Long Lake, located near Lake Michigan within the dune-complexes of Ind
iana Dunes National Lakeshore, USA, was formed some time during the Pl
eistocene and Holocene epochs. A surficial or sink for the later. The
hydrologic processes in the lakeshore and surrounding environs have be
en significantly altered during the agricultural, municipal, and indus
trial development of the region. Limited data suggest that the organis
ms of Long Lake have elevated levels of several contaminants. This stu
dy attempts to quantify seepage within the lake to assess the potentia
l threat to groundwater quality. Seepage measurements and minipiezomet
ric tests were used to determine seepage within the lake. Seepage meas
urements and minipiezometric tests suggest that water seep out of Long
Lake, thus recharging the groundwater that flows southwest away from
the lake. There is a great deal of variability in the seepage rate, wi
th a mean of 11.5 x 10(-4) +/- 11.2 x 10(-4) m d(-1). The mean seepage
rate of 0.3 m yr(-1) for Long Lake is greater than the 0.2 m yr(-1) r
echarge rate estimated for the drainage basin area. The Long Lake rech
arge volume of 2.5 x 10(5) m(3) yr(-1) is approximately 22% of the vol
ume of the lake and is significant when compared to the total surface
recharge volume of 4.8 x 10(5) m(3) yr(-1) to the upper aquifer of the
drainage area. There is a potential for contamination of the groundwa
ter system through seepage from the lake from contaminants derived fro
m aerial depositions.