Took a pic today of Fraggle at Sugarloaf Mountain in Maryland before dropping it off in Easy Money cache. Geologically, Sugarloaf is known as a monadnock, a mountain that remains after the erosion of the surrounding land. Here, that process took approximately 14 million years. At an elevation of 1,282 feet, Sugarloaf rises more than 800 feet above the farmland below. The rugged cliffs on the summit are composed primarily of quartzite, the predominant type of rock on the mountain. Sugarloaf came by its name because its shape reminded early hunters and pioneers of the sugar loaves common in those days.