http://dbpedia.org/ontology/abstract
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The geology of Liechtenstein formed at the … The geology of Liechtenstein formed at the intersection of the Eastern and Western Alps and the country occupies a wider than average river valley on the Rhine River, running north–south. A spur of the flanks the river to the east, while Schellenberg hill is a defining topographic high in the north. a defining topographic high in the north.
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2210
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1070463406
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http://dbpedia.org/resource/Maastrichtian +
, http://dbpedia.org/resource/Nappe +
, http://dbpedia.org/resource/Holocene +
, http://dbpedia.org/resource/Turbidite +
, http://dbpedia.org/resource/Shale +
, http://dbpedia.org/resource/Rhine_River +
, http://dbpedia.org/resource/Foraminifera +
, http://dbpedia.org/resource/Paleocene +
, http://dbpedia.org/resource/Early_Cretaceous +
, http://dbpedia.org/resource/Jurassic +
, http://dbpedia.org/resource/Liechtenstein +
, http://dbpedia.org/resource/Anticline +
, http://dbpedia.org/resource/Ratikon_Mountains +
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http://www.w3.org/ns/prov#wasDerivedFrom
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http://en.wikipedia.org/wiki/Geology_of_Liechtenstein?oldid=1070463406&ns=0 +
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http://en.wikipedia.org/wiki/Geology_of_Liechtenstein +
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, http://dbpedia.org/resource/Geology_of_Liechtenstein +
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rdfs:comment |
The geology of Liechtenstein formed at the … The geology of Liechtenstein formed at the intersection of the Eastern and Western Alps and the country occupies a wider than average river valley on the Rhine River, running north–south. A spur of the flanks the river to the east, while Schellenberg hill is a defining topographic high in the north. a defining topographic high in the north.
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rdfs:label |
Geology of Liechtenstein
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