STABLE ISOTOPE COMPOSITION OF PERENNIAL ICE IN CAVES AS AN AID TO CHARACTERIZING ICE CAVE TYPES Charles J. Yonge William D. MacDonald Yonge Cave & Karst Consulting Inc., Yonge Cave & Karst Consulting Inc., 1009 Larch Place, 1009 Larch Place, Canmore, AB T1W 1S7, Canada
[email protected] Canmore, AB T1W 1S7, Canada Abstract We examine caves which are dominated by a cold zone Stable isotope studies of perennial ice from western close to the entrance (Cold Zone type), in Permafrost North American ice caves suggest that three main (Permafrost type) and in pit caves where cold air and types can be defined: cold trap, permafrost, and cold snow is trapped (Cold Trap type). Formation of ice in zone. Some complex cave systems may comprise two the latter is most likely to resemble glacial ice by direct or more types. While 14 caves were sampled from the accumulation of snow in open pits and in some cases - region, in this study, 9 definitive sites were examined where ice flow has been demonstrated - the system is in more detail where they exemplified classic perennial referred to as a Glacier Cave (Holmlund et al., 2005; ice features: massive ice, hoar frost, ice stalagmites MacDonald, 1994). and so on. Stable isotopes of the ice (δ18O and δ2H) assist in the understanding the origin of the freezing Methodology moisture, whether from direct snow (cold trap), moist summer air (permafrost) or from humid air within Field Sites the cave (cold zone). Furthermore, delineating the While stable isotope data has been acquired from 14 complex systematics of cave ice formation is vitally cave sites, we focus on 3 caves from west of the Divide: important if it is to be used (or rejected) as a proxy climate record.