Spannagel Cave
   HOME

TheInfoList



OR:

The Spannagel Cave (german: Spannagelhöhle) is a
show cave A show cave—also called tourist cave, public cave, and, in the United States, commercial cave—is a cave which has been made accessible to the public for guided visits. Definition A show cave is a cave that has been made accessible to ...
near
Hintertux Tux is a municipality in the Schwaz district in the Austrian state of Tyrol. Geography The parish of Tux covers the higher and largest part of the Tuxertal, a side valley of the Zillertal that branches off at Mayrhofen. The territory of the parish ...
, in the
Zillertal Alps The Zillertal Alps ( it, Alpi Aurine; german: Zillertaler Alpen) are a mountain range of the Central Eastern Alps on the border of Austria and Italy. Name The range is named after the Zillertal (Ziller river valley) on its north. Geography The ...
in the Austrian state of
Tyrol Tyrol (; historically the Tyrole; de-AT, Tirol ; it, Tirolo) is a historical region in the Alps - in Northern Italy and western Austria. The area was historically the core of the County of Tyrol, part of the Holy Roman Empire, Austrian Emp ...
. Currently about 10 kilometres of cave have been discovered; guided tours enable access to 500 metres of the cave. Its entrance lies below the Spannagelhaus (2531 m), a mountain hut formerly run by the
Austrian Tourist Club The Austrian Tourist Club (german: Österreichische Touristenklub) or ÖTK is the second oldest and third largest Alpine club in Austria. The foundation of the club goes back to an initiative by Gustav Jäger, publisher of ''Der Tourist'', the f ...
(ÖTK). The cave and the hut are named after Dr. Rudolf Spannagel, who was the president of the ÖTK from 1902 to 1904.


Formation

The overwhelming part of the Zillertal Alps consists of the crystalline primary rocks,
pluton In geology, an igneous intrusion (or intrusive body or simply intrusion) is a body of intrusive igneous rock that forms by crystallization of magma slowly cooling below the surface of the Earth. Intrusions have a wide variety of forms and com ...
s and
metamorphic rock Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causin ...
, that do not support the formation of caves. The only exceptions are pockets of rock capable of
karst Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant ro ...
ification such as
limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms whe ...
,
dolomite Dolomite may refer to: *Dolomite (mineral), a carbonate mineral *Dolomite (rock), also known as dolostone, a sedimentary carbonate rock *Dolomite, Alabama, United States, an unincorporated community *Dolomite, California, United States, an unincor ...
,
gypsum Gypsum is a soft sulfate mineral composed of calcium sulfate dihydrate, with the chemical formula . It is widely mined and is used as a fertilizer and as the main constituent in many forms of plaster, blackboard or sidewalk chalk, and drywall. ...
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 The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The J ...
calcite marble of the Hochstegen Formation, a
marble Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or Dolomite (mineral), dolomite. Marble is typically not Foliation (geology), foliated (layered), although there are exceptions. In geology, the ...
with over 90% total carbonate content, that runs through the slate mantle of the ''Western
Tauern window The Hohe Tauern window is a geological structure in the Austrian Central Eastern Alps. It is a window (in German ''fenster'') in the Austroalpine nappes where high-grade metamorphic rocks of the underlying Penninic nappes crop out. The structu ...
''. The formation of this extensive cave as a result of geological
corrosion Corrosion is a natural process that converts a refined metal into a more chemically stable oxide. It is the gradual deterioration of materials (usually a metal) by chemical or electrochemical reaction with their environment. Corrosion engine ...
(and mixing corrosion) is explained by the
tectonics Tectonics (; ) are the processes that control the structure and properties of the Earth's crust and its evolution through time. These include the processes of mountain building, the growth and behavior of the strong, old cores of continents k ...
of the region.


Features

The cave is characterised by the strong presence of
damps Damage-associated molecular patterns (DAMPs) are molecules within cells that are a component of the innate immune response released from damaged or dying cells due to trauma or an infection by a pathogen. They are also known as danger-associated m ...
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
helictite A helictite is a speleothem (cave-formed mineral) found in a limestone cave that changes its axis from the vertical at one or more stages during its growth. Helictites have a curving or angular form that looks as if they were grown in zero grav ...
s. The Spannagel Cave System extends from the ''Gefrorne-Wand-Kees''
glacier A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires dis ...
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 Calcareous sinter is a freshwater calcium carbonate deposit, also known as calc-sinter. Deposits are characterised by low porosity and well-developed lamination, often forming crusts or sedimentary rock layers. Calcareous sinter should not be conf ...
formations,
speleothem A speleothem (; ) is a geological formation by mineral deposits that accumulate over time in natural caves. Speleothems most commonly form in calcareous caves due to carbonate dissolution reactions. They can take a variety of forms, depending on ...
s, crystals, banded marbles and 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 A natural monument is a natural or natural/cultural feature of outstanding or unique value because of its inherent rarity, representative of aesthetic qualities or cultural significance. Under World Commission on Protected Areas guidelines, nat ...
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" 26


External links

Tyrol Landesverein / Spannagel Cave
server not found -->
Spannagelhaus
{{Show caves in Austria Protected areas of Austria Caves of Austria Show caves in Austria Zillertal Alps Schwaz District Landforms of Tyrol (state) Tourist attractions in Tyrol (state)