Lock Tender's House
Red Covered Bridge
Color on the Hennepin Canal
Colorful Walk
Fall
Wavy Skyline
Green Valley
Low Ceiling, High Waves
Slope
Liquid Mountain Range
Solitary
An unusual morning at Kintzele Ditch - the stream was not flowing into Lake Michigan. Apparently the high waves of the previous day built up the beach so high, it dammed the stream. We watched as the edge of the water moved slowly across the sand, at the rate of about an inch every 20 seconds, looking for a way to the lake. The edge of the water appeared to breathe, as it moved back and forth.
I imagine by the early afternoon, the stream found the lowest point in the sand, and finally made it to Lake Michigan. First a trickle, then after eroding a path, a steady flow of water.
Geographic construction in progress, right before our eyes.
Cove
Valley of Shadows
Bean Field
Delta
Confluence
Updated Classic
Running in the Rays
From Indian Head
Meandering
The boys walk through Kintzele Ditch, a small stream that flows between two sand dunes, and into Lake Michigan. The waves and wind constantly change the path the stream takes to the Lake, at times, by hundreds if not thousands of feet. Like us, it meanders along the shoreline. Often, this stream flows directly perpendicular into the lake, but following stormy or windy weather, the sand is piled up by strong waves, so the stream must meander along the shore until it finds a point to enter the lake.
This changing shoreline offers so many new things to explore each time we visit. Last week, the stream flowed in a different direction, depositing mud onto the beach. Once the water changed direction, the mud began to dry in the sun, forming familiar cracks in the mud. However, at only 1/4 inch thick, the mud began to curl as it dried, revealing the sand beneath, creating an unusual pattern on the beach, reminding me of chocolate nonpareils.
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