Formation
The overwhelming part of the Zillertal Alps consists of the crystalline primary rocks, plutons and metamorphic rock, that do not support the formation of caves. The only exceptions are pockets of rock capable of karstification such as limestone, Dolomite (rock), dolomite, gypsum and other carbonates. These pockets are generally of quite low thickness, and only allow small caves to be formed. The creation of caves also requires water solubility. The Spannagel Cave has arisen in a large vein of Jurassic calcite marble of the Hochstegen Formation, a marble with over 90% total carbonate content, that runs through the slate mantle of the ''Western Tauern window''. The formation of this extensive cave as a result of geological corrosion (and mixing corrosion) is explained by the tectonics of the region.Features
The cave is characterised by the strong presence of damp (mining), damps and heavy moisture penetration (even leading to cascades). The various stream passages (''Mündungslöcher'') form siphons in places that are only accessible by diving. In those cave passages far from daylight there are rare helictites. The Spannagel Cave System extends from the ''Gefrorne-Wand-Kees'' glacier to the ''Lärmstange'', 2,686 m, and is the highest large cave in Europe Jacoby, E. (1977) with a measured length to date of 10 kilometres. During guided tours the cave's many features (coloured marble, various calc-sinter formations, speleothems, crystals, banded marbles and kolk (vortex), kolks) are explained. In addition, the age of the cave and its formation are described, as are its flora and fauna, climate and cave atmosphere which is beneficial for those suffering from lung ailments. Bats only appear in the vicinity of the cave exits - albeit some get lost in the entrance area. A cave museum has been established in the eastern section of this passageway where several discoveries from the interior of the mountain are displayed.Discovery
In 1919 Alois Hotter, the proprietor of the Spannagelhaus, discovered the cave entrance. He called the cave the Grausliches Loch and used it, as did several other tenants after him, as a rubbish pit. In 1960 Rudolf Radislovich first explored the front part of the cave with its main entrance (''Hauptgang'') and "water entrance" (''Wassergang''), both of which meet in the Hall of Union (''Halle der Vereinigung''). In the following year, Max H. Fink surveyed the known section of the cave and discovered the ''Labyrinth''. In 1964 the Federal Monuments Office (''Bundesdenkmalamt'') designated the cave as a natural monument because of its scientific importance. In 1968 Walter Knezicek and Günther J. Wolf discovered two shafts and the ''Knesi-Harnisch'' at the right hand edge of the ''Halle der Vereinigung'', which all led down into a tunnel about 10 metres below. This was the start of what later became known as the ''Schrauben-Cañon'' ("Screw Canyon"). In 1970 Hannes Jodl found the ''Postkastl'' ("Postbox") at the left hand end of the ''Halle der Vereinigung'', which turned out to be a continuation of the Spannagel Cave. The first person to enter this section was Günther J. Wolf with seven members of his ice course. The research of the ''Kolkgang'' passage (ascending to the ''Elchschädelgang'' passage and ''Dirndlkammer'' chamber, a link with the ''Wassergang'', and descending via the ''Kolkgang'' to the ''Hannes-Jodl-Dom'', at whose ceiling the ''Schrauben-Cañon'' enters, onwards to the ''Dr.-Klaus-Karger-Halle'' and continuing as the ''Kolkgang'' to the edge of the ''ÖTK-Schacht'' shaft) resulted in a doubling of the hitherto known extent of the cave and offered an incentive for further exploration. The years 1972 to 1975 saw four survey expeditions by the State Caving Club in Tyrol (''Landesverein für Höhlenkunde in Tirol''), that advanced as far as the Gneisbach stream. In 1975, as part of a research week by the ''Groupe Spéléologique Luxembourgeois'' with E. Jacoby, M. Möller, G. Mutschlechner and B. Schmitz, the course of the Höhlenbach stream was established. By dying the water it was demonstrated that it surfaced at about 1,980 m in the middle of a rock face south of Waldeben. Likewise the Schneefleck Cave (''Schneefleckhöhle''), which runs parallel to the Spannagel Cave, was discovered and surveyed. In 1976 the Caving Club erected a bivouac in the ''Umkehrhalle'' hall. A 50-hour expedition led by E. Jacoby in 1976/77 discovered and researched the ''Spinnengang'' passage, the ''Mutschlechner-Dom'' cavern and the ''Schatzkammer'' chamber. In 1978 F. Maiberger and W. Mayr reached the westernmost point of the cave, the ''Bauchbad''. In 1984 German speleologists in the Tyrolean Caving Club under the direction of C. Cavelius surveyed the South System (''Südsystem''). In 1987 and 1988 the entrance area of the cave was cleared out, and the gallery joining the ''Trümmerhalle'' and ''Gneisbach'' were discovered and surveyed by W. Mayr and G. Völkl. The ''Schrauben-Cañon'' was first negotiated in 1989 by E. Türke and R. Tobitsch.References
Sources
*Max H. Fink (1961): ''Die Höhle unter dem Spannagelhaus''. – Österr. Touristenzeitung (Vienna) 74 (6): 70 *Günther J. Wolf (1971): ''Bergfahrt in die Unterwelt''. – Österr. Touristenzeitung (Vienna) 84 (2): 24-25 *Gerhard Schirmer (1976): ''Die Höhle beim Spannagelhaus''. – Österr. Touristenzeitung (Vienna) 88 (9): 109-111 *Heinz Ilming, Hans Mrkos (1979): ''Höhlenforschung in Österreich seit 1961''. – Wissenschaftliche Beihefte zur Zeitschrift "Die Höhle" (Vienna) 13: 67-81 *Gerhard Schirmer (1979): ''Die Höhle unter dem Spannagelhaus''. – Festschrift "50 Jahre Bergsteigergruppe im Österr. Touristenklub" (Vienna) 123-125 *Ernest Jacoby, Günter Krejci (1992): ''Die Höhle beim Spannagelhaus und ihre Umgebung''. – Wissenschaftliche Beihefte zur Zeitschrift "Die Höhle" 26External links
Tyrol Landesverein / Spannagel Cave