The persistence of a landform varies with the magnitude and recurrence interval of the event which brought it about. Calver and Anderson (2004, TIBG 29, 1) suggest the terms static persistence where ‘spatial positioning is constant, [and there is] virtually no change in the feature over time’, and dynamic persistence where ‘the type of feature remains in evidence…but individual representations are formed and/or degrade’. See also Wilcock and Iverson, eds (2003) Geophys. Monog. Ser. 135.