Lichenometric-dating studies using the yellow-green Rhizocarpon subgenus at
Mueller Glacier in the region of Mt Cook, Southern Alps, New Zealand, reve
al a 'Little Ice Age' maximum about ad 1725/1730. Differences from previous
studies are shown to result from different methods, especially the type of
mathematical functions used for calculating the lichenometric dating curve
s. Previous work also used variable sample sizes, distal moraine slopes, an
d, to some extent, different fixed points. Schmidt hammer measurements enab
le the differentiation of 'Little Ice Age' from pre-'Little Ice Age' fronta
l moraines in the outer glacier foreland and confirm the status of the 'Lit
tle Ice Age' as a separate glacier advance among several advances during th
e Holocene.