Unsorted rocky debris that is formed by a melting glacier is called moraine. There are many different types of moraine depending on where the debris is found and deposited.
Till
The accumulation of unsorted rocky debris that is formed by a melting glacier is called a moraine. There are many large moraines throughout the northern parts of North America, Europe, and Asia.
moraines
Simply put a tornado is made of rapidly spinning wind. Condensation like that in an ordinary cloud and a cloud of swirling dust and debris often form within the tornado.A twister, more formally called a tornado, consists of violent rotating wind. The pressure drop inside a tornado typically produces a condensation funnel that makes it visible.n The violent winds pick up dust and debris.
by researching the archaeological debris of different societies
Mt St Helens in Washington gave off steam and debris a few years ago but I don't think that's called an eruption so I would say May 18th, 1980 at Mt St Helens. Hawaii gets lava flow.
The accumulation of unsorted rocky debris that is formed by a melting glacier is called a moraine. There are many large moraines throughout the northern parts of North America, Europe, and Asia.
Unsorted rocky debris that is formed during the melting of a glacier is known as a till. When there are many tills that are present the sediment that is deposited forms a till plain.
The term "till" is the name given to unsorted rocky debris formed by melting glaciers.
Such ridges are referred to as lateral moraines. As a glacier moves, it shears debris, such as rock and soil, on both sides, and this unsorted sediment forms ridges along the edges of the glacier.
The retreating glacier leaves behind linear mounds of till (till being unsorted debris) and is known as moraine.
Moraine is the term used for the unsorted rock and material deposited by the melting and retreat of a glacier. So moraines are mainly rocky areas that used to be covered by a glacier.
The rock is called a glacial erratic when it is left behind by a glacier, and is of a completely different material composition than the rocks on which it was deposited.
Ridges of rock debris that form in front of a glacier are called terminal moraines at the point that the glacier stops moving ahead.
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.
The glacial formation of the collection of loosely arranged glacial debris which may include rock and soil that occurs in recently glaciated and previously glaciated parts on Earth is called moraine. It may contain debris ranging in size from sand-sized glacial flour to huge boulders.
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.
Terminal moraines or terminal