1.
United States
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Forty-eight of the fifty states and the federal district are contiguous and located in North America between Canada and Mexico. The state of Alaska is in the northwest corner of North America, bordered by Canada to the east, the state of Hawaii is an archipelago in the mid-Pacific Ocean. The U. S. territories are scattered about the Pacific Ocean, the geography, climate and wildlife of the country are extremely diverse. At 3.8 million square miles and with over 324 million people, the United States is the worlds third- or fourth-largest country by area, third-largest by land area. It is one of the worlds most ethnically diverse and multicultural nations, paleo-Indians migrated from Asia to the North American mainland at least 15,000 years ago. European colonization began in the 16th century, the United States emerged from 13 British colonies along the East Coast. Numerous disputes between Great Britain and the following the Seven Years War led to the American Revolution. On July 4,1776, during the course of the American Revolutionary War, the war ended in 1783 with recognition of the independence of the United States by Great Britain, representing the first successful war of independence against a European power. The current constitution was adopted in 1788, after the Articles of Confederation, the first ten amendments, collectively named the Bill of Rights, were ratified in 1791 and designed to guarantee many fundamental civil liberties. During the second half of the 19th century, the American Civil War led to the end of slavery in the country. By the end of century, the United States extended into the Pacific Ocean. The Spanish–American War and World War I confirmed the status as a global military power. The end of the Cold War and the dissolution of the Soviet Union in 1991 left the United States as the sole superpower. The U. S. is a member of the United Nations, World Bank, International Monetary Fund, Organization of American States. The United States is a developed country, with the worlds largest economy by nominal GDP. It ranks highly in several measures of performance, including average wage, human development, per capita GDP. While the U. S. economy is considered post-industrial, characterized by the dominance of services and knowledge economy, the United States is a prominent political and cultural force internationally, and a leader in scientific research and technological innovations. In 1507, the German cartographer Martin Waldseemüller produced a map on which he named the lands of the Western Hemisphere America after the Italian explorer and cartographer Amerigo Vespucci
2.
Utah
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Utah is a state in the western United States. It became the 45th state admitted to the U. S. on January 4,1896, Utah is the 13th-largest by area, 31st-most-populous, and 10th-least-densely populated of the 50 United States. Utah has a population of more than 3 million, approximately 80% of whom live along the Wasatch Front, Utah is bordered by Colorado to the east, Wyoming to the northeast, Idaho to the north, Arizona to the south, and Nevada to the west. It also touches a corner of New Mexico in the southeast, approximately 62% of Utahns are reported to be members of The Church of Jesus Christ of Latter-day Saints or LDS, which greatly influences Utahn culture and daily life. The LDS Churchs world headquarters is located in Salt Lake City, Utah is the only state with a majority population belonging to a single church. The state is a center of transportation, education, information technology and research, government services, mining, in 2013, the U. S. Census Bureau estimated that Utah had the second fastest-growing population of any state. St. George was the metropolitan area in the United States from 2000 to 2005. Utah also has the 14th highest median income and the least income inequality of any U. S. state. A2012 Gallup national survey found Utah overall to be the best state to live in based on 13 forward-looking measurements including various economic, lifestyle, the name Utah is derived from the name of the Ute tribe. It means people of the mountains in the Ute language, according to other sources Utah is derived from the Apache name Yudah which means Tall. These Native American tribes are subgroups of the Ute-Aztec Native American ethnicity and were sedentary, the Ancestral Pueblo people built their homes through excavations in mountains, and the Fremont people built houses of straw before disappearing from the region around the 15th century. Another group of Native Americans, the Navajo, settled in the region around the 18th century, in the mid-18th century, other Uto-Aztecan tribes, including the Goshute, the Paiute, the Shoshone, and the Ute people, also settled in the region. These five groups were present when the first European explorers arrived, the southern Utah region was explored by the Spanish in 1540, led by Francisco Vásquez de Coronado, while looking for the legendary Cíbola. A group led by two Catholic priests—sometimes called the Dominguez-Escalante Expedition—left Santa Fe in 1776, hoping to find a route to the coast of California, the expedition traveled as far north as Utah Lake and encountered the native residents. The Spanish made further explorations in the region, but were not interested in colonizing the area because of its desert nature, in 1821, the year Mexico achieved its independence from Spain, the region became known as part of its territory of Alta California. European trappers and fur traders explored some areas of Utah in the early 19th century from Canada, the city of Provo, Utah was named for one, Étienne Provost, who visited the area in 1825. The city of Ogden, Utah was named after Peter Skene Ogden, in late 1824, Jim Bridger became the first known English-speaking person to sight the Great Salt Lake. Due to the salinity of its waters, Bridger thought he had found the Pacific Ocean
3.
Chairlift
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They are the primary onhill transport at most ski areas, but are also found at amusement parks, various tourist attractions, and increasingly in urban transport. Depending on carrier size and loading efficiency, a passenger ropeway can move up to 4000 people per hour, and the fastest lifts achieve operating speeds of up to 12 m/s or 43.2 km/h. The two-person double chair, which for years was the workhorse of the ski industry. The four person detachable chairlift can transport 2400 people per hour with an average speed of 5 m/s. Some bi and tri cable elevated ropeways and reversible tramways achieve much greater operating speeds, a chairlift consists of numerous components to provide safe efficient transport. Especially at ski areas, chairlifts are referred to with a ski industry vernacular, a one-person lift is a single, a two-person lift is a double, a three-person lift a “triple”, four-person lifts are “quads”, and a six-person lift is a six pack. If the lift is a chairlift, it is typically referred to as a “high-speed” lift. Because fixed grip lifts move faster than detachables at load and unload, misloads are more frequent on fixed grips, detachable grips allow a greater rope speed to be used, usually twice that of a fixed grip chair, while simultaneously having slower loading and unloading sections. The capacity of a lift is constrained by the power, the rope speed, the carrier spacing, the vertical displacement. Human passengers can load only so quickly until loading efficiency decreases, the rope is the defining characteristic of an elevated passenger ropeway. The rope stretches and contracts as the tension exerted upon it increases and decreases, the fibre core contains a lubricant which protects the rope from corrosion and also allows for smooth flexing operation. The rope must be lubricated to ensure safe operation and long life. Various techniques are used for constructing the rope, dozens of wires are wound into a strand. Several strands are wound around a core, their twist is oriented in the same or opposite direction as the individual wires. Rope is constructed in a fashion, and must be spliced together before carriers are affixed. Splicing involves unwinding long sections of either end of the rope, sections of rope must be removed, as the strands overlap during the splicing process. Every lift involves at least two terminals and may also have intermediate supporting towers, a bullwheel in each terminal redirects the rope, while sheaves on the towers support the rope well above the ground. The number of towers is engineered based on the length and strength of the rope, worst case environmental conditions, the bullwheel with the prime mover is called the drive bullwheel, the other is the return bullwheel
4.
Aerial tramway
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An aerial tramway, sky tram, cable car, ropeway or aerial tram is a type of aerial lift which uses one or two stationary ropes for support while a third moving rope provides propulsion. With this form of lift, the grip of an aerial tramway cabin is fixed onto the propulsion rope, as such, careful phrasing is necessary to prevent confusion. It is also called a ropeway or even incorrectly referred to as a gondola lift. A gondola lift has cabins suspended from a continuously circulating cable whereas aerial trams simply shuttle back, in Japan, the two are considered as the same category of vehicle and called ropeway, while the term cable car means Cable car and funicular. An aerial railway where the vehicles are suspended from a track is known as a suspension railway. An aerial tramway consists of one or two fixed cables, one loop of cable, and a number of passenger cabins, the fixed cables provide support for the cabins while the haulage rope, by means of a grip, is solidly connected to the truck. An electric motor drives the haulage rope which provides propulsion, Aerial tramways differ from gondola lifts in that gondola lifts are considered continuous systems. A similar system of cables is used in a funicular railway, the two passenger cabins, which carry from 4 to over 150 people, are situated at opposite ends of the loops of cable. Thus, while one is coming up, the other is going down the mountain, some aerial trams have only one cabin, which lends itself better for systems with small elevation changes along the cable run. The first operational aerial tram was built in 1644 by Adam Wiebe in Gdańsk and it was moved by horses and used to move soil over the river to build defences. It is called the first known cable lift in European history and it is not known how long this lift was used. In any case, it would be another 230 years before Germany would get the cable lift. Other mining systems were developed in the 1860s by Hodgson, Hallidie went on to perfect a line of mining and people tramways after 1867 in California and Nevada. Tramways are sometimes used in regions to carry ore from a mine located high on the mountain to an ore mill located at a lower elevation. Ore tramways were common in the early 20th century at the mines in North and South America, one can still be seen in the San Juan Mountains of the US state of Colorado. Over one thousand mining tramways were built around the world—Spitsbergen, Russia, Alaska, Argentina, New Zealand and this experience was replicated with the use of tramways in the First World War particularly on the Isonzo Front in Italy. The German firm of Bleichert built hundreds of freight and military tramways, strangely, Bleichert even built the first tourist tramway at Bolzano/Bozen, in then Tyrolian Austria in 1913. Other firms entered the mining tramway business- Otto, Leschen, Breco Ropeways Ltd, ceretti and Tanfani, and Riblet for instance
5.
Gondola lift
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A gondola lift, as opposed to a cable car, is a means of cable transport and type of aerial lift which is supported and propelled by cables from above. It consists of a loop of cable that is strung between two stations, sometimes over intermediate supporting towers. The cable is driven by a bullwheel in a terminal, which is connected to an engine or electric motor. They are often considered continuous systems since they feature a haul rope which moves and circulates around two terminal stations. Depending on the combination of cables used for support and/or haulage and the type of grip, the capacity, cost, because of the proliferation of such systems in the Alpine regions of Europe, the French language name of Télécabine is also used in an English language context. Gondola lifts should not be confused with cable cars or the US aerial tramways as the latter solely operates with fixed grips and simply shuttles back and forth between two end terminals. In some systems the passenger cabins, which can hold between two and 8 people, are connected to the cable by means of spring-loaded grips. These grips allow the cabin to be detached from the cable and slowed down in the terminals, to allow passengers to board. Doors are almost always automatic and controlled by a lever on the roof or on the undercarriage that is pushed up or down, cabins are driven through the terminals either by rotating tires, or by a chain system. To be accelerated to and decelerated from line speed, cabins are driven along by progressively swifter rotating tires until they reach line or terminal speed, on older installations, gondolas are accelerated manually by an operator. Gondola lifts can have intermediate stops that allow for uploading and downloading on the lift, examples of a lift with three stops instead of the standard two are the Village Gondola and the Excalibur Gondolas at Whistler Blackcomb. In 1986, Doppelmayr built the worlds first eight-passenger gondola at Steamboat Ski Resort, such a system is called Pulse Cabin because usually more than one cabin are loaded at a time before the trip begins. Another type of lift is the bi-cable gondola, which has one other stationary cable, besides the main haul rope. One of the famous examples of this type of lift include the Ngong Ping Cable Car in Hong Kong, the Singapore Cable Car. This system has the advantage that the stationary cables strength and properties can be tailored to each span, there are also tri-cable gondolas that have two stationary cables that support the cabins. They differ from cable cars in that the latter consist only of one or two usually larger cabins, moving up and down, not circulating, bi and tri cable systems provide greater lateral stability allowing the system to operate in higher cross-winds. Open-air gondolas, or cabriolet as commonly called, are uncommon and are quite primitive because they are exposed to the elements. Their cabins are usually hollow cylinder, open from chest height up, with a floor and they are usually used as village gondolas and for short distances
6.
Surface lift
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A surface lift is a means of cable transport and is a transportation system used to transport skiers and snowboarders where riders remain on the ground as they are pulled uphill. Once prevalent, they have gradually been overtaken in popularity by higher capacity aerial lifts like chairlifts, today, surface lifts are most often found on beginner slopes and very small ski areas. Surface lifts have many disadvantages compared to aerial lifts, they require more passenger skills, surface must be continuous, they impede skiable terrain, slow speed, with the increase in snowboarding, surface lifts are replaced by chairlifts. They are often utilized at glacier skiing resorts because their supports can be anchored in glacier ice due to the lower forces, the first surface lift was built in 1908 by German Robert Winterhalder in Schollach/Eisenbach, Hochschwarzwald. A steam-powered toboggan tow,950 feet in length, was built in Truckee, California, the first skier-specific tow in North America was apparently installed in 1933 by Alec Foster at Shawbridge in the Laurentians outside Montreal, Quebec. The Shawbridge tow was quickly copied at Woodstock, Vermont in New England in 1934 by Bob and Betty Royce and their tow was driven by the rear wheel of a Ford Model A. Their relative simplicity made tows widespread and contributed to an explosion of the sport in the United States, before tows, only people willing to walk uphill could ski. Suddenly relatively unathletic people could participate, greatly increasing the appeal of the sport, within five years, more than 100 tow ropes were operating in North America. A rope tow consists of a cable or rope running through a bullwheel at the bottom and one at the top, in the simplest case, passengers grab hold of the rope and are pulled along while standing on their skis or snowboards and sliding up the hill. The grade of this style of rope tow is limited by passenger grip strength, metal handles can be attached to the rope to help grip. Steeper, faster and longer rope tows require the use of a nutcracker, the rider wears a harness around the hips. To this is attached a clamp, much like the nutcracker from which it derives its name and this eliminates the need to hold on and allows the rope to be supported at waist height by pulleys. This ssystem was used on many fields worldwide from the 1940s, a T-bar or J-bar lift is employed for low-capacity slopes in large resorts and small local areas. It consists of a cable loop running over a series of wheels. Hanging from the rope are a series of vertical recoiling cables, the horizontal bar is placed behind the skiers buttocks or between the snowboarders legs, and pushes the passengers uphill while they slide across the ground. The first T-bar lift in the United States was installed in 1940 at the Pico Mountain ski area and it was considered a great improvement over the rope tow. An earlier, potentially home-grown, T-bar was installed at Rib Mountain, Wisconsin, in 1937, invented in the 1930s, J-Bars were installed in the 1930s in North America and Australia, with the Ski Hoist at Charlotte Pass in Australia dating from 1938. J-bars have been superseded by T-bars which have twice the capacity, a J-bar closely resembles a T-bar, except that each carrier holds only one passenger
7.
Snow
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Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes nucleate around particles in the atmosphere by attracting supercooled water droplets, snowflakes take on a variety of shapes, basic among these are platelets, needles, columns and rime. As snow accumulates into a snowpack, it may blow into drifts, over time, accumulated snow metamorphoses, by sintering, sublimation and freeze-thaw. Where the climate is cold enough for year-to-year accumulation, a glacier may form, otherwise, snow typically melts seasonally, causing runoff into streams and rivers and recharging groundwater. Major snow-prone areas include the regions, the upper half of the Northern Hemisphere and mountainous regions worldwide with sufficient moisture. In the Southern Hemisphere, snow is confined primarily to mountainous areas, Snow affects ecosystems, as well, by providing an insulating layer during winter under which plants and animals are able to survive the cold. Snow develops in clouds that themselves are part of a weather system. The physics of snow crystal development in clouds results from a set of variables that include moisture content. The resulting shapes of the falling and fallen crystals can be classified into a number of shapes and combinations. Occasionally, some plate-like, dendritic and stellar-shaped snowflakes can form under clear sky with a cold temperature inversion present. Two additional and locally productive sources of snow are lake-effect storms and elevation effects, miid-latitude cyclones are low pressure areas which are capable of producing anything from cloudiness and mild snow storms to heavy blizzards. During a hemispheres fall, winter, and spring, the atmosphere over continents can be cold enough through the depth of the troposphere to cause snowfall, in the Northern Hemisphere, the northern side of the low pressure area produces the most snow. For the southern mid-latitudes, the side of a cyclone that produces the most snow is the southern side, a cold front, the leading edge of a cooler mass of air, can produce frontal snowsqualls—an intense frontal convective line, when temperature is near freezing at the surface. The strong convection that develops has enough moisture to produce whiteout conditions at places which line passes over as the wind causes intense blowing snow. This type of snowsquall generally lasts less than 30 minutes at any point along its path, in cases where there is a large amount of vertical growth and mixing the squall may develop embedded cumulonimbus clouds resulting in lightning and thunder which is dubbed thundersnow. A warm front can produce snow for a period, as warm, moist air overrides below-freezing air, often, snow transitions to rain in the warm sector behind the front. The same effect occurs over bodies of salt water, when it is termed ocean-effect or bay-effect snow. The effect is enhanced when the air mass is uplifted by the orographic influence of higher elevations on the downwind shores
8.
Snowmaking
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Snowmaking is the production of snow by forcing water and pressurized air through a snow gun, also known as a snow cannon, on ski slopes. Snowmaking is mainly used at ski resorts to supplement natural snow and this allows ski resorts to improve the reliability of their snow cover and to extend their ski seasons from late autumn to early spring. Indoor ski slopes often use snowmaking and they can generally do so year-round as they have a climate-controlled environment. The production of snow requires low temperatures, the threshold temperature for snowmaking increases as humidity decreases. Wet bulb temperature is used as a metric since it takes air temperature, snowmaking is a relatively expensive process in its energy use, thereby limiting its use. Art Hunt, Dave Richey, and Wayne Pierce invented the snow cannon in 1950, in 1952, Grossingers Catskill Resort Hotel became the first in the world to use artificial snow. Snowmaking began to be used extensively in the early 1970s, many ski resorts depend heavily upon snowmaking. Snowmaking has achieved greater efficiency with increasing complexity, traditionally, snowmaking quality depended upon the skill of the equipment operator. Computer control supplements that skill with greater precision, such that a snow gun operates only when snowmaking is optimal, all-weather snowmakers have been developed by IDE. The key considerations in production are increasing water and energy efficiency. Snowmaking plants require water pumps and sometimes air compressors when using lances, the energy required to make artificial snow is about 0.6 -0.7 kW h/m³ for lances and 1 -2 kW h/m³ for fan guns. The density of snow is between 400 and 500 kg/m³ and the water consumption for producing snow is roughly equal to that number. Snowmaking begins with a water supply such as a river or reservoir, water is pushed up a pipeline on the mountain using very large electric pumps in a pump house. This water is distributed through a series of valves and pipes to any trails that require snowmaking. Many resorts also add a nucleating agent to ensure that as much water as possible freezes and these products are organic or inorganic materials that facilitate the water molecules to form the proper shape to freeze into ice crystals. The products are non-toxic and biodegradable, the next step in the snowmaking process is to add air using an air plant. This plant is often a building which contains electric or diesel industrial air compressors the size of a van or truck, however, in some instances air compression is provided using diesel-powered, portable trailer-mounted compressors which can be added to the system. Many fan-type snow guns have on-board electric air compressors, which allows for cheaper, a ski area may have the required high-output water pumps, but not an air pump
9.
Western United States
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The Western United States, commonly referred to as the American West, the Far West, or simply the West, traditionally refers to the region comprising the westernmost states of the United States. Because European settlement in the U. S. expanded westward after its founding, prior to about 1800, the crest of the Appalachian Mountains was seen as the western frontier. Since then, the frontier moved westward and eventually lands west of the Mississippi River came to be referred to as the West. The West contains several major biomes, the Western U. S. is the largest region of the country, covering more than half the land area of the United States. Given this expansive and diverse geography it is no wonder the region is difficult to specifically define, a majority of the historian respondents placed the eastern boundary of the West east of the Census definition out on the eastern edge of the Great Plains or on the Mississippi River. The survey respondents as a whole showed just how little agreement there was on the boundaries of the West, within a region as large and diverse as the Western United States, smaller areas with more closely shared demographics and geography have developed as subregions. Meanwhile, the states of Idaho, Montana, Oregon and Washington can be considered part of the Northwest or Pacific Northwest, West Texas in the Chihuahuan Desert may be considered as part of the Western U. S. Fort Worth has long laid claim to be Where the West Begins, the West is still one of the most sparsely settled areas in the United States with 49.5 inhabitants per square mile. Only Texas with 78.0 inhabitants/sq mi, Washington with 86.0 inhabitants/sq mi. and California with 213.4 inhabitants/sq mi. exceed the national average of 77.98 inhabitants/sq mi. The entire Western region has also strongly influenced by European, Hispanic or Latino, Asian and Native Americans. African and European Americans, however, continue to wield a stronger political influence because of the rates of citizenship and voting among Asians. The West also contains much of the Native American population in the U. S. particularly in the reservations in the Mountain. The Western United States has a sex ratio than any other region in the United States. Because the tide of development had not yet reached most of the West when conservation became an issue, agencies of the federal government own. National parks are reserved for activities such as fishing, camping, hiking, and boating, but other government lands also allow commercial activities like ranching, logging. The largest city in the region is Los Angeles, located on the West Coast, Other West Coast cities include San Diego, San Bernardino, San Jose, San Francisco, Oakland, Bakersfield, Sacramento, Seattle, Tacoma, and Portland. Prominent cities in the Mountain States include Denver, Colorado Springs, Phoenix, Tucson, Albuquerque, Las Vegas, Salt Lake City, Boise, El Paso, and Cheyenne. Along the Pacific Ocean coast lie the Coast Ranges, which and they collect a large part of the airborne moisture moving in from the ocean
10.
Wasatch Range
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The Wasatch Range /ˈwɑːsætʃ/ is a mountain range that stretches approximately 160 miles from the Utah-Idaho border, south through central Utah in the western United States. It is the edge of the greater Rocky Mountains. The northern extension of the Wasatch Range, the Bear River Mountains, extends just into Idaho, according to the Utah History Encyclopedia, Wasatch in Ute means mountain pass or low pass over high range. According to William Bright the mountains were named for a Shoshoni leader who was named with the Shoshoni term wasattsi, since the earliest days of settlement, the majority of Utahs population has chosen to settle along the ranges western front, where numerous river drainages exit the mountains. The mountains were a source of water, timber. Today, 85% of Utahs population lives within 15 miles of the Wasatch Range and this concentration is known as the Wasatch Front and has a population of just over 2,000,000 residents. Salt Lake City lies between the Wasatch Range and the Great Salt Lake, at 11,928 feet, Mount Nebo, a triple peak rising above Nephi, Utah at the southern end of the range, is the highest peak of the Wasatch. In some places the mountains rise immediately from the base elevation of 4,330 feet to over 11,000 feet. Since they top out just below 12,000 feet, Wasatch peaks are not especially high compared to the Colorado Rockies or even the Uinta Mountains, the other main portion of the Rocky Mountains in Utah. However, they are sculpted by glaciers, yielding notably rugged and they also receive heavy falls of snow, in some places over 500 inches per year. This great snowfall, with its runoff, made possible a prosperous urban strip of some 25 cities along nearly 100 miles of mountain frontage. The Wasatch Range is home to a concentration of ski areas, with 11 stretching from Sundance in northern Utah County to Powder Mountain. There is also one ski resort in the Bear River Mountains, Park City alone is bordered by two ski resorts. Further north, Big Cottonwood Canyon features tricky climbing on quartzite, the canyons are located within 24 miles of downtown Salt Lake City and the year-round paved roadways can reach 5,000 ft higher in elevation above the city within a short distance. Dirt roads readily drivable in passenger cars with moderate clearance stretch up from Park City, Heber and these reach about 10,000 feet above sea level and provide impressive long-range high country views. Mount Nebo, the highest peak of the Wasatch, is located at the edge of the range. The Colorado Plateau comes to its northwest corner here as it meets the end of the Rocky Mountains. The range is punctuated by a series of faults, chief among them the Wasatch fault
11.
Ogden, Utah
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Ogden /ˈɒɡdɛn/ is a city and the county seat of Weber County, Utah, United States, approximately 10 miles east of the Great Salt Lake and 40 miles north of Salt Lake City. The population was 84,316 in 2014, according to the US Census Bureau, the city served as a major railway hub through much of its history, and still handles a great deal of freight rail traffic which makes it a convenient location for manufacturing and commerce. Ogden is also known for its historic buildings, proximity to the Wasatch Mountains. Ogden is a city of the Ogden–Clearfield, Utah Metropolitan Statistical Area, which includes all of Weber, Morgan, Davis. The 2010 Census placed the Metro population at 597,159, in 2010, Forbes rated the Ogden-Clearfield MSA as the 6th best place to raise a family. Ogden has had a Sister City relationship to Hof since 1954, originally named Fort Buenaventura, the city of Ogden was the first permanent settlement by people of European descent in the region that is now Utah. It was established by the trapper Miles Goodyear in 1846 about a mile west of where downtown Ogden is currently located, in November 1847, Fort Buenaventura was purchased by the Mormon settlers for $1,950. There is some confusion in which Ogden was the first to set foot in the Utah city, peters older brother Samuel Ogden traveled though the western United States on an exploration trip in 1818. The site of the original Fort Buenaventura is now a Weber County park, Ogden is the closest sizable city to the Golden Spike location at Promontory Summit, Utah, where the First Transcontinental Railroad was joined in 1869. Railroad passengers traveling west to San Francisco from the eastern United States typically passed through Ogden, in 1972, The Church of Jesus Christ of Latter-day Saints completed construction of and dedicated the Ogden Utah Temple in Ogden. The temple was built to serve the large LDS population in the area, in 2010, the LDS Church announced a major renovation of the Ogden Temple and the adjacent Tabernacle. The Temple was rededicated in 2014, because Ogden has historically been the second largest city in Utah, it is home to a large number of historic buildings. However, by the 1980s, several Salt Lake City suburbs, the Defense Depot Ogden Utah operated in Ogden from 1941 to 1997. Some of its 1,128 acres has since converted into a commercial and industrial park called the Business Depot Ogden. Ogden is located at 41°13′11″N 111°58′16″W, at the foot of the Wasatch Mountains, according to the United States Census Bureau, the city has a total area of 26.6 square miles, all land. Elevations in the city range from about 4,300 to 5,200 feet above sea level, the Ogden and Weber Rivers, which originate in the mountains to the east, flow through the city and meet at a confluence just west of the city limits. Pineview Dam is located in the Ogden River Canyon 7 miles east of Ogden, the reservoir behind the dam provides over 110,000 acre feet of water storage and water recreation for the area. Prominent mountain peaks near Ogden include Mount Ogden to the east, Ogden experiences a dry summer continental climate
12.
2002 Winter Olympics
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Approximately 2,400 athletes from 78 nations participated in 78 events in fifteen disciplines, held throughout 165 sporting sessions. The 2002 Winter Olympics and the 2002 Paralympic Games were both organized by the Salt Lake Organizing Committee, Utah became the fifth state in the United States to host the Olympic Games, and the 2002 Winter Olympics are the most recent games to be held in the United States. These were the first Olympic Games under the IOC presidency of Jacques Rogge, the opening ceremony was held on February 8,2002, and sporting competitions were held up until the closing ceremony on February 24,2002. Production for both ceremonies was designed by Seven Nielsen, and music for both ceremonies was directed by Mark Watters, Salt Lake City became the most populous area ever to have hosted the Winter Olympics, although the two subsequent host cities populations were larger. Following a trend, the 2002 Olympic Winter Games were also larger than all prior Winter Games, with 10 more events than the 1998 Winter Olympics in Nagano, Japan. The Salt Lake Games faced a scandal and some local opposition during the bid. Nevertheless, from sporting and business standpoints, this was one of the most successful Winter Olympiads in history, over 2 billion viewers watched more than 13 billion viewer-hours. The Games were also financially successful raising more money with fewer sponsors than any prior Olympic Games, the surplus was used to create the Utah Athletic Foundation, which maintains and operates many of the remaining Olympic venues. U. S. Federal subsidies amounted to $1.3 billion, Salt Lake City was chosen over Québec City, Canada, Sion, Switzerland, and Östersund, Sweden, on June 16,1995, at the 104th IOC Session in Budapest, Hungary. The 1976 Winter Olympics were ultimately awarded to Innsbruck, Austria, 1Because of the no-commercialization policy of the Olympics, the Delta Center, now the Vivint Smart Home Arena, was labeled as the Salt Lake Ice Center, causing some confusion for visitors. The Oxford Olympics Study established the outturn cost of the Salt Lake City 2002 Winter Olympics at USD2.5 billion in 2015-dollars and cost overrun at 24% in real terms. This includes sports-related costs only, that is, operational costs incurred by the committee for the purpose of staging the Games. The competition venues, the Olympic village, international broadcast center, and media and press center, average cost for Winter Games since 1960 is USD3.1 billion, average cost overrun is 142%. A total 78 National Olympic Committees sent athletes to the Salt Lake City games, cameroon, Hong Kong, Nepal, Tajikistan, and Thailand participated in their first Winter Olympic Games. There were 78 events contested in 7 sports, in the following calendar for the 2002 Winter Olympic Games, each blue box represents an event competition, such as a qualification round, on that day. The yellow boxes represent days during which medal-awarding finals for a sport are held, the number in each box represents the number of finals that were contested on that day. All dates are in Mountain Standard Time Host country To sort this table by nation, total medal count, or any other column, several medals records were set and/or tied. They included, Norway tied the Soviet Union at the 1976 Winter Olympics for most gold medals at a Winter Olympics, germany set a record for most total medals at a Winter Olympics, with 36
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