There are different types of moraines, depending on their location and how they formed:
* Terminal moraine: This is the most prominent type, forming at the glacier's furthest point of advance.
* Lateral moraine: These run along the sides of the glacier, made of debris that fell from the valley walls.
* Medial moraine: Formed when two lateral moraines merge, running down the center of the glacier.
* Recessional moraine: A series of moraines left behind as a glacier retreats in stages.
* Ground moraine: A thin, uneven layer of debris spread across the landscape as the glacier melts.
Moraines are important geological features, providing evidence of past glacial activity and helping to shape the landscape.
