Arête

An arête (/əˈrɛt/ ə-RET; French: [aʁɛt])[1] is a narrow ridge of rock that separates two valleys.

Arêtes can also form when two glacial cirques erode headwards towards one another, although frequently this results in a saddle-shaped pass, called a col.[2] The edge is then sharpened by freeze-thaw weathering, and the slope on either side of the arête steepened through mass wasting events and the erosion of exposed, unstable rock.

[3] The word arête is French for "edge" or "ridge"; similar features in the Alps are often described with the German equivalent term Grat.

A cleaver is a type of arête that separates a unified flow of glacial ice from its uphill side into two glaciers flanking, and flowing parallel to, the ridge, analogous to an exposed mid-channel bar in a braided river.

For example, following a cleaver up or down a mountain may avoid travelling on or under an unstable glacial, snow, or rock area.

Striding Edge, an arête viewed from Helvellyn with the corrie Red Tarn to the left and Nethermost Cove to the right
Crib Goch , Snowdonia , is an arête.