Relevant bibliographies by topics / Dachstein-Mammuthöhle

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Academic literature on the topic 'Dachstein-Mammuthöhle'

Author: Grafiati
Published: 28 July 2024
Last updated: 31 July 2025

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Journal articles on the topic "Dachstein-Mammuthöhle"

1

Kern, Z., I. Fórizs, M. Molnár, B. Nagy, and R. Pavuza. "Isotope hydrological studies on the perennial ice deposit of Saarhalle, Mammuthöhle, Dachstein Mts, Austria." Cryosphere Discussions 4, no. 3 (2010): 1449–65. http://dx.doi.org/10.5194/tcd-4-1449-2010.

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Abstract. A 5.28 m long ice core was extracted from the major cave ice block of the Mammuthöhle cave system. Tritium concentration in eight samples from the upper 1.2 m of the core was measured. Electrical conductivity measurements were achieved on molten water samples and stable oxygen and hydrogen isotopic compositions were also analysed. The upper ~1.2 m of ice has been deposited from precipitation fallen before the 1960s (based on tritium < 8.5 TU). The Saarhalle ice block is build from atmospheric precipitation and the water perfectly preserved the isotopic composition; however the mea
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2

Rummler, Lina, and Lukas Plan. "Cave Levels in the Dachstein Massif (Eastern Alps)." Austrian Journal of Earth Sciences 116, no. 1 (2023): 151–63. http://dx.doi.org/10.17738/ajes.2023.0009.

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Abstract This paper investigates the vertical distribution of horizontal and subhorizontal cave passages in the Dachstein Massif of Austria. Cave passages that are confined to vertical ranges, so-called cave levels, can be correlated with former valley floors and thus reflect tectonically and climatically stable periods. Previous studies analyzed significant karst Massifs (or parts of them) in the Northern Calcareous Alps but have excluded the Dachstein massif so far. The Dachstein is the second largest massif in the area, contains many extensive caves, and plays a key role in reconstruction o
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3

Kern, Z., I. Fórizs, R. Pavuza, M. Molnár, and B. Nagy. "Isotope hydrological studies of the perennial ice deposit of Saarhalle, Mammuthöhle, Dachstein Mts, Austria." Cryosphere 5, no. 1 (2011): 291–98. http://dx.doi.org/10.5194/tc-5-291-2011.

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Abstract. A 5.28 m-long ice core was extracted from a major cave ice body in the Mammuthöhle cave system. The upper ~1.2 m of ice most likely originate from precipitation fallen before the 1960s (based on <8.5 TU). Characteristic fluctuations in electrical conductivity were observed in the cave ice profile, which seem to mirror the fluctuation of karst and surface water in the water supply of the ice accumulation. The stable isotope composition does not support the hypothesis that ice layers with low conductivity are formed by freezing out of water vapour. Isotope fractionation effects duri
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4

Plan, Lukas, Gottfried Buchegger, Eva Kaminsky, Gabriella Koltai, Tanguy Racine, and Jacek Szczygieł. "Flow regime evolution of a major cave system in the Eastern Alps (Hirlatzhöhle, Dachstein)." International Journal of Speleology 51, no. 3 (2022): 181–91. http://dx.doi.org/10.5038/1827-806x.51.3.2433.

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The 116 km-long and 1560 m-deep Hirlatzhöhle is one of the major cave systems in the Northern Calcareous Alps (NCA; Austria). It is located in the NW part of the Dachstein, an extensive karst massif encompassing 576 km² with its highest point at 2995 m a.s.l. In contrast to most other caves in the NCA, Hirlatzhöhle comprises old (epi)phreatic passages located up to 1 km above the base level as well as two modern major drainage systems. The aim of this study is to define the palaeo- and the active flow conditions in combination with speleogenesis, and the age of the cave levels of Hirlatzhöhle.
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5

Kern, Z., L. Palcsu, R. Pavuza, and M. Molnár. "Age Estimates on the Deposition of the Cave Ice Block in the Saarhalle Dachstein-Mammoth Cave (Mammuthöhle, Austria) based on 3H and 14C." Radiocarbon 60, no. 5 (2018): 1379–89. http://dx.doi.org/10.1017/rdc.2018.96.

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ABSTRACTMeasurements of the radiocarbon (14C) and tritium (3H) activity in a 5.8-m-long ice core from the Saarhalle, Dachstein-Mammoth Cave allowed a substantial revision of previous opinions concerning the age of the ice block, and provide useful experience that may be applied to future 14C dating of cave ice deposits. The stepped combustion technique results in a remarkably older radiocarbon age for the 800°C than for the 400°C fractions of the carbonaceous matter from ice layer samples. The highest tritium activity (37.2±1.2 TU) can be linked to the period of anthropogenically increased tri
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6

Holzer, Franziska, Lukas Plan, and Susanne Gier. "Constructing a cave sediment stratigraphy for the Dachstein Massif sheds light on landscape evolution (Eastern Alps)." Depositional Record, July 3, 2025. https://doi.org/10.1002/dep2.70028.

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AbstractThe Dachstein in Austria is the second largest karst massif in the Alps. It is dominated by Upper Triassic limestone and 290 km of cave passages have been documented. For this study, five major cave systems on the northern edge of the Dachstein were investigated: Hirlatzhöhle, Mammuthöhle, Rieseneishöhle, Schönberghöhle and Günter‐Stummer‐Höhle. Thirty‐five sediment profiles or exposures between 860 m a.s.l. and 1945 m a.s.l. were analysed with respect to stratigraphy, grain size, mineral composition and carbon content. Our study distinguishes the following main types of non‐autochthon
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