| Joss Pass | |
|---|---|
  Location in Nunavut | |
| Location | Nunavut, Canada |
| Range | United States Range |
| Coordinates | 82°24′07″N68°14′33″W / 82.40194°N 68.24250°W |
| Topo map | NTS 120F6 Barrier Glacier |
Piper Pass is a mountain pass in the United States Range, Nunavut, Canada. [1]
The Cascade Range or Cascades is a major mountain range of western North America, extending from southern British Columbia through Washington and Oregon to Northern California. It includes both non-volcanic mountains, such as many of those in the North Cascades, and the notable volcanoes known as the High Cascades. The small part of the range in British Columbia is referred to as the Canadian Cascades or, locally, as the Cascade Mountains. The highest peak in the range is Mount Rainier in Washington at 14,411 feet (4,392 m).
The Alaska Range is a relatively narrow, 600-mile-long (950 km) mountain range in the southcentral region of the U.S. state of Alaska, from Lake Clark at its southwest end to the White River in Canada's Yukon Territory in the southeast. Denali, the highest mountain in North America, is in the Alaska Range. The range is part of the American Cordillera.
McKenzie Pass, elevation 5,325 feet (1,623 m), is a mountain pass in the Cascade Range in central Oregon in the United States.
The Selkirk Mountains are a mountain range spanning the northern portion of the Idaho Panhandle, eastern Washington, and southeastern British Columbia which are part of a larger grouping of mountains, the Columbia Mountains. They begin at Mica Peak and Krell Hill near Spokane and extend approximately 320 km north from the border to Kinbasket Lake, at the now-deserted location of the onetime fur company post, Boat Encampment. The range is bounded on its west, northeast and at its northern extremity by the Columbia River, or the reservoir lakes now filling most of that river's course. From the Columbia's confluence with the Beaver River, they are bounded on their east by the Purcell Trench, which contains the Beaver River, Duncan River, Duncan Lake, Kootenay Lake and the Kootenay River. The Selkirks are distinct from, and geologically older than, the Rocky Mountains. The neighboring Monashee and Purcell Mountains, and sometimes including the Cariboo Mountains to the northwest, are also part of the larger grouping of mountains known as the Columbia Mountains. A scenic highway loop, the International Selkirk Loop, encircles the southern portions of the mountain range.
Deep Springs Valley is a high desert valley in the Inyo-White Mountains of Inyo County, California. It is east of the Owens Valley and the Sierra Nevada mountain range, and south of Fish Lake Valley, Nevada, near the California-Nevada state border.
East Canada Creek is a 34.6-mile-long (55.7 km) river in upstate New York, United States. It is a tributary of the Mohawk River and flows southward from New York's Adirondack Park. The name "Canada" may be derived from the St. Lawrence Iroquoian word Kanata, meaning "village"; the name may also refer to the creek's importance as a trail to Canada in colonial times.
Street Mountain is a mountain located in Essex County, New York, named after Alfred Billings Street (1811–1881), a poet and New York State Librarian. The mountain is the high point of the Street Range of the Adirondack Mountains. Street's northeast ridge is Nye Mountain.
The Madison Limestone is a thick sequence of mostly carbonate rocks of Mississippian age in the Rocky Mountain and Great Plains areas of the western United States. The rocks serve as an important aquifer as well as an oil reservoir in places. The Madison and its equivalent strata extend from the Black Hills of western South Dakota to western Montana and eastern Idaho, and from the Canada–United States border to western Colorado and the Grand Canyon of Arizona.
Gordon Glacier is an Antarctic glacier of at least 24 nautical miles in length flowing in a northerly direction beginning in the Crossover Pass, flowing through the Shackleton Range to finally meet the Slessor Glacier.
Colorado is a geologic name applied to certain rocks of Cretaceous age in the North America, particularly in the western Great Plains. This name was originally applied to classify a group of specific marine formations of shale and chalk known for their importance in Eastern Colorado. The surface outcrop of this group produces distinctive landforms bordering the Great Plains and it is a significant feature of the subsurface of the Denver Basin and the Western Canadian Sedimentary Basin. These formations record important sequences of the Western Interior Seaway. As the geology of this seaway was studied, this name came to be used in states beyond Colorado but later was replaced in several of these states with more localized names.
The Ellis Group is a stratigraphical unit of Bajocian-Oxfordian age in Alberta, Saskatchewan, Montana and Wyoming in the Western Canadian Sedimentary Basin. It takes the name from Fort Ellis, Montana, and was first described in outcrop in the Rocky Creek Canyon by A.C. Peale in 1893.
The Endicott Mountains are a range of mountains, part of the Brooks Range in northern Alaska. They are located in the middle of the Brooks range and run some 151 miles (243 km) east–west. To the east are the Philip Smith Mountains and to the west are the Schwatka Mountains. The Endicott Mountains are separated from the Philip Smith Mountains by the Middle Fork of the Koyukuk River, the Dalton Highway, and Atigun Pass. The Endicott Mountains are separated from the Schwatka Mountains by Walker Lake, the upper reaches of the West Fork of the Kobuk River, Akabluak Pass, and the Noatak River. The Endicott Mountains are separated from the mountains north of the Schwatka by Lucky Six Creek, Gull Pass, Gull Creek, a portion of the Alatna River and the Killik River.
Wright Peninsula is a peninsula on the east coast of Adelaide Island, Antarctica, lying between Stonehouse Bay to the north and Ryder Bay to the south. On its northern coastline the peninsula is fringed by the Stokes Peaks; on its southern side by the Reptile Ridge. The Princess Royal Range separates the peninsula from the rest of Adelaide Island; the only 'gap' is provided by McCallum Pass.
The Blaiklock Glacier is a glacier 16 nautical miles (30 km) long, flowing north from Turnpike Bluff, then northwest to Mount Provender and Mount Lowe in the western part of the Shackleton Range, Antarctica.
Cornwall Glacier is a glacier 9 nautical miles (17 km) long, flowing south from Crossover Pass in the Shackleton Range to join Recovery Glacier east of Ram Bow Bluff.
The Snake River Range is located in the U.S. states of Wyoming and Idaho and includes 10 mountains over 9,000 feet (2,700 m). The tallest peak in the range is Mount Baird at 10,030 feet (3,060 m). The range trends northwest to southeast and is bordered on the north by the Teton Range and the two ranges meet at Teton Pass. The Snake River Range is bordered by the Palisades Reservoir to the west and the Snake River, which sweeps completely around the eastern, southern and western part of the range. The range is approximate 30 miles (48 km) north to south and 33 miles (53 km) west to east, covering 528 square miles (1,370 km2). Along the southern boundary, the Snake River passes through Grand Canyon, also known as the Snake River Canyon. U.S. Route 26/U.S. Route 89 follows the course of the Snake River from Hoback Junction to the Palisades Reservoir.
Coleanor, also known as Coal-Eleanor, is an unincorporated community in Bibb County, Alabama, United States.
Whiteley Peak, elevation 10,092 ft (3,076 m), is a mountain in Grand County, Colorado north of Kremmling and close to U.S. Highway 40. The mountain is in the Rabbit Ears Range, a range composed chiefly of volcanic rock, and Whiteley Peak has some columnar jointing near the top.
... A strikingly deep, narrow trench, Piper Pass, transects the United States Range, and several streams on the southeast side of ...
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