Dieselbe Sandsteinformation ist bei <choice xmlns="http://www.tei-c.org/ns/1.0"> <abbr>d.</abbr> <expan>der</expan> </choice> Stadt <placeName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H0018549 https://www.geonames.org/2658377">Thun</placeName><supplied xmlns="http://www.tei-c.org/ns/1.0" cert="high">,</supplied> die <lb xmlns="http://www.tei-c.org/ns/1.0" />grobkörnigste in der ganzen <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> enthält <choice xmlns="http://www.tei-c.org/ns/1.0"> <abbr>12 zoll.</abbr> <expan>12-zölliges</expan> </choice> <choice xmlns="http://www.tei-c.org/ns/1.0"> <abbr>Kalkst.</abbr> <expan>Kalkstein</expan> </choice><supplied xmlns="http://www.tei-c.org/ns/1.0" cert="high">-</supplied><lb xmlns="http://www.tei-c.org/ns/1.0" break="no" />Geschiebe. Unter diesem Sandstein <choice xmlns="http://www.tei-c.org/ns/1.0"> <abbr>Alpenkalkst.</abbr> <expan>Alpenkalkstein</expan> </choice><supplied xmlns="http://www.tei-c.org/ns/1.0" cert="high">,</supplied> eigene Ab<g xmlns="http://www.tei-c.org/ns/1.0" ref="#typoHyphen" /><lb xmlns="http://www.tei-c.org/ns/1.0" break="no" />änderung<supplied xmlns="http://www.tei-c.org/ns/1.0" cert="high">,</supplied> sehr weiß, <add xmlns="http://www.tei-c.org/ns/1.0" place="superlinear">fast </add>ohne Kalkspattrüm̅er <choice xmlns="http://www.tei-c.org/ns/1.0"> <abbr>u</abbr> <expan>und</expan> </choice> sehr hölig porös. <lb xmlns="http://www.tei-c.org/ns/1.0" /><choice xmlns="http://www.tei-c.org/ns/1.0"> <orig>streicht</orig> <reg>Streicht</reg> </choice> wie <placeName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H0018550 https://www.geonames.org/2658375">Thuner See</placeName> <choice xmlns="http://www.tei-c.org/ns/1.0"> <abbr>St</abbr> <expan>Stunde</expan> </choice> 11 mit 45° <choice xmlns="http://www.tei-c.org/ns/1.0"> <abbr>Oc.</abbr> <expan>Occidens</expan> </choice><supplied xmlns="http://www.tei-c.org/ns/1.0" cert="high">,</supplied> viel und sehr regel<g xmlns="http://www.tei-c.org/ns/1.0" ref="#typoHyphen" /><lb xmlns="http://www.tei-c.org/ns/1.0" break="no" />mäßige Schichten Mergelschiefer darinn. Unter <choice xmlns="http://www.tei-c.org/ns/1.0"> <abbr>Alpenkalkst.</abbr> <expan>Alpenkalkstein</expan> </choice> <lb xmlns="http://www.tei-c.org/ns/1.0" />am <placeName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H1332824 https://www.geonames.org/2661586/beatenberg.html">Beatenberg</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/H0001668 http://www.geonames.org/2659446">Niesen</placeName><note xmlns="http://www.tei-c.org/ns/1.0" place="left" hand="#author"><placeName ref="https://edition-humboldt.de/H0001668 http://www.geonames.org/2659446">Niesen</placeName></note> <hi xmlns="http://www.tei-c.org/ns/1.0" rendition="#u">Flözthonschiefer</hi>. Gyps am <placeName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H0018550 https://www.geonames.org/2658375">Thuner <lb />See</placeName> im <choice xmlns="http://www.tei-c.org/ns/1.0"> <abbr>Alpenkalkst.</abbr> <expan>Alpenkalkstein</expan> </choice><supplied xmlns="http://www.tei-c.org/ns/1.0" cert="high">.</supplied> Aber <placeName xmlns="http://www.tei-c.org/ns/1.0" ref="https://edition-humboldt.de/H0001668 http://www.geonames.org/2659446">Nieser</placeName> Sandstein<supplied xmlns="http://www.tei-c.org/ns/1.0" cert="low">:</supplied> gehört er <lb xmlns="http://www.tei-c.org/ns/1.0" />nicht zur alten Formation, zum Grauwakkengebirge<supplied xmlns="http://www.tei-c.org/ns/1.0" cert="low">?</supplied>