Picture is non-ideal, taken after the snow has settled for a few hours. Still, it shows one good mound formed over a line between older pavement and a newer patch. The crack itself is not a gap or a bump; it's just a very slight offset.
What's happening?
Conditions are strictly normal. 32/20 for several days, no wind. (Thank God!) The only variable I can imagine is the heavy rain about 9 days ago. Maybe the cracks and joints are still full of warm moisture, which sort of soufflés the snow above them? Labels: Heimatkunde
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