While over 65% of Merry Lea was historically submerged under a kettle lake during the immediate post-glacial period, there were (and continue to be) higher elevated landforms. These include glacially-formed eskers and kames and a system of wind-deposited sand dunes between what is now High Lake and Bear Lake.
This ancient dune system’s well-drained soils dry out quickly, thus limiting tree cover to black oak and white oak— species that tolerate limited water availability. Competition for water results in tree cover that is sparser than that of close-canopied forests. The partially sun-lit conditions promote the growth of the native herbaceous prairie species that can tolerate partial shade. These pre-European settlement ecosystems were most likely oak woodlands and savannas. These dry-site plant communities were most likely maintained by periodic fire—naturally-occurring or ignited by Native American peoples who were known to inhabit this site. The 1919 State Archeological Survey describes evidence of their presence on a ridge near Luckey’s Landing.