Classifier Instance:

Anchor text: Chorleywood
Target Entity: Chorleywood
Preceding Context: Prior to the last Ice Age, the River Thames followed a more northerly route to the North Sea, from Reading via Marlow,
Succeeding Context: , St Albans, Hertford and along the present Suffolk-Essex border. During this period, the Mole is thought to have merged with the River Wey near Byfleet and then flowed in a north-easterly direction via Richmond to meet the proto-Thames near Ware in Hertfordshire. (Today the Mole and Wey are less than apart at their closest point south of Esher.) During the mid-Pleistocene period (500 000 years before present), a large ice sheet built up across much of the East of England, reaching as far south as St Albans and Chelmsford, blocking the path of the proto-Thames. Glacial meltwater from the Anglian ice sheet, caused the Thames to divert southwards into the valley of the Mole-Wey river, thus adopting its present route through London.
Paragraph Title: Lower Mole
Source Page: River Mole

Ground Truth Types:

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Predicted Types:

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