Archival tags record information about the environment of tagged animals ov
er long periods of time (months to years). In theory, position can be estim
ated from a record of changes in light intensity with time. We describe two
approaches to estimating geoposition based on estimating either the time o
f maximal rate of change in light intensity or the time that a reference li
ght intensity is reached. Digital signal processing is investigated as a me
thod of increasing the signal-to-noise ratio of the light record. Our test
data suggest that the daily position of a tagged animal can potentially be
estimated within an average error of about 140 km (SD's of 0.9 degrees of l
ongitude and 1.2 degrees of latitude), approaching the resolution of the be
st eddy-resolving physical oceanographic models of ocean currents. The sour
ce of the remaining large-scale errors in geoposition appears to be extrins
ic to the tags and may be related to large-scale weather systems. The accur
acy of current archival tags is sufficient to permit an assessment of the o
pen-ocean migration pathways of animals such as maturing salmon and may be
sufficient for use in some parts of the continental shelf as well.