Moraine
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A moraine forms by sediment ridges. 👍 or 👎
moraine
moraine
A moraine forms when a glacier carries and deposits rocks, soil, and other debris as it moves. These materials accumulate at the glacier's edges or are left behind when the glacier retreats, creating a ridge or mound called a moraine.
A moraine is a landform made up of glacial deposits, such as rocks, gravel, and sand, that were pushed by a glacier to form a ridge or hill. Unlike an ordinary hill, a moraine is specifically associated with glacial activity and can reveal information about past glacier movement and deposition.
There are many types of moraines. These include medial moraine, lateral moraine, ground moraine, and terminal moraine. The type that forms along each side of a glacier is a terminal moraine. The one that forms from unsorted rock materials is called a medial moraine.
A lateral moraine forms along the sides of a glacier, where debris is pushed and deposited by the glacier as it moves and erodes the surrounding landscape.
Moraine
Lateral moraine, Medial moraine and Terminal moraine.
You may be referring to an "esker," a snake-like deposit of sediment left by a stream of running water underneath a glacier. At the edge of a glacier, a "moraine" also can form. A moraine is a pile of sediment and debris pushed by the glacier that forms alongside the glacier - a lateral moraine - or at the end of a glacier's run - a terminal moraine.
A terminal moraine is a glacial feature that results from deposition. Terminal moraines are long, low ridges of debris that mark the furthest advance of a glacier.
A moraine is unsorted. Plucking and abrasion by glaciers do not discriminate in size of material debris. It might grind rock matter into what is called "rock flour" and this may be visible at the snout of a glacier, but this and other debris of any size will be be deposited as unsorted till in the form of an end moraine (terminal moraine). A moraine between 2 glaciers is a medial moraine, a moraine along side the glacier is a lateral moraine. Sometimes till can contain glacial erratics... that is, material that came from very far away and does not fit with other materials in the till deposit. Glaciers act as a conveyor belt depending on budget, and material moves with the plasticity of the ice. I hope this helps a little bit.