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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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Central Europe
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Bohemian Massif (4)
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Czech Republic
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Bohemia
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Prague Basin (1)
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Czech Sudeten Mountains (1)
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Germany
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Bavaria Germany (1)
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Thuringia Germany (1)
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Poland
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Dolnoslaskie Poland (1)
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Lower Silesia (1)
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Polish Sudeten Mountains (3)
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Sudeten Mountains
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Czech Sudeten Mountains (1)
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Izera Mountains (3)
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Karkonosze Mountains (13)
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Polish Sudeten Mountains (3)
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Variscides (2)
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commodities
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metal ores
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polymetallic ores (1)
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elements, isotopes
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hydrogen (1)
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incompatible elements (1)
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metals
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alkali metals
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potassium (1)
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copper (1)
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rare earths (2)
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silver (1)
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thallium (1)
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Invertebrata (1)
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Precambrian (1)
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Saxothuringian (1)
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igneous rocks
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igneous rocks
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plutonic rocks
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granites (6)
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granodiorites (1)
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pegmatite (1)
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metamorphic rocks
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metamorphic rocks
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amphibolites (2)
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orthosilicates
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nesosilicates
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sulfates
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sulfides
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aikinite (2)
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chalcopyrite (1)
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joseite (1)
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stannoidite (1)
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tetradymite (1)
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sulfosalts
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sulfantimonites
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bournonite (1)
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freibergite (1)
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tetrahedrite (1)
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sulfarsenites
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tennantite (1)
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sulfobismuthites
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berryite (1)
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emplectite (1)
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gustavite (1)
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matildite (1)
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wittichenite (1)
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tellurides
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joseite (1)
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tetradymite (1)
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Primary terms
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absolute age (1)
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associations (1)
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Cenozoic
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Quaternary
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Holocene
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upper Holocene (1)
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crystal chemistry (4)
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crystal growth (1)
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crystal structure (3)
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deformation (1)
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Europe
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Central Europe
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Bohemian Massif (4)
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Czech Republic
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Bohemia
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Prague Basin (1)
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Czech Sudeten Mountains (1)
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Germany
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Bavaria Germany (1)
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Thuringia Germany (1)
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Poland
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Dolnoslaskie Poland (1)
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Lower Silesia (1)
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Polish Sudeten Mountains (3)
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Sudeten Mountains
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Czech Sudeten Mountains (1)
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Izera Mountains (3)
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Karkonosze Mountains (13)
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Polish Sudeten Mountains (3)
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Variscides (2)
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foliation (1)
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geochemistry (1)
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geomorphology (1)
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glacial geology (1)
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Graptolithina (1)
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hydrogen (1)
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igneous rocks
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plutonic rocks
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granites (6)
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granodiorites (1)
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pegmatite (1)
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inclusions (1)
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intrusions (3)
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Invertebrata (1)
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magmas (3)
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metal ores
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polymetallic ores (1)
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metals
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alkali metals
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potassium (1)
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copper (1)
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rare earths (2)
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silver (1)
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thallium (1)
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metamorphic rocks
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amphibolites (2)
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metaigneous rocks
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metabasite (2)
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metasedimentary rocks
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metapelite (1)
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mylonites (1)
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schists
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blueschist (1)
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metamorphism (2)
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mineralogy (1)
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paleoclimatology (1)
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Paleozoic
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Cambrian
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Upper Cambrian (1)
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Carboniferous
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Upper Carboniferous (1)
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Ordovician
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Upper Ordovician
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Ashgillian (1)
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Hirnantian (1)
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Silurian
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Lower Silurian (1)
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phase equilibria (1)
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Precambrian (1)
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sea-level changes (1)
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sedimentary rocks
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clastic rocks
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black shale (1)
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diamictite (1)
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sedimentation (1)
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stratigraphy (1)
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tectonics (1)
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thermal analysis (1)
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weathering (1)
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sedimentary rocks
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sedimentary rocks
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clastic rocks
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black shale (1)
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diamictite (1)
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volcaniclastics (1)
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sediments
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volcaniclastics (1)
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Karkonosze Mountains
Oxy-dravite from Wołowa Góra Mountain, Karkonosze massif, SW Poland: Crystallochemical and structural studies
Pressure–temperature estimates of the blueschists from the Kopina Mt., northern Bohemian Massif, Poland – constraints on subduction of the Saxothuringian continental margin
Rediscovering geoheritage, reinventing geotourism: 200 years of experience from the Sudetes, Central Europe
Abstract The Sudetes is a mountain range in Central Europe and an area of remarkable geodiversity. In recent years, the area has been promoted as a geotourist destination and various initiatives aimed at better understanding geoheritage have been implemented. An interest in scenic landscapes is not new however, and dates back to the end of the eighteenth century. Two areas within the Sudetes are cradles of local nature-based tourism. These are the granite massif of the Karkonosze in the west and the sandstone stepped plateau of Broumov Highland and Stołowe Mountains in the central part of the Sudetes. In both, physical access to the key geosites was provided as early as in the nineteenth century, while an interpretation component was added in the early twentieth century. A side-effect of political change following the end of World War II was the neglect and dilapidation of many sites, as well as the disappearance of geoheritage appreciation from the collective social memory. In the last decade many of those early achievements were rediscovered and provided the foundations for contemporary activities. An educational component based on modern science is now included in the features which were discovered as tourist attractions long ago.