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Big Baldy Mountain (Montana)
Big Baldy Mountain is the tallest mountain in the Little Belt Mountains located in Judith Basin County, Montana. The mountain is high. The mountain is locally known as ''Mount Baldy''. History Several people in the area around the mountain, including some scientists, believe that Big Baldy Mountain including nearby mountain ranges were formed from magma that never made it to the earth's surface several thousands of years ago. Even though evidence is slim at the summit of Big Baldy itself, satellite views of the mountain show noticeable craters and features that indicate possible volcanic activity. Many features such as craters, lakes at the summit of the mountain, and stains that look like an old lava trail or spill make the mountain look as if it were a volcano many years ago. It is believed that when the Rocky Mountains were forming from plate tectonics, the Little Belt Mountains underwent a period of being subjected to magma moving close to the surface in which created several ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Google Earth
Google Earth is a computer program that renders a 3D computer graphics, 3D representation of Earth based primarily on satellite imagery. The program maps the Earth by superimposition, superimposing satellite images, aerial photography, and geographic information system, GIS data onto a 3D globe, allowing users to see cities and landscapes from various angles. Users can explore the globe by entering addresses and coordinates, or by using a Computer keyboard, keyboard or computer mouse, mouse. The program can also be downloaded on a smartphone or Tablet computer, tablet, using a touch screen or stylus to navigate. Users may use the program to add their own data using Keyhole Markup Language and upload them through various sources, such as forums or blogs. Google Earth is able to show various kinds of images overlaid on the surface of the earth and is also a Web Map Service client. In 2019, Google has revealed that Google Earth now covers more than 97 percent of the world, and has c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Belt Mountains
The Little Belt Mountains are a section of the Rocky Mountains in the U.S. The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 states, a federal district, five major unincorporated territori ... state of Montana. Situated mainly in the Lewis and Clark National Forest, the mountains are used for logging and recreation for the residents of Great Falls, Montana. Showdown Ski Area, Showdown is a ski area located within the mountains located off US Highway 89 which splits the mountains in half connecting White Sulphur Springs, MT, White Sulphur Springs and Belt, MT. The highest point in the Little Belt Range is Big Baldy Mountain at . The Little Belts have been mined for silver since the 1880s, and for sapphire since 1896. The sapphires, called Yogo sapphires as they are mined near Yogo Creek, occur in a formation long and across. The mountains are nam ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Judith Basin County, Montana
Judith Basin County is a county in the U.S. state of Montana. As of the 2020 census, the population was 2,023. Its county seat is the town of Stanford. History Judith Basin County was formed of area taken from western Fergus and eastern Cascade counties on December 10, 1920. In 1895, Yogo sapphires were discovered at Yogo Gulch, about 15 miles southwest of Utica, which at the time was in Fergus County. Geography According to the United States Census Bureau, the county has a total area of , of which is land and (0.04%) is water. Adjacent counties * Chouteau County – north * Fergus County – east * Wheatland County – south * Meagher County – south * Cascade County – west National protected area * Lewis and Clark National Forest (part) City * Hobson Town * Stanford (county seat) Census-designated places * Geyser * Moccasin * Raynesford * Sapphire Ridge * Surprise Creek Colony * Utica * Windham Other unincorporated communities * Arrow Creek * Benc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Montana
Montana () is a state in the Mountain West division of the Western United States. It is bordered by Idaho to the west, North Dakota and South Dakota to the east, Wyoming to the south, and the Canadian provinces of Alberta, British Columbia, and Saskatchewan to the north. It is the fourth-largest state by area, the eighth-least populous state, and the third-least densely populated state. Its state capital is Helena. The western half of Montana contains numerous mountain ranges, while the eastern half is characterized by western prairie terrain and badlands, with smaller mountain ranges found throughout the state. Montana has no official nickname but several unofficial ones, most notably "Big Sky Country", "The Treasure State", "Land of the Shining Mountains", and " The Last Best Place". The economy is primarily based on agriculture, including ranching and cereal grain farming. Other significant economic resources include oil, gas, coal, mining, and lumber. The health ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Judith Basin County
Judith Basin County is a county in the U.S. state of Montana. As of the 2020 census, the population was 2,023. Its county seat is the town of Stanford. History Judith Basin County was formed of area taken from western Fergus and eastern Cascade counties on December 10, 1920. In 1895, Yogo sapphires were discovered at Yogo Gulch, about 15 miles southwest of Utica, which at the time was in Fergus County. Geography According to the United States Census Bureau, the county has a total area of , of which is land and (0.04%) is water. Adjacent counties * Chouteau County – north * Fergus County – east * Wheatland County – south * Meagher County – south * Cascade County – west National protected area * Lewis and Clark National Forest (part) City * Hobson Town * Stanford (county seat) Census-designated places * Geyser * Moccasin * Raynesford * Sapphire Ridge * Surprise Creek Colony * Utica * Windham Other unincorporated communities * Arrow Creek * Benc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Magma
Magma () is the molten or semi-molten natural material from which all igneous rocks are formed. Magma is found beneath the surface of the Earth, and evidence of magmatism has also been discovered on other terrestrial planets and some natural satellites. Besides molten rock, magma may also contain suspended crystals and gas bubbles. Magma is produced by melting of the mantle or the crust in various tectonic settings, which on Earth include subduction zones, continental rift zones, mid-ocean ridges and hotspots. Mantle and crustal melts migrate upwards through the crust where they are thought to be stored in magma chambers or trans-crustal crystal-rich mush zones. During magma's storage in the crust, its composition may be modified by fractional crystallization, contamination with crustal melts, magma mixing, and degassing. Following its ascent through the crust, magma may feed a volcano and be extruded as lava, or it may solidify underground to form an intrusion, such as a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rocky Mountains
The Rocky Mountains, also known as the Rockies, are a major mountain range and the largest mountain system in North America. The Rocky Mountains stretch in straight-line distance from the northernmost part of western Canada, to New Mexico in the southwestern United States. Depending on differing definitions between Canada and the U.S., its northern terminus is located either in northern British Columbia's Terminal Range south of the Liard River and east of the Trench, or in the northeastern foothills of the Brooks Range/ British Mountains that face the Beaufort Sea coasts between the Canning River and the Firth River across the Alaska-Yukon border. Its southernmost point is near the Albuquerque area adjacent to the Rio Grande rift and north of the Sandia–Manzano Mountain Range. Being the easternmost portion of the North American Cordillera, the Rockies are distinct from the tectonically younger Cascade Range and Sierra Nevada, which both lie farther to its west. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plate Tectonics
Plate tectonics (from the la, label=Late Latin, tectonicus, from the grc, τεκτονικός, lit=pertaining to building) is the generally accepted scientific theory that considers the Earth's lithosphere to comprise a number of large tectonic plates which have been slowly moving since about 3.4 billion years ago. The model builds on the concept of ''continental drift'', an idea developed during the first decades of the 20th century. Plate tectonics came to be generally accepted by geoscientists after seafloor spreading was validated in the mid to late 1960s. Earth's lithosphere, which is the rigid outermost shell of the planet (the crust and upper mantle), is broken into seven or eight major plates (depending on how they are defined) and many minor plates or "platelets". Where the plates meet, their relative motion determines the type of plate boundary: '' convergent'', '' divergent'', or ''transform''. Earthquakes, volcanic activity, mountain-building, and oceanic tr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Judith Basin 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 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 terrain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
