Ridgeline Instability Observed

The Utah Avalanche Center’s assessment is, predictably, dire. A D2.5 slide triggered by mitigation on the Park City ridgeline—sufficient to inconvenience a Range Rover, I am told—suggests a certain lack of composure in the upper elevations. Nineteen inches of powder is a generous gift, certainly, but one must always consider the cost of generosity. The mercury-colored clouds hanging over the Wasatch are not merely atmospheric decoration; they are indicators of a system actively undermining structural integrity. I observed a regrettable number of sideways sliders gathering near the base of Carpenter Lift this morning, no doubt anticipating the newly refreshed powder. A lamentable sight. Silver Lake remains, thankfully, relatively untouched, though one anticipates a deluge of the uninvited once the conditions are misrepresented on social media. The grooming on Bonanza has the texture of a freshly pressed linen suit, a detail that should not be overlooked. The older snowpack, buried and weakened, is the true concern, a lesson in patience that few seem willing to heed. One can almost feel the mountain’s disapproval. It is a nuanced feeling, akin to a perfectly chilled Chablis being served in a plastic cup. Avoid the East Wall entirely. Seek, instead, the gentle incline of Claimjumper. Begin there. You will find a measure of peace, and possibly, a moment of solitude before the masses descend.