Classifier Instance:

Anchor text: Friesland
Target Entity: Friesland
Preceding Context: At the end of the most recent glacial period, known in Britain as the Devensian, ten thousand years ago, Britain and continental Europe were joined by the ridge between
Succeeding Context: and Norfolk. The topography of the bed of the North Sea indicates that the rivers of the southern part of eastern England flowed into the Rhine, hence through the English Channel. From the Fens northward along the modern coast, the drainage flowed into the northern North Sea basin. As the ice melted, the rising sea level drowned the lower lands, leading ultimately to the present coastline.
Paragraph Title: Formation and geography
Source Page: The Fens

Ground Truth Types:

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