Classifier Instance:

Anchor text: Channeled Scablands
Target Entity: Channeled_Scablands
Preceding Context: However, a new study by Gupta et al. (2007) suggests that the English Channel was formed by erosion caused by two major floods. The first was about 425 000 years ago, when an ice-dammed lake in the southern North Sea overflowed and broke the Weald-Artois chalk range in a catastrophic erosion and flood event. Afterwards, the Thames and Scheldt flowed through the gap into the English Channel, but the Meuse and Rhine still flowed northwards. In a second flood about 225 000 years ago the Meuse and Rhine were ice-dammed into a lake that broke catastrophically through a high weak barrier (perhaps chalk, or an end-moraine left by the ice sheet). Both floods cut massive flood channels in the dry bed of the English Channel, somewhat like the
Succeeding Context: or the Wabash river in the USA.
Paragraph Title: null
Source Page: Strait of Dover

Ground Truth Types:

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