1.
Manzanar
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Located at the foot of the Sierra Nevada in Californias Owens Valley between the towns of Lone Pine to the south and Independence to the north, it is approximately 230 miles north of Los Angeles. Long before the first incarcerees arrived in March 1942, Manzanar was home to Native Americans, ranchers and miners formally established the town of Manzanar in 1910, but abandoned the town by 1929 after the City of Los Angeles purchased the water rights to virtually the entire area. As different as these groups were, their histories displayed a common thread of forced relocation, the primary focus is the Japanese American incarceration era, as specified in the legislation that created the Manzanar National Historic Site. The site also interprets the former town of Manzanar, the days, the settlement by the Owens Valley Paiute. Let us review the main points of the debate, over 120,000 residents of the U. S. A. two thirds of whom were American citizens, were incarcerated under armed guard. There were no crimes committed, no trials, and no convictions, to detain American citizens in a site under armed guard surely constitutes a concentration camp. But what were the used by the government officials who were involved in the process. Raymond Okamura provides us with a detailed list of terms, lets consider three such euphemisms, evacuation, relocation, and non-aliens. Earthquake and flood victims are evacuated and relocated, the words refer to moving people in order to rescue and protect them from danger. The official government policy makers consistently used evacuation to refer to the removal of the Japanese Americans. These are euphemisms as the terms do not imply forced removal nor incarceration in enclosures patrolled by armed guards. Hirabayashi went on to describe the harm done by the use of such euphemisms, the harm in continuing to use the governments euphemisms is that it disguises or softens the reality which subsequently has been legally recognized as a grave error. The actions abrogated some fundamental principles underlying the Constitution, the document under which we govern ourselves. This erosion of fundamental rights has consequences for all citizens of our society, some have argued that the Nazi Germany camps during the Holocaust were concentration camps and to refer to the Japanese American camps likewise would be an affront to the Jews. It is certainly true that the Japanese Americans did not suffer the fate of the Jews in the terrible concentration camps or death camps where Nazi Germany practiced a policy of genocide. Although the loss of life was minimal in Americas concentration camps, michi and Walter Weglyns research concerning Nazi Germanys euphemisms for their concentration camps revealed such phrases as protective custody camps, reception centers, and transit camps. Ironically, two Nazi euphemisms were identical to our governments usage, assembly centers and relocation centers and it might be well to point out, also, that the Nazis were not operating under the U. S. Constitution. Comparisons usually neglect to point out that Hitler was operating under the rules of the Third Reich
2.
Owens Valley
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The mountain peaks on either side reach above 14,000 feet in elevation, while the floor of the Owens Valley is at 4,000 feet, making the valley one of the deepest in the United States. The Sierra Nevada casts the valley in a shadow, which makes Owens Valley the Land of Little Rain. The bed of Owens Lake, now a predominantly dry endorheic alkali flat and these episodes inspired aspects of the film Chinatown. Towns in the Owens Valley include Bishop, Lone Pine, Independence, the major road in the valley is U. S. Route 395. Owens Valley is a graben—a downdropped block of land between two vertical faults, Owens Valley is the westernmost graben in the Basin and Range Province. It is also part of a trough which extends from Oregon to Death Valley called the Walker Lane, the western flank of much of the valley has large moraines coming off the Sierra Nevada. These unsorted piles of rock, boulders, and dust were pushed to where they are by glaciers during the last ice age, an excellent example of a moraine is on State Route 168 as it climbs into Buttermilk Country. This graben was formed by a series of earthquakes, such as the 1872 Lone Pine earthquake. The topmost part of this escarpment is exposed at Alabama Hills, the Owens Valley is also part of the Long Valley Caldera, a super-volcano that last erupted 260,000 years ago. It is filled with many mini-volcanoes, which look like hills, see also, Inyo and Mono Craters. Smaller versions of the Devils Postpile, can be found, for example, the valley contains plants adapted to alkali flat habitat. One of these, the Owens Valley checkerbloom, is endemic to Owens Valley, the valley was inhabited in late prehistoric times by the Timbisha in the extreme south end around Owens Lake and by the Mono tribe in the central and northern portions of the valley. The Timbisha speak the Timbisha language, classified in the Numic branch of Uto-Aztecan language family, the closest related languages are Shoshoni and Comanche. The Eastern Mono speak a dialect of the Mono language which is also Numic, the Timbisha presently live in Death Valley at Furnace Creek although most families also have summer homes in the Lone Pine colony. The Eastern Mono live in colonies from Lone Pine to Bishop. Trade between Native Americans of the Owens Valley between coastal tribes such as the Chumash has been indicated by the archaeological record, on May 1,1834, Joseph R. Walker entered Owens Valley at the mouth of Walker Pass. He and his group of 52 men traveled up the valley on their way back to the Humboldt Sink, fremont named the Owens valley, river and lake for Richard Owens, one of his guides. Camp Independence was established on Oak Creek nearby modern Independence, California, on July 4,1862, from 1942 to 1945 during World War II, the first Japanese American Internment camp operated in the valley at Manzanar near Independence, California
3.
Summit
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A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. Mathematically, a summit is a maximum in elevation. The topographic terms acme, apex, peak, and zenith are synonymous, the UIAA definition is that a summit is independent if it has a prominence of 30 metres or more, it is a mountain if it has a prominence of at least 300 metres. This can be summarised as follows, A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top, Summit may also refer to the highest point along a line, trail, or route. In many parts of the western United States, the term refers to the highest point along a road, highway. For example, the highest point along Interstate 80 in California is referred to as Donner Summit while the highest point on Interstate 5 is Siskiyou Mountain Summit, geoid Hill List of highest mountains Maxima and minima Nadir Summit accordance Peak finder
4.
Topographic prominence
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It is a measure of the independence of a summit. A peaks key col is a point on this contour line. By convention, the prominence of Mount Everest, the Earths highest mountain, is taken to equal the elevation of its summit above sea level, if the peaks prominence is P metres, to get from the summit to any higher terrain one must descend at least P metres. Together with the convention for Mount Everest, this implies that the prominence of any island or continental highpoint is equal to its elevation above sea level, for every ridge connecting the peak to higher terrain, find the lowest point on the ridge. The key col is defined as the highest of these cols, the prominence is the difference between the elevation of the peak and the elevation of the key col. The following mental exercise may illustrate the meaning of topographic prominence, imagine you are standing at the top of a peak and imagine that an imaginary sea level rises to your feet. Now slowly lower the sea level and an imaginary island appears beneath your feet. Your island will grow and will merge with other islands that emerge, the parent peak may be either close or far from the subject peak. The summit of Mount Everest is the parent peak of Aconcagua at a distance of 17,755 km, the key col may also be close or far from the subject peak. The key col for Aconcagua is the Bering Strait at a distance of 13,655 km, the key col for the South Summit of Mount Everest is about 100 m distant. Prominence is interesting to many mountaineers because it is a measurement that is strongly correlated with the subjective significance of a summit. Peaks with low prominences are either subsidiary tops of some higher summit or relatively insignificant independent summits, peaks with high prominences tend to be the highest points around and are likely to have extraordinary views. Only summits with a sufficient degree of prominence are regarded as independent mountains, for example, the worlds second-highest mountain is K2. While Mount Everests South Summit is taller than K2, it is not considered an independent mountain because it is a subsummit of the main summit, many lists of mountains take topographic prominence as a criterion for inclusion, or cutoff. John and Anne Nuttalls The Mountains of England and Wales uses a cutoff of 15 m, in the contiguous United States, the famous list of fourteeners uses a cutoff of 300 ft /91 m. Also in the U. S.2000 feet of prominence has become a threshold that signifies that a peak has major stature. This generates lists of peaks ranked by prominence, which are different from lists ranked by elevation. Such lists tend to emphasize isolated high peaks, such as range or island high points, one advantage of a prominence-ranked list is that it needs no cutoff, since a peak with high prominence is automatically an independent peak
5.
Topographic isolation
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The topographic isolation of a summit is the minimum great-circle distance to a point of equal elevation, representing a radius of dominance in which the peak is the highest point. It can be calculated for small hills and islands as well as for major mountain peaks, the following sortable table lists the Earths 40 most topographically isolated summits. The nearest peak to Germanys highest mountain, the 2, 962-metre-high Zugspitze, the distance between the Zugspitze and this contour is 25.8 km, the Zugspitze is thus the highest peak for a radius of 25.8 km around. Its isolation is thus 25.8 km, because there are no higher mountains than Mount Everest, it has no definitive isolation. Many sources list its isolation as the circumference of the earth over the poles or – questionably, after Mount Everest the Aconcagua, highest mountain of the American continents, has the greatest isolation of all mountains. There is no land for 16,534 kilometres when its height is first exceeded by Tirich Mir in the Hindu Kush. Mont Blanc is the highest mountain of the Alps, the geographically nearest higher mountains are all in the Caucasus. The Kukurtlu, which rises near the Elbrus, is the peak for Mont Blanc. com Canadian Mountain Encyclopedia peakbagger. com peaklist. org peakware. com World Mountain Encyclopedia summitpost. org
6.
Mount Whitney
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Mount Whitney is the highest summit in the contiguous United States and the Sierra Nevada, with an elevation of 14,505 feet. The west slope of the mountain is in Sequoia National Park, the east slope is in the Inyo National Forest in Inyo County. The summit of Whitney is on the Sierra Crest and the Great Basin Divide and it lies near many of the highest peaks of the Sierra Nevada. The peak rises dramatically above the Owens Valley, sitting 10,778 feet or just over two miles above the town of Lone Pine 15 miles to the east, in the Owens Valley. It rises more gradually on the west side, lying only about 3,000 feet above the John Muir Trail at Guitar Lake, the mountain is partially dome-shaped, with its famously jagged ridges extending to the sides. Mount Whitney is above the line and has an alpine climate. Very few plants grow near the summit, one example is the Skypilot, the only animals are transient, such as the butterfly Parnassius phoebus and the gray-crowned rosy finch. The mountain is the highest point on the Great Basin Divide, waterways on the west side of the peak flow into Whitney Creek, which flows into the Kern River. The Kern River terminates in the Tulare Basin, during very wet years, water overflows from the Tulare Basin into the San Joaquin River which flows to the Pacific Ocean. From the east, water from Mount Whitney flows to Lone Pine Creek, which joins the Owens River, which in turn terminates at Owens Lake, the estimated elevation of the summit of Mount Whitney has changed over the years. The technology of elevation measurement has become refined and, more importantly. The peak was commonly said to be at 14,494 ft, an older plaque on the summit reads elevation 14,496.811 feet but this was estimated using the older vertical datum from 1929. Since then the shape of the Earth has been estimated more accurately, using a new vertical datum established in 1988 the benchmark is now estimated to be at 14,505 ft. The rise is caused by a fault system that runs along the eastern base of the Sierra. Thus, the granite that forms Mount Whitney is the same as the granite that forms the Alabama Hills, the raising of Whitney is due to the same geological forces that cause the Basin and Range Province, the crust of much of the intermontane west is slowly being stretched. The granite that forms Mount Whitney is part of the Sierra Nevada batholith, in Cretaceous time, masses of molten rock that originated from subduction rose underneath what is now Whitney and solidified underground to form large expanses of granite. In July 1864, the members of the California Geological Survey named the peak after Josiah Whitney, during the same expedition, geologist Clarence King attempted to climb Whitney from its west side, but stopped just short. In 1871, King returned to climb what he believed to be Whitney, upon learning of his mistake in 1873, King finally completed his own first ascent of Whitney, but did so a month too late to claim the first recorded ascent
7.
Sierra Peaks Section
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The Sierra Peaks Section was established in 1955. The Section maintains historic summit registers at Bancroft Library on the University of California, Berkeley campus. To become a member of the SPS, one must be a Sierra Club member and have climbed at least six peaks on the SPS List, for verification purposes, two of those ascents must be done on an official SPS trip. Completing the list is highly prestigious in American mountaineering circles, the list is divided into three levels of importance. The Emblem peaks are considered the most iconic peaks of the Sierra Nevada, finally, there are the numerous general peaks of lesser note. The list is an example of a decision by committee list with the peaks on the list being determined by the Sierra Club, Peaks are occasionally added or removed from the list due to a variety of factors, such as accessibility, notability, and interest. The list is followed by thousands of hikers and has noted in numerous books. There are 15 Emblem peaks,35 Mountaineers peaks, and 197 general peaks, the elevations listed below are those officially described on the list, and may not be the actual elevations of those peaks, although they are usually accurate to within 50 feet. Other peak bagging lists, New England Fifty Finest Adirondack High Peaks Secor, the High Sierra, peaks, passes, trail
8.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
9.
Inyo County, California
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Inyo County is a county in the U. S. state of California. As of the 2010 census, the population was 18,546, Inyo County is on the east side of the Sierra Nevada and southeast of Yosemite National Park in Central California. It contains the Owens River Valley, it is flanked to the west by the Sierra Mountains and to the east by the White Mountains, Mount Whitney, the highest peak in the Contiguous United States, is on Inyo Countys western border. The Badwater Basin in Death Valley National Park, the lowest place in North America, is in eastern Inyo County. The two points are not visible from other, but both can be observed from the Panamint Range on the west side of Death Valley, above the Panamint Valley. It has the biggest elevation difference of all of the counties, with an area of 10,192 square miles, Inyo County is the second-largest county by area in California, after San Bernardino County. Almost one-half of that area is within Death Valley National Park, however, with a population density of 1.8 people per square mile, it has the lowest population density of any county in California. Present day Inyo county has been the homeland for thousands of years of the Mono tribe, Coso people, Timbisha. They spoke the Timbisha language and the Mono language with Mono traditional narratives, the descendants of these ancestors continue to live in their traditional homelands in the Owens River Valley and in Death Valley National Park. Inyo County was formed in 1866 from the territory of the unorganized Coso County created on April 4,1864 from parts of Mono and it acquired more territory from Mono County in 1870 and Kern County and San Bernardino County in 1872. For many years it has been believed that the county derived its name from the Mono tribe of Native Americans name for the mountains in its former homeland. The local Paiutes responded that that was the land of Inyo and they meant by this that those lands belonged to the Shoshone tribe headed by a man whose name was Inyo. Indian George, a fixture of many of the stories of early Death Valley days, was Inyos son, in order to provide water needs for the growing City of Los Angeles, water was diverted from the Owens River into the Los Angeles Aqueduct in 1913. The Owens River Valley cultures and environments changed substantially, from the 1910s to 1930s the Los Angeles Department of Water and Power purchased much of the valley for water rights and control. In 1941 the Los Angeles Department of Water and Power extended the Los Angeles Aqueduct system further upriver into the Mono Basin, Inyo County is host to a number of natural superlatives. Among them are, Mount Whitney, with an elevation of 14,505 feet, is the highest point in the contiguous United States, the 12th highest peak in the U. S. and the 24th highest peak in North America. S. Census Bureau, the county has an area of 10,227 square miles. It is the second-largest county by area in California and the ninth-largest in the United States, Death Valley National Park Inyo National Forest Manzanar National Historic Site There are 22 official wilderness areas in Inyo County that are part of the National Wilderness Preservation System
10.
Mountain range
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A mountain range is a geographic area containing numerous geologically related mountains. A mountain system or system of ranges, sometimes is used to combine several geological features that are geographically related. Mountain ranges are usually segmented by highlands or mountain passes and valleys, individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, most geologically young mountain ranges on the Earths land surface are associated with either the Pacific Ring of Fire or the Alpide Belt. The Andes is 7,000 kilometres long and is considered the worlds longest mountain system. The Alpide belt includes Indonesia and southeast Asia, through the Himalaya, the belt also includes other European and Asian mountain ranges. The Himalayas contain the highest mountains in the world, including Mount Everest, mountain ranges outside of these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Altai Mountains and the Hijaz Mountains. If the definition of a range is stretched to include underwater mountains. The mountain systems of the earth are characterized by a tree structure, the sub-range relationship is often expressed as a parent-child relationship. For example, the White Mountains of New Hampshire and the Blue Ridge Mountains are sub-ranges of the Appalachian Mountains, equivalently, the Appalachians are the parent of the White Mountains and Blue Ridge Mountains, and the White Mountains and the Blue Ridge Mountains are children of the Appalachians. The position of mountains influences climate, such as rain or snow, when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the side, it warms again and is drier. Often, a shadow will affect the leeward side of a range. Mountain ranges are constantly subjected to forces which work to tear them down. Erosion is at work while the mountains are being uplifted and long after until the mountains are reduced to low hills, rivers are traditionally believed to be the principle erosive factor on mountain ranges, with their ability of bedrock incision and sediment transport. The rugged topography of a range is the product of erosion. The basins adjacent to a mountain range are filled with sediments which are buried and turned into sedimentary rock. The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example and this mass of rock was removed as the range was actively undergoing uplift
11.
Sierra Nevada (U.S.)
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The Sierra Nevada is a mountain range in the Western United States, between the Central Valley of California and the Basin and Range Province. The vast majority of the lies in the state of California. The Sierra runs 400 miles north-to-south, and is approximately 70 miles across east-to-west, the Sierra is home to three national parks, twenty wilderness areas, and two national monuments. These areas include Yosemite, Sequoia, and Kings Canyon National Parks, the character of the range is shaped by its geology and ecology. More than one hundred years ago during the Nevadan orogeny. The range started to uplift four M. A. ago, the uplift caused a wide range of elevations and climates in the Sierra Nevada, which are reflected by the presence of five life zones. Uplift continues due to faulting caused by forces, creating spectacular fault block escarpments along the eastern edge of the southern Sierra. The Sierra Nevada has a significant history, the California Gold Rush occurred in the western foothills from 1848 through 1855. Due to inaccessibility, the range was not fully explored until 1912, the Sierra Nevada lies in Central and Eastern California, with a very small but historically important spur extending into Nevada. West-to-east, the Sierra Nevadas elevation increases gradually from 1,000 feet in the Central Valley to an height of about 10,500 feet at its crest only 50–75 miles to the east. The east slope forms the steep Sierra Escarpment, unlike its surroundings, the range receives a substantial amount of snowfall and precipitation due to orographic lift. The Sierra Nevada stretches from the Susan River and Fredonyer Pass in the north to Tehachapi Pass in the south and it is bounded on the west by Californias Central Valley and on the east by the Basin and Range Province. The geographical boundary between the Sierra and the Cascades is virtually indistinguishable, with the Fredonyer Pass designation being traditional, physiographically, the Sierra is a section of the Cascade-Sierra Mountains province, which in turn is part of the larger Pacific Mountain System physiographic division. The range is drained on its western slope by the Central Valley watershed, the northern third of the western Sierra is part of the Sacramento River watershed, and the middle third is drained by the San Joaquin River. The eastern slope watershed of the Sierra is much narrower, its rivers flow out into the endorheic Great Basin of eastern California and western Nevada. Although none of the eastern rivers reach the sea, many of the streams from Mono Lake southwards are diverted into the Los Angeles Aqueduct which provides water to Southern California, the height of the mountains in the Sierra Nevada increases gradually from north to south. Between Fredonyer Pass and Lake Tahoe, the range from 5,000 feet to more than 9,000 feet. The crest near Lake Tahoe is roughly 9,000 feet high, farther south, the highest peak in Yosemite National Park is Mount Lyell
12.
Topographic map
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Traditional definitions require a topographic map to show both natural and man-made features. A topographic map is published as a map series, made up of two or more map sheets that combine to form the whole map. A contour line is a line connecting places of equal elevation, however, in the vernacular and day to day world, the representation of relief is popularly held to define the genre, such that even small-scale maps showing relief are commonly called topographic. The study or discipline of topography is a broader field of study. Topographic maps are based on topographical surveys, performed at large scales, these surveys are called topographical in the old sense of topography, showing a variety of elevations and landforms. This is in contrast to older cadastral surveys, which primarily show property, the first multi-sheet topographic map series of an entire country, the Carte géométrique de la France, was completed in 1789. Topographic surveys were prepared by the military to assist in planning for battle, as such, elevation information was of vital importance. As they evolved, topographic map series became a resource in modern nations in planning infrastructure. Excluding borders, each sheet was 44 cm high and up to 66 cm wide, although the project eventually foundered, it left an indexing system that remains in use. TIGER was developed in the 1980s and used in the 1990, digital elevation models were also compiled, initially from topographic maps and stereographic interpretation of aerial photographs and then from satellite photography and radar data. Since all these were government projects funded with taxes and not classified for security reasons. Initial applications were mostly professionalized forms such as innovative surveying instruments, by the mid-1990s, increasingly user-friendly resources such as online mapping in two and three dimensions, integration of GPS with mobile phones and automotive navigation systems appeared. As of 2011, the future of standardized, centrally printed topographical maps is left somewhat in doubt, the various features shown on the map are represented by conventional signs or symbols. For example, colors can be used to indicate a classification of roads and these signs are usually explained in the margin of the map, or on a separately published characteristic sheet. Topographic maps are commonly called contour maps or topo maps. In the United States, where the national series is organized by a strict 7. 5-minute grid. Topographic maps conventionally show topography, or land contours, by means of contour lines, contour lines are curves that connect contiguous points of the same altitude. In other words, every point on the line of 100 m elevation is 100 m above mean sea level
13.
United States Geological Survey
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The United States Geological Survey is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its resources. The organization has four science disciplines, concerning biology, geography, geology. The USGS is a research organization with no regulatory responsibility. The USGS is a bureau of the United States Department of the Interior, the USGS employs approximately 8,670 people and is headquartered in Reston, Virginia. The USGS also has major offices near Lakewood, Colorado, at the Denver Federal Center, the current motto of the USGS, in use since August 1997, is science for a changing world. The agencys previous slogan, adopted on the occasion of its anniversary, was Earth Science in the Public Service. Prompted by a report from the National Academy of Sciences, the USGS was created, by a last-minute amendment and it was charged with the classification of the public lands, and examination of the geological structure, mineral resources, and products of the national domain. This task was driven by the need to inventory the vast lands added to the United States by the Louisiana Purchase in 1803, the legislation also provided that the Hayden, Powell, and Wheeler surveys be discontinued as of June 30,1879. Clarence King, the first director of USGS, assembled the new organization from disparate regional survey agencies, after a short tenure, King was succeeded in the directors chair by John Wesley Powell. Administratively, it is divided into a Headquarters unit and six Regional Units, Other specific programs include, Earthquake Hazards Program monitors earthquake activity worldwide. The National Earthquake Information Center in Golden, Colorado on the campus of the Colorado School of Mines detects the location, the USGS also runs or supports several regional monitoring networks in the United States under the umbrella of the Advanced National Seismic System. The USGS informs authorities, emergency responders, the media, and it also maintains long-term archives of earthquake data for scientific and engineering research. It also conducts and supports research on long-term seismic hazards, USGS has released the UCERF California earthquake forecast. The USGS National Geomagnetism Program monitors the magnetic field at magnetic observatories and distributes magnetometer data in real time, the USGS operates the streamgaging network for the United States, with over 7400 streamgages. Real-time streamflow data are available online, since 1962, the Astrogeology Research Program has been involved in global, lunar, and planetary exploration and mapping. USGS operates a number of related programs, notably the National Streamflow Information Program. USGS Water data is available from their National Water Information System database
14.
First ascent
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In climbing, a first ascent is the first successful, documented attainment of the top of a mountain, or the first to follow a particular climbing route. First ascents are notable because they entail genuine exploration, with risks, challenges. The person who performs the first ascent is called the first ascensionist, the details of the first ascents of even many prominent mountains are scanty or unknown, sometimes the only evidence of prior summiting is a cairn, artifacts, or inscriptions at the top. Today, first ascents are generally recorded and usually mentioned in guidebooks. Overwhelmingly, the idea of a first ascent is a one, especially in places such as Africa. There may be little or no evidence or documentation about the climbing activities of indigenous peoples living near the mountain. The term is used when referring to ascents made using a specific technique or taking a specific route, such as via the North Face. In rock climbing, some of the earlier first ascents, particularly for difficult routes, involved a mix of free, as a result, purist free climbers have developed the designation first free ascent to acknowledge ascents intentionally made more challenging by using equipment for protection only. Some other first ascents could be recorded for particular mountains or routes, one is the First Winter Ascent, which is, as the name easily suggests, the first ascent made during winter season. This is most important where the climate of winter is a factor in increasing the difficulty grade of the route, in the Northern Hemisphere conventional winter ascents are made between December 21 and March 21 and are not related to the conditions. Also in the Himalayan area, although Nepal and Chinas winter season permits start on December 1, another is the First Solo Ascent, which is the first ascent made by a single climber. This is most important on high-level rock climbing, when the climber has to provide his own security or even when climbing without any protection at all, another type of ascent, also known as FFA is the first female ascent. The term last ascent has been used to refer to an ascent of a mountain or face that has changed to such an extent – often because of rockfall – that the route no longer exists. It can also be used facetiously to refer to a climb that is so unpleasant or unaesthetic that no one would willingly repeat the first ascent partys ordeal. List of first ascents List of first ascents in the Alps List of first ascents in the Himalaya Glossary of climbing terms Alpinist Magazine – Peter Mortimers First Ascent, Issue 17
15.
Scrambling
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Scrambling is a walk up steep terrain involving the use of ones hands. It is a term that lies somewhere between hiking, hillwalking, mountaineering, and easy rock climbing. Alpine scrambling is a term applied to scrambling in high mountains like the Alps and the Rockies of North America, the Mountaineers climbing organization defines alpine scrambling as follows, Alpine Scrambles are off-trail trips, often on snow or rock, with a non-technical summit as a destination. A non-technical summit is one that is reached without the need for certain types of climbing equipment, however, this can mean negotiating lower angle rock, traveling through talus and scree, crossing streams, fighting ones way through dense brush, and walking on snow-covered slopes. Although ropes may be sensible on harder scrambles, sustained use of rope and belay counts as climbing, typically, for this reason mountain walkers are advised to carry a rope on harder scrambles. Scramblers are also advised to know their limits and to turn back before they get into difficulties, some mountain tops may be reached by walking or scrambling up their least-steep side. The essence of a modern via ferrata is a cable which runs along the route and is periodically fixed to the rock. Using a via ferrata kit, climbers can secure themselves to the cable, the cable can also be used as aid to climbing, and additional climbing aids, such as iron rungs, pegs, carved steps and even ladders and bridges are often provided. Thus via ferratas allow otherwise dangerous routes to be undertaken without the associated with unprotected scrambling and climbing or the need for climbing equipment such as ropes. Many of theses routes include a bad step, where the scrambling suddenly becomes more serious. The bad step on Crib Goch for example, involves only 20 feet or so of climbing, the rock face here is well polished by countless boots, but there are many holds which offer firm support. By contrast, the traverse of the Cuillin Ridge on Skye demands use of a rope at one point at least, the ridge routes of Liathach and Beinn Eighe in Wester Ross are easier to traverse but are extremely exposed. Descent from such ridges is very limited, so once committed, an Teallach to the north offers scrambling, as does Stac Pollaidh further north in Sutherland, which includes a bad step. One resource for scramblers in Britain are the guides by W A Poucher, though these are now dated, a guide to 156 scrambling routes in the Canadian Rockies can be found in Scrambles in the Canadian Rockies by Alan Kane. Backpacker magazine has featured the book as an expedition guide. The Canadian Alpine Journal referred to it as a scree gospel, mount Jefferson is in Coos County, New Hampshire, and is the third highest mountain in the state. Mount Jefferson has a direct ascent along the Caps Ridge Trail, whose base and this route, gaining only 2,700 feet vertically to the summit, makes for the easiest ascent of any Presidential mountain. However, climbing over the caps involves some exposed scrambling and can be steep, many easy scrambles become serious climbs in bad weather
16.
California
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California is the most populous state in the United States and the third most extensive by area. Located on the western coast of the U. S, California is bordered by the other U. S. states of Oregon, Nevada, and Arizona and shares an international border with the Mexican state of Baja California. Los Angeles is Californias most populous city, and the second largest after New York City. The Los Angeles Area and the San Francisco Bay Area are the nations second- and fifth-most populous urban regions, California also has the nations most populous county, Los Angeles County, and its largest county by area, San Bernardino County. The Central Valley, an agricultural area, dominates the states center. What is now California was first settled by various Native American tribes before being explored by a number of European expeditions during the 16th and 17th centuries, the Spanish Empire then claimed it as part of Alta California in their New Spain colony. The area became a part of Mexico in 1821 following its war for independence. The western portion of Alta California then was organized as the State of California, the California Gold Rush starting in 1848 led to dramatic social and demographic changes, with large-scale emigration from the east and abroad with an accompanying economic boom. If it were a country, California would be the 6th largest economy in the world, fifty-eight percent of the states economy is centered on finance, government, real estate services, technology, and professional, scientific and technical business services. Although it accounts for only 1.5 percent of the states economy, the story of Calafia is recorded in a 1510 work The Adventures of Esplandián, written as a sequel to Amadis de Gaula by Spanish adventure writer Garci Rodríguez de Montalvo. The kingdom of Queen Calafia, according to Montalvo, was said to be a land inhabited by griffins and other strange beasts. This conventional wisdom that California was an island, with maps drawn to reflect this belief, shortened forms of the states name include CA, Cal. Calif. and US-CA. Settled by successive waves of arrivals during the last 10,000 years, various estimates of the native population range from 100,000 to 300,000. The Indigenous peoples of California included more than 70 distinct groups of Native Americans, ranging from large, settled populations living on the coast to groups in the interior. California groups also were diverse in their organization with bands, tribes, villages. Trade, intermarriage and military alliances fostered many social and economic relationships among the diverse groups, the first European effort to explore the coast as far north as the Russian River was a Spanish sailing expedition, led by Portuguese captain Juan Rodríguez Cabrillo, in 1542. Some 37 years later English explorer Francis Drake also explored and claimed a portion of the California coast in 1579. Spanish traders made unintended visits with the Manila galleons on their trips from the Philippines beginning in 1565
17.
Contiguous United States
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The contiguous United States consists of the 48 adjoining U. S. states plus Washington, D. C. on the continent of North America. S. The greatest distance entirely within the 48 contiguous states is 2,802 miles, the greatest north-south line is 1,650 miles. Together, the 48 contiguous states and Washington, D. C. occupy an area of 3,119,884.69 square miles. Of this area,2,959,064.44 square miles is land, composing 83. 65% of U. S. land area, officially,160,820.25 square miles is water area, composing 62. 66% of the nations total water area. The contiguous United States would be placed 5th in the list of states and dependencies by area. The 2010 census population of area was 306,675,006, comprising 99. 33% of the nations population. While conterminous U. S. has the meaning of contiguous U. S. other terms commonly used to describe the 48 contiguous states have a greater degree of ambiguity. The term was in use prior to the admission of Alaska and Hawaii as states of the United States, the District of Columbia is not always specifically mentioned as being part of CONUS. OCONUS is derived from CONUS with O for outside added, thus referring to Outside of Continental United States, the term Lower 48 is also used to refer to the conterminous United States. The National Geographic style guide recommends the use of contiguous or conterminous United States instead of lower 48 when the 48 states are meant, both Alaskans and Hawaiians have unique labels for the contiguous United States because of their own locations relative to them. Alaska became the 49th state of the United States on January 3,1959, Alaska is on the northwest end of the North American continent, but separated from the rest of the United States Pacific coast by the Canadian province of British Columbia. In Alaska, given the ambiguity surrounding the usage of continental, several other terms have been used over the years. Hawaii became the 50th state of the United States on August 21,1959 and it is the southernmost and so far, the latest state to join the Union. Not part of any continent, Hawaii is located in the Pacific Ocean, about 2,200 miles from North America, in Hawaii and overseas American territories, for instance, the terms the Mainland or U. S. Mainland are often used to refer to the continental United States, apart from off-shore US islands, a few continental portions of the contiguous US are accessible by road only by traveling through Canada. Point Roberts, Washington, Elm Point, Minnesota, and the Northwest Angle in Minnesota are three such places, alburgh, Vermont, is not directly connected by land, but is accessible by road via bridges from within Vermont and from from New York. The 48 contiguous United States are, Washington, D. C. is distinct from the state of Washington, extreme points of the United States Mainland Definition of continental Definition of contiguous Definition of coterminous and conterminous
18.
John Muir Wilderness
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The John Muir Wilderness is a wilderness area that extends along the crest of the Sierra Nevada of California for 90 miles, in the Inyo and Sierra National Forests. Established in 1964 by the Wilderness Act and named for naturalist John Muir, the wilderness lies along the eastern escarpment of the Sierra from near Mammoth Lakes and Devils Postpile National Monument in the north, to Cottonwood Pass near Mount Whitney in the south. The wilderness area also spans the Sierra crest north of Kings Canyon National Park, the wilderness contains some of the most spectacular and highest peaks of the Sierra Nevada, with 57 peaks over 13,000 feet in elevation. The peaks are made of granite from the Sierra Nevada Batholith. The southernmost glacier in the United States, the Palisade Glacier, is contained within the wilderness area, notable eastside glaciated canyons are drained by Rock, McGee, and Bishop Creeks. The eastern escarpment in the wilderness rises from 6,000 to 8,000 feet from base to peak, the Sierra crest contains peaks from 12,000 to 14,000 feet in elevation, including Mount Whitney, the highest peak in the continental United States. Other notable mountains in the area include the Palisades and Mount Humphreys. Mount Muir is located 2 miles south of Mount Whitney, Mount Williamson is the second-highest peak in the wilderness, at 14,375 feet, it rises in one continuous sweep of granite from the floor of the Owens Valley to a peak just east of the main range. The John Muir Wilderness contains the largest contiguous area above 10,000 feet in the continental United States and it contains large areas of subalpine meadows and fellfields above 10,800 feet, containing stands of whitebark and foxtail pine. From 9,000 feet to 10,800 feet, the wilderness is dominated by lodgepole pines, below the lodgepole forest is forest dominated by Jeffrey pine. Common animals in the wilderness include yellow-bellied marmots, pikas, golden-mantled ground squirrels, Clarks nutcrackers, golden trout, the wilderness area also includes California bighorn sheep zoological areas, which are set aside for the protection of the species. The wilderness contains 589.5 miles of hiking trails, including the John Muir Trail and the Pacific Crest Trail, the John Muir Wilderness is the second most-visited wilderness in the United States, and quota are required for overnight use on virtually all trailheads. Duck Lake Lake Virginia Squaw Lake Bibliography of the Sierra Nevada, for further reading Wilderness. net TopoQuest map
19.
Inyo National Forest
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Inyo National Forest is a United States National Forest covering parts of the eastern Sierra Nevada of California and the White Mountains of California and Nevada. The forest covers 1,903,381 acres and includes nine designated wilderness areas which protect over 800,000 acres, most of the forest is in California, but it includes about 60,700 acres in western Nevada. It stretches from the side of Yosemite to south of Sequoia National Park. Geographically it is split in two, one on side of the Long Valley Caldera and Owens Valley. The John Muir Wilderness is a part of the Inyo National Forest and abuts Sequoia, the northern part of the Inyo National Forest is preserved as a part of the Ansel Adams Wilderness area, which borders Yosemite National Park. Together, the areas and parks form one contiguous area of protected wilderness of more than 1.5 million acres. The Inyo National Forest was named after Inyo County, California, the name Inyo comes from a Native American word meaning dwelling place of the great spirit. The forest spans parts of Inyo, Mono, Tulare, Fresno and Madera counties in California, the forests headquarters are in Bishop, California, with ranger district offices in Bishop, Lee Vining, Lone Pine, and Mammoth Lakes. The forest was established on May 25,1907, on July 1,1945 land from the former Mono National Forest was added. There are nine wilderness areas lying within Inyo NF that are part of the National Wilderness Preservation System. One of these Bristlecone Pines is Methuselah, the second oldest known living tree on earth, over 4,839 years old. It was also the location of the 1998 Sci-fi film. Inyo Forest also served as the location for the second half of the second episode in BBCs Walking with Monsters. Forest Service Inyo National Forest Map
20.
Independence, California
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Independence is a census-designated place in Inyo County, California. Independence is located 41 miles south-southeast of Bishop, at an elevation of 3930 feet and it is the county seat of Inyo County, California. The population of this place was 669 at the 2010 census. The tiny village of Independence is bisected by U. S. Route 395, the Sierra Nevada mountains to the west lie within the John Muir Wilderness Area. Onion Valley, one of the entry routes to the John Muir Wilderness, is accessed via the Onion Valley road which heads directly west out of Independence. The highest pass along the trail,13,153 foot Forester Pass, is directly west of Independence. According to the United States Census Bureau, Independence covers an area of 4.9 square miles, the elevation of Independence is 3,925 feet above sea level. Independence, as well as most of the Owens Valley, has a desert climate with hot summers. January temperatures range from a high of 54.0 °F to an average low of 27.4 °F. July temperatures range from a high of 97.6 °F to an average low of 63.9 °F. The highest recorded temperature was 114 °F on July 7,1989, the lowest recorded temperature was −5 °F on January 9,1937. There are an average of 97.7 days annually with highs of 90 °F or higher, annual precipitation averages only 5.82 inches. The most precipitation in one month was 23.90 inches in February 1904, the most precipitation in 24 hours was 5.72 inches on December 6,1966. Snowfall varies greatly from year to year, averaging only 5.2 inches, the most snow in one month was 112.0 inches in February 1904. Charles Putnam founded a trading post at the site in 1861 and it became known as Putnams, and later Little Pine from the Little Pine Creek. Independence began as the US Army Camp Independence established by Lieutenant Colonel George S. Evans on July 4,1862, col. Evans established the camp at the request of local settlers who feared Indian hostilities. The camp was closed, but was re-established as Fort Independence when hostilities resumed in 1865. The fort was abandoned in 1877, and it is currently a reservation for the Fort Independence Indian Community of Paiute Indians
21.
Robert S. Williamson
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Robert Stockton Williamson was an American soldier and engineer, noted for conducting surveys for the transcontinental railroad in California and Oregon. Williamson was born in Oxford, New York and lived in Elizabeth and he was named after Commodore Robert F. Stockton, a family friend. He joined the Navy in 1843 as a mate under Stockton on the USS Princeton. Williamson was detached from the ship 10 days before one of its guns exploded and it was through Stocktons influence that Williamson was appointed to the United States Military Academy. He graduated fifth in his class in 1848 and appointed a lieutenant in the Corps of Topographical Engineers. He was assigned to conduct surveys for proposed routes for the railroad in California. He was then assigned to the staff of the general of the Department of the Pacific. He was then assigned as Chief Topographical Engineer for the Army of the Potomac, Williamson returned to California as the Chief Topographical Engineer of the Department of the Pacific. In 1863, Williamson transferred to the Corps of Engineers and served as engineer for the Pacific Coast. He also worked on defenses and harbors along the coast and he retired from the Army as a lieutenant colonel in 1882, due to illness. Williamson had suffered bad health for the last 20 years of his life and died of tuberculosis in San Francisco. He was buried at the Masonic Cemetery in San Francisco, mount Williamson in California, a western woodpecker, the Williamsons sapsucker, and Williamson Mountain and the Williamson River in Oregon are named in his honor. 14th Annual Reunion of the Association of Graduates of the United States Military Academy at West Point, New York, east Saginaw, Michigan, Courier Publishing Co.1883. Robert S. Williamson at Find a Grave
22.
Pacific Railroad Surveys
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The Pacific Railroad Surveys consisted of a series of explorations of the American West to find possible routes for a transcontinental railroad across North America. The expeditions included surveyors, scientists, and artists and resulted in a body of data covering at least 400,000 square miles on the American West. Starting in the late 18th and early 19th centuries, many Americans began a migration that would come to greatly influence the development American history. However, water remained the most common and most efficient form of transit available. Soon, the development of the engine became an invaluable contribution to this westward expansion. As railroads gained popularity in the eastern United States during the 1830s, beginning in the 1840s, several government sponsored expeditions hoped to find potential railroad routes across the west. However, no consensus route emerged due to the economic motives of rival companies. In addition, cities and states competed for the route and terminus so no consensus was reached, southerns states and cities wanted to use the railroad to extend slavery, northern ones the opposite. Brigham Young, President of LDS Church, wrote, We never went through the canyons or worked our way over the ridges without asking where the rails could be laid. ”The most important concern for the United States Congress involved the location of where to build the railroad. With government involvement, lobbyists attempted to influence the selected locations because of the important social, political, in addition, a transcontinental railroad would become a very costly endeavor. In fact, “Even the least expensive proposed routes would equal the federal budget for one year. ”Despite these obstacles, on August 16,1856, Mr. Five surveys were conducted. The Central Pacific survey followed between the 37th parallel north and 39th parallel north from St. Louis, Missouri to San Francisco and this survey was led by Lt. John W. Gunnison until his death by the Utes in Utah. Lt. Edward Griffin Beckwith then took command, also participating in this survey was Frederick W. von Egloffstein, George Stoneman and Lt. Gouverneur K. Warren. There were two Southern Pacific surveys and this survey was led by Lt. John Parke and John Pope. The fifth survey was along the Pacific coast from San Diego to Seattle, Washington conducted by Lt. Robert S. Williamson, the Pacific Railroad Surveys provided valuable information to determining the best location of the transcontinental railroad. In addition, three important trends also influenced Congress’ final decision, first, the California Gold Rush and the discovery of silver in Nevada led to a dramatic increase in population in the west. Second, the secession of the South from the Union during the beginnings of the American Civil War discounted southern politicians from interfering with a plan to build a northern route. Third, a popularity of railroad specialists allowed Congress several options to consider the most efficient
23.
Independence Airport
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Independence Airport is a public airport located one mile north of Independence, serving Inyo County, California, USA. The airport has two runways and is used for general aviation. California World War II Army Airfields This article incorporates public domain material from the Air Force Historical Research Agency website http, //www. afhra. af. mil/
24.
Mount Tyndall
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Mount Tyndall is a peak in the Mount Whitney region of the Sierra Nevada in the U. S. state of California. It rises to 14,025 feet, and is the tenth highest peak in the state, the mountain was named in honor of the Irish scientist and mountaineer, John Tyndall. Mount Tyndall is 1.5 miles west of the higher Mount Williamson, King and Cotter were attempting to make the first ascent of Mount Whitney, and had made a long trek from Kings Canyon, only to realize months later that they had climbed the wrong peak. The easiest route on Mount Tyndall in terms of access and climbing is the Northwest Ridge and it begins about one half mile west of Shepherd Pass and about 1 mile north of the peak. Other non-technical routes exist on the gently sloped west side of the peak, at least two significant technical routes lie on the much steeper east face, the first of these routes was climbed by noted mountaineer Fred Beckey and Charlie Raymond in 1970. List of mountain peaks of California List of California fourteeners Mount Tyndall, in Chapter 3 of the free online version of this book, King gives an account of the first ascent of Mount Tyndall
25.
Sierra Nevada bighorn sheep
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Sierra Nevada bighorn sheep is subspecies of bighorn sheep unique to the Sierra Nevada mountains of California. Sierra Nevada bighorn sheep were listed as an endangered subspecies in 2000. Today, about 500 Sierra bighorn remain in the wild, Sierra bighorn range in color from white to dark brown, with a white rump and dark tail. There is some change in coloration due to the shedding of a thicker winter layer. Specialized hooves with adhesive soles provide traction in steep rocky terrain, female bighorn can weigh up to 70 kilograms and have shorter, narrow horns, while male bighorn can weigh as much as 100 kilograms and have massive, curving horns. The horns of both rams and ewes are composed of a layer of keratin covering a core of bone. The average lifespan for Sierra bighorn males and females has been observed as 8 to 12 years, Sierra Nevada bighorn sheep are gregarious, with group size and composition depending on gender and season. Spatial segregation by gender occurs outside of the mating season, Bighorn sheep ewes generally remain with the same band in which they were born. Males older than 2 years of age remain apart from females, during the late fall and winter, the groups come together and concentrate in suitable winter habitat. During this time, males compete for dominance with behaviors like horn clashes, breeding takes place in late fall, generally November and December. Lambing occurs between late April and early July on safe, precipitous, rocky slopes, most lambs in the Sierra Nevada are born in May, ewes and lambs often occupy steep terrain that provides a diversity of exposures and slopes for escape cover. Sierra bighorn are found in portions of the Sierra Nevada from Yosemite National Park to Olancha Peak, habitat occurs from the eastern base of the range as low as 1,460 m to peaks above 4,300 m. Sierra bighorn inhabit open areas where the land is rocky, sparsely vegetated, wehausen provides a detailed description of Sierra bighorn habitat throughout their range. Bighorn prefer open ground with high visibility to better detect predators and allow time to reach steep. Forests and thick brush are usually avoided if possible, most bighorn live at elevations from 3, 000–4,300 m in subalpine and alpine areas during the summer. During winter, some bighorn occupy high-elevation, windswept ridges, while others migrate to lower elevations to avoid deep snow, Sierra bighorn are ruminant herbivores with four-chambered stomachs. Bighorn are primarily grazers, consuming grasses, forbs. Naturally occurring mineral licks provide necessary minerals for bone and muscle growth, centuries of unregulated hunting, disease outbreaks, and mountain lion predation took a heavy toll on the Sierra bighorn population
26.
Sierra Club
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The Sierra Club is an environmental organization in the United States. It was founded on May 28,1892, in San Francisco, California, by the Scottish-American preservationist John Muir, in recent years, the club has gravitated toward green politics and especially toward bright green environmentalism. Recent focuses of the club include promoting green energy, mitigating global warming, in 2015 Sierra Club launched its activism platform AddUp. The Sierra Club does not set standards for or regulate alpinism, but it organizes wilderness courses, hikes, rock climbs, the Sierra Club is governed by a 15-member Board of Directors. Each year, five directors are elected to terms. A president is elected annually by the Board from among its members, the Executive Director runs the day-to-day operations of the group. Michael Brune, formerly of Rainforest Action Network, has served as the executive director since 2010. Pope stepped down amid discontent that the group had strayed from its core principles, Sierra Club members belong to statewide chapters and local groups. National and local special-interest sections, committees, and task forces address particular issues, the national Sierra Club sets the organizations policy agenda. As early as 1889, Johnson had encouraged Muir to form an association to protect the Sierra Nevada. Others involved in the planning included artist William Keith, Willis Linn Jepson, Willard Drake Johnson, Joseph LeConte. The Sierra Clubs charter members elected Muir president, an office he held until his death in 1914, Muir escorted President Theodore Roosevelt through Yosemite in 1903, and two years later the California legislature ceded Yosemite Valley and Mariposa Grove to the federal government. The Sierra Club won its first lobbying victory with the creation of the second national park. In the first decade of the 1900s, the Sierra Club became embroiled in the Hetch Hetchy Reservoir controversy that divided preservationists from resource management conservationists. In the late 19th century, the city of San Francisco was rapidly outgrowing its limited water supply, which depended on intermittent local springs and streams. Gifford Pinchot, a supporter of public utilities and head of the US Forest Service. Muir appealed to his friend U. S. President Roosevelt, Muir and attorney William Edward Colby began a national campaign against the dam, attracting the support of many eastern conservationists. With the 1912 election of U. S. President Woodrow Wilson, the bill to dam Hetch Hetchy passed Congress in 1913, and so the Sierra Club lost its first major battle
27.
Geographic Names Information System
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It is a type of gazetteer. GNIS was developed by the United States Geological Survey in cooperation with the United States Board on Geographic Names to promote the standardization of feature names, the database is part of a system that includes topographic map names and bibliographic references. The names of books and historic maps that confirm the feature or place name are cited, variant names, alternatives to official federal names for a feature, are also recorded. Each feature receives a permanent, unique feature record identifier, sometimes called the GNIS identifier, the database never removes an entry, except in cases of obvious duplication. The GNIS accepts proposals for new or changed names for U. S. geographical features, the general public can make proposals at the GNIS web site and can review the justifications and supporters of the proposals. The Bureau of the Census defines Census Designated Places as a subset of locations in the National Geographic Names Database, U. S. Postal Service Publication 28 gives standards for addressing mail. In this publication, the postal service defines two-letter state abbreviations, street identifiers such as boulevard and street, department of the Interior, U. S. Geological Survey, National Mapping Division, Digital Gazeteer, Users Manual. Least Heat Moon, William, Blue Highways, A Journey Into America, standard was withdrawn in September 2008, See Federal Register Notice, Vol.73, No. 170, page 51276 Report, Principles, Policies, and Procedures, Domestic Geographic Names, U. S. Postal Service Publication 28, November 2000. Board on Geographic Names website Geographic Names Information System Proposals from the general public Meeting minutes
28.
The Mountaineers (club)
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The Mountaineers is an outdoor recreation, education, and conservation 501 nonprofit based in Seattle, Washington, founded in 1906. It has 7 branches in Western Washington,3 mountain lodges, and 2 program centers, one in Magnuson Park in Seattle, the Mountaineers also publishes books, ebooks and guides on outdoor education, recreation and conservation. There are no restrictions on who may join, the club constitution was officially adopted in 1907 by a membership of 151. Among these original members were Henry Landes, Edmond S. Meany, the famous photographer Asahel Curtis, the activities initially were local walks with the first trip being a hike through Fort Lawton to the West Point Lighthouse. The first mountain climbing trip was Mount Si, in 1907,65 members made a group climb of Mount Olympus and exploration of the Olympic Mountains. The next year a summit of Mount Baker was organized, followed by Mount Rainier in 1909, in 1915, a club outing became the first sizable group to hike around Mount Rainier and established the route that would later become known as the Wonderland Trail. The club organizes thousands of trips per year, has a library and historical archive, teaches instructional courses. From 1907 to 1995, new climbs in the Cascades were reported in the Mountaineers Annual, since 2004, the Northwest Mountaineering Journal, hosted by the Mountaineers, has recorded this information. The organization provides a forum for members to organize their own trips, many classes are offered beyond climbing skills including nature photography. A thirty-hour wilderness first aid course called Mountaineering Oriented First Aid was produced by the organization, in 2008, the Mountaineers moved from Lower Queen Anne to an old naval building in Magnuson Park, now leased from the City of Seattle. The new facility features indoor and outdoor climbing walls, including an ice climbing wall. The grounds also feature native plants and an amphitheater for practicing scrambling. The Mountaineers Library was founded in 1915, as of 2011 it contains 6000 books and subscribes to 40 periodicals. It specializes in studies on climbing, environmental studies, biographies of exploratory mountaineers, the history of exploratory mountaineering, Mountaineers Books, based in Seattle, Washington, is the professional book publishing division of The Mountaineers. Mountaineers Books was informally started in 1955 when a committee was formed to create a mountaineering training text from the materials that the Club was using for its classes. The editorial committee created Mountaineering, The Freedom of the Hills, the first edition of Freedom, as it is commonly called, was published in April 1960. Mountaineers Books has produced more than 1,000 titles since its foundation in 1960 and it shares the Clubs 501 nonprofit status. It also publishes conservation advocacy titles under the Braided River imprint, Seattle 1900-1920, From Boomtown, Urban Turbulence, to Restoration
29.
International Standard Book Number
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The International Standard Book Number is a unique numeric commercial book identifier. An ISBN is assigned to each edition and variation of a book, for example, an e-book, a paperback and a hardcover edition of the same book would each have a different ISBN. The ISBN is 13 digits long if assigned on or after 1 January 2007, the method of assigning an ISBN is nation-based and varies from country to country, often depending on how large the publishing industry is within a country. The initial ISBN configuration of recognition was generated in 1967 based upon the 9-digit Standard Book Numbering created in 1966, the 10-digit ISBN format was developed by the International Organization for Standardization and was published in 1970 as international standard ISO2108. Occasionally, a book may appear without a printed ISBN if it is printed privately or the author does not follow the usual ISBN procedure, however, this can be rectified later. Another identifier, the International Standard Serial Number, identifies periodical publications such as magazines, the ISBN configuration of recognition was generated in 1967 in the United Kingdom by David Whitaker and in 1968 in the US by Emery Koltay. The 10-digit ISBN format was developed by the International Organization for Standardization and was published in 1970 as international standard ISO2108, the United Kingdom continued to use the 9-digit SBN code until 1974. The ISO on-line facility only refers back to 1978, an SBN may be converted to an ISBN by prefixing the digit 0. For example, the edition of Mr. J. G. Reeder Returns, published by Hodder in 1965, has SBN340013818 -340 indicating the publisher,01381 their serial number. This can be converted to ISBN 0-340-01381-8, the check digit does not need to be re-calculated, since 1 January 2007, ISBNs have contained 13 digits, a format that is compatible with Bookland European Article Number EAN-13s. An ISBN is assigned to each edition and variation of a book, for example, an ebook, a paperback, and a hardcover edition of the same book would each have a different ISBN. The ISBN is 13 digits long if assigned on or after 1 January 2007, a 13-digit ISBN can be separated into its parts, and when this is done it is customary to separate the parts with hyphens or spaces. Separating the parts of a 10-digit ISBN is also done with either hyphens or spaces, figuring out how to correctly separate a given ISBN number is complicated, because most of the parts do not use a fixed number of digits. ISBN issuance is country-specific, in that ISBNs are issued by the ISBN registration agency that is responsible for country or territory regardless of the publication language. Some ISBN registration agencies are based in national libraries or within ministries of culture, in other cases, the ISBN registration service is provided by organisations such as bibliographic data providers that are not government funded. In Canada, ISBNs are issued at no cost with the purpose of encouraging Canadian culture. In the United Kingdom, United States, and some countries, where the service is provided by non-government-funded organisations. Australia, ISBNs are issued by the library services agency Thorpe-Bowker
30.
Francis P. Farquhar
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Francis Peloubet Farquhar was an American mountaineer, environmentalist and author in addition to his career as a Certified Public Accountant. Farquhar was born in Newton, Massachusetts, the son of David Webber Farquhar and he attended Harvard University, where he edited The Harvard Crimson for three years and studied under, among others, Bliss Perry and George Santayana. Graduating from Harvard in 1909, he came to San Francisco in 1910 and he visited Yosemite and joined the Sierra Club in 1911. He then returned to New England to pursue the profession of accounting, studying under Clinton Scovell, in 1914 he moved again to California. He served in the Navy there and in Washington, D. C. during World War I, in 1922 he set up his own accounting firm in San Francisco. In 1936 he brought in Clifford Heimbuchder, who became a full partner in the firm, renamed Farquhar. Farquhar was active in the Sierra Club, serving on its board of directors from 1924 to 1951 and president in 1933-1935 and he served as Sierra Club Bulletin editor from 1926 to 1946. Farquhar was a mountaineer who invited Robert L. M. Underhill to introduce proper use of modern Alpine rope techniques to Sierra Club members on an annual club High Trip in 1931. On August 26,1921, he completed the first ascent of Middle Palisade by the south-west chute with Ansel Hall and he was the author of numerous articles for the Sierra Club and the California Historical Society, some of which were reprinted in book form. In 1956-59 he was editor of the American Alpine Journal published by the American Alpine Club and he edited and wrote forewords for several books on California history. His best known book is History of the Sierra Nevada, which is still in print, in addition to serving as Sierra Club president, he was president of the California Society of Certified Public Accountants, California Academy of Sciences, and the California Historical Society. In 1965 he was awarded the Sierra Clubs John Muir Award for distinguished work as a conservationist and he received the Henry R. Wagner Memorial Award of the California Historical Society in 1966. The University of California at Los Angeles conferred on him the degree of Doctor of Humane Letters in 1967. In 1934 he married Marjory Bridge, fellow mountaineer, they had three children, Peter, Suzanne and Roger and his half brother was the Los Angeles architect Robert D. Farquhar, who moved in with the Farquhars in Berkeley in 1953. Marjorie Bridge Farquhar died in 1999 in San Francisco, Mount Farquhar, located 1.6 miles northwest of Mount Brewer in Kings Canyon National Park, was named in his honor. Since 1970, the Sierra Club has given the Francis P. Farquhar Mountaineering Award in his honor
31.
Bishop, California
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Bishop is a city in Inyo County, California, United States. Though Bishop is the city and the largest populated place in Inyo County. Bishop is located near the end of the Owens Valley. The population was 3,879 at the 2010 census, up from 3,575 at the 2000 census, the town was named after Bishop Creek, flowing out of the Sierra Nevada, the creek was named after Samuel Addison Bishop, a settler in the Owens Valley. Bishop lies west of the Owens River at the end of the Owens Valley. It is on U. S. Route 395, the main artery through the Owens Valley, connecting the Inland Empire to Reno. US395 also connects Bishop to Los Angeles via State Route 14 through Palmdale, Bishop is the western terminus of U. S. Route 6. The Paiute-Shoshone Indians of the Bishop Community of the Bishop Colony control land just west of the town, the Los Angeles Department of Water and Power controls much of the upstream and surrounding area. Bishop is immediately to the east of the Sierra Nevada, numerous peaks are within a short distance of Bishop, including Mount Humphreys, to the west, White Mountain Peak in the northeast, and pyramidal Mount Tom northwest of town. Basin Mountain is viewed to the west from Bishop as it rises above the Buttermilks, according to the United States Census Bureau, the city has a total area of 1.9 square miles, over 97% of it land. The festival attracts tourists, primarily from the Southern California area. Bishop is well known in the climbing community. Near the city are numerous climbing spots that attract visitors from around the world, there are over 2,000 bouldering problems in Bishop. The two main types of rock are volcanic tuff and granite.18 inches of precipitation, and is part of USDA Plant Hardiness Zone 7. The wettest year was 1969 with 17.09 in of precipitation, measurable precipitation occurs on an average of 27.6 days annually. The most precipitation in one month was 8.93 in in January 1969, which included 4.00 in on January 4, snowfall averages 6.8 inches per year. The snowiest season was from July 1968 to June 1969 with 57.1 inches, which included the snowiest month, January 1969, at 23.2 inches. There is an average of 2.5 nights of sub 10 °F lows,134 nights where the low reaches the mark,100 days with 90 °F + highs
32.
Denali
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Denali is the highest mountain peak in North America, with a summit elevation of 20,310 feet above sea level. With a topographic prominence of 20,156 feet and an isolation of 4,629 miles, Denali is the third most prominent and third most isolated peak after Mount Everest. Located in the Alaska Range in the interior of the U. S. state of Alaska, Denali is the centerpiece of Denali National Park, the Koyukon people who inhabit the area around the mountain have referred to the peak as Denali for centuries. In August 2015, following the 1975 lead of the state of Alaska, prior to this, most Alaskans already referred to the mountain as Denali. In 1903, James Wickersham recorded the first attempt at climbing Denali, in 1906, Frederick Cook claimed the first ascent, which was later proven to be false. The first verifiable ascent to Denalis summit was achieved on June 7,1913, by climbers Hudson Stuck, Harry Karstens, Walter Harper, and Robert Tatum, who went by the South Summit. In 1951, Bradford Washburn pioneered the West Buttress route, considered to be the safest and easiest route, and therefore the most popular currently in use. On September 2,2015, the U. S. Geological Survey announced that the mountain is 20,310 feet high, not 20,320 feet, the forces that lifted Denali also cause many deep earthquakes in Alaska and the Aleutian Islands. The Pacific Plate is seismically active beneath Denali, a region that is known as the McKinley cluster. Denali has an elevation of 20,310 feet above sea level, making it the highest peak in North America. Measured from base to peak at some 18,000 ft, Denali rises from a sloping plain with elevations from 1,000 to 3,000 ft, for a base-to-peak height of 17,000 to 19,000 ft. By comparison, Mount Everest rises from the Tibetan Plateau at a higher base elevation. Denali has two significant summits, the South Summit is the one, while the North Summit has an elevation of 19,470 ft. The North Summit is sometimes counted as a peak and sometimes not, it is rarely climbed. Five large glaciers flow off the slopes of the mountain, the Peters Glacier lies on the northwest side of the massif, while the Muldrow Glacier falls from its northeast slopes. Just to the east of the Muldrow, and abutting the eastern side of the massif, is the Traleika Glacier, the Ruth Glacier lies to the southeast of the mountain, and the Kahiltna Glacier leads up to the southwest side of the mountain. With a length of 44 mi, the Kahiltna Glacier is the longest glacier in the Alaska Range, the Koyukon Athabaskans who inhabit the area around the mountain have for centuries referred to the peak as Dinale or Denali. The name is based on a Koyukon word for high or tall, during the Russian ownership of Alaska, the common name for the mountain was Bolshaya Gora, which is the Russian translation of Denali
33.
Mount Logan
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Mount Logan /ˈloʊɡən/ is the highest mountain in Canada and the second-highest peak in North America, after Denali. The mountain was named after Sir William Edmond Logan, a Canadian geologist, Mount Logan is located within Kluane National Park and Reserve in southwestern Yukon, less than 40 kilometres north of the Yukon/Alaska border. Mount Logan is the source of the Hubbard and Logan Glaciers, Logan is believed to have the largest base circumference of any non-volcanic mountain on Earth, including a massif with eleven peaks over 5,000 metres. Due to active tectonic uplifting, Mount Logan is still rising in height, before 1992, the exact elevation of Mount Logan was unknown and measurements ranged from 5,959 to 6,050 metres. In May 1992, a GSC expedition climbed Mount Logan and fixed the current height of 5,959 metres using GPS, temperatures are extremely low on and near Mount Logan. On the 5,000 m high plateau, air temperature hovers around −45 °C in the winter, minimal snow melt leads to a significant ice cap, reaching almost 300 m in certain spots. An international team of Canadian, British and American climbers was assembled and initially they had planned their attempt in 1924 but funding, the international team of climbers began their journey in early May, crossing the mainland from the Pacific coast by train. They then walked the remaining 200 kilometres to within 10 kilometres of the Logan Glacier where they established base camp, in the early evening of June 23,1925, Albert H. MacCarthy, H. F. Lambart, Allen Carpé, W. W. Foster, Norman H. Read and Andy Taylor stood on top for the first time and it had taken them 65 days to approach the mountain from the nearest town, McCarthy, summit and return, with all climbers intact. Don Monk, Gil Roberts and 3 others reached the summit on July 19, dick Long, Allen Steck, Jim Wilson, John Evans, Franklin Coale Sr. and Paul Bacon over 30 days, mid-July to Mid-August. Fred Beckey remarked, When they got back we just couldnt believe that they had climbed that thing and we didnt think they had a chance. Featured in Fifty Classic Climbs of North America, dave Jones, Frank Baumann, Fred Thiessen, Jay Page and Rene Bucher in 22 days. Michael Down, Paul Kindree, John Howe, Reid Carter and John Wittmayer climbed to the summit over 22 days, raymond Jotterand, Alan Burgess, Jim Elzinga and John Laughlan reached the summit after 15 days of climbing on June 30 and July 1. 1992 June 6, an expedition sponsored by the Royal Canadian Geographic Society confirmed the height of Mount Logan using GPS, the leader was Michael Schmidt, with Lisel Currie, Leo Nadeay, Charlie Roots, J-C. Lavergne, Roger Laurilla, Pat Morrow, Karl Nagy, Sue Gould, Alan Björn, Lloyd Freese, Kevin McLaughlin, a mountain in British Columbias Premier Range was named Mount Pierre Elliott Trudeau instead. During the last few days of May 2005, three climbers from the North Shore Search and Rescue team of North Vancouver became stranded on the mountain, a joint operation by Canadian and American forces rescued the three climbers and took them to Anchorage, Alaska for treatment of frostbite. London, J. M. Dent & Sons, Fifty Classic Climbs of North America. San Francisco, CA, USA, Sierra Club Books, pushing the Limits, The Story of Canadian Mountaineering
34.
Pico de Orizaba
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Pico de Orizaba, also known as Citlaltépetl, is a stratovolcano, the highest mountain in Mexico and the third highest in North America, after Denali of the United States and Mount Logan of Canada. It rises 5,636 metres above sea level in the end of the Trans-Mexican Volcanic Belt. The volcano is currently dormant but not extinct, with the last eruption taking place during the 19th century and it is the second most prominent volcanic peak in the world after Africas Mount Kilimanjaro. Pico de Orizaba overlooks the valley and city of Orizaba, from which it gets its name, the name Citlaltépetl is not used by Nahuatl speakers of the Orizaba area, who instead call it Istaktepetl, or White Mountain. In the earliest mention of the volcano, it was referred to by the natives during the Pre-Columbian Era as Poyautécatl, Citlaltépetl was the common name in the Náhuatl language when the Spanish arrived in Mexico. Citlaltépetl comes from the Náhuatl citlalli and tepētl and thus means Star Mountain and this name is thought to be based on the fact that the snow-covered peak can be seen year round for hundreds of kilometers throughout the region. A legend from the city of Coscomatepec tells of how the planet Venus can be seen settling into the crater of Citlaltépetl, during the colonial era, the volcano was also known as Cerro de San Andrés due to the nearby settlement of San Andrés Chalchicomula at its base. A third name, Poyauhtecatl, which means the one that colors or illuminates, has also been recorded and this name was given by the Tlaxcaltecas in memory of their lost country. The peak of Citlaltépetl rises dramatically to an elevation of 5,636 m above sea level, it has a topographic prominence of 4,922 m. Regionally dominant, Pico de Orizaba is the highest peak in Mexico, Orizaba is ranked 7th in the world in topographic prominence. It is the second most prominent volcanic peak in the world after Africas Mount Kilimanjaro, the topography of Pico de Orizaba is asymmetrical from the center of the crater, the eastern face is the steepest side of the volcano and the northwestern face the most gradual side. The gradual slopes of the face of the volcano allows for the presence of large glaciers and is the most traveled route to take for hikers traveling to the summit. Pico de Orizaba is one of three volcanoes in México that continue to support glaciers and is home to the largest glacier in Mexico. Orizaba has nine known glaciers, Gran Glaciar Norte, Lengua del Chichimeco, Jamapa, Toro, Glaciar de la Barba, Noroccidental, Occidental, Suroccidental, the equilibrium line altitude is not known for Orizaba. Snow on the south and southeast sides of the volcano melts quickly because of solar radiation, the insolation angle and wind redeposition on the northwest and north sides allow for constant accumulation of snow providing a source for the outlet glaciers. On the north side of Orizaba, the Gran Glaciar Norte fills the elongated highland basin and is the source for seven outlet glaciers. The main glacier extends 3.5 km north of the rim, has a surface area of about 9.08 km2 descending from 5,650 m to about 5,000 m. It has an irregular and stepped profile that is caused in part by the configuration of the bedrock
35.
Mount Saint Elias
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It lies about 40 kilometres southwest of Mount Logan, the highest mountain in Canada. The Canadian side is part of Kluane National Park and Reserve and its name in Tlingit is Yasʼéitʼaa Shaa, meaning mountain behind Icy Bay, and is occasionally called Shaa Tlein Big Mountain by the Yakutat Tlingit. It is one of the most important crests of the Kwaashkʼiḵwáan clan since they used it as a guide during their journey down the Copper River and their children, the mountains in between the two peaks, are called Tsalx̱aan Yátxʼi. The mountain was first sighted by European explorers on July 16,1741 by Vitus Bering of Denmark, while some historians contend that the mountain was named by Bering, others believe that eighteenth century mapmakers named it after Cape Saint Elias, when it was left unnamed by Bering. Mount Saint Elias is notable for its immense vertical relief and its summit rises 18,008 feet vertically in just 10 miles horizontal distance from the head of Taan Fjord, off of Icy Bay. In 2007, an Austrian documentary movie called Mount, the climbers ended up summiting on the second attempt and skiing down to 13,000 feet. Mt. St. Elias was first climbed on July 31,1897 by a led by famed explorer Prince Luigi Amadeo di Savoia. The second ascent was not until 1946, when a group from the Harvard Mountaineering Club including noted mountain historian Dee Molenaar climbed the Southwest Ridge route. The summit party comprised Molenaar, his brother Cornelius, Andrew and Betty Kauffman, Maynard Miller, William Latady, William Putnam was a member of the expedition but did not make the summit. They used eleven camps, eight of which were on the approach from Icy Bay and they were supported by multiple air drops of food. The first winter ascent was made on February 13,1996 by David Briggs, Gardner Heaton and Joe Reichert. After being flown in to 2,300 feet on the Tyndal Glacier, they climbed the southwest ridge, the team had originally planned to begin their ascent from the ocean and cross the Tyndal Glacier but the terrain was in very poor condition. Mount Saint Elias is infrequently climbed today, despite its height, because it has no route to the summit
36.
Mount Foraker
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Mount Foraker is a 17, 400-foot mountain in the central Alaska Range, in Denali National Park,14 mi southwest of Denali. It is the second highest peak in the Alaska Range, and it rises almost directly above the standard base camp for Denali, on a fork of the Kahiltna Glacier also near Mount Hunter in the Alaska Range. Its north peak was first climbed on August 6,1934, graham Brown, and Chychele Waterston, via the west ridge. Mount Foraker was named in 1899 by Lt. J. S. Herron after Joseph B, the mountain, along with Denali, was called Bolshaya Gora in Russian. The Tanana Indians in the Lake Minchumina area, however, had a view of the mountains. According to Hudson Stuck, these Indians had two names for Mount Foraker, Sultana meaning the woman and Menlale meaning Denalis wife,1934 West Ridge FA of Mount Foraker by Charles Houston, T. 1968 Talkeetna Ridge, South Ridge FA by Alex Bertulis, Warren Bleser, the summit was reached on July 26,1968. 1974 Southwest Toe of Southeast Ridge, variation to the South Ridge, ascent by Peter Reagan, Joe Davidson, Bob Fries, Jim Given, Mark Greenfield, Pippo Lionni, Eric Morgan and Frank Uher. 1975 Archangel Ridge, the ridge, FA by Gerard and Barbara Roach, Brad Johnson, David Wright, Stewart Krebs. Summit reached on July 14,1975,1976 French Ridge, the South/Southeast Ridge, FA by Henri Agresti, Jean-Marie Galmiche, Gerard Creton, Herve Thivierge, Isabelle Agresti and Werner Landry. Summit reached on June 3 and 4,1976,1977 Infinite Spur, on the south face by Michael Kennedy and George Lowe. 1977 Southwest Ridge, Nancey Goforth, Erik LeRoy, Chris Liddle, the summit was reached on June 25,1977, after 47 days spent on Mount Foraker. 1989 Infinite Spur, second ascent or route by Mark Bebie, summit reached on June 24,1989 after 13 days on the mountain. 1990 False Dawn, on the southeast face, first ascent by John Phelan, summit reached on May 27,1990 after 5 days on the mountain. PhotoMountains, High resolution aerial photographs of Mount Foraker climbing routes
37.
Mount Lucania
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Mount Lucania is the third highest mountain located entirely in Canada. A long ridge connects Mount Lucania with Mount Steele, the fifth highest in Canada, Lucania was named by the Duke of Abruzzi, as he stood on the summit of Mount Saint Elias on July 31,1897, having just completed the first ascent. Seeing Lucania in the far distance, beyond Mount Logan, he named it after the ship on which the expedition had sailed from Liverpool to New York. The first ascent of Mount Lucania was made in 1937 by Bradford Washburn and they used an airplane to reach Walsh Glacier,2,670 m above sea level, the use of air support for mountaineering was novel at the time. Washburn called upon Bob Reeve, a famous Alaskan bush pilot, the ski-equipped Fairchild F-51 made several trips to the landing site on the glacier without event in May, but on landing with Washburn and Bates in June, the plane sank into unseasonal slush. The second ascent of Lucania was made in 1967 by Jerry Halpern, Mike Humphreys, Gary Lukis, list of mountain peaks of Canada David Roberts, Escape from Lucania, An Epic Story of Survival, Simon & Schuster, ISBN 0-7432-2432-9
38.
Iztaccihuatl
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Iztaccíhuatl, is a 5,230 m dormant volcanic mountain in Mexico located on the border between the State of Mexico and Puebla. It is the third highest, after Pico de Orizaba 5,636 m. The name Iztaccíhuatl is Nahuatl for White woman, reflecting the four individual snow-capped peaks which depict the head, chest, knees, Iztaccíhuatl lies to the north of Popocatépetl, to which it is connected by the high altitude Paso de Cortés. Depending on atmospheric conditions the dormant volcano is visible much of the year from Mexico City some 70 km to the northwest, the first recorded ascent was made in 1889, though archaeological evidence suggests the Aztecs and previous cultures climbed it previously. It is the lowest peak containing permanent snow and glaciers in Mexico, the summit ridge of the massive 450 km3 volcano is a series of overlapping cones constructed along a NNW-SSE line to the south of the Pleistocene Llano Grande caldera. Andesitic and dacitic Pleistocene and Holocene volcanism has taken place from vents at or near the summit, areas near the El Pecho summit vent are covered in flows and tuff beds post-dating glaciation approximately 11 ka. The most recent vents are located at El Pecho and a depression at 5,100 m along the summit ridge midway between that summit and Los Pies, in Aztec mythology, Iztaccíhuatl was a princess who fell in love with one of her fathers warriors, Popocatépetl. The emperor sent Popocatépetl to war in Oaxaca, promising him Iztaccíhuatl as his wife when he returned, Iztaccíhuatl was falsely told Popocatépetl had died in battle, and believing the news, she died of grief. When Popocatépetl returned to find his dead, he took her body to a spot outside Tenochtitlan. The gods covered them with snow and changed them into mountains, iztaccíhuatls mountain is called White Woman because it resembles a woman lying on her back, and is often covered with snow. (The peak is sometimes nicknamed La Mujer Dormida Popocatépetl became an active volcano, iztaccihuatl is usually listed at 5,286 m. SRTM data and the Mexican national mapping survey assert that a range of 5,220 to 5,230 m is more accurate, the Global Volcanism Program cites 5,230 m
39.
Mount Bona
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Mount Bona is one of the major mountains of the Saint Elias Mountains in eastern Alaska, and is the fifth-highest independent peak in the United States. Mount Bona and its adjacent neighbor Mount Churchill are both large ice-covered stratovolcanoes, the mountain also contributes a large volume of ice to the north-flowing Russell Glacier system. Mount Bona was named by Prince Luigi Amedeo, Duke of the Abruzzi in 1897 and he named it after the Bona, his racing yacht. The mountain was first climbed in 1930 by Allen Carpé, Terris Moore, the current standard route is the East Ridge, a climb of nearby Mount Churchill is a relatively easy addition via this route as well
40.
Mount Steele
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For the mountain in Antarctica, see Mount Steele. Mount Steele is the fifth highest mountain in Canada and the eleventh highest peak in North America reaching the height of 5,073 metres, a lower southeast peak of Mt. Steele stands at 4,300 m. It was named after Sir Sam Steele, the North-West Mounted Police officer in charge of the force in the Yukon during the Klondike Gold Rush. Walter A. Wood led a team consisting of Foresta Wood, Swiss guide Hans Fuhrer, Joseph W. Fobes, Harrison Wood, the expedition approached the peak on the eastern side from Kluane Lake. Base camp was established at the foot of the Steele Glacier with horses carrying loads to Advance Base Camp further along the glacier, ABC provided good views of the mountain and the team decided on the east ridge as their line of ascent. After waiting for the weather to improve after heavy snowfalls, a team consisting of Walter Wood, Harrison Wood, Fuhrer. Their plan to was to make a 2,440 m push to the summit, after steady upwards progress, deteriorating weather forced them to return to Camp 8 where they waited out a five-day storm which dumped over a metre of fresh snow. They started out again on August 15 and the ascent was made easier this time by windblown, at 4,570 m, a plateau of wretched snow forced the team to crawl on all fours. Walter Wood commented, The humour of it impressed me, here were four supposedly normal human beings crawling across a snow field 15,000 ft. up in the air, engaged in what they fondly believed to be a sporting venue. Alternating the lead every 100 paces, they made their way from the plateau to the top, the team enjoyed a blissful thirty minutes of windless conditions on top before beginning their descent. List of mountain peaks of North America List of mountain peaks of Canada
41.
Mount Blackburn
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Mount Blackburn is the highest peak in the Wrangell Mountains of Alaska in the United States. It is the fifth-highest peak in the United States and the twelfth-highest peak in North America, the mountain is an old, eroded shield volcano, the second-highest volcano in the U. S. behind Mount Bona and the fifth-highest in North America. It was named in 1885 by Lt. Henry T. Allen of the U. S. Army after Joseph Clay Stiles Blackburn and it is located in the heart of Wrangell – St. Elias National Park, the largest national park in the country. The mountain also contributes a large volume of ice to the north-flowing Nabesna Glacier, Mount Blackburn is a large, dramatic peak, with great local relief and independence from higher peaks. Its west face drops over 11,000 ft to the Kuskulana Glacier in less than 4 horizontal miles and its other faces drop 8, 000–10,000 ft, all in less than 8 miles. The toe of the Kuskulana Glacier, less than 12 miles from the summit, lies at an elevation of 2,400 ft, while these figures speak to the peaks relief, one measure of its independence is that it is the 50th-most topographically prominent peak in the world. The western of Blackburns two summits is the mountains highest point, a fact that was not understood until the 1960s when new USGS maps were published. The first ascent of the west peak, and hence Mount Blackburn, was done on May 30,1958, by Bruce Gilbert, Dick Wahlstrom, Hans Gmoser, Adolf Bitterlich, and Leon Blumer via the North Ridge. This team made the first ascent of Blackburn, but did not even know it at the due to the incorrect identification of the highest point. In fact, Blumers article in the 1959 American Alpine Journal is titled Mount Blackburn – Second Ascent, kennedy Peak, or East Blackburn,16,286 ft, is the eastern summit and was originally thought to be the highest point. The first ascent of this summit was made in 1912 by Dora Keen and George Handy via the Kennicott Glacier and this heady exploit was ahead of its time. Keen went on to write an article for the Saturday Evening Post titled, “First up Mount Blackburn. ”In 1912, Keen. Todays standard route on the peak is the 1958 ascent route, the North Ridge, the route starts from an airstrip on the glacier at an altitude of 7,200 feet. It is a climb by Alaskan standards. Richter, Donald H. Rosenkrans, Danny S. Steigerwald, Margaret J. Guide to the Volcanoes of the Western Wrangell Mountains, a Geologic Guide to Wrangell—Saint Elias National Park and Preserve, Alaska, A Tectonic Collage of Northbound Terranes. Richter, Donald H. Preller, Cindi C, labay, Keith A. Shew, Nora B. Geologic Map of the Wrangell-Saint Elias National Park and Preserve, Alaska
42.
Mount Sanford (Alaska)
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Mount Sanford is a shield volcano in the Wrangell Volcanic Field, in eastern Alaska near the Copper River. It is the third highest volcano in the United States behind Mount Bona, the south face of the volcano, at the head of the Sanford Glacier, rises 8,000 feet in 1 mile resulting in one of the steepest gradients in North America. Mount Sanford is mainly composed of andesite, and is an ancient peak, being mostly Pleistocene, the mountain first began developing 900,000 years ago, when it began growing on top of three smaller shield volcanoes that had coalesced. The second flow was basaltic in nature and marks the most recent activity of the volcano, the flow was dated using radiometric methods. The mountain was named in 1885 by Lieutenant Henry T. Allen of the U. S. Army after the Sanford family. Mount Sanford was first climbed on July 21,1938 by noted mountaineers Terris Moore and Bradford Washburn, via the still standard North Ramp route up the Sheep Glacier. This route offers little technical difficulty and is a glacier hike all the way to the summit but is still a serious mountaineering challenge due to the altitude and latitude of the peak. The base of the route is accessed by air. On March 12,1948, Northwest Airlines Flight 4422 crashed into Mount Sanford, all 24 passengers and 6 crew members were killed. The wreckage was covered by snow and was not found again until 1999. The first solo ascent of Sanford was achieved on September 19,1968, by Japanese mountaineer Naomi Uemura, rosenkrans, Danny S. Steigerwald, Margaret J. Guide to the Volcanoes of the Western Wrangell Mountains, Alaska. Richter, Donald H. Preller, Cindi C, labay, Keith A. Shew, Nora B. Geologic Map of the Wrangell-Saint Elias National Park and Preserve, Alaska, a Geologic Guide to Wrangell—Saint Elias National Park and Preserve, Alaska, A Tectonic Collage of Northbound Terranes. Wood, Charles A. Kienle, Jürgen, eds, mt. Sanford Expedition via the Sheep Glacier,2014
43.
Mount Vancouver
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Mount Vancouver is the 15th highest mountain in North America. Mount Vancouver has three summits, north, middle, and south, with the summit being the lowest. The south summit, Good Neighbor Peak at 4,785 m, the mountain was named by William Healey Dall in 1874 after George Vancouver, who explored the southeast coast of Alaska from 1792 to 1794. 1949 North Buttress, FA of mountain by William Hainsworth, Alan Bruce-Robertson, Bob McCarter, Noel Odell,1975 Northeast Ridge, FA by Cliff Cantor, Bob Dangel, Paul Ledoux, Rob Milne, Hal Murray, Bob Walker, John Yates and Barton DeWolf. 1977 West Face, FA by John Lauchlan, John Calvert, Trevor Jones, pushing the Limits, The Story of Canadian Mountaineering. Calgary, Alberta, Canada, Rocky Mountain Books
44.
Nevado de Toluca
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Nevado de Toluca is a large stratovolcano in central Mexico, located about 80 kilometres west of Mexico City near the city of Toluca. It is generally cited as the fourth highest of Mexicos peaks, after Pico de Orizaba, Popocatépetl and Iztaccíhuatl, although by some measurements, recently other evidence regarding the etymologies of this mountain have surfaced and after many archeology discoveries in and around the area. It has been concluded that its etymology is Chicnauhtecatl meaning nine lakes as the top of the cone has various deep lakes. The volcano has a 1. 5-kilometre wide summit caldera which is open to the east. The highest summit,4, 680-metre Pico del Fraile, is on the southwest side of the crater and the second highest,4, 640-metre Pico del Aguila, is on the northwest. There are two lakes on the floor of the basin at about 4,200 m, the larger Lago del Sol and the smaller. A road formerly ran into the caldera to the lakes, making perhaps the most accessible major Mexican peak. The road is now gated 2 km before the lakes, the last major eruption of Nevado de Toluca occurred about 10,500 years ago, as the volcano erupted a total estimated volume of 14 km3 for a VEI strength of 6. The eruption emplaced 1.5 m of pebble-sized pumice in the City of Toluca region, distal lahar deposits derived from the Upper Toluca Pumice event incorporated mammoth bones and other mammals in the basin of Mexico. A future event of magnitude would disrupt the lives of 30 million people now living in these cities. From the southeast, Nevado de Toluca looks flat-topped, like shoulders without a head, a Nahuatl legend provides a mythical explanation. The volcano and the area around it is now a national park, near the summit, Nevado de Toluca has a cold alpine climate with cold temperatures year round. There is little variation in the temperatures and frost and snow can occur in any month, the dry season covers from November to March and precipitation is low, averaging 12.4 millimetres in March, the driest month. Temperatures during this time are cold, averaging 2.3 °C in January, the wet season spans from May to October and precipitation is very high, averaging 243.5 millimetres in July. The summit is often foggy, averaging 110 days with fog, the wettest record month was July 2008 when 513.5 millimetres of precipitation fell and the wettest recorded day was July 16,1999 when 90.5 millimetres of precipitation fell. The highest temperature recorded was 23 °C on August 16,1993. There are 18 registered archeological sites in the park, as this was a ritual center during pre-Hispanic periods, bernardino de Sahagún wrote about the lakes as a place where the indigenous held ceremonies and sacrifices. The lakes themselves are considered to be two sites, as a number of offerings, especially copal, were deposited in the lakes
