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In the western Churchill Province of south-central Nunavut are the Noomut, Heninga Lake and Meliadine gold deposits, and the Victory Lake and Ferguson Lake base metals deposits. Ultramafic volcanic rocks, quartzite and iron formations in the northern Churchill Province hold the Woodhurn, Prince Albert and Meadowbank gold deposits.
The Canadian territory of Nunavut covers about 1.9 million square kilometres (733,594 sq. miles) of land and water including part of the mainland, most of the Arctic islands, and all of the islands in Hudson Bay, James Bay, and Ungava Bay (including the Belcher Islands) which belonged to the Northwest Territories.
Pages in category "Geology of Nunavut" The following 15 pages are in this category, out of 15 total. This list may not reflect recent changes. ...
This is a map of the Canadian Territory of Nunavut. The Eureka Sound Formation is a geologic formation found in the Canadian Territory of Nunavut on Ellesmere Island, which is part of the Canadian Arctic Archipelago. The Eureka Sound Formation is Tertiary in age. [1]
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 tectono metamorphic intervals, including many discrete accretionary magmatic events.
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The Tree River (Kogluktualuk) is a river in Nunavut, Canada.It flows into Coronation Gulf, an arm of the Arctic Ocean.. Glacial landforms, such as a kame delta, are represented in the area of the Tree River.
The Muskox intrusion is a layered intrusion in Nunavut, Canada. It is located 144 km (89 mi) northeast of Great Bear Lake and 90 km (56 mi) south of Kugluktuk on Coronation Gulf . It was formed during a large magmatic event during the Proterozoic by hotspot or mantle plume volcanism that emplaced the widespread Coppermine River Group flood ...