Glacial plucking exploits pre-existing fractures in the bedrock. This plays a key role in opening and creating new fractures but has only provided small segments of loose material. This is then followed by the entrainment of the loosened rock by the ice. During the process of entrainment, loose rock material is frozen onto the base of the glacier

Glacier

A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation over many years, often centuries. At least 0.1 km² in area and 50 m thick, but often much larger, a glacier slowly deforms and flows due to stresses induced by its weight...

and incorporated into the glacial ice. It is significant when the bedrock is highly jointed, as this allows meltwater to penetrate. Plucking is also known as quarrying.

As the valley glacier moves down the valley there is friction with the rock floor. This causes the basal ice of the glacier to melt (which helps lubricate the movement of the glacier) and infiltrate joints in the bedrock where it then freezes. As the glacier moves on, the rock now bonded to the glacier, is plucked from the floor into the base of the glacier and carried with it.

External links

• Plucking animation (source article)