The first documented ascent of the peak (then spelled as "Stone's Peak") was made by Frederick H. Chapin and William L. Hallett as published in Chapin's 1889 book, Mountaineering in Colorado: The Peaks about Estes Park.[8]
Climate
According to the Köppen climate classification system, Stones Peak is located in an alpine subarctic climate zone with cold, snowy winters, and cool to warm summers.[9] Due to its altitude, it receives precipitation all year, as snow in winter and as thunderstorms in summer, with a dry period in late spring. This climate supports the Sprague Glacier on the southwest aspect of Stones Peak.[10]
Gallery
Southeast aspect
North aspect of Stones Peak, with Longs Peak (distant left)
^Lisa Foster, 2005, Rocky Mountain National Park: The Complete Hiking Guide, Westcliffe Publishers, ISBN9781565795501, p. 94.
^Frederick Hastings Chapin (1889), Mountaineering in Colorado: The Peaks about Estes Park, Appalachian Mountain Club, p. 147–55.
^Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11. ISSN1027-5606.
^James Fargo Balliett (2016), Mountains Environmental Issues, Global Perspectives, Publisher: Taylor & Francis, ISBN9781315496993