By C. Spötl, M. Luetscher, P. Rittig
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Additional resources for 4th International Workshop on Ice Caves
L. Most Austrian caves are developed in those areas. 6 km in vertical difference (Lamprechtsofen). 26 caves are longer than 10 km and 15 are deeper than 1 km. Often, these cave systems comprise several levels of conduits and mazes that developed in the Upper Miocene. They formed under (epi)phreatic conditions but are hydrologically inactive now as they lie far above the base level. Later, vadose canyon-shaft-systems, which are still partly active, intersect the older subhorizontal parts. Only in some cave systems a low lying hydrologically active epiphreatic level is accessible.
31 Ichnusa Glacier: new evidence of perennial ice deposit in Steinugleflåget doline (Plura Valley - North Norway) L. Sanna 1, S. Lauritzen 1, R. W. 5 km long underground course of the Plura river. In this fluviokarst area, a spectacular South-North oriented canyon fed by the Sprutfossen waterfall (resurgence of the active Jordbrugrotta cave) halts in front of rock threshold. ) explored by cave divers during the last decade and revealed relatively shallow (< 30 m) and large NorthSouth circular passages.
Schulte, I. Dorsten Ruhr-University Bochum, Germany Local accumulations of small calcite crystals (< 1mm) and up to cm-sized calcite aggregates are present on the cave floor and on collapsed blocks in the Breitscheid-Erdbach Cave, Germany. The cave hostrock is composed of mid-Devonian Massenkalk and the thickness of the carbonates overlying the cave reaches 30 m. 2 ka; Kempe, 2008); (b) moderately transparent to milky single crystals and crystal aggregates with non-planar (convex) rhombohedra surfaces, and (c) several sub-types of milky spherolites.