Based on a laboratory simulation, Glew and Ford (Earth Surface Processes, 1
980, vol. 5, pp. 25-36) put forward a model of solution flute formation whi
ch embraces both morphological evolution and time to formation. The occurre
nce of dated fluted surfaces in the field presents opportunities to test th
is model. The morphological development of flutes is consistent with the ex
perimental observations in that width stabilizes early whereas depth contin
ues to increase. The time to formation of flutes is confirmed as limestone
(10(3) years) > gypsum (10(2) years) > salt (10(1) years), and is consisten
t with the solubility of the main rock-forming minerals. Copyright (C) 2001
John Wiley & Sons, Ltd.