When glaciers sculpted the Great Lakes region, they left a terminal moraine about 10,000 years ago that forms the southern border of the Stony Lake watershed (the edge of it can be easily seen driving north from Montague). The ridge is a small element in a landscape
of hills and ridges known as the Port Huron systems -- one of America’s major glacial features. This great line of moraines can be traced almost continually from Minnesota, through Canada and the upper Midwest, to New York state. Over many thousands of years, wind, rain, rushing waters, and surging surf formed what
we know today as Stony Lake.

This shawl is a relaxing knit with an easy-to-memorize repeat and is constructed asymmetrically, which allows the knitter to blissfully knit until it’s time to bind off.