Classifier Instance:

Anchor text: Olympic Peninsula
Target Entity: Olympic_Peninsula
Preceding Context: As the Vashon glacier receded a series of proglacial lakes formed, filling the main trough of Puget Sound and inundating the southern lowlands. Glacial Lake Russell was the first such large recessional lake. From the vicinity of Seattle in the north the lake extended south to the Black Hills, where it drained south into the Chehalis River. Sediments from Lake Russell form the blue-gray clay identified as the Lawton Clay. The second major recessional lake was Glacial Lake Bretz. It also drained to the Chehalis River until the Chimacum Valley, in the northeast
Succeeding Context: , melted, allowing the lake's water to rapidly drain north into the marine waters of the Strait of Juan de Fuca, which was rising as the ice sheet retreated.
Paragraph Title: null
Source Page: Puget Sound

Ground Truth Types:

Predicted Types:

Type	Confidence	Decision
wordnet_artifact_100021939	-2.1849921465633217	0
wordnet_event_100029378	-2.022183121512702	0
wordnet_organization_108008335	-2.9010707070510047	0
wordnet_person_100007846	-2.6686046538450365	0
yagoGeoEntity	1.9396053467219447	1
wordnet_location_100027167	-2.270955405659942	0
wordnet_structure_104341686	-2.4434955418393955	0
wordnet_facility_103315023	-1.9595059549624925	0
wordnet_body_of_water_109225146	-0.14193128031183702	0
wordnet_geological_formation_109287968	-1.8275528206553426	0
wordnet_way_104564698	-2.227890687870009	0
wordnet_land_109334396	1.7097680889590883	1
wordnet_island_109316454	-1.4051008962602511	0