Classifier Instance:

Anchor text: North Sea
Target Entity: North_Sea
Preceding Context: At the end of the most recent glacial period, known in Britain as the Devensian, ten thousand years ago, Britain and continental Europe were joined by the ridge between Friesland and Norfolk. The topography of the bed of the
Succeeding Context: indicates that the rivers of the southern part of eastern England flowed into the Rhine, hence through the English Channel. From the Fens northward along the modern coast, the drainage flowed into the northern North Sea basin. As the ice melted, the rising sea level drowned the lower lands, leading ultimately to the present coastline.
Paragraph Title: Formation and geography
Source Page: The Fens

Ground Truth Types:

Predicted Types:

Type	Confidence	Decision
wordnet_artifact_100021939	-1.5020844267208735	0
wordnet_event_100029378	-3.0531696954575387	0
wordnet_organization_108008335	-3.316632276981709	0
wordnet_person_100007846	-3.013984863917335	0
yagoGeoEntity	2.023694404137616	1
wordnet_location_100027167	-0.9123437529281909	0
wordnet_structure_104341686	-1.4762203967070935	0
wordnet_facility_103315023	-3.4233516602192577	0
wordnet_body_of_water_109225146	2.4276784743229376	1
wordnet_stream_109448361	-0.8391236562435607	0
wordnet_lake_109328904	-1.4261319909474997	0
wordnet_bay_109215664	-1.2288923193563535	0
wordnet_geological_formation_109287968	-2.181862147178835	0
wordnet_way_104564698	-2.9855343402396133	0
wordnet_land_109334396	-1.2256608193647462	0