Classifier Instance:

Anchor text: English Channel
Target Entity: English_Channel
Preceding Context: The Rhine flowed northwards into the North Sea as the sea level fell during the start of the first of the Pleistocene Ice Ages. The ice created a dam from Scandinavia to Scotland, and the Rhine, combined with the Thames and drainage from much of north Europe, created a vast lake behind the dam, which eventually spilled over the Weald into the
Succeeding Context: . This overflow channel was gradually widened and deepened into the Strait of Dover. A narrow deeper channel along the middle of the strait was the bed of the Rhine in the last Ice Age. In East Anglia there is a geological deposit that marks the old preglacial northward course of the Rhine.
Paragraph Title: Geological formation
Source Page: Strait of Dover

Ground Truth Types:

Predicted Types:

Type	Confidence	Decision
wordnet_artifact_100021939	-1.8722923938830307	0
wordnet_event_100029378	-2.4311441123980986	0
wordnet_organization_108008335	-2.1436179590598923	0
wordnet_person_100007846	-1.9128402338080601	0
yagoGeoEntity	1.9910584158798863	1
wordnet_location_100027167	-1.9866085746978224	0
wordnet_structure_104341686	-1.741597773761671	0
wordnet_facility_103315023	-2.417110929230633	0
wordnet_body_of_water_109225146	2.341406953776512	1
wordnet_stream_109448361	-1.4449713652657843	0
wordnet_lake_109328904	-1.1147589185979705	0
wordnet_bay_109215664	-1.429612144512222	0
wordnet_geological_formation_109287968	-1.479662849822472	0
wordnet_way_104564698	-2.052554754054839	0
wordnet_land_109334396	-1.6210895106481353	0