They were created by glacial movement 10.000 years ago, in the last ice age.
Eskers are winding ridges of sediment deposited by meltwater streams flowing under glaciers. Kettle lakes are formed when a block of ice from a retreating glacier gets buried in sediment and then melts. Both eskers and kettle lakes are common features of glacial landscapes.
an esker is formed by a Glacier
As the ice blocks left behind by the continental glacier melted after the last ice age, they formed bodies of water known as kettle lakes. These kettle lakes are depressions in the landscape caused by the melting of the ice blocks, which were then filled with water from the melted ice.
Eskers were formed by depositional processes. They are long, winding ridges of sand and gravel that were deposited by meltwater streams flowing in tunnels beneath glaciers during the last Ice Age.
After a glacier retreats, it leaves behind various landforms such as moraines, eskers, and kettle lakes. These landforms are a result of the glacier's movement and deposition of rocks, sediment, and meltwater. Over time, the landscape may also undergo further erosion and reshaping by other geological processes.
Eskers are winding ridges of sediment deposited by meltwater streams flowing under glaciers. Kettle lakes are formed when a block of ice from a retreating glacier gets buried in sediment and then melts. Both eskers and kettle lakes are common features of glacial landscapes.
A kettle lake is a shallow, sediment-filled body of water formed by retreating glaciers or draining flood-waters.
eskers
Eskers
A kettle lake is a shallow, sediment-filled body of water formed by retreating glaciers or draining flood-waters.
an esker is formed by a Glacier
i think it is because they look like kettles
The area of Kettle Lakes Provincial Park is 12.61 square kilometers.
Eskers
Eskers are formed when a subglacial stream of meltwater flows within, on, or beneath glaciers. As the glacier melts and retreats, sediment and gravel carried by the stream are deposited in long winding ridges. These deposits form the characteristic winding shape of eskers.
As the glaciers retreated after the last ice age, landforms such as moraines, eskers, and kettle lakes were left behind. The melting ice also contributed to the formation of valleys, fjords, and depressions that filled with water to create lakes and rivers. Additionally, the receding glaciers exposed previously buried land, allowing for the colonization and migration of plant and animal species.
A kettle lake is a shallow body of water formed by receding glaciers or draining flood waters. Chunks or blocks of ice break free and soil, rocks, and gravel filled in around the ice. When the block of ice melted, some of the debris falls into the hole, creating a sediment filled basin. When a kettle is filled with water, it is called a kettle lake.