Abstract
In the course of researches into the glaciation of the western part of the Southern Uplands of Scotland the writer accidentally stumbled upon a series of large and continuous moraines bordering the Central Valley. Some of these had been observed and described by earlier workers, others—probably constituting the larger part—had either escaped detection or had been differently interpreted.The solution of the problem presented by these moraines not only required their careful mapping from coast to coast, but also inevitably led to an attempt to decipher the history of the retreat of the ice out of the Central Valley.

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