Classifier Instance:

Anchor text: Lake Lewis
Target Entity: Lake_Lewis
Preceding Context: The floodwaters rushed across eastern Washington, creating the channeled scablands, which are a complex network of dry canyon-like channels, or coulees that are often braided and sharply gouged into the basalt rock underlying the region's deep topsoil. Numerous flat-topped buttes with rich soil stand high above the chaotic scablands. Constrictions at several places caused the floodwaters to pool into large temporary lakes, such as
Succeeding Context: , in which sediments were deposited. Water depths have been estimated at at Wallula Gap, at Bonneville Dam, and over modern Portland, Oregon. Sediments were also deposited when the floodwaters slowed in the broad flats of the Quincy, Othello, and Pasco Basins. The floods' periodic inundation of the lower deposited rich sediments; 21st-century farmers in the Willamette Valley "plow fields of fertile Montana soil and clays from Washington's Palouse".
Paragraph Title: null
Source Page: Columbia River

Ground Truth Types:

Predicted Types:

Type	Confidence	Decision
wordnet_artifact_100021939	-1.9368797887823859	0
wordnet_event_100029378	-2.927179206239473	0
wordnet_organization_108008335	-2.736101561044167	0
wordnet_person_100007846	-1.1635688937536064	0
yagoGeoEntity	1.0185768887984792	1
wordnet_location_100027167	-2.2285001197784875	0
wordnet_structure_104341686	-1.7629809868556678	0
wordnet_facility_103315023	-1.3608946048111732	0
wordnet_body_of_water_109225146	1.5043131448544877	1
wordnet_stream_109448361	-1.5553075749002154	0
wordnet_lake_109328904	1.3545930766056993	1
wordnet_bay_109215664	-1.353813173357467	0
wordnet_geological_formation_109287968	-1.89956939609329	0
wordnet_way_104564698	-2.1679906778280706	0
wordnet_land_109334396	-1.6171271173148631	0