A kettle is a depression left by melted blocks of ice in glacial deposits.
The depressions left behind are called kettles. The raised areas are called moraines.
The depressions left by melted blocks of ice in glacial deposits are called kettle holes. They are circular or oval-shaped depressions that form when large chunks of ice left behind by a retreating glacier become buried in sediment. When the ice eventually melts, it creates a hole in the ground.
When the glacier melted from North America it left a mass of "heterogeneous" rock debris (loosely termed "glacial drift") etc
Global deposits related to streams of melted water.
After the last ice age stranded ice blocks left behind by the continental glacier melted and formed lakes.
The depressions left behind are called kettles. The raised areas are called moraines.
The depressions left by melted blocks of ice in glacial deposits are called kettle holes. They are circular or oval-shaped depressions that form when large chunks of ice left behind by a retreating glacier become buried in sediment. When the ice eventually melts, it creates a hole in the ground.
A kettle is a depression left by melted blocks of ice in glacial deposits.
A kettle pond is a glacial formed depression. As the glaciers receded massive chunks of ice fell that melted and sank into the earth, the resulting "puddle" is a kettle pond. Here in Rhode Island there are many kettle ponds along the coast along the Lateral MORAINES. Kettle ponds are isolated with no springs or streams in or out, that would be a glacial lake if it did. Neil USFWS Ranger
When the glacier melted from North America it left a mass of "heterogeneous" rock debris (loosely termed "glacial drift") etc
All over the world. They can be found anywhere from on a mountain, like at Mount Washington's Lake of the Clouds Hut, to underground, like at Howe's Caverns.
Glacial errosion
A glacial lake is a lake with origins in a melted glacier. Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks.
a glacial deposit that is sorted and layered by streams or melted water is called
Global deposits related to streams of melted water.
Water is abundant by melting glacial ice or by desalinating sea water.
Varves are glacial lake deposits, usually an annual sediment of thick pale sediment denoting summer deposition when some ice melted and left silt and sand to settle in a lake, and a thin, dark layer of clay for a winter deposit when little sediment entered the lake.