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Updated: June 16, 2025
Henceforward the obscuring changes are so manifold that the original lake-meadow can be unveiled and seen only by the geologist.
Where the soil happens to be composed of the finer qualities of glacial detritus and the water is not in excess, the nearest approach is made by the vegetation to that of the lake-meadow. But where, as is more commonly the case, the soil is coarse and bouldery, the vegetation is correspondingly rank.
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