Stone stripe

A stone stripe, also called a lava stringer,[1] is an elongated concentration of mostly talus-like basalt rock found along a hillside or the base of a cliff.

[2] Stone stripes are thought to have been originally created by periglacial conditions of the Quaternary period during an Ice age.

It is likely their formation originates from multiple processes including frost action, surface erosion, eluviation, and mass wasting.

However, it is likely that intense freeze and thaw cycles account for the natural sorting of the rock debris within a stone stripe, and also accounts for the shallow depth of the stripes, since frost penetration is thought to not penetrate deeper than 1 meter in the region.

[3] Stone stripes are also found surrounding soil mounds of central Oregon which also owe their formation to freeze and thaw cycles.