Classifier Instance:

Anchor text: Bristol Channel
Target Entity: Bristol_Channel
Preceding Context: The yellow-grey cliffs on the Glamorgan Heritage Coast (which stretches between Llantwit Major to Ogmore-by-Sea) are unique on the Celtic Sea coastline (i.e. Cornwall, Wales, Ireland and Brittany) as they are formed of a combination of liassic limestone, shale and carboniferous sandstone/limestone. They were allegedly formed 200 million years ago when Wales (as well as Cornwall, Brittany and Ireland) lay underneath a warm, shallow, equatorial sea during the beginning of the Jurassic age. Today the cliffs contain elements of Jurassic age sea-creatures (although not land dinosaurs – what is now the Celtic Sea coastline was underneath the sea), such as ammonites. The stratification of overlapping shale, sandstone and limestone was caused by a geological upheaval known as the Variscan orogeny, which literally pushed the cliffs out of the sea, contorting them as they did so. (This stratification can also be found on other parts of the Celtic seaboard, such as Bude in Cornwall, across the
Succeeding Context: ). As the cliffs and land contain elements of calcium carbonate found in the limestone, it allows farmers in the vale to grow crops which would be difficult elsewhere in Wales or the West country, such as Devon and Cornwall (whose soil is predominantly acidic as most of the west country is made of poor quality Devonian soils). The liassic limestone and carboniferous sandstone is also used in the vale for building materials; in previous centuries it was taken by sloops across the Bristol Channel to north Cornish ports such as Bude, Boscastle and Port Isaac to fertilise Cornwall's poor slate soils for the farming communities; while the hard Devonian slate of Cornwall was brought back as a roofing material for houses in the Vale.
Paragraph Title: Geography
Source Page: Vale of Glamorgan

Ground Truth Types:

Predicted Types:

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