Question: What is the other name for the area at which Ranney Hill, Northwest Territories anomaly  rose? 

full_context: Document 1: Innuitian Mountains: The Innuitian Mountains are a mountain range in Nunavut and the Northwest Territories, Canada . They are part of the Arctic Cordillera and are largely unexplored, due to the hostile climate. They are named after the northern indigenous people, who live in the region. In some locations the Innuitian Mountains measure over 2500 m in height, and 1290 km in length. The highest point is Barbeau Peak at 2616 m . There are no trees or wildlife in the Innuitian Mountains due to the harsh cold climate as well as being located north of the Arctic tree line. This region is mostly barren with vast areas of permafrost. There are metallic mineral resources including iron and zinc and fossil fuel resources such as coal.
Document 2: Claybank Brick Plant: Claybank Brick Plant was a brickworks factory for the manufacturing of bricks from clay located with a quarry for clay on site. The Claybank Brick plant has been conserved as a part of Saskatchewan's industrial heritage with its official announcement June 29, 1997 as a National Historic Site of Canada by Minister of Canadian Heritage Sheila Copps. $2 million for the conservation and presentation of the Brick Plant by Claybank was contributed jointly between Federal and Provincial Government funding departments. Claybank Brick Plant used neighboring clay from the Massold Clay Canyons. The Cretaceous period resulted in the "Whitemud Formation" which is the underlying zone of the Claybank Hills. The Whitemud Formation is noted for two main types of clay; white and grey in colour which possess different properties. Also close to Claybank are the Dirt Hills where a "bentonitic clay" can be found. Therefore, the brick produced is used for different purposes. Claybank Brick Plant is known for its face brick, as well as tiles, fire brick, insulating brick
Document 3: Gahcho Kue Diamond Mine Project: The Gahcho Kué Diamond Mine is located on the Canadian tundra in the Northwest Territories. It is situated at Kennady Lake ( ), in the Akaitcho Treaty 8 Territory AK claim block, which is 85 km southeast of the Snap Lake Diamond Mine and approximately 280 km east northeast of Yellowknife. The site is served by Gahcho Kue Aerodrome, which has both an ice runway in winter and a year-round gravel runway, and a spur of the Tibbitt to Contwoyto Winter Road from Lupin Mine. the main camp is at , north of the ice strip, with a smaller site at , south of the runway.
Document 4: Lac de Gras: Lac de Gras is a lake approximately 300 km north east of Yellowknife, in the Northwest Territories of Canada. Lac de Gras was the centre of the diamond rush of the 1990s. There are three working diamond mines in the area, Diavik Diamond Mine, Ekati Diamond Mine, and Snap Lake Diamond Mine. It was called Ekati by aboriginal peoples.
Document 5: 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.
Document 6: Geology of Singapore: Igneous rocks are found in Bukit Timah, Woodlands, and Pulau Ubin island. Granite makes up the bulk of the igneous rock. Gabbro is also found in the area and is found in an area called Little Guilin, named for its resemblance to Guilin in Southern China. This area is in Bukit Gombak. Sedimentary rocks are found on the western part of Singapore, and is mainly made of sandstone and mudstones. It also includes the southwestern area. Metamorphic rocks are found in the northeastern part of Singapore, and also on Pulau Tekong, off the east coast of Singapore. The rocks are mainly made up of quartzite, and also make up the Sajahat Formation.
Document 7: Geology of the Lassen volcanic area: The geology of the Lassen volcanic area presents a record of sedimentation and volcanic activity in the area in and around Lassen Volcanic National Park in Northern California, U.S. The park is located in the southernmost part of the Cascade Mountain Range in the Pacific Northwest region of the United States. Pacific Oceanic tectonic plates have plunged below the North American Plate in this part of North America for hundreds of millions of years. Heat from these subducting plates has fed scores of volcanoes in California, Oregon, Washington and British Columbia over at least the past 30 million years (see Geology of the Pacific Northwest) and is also responsible for activities in the Lassen volcanic area.
Document 8: Northland Pyrite Mine: The Northland Pyrite Mine, also known as James Lake Mine, Rib Lake Mine, Harris Mine or simply Northland Mine, is an abandoned underground mine in Northeastern Ontario, Canada, located on the southwestern shore of James Lake in Best Township of Temagami. It was operated by the Northland Mining Company during the early 1900s with the construction of a 91 m shaft and many open-cuts north of the shaft. Minerals present at the mine include chalcopyrite, pyrite and pyrrhotite, deposited in Precambrian volcanic rock of the Canadian Shield.
Document 9: Cavanal Hill: Cavanal Hill (officially Cavanal Mountain), located near Poteau, Oklahoma, is billed by a local chamber of commerce as the, "tallest hill in the world", because the elevation of its summit is 1999 ft . The actual summit elevation is 2385 ft above sea level; the difference in elevation between the summit and the Poteau River 3 mi to the north is 1960 ft .
Document 10: Northern Region, Manitoba: The Northern Region is a region in the Canadian province of Manitoba. It is situated on the Canadian Shield and includes Manitoba's Hudson Bay coastline. The major economic activities are mining and tourism. The region is composed of four census divisions: 19 and 21–23 . The land area of the region is 438,491.51 km² (169,302.52 mi²), which encompasses 67% of Manitoba's total land area. The vast majority of the region is undeveloped wilderness. Its total population at the 2011 census was 88,146, which was only 7.3% of Manitoba's total population in the 2011 census. The largest municipality is the city of Thompson. Other major population centers include the city of Flin Flon and the town of The Pas. Indian reserves comprise more than 49% of the region's population. There are 54 reserves with a total population of 40,572. The largest of these are Norway House 17 and Peguis 1B.
Document 11: North Hill, Minot: North Hill is a neighborhood in Minot, North Dakota, located north of the Souris River, above the Souris River Valley. It is a primarily residential neighborhood, though there are industries and businesses in the area, primarily along North Broadway and 21st Ave NW. North Hill is also home to Minot International Airport.
Document 12: Iron Range: Iron Range refers collectively or individually to a number of elongated iron-ore mining districts around Lake Superior in the United States and Canada. Despite the word "range," the iron ranges are not mountain chains, but outcrops of Precambrian sedimentary formations containing high percentages of iron. These cherty iron ore deposits are Precambrian in age for the Vermilion Range, while middle Precambrian in age for the Mesabi and Cuyuna Ranges, all in Minnesota. Similarly, the Gogebic Range in Wisconsin and the Marquette Iron Range and Menominee Range in Michigan. Natural ores and concentrates were produced from 1848 until the mid 1950s, when taconites and jaspers were concentrated and pelletized started to become the major source of iron production.
Document 13: Ruth Mine: The Ruth Mine was a small gold producer about 65 km (40 miles) east of Yellowknife, Northwest Territories. It operated briefly during 1942 and then again in 1959, extracting only 550 troy ounces (17 kg) of gold thus far. The old mine is today (2012) significant as one of the last intact abandoned mining properties from the 1940s period in the Northwest Territories, although the site was scheduled to be remediated by the federal government.
Document 14: Karmutsen Formation: The Karmutsen Formation is a Late Triassic volcanic sequence of tholeiitic pillow basalts and breccias on Vancouver Island, British Columbia, Canada. It is perhaps the thickest accreted section of an oceanic plateau worldwide, exposing up to 6000 m of basal sediment-sill complexes, basaltic to picritic pillow lavas, pillow breccia, and thick, massive basalt flows. The widespread succession of basalts and breccias are part of the Insular Mountains, a large volcanic mountain range that forms Vancouver Island and the Queen Charlotte Islands. In Strathcona Provincial Park, pillow basalts is the most abundant rock unit. About half the mountains, including the highest ones, are carved from these basalts, such as Golden Hinde, which is the highest peak on Vancouver Island.
Document 15: 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.
ground_truth: Laurentian Plateau