Kettle Hole Geology at Collette Brown blog

Kettle Hole Geology. A kettle hole is an enclosed topographic depression that is formed at the surface of outwash deposits in recently. Kettle, in geology, depression in a glacial outwash drift made by the melting of a detached mass of glacial ice that became wholly or partly buried. A kettle (also known as a kettle hole, kettlehole, or pothole) is a depression or hole in an outwash plain formed by retreating glaciers or draining. Depressions, known as kettles, often pockmark these outwash plains and other areas with glacial deposits. The occurrence of these stranded ice masses is thought to be the result of gradual accumulation of outwash atop the irregular glacier terminus. These are formed by blocks of ice that are seperated from the main glacier by either the glacial ice retreating or by. As the glacier retreats the block of ice is left. Kettles form when a block of stagnant ice (a serac). Kettle holes are formed when large blocks of ice calve from the main glacier onto an outwash plain.

The occurrence of these stranded ice masses is thought to be the result of gradual accumulation of outwash atop the irregular glacier terminus. These are formed by blocks of ice that are seperated from the main glacier by either the glacial ice retreating or by. Kettle, in geology, depression in a glacial outwash drift made by the melting of a detached mass of glacial ice that became wholly or partly buried. Depressions, known as kettles, often pockmark these outwash plains and other areas with glacial deposits. A kettle (also known as a kettle hole, kettlehole, or pothole) is a depression or hole in an outwash plain formed by retreating glaciers or draining. Kettle holes are formed when large blocks of ice calve from the main glacier onto an outwash plain. Kettles form when a block of stagnant ice (a serac). A kettle hole is an enclosed topographic depression that is formed at the surface of outwash deposits in recently. As the glacier retreats the block of ice is left.

A Giant`s Kettle or Pothole in a Stone Created by the Streaming Stock Image Image of round

Kettle Hole Geology Kettles form when a block of stagnant ice (a serac). Depressions, known as kettles, often pockmark these outwash plains and other areas with glacial deposits. A kettle hole is an enclosed topographic depression that is formed at the surface of outwash deposits in recently. These are formed by blocks of ice that are seperated from the main glacier by either the glacial ice retreating or by. Kettle holes are formed when large blocks of ice calve from the main glacier onto an outwash plain. Kettle, in geology, depression in a glacial outwash drift made by the melting of a detached mass of glacial ice that became wholly or partly buried. The occurrence of these stranded ice masses is thought to be the result of gradual accumulation of outwash atop the irregular glacier terminus. Kettles form when a block of stagnant ice (a serac). As the glacier retreats the block of ice is left. A kettle (also known as a kettle hole, kettlehole, or pothole) is a depression or hole in an outwash plain formed by retreating glaciers or draining.