|
Angel Wing (Glacier National Park)
Angel Wing is a elevation mountain summit located in the Lewis Range, of Glacier National Park (US), Glacier National Park in the U.S. state of Montana. It is situated one mile east of the Continental Divide of the Americas, Continental Divide, in Glacier County, Montana, Glacier County. It can be seen from the Many Glacier area, and up close from the Grinnell Glacier Trail. Topographic relief is significant as the north aspect rises nearly above Grinnell Lake in one-half mile. Climate Based on the Köppen climate classification, Angel Wing is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers. Temperatures can drop below −10 °F with wind chill factors below −30 °F. Precipitation Surface runoff, runoff from the peak drains into Grinnell and Cataract Creeks, which are part of the St. Mary River (Alberta–Montana), St. Mary River drainage basin. Geology Like other mountains in Glacier National Park, Angel Wing is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Gould (Montana)
Mount Gould () is a peak on the Continental Divide of the Americas, Continental Divide in Glacier National Park (U.S.), Glacier National Park, Montana, United States. It is the highest point of the Garden Wall, a distinctive ridge of the Lewis Range. It is most notable for its huge, steep east face, which drops in only one-half mile (0.8 km). This face provides a backdrop to Grinnell Lake, and is often photographed. Mount Gould was named in 1887 by George Bird Grinnell for his hunting companion, George H. Gould, and the name was officially adopted in 1929 by the United States Board on Geographic Names. The first recordedSince access to the summit is nontechnical, an earlier ascent, and perhaps a much earlier Native Americans in the United States, Native American ascent, is possible. ascent of Mount Gould was in 1920, by Frank B. Wynn, Harry R. Horn, Henry H. Goddard, and party. They used the West Face route, which is the easiest and most commonly used route today. It starts ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Garden Wall
The Garden Wall is a steep alpine area within Glacier National Park well known during the summer months to be heavily covered in dozens of species of flowering plants and shrubs. Located along the west side of the Continental divide and extending northward from Logan Pass, the Garden Wall can be traversed via the popular Highline Trail and for a distance of over to the Granite Park Chalet. The Going-to-the-Sun Road also passes through portions of the Garden Wall northwest of Logan Pass. The Weeping Wall is a short stretch of the Going-to-the-Sun Road where water cascades over the Garden Wall to the roadway below. The Garden Wall is an arête or rock spine that separates the Many Glacier region of the park from Lake McDonald Lake McDonald is the largest lake in Glacier National Park. It is located at in Flathead County in the U.S. state of Montana. Lake McDonald is approximately 10 miles (16 km) long, and over a mile (1.6 km) wide and 472 feet (130 m) ... valle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Siyeh
Mount Siyeh, with a height of , is the fifth tallest and one of six peaks over in Glacier National Park, Montana, United States. Mount Siyeh was named after a Blackfeet Indian, Sai-yeh, whose name means "Crazy Dog" or "Mad Wolf." Mount Siyeh stands about two miles east of the Continental Divide, within the watershed of the Saint Mary River, which drains into the Saskatchewan River, and ultimately into Hudson Bay. Mount Siyeh is rather easily accessible from a variety of different routes. It can be ascended via a long scree scramble from the Preston Park area, or from Piegan Pass via Cataract Mountain. The summit can also be reached via a long hiking/mountaineering route dubbed the "Skyline Experience"; this route starts from the Many Glacier Hotel and involves ridge walk and includes the summits of Wynn Mountain () and Cracker Peak () before reaching the top of Siyeh. Route Descriptions can be found oSummitpostor iA Climbers Guide to Glacier National Park Geology Like ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Allen Mountain (Montana)
Allen Mountain () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Allen Mountain is NNW of Cracker Lake. The mountain is named to honor Cornelia Seward Allen, the granddaughter of President Abraham Lincoln's Secretary of State William H. Seward Sr. The mountain was named in 1891 by a party of explorers headed by George Bird Grinnell that included Cornelia's brother, William Henry Seward III, a Yale University classmate of Grinnell. See also * List of mountains and mountain ranges of Glacier National Park (U.S.) Mountains in Glacier National Park (U.S.) are part of the Rocky Mountains. There are at least 150 named mountain peaks over in Glacier in three mountain ranges--the Clark Range, Lewis Range, Livingston Range. Mount Cleveland at is the highes ... Gallery File:Allen Mountain.jpg, Allen Mountain's northeast aspect reflected in Lake Sherburne File:Sherburne in Spring.jpg, Allen in Spring File:Grinnell Lake.jpg, West aspect above ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Josephine (Montana)
Lake Josephine is located in Glacier National Park, in the U. S. state of Montana. Swiftcurrent Lake is immediately to the northeast of Lake Josephine and the two lakes are separated by a short () stream. Lake Josephine is accessible via the Grinnell Glacier Trail which follows the west shoreline of the lake for . See also *List of lakes in Glacier County, Montana There are at least 118 named lakes and reservoirs in Glacier County, Montana. Lakes * Alkali Lake, , el. * Allison Lake, , el. * Atsina Lake, , el. * Aubery Lake, , el. * Bench Lake, , el. * Big Spring Lake, , el. * Boundary Lake, ... References Josephine Josephine {{GlacierCountyMT-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains And Mountain Ranges Of Glacier National Park (U
A ''list'' is any set of items in a row. List or lists may also refer to: People * List (surname) Organizations * List College, an undergraduate division of the Jewish Theological Seminary of America * SC Germania List, German rugby union club Other uses * Angle of list, the leaning to either port or starboard of a ship * List (information), an ordered collection of pieces of information ** List (abstract data type), a method to organize data in computer science * List on Sylt, previously called List, the northernmost village in Germany, on the island of Sylt * ''List'', an alternative term for ''roll'' in flight dynamics * To ''list'' a building, etc., in the UK it means to designate it a listed building that may not be altered without permission * Lists (jousting), the barriers used to designate the tournament area where medieval knights jousted * ''The Book of Lists'', an American series of books with unusual lists See also * The List (other) * Listing (di ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of The Rocky Mountains
The geology of the Rocky Mountains is that of a discontinuous series of mountain ranges with distinct geological origins. Collectively these make up the Rocky Mountains, a mountain system that stretches from Northern British Columbia through central New Mexico and which is part of the great mountain system known as the North American Cordillera. The rocky cores of the mountain ranges are, in most places, formed of pieces of continental crust that are over one billion years old. In the south, an older mountain range was formed 300 million years ago, then eroded away. The rocks of that older range were reformed into the Rocky Mountains. The Rocky Mountains took shape during an intense period of plate tectonic activity that resulted in much of the rugged landscape of the western North America. The Laramide orogeny, about 80–55 million years ago, was the last of the three episodes and was responsible for raising the Rocky Mountains. Subsequent erosion by glaciers has created the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neogene
The Neogene ( ), informally Upper Tertiary or Late Tertiary, is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period million years ago ( Mya) to the beginning of the present Quaternary Period Mya. The Neogene is sub-divided into two epochs, the earlier Miocene and the later Pliocene. Some geologists assert that the Neogene cannot be clearly delineated from the modern geological period, the Quaternary. The term "Neogene" was coined in 1853 by the Austrian palaeontologist Moritz Hörnes (1815–1868). During this period, mammals and birds continued to evolve into modern forms, while other groups of life remained relatively unchanged. The first humans (''Homo habilis'') appeared in Africa near the end of the period. Some continental movements took place, the most significant event being the connection of North and South America at the Isthmus of Panama, late in the Pliocene. This cut off the warm ocean currents from the Pacific to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Empire Formation
The Empire Formation is a geologic formation in Oregon. It preserves fossils dating back to the Neogene period. See also * List of fossiliferous stratigraphic units in Oregon * Paleontology in Oregon The location of the state of Oregon Paleontology in Oregon refers to paleontological research occurring within or conducted by people from the U.S. state of Oregon. Oregon's geologic record extends back approximately 400 million years ago to the ... References * Neogene geology of Oregon {{Neogene-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, 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 Latinised 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 fossil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
