The study of the sedimentary strata within the Teton Range, shows that these strata consist mostly of limestones and dolomites. The Madison Limestone consists of a basal, dark-colored, fine-grained dolomitic limestones overlain by hundreds of feet of gray limestone that is classified as fossiliferousoosparite and fossiliferous pelsparite.[6] Abundant fossils of shells and corals, which are protected by federal laws, have been found in the Madison Limestone at Fossil Mountain.[7] Underlying the Madison Limestone, the Darby Formation consists predominantly of dolomites and limestones that commonly contain discontinous layers of calcareous shale or sandstone.[6]
Fossil Mountain Ice Cave
Fossil Mountain Ice Cave is a notable solutional cave in the Madison Limestone west of Fossil Mountain. This cave is also known as Darby Ice Cave, Darby Canyon Caves, or Wind Cave. This cave has about 3 mi (4.8 km) of passage. The underground distance between entrances is about 1.5 mi (2.4 km) of travel underground 1 mi (1.6 km) on the surface. It is noted for the presence of layered ice and sediments depoists up to 42 ft (13 m) thick.[8][9][10]
Fossil Mountain Ice Cave has a combination of hazards that have resulted in frequent rescues. The safe exploration of this cave requires the participation of cavers with previous experience with this cave; expertise in ice and rock caving; specialized and appropriate caving equipment; and detailed planning and preparation, including the prepositioning of ropes, for a visit to this cave. Also, visiting this cave has detrimental effects on the preservation of scientifically significant ice deposits found within this cave. For example, visitor-induced melting of ice deposits was noted as early as 1975.[8][9][10]
The analysis of measurements of stable isotopes of oxygen and hydrogen recovered form samples of ice collected from Fossil Mountain Ice Cave provided a record of paleotemperatures of this part of the Teton Range for the past 175 years. They showed a continuing increase in local temperatures over the past the past 160 years. In addition, two consecutive very cold years in the early 1870s were found.[11]
^Reed, J.C. and Love, J.D., 1971, Preliminary geologic map of the Mount Bannon quadrangle, Teton County, Wyoming , Open-File Report OF-71-233, 1:24,000, one sheet. Reston, Virginia, U.S. Geological Survey.
^Love, J.D., Reed Jr, J.C. and Christiansen, A.C., 1992. Geologic map of Grand Teton National Park, Teton County, Wyoming, Miscellaneous Investigations Series Map. I-2031, 1:62,500, one sheet. Reston, Virginia, U.S. Geological Survey.
^ abDixon, J.R. and Reeves, C.C., 1965. Representative carbonate petrography of some lower and middle Paleozoic rocks, west flank Teton Mountains, Wyoming. Journal of Sedimentary Research, 35(3), pp.704-72.
^ abHigham, S.R., Palmer, A.N., 2018. Ice caves in the USA. In Persoiu, A., and Lauritzen, S.-E., eds., pp. 706-715. Ice Caves. Amsterdam, Netherlands, Elsevier. 730 pp. ISBN978-0-631-20472-5
^ abHill, C., Sutherland, W., and Tierney, L., 1976, Caves of Wyoming. Bulletin 59. Geological Laramie, Wyoming, Geological Survey of Wyoming. 230 pp.
^ abIWIC, 2014. International Workshop on Ice Caves 17-22 August 2014, Idaho Falls, Idaho. Craters of the Moon National Monument and Preserve Timpanogos Cave National Monument, Idaho, U.S. National Park Service. 24 pp.
^Fuller, N., 2006, A reconstruction of Late Holocene climate in the Teton area from layers of sediment contained in ice from Fossil Mountain Ice Cave, Teton County, Wyoming. Alpine Karst, 2, pp. 1–14.