Layers of volcanic ash, or tephra form widespread chronostratigraphic
marker horizons which are important because of their distinctive chara
cteristics and rapid deposition over large areas. Absolute dating of p
rehistoric layers effectively depends upon C-14 analysis. We focus her
e on Icelandic tephra layers at both proximal and distal sites and con
sider three strategies to obtain age estimates: 1) the conventional da
ting of individual profiles; 2) high-precision multisample techniques
or ''wiggle-matching'' using stratigraphic sequences of peat; and 3) a
combination of routine analyses from multiple sites. The first approa
ch is illustrated by the dating of a peat profile in Scotland containi
ng tephra from the AD 1510 eruption of Hekla. This produced a C-14 age
compatible with AD 1510, independently derived by geochemical correla
tion with historically dated Icelandic deposits. In addition, the ca.
2100 sp date for the Glen Garry tephra in Scotland, determined by a se
ries of dates on a peat profile in Caithness, is supported by its stra
tigraphic position within C-14 dated profiles in Sutherland, and may b
e applied over a very large area of Scotland. More precise dates for i
ndividual tephras may be produced by ''wiggle-matching'', although thi
s approach could be biased by changes in peat-bog stratigraphy close t
o the position of the tephra fall. As appropriate sites for ''wiggle-m
atch'' exercises may be found only for a few Icelandic tephras, we als
o consider the results of a spatial approach to C-14 dating tephra lay
ers. We combined dates on peat underlying the same layer at several si
tes to estimate the age of the tephra: 3826 +/- 12 BP for the Hekla-4
tephra and 2879 +/- 34 BP for the Hekla-3 tephra. This approach is eff
ective in terms of cost, the need for widespread applicability to Icel
andic tephra stratigraphy and the production of ages of a useful resol
ution. We stress the need for accurate identification of tephra deposi
ts without which the conclusions drawn from subsequent C-14 dating wil
l be fundamentally flawed.