Classifier Instance:

Anchor text: Rhenish Massif
Target Entity: Rhenish_Massif
Preceding Context: Wetzlar lies on the eastern edge of the
Succeeding Context: . The substrate consists of geologically young sediments of the Lahn and much older Devonian and Carboniferous rocks of the two main geological units of the Massif, the Lahnmulde and the so-called Giessen nappe. The northwestern part of the urban area lies on the Lahntal silt, sand and gravel, which have only slightly hardened. They were deposited by the river Lahn, at a point where its valley (which is still up to one kilometre wide) to the west becomes increasingly narrow and deep. The main part of the city is built on in part intensively folded, faulted and slated layers of shales, sandstone, quartzite and limestone. They were deposited in the Devonian and Carboniferous eras in a sea characterised by island chains, volcanoes and atolls that were pushed together and covered by a layer of rock that had been transported from another location during the Variscan orogeny period of mountain building. The marine sedimentary rocks which resulted from this tectonic action now give the town its character as they were often used for building material.
Paragraph Title: Geology
Source Page: Wetzlar

Ground Truth Types:

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|  |  |  |  |---wordnet_mountain_109359803
|  |  |  |  |---wordnet_hill_109303008

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