Classifier Instance:

Anchor text: Byfleet
Target Entity: Byfleet
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 Suffolk-Essex border. During this period, the Mole is thought to have merged with the River Wey near
Succeeding Context: 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:

|---wordnet_entity_100001740
|  |---wordnet_entity_100001740_rest

Predicted Types:

TypeConfidenceDecision
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wordnet_land_109334396-1.0802641057277398 0
|---wordnet_entity_100001740
|  |---wordnet_artifact_100021939
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|  |  |---wordnet_way_104564698
|  |---wordnet_event_100029378
|  |---wordnet_organization_108008335
|  |---wordnet_person_100007846
|  |---yagoGeoEntity
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|  |  |  |  |---wordnet_geographical_area_108574314
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|  |  |---wordnet_structure_104341686
|  |  |---wordnet_facility_103315023
|  |  |---wordnet_body_of_water_109225146
|  |  |---wordnet_geological_formation_109287968
|  |  |---wordnet_way_104564698
|  |  |---wordnet_land_109334396