Classifier Instance:

Anchor text: Paya Terubong
Target Entity: Paya_Terubong
Preceding Context: There are three main geological formations in Penang, i.e. the orthoclase to intermediate microcline granite, microcline granite, and the Mahang formation (mainly ferruginous spotted slate). Penang Island has no sedimentary rocks and most of the island is underlain by igneous rocks which are granites in the IUGS or Streckeisen classification. On the basis of proportions of alkali feldspar to total feldspar, granites on Penang island are further distinguished into two main groups: the North Penang Pluton (approximately north of latitude 5° 23'), and the South Penang Pluton. The former group is subdivided into the Ferringhi Granite, the Tanjung Bungah Granite and the Muka Head Microgranite, whereas the latter is subdivided into the Batu Maung Granite and the Sungai Ara Granite. A study of three disparate locations on the island show that the soil profile in Batu Ferringhi (of early Jurassic age) is silty whereas those in
Succeeding Context: (early Permian – late Carboniferous) and Tanjung Bungah (early ) are clayey.
Paragraph Title: Geology
Source Page: Penang

Ground Truth Types:

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Predicted Types:

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