Classifier Instance:

Anchor text: Rhine
Target Entity: Rhine
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 English Channel. 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
Succeeding Context: 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	-1.4077167547226446	0
wordnet_event_100029378	-1.513605355407561	0
wordnet_organization_108008335	-3.9596600501197132	0
wordnet_person_100007846	-2.416779374265137	0
yagoGeoEntity	2.125319641135841	1
wordnet_location_100027167	-1.2052333692005488	0
wordnet_structure_104341686	-1.1557880010458939	0
wordnet_facility_103315023	-3.2648753908509582	0
wordnet_body_of_water_109225146	1.7092292522494152	1
wordnet_stream_109448361	1.1556540209255888	1
wordnet_river_109411430	1.3404106841474044	1
wordnet_lake_109328904	-2.11194457554318	0
wordnet_bay_109215664	-2.02490665666161	0
wordnet_geological_formation_109287968	1.44141737109928	1
wordnet_beach_109217230	-1.6967077414968421	0
wordnet_natural_depression_109366017	1.1243339942526196	1
wordnet_valley_109468604	1.1104352154986787	1
wordnet_natural_elevation_109366317	-1.535193829939254	0
wordnet_volcanic_crater_109472413	-1.6721931172090034	0
wordnet_range_109403734	-1.7818032467063227	0
wordnet_way_104564698	-3.872380660597841	0
wordnet_land_109334396	-3.100001578362566	0