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stratification
Stratification as this is a term that describes the layering of rocks and so is not a term that is related to sediment transport (i.e. erosion) but is instead the result of deposition, compaction and cementation.
a kettle
Glacial till is unsorted sediment deposited directly by glacial ice.
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.
stratification
Stratification as this is a term that describes the layering of rocks and so is not a term that is related to sediment transport (i.e. erosion) but is instead the result of deposition, compaction and cementation.
Yes. Glaciers carry large amounts of sediment. When that sediment is deposited it is called glacial till.
Agents for erosion and transporting sediments include gravity, wind, water (including currents), or ice. Other forces in nature do not act in the same way, for example, lava.
a kettle
only when the fluid transporting the sediments slows down or when glacial ice melts
only when the fluid transporting the sediments slows down or when glacial ice melts
Glacial till is unsorted sediment deposited directly by glacial ice.
water moves a greater amount of sediment in a much faster way
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.
kettle
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.