Old Man of the Mountain

The Old Man of the Mountain, also known as the Great Stone Face or the Profile, was a series of five granite cliff ledges on Cannon Mountain in the White Mountains of New Hampshire, United States, that appeared to be the jagged profile of a face when viewed from the north. The rock formation was 1,200 feet above Profile Lake, and measured 40 feet tall and 25 feet wide. The site is located in the town of Franconia.

Franconia Notch is a U-shaped valley that was shaped by glaciers. The Old Man formation was probably formed from freezing and thawing of water in cracks of the granite bedrock sometime after the retreat of glaciers 12,000 years ago. The formation was first noted in the records of a Franconia surveying team around 1805. Francis Whitcomb and Luke Brooks, part of the surveying team, were the first two to record observing the Old Man. The official state history says several groups of surveyors were working in the Franconia Notch area at the time and claimed credit for the discovery.

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