INLET LAKES The process by which a drowned river valley becomes an inlet (or baymouth) lake is
shown below. Note the two inlet lakes in the lower left part of the diagram, and the
baymouth bars (BMB) that seal them off. The images and maps below show but a few of the many inlet lakes in the state. If the lake is small and has no or only a small stream entering it, such as the one
below, the lake may have no outlet. That is, the water entering it may leave as
groundwater. However, when the lake has a significant river flowing into it, the inlet lake will
have been able to maintain it's outlet to Lake Michigan, despite the fast pace at which
sand is being deposited in the spit that forms the "dam" between it and the main
lake (Michigan). Thus, Hamlin Lake (below, north of Ludington) maintains an outlet
to Lake Michigan even today. The sand barrier on many lakes, like the one between
Hamlin Lake and Lake Michigan, is often capped with sand dunes. (Hamlin Lake is in Mason County, just north of Ludington.)
This material has been compiled for educational use only, and
may not be reproduced without permission. One copy may be printed for personal
use. Please contact Randall Schaetzl (soils@msu.edu)
for more information or permissions. |