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.
Worswick Hill Worswick Hill ( ) is a rounded summit, 36 km, at the west end of Brisbane Heights on Coronation Island, in the South Orkney Islands. The peak appears on some early charts of the South Orkney Islands but is not accurately located. It was roughly surveyed by DI personnel in 1933 and resurveyed by the Falkland Islands Dependencies Survey (FIDS) in 1948-49. Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) for Robert F. Worswick of the FIDS, meteorologist at Signy Island in 1950 and 1951, who reached this hill during a sledge journey in 1950.