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Pomp Peak
Pomp Peak is a mountain summit in Gallatin County, Montana, United States. Description Pomp Peak is the third-highest peak in the Bridger Range which is a subrange of the Rocky Mountains. The peak is situated north of Bozeman in the Gallatin National Forest. Precipitation runoff from the mountain's east slope drains to Fairy Creek → Flathead Creek → Shields River → Yellowstone River, whereas the west slope drains to Reese Creek → Smith Creek → East Gallatin River. Topographic relief is significant as the summit rises above Fairy Lake in . This mountain's toponym was officially adopted on June 12, 2008, by the United States Board on Geographic Names to honor Jean Baptiste "Pomp" Charbonneau (1805–1866), the son of Sacagawea, the Shoshone Indian scout on the Lewis and Clark Expedition. Pomp Peak is located less than one mile immediately northwest of Sacagawea Peak. Pompeys Pillar National Monument is also named for Pomp. Climate According to the Köppen climate c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jean Baptiste Charbonneau
Jean Baptiste Charbonneau (February 11, 1805 – May 16, 1866) was a Native American-French Canadian explorer, guide, Animal trapping, fur trapper, trader, military scout during the Mexican–American War, ''alcalde'' (mayor) of Mission San Luis Rey de Francia and a gold digger and hotel operator in Northern California. His mother was Sacagawea, a Shoshone Native who worked as a guide and interpreter for the Lewis and Clark Expedition. Charbonneau spoke French and English and learned German and Spanish during his six years in Europe from 1823 to 1829. He spoke Shoshoni language, Shoshone and other western Native American languages, which he picked up during his years of trapping and guiding. Jean Baptiste's father was also a member of the Lewis and Clark expedition, a French Canadians, French Canadian explorer and trader named Toussaint Charbonneau. Jean Baptiste was born at Fort Mandan in North Dakota. In his early childhood, he accompanied his parents as they traveled acros ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fairy Lake
Fairy Lake is a lake in Gallatin County, Montana at the base of Sacagawea Peak, a part of the Bridger mountains in south central Montana. It is located within the northwestern section of the Gallatin National Forest The Gallatin National Forest (now known as the Custer-Gallatin National Forest) is a United States National Forest located in South-West Montana. Most of the Custer-Gallatin goes along the state's southern border, with some of it a part of North- ... and sits at an elevation of . References External links Montana Fish, Wildlife, and Parks page on Fairy Lake Bodies of water of Gallatin County, Montana Lakes of Montana Gallatin National Forest Protected areas of Gallatin County, Montana {{GallatinCountyMT-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains 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 300 metres (1,000 feet) 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Gallatin County, 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 (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hardscrabble Peak
Hardscrabble or Hard Scrabble is land that is rocky or of poor quality, as in the term ''hardscrabble farm''. It is often used as a euphemism for any sort of hard working or poverty, as in ''hardscrabble childhood''. A number of towns use this name: * Hardscrabble (Harrisburg), Pennsylvania, a former neighborhood in Midtown Harrisburg, Pennsylvania * Hardscrabble, California, now Ione, California * Hardscrabble, Colorado, an extinct town in Colorado * Hardscrabble, Illinois, now Streator, Illinois * Hardscrabble, Indiana, a town in Indiana * Hardscrabble, New York, now Farmingdale, New York * Hardscrabble, Ohio * Hardscrabble, Ontario, a village incorporated into the town of Hamilton, Ontario, today's Cobourg, Ontario, Canada * Hardscrabble, Virginia, an unincorporated community in Highland County, Virginia * Hardscrabble, West Virginia, now Scrabble, West Virginia * Hardscrabble or Hard Scrabble, Wisconsin, now Hazel Green (town), Wisconsin * Hard Scrabble and Snow Town, two ... [...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 t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N, poleward of the humid continental climates. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification ''Dfc'', ''Dwc'', ''Dsc'', ''Dfd'', ''Dwd'' and ''Dsd''. Description This type of climate offers some of the most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below and in summer, the temperature may exceed . However, the summers are short; no more than three months of the year (but at least one month) must have a 24-hour average temperature of at least to fall into this category of climate, and the coldest month should a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pompeys Pillar National Monument
Pompeys Pillar National Monument is a rock formation located in south central Montana, United States. Designated a National Monument on January 17, 2001, and managed by the U.S. Bureau of Land Management in conjunction with The Friends of Pompeys Pillar, it consists of only , making it one of the smallest National Monuments in the U.S. The community of Pompeys Pillar lies just east of the monument. History It was previously designated a National Historic Landmark on July 25, 1965. The new Pompeys Pillar Interpretive Center opened in 2006. Exhibits in the 5,700-square foot center relate the journey of Captain William Clark and his detachment, including Sacagawea and her son Pomp, down the Yellowstone River Valley in 1806. The pillar itself stands 150 feet (45 m) above the Yellowstone River and consists of sandstone from the late Cretaceous Hell Creek Formation, 75 – 66 million years ago. The base of the pillar is approximately . The pillar features an abundance of Native ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sacagawea Peak
Sacagawea Peak is the highest mountain in the Bridger Range in south-western Montana. The peak is named for Sacagawea, a Lemhi Shoshone woman that accompanied the Lewis and Clark Expedition The Lewis and Clark Expedition, also known as the Corps of Discovery Expedition, was the United States expedition to cross the newly acquired western portion of the country after the Louisiana Purchase. The Corps of Discovery was a select gr .... Recreation The mountain is a popular hiking destination. The main trailhead starts at 7,788 feet and climbs 1,800 feet reaching the summit in 2 miles. The mountain holds snow in chutes through the early summer and local skiers often ski there through August. References Mountains of Montana Sacagawea {{GallatinCountyMT-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lewis And Clark Expedition
The Lewis and Clark Expedition, also known as the Corps of Discovery Expedition, was the United States expedition to cross the newly acquired western portion of the country after the Louisiana Purchase. The Corps of Discovery was a select group of U.S. Army and civilian volunteers under the command of Captain Meriwether Lewis and his close friend Second Lieutenant William Clark. Clark and 30 members set out from Camp Dubois, Illinois, on May 14, 1804, met Lewis and ten other members of the group in St. Charles, Missouri, then went up the Missouri River. The expedition crossed the Continental Divide of the Americas near the Lemhi Pass, eventually coming to the Columbia River, and the Pacific Ocean in 1805. The return voyage began on March 23, 1806, at Fort Clatsop, Oregon, and ended on September 23 of the same year. President Thomas Jefferson commissioned the expedition shortly after the Louisiana Purchase in 1803 to explore and to map the newly acquired territory, to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
