What is the other name for the area at which Ranney Hill, Northwest Territories anomaly  rose?
Ranney Hill, Northwest Territories Ranney Hill (pronounced, 'Ran-ee") is a rock outcrop approximately 10 kilometers north of Yellowknife, the capital city of the Northwest Territories of Canada. At 682 ft / 208 m. high, it is one of three visible outcrops that can be seen north of the city. It is an anomaly rising from the relatively flat Canadian Shield.
Ridge Hill Shelf The Ridge Hill Shelf is a landform that forms part of the foothills of the Darling Scarp, a low escarpment that runs parallel with the west coast in southwest Western Australia. It was formed by coastal erosion of the scarp in the Pleistocene, when the sea level was higher, and the scarp located further west than at present. The action of coastal forces produced sand dunes that subsequently lithified into eolianite, and eroded the ironstone of the scarp, resulting in an iron-rich sandstone with a laterite cap. The iron gives the sandstone a dull purple-brown colour; depending on the extent of iron-enrichment, the sandstone may appear predominantly yellow, predominantly purple-brown, or a mottled combination of the two.