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By C. Spötl, M. Luetscher, P. Rittig

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A narrow descending passage beneath the blocks allows an easy access through an about 50 m-long tunnel developed between this ice body (called Ichnusa Glacier) and the marble rock, where a 5 m-thick succession of clear ice, locally with some boulders, is well exposed with stratigraphic continuity. The accumulation process seems to be represented only by some small seasonal ice speleothems. Air circulation and sublimation are active inside the cave conduit as shown by the large ablation scallops on the ice wall.

Temperature oscillations in the PZ were considered to be the crucial process necessary for keeping individual pearls separated, due to their seasonal movement under the influence of waxing and waning ice. Pearls in the PZ of the DIC were first noted by F. E. Brückmann (a letter dated from December 1, 1728; published in Wolfenbüttel, Germany in 1749). The locality was later repeatedly mentioned in the literature but never studied in detail. Pearls of the DIC and SIC were subjected to a comparative petrographic and geochemical study.

But, unfortunately, until now no reliable data of observations and no isotopic studies of cave ice in Russia are available. In general, the 21th century is characterized by an increase in the awareness of the problems of ice-cave protection, whereas Kungur Ice Cave remains the only excursional route to caves with perennial ice in Russia. 38 Kungur Ice Cave venting schedule N. Trushkova Organization of the Russian Academy of Sciences Mining Institute Ural Branch RAS, Russia An air-depression survey has been conducted in the Kungur Ice cave over three years to analyze the air distribution and its motion.

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