Classifier Instance:

Anchor text: Baja California
Target Entity: Baja_California
Preceding Context: Prior to channelization of the lower Colorado in the 20th century, the river was characterized by sweeping meanders, sandbars and islands that were subject to frequent course changes. Joseph C. Ives, who surveyed the lower river in 1861, wrote that "the shifting of the channel, the banks, the islands, the bars is so continual and rapid that a detailed description, derived from the experiences of one trip, would be found incorrect, not only during the subsequent year, but perhaps in the course of a week, or even a day." The delta and estuary of the Colorado River were once also subjected to a major tidal bore that has almost disappeared with reductions in river flow and some dredging of the estuary channel. The first historical record of the tidal bore was that made by the Croatian missionary in Spanish service Father Ferdinand Konščak on 18 July 1746. During spring tide conditions, the tidal bore formed in the estuary about Montague Island in
Succeeding Context: and propagated upstream. It was locally called El Burro or burro.
Paragraph Title: null
Source Page: Colorado River

Ground Truth Types:

Predicted Types:

Type	Confidence	Decision
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wordnet_event_100029378	-2.421079652572112	0
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wordnet_person_100007846	-3.4895139525792955	0
yagoGeoEntity	1.4073374483780206	1
wordnet_location_100027167	0.8589960805307525	1
wordnet_region_108630985	0.7110052979249885	1
wordnet_geographical_area_108574314	0.09397368249080613	1
wordnet_tract_108673395	-2.5336420899892165	0
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wordnet_town_108665504	-0.9731296024250468	0
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wordnet_region_108630039	1.2671917532289603	1
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