In der hohen <placeName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H0005696 https://www.geonames.org/6255148"><choice> <abbr>Europ.</abbr> <expan>Europäischen</expan> </choice></placeName> <placeName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H0002402 https://www.geonames.org/2661786">Alpen</placeName>kette <placeName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H0010179 https://www.geonames.org/2658434">Schweiz</placeName><supplied xmlns="http://www.tei-c.org/ns/1.0" cert="high">,</supplied> <placeName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H0009409 https://www.geonames.org/2763586">Tyrol</placeName>, <placeName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H0009764 https://www.geonames.org/2766824">Salz<lb break="no" />burg</placeName> kom̅t Zinnformation im Granit nicht <lb xmlns="http://www.tei-c.org/ns/1.0" />vor. Sonderbar! <choice xmlns="http://www.tei-c.org/ns/1.0"> <orig>wohl</orig> <reg>Wohl</reg> </choice> aber in <placeName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H0009409 https://www.geonames.org/2763586">Tyrol</placeName> <choice xmlns="http://www.tei-c.org/ns/1.0"> <abbr>u</abbr> <expan>und</expan> </choice> <placeName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H0020511 https://www.geonames.org/2660522">Grau<lb break="no" />bündten</placeName> (laut <persName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H0013680 http://d-nb.info/gnd/117572349">Gruner</persName>) Eisenglimmer <subst xmlns="http://www.tei-c.org/ns/1.0"> <del rendition="#s">wie</del> <lb /> <add place="left">statt</add> </subst> <choice xmlns="http://www.tei-c.org/ns/1.0"> <sic>gemeiner</sic> <corr cert="high">gemeinem</corr> </choice> Glimer als Bestandtheil des Granits <lb xmlns="http://www.tei-c.org/ns/1.0" />vor. Dies Phänomen in <placeName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H0007765 https://www.geonames.org/2859444/upper-palatinate.html">obren Pfalz</placeName>, wo <lb xmlns="http://www.tei-c.org/ns/1.0" />auch ganze Granitmassen von Kobolt durch<lb xmlns="http://www.tei-c.org/ns/1.0" break="no" />drungen erscheinen.