Lateral moraine, Medial moraine and Terminal moraine.
The four types of moraines are lateral, medial, terminal, and ground moraines. Lateral moraines form along the sides of a glacier, medial moraines are formed when two glaciers merge and their lateral moraines combine, terminal moraines mark the furthest extent of a glacier's advance, and ground moraines are the debris left behind beneath a glacier as it retreats.
It can certainly reduce mountains in size, but it can also form small hummocks called moraines, of various types, which are deposits of the material it has eroded from the higher ground.
Some of moraines types are rogen and veiki Moraines,Generally moraines can be classified either by their origin, location with respect to a glacier or former glacier, or by their shape.The first approach is suitable for moraines associated to contemporary glaciers but more difficult to apply to old moraines whose glaciers have disappeared long ago.Moraines types like rogen and veiki moraines are defined by their particular morphology since their origin has been a matter of dispute. Some moraine types are only known from ancient glaciers, like the two former ones, while medial moraines of valley glaciers are poorly preserved and difficult to distinguish after the retreat or melting of the glacier.Refer to link below for more details.
Moraines are often fragmentary because they are created by the accumulation of debris carried by a glacier. As the glacier moves and melts, it can deposit various sizes of rock fragments and till in a chaotic manner, leading to the fragmented appearance of the moraines. Additionally, the mixing and rearrangement of the debris by glacial processes can contribute to the irregular and broken nature of moraines.
A ridge or mound of debris chiefly composed of boulders, gravel, sand, and clay is called a moraine. Moraines are deposited by glaciers and can be found in various formations, such as lateral moraines along the sides of glaciers or terminal moraines at the end of a glacier's advance. Moraines are important features in understanding past glacial activity.
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.
A famous example of a moraine is the Terminal Moraine of the Wisconsin glaciation that forms Long Island in New York, USA. This ridge of debris was left behind as the glacier retreated and is a classic example of a moraine.
drumlin
there is glacial drift and that is the act of rock material carried and deposited by glaciers. there is till which is the act of unsorted rock material that is deposited directly by a melting glacier and there is stratified drift which is the result of a glacial deposit that has been sorted and layered by action of streams or meltwater
Ground moraines are located at the base of the glacier.
these moraines are abrasive elements carried in the bottom of a frozen glaicer aplus ground moraines
Moraines are found along the edges, flanks, and in the middle of glaciers. They are formed from debris and rocks that have been transported and deposited by the glacier's movement. Lateral moraines form along the sides, medial moraines run down the center, and terminal moraines are found at the glacier's terminus.