Theses are known as lateral moraines.
Moraines
Glaciers shape the landscape through processes such as erosion, transportation, and deposition. As they move, they carve out valleys, create U-shaped formations, and leave behind features like moraines, which are ridges of debris deposited at their edges. Additionally, glaciers can create glacial lakes and striations on rock surfaces, marking their paths. The melting of glaciers also contributes to sediment deposition in various landforms, altering the ecosystem.
Ridges that form along the sides of glacial valleys as a glacier melts are called moraines. Specifically, lateral moraines are found along the edges of a glacier, while terminal moraines accumulate at the glacier's end. These features are composed of debris and sediment that the glacier has transported and deposited as it advances and retreats.
A moraine is the accumulation of solid material - rock, gravels, sand and clay, carried by a glacier, and deposited when the glacier shrank. The material is mainly from avalanches off surrounding mountains, which include rocky material as well as ice and snow.
Ground moraines are located at the base of the glacier.
Terminal moraines or terminal
Glaciers push up mounds of dirt as the advance forward. When they recede, they leave these mounds of earth, debris and rock What are these mounds called? In my ancient memory, I thought they were called doldrums, but this doesn't seem to be right judging from the responses I have obtained from this site. The hills are called moraines or just a moraine.
Friction ridges or fingerprints are formed by the patterns of raised skin ridges in the papillary layer of the dermis. These ridges are made up of dermal papillae, which project into the epidermis and create unique patterns that form fingerprints.
There are no ridges on a US Penny or the US Nickel, the edges are smooth.
A till is an unsorted mixture of sediment deposited by a glacier, while a moraine is a landform made up of till deposited at the edge or beneath a glacier. Tills are deposited directly by the moving glacier, while moraines are created from the accumulation of till as the glacier advances, retreats, or melts.
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.
A moraine is a type of landform that consists of accumulated glacial debris, such as rocks, gravel, and sand, deposited by moving glaciers. Moraines are usually elongated and can be found along the edges or in the middle of glaciers, serving as records of past glacier activity. They come in various forms, including lateral, medial, terminal, and ground moraines.