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.
Churchill Craton The Churchill Craton is the northwest section of the Canadian Shield and stretches from southern Saskatchewan and Alberta to northern Nunavut. It has a very complex geological history punctuated by at least seven distinct regional tectonometamorphic intervals, including many discrete accretionary magmatic events. The Western Churchill province is the part of the Churchill Craton that is exposed north and west of the Hudson Bay. The Archean (ca. 1.83 Ga) Western Churchill province contributes to the complicated and protracted tectonic history of the craton, and marks a major change in the behaviour of the Churchill Craton with many remnants of Archean supracrustal and granitoid rocks.