KAME Meaning and
Definition
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A kame is a geological feature that is formed as a result of glacial activity. It is a small, cone-shaped hill or ridge made up of sand, gravel, and other sediment deposits. Kames are typically found in areas that were previously covered by glaciers, such as in regions located near the edges or terminus of glaciers.
The formation of a kame begins when a glacier retreats or melts, leaving behind a mound of sediment that was previously carried and deposited by the glacial ice. As the ice melts, the sediment is left behind in a conical shape, with the apex typically pointing upward. Kames often have irregular and undulating surfaces due to the uneven distribution of the sediment deposits.
Kames are commonly found in areas where the ice melts more rapidly, such as in depressions or crevasses within the glacier. They may occur individually or in clusters, forming a kame field. Kame fields can range in size from small groupings to extensive areas of numerous kames.
The name "kame" is derived from the Scottish word "kaim," meaning a ridge or comb. Kames are significant features in glacial landscapes and provide key insights into past glacial activity. They can be used by geologists to determine the direction and movement of ancient glaciers, as well as to understand the process of glacial retreat and the subsequent formation of landforms.
Common Misspellings for KAME
- kzme
- ksme
- kwme
- kqme
- kaje
- kamd
- kamr
- kam4
- kam3
- jkame
- kjame
- mkame
- kmame
- okame
- koame
- ikame
- kiame
- kzame
- kazme
Etymology of KAME
The word "kame" has its origins in the Old Norse language. It comes from the Old Norse word "kamr", which means "comb" or "crest". This term eventually found its way into the English language, referring to a ridge or mound formed by glacial activity. In geology, a kame is a small hill or mound of sand, gravel, and other sediments that accumulated in a depression on the surface of a retreating glacier.
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