INLET LAKES

Inlet lakes occur along the shores of the Great Lakes, and are particularly common along the Lake Michigan shore.  They occur due to two main processes of landscape development.  First, during the Holocene, when lake levels were low, rivers draining into the Great Lakes incised their valleys, creating deep valleys that entered the lakes (i.e., fluvial incision). Later, lake levels rose, drowning these old river valleys.  Finally, longshore transport of sand along the beach front has created spits and finally joined these sandy spits across the baymouth, effectively "sealing off"  the old river valley mouth to form an inlet lake (i.e., coastal processes).  The sandy spits that separate the two lakes are called "baymouth bars".

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.
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The images and maps below show but a few of the many inlet lakes in the state.
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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.
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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.
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(Hamlin Lake is in Mason County, just north of Ludington.)

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At the far eastern end of Little Traverse Bay lies the city of Petosky, and the inlet lake known as Round Lake (see below).  Petosky State Park is found within the sand barrier that lies between Round Lake and Little Traverse Bay (Lake Michigan).
round-lake.jpeg (332521 bytes)

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.