Lake damp and hill wind on Columbia roofs
The lake keeps its shoreline damp and foggy, so north slopes and shaded cottage roofs grow moss and dry slowly. Away from the water the hills take wind across open fields and heavy inland snow that stays for weeks. Ice forms at the eaves on the cold attics of cottages and the warm attics of mid-century houses alike. Tree cover is thick, so valleys and gutters fill each fall and limbs come down in ice storms. Spring freeze and thaw is long in eastern Connecticut and works at old flashing.

