What is the other name for the area at which Ranney Hill, Northwest Territories anomaly  rose?
Canadian Shield The Canadian Shield, also called the Laurentian Plateau, or "Bouclier canadien " (French), is a large area of exposed Precambrian igneous and high-grade metamorphic rocks (geological shield) that forms the ancient geological core of the North American continent (the North American Craton or Laurentia). Composed of igneous rock resulting from its long volcanic history, the area is covered by a thin layer of soil. With a deep, common, joined bedrock region in eastern and central Canada, it stretches north from the Great Lakes to the Arctic Ocean, covering over half of Canada; it also extends south into the northern reaches of the United States. Human population is sparse, and industrial development is minimal, while mining is prevalent.
Drune Hill Drune Hill ( ) is a rounded flat topped mountain rising to about 680 m , and located about 0.5 nautical miles (1 km) north of Khufu Peak, separated from it by Khufu Corrie, and about 0.5 nautical miles northeast of Pearce Dome, situated on the east coast of Alexander Island, Antarctica. The name is used by those working in the area, however, the origin of the name remains unknown.