Cirques have growth spurts during deglacial and interglacial periods: Evidence from 10Be and 26Al nuclide inventories in the central and eastern Pyrenees
Low 10Be denudation rates document low Würmian glacial denudation in the Pyrenees Cirques grew faster during temperate cirque glaciation than under icefield conditions Subglacial denudation peaked during the Younger Dryas and Holocene glacial advances Supraglacial ridgetop lowering during the Würm and Holocene was 10–25 mm/ka Pyrenean topography has not reached a buzzsaw equilibrium state