Classifier Instance:

Anchor text: Dollis Brook
Target Entity: Dollis_Brook
Preceding Context: Finchley is situated on a plateau, 90 metres (300 ft) above sea level about north of Charing Cross and about south of Barnet. To the west is the Dollis valley formed by
Succeeding Context: which is the natural western boundary of Finchley. Mutton Brook forms the southern boundary, joining the Dollis Brook to become the River Brent. Geologically, Finchley is formed of three layers. Most of Finchley is on Boulder clay or glacial moraine, skirted by a layer of gravel, then the underlying layer of London clay. This roughly triangular gravel line was the most fertile area, hamlets grew at the three corners, which evolved into Finchley's early population centres corresponding to the three town centres in the area:
Paragraph Title: Geography
Source Page: Finchley

Ground Truth Types:

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|  |  |  |---wordnet_stream_109448361
|  |  |  |  |---wordnet_river_109411430

Predicted Types:

TypeConfidenceDecision
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wordnet_event_100029378-1.794336346027714 0
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yagoGeoEntity0.8687372675084283 1
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wordnet_structure_104341686-1.544911349806831 0
wordnet_facility_103315023-2.347216872957248 0
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wordnet_lake_109328904-1.5044867979238268 0
wordnet_bay_109215664-1.2167551756595525 0
wordnet_geological_formation_109287968-1.8438181683190278 0
wordnet_way_104564698-2.2600539740508228 0
wordnet_land_109334396-1.6647661540369014 0
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|  |  |  |---wordnet_lake_109328904
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