Several temporal and event classifications are used for the Quaternary
glacial and interglacial record in the Great Lakes region of North Am
erica, Although based on contrasting principles, the classifications,
as practiced, are similar to one another in most respects and they dif
fer little from the classification proposed by Chamberlin a century ag
o, All are based on stratigraphic units having time-transgressive boun
daries; thus the associated time spans and events are diachronous. Whe
re application of geochronologic classification based on isochronous b
oundaries is not practical or useful, we advocate the use of diachroni
c principles to establish local and regional temporal and event classi
fications, Diachronic and event classifications based on such principl
es are proposed herein for the Great Lakes region, Well-established na
mes, including Wisconsin, Sangamon, and Illinois, are used at the epis
ode (or glaciation/interglaciation) rank without significant redefinit
ion, The Hudson Episode (Interglaciation) is introduced for postglacia
l time, the current interglacial interval, The Wisconsin Episode is di
vided into the Ontario, Elgin, and Michigan Subepisodes in the eastern
and northern parts of the Great Lakes region and into the Athens and
Michigan Subepisodes in the southern and western parts of the Great La
kes region. (C) 1997 University of Washington.