsula]] (Northern Siberia), adjacent to the [[Gulf of Ob]] (right). The lake colors indicate amounts of sediment or depth.

kettle hole         
¦ noun Geology a hollow, typically filled by a lake, resulting from the melting of a mass of ice trapped in glacial deposits.
Kettle (landform)         
A kettle (also known as a kettle lake, kettle hole, or pothole) is a depression/hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased friction.
Kettle         
  • A traditional [[stainless steel]] kettle with a handle
  • An electric kettle, with boiling water visible in its transparent water chamber
  • A [[stovetop]] kettle on a [[gas burner]]; this type, without a lid, is filled through the ''spout''.
  • A modern white [[Philips]] electric kettle
  • Thermal Vision video of water being boiled in an electric kettle
  • A kettle, with a detachable whistle over its spout
APPLIANCE FOR BOILING WATER
Teakettle; Tea kettle; Electric kettle; Electric jug; Water kettle; Electric kettles; Whistling kettle; Whistling tea kettle
·noun A metallic vessel, with a wide mouth, often without a cover, used for heating and boiling water or other liguids.

Wikipedia

Kettle (landform)

A kettle (also known as a kettle lake, kettle pond, kettle hole, or pothole) is a depression or hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased friction. The ice becomes buried in the sediment and when the ice melts, a depression is left called a kettle hole, creating a dimpled appearance on the outwash plain. Lakes often fill these kettles; these are called kettle hole lakes. Another source is the sudden drainage of an ice-dammed lake. When the block melts, the hole it leaves behind is a kettle. As the ice melts, ramparts can form around the edge of the kettle hole. The lakes that fill these holes are seldom more than 10 m (33 ft) deep and eventually fill with sediment. In acid conditions, a kettle bog may form but in alkaline conditions, it will be kettle peatland.