Classifier Instance:

Anchor text: Suffolk
Target Entity: Suffolk
Preceding Context: Prior to the last Ice Age, the River Thames followed a more northerly route to the North Sea, from Reading via Marlow, Chorleywood, St Albans, Hertford and along the present
Succeeding Context: -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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|  |  |  |  |---wordnet_county_108546183

Predicted Types:

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yagoGeoEntity1.2957466899793242 1
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wordnet_structure_104341686-4.525517805467995 0
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wordnet_way_104564698-1.064368210790189 0
wordnet_land_109334396-3.88698572300861 0
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