Classifier Instance:

Anchor text: Yamuna
Target Entity: Yamuna
Preceding Context: The wide river bed (paleo-channel) of the Ghaggar river suggest that the river once flowed full of water during the great meltdown of the Himalayan Ice Age glaciers, some 10,000 years ago, and that it then continued through the entire region, in the presently dry channel of the Hakra River, possibly emptying into the Rann of Kutch. It supposedly dried up due to the capture of its tributaries by the Indus system and the
Succeeding Context: river, and later on, additionally, the loss of water in much of its catchment area due to deforestation and overgrazing.
Paragraph Title: Ghaggar-Hakra River
Source Page: Sarasvati River

Ground Truth Types:

Predicted Types:

Type	Confidence	Decision
wordnet_artifact_100021939	-2.2218906995267016	0
wordnet_event_100029378	-2.4615376260021296	0
wordnet_organization_108008335	-3.0912729368837337	0
wordnet_person_100007846	-1.6854524390214896	0
yagoGeoEntity	1.4795286209595397	1
wordnet_location_100027167	-3.0980499040432825	0
wordnet_structure_104341686	-1.8658785288741524	0
wordnet_facility_103315023	-1.9310097529799015	0
wordnet_body_of_water_109225146	2.8976494453294164	1
wordnet_stream_109448361	1.7982022099125539	1
wordnet_river_109411430	1.3786248437125062	1
wordnet_lake_109328904	-1.5191997208332892	0
wordnet_bay_109215664	-1.7052186438873695	0
wordnet_geological_formation_109287968	-2.680207700163239	0
wordnet_way_104564698	-2.257898659935563	0
wordnet_land_109334396	-2.8218994294686746	0