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| GEOLOGY
OF RED HILL
The red soil of Red Hill is the
result of weathering of a rock called hornfels. Hornfels is a metamorphosed sedimentary
rock. The molten volcanic rock intrusion which provided the heat to metamorphose
the hornfels lies under the golf course. Good places to take a closer look at
the hornfels are: between the summit restaurant and the golf course access road,
and in the old quarry 50m south of the restaurant. 
Hornsfel
rock near summit restaurant, showing banding More information
about the geology of Red Hill can be found at Wikipedia. |