Classifier Instance:

Anchor text: Great Britain
Target Entity: Great_Britain
Preceding Context: The strait is believed to have been created through erosion. At one time there was land where the strait is now, a south-east extension of the Weald joining what is now
Succeeding Context: to continental Europe. The eastern end of this old longer Weald is the Boulonnais chalk area in the Pas de Calais. The predominant geology on both the British and French sides and on the sea floor between is chalk. Although somewhat resistant to erosion, such erosion of the chalk can be seen on both coasts as impressive sea cliffs, the famous white cliffs of Dover, and Cap Blanc Nez on the French side of the strait. This same rock provided an excellent tunnelling medium for the Channel Tunnel.
Paragraph Title: Geological formation
Source Page: Strait of Dover

Ground Truth Types:

Predicted Types:

Type	Confidence	Decision
wordnet_artifact_100021939	-1.2687026385819653	0
wordnet_event_100029378	-2.540342813643759	0
wordnet_organization_108008335	-1.0735776036325337	0
wordnet_person_100007846	-2.634467488995077	0
yagoGeoEntity	2.519378050179191	1
wordnet_location_100027167	-0.7265847202686269	0
wordnet_structure_104341686	-3.2789083570648647	0
wordnet_facility_103315023	-1.4466639390133191	0
wordnet_body_of_water_109225146	-3.054929122718888	0
wordnet_geological_formation_109287968	-3.081587374017917	0
wordnet_way_104564698	-2.7852055660832806	0
wordnet_land_109334396	-0.018439163450277386	0