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Lewis Range
The Lewis Range is a mountain range located in the Rocky Mountains of northern Montana, United States and extreme southern Alberta, Canada. It was formed as a result of the Lewis Overthrust, a geologic thrust fault involving the overlying of younger Cretaceous rocks by older Proterozoic rocks. The range is located within Waterton Lakes National Park in Alberta, Canada and Glacier National Park and the Bob Marshall Wilderness Complex in Montana, United States. The highest peak is Mount Cleveland at . Geography The Lewis Range is within Waterton Lakes National Park in Canada, and in Glacier National Park in Montana. The Continental Divide spans much of the uppermost sections of the range. Major peaks in the range include Mount Cleveland (), which is the highest peak in the range and in Glacier National Park . Other prominent peaks include Mount Stimson (), Mount Jackson (), Mount Siyeh (), Going to the Sun Mountain, () and the isolated Chief Mountain (). This sharp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Cleveland (Montana)
Mount Cleveland is the highest mountain in Glacier National Park, located in Montana, United States. It is also the highest point in the Lewis Range, which spans part of the northern portion of the park and extends into Canada. It is located approximately southeast of the southern end of Waterton Lake, and approximately south of the US–Canada border. The east side of the future national park was purchased by the federal government from the Blackfoot Confederacy in 1895 during the second term of President Grover Cleveland. According to the United States Board on Geographic Names, the mountain is named for the former president. While not of great absolute elevation (the mountain is more than lower than Granite Peak, the highest peak in Montana), Mount Cleveland is notable for its large, steep rise above local terrain. For example, its west flank rises over in less than ; the northwest face, the steepest on the mountain, rises in less than . The other faces show almost as m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Stimson
Mount Stimson () is the second highest peak in Glacier National Park, located in Montana, United States. It is part of the Lewis Range, which spans much of the park. It is located in the remote southwestern portion of the park, approximately west of the Continental Divide and southeast of Lake McDonald. It is drained by Pinchot Creek (on the south) and Nyack Creek (on the other sides), both of which flow into the Middle Fork of the Flathead River. The mountain is named for Henry L. Stimson (1867–1950), former U.S. Secretary of State and twice Secretary of War, who hiked and assisted George Bird Grinnell survey the area in and around Glacier National Park in the 1890s, and supported efforts to establish the national park. Notability Mount Stimson is notable for its large, steep rise above local terrain. For example, its northwest face rises over from Nyack Creek in only . This makes it "truly a monster of a mountain." It is also notable for its isolation; it is one of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Flathead County, Montana
A landform is a land feature on the solid surface of the Earth or other planetary body. They may be natural or may be anthropogenic (caused or influenced by human activity). Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great oceanic basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, structure stratification, rock exposure, and soil type. Gross physical features or landforms include intuitive elements such as berms, cliffs, hills, mounds, peninsulas, ridges, rivers, valleys, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbod ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Montana
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lewis Range
The Lewis Range is a mountain range located in the Rocky Mountains of northern Montana, United States and extreme southern Alberta, Canada. It was formed as a result of the Lewis Overthrust, a geologic thrust fault involving the overlying of younger Cretaceous rocks by older Proterozoic rocks. The range is located within Waterton Lakes National Park in Alberta, Canada and Glacier National Park and the Bob Marshall Wilderness Complex in Montana, United States. The highest peak is Mount Cleveland at . Geography The Lewis Range is within Waterton Lakes National Park in Canada, and in Glacier National Park in Montana. The Continental Divide spans much of the uppermost sections of the range. Major peaks in the range include Mount Cleveland (), which is the highest peak in the range and in Glacier National Park . Other prominent peaks include Mount Stimson (), Mount Jackson (), Mount Siyeh (), Going to the Sun Mountain, () and the isolated Chief Mountain (). This sharp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains And Mountain Ranges Of Glacier National Park (U
A list is a set of discrete items of information collected and set forth in some format for utility, entertainment, or other purposes. A list may be memorialized in any number of ways, including existing only in the mind of the list-maker, but lists are frequently written down on paper, or maintained electronically. Lists are "most frequently a tool", and "one does not ''read'' but only ''uses'' a list: one looks up the relevant information in it, but usually does not need to deal with it as a whole".Lucie Doležalová,The Potential and Limitations of Studying Lists, in Lucie Doležalová, ed., ''The Charm of a List: From the Sumerians to Computerised Data Processing'' (2009). Purpose It has been observed that, with a few exceptions, "the scholarship on lists remains fragmented". David Wallechinsky, a co-author of ''The Book of Lists'', described the attraction of lists as being "because we live in an era of overstimulation, especially in terms of information, and lists help us ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precambrian
The Precambrian ( ; or pre-Cambrian, sometimes abbreviated pC, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinized name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Logan Pass
Logan Pass (elevation ) is located along the Continental Divide in Glacier National Park, in the U.S. state of Montana. It is the highest point on the Going-to-the-Sun Road. The pass is named after Major William R. Logan, the first superintendent of the park. The Logan Pass Visitor Center is open during the summer season just east of the pass. The pass is a popular starting point for hiking and backpacking trips. The most popular trail is the Highline Trail which heads north along the west side of the continental divide, through an area known as the Garden Wall, due to the proliferation of wildflowers which grow there during the summer. Just east of the pass, an area known as Big Drift often records over 100 feet (30 m) of snowfall, much of which has been pushed over the continental divide by the prevailing westerly winds during the winter. The pass is closed during the winter due to avalanche hazards and the virtual impossibility of keeping the Going-to-the-Sun Road open, ye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marias Pass
Marias Pass (elevation ) is a mountain pass in the Rocky Mountains in the western US state of Montana. Lying on the southern border of Glacier National Park, it is traversed by US Highway 2 and by the BNSF Hi-Line Subdivision. The pass is the lowest crossing of the Continental Divide between Canada and central New Mexico, and is the northernmost pass in the US open to automobile traffic year-round. Geography Marias Pass traverses the Continental Divide in the Lewis Range, along the boundary between the Lewis and Clark National Forest and the Flathead National Forest. The pass forms the southern limit of the Continental Ranges, a major grouping of the Rocky Mountains which extends as far north as McGregor Pass in the Northern Rockies of the Canadian province of British Columbia. The Great Bear Wilderness in Lewis and Clark National Forest is south of the pass and Glacier National Park is to the north. Climate History As a low pass through the Rocky Mounta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chief Mountain
Chief Mountain ('' Blackfoot: Ninaistako'') () is located in the U.S. state of Montana on the eastern border of Glacier National Park and the Blackfeet Indian Reservation. The mountain is one of the most prominent peaks and rock formations along the Rocky Mountain Front, a long overthrust fault, known as the Lewis Overthrust, which extends from central Montana into southern Alberta, Canada. Geology Chief Mountain is an example of a klippe. It consists of a Precambrian block which rests directly above much younger Cretaceous gray shales. The 1450-1400 million year old Precambrian rocks are 1300-1400 million years older than the Cretaceous rocks at the base of the mountain. Having an older layer of rock juxtaposed atop younger basement rocks is found on occasion in thrust faults and is commonplace along the Lewis Overthrust which extends from central Montana to far southern Alberta. The surrounding portion of the thrust sheet has been removed by erosion leaving ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Going To The Sun Mountain
Going-to-the-Sun Mountain is a mountain peak located in Glacier National Park in the U.S. state of Montana. It rises dramatically above St. Mary Valley just north of the Going-to-the-Sun Road. The mountain was named by James Willard Schultz in 1888. Origin of name During the winter of 1887–1888, James Willard Schultz, an early hunting guide in the St. Mary Lakes region, and his family built a cabin on the north shore of upper Saint Mary Lake. While hunting on Red Eagle Mountain with his Pikuni friend, Tail-Feathers-Coming-Over-the-Hill, Schultz gave this mountain the name it bears today. Warren Hanna, Schultz's biographer describes the naming thus: Alternatively, numerous Blackfeet Indian legends are credited with the origins of the mountains' name. Used by the Blackfeet as a location for vision quests, it is one of the most accessible major mountain peaks in Glacier National Park. According to several sources, the actual Blackfeet name for the mountain is ''The-Fa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
