Salt caves respond rapidly to environmental changes. Direct measuremen
t and C-14 dating show that complex cross-sections may develop in a fe
w hundred years. Two basic forms are discussed: (1) ingrowing vadose c
anyons where changing width may correspond to changing discharge; (2)
wide low passages with flat ceilings, developed by upward dissolution,
which may indicate rising base level. Some cross-sections are deforme
d by Holocene tectonics. (C) 1998 Elsevier Science B.V. All rights res
erved.