The depressions left behind are called kettles. The raised areas are called moraines.
Kettle holes are depressions left by melted blocks of ice in glacial deposits. These features are typically surrounded by mounds of sediment called kames. Kettle holes are common in areas that were once covered by glaciers during the last Ice Age.
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.
Cirques. They are the bowl-shaped depressions formed by the erosion of glaciers in the upper parts of alpine valleys.
With glaciers, you typically get deposits like moraines (made up of rocks and sediment) and glacial till (unsorted material deposited by the ice). Wind deposits mainly consist of sand dunes, known as aeolian deposits, which form in deserts and coastal areas with strong winds.
The layered sediments that form on the bottom of a glacial lake are called "glacial lacustrine deposits." These deposits typically consist of fine-grained sediments, such as silt and clay, which settle in calm waters. Over time, they can accumulate in distinct layers, reflecting variations in sediment supply and water conditions.
Kettle holes are depressions left by melted blocks of ice in glacial deposits. These features are typically surrounded by mounds of sediment called kames. Kettle holes are common in areas that were once covered by glaciers during the last Ice Age.
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.
Erratic blocks or "erratics" for short.
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They are called varves.
Cirques. They are the bowl-shaped depressions formed by the erosion of glaciers in the upper parts of alpine valleys.
With glaciers, you typically get deposits like moraines (made up of rocks and sediment) and glacial till (unsorted material deposited by the ice). Wind deposits mainly consist of sand dunes, known as aeolian deposits, which form in deserts and coastal areas with strong winds.
The layered sediments that form on the bottom of a glacial lake are called "glacial lacustrine deposits." These deposits typically consist of fine-grained sediments, such as silt and clay, which settle in calm waters. Over time, they can accumulate in distinct layers, reflecting variations in sediment supply and water conditions.
The debris of boulders eroded and carried down by glaciers will eventually form moraines (mounds) where the front of the glacier melts and retreats, leaving the debris behind. Moraines can be high and wide enough to form a dam, behind which glacial melt water is trapped and lakes are formed.
A large hole in the ground left from the melting of a huge chunk of glacial ice is called a kettle Also . . . Large bowl shaped depressions that occur at the head of mountain glaciers that result from a combination of frost wedging, glacial plucking, and abrasion are called cirques
A physical feature on Rocky uplands lakes and swamps in Canada is called a "kettle." Kettles are depressions formed by glacial activity, where blocks of ice were buried in sediment and subsequently melted, leaving behind a hollow that can fill with water. These features contribute to the unique landscape of the region, creating diverse ecosystems and habitats.
Marshes formed when glaciers created depressions on the Earth's surface are called kettle ponds. These ponds are commonly found in areas where the glacial ice melted and left behind depressions that filled with water. Kettle ponds support unique ecosystems and are important habitats for diverse plant and animal species.