medial moraine

Till is the material that makes up ground, lateral and (not always present) medial moraines.

Features observed during the active or surge phase include potholes, known as lacunas and medial moraines.

When lateral moraines adjacent to each other join, they create medial moraines, which are also carried down on the surface of the moving ice.

It has been debated what kind of landform it should be, suggestions ranging from medial moraines to mega-flutes.

Landslides and medial moraines cover much of eastern side of the glacier extending to about two-thirds width of the ice face.

Medial moraines are formed when the lateral moraines of two glaciers are combined when they flow together.

The lowest part of the great Aletsch Glacier is largely covered with detritus of the lateral and medial moraines.

Till is deposited at the terminal moraine, along the lateral and medial moraines and in the ground moraine of a glacier.

Medial moraines are formed when two different glaciers merge and the lateral moraines of each coalesce to form a moraine in the middle of the combined glacier.

Kachina Peaks Wilderness features Arizona's best examples of Ice Age glaciation, found in lateral and medial moraines and abandoned stream beds.

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.

He says all the blocks on the surface of the glaciers are angular, and those in the moraines rounded, yet he says the medial moraines whence the surface rocks come and are a part [of], are only two lateral moraines united.