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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Europe
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Alps
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Eastern Alps
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Northern Limestone Alps (1)
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Limestone Alps
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Northern Limestone Alps (1)
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North Austrian Alps (1)
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Prealps (2)
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Central Europe
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Austria
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Burgenland Austria (1)
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Lower Austria
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Vienna Austria (1)
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North Austrian Alps (1)
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North Austrian Molasse (2)
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Salzkammergut (2)
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Styria Austria (1)
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Tyrol Austria (1)
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Upper Austria
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Gosau Austria (2)
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Bohemian Massif (3)
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Molasse Basin
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North Austrian Molasse (2)
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Northern Limestone Alps (1)
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Variscides (1)
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commodities
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petroleum
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natural gas (1)
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elements, isotopes
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carbon
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C-13/C-12 (1)
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isotope ratios (1)
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isotopes
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stable isotopes
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C-13/C-12 (1)
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O-18/O-16 (1)
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metals
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iron (1)
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oxygen
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O-18/O-16 (1)
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fossils
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Invertebrata
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Cnidaria
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Anthozoa
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Zoantharia
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Scleractinia (1)
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microfossils (2)
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palynomorphs
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Dinoflagellata (1)
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Plantae
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algae
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Rhodophyta (1)
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geologic age
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Cenozoic
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Quaternary
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Holocene
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upper Holocene (2)
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Tertiary
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Neogene
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Miocene (1)
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Paleogene
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Eocene
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upper Eocene (1)
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Oligocene
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lower Oligocene
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Rupelian (1)
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Mesozoic
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Cretaceous
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Gosau Formation (1)
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Upper Cretaceous
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Santonian (1)
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Senonian (1)
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igneous rocks
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igneous rocks
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plutonic rocks
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granites (1)
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metamorphic rocks
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metamorphic rocks
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metasedimentary rocks
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metapelite (1)
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minerals
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carbonates (1)
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silicates
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ring silicates
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cordierite (2)
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sheet silicates
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chlorite group
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chlorite (1)
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clay minerals
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kaolinite (1)
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smectite (1)
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illite (1)
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Primary terms
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carbon
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C-13/C-12 (1)
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Cenozoic
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Quaternary
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Holocene
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upper Holocene (2)
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-
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Tertiary
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Neogene
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Miocene (1)
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Paleogene
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Eocene
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upper Eocene (1)
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Oligocene
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lower Oligocene
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Rupelian (1)
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chemical analysis (1)
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clay mineralogy (1)
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climate change (1)
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crystal chemistry (1)
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data processing (1)
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deformation (2)
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diagenesis (1)
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Europe
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Alps
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Eastern Alps
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Northern Limestone Alps (1)
-
-
Limestone Alps
-
Northern Limestone Alps (1)
-
-
North Austrian Alps (1)
-
Prealps (2)
-
-
Central Europe
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Austria
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Burgenland Austria (1)
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Lower Austria
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Vienna Austria (1)
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North Austrian Alps (1)
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North Austrian Molasse (2)
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Salzkammergut (2)
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Styria Austria (1)
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Tyrol Austria (1)
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Upper Austria
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Gosau Austria (2)
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-
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Bohemian Massif (3)
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Molasse Basin
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North Austrian Molasse (2)
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Northern Limestone Alps (1)
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Variscides (1)
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faults (1)
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geochemistry (1)
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geomorphology (1)
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geophysical methods (1)
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igneous rocks
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plutonic rocks
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granites (1)
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intrusions (1)
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Invertebrata
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Cnidaria
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Anthozoa
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Zoantharia
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Scleractinia (1)
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isotopes
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stable isotopes
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C-13/C-12 (1)
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O-18/O-16 (1)
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magmas (1)
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Mesozoic
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Cretaceous
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Gosau Formation (1)
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Upper Cretaceous
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Santonian (1)
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Senonian (1)
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metals
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iron (1)
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metamorphic rocks
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metasedimentary rocks
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metapelite (1)
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oxygen
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O-18/O-16 (1)
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paleoclimatology (1)
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paleoecology (2)
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palynomorphs
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Dinoflagellata (1)
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petroleum
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natural gas (1)
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Plantae
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algae
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Rhodophyta (1)
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pollution (1)
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sedimentary rocks
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carbonate rocks
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limestone
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algal limestone (1)
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coal (1)
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sedimentary structures
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planar bedding structures
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varves (1)
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sedimentation (1)
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sediments (3)
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spectroscopy (2)
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structural analysis (1)
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weathering (1)
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sedimentary rocks
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sedimentary rocks
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carbonate rocks
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limestone
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algal limestone (1)
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coal (1)
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siliciclastics (1)
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sedimentary structures
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sedimentary structures
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planar bedding structures
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varves (1)
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sediments
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sediments (3)
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siliciclastics (1)
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Upper Austria
Stable oxygen and carbon isotopes of carbonates in lake sediments as a paleoflood proxy
The dinoflagellate cyst Molassedinium bicornutum gen. et sp. nov. from the Oligocene of the North Alpine Foreland Basin, Austria
Abstract Based on existing classifications of caves that often involve descriptive terms, a classification is presented that is based purely on genetic processes. An attribute key is developed that allows the classification of caves by means of cave maps, photographs and reports. This method is applied to a dataset of 6007 caves in a study area in eastern Austria. The area comprises diverse geological units of the Eastern Alps and the southern Bohemian Massif. A total of 94% of the caves could be classified with the surprising result that mechanical weathering and erosion caves are almost as common as solution caves even though the vast majority of caves are developed in carbonate rocks. Field checks confirmed the result and showed that the error is acceptable. The classified caves can also be used as indicator of natural phenomena like gravitational mass movements or vulnerable karst areas by decision-makers non-specialized in cave genesis.