Glacial Kettle Hole at Pablo Agnes blog

Glacial Kettle Hole. A giant's kettle, also known as either a giant's cauldron, moulin pothole, or glacial pothole, is a typically large and cylindrical pothole drilled in. A kettle hole is a depression formed by the melting of ice blocks buried in fluvioglacial plains, commonly found in quaternary glacial landsystems,. 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. A kettle, also called a kettle hole or a pothole, is a shallow depression that fills with glacial water in addition to water from other sources and has sediments. Kettles form when previously buried blocks of ice melt. The most widely accepted origin involves the melting of buried ice. 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.

Schematic comparison between kettle holes and craters. (a,b) Kettle
from www.researchgate.net

The occurrence of these stranded ice masses is thought to be the result of gradual accumulation of outwash atop the irregular glacier terminus. The most widely accepted origin involves the melting of buried ice. 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. A kettle, also called a kettle hole or a pothole, is a shallow depression that fills with glacial water in addition to water from other sources and has sediments. Kettles form when previously buried blocks of ice melt. A kettle hole is a depression formed by the melting of ice blocks buried in fluvioglacial plains, commonly found in quaternary glacial landsystems,. A giant's kettle, also known as either a giant's cauldron, moulin pothole, or glacial pothole, is a typically large and cylindrical pothole drilled in.

Schematic comparison between kettle holes and craters. (a,b) Kettle

Glacial Kettle Hole A kettle, also called a kettle hole or a pothole, is a shallow depression that fills with glacial water in addition to water from other sources and has sediments. These are formed by blocks of ice that are seperated from the main glacier by either the glacial ice retreating or by. A kettle, also called a kettle hole or a pothole, is a shallow depression that fills with glacial water in addition to water from other sources and has sediments. Kettles form when previously buried blocks of ice melt. 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. A kettle hole is a depression formed by the melting of ice blocks buried in fluvioglacial plains, commonly found in quaternary glacial landsystems,. A giant's kettle, also known as either a giant's cauldron, moulin pothole, or glacial pothole, is a typically large and cylindrical pothole drilled in. The most widely accepted origin involves the melting of buried ice.

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