Classifier Instance:

Anchor text: Escher von der Linth
Target Entity: Arnold_Escher_von_der_Linth
Preceding Context: On the south side, the massif of the Tödi is mainly composed of gneiss, which, according to
Succeeding Context: , overlies a pioritic granite with large felspar crystals. The summit and the northern flank are mainly composed of metamorphic slate, in which talc predominates, but is sometimes replaced by felspar, so that the rock sometimes approaches the condition of gneiss and sometimes that of mica slate. There are manifest traces of anthracite, especially at the Bifertengrätli, where the rock in some places assumes the appearance of a quartzite mixed with fragment of talc, which has elsewhere in this region been referred to the Verrucano. To these strata succeed dolomite and Jurassic limestone, similar in character to those developed on a large scale in the canton of Glarus.
Paragraph Title: Geology
Source Page: Tödi

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