Classifier Instance:

Anchor text: ripples
Target Entity: Ripple_marks
Preceding Context: Uluru is dominantly composed of coarse-grained arkose (a type of sandstone characterized by an abundance of feldspar) and some conglomerate. Average composition is 50% feldspar, 25–35% quartz and up to 25% rock fragments; most feldspar is K-feldspar with only minor plagioclase as subrounded grains and highly altered inclusions within K-feldspar. The grains are typically in diameter, and are angular to subangular; the finer sandstone is well sorted, with sorting decreasing with increasing grain size. The rock fragments include subrounded basalt, invariably replaced to various degrees by chlorite and epidote. The minerals present suggest derivation from a predominantly granite source, similar to the Musgrave Block exposed to the south. When relatively fresh, the rock has a grey colour, but weathering of iron-bearing minerals by the process of oxidation gives the outer surface layer of rock a red-brown rusty colour. Features related to deposition of the sediment include cross-bedding and
Succeeding Context: , analysis of which indicated deposition from broad shallow high energy fluvial channels and sheet flooding, typical of alluvial fans.
Paragraph Title: Composition
Source Page: Uluru

Ground Truth Types:

Predicted Types:

Type	Confidence	Decision
wordnet_artifact_100021939	-0.04686500450620527	0
wordnet_event_100029378	-0.7779093990210906	0
wordnet_organization_108008335	-3.047328497183017	0
wordnet_person_100007846	-2.560569369030027	0
yagoGeoEntity	-0.28124256776497786	0