Classifier Instance:

Anchor text: North Sea
Target Entity: North_Sea
Preceding Context: Prior to the last Ice Age, the River Thames followed a more northerly route to the
Succeeding Context: , 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 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:

Predicted Types:

Type	Confidence	Decision
wordnet_artifact_100021939	-0.8751504434351046	0
wordnet_event_100029378	-2.493240925300395	0
wordnet_organization_108008335	-3.2562872099086926	0
wordnet_person_100007846	-3.1098813122242737	0
yagoGeoEntity	1.4026387131455966	1
wordnet_location_100027167	-1.0495083889294605	0
wordnet_structure_104341686	-1.1456129042598284	0
wordnet_facility_103315023	-3.310769909849874	0
wordnet_body_of_water_109225146	1.4442459447185676	1
wordnet_stream_109448361	-1.0006430869900103	0
wordnet_lake_109328904	-1.1072560557611664	0
wordnet_bay_109215664	-1.4535507565671866	0
wordnet_geological_formation_109287968	-2.6439267593638216	0
wordnet_way_104564698	-2.424390393989723	0
wordnet_land_109334396	-0.9477130130849591	0