Lakes and Ponds

Fall color along an inland lake

NPS photo

Lake Superior is the major water body in the area and forms the northern border of Pictured Rocks National Lakeshore. The lake has a maximum depth of 420 m (1,335 feet) but is relatively shallow near PRNL's shoreline. Its surface lies at an elevation of 187 m (600 feet) above sea level. The maximum tidal/storm elevation has been recorded at 604.3 feet. In recent times lake level has varied on the order of several feet due to changes in precipitation and evaporation.

The more prominent inland lakes are Grand Sable, Beaver, Little Beaver, Chapel, Little Chapel, Miners, Trappers, Legion, Kingston, and the Shoe Lakes. These lakes range in size from 762 acre Beaver Lake to 10 acre Miners Lake. Most of the inland lakes, with the exception of Grand Sable Lake and Chapel Lake, are quite shallow (3 to 6 m, 10 to 20 feet in average depth), but have lengthy flow-through rate times.

Many of the lakes are mesotrophic and have Secchi disk (water visibility) readings between 2 and 5 meters. The intensive logging in the area and recurrent fires may have caused erosion and nutrient deposition in the lakes. Miners Lake and Little Chapel Lake exhibit the greatest trend toward eutrophication. The most oligotrophic lakes are Legion Lake, the Shoe Lakes, and Grand Sable Lake. The inland lakes vary considerably in their water chemistry, but many can be classified as productive, brown, alkaline water lakes.

Although Legion, the Shoe, Kingston, and Trappers Lakes are alike in that they are closed basin lakes (having no streams flowing in or out) they were formed in different ways. Kingston, Legion, and the Shoe Lakes are kettle lakes, formed by the melting of a block of ice that separated from the retreating glacier about 10,000 years ago. In particular, Legion Lake and the Shoe Lakes lie high on the watershed divide between Lake Superior and Lake Michigan and receive very little groundwater input of elements like calcium, magnesium, and silica. They are acidic (pH 4.8-5.1), poorly buffered, and have high Secchi disk readings (5-9 m).

Trappers, Beaver, and Little Beaver Lakes are located in Beaver Basin, which was once an embayment of Lake Superior when the lake level was considerably higher. As the lake level dropped, sandy beach ridges separated the lakes from Lake Superior, creating these relict lakes. Miners Lake lies along the Miners River in Miners Basin, which was also an embayment of Lake Superior during higher lake levels approximately 5,000 years ago.

Chapel Lake is elongate and was likely formed by a large plunge pool in a glacial meltwater channel. Its southern basin is about 43 m (140 feet) deep, extending into the Jacobsville Sandstone, and is shallow toward the northern end, where rooted, aquatic plants emerge at the surface. Chapel Lake is meromictic; the deepest layer of water does not mix with the upper lakewater during spring and fall turnovers. The water below approximately 18 m (60 feet) is cold, dense, and anoxic (extremely limited dissolved oxygen).

 

Lake Superior Shoreviewer

Lake Superior ShoreViewer
Are you planning a summer kayak trip on the shores of Lake Superior? Ever wondered what the mouth of the Hurricane River looks like?

The Superior Watershed Partnership website hosts the Lake Superior ShoreViewer. The ShoreViewer covers every Upper Peninsula coastal county (9) and township (32) bordering Lake Superior. It offers user-friendly advantages such as easy-to-recognize birds-eye oblique photography. It also provides detailed planning information including soils, elevation, slope, cover types, U.S. Geological Survey quad maps, color infrared photography and wetland data.

www.superiorwatersheds.org/shorelineviewer