| Strand Fiord Pass | |
|---|---|
  Location in Nunavut | |
| Location | Nunavut, Canada |
| Coordinates | 79°16′07″N88°45′00″W / 79.26861°N 88.75000°W |
| Topo map | NTS 59H8 Strand Fiord Pass |
Strand Fiord Pass is a mountain pass on southern Axel Heiberg Island, Nunavut, Canada. [1]
The District of Franklin was a regional administrative district of Canada's Northwest Territories. The district consisted of the Canadian high Arctic Islands, notably Ellesmere Island, Baffin Island, and Victoria Island. The district also contained the mainland Melville Peninsula and Boothia Peninsula.
Lougheed Island is one of the uninhabited members of the Queen Elizabeth Islands of the Arctic Archipelago in the Qikiqtaaluk Region, Nunavut. It measures 1,312 km2 (507 sq mi) in size. It is relatively isolated compared to other Canadian Arctic islands, and is located in the Arctic Ocean, halfway between Ellef Ringnes Island to the northeast and Melville Island to the southwest. It is part of the Findlay Group.
Israel Cook Russell, LL.D. was an American geologist and geographer who explored Alaska in the late 19th century.
Russell Fiord, also spelled Russell Fjord, is a fjord in the U.S. state of Alaska. It extends north to Disenchantment Bay, the terminus of Hubbard Glacier, at the head of Yakutat Bay. The fjord was named in 1901 by Marcus Baker of the U.S. Geological Survey for explorer Israel Russell, who discovered the estuary in 1891 while exploring the Yakutat region.
The Ellesmere Island Volcanics are a Late Cretaceous volcanic group of volcanoes and lava flows in the Qikiqtaaluk Region of northern Ellesmere Island, Nunavut, Canada.
The Alpha Ridge is a major volcanic ridge under the Arctic Ocean between the Canada Basin and the Lomonosov Ridge. It was active during the formation of the Amerasian Basin. It was discovered in 1963. The highest elevation is about 2,700 m over the ocean floor. It is 200 to 450 km wide. The Alpha Ridge, Lomonosov Ridge, and Nansen-Gakkel Ridge are the three major ranges that divide the Arctic Ocean floor, running generally parallel to each other.
The Strand Fiord Formation is a Late Cretaceous volcanic component, located on northwestern and west-central Axel Heiberg Island, Nunavut, Canada. The formation contains flood basalts which are found on western Axel Heiberg Island at Dragon Cliff 300 m (980 ft) tall.
Dragon Cliff is a basaltic monolith located on western Axel Heiberg Island, Nunavut, Canada. It is the most striking feature of Expedition Fiord and rises several hundred metres out of the fiord. Dragon Cliff is made of flood basalt lava flows that contain more than 10 flow units totalling over 200 m (660 ft) of stratigraphic thickness. It is part of the Albian Strand Fiord Formation, which in turn forms part of the High Arctic Large Igneous Province. The Strand Fiord Formation is interpreted to represent the cratonward extension of the Alpha Ridge.
Disraeli Glacier is a glacier on northern Ellesmere Island, Nunavut, Canada. It lies in Quttinirpaaq National Park, South-West of the Disraeli Fiord. It is believed to have been named after Benjamin Disraeli, a British politician in the mid 1800s.
Ayr Pass is a mountain pass in the central Baffin Mountains, Nunavut, Canada.
Atagulisaktalik formerly known as Revoir Pass is a mountain pass in the central Baffin Mountains, Nunavut, Canada. It is named after the Revoir River.
Greely Fiord is a natural inlet in the west of Ellesmere Island, Qikiqtaaluk Region, Nunavut in the Arctic Archipelago. To the south lies the Cañon Fiord and the Agassiz Ice Cap. To the northwest is Borup Fiord and Tanquary Fiord is northeast.
The Sverdrup Basin Magmatic Province is a large igneous province located on Axel Heiberg Island and Ellesmere Island, Nunavut, Canada near the rifted margin of the Arctic Ocean at the end of Alpha Ridge.
The Kanguk Formation is a geological formation in the Northwest Territories and Nunavut, Canada whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.
Bjarnason Island is an island of the Arctic Archipelago in the territory of Nunavut. It lies in the Arctic Ocean, north-west of Axel Heiberg Island, separated from it by Bukken Fiord to its north and Bunde Fiord to its south.
Volcanism in Northern Canada has produced hundreds of volcanic areas and extensive lava formations across Northern Canada. The region's different volcano and lava types originate from different tectonic settings and types of volcanic eruptions, ranging from passive lava eruptions to violent explosive eruptions. Northern Canada has a record of very large volumes of magmatic rock called large igneous provinces. They are represented by deep-level plumbing systems consisting of giant dike swarms, sill provinces and layered intrusions.
Tanquary Fiord is a fjord on the north coast of the Arctic Archipelago's Ellesmere Island, Nunavut, Canada. It is located in the Quttinirpaaq National Park and extends 48 km (30 mi) in a north-westerly direction from Greely Fiord.
Hektoria Glacier is a glacier flowing south from the area around Mount Johnston between Mount Quandary and Zagreus Ridge into Vaughan Inlet next west of Brenitsa Glacier and east of Green Glacier, on the east coast of the Antarctic Peninsula.
Strathcona Fiord is a fiord on the west central coast of Ellesmere Island, the most northern island within the Arctic Archipelago, Nunavut, Canada.
The Devon Island Formation is a geologic formation in the Canadian Arctic. It preserves fossils dating back to the late Silurian and Devonian periods.
 | This article related to a mountain, mountain range, or peak in Canada is a stub. You can help Wikipedia by expanding it. |
 | This Qikiqtaaluk Region, Nunavut location article is a stub. You can help Wikipedia by expanding it. |