Classifier Instance:

Anchor text: Great Dividing Range
Target Entity: Great_Dividing_Range
Preceding Context: Australia has moved northwards at a rate of per year, starting during the Cainozoic. Eastern Australia experienced a period of tectonic uplift, which moved the drainage divide in Queensland inland. Also during this time, Queensland experienced volcanic eruptions leading to central and shield volcanoes and basalt flows. Some of these granitic outcrops have become high islands. After the Coral Sea Basin formed, coral reefs began to grow in the Basin, but until about 25 million years ago, northern Queensland was still in temperate waters south of the tropics—too cool to support coral growth. The Great Barrier Reef's development history is complex; after Queensland drifted into tropical waters, it was largely influenced by reef growth and decline as sea level changed. Reefs can increase in diameter by per year, and grow vertically anywhere from per year; however, they grow only above a depth of due to their need for sunlight, and cannot grow above sea level. When Queensland edged into tropical waters 24 million years ago, some coral grew, but a sedimentation regime quickly developed with erosion of the
Succeeding Context: ; creating river deltas, oozes and turbidites, unsuitable conditions for coral growth. 10 million years ago, the sea level significantly lowered, which further enabled sedimentation. The reef's substrate may have needed to build up from the sediment until its edge was too far away for suspended sediments to inhibit coral growth. In addition, approximately 400,000 years ago there was a particularly warm interglacial period with higher sea levels and a water temperature change.
Paragraph Title: Geology and geography
Source Page: Great Barrier Reef

Ground Truth Types:

Predicted Types:

Type	Confidence	Decision
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