
A Delicate Balance
Geologists speculate that the Old Man of the Mountain, formed by a retreating glacier during the last ice age, looked out over Profile Lake for more than 12,000 years. On May 3, 2003, the delicate balance that had held the "Great Stone Face" in position through the ages came to an abrupt end.
He was universally recognized, that Old Man staring stoically for centuries from his perch atop Franconia Notch. But how many of us really knew him? Most folks stopping beside the road and looking up the mountain, only saw his good side.
His stark, stony features only showed clearly when viewed from the north, looking south. Yet, according to Brian Fowler, owner and president of North American Reserve -- a mining engineering company in Laconia, NH -- who studied The Old Man of the Mountain for the state when it was preparing to build Franconia Notch Parkway in 1976, it was The Old Man's south side -- the side few would recognize -- and other flaws he kept hidden inside, that most likely led to his downfall.

The Old Man actually was made of five slabs of Conway granite balanced atop one another. Seen in this view, but hidden in the familiar view from the north, was a cavern, about four feet wide, behind the Old Man's chin (Block 5) that ran almost the entire width of the Old Man's face. About 80 percent of the chin block hung out over the cliff, according to Fowler. Thus, just about two feet of the chin was anchored to the cliff, held there only by the weight of the four slabs above it. Amazingly, the other four slabs were positioned just so, so that the center of gravity of the chin block was within that two-foot span, allowing the entire Old Man to balance on its chin for centuries.
However, through the years, rain and snow, blown through Franconia Notch on southerly winds, was driven into the cavern and the other cracks between and within the five slabs. One property of water is that it expands when it freezes, and water freezing in a crack in a rock will act as a wedge when it expands, making such cracks larger, eventually splitting the rock. Meanwhile, rocks are comprised of minerals, many of which react chemically with water. Those reactions can weaken the rock from within, eventually breaking it down. Conway granite is loaded with the mineral potash feldspar, which is particularly reactive with water.
According to Fowler, the physical and chemical damage to the Old Man's granite through the years, especially in the cavern, eventually wore away enough rock just behind the chin that the center of gravity of that block moved slightly forward, past the cliff face. When that happened, Fowler believes, the chin tumbled down the cliff, and the rest of the Old man quickly followed.
The Old Man of the Mountain