Misplaced Pages

#679320

81-911: The Lone Pine Paiute-Shoshones traditionally spoke two different languages. The Mono ("Paiutes") spoke the Mono language and the Timbisha ("Shoshones") spoke the Timbisha language , both of which were members of the Numic subgroup of the Uto-Aztecan language family. The Paiute-Shoshone Indians of the Lone Pine Community is a federal recognized tribe and reside on the reservation, the Lone Pine Indian Reservation in Inyo County, in central-eastern California , in

162-666: A Native American people who traditionally live in the central Sierra Nevada , the Eastern Sierra (generally south of Bridgeport ), the Mono Basin , and adjacent areas of the Great Basin . They are often grouped under the historical label " Paiute " together with the Northern Paiute and Southern Paiute – but these three groups, although related within the Numic group of Uto-Aztecan languages, do not form

243-532: A foreman working for Sacramento pioneer John Sutter , found shiny metal in the tailrace of a lumber mill Marshall was building for Sutter on the American River . Rumors soon started to spread and were confirmed in March 1848 by San Francisco newspaper publisher and merchant Samuel Brannan . Brannan strode through the streets of San Francisco, holding aloft a vial of gold, shouting "Gold! Gold! Gold from

324-571: A portion of the area, a triangle whose vertices are Reno, Nevada ; Fresno, California ; and Las Vegas, Nevada , has been dubbed the " Nevada Triangle ", in reference to the Bermuda Triangle . Some counts put the number of crashes in the triangle at 2,000, including millionaire and record-breaking flyer Steve Fossett . Hypotheses that the crashes are related in some way to the United States Air Force 's Area 51 , or to

405-448: A powerful stream or jet of water at gold-bearing gravel beds. It is estimated that by the mid-1880s, 11 million troy ounces (340 metric tons) of gold (worth approximately US$ 16 billion in 2020 prices) had been recovered by "hydraulicking". A consequence of these extraction methods was that large amounts of gravel, silt , heavy metals , and other pollutants were washed into streams and rivers. As of 1999 , many areas still bear

486-706: A publication of his photographs under the title Parmelian Prints of the High Sierras , commented, "The name Sierra is already a plural. To add an s is a linguistic, Californian, and mountaineering sin." The Sierra Nevada lies primarily in Central and Eastern California , with the Carson Range , a small but historically important spur, extending into Nevada. West-to-east, the Sierra Nevada's elevation increases gradually from 500 feet (150 m) in

567-501: A short period, and the lightning can start fires. Summer high temperatures average 42–90 °F (6–32 °C). Winters are comparatively mild, and the temperature is usually only just low enough to sustain a heavy snowpack. For example, Tuolumne Meadows , at 8,600 feet (2,600 m) elevation, has winter daily highs about 40 °F (4 °C) with daily lows about 10 °F (−12 °C). The growing season lasts 20 to 230 days, strongly dependent on elevation. The highest elevations of

648-769: A single, unique, unified group of Great Basin tribes. Today, many of the tribal citizens and descendants of the Mono tribe inhabit the town of North Fork (thus the label "Northfork Mono") in Madera County . People of the Mono tribe are also spread across California in: the Owens River Valley ; the San Joaquin Valley and foothills areas, especially Fresno County ; and in the San Francisco Bay Area . The Mono lived on both sides of

729-447: Is Mount Lyell (13,120 ft or 3,999 m). The Sierra rises to almost 14,000 feet (4,300 m) with Mount Humphreys near Bishop, California . Finally, near Lone Pine , Mount Whitney is at 14,505 feet (4,421 m), the highest point in the contiguous United States . South of Mount Whitney, the elevation of the range quickly dwindles. The crest elevation is almost 10,000 feet (3,000 m) near Lake Isabella , but south of

810-534: Is difficult to determine how many of these are Mono. Sierra Nevada The Sierra Nevada ( / s i ˌ ɛr ə n ɪ ˈ v æ d ə , - ˈ v ɑː d -/ see- ERR -ə nih- VA(H)D -ə ) is a mountain range in the Western United States , between the Central Valley of California and the Great Basin . The vast majority of the range lies in the state of California , although

891-456: Is either protected from development or strictly managed. The mountain range is home to three National Parks  – Yosemite , Kings Canyon , and Sequoia  – and two national monuments  – Devils Postpile and Giant Sequoia . Ten national forests span much of the mountain range's remaining area. Within these national parks, monuments, and forests lie 26 wilderness areas , which together protect 15.4% of

SECTION 10

#1732771835680

972-428: Is higher in the east. A list of biotic zones, and corresponding elevations, is presented below: Archaeological excavations placed Martis people of Paleo-Indians in northcentral Sierra Nevada during the period of 3,000 BCE to 500 CE. The earliest identified sustaining indigenous people in the Sierra Nevada were the Northern Paiute tribes on the east side, with the Mono tribe and Sierra Miwok tribe on

1053-831: Is the Tribal Chairman for the North Fork Mono Tribe, which is not a federally recognized tribe. The North Fork Rancheria of Mono Indians is the federally recognized tribe in North Fork and their Chairperson is Elaine Fink. Ceremonies are performed at the Sierra Mono Museum in North Fork, California , and an annual Indian Fair Days festival takes place on the first weekend of August every year to revive many traditions and rituals for tribal kin and tourists alike to enjoy. The Eastern Mono speak

1134-771: Is the source of much of the sedimentary rock in California. In the Cretaceous , a subduction zone formed at the edge of the continent. This means that an oceanic plate started to dive beneath the North American Plate . Magma, formed through the subduction of the ancient Farallon Plate , rose in plumes ( plutons ) deep underground, their combined mass forming what is called the Sierra Nevada batholith . These plutons formed at various times, from 115  Ma to 87 Ma. The earlier plutons formed in

1215-711: The 2010 Census the population was 212. The tribe is governed by a five-person tribal council, who are as follows: The Lone Pine Indian Community is headquartered in Lone Pine, California . They have their own public works department, environmental department, and tribal administration. The reservation is served by the Lone Pine Unified School District . 36°35′49″N 118°03′22″W  /  36.59694°N 118.05611°W  / 36.59694; -118.05611 Mono people The Mono ( / ˈ m oʊ n oʊ / MOH -noh ) are

1296-462: The Basin and Range Province . As this andesitic volcanism began waning about five million years ago, the rivers were able to begin eroding away the 100s of meters of volcanic deposits and resume the incision that had been halted by the first period of volcanism. Some studies have argued that this recent incision is a sign of recent tectonic uplift. Other geologists claim that the elevations of many of

1377-580: The Carson Range spur lies primarily in Nevada . The Sierra Nevada is part of the American Cordillera , an almost continuous chain of mountain ranges that forms the western "backbone" of the Americas. The Sierra runs 400 mi (640 km) north-south, and its width ranges from 50 mi (80 km) to 80 mi (130 km) across east–west. Notable features include General Sherman ,

1458-661: The Carson River runs into Carson Sink , the Walker River into Walker Lake ; Rush , Lee Vining and Mill Creeks flow into Mono Lake ; and the Owens River into dry Owens Lake . 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

1539-487: The Central Valley to more than 14,000 feet (4,300 m) atop the highest peaks of its crest 50 to 75 miles (80 to 121 km) 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's irregular northern boundary stretches from the Susan River and Fredonyer Pass to

1620-595: The Nevadan orogeny , granite formed deep underground. The range started to uplift less than five million years ago, and erosion by glaciers exposed the granite and formed the light-colored mountains and cliffs that make up the range. The uplift caused a wide range of elevations and climates in the Sierra Nevada, which are reflected by the presence of five life zones (areas with similar plant and animal communities). Uplift continues due to faulting caused by tectonic forces, creating spectacular fault block escarpments along

1701-611: The North Fork Feather River . It represents where the granitic bedrock of the Sierra Nevada dives below the southern extent of Cenozoic igneous surface rock from the Cascade Range . It is bounded on the west by California 's Central Valley , on the east by the Basin and Range Province , and on the southeast by the Mojave Desert . The southern boundary is at Tehachapi Pass . Physiographically,

SECTION 20

#1732771835680

1782-676: The Owens River Valley on the eastern side of the Sierra Nevada Mountains . The reservation is 237 acres (0.96 km) large. Approximately 350 of the 1400 enrolled tribal members live on the reservation. The reservation was established on April 20, 1939 through a land exchange negotiated between the Department of the Interior and the City of Los Angeles . In 1990-1, 168 out of 296 enrolled members lived on reservation. As of

1863-503: The San Joaquin Valley ( San Joaquin River was called typici h huu' – "important, great river"), Kings River and Kaweah River (in today's counties of Madera, Fresno and Tulare) lived mostly as typical semi-nomadic hunters and gatherers of fishing, hunting and gathering as well as agriculture. In the winter, several families descended into the river valleys and built together fixed settlements, most of which were used for several years. In

1944-461: The San Joaquin Valley to the rest of the state in the 1870s. This facilitated the nationwide distribution of lumber. In addition, technological advancements, such as the shay locomotive and the v-shaped log flume , made it easier to transport lumber across mountainous terrain. The tourism potential of the Sierra Nevada was recognized early in the European history of the range. Yosemite Valley

2025-537: The United States started to move to California via Sonora and Walker Passes . In the winter of 1844, Lt. John C. Frémont , accompanied by Kit Carson , was the first European American to see Lake Tahoe . The Frémont party camped at 8,050 ft (2,450 m). The California Gold Rush began at Sutter's Mill , near Coloma , in the western foothills of the Sierra. On January 24, 1848, James W. Marshall,

2106-524: The endorheic basin of Tulare Lake , which rarely overflows into the San Joaquin during wet years. 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 . From north to south, the Susan River flows into intermittent Honey Lake , the Truckee River flows from Lake Tahoe into Pyramid Lake ,

2187-637: The "Eastern Mono bands" bordered in the northwest on the areas of the hostile Southern Sierra Miwok with which it often came to conflicts, in the northeast several Northern Paiute bands migrated, in the southeast and south the Timbisha Shoshone and Western Shoshone bands, in the southwest the Tübatulabal (also: Kern River Indians ) and in the west the "Western Mono bands". The Owens Valley Paiute were also more aggressive and hostile towards neighboring Indian tribes and most recently they fought

2268-443: The "Monachi/Monache" dialect (better known as: "Mono/Monache" or "Mono Lake Paiute"). Of the 1,000 "Owens Valley Paiute (Eastern Mono) people" there are only 30 active speakers of the "Eastern Mono" or "Owens Valley Northern Paiute" dialect left. Estimates for the pre-contact populations of most native groups in California have varied substantially. (See Population of Native California .) Alfred L. Kroeber (1925:883) suggested that

2349-505: The "Mono language" and culture through the immigration of the "Western Mono" and soon became bilingual) or as "Western Mono" bands (who would have adopted the language of the dominant "Foothill Yokuts"). In particular, the classification of the two Kings River bands – the Michahai / Michahay and Entimbich – is difficult. The Western Mono self-designation is Nyyhmy, Nimi, Nim or Nium , meaning "People" or cawu h nyyhmy . By contact with

2430-446: The "Western Mono bands", to feed larger groups. The Sedentism is also reflected in their socio-political organization in different "districts" (each with communistic hunting and seed rights, political unity, and a number of villages), whose name mostly ended with "patü/witü" , meaning "place" or "land"; each "district" was under the command of a headman or pohenaby . Some "Owens Valley Northern Paiute" districts: The tribal areas of

2511-556: The 1770 population of the Mono was 4,000. Sherburne F. Cook (1976:192) set the population of the Western Mono alone at about 1,800. Kroeber reported the population of the Mono in 1910 as 1,500. Today, there are approximately 2,300 enrolled Mono people. The Cold Springs Mono have 275 tribal members. The Northfork Mono's enrollment is 1,800, making them one of California's largest native tribes. The Big Sandy Mono have about 495 members. The Big Pine Band has 462 tribal members, but it

Lone Pine Paiute-Shoshone Tribe - Misplaced Pages Continue

2592-742: The American River!" On August 19, 1848, the New York Herald was the first major newspaper on the East Coast to report the discovery of gold. On December 5, 1848, President James Polk confirmed the discovery of gold in an address to Congress . Soon, waves of immigrants from around the world, later called the "forty-niners", invaded the Gold Country of California or "Mother Lode". Miners lived in tents, wood shanties, or deck cabins removed from abandoned ships. Wherever gold

2673-467: The Americans in the " Owens Valley Indian War " (1862 to 1863) with allied Shoshone, Kawaiisu and Tübatulabal The Owens Valley Paiutes are The Southernmost Northern Paiute Band. Their self-designation is Numa , Numu, or Nüümü , meaning "People" or Nün'wa Paya Hup Ca'a' Otuu'mu —"Coyote's children living in the water ditch". The "Western Mono" bands in the western southern Sierra Nevada foothills in

2754-612: The Europeans, the following bands (or local groups) could be distinguished (from north to south): If the Entimbich and Michahai are counted as "Kings River Yokuts" then beside the above-mentioned bands sometimes the following bands are listed: The two clans of the North Fork Mono Tribe are represented by the golden eagle and the coyote. Mono traditions still in practice today include fishing, hunting, acorn gathering, cooking, healing, basket making, and games. The Honorable Ron Goode

2835-432: The Mono people is referred to as "Nim." Mun a hoo e boso. Mun a hoo e num. Mun a hoo to e hun noh pa teh can be translated as "Hello to my friends. Hello to the Mono people. Hello to the people from all over." Today, the Mono language (including its two dialects) is critically endangered. Among about 1,300 "Western Mono (Mono or Monache) people", only about 20 active speakers and 100 half speakers speak "Western Mono" or

2916-597: The Mono/Bannock language dialect, which together with the Northern Paiute language (a dialect continuum ), forms the Western Numic branch of the Uto-Aztecan language family. Due to the geographical separation as well as the interaction with neighboring tribes and peoples (incorporation of loanwords and/or frequent Bilingualism ) two very different dialects developed in the course of time which are difficult to understand for each other. The native language of

2997-806: The Pacific Ocean at San Francisco . The northern third of the western Sierra is part of the Sacramento River watershed (including the Feather , Yuba , and American River tributaries), and the middle third is drained by the San Joaquin River (including the Mokelumne , Stanislaus , Tuolumne , and Merced River tributaries). The southern third of the range is drained by the Kings , Kaweah , Tule , and Kern rivers, which flow into

3078-722: The Park in 1906. In the same year, Sequoia National Park was formed to protect the Giant Sequoia: all logging of the Sequoia ceased at that time. In 1903, the city of San Francisco proposed building a hydroelectric dam to flood Hetch Hetchy Valley . The city and the Sierra Club argued over the dam for 10 years, until the U.S. Congress passed the Raker Act in 1913 and allowed dam building to proceed. O'Shaughnessy Dam

3159-519: The Sierra Nevada and are divided into two regional tribal/dialect groups, roughly based on the Sierra crest: The current tribal name "Mono" is a Yokutsan loanword from the tribe's western neighbors, the Yokuts , who however hereby designated the Owens valley Paiutes as the southernmost Northern Paiute band living around "owens lake" / Mono Lake as monachie/monoache (" fly people") because fly larvae

3240-478: The Sierra Nevada increases gradually from north to south. Between Fredonyer Pass and Lake Tahoe, the peaks range from 5,000 feet (1,500 m) to more than 9,000 feet (2,700 m). The crest near Lake Tahoe is roughly 9,000 feet (2,700 m) high, with several peaks approaching the height of Freel Peak (10,881 ft or 3,317 m). Farther south, the highest peak in Yosemite National Park

3321-559: The Sierra Nevada is influenced by the Mediterranean climate of California. During the fall, winter and spring, precipitation in the Sierra ranges from 20 to 80 in (510 to 2,030 mm) where it occurs mostly as snow above 6,000 ft (1,800 m). Precipitation is highest on the central and northern portions of the western slope between 5,000 and 8,000 feet (1,500 and 2,400 m) elevation, due to orographic lift . Above 8,000 feet (2,400 m), precipitation diminishes on

Lone Pine Paiute-Shoshone Tribe - Misplaced Pages Continue

3402-508: The Sierra Nevada started in the early 1800s, when settlers relied on hand tools and ox-teams. Before the California Gold Rush, the industry was relatively small, and most of the lumber used in the state was imported. However, as the demand for lumber to support the mining industry increased, logging became a major industry in the region. Initially, most of the lumber produced in California was used in mining. The Comstock Lode

3483-431: The Sierra have an alpine climate . The Sierra Nevada snowpack is the major source of water and a significant source of electric power generation in California. Many reservoirs were constructed in the canyons of the Sierra throughout the 20th century, Several major aqueducts serving both agriculture and urban areas distribute Sierra water throughout the state. However, the Sierra casts a rain shadow , which greatly affects

3564-662: 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 California Geological Survey states that "the northern Sierra boundary is marked where bedrock disappears under the Cenozoic volcanic cover of the Cascade Range." The range is drained on its western slope by the Central Valley watershed, which discharges into

3645-497: The Sierra's 63,118 km (24,370 sq mi) from logging and grazing. The United States Forest Service and the Bureau of Land Management currently control 52% of the land in the Sierra Nevada. Logging and grazing are generally allowed on land controlled by these agencies, under federal regulations that balance recreation and development on the land. The California Bighorn Sheep Zoological Area near Mount Williamson in

3726-476: The Sierra. The combination of river and glacier erosion exposed the uppermost portions of the plutons emplaced millions of years before, leaving only a remnant of metamorphic rock on top of some Sierra peaks. Extension of the Basin and Range continues today, leading to downdropping of crustal blocks just east of the Sierra Nevada during large earthquakes, such as the Lone Pine earthquake of 1872. The climate of

3807-650: The Tuolumne and Merced River drainage. The group may have been the first non-indigenous people to see Yosemite Valley . The Walker Party probably visited either the Tuolumne or Merced Groves of giant sequoia , becoming the first non-indigenous people to see the giant trees, but journals relating to the Walker party were destroyed in 1839, in a print shop fire in Philadelphia. Starting in 1841, emigrants from

3888-444: The activities of extra-terrestrial aliens , have no evidence to support them. The Sierra Nevada is divided into a number of biotic zones , each of which is defined by its climate and supports a number of interdependent species. Life in the higher elevation zones adapted to colder weather, and to most of the precipitation falling as snow. The rain shadow of the Sierra causes the eastern slope to be warmer and drier: each life zone

3969-505: The area around Yosemite National Park and what would become Kings Canyon National Park . James S. Hutchinson , a noted mountaineer, climbed the Palisades (1904) and Mount Humphreys (1905). By 1912, the USGS published a set of maps of the Sierra Nevada, and the era of exploration was over. Logging in the Sierra Nevada has significantly impacted the landscape. The logging industry in

4050-405: The climate and ecology of the central Great Basin . This rain shadow is largely responsible for Nevada being the driest state in the United States. Precipitation varies substantially from year to year. It is not uncommon for some years to receive precipitation totals far above or below normal. The height of the range and the steepness of the Sierra Escarpment, particularly at the southern end of

4131-412: The crest and north of 37.2°N. In the Triassic and into the Jurassic , an island arc collided with the west coast of North America and raised a chain of volcanoes, in an event called the Nevadan orogeny . Nearly all subaerial Sierran Arc volcanoes have since disappeared; their remains were redeposited during the Great Valley Sequence and the subsequent Cenozoic filling of the Great Valley, which

SECTION 50

#1732771835680

4212-407: The eastern edge of the southern Sierra. The Sierra Nevada has played an important role in the history of California and the United States. The California gold rush occurred in the western foothills from 1848 through 1855. Due to its inaccessibility, the range was not fully explored until 1912. Used in 1542 by Juan Rodríguez Cabrillo to describe a Pacific Coast Range ( Santa Cruz Mountains ),

4293-406: The highest peak in the range. In 1873, Mount Whitney was climbed for the first time by 3 men from Lone Pine, California, on a fishing trip. From 1892 to 1897 Theodore Solomons made the first attempt to map a route along the crest of the Sierra. Other people finished exploring and mapping the Sierra. Bolton Coit Brown explored the Kings River watershed in 1895–1899. Joseph N. LeConte mapped

4374-442: The lake, the peaks reach only a modest 8,000 feet (2,400 m). There are several notable geographical features in the Sierra Nevada: Communities in the Sierra Nevada include Paradise , South Lake Tahoe , Truckee , Grass Valley , Lee Vining , Mammoth Lakes , Sonora , Nevada City , Placerville , Pollock Pines , Portola , Auburn , Colfax and Kennedy Meadows . Much of the Sierra Nevada consists of federal lands and

4455-620: The largest tree in the world by volume; Lake Tahoe , the largest alpine lake in North America; Mount Whitney at 14,505 ft (4,421 m), the highest point in the contiguous United States ; and Yosemite Valley sculpted by glaciers from one-hundred-million-year-old granite , containing high waterfalls . The Sierra is home to three national parks , twenty-six wilderness areas, ten national forests, and two national monuments. These areas include Yosemite , Sequoia , and Kings Canyon National Parks , as well as Devils Postpile National Monument . More than one hundred million years ago during

4536-429: The late 1800s due to several factors. The Timber and Stone Act of 1878 allowed individuals to claim ownership of old-growth timber tracts, which were later consolidated under joint-stock companies , such as those founded by Midwestern lumber magnates. These companies had the financial resources to transport timber from remote locations and build sawmills near the tracks of the Southern Pacific railroad which connected

4617-455: The late 1800s, the logging industry moved westward due to the depletion of white pine forests in the upper Midwest. This shift was encouraged by the positive portrayal of the Sierra Nevada as a promising timber region. In 1859, Horace Greely marveled, "I never saw anything so much like good timber in the course of any seventy-five miles' travel as I saw in crossing the Sierra Nevada." The logging industry experienced significant growth in

4698-417: The miners, provoking counter-attacks on native villages. The Native Americans, out-gunned, were often slaughtered. The Gold Rush populated the western foothills of the Sierra Nevada, but even by 1860, most of the Sierra was unexplored. The state legislature authorized the California Geological Survey to officially explore the Sierra (and survey the rest of the state). Josiah Whitney was appointed to head

4779-440: The modern rivers flowing down the range are only 100–300 meters (300–1,000 ft) lower than their ancient counterparts from 30–40 million years ago and the overall elevation and bedrock topography of the northern Sierra Nevada has changed little since at least 30–40 million years ago. About 2.5 Ma, the Earth's climate cooled, and ice ages started. Glaciers carved out characteristic U-shaped canyons throughout

4860-472: The mountains were amongst a group led by fur trapper Jedediah Smith , crossing north of the Yosemite area in May 1827, at Ebbetts Pass . In 1833, a subgroup of the Bonneville Expedition led by Joseph Reddeford Walker was sent westward to find an overland route to California . Eventually the party discovered a route along the Humboldt River across present-day Nevada , ascending the Sierra Nevada, starting near present-day Bridgeport and descending between

4941-409: The mountains. Washo and Maidu were also in this area prior to the era of European exploration and displacement. American exploration of the mountain range started in 1827. Although prior to the 1820s there were Spanish missions , pueblos (towns), presidios (forts), and ranchos along the coast of California, no Spanish explorers visited the Sierra Nevada. The first Americans to visit

SECTION 60

#1732771835680

5022-447: The north to Owens Lake on the south, and from the crest of the Sierra Nevada on the west to the White and Inyo Mountains including the Fish Lake and Deep Springs Valleys on the east. They were predominantly sedentary and settled in fixed settlements along rivers or springs (or artificial canals). The more intensive arable farming by means of partly artificial irrigation enabled them to build up food reserves and thus, in contrast to

5103-399: The northern Sierran valleys with volcanic deposits. These pyroclastic flows, which continued for about 10 million years, were followed by andesitic lahars which nearly completely buried the northern Sierran landscape such that only the tallest peaks emerged above a volcanic plain. This second period of volcanism appears to have been triggered by crustal extension associated with extension of

5184-399: The oldest being metasedimentary rocks from the Cambrian in the Mount Morrison region. These dark-colored hornfels , slates , marbles , and schists are found in the western foothills (notably around Coarsegold , west of the Tehachapi Pass ) and east of the Sierra Crest. The earliest granite of the Sierra started to form in the Triassic period. This granite is mostly found east of

5265-413: The plural ( Smokies , Rockies , Cascades , etc.), since Sierra is already pluralized in its native language, some locals who live in "the Sierra" are not hesitant to admonish those who refer to the area as "the Sierras". However, there are historical and literary references that use the plural, such as the 1871 collection of Joaquin Miller poems, Songs of the Sierras . Ansel Adams , in response to

5346-420: The range, produces a wind phenomenon known as the "Sierra Rotor". This is a horizontal rotation of the atmosphere just east of the crest of the Sierra, set in motion as an effect of strong westerly winds. Because of the large number of airplanes that have crashed in the Sierra Nevada, primarily due to the complex weather and atmospheric conditions such as downdrafts and microbursts caused by geography there,

5427-502: The scars of hydraulic mining, since the resulting exposed earth and downstream gravel deposits do not support plant life. It is estimated that by 1855, at least 300,000 gold-seekers, merchants, and other immigrants had arrived in California from around the world. The huge numbers of newcomers brought by the Gold Rush drove Native Americans out of their traditional hunting, fishing and food-gathering areas. To protect their homes and livelihood, some Native Americans responded by attacking

5508-445: The southeast and the Foothill Yokuts in the west. Some "Western Mono" bands formed bilingual bands or units with "Foothill Yokuts" and partly took over their culture, so that today – except for one – each "Western Mono" band are only known under its "Yokuts" name. Even in the ethnological literature the original ethnic classification of the bands listed below is controversial; partly they are listed as "Foothill Yokuts bands" (who adopted

5589-407: The southern Sierra was established to protect the endangered Sierra Nevada bighorn sheep . Starting in 1981, hikers were unable to enter the Area from May 15 through December 15, in order to protect the sheep. As of 2010, the restriction has been lifted and access to the Area is open for the whole year. The earliest rocks in the Sierra Nevada are metamorphic roof pendants of Paleozoic age,

5670-401: The summer, the family groups migrated as hunters and gatherers to the more sheltered and cooler altitudes of the mountains. Therefore, these smaller groups are sometimes considered socio-politically not as bands but as local groups. The tribal areas of the "Western Mono" bordered the (mostly) hostile Southern Sierra Miwok in the north, the "Eastern Mono" settled in the east, the Tübatulabal in

5751-425: The survey. Men of the survey, including William H. Brewer , Charles F. Hoffmann and Clarence King , explored the backcountry of what would become Yosemite National Park in 1863. In 1864, they explored the area around Kings Canyon . In 1869, John Muir started his wanderings in the Sierra Nevada range, and in 1871, King was the first to climb Mount Langley , mistakenly believing he had summited Mount Whitney ,

5832-490: The term "Sierra Nevada" was a general identification of less familiar ranges toward the interior. In 1776, Pedro Font 's map applied the name to the range currently known as the Sierra Nevada. The literal translation is "snowy mountains", from sierra "a range of mountains", 1610s, from Spanish sierra "jagged mountain range", lit. "saw", from Latin serra "a saw"; and from fem. of Spanish nevado "snowy". While many mountain ranges are unanimously referred to in

5913-424: The water from an entire river into a sluice alongside the river, and then dig for gold in the newly exposed river bottom. By 1853, most of the easily accessible gold had been collected, and attention turned to extracting gold from more difficult locations. Hydraulic mining was used on ancient gold-bearing gravel beds on hillsides and bluffs in the gold fields. In hydraulic mining, a high-pressure hose directed

5994-625: The west as Panan witü / Pana witü ("western place" People); the "Western Mono" called themselves Nyyhmy/Nimi or Nim/Nium ("People"); a full blooded "Western Mono" person was called cawu h nyyhmy . The Owens Valley Paiute or Eastern Mono live on the California-Nevada border, they formerly ranged on the eastern side of the southern Sierra Nevada across the Owens Valley along the Owens Rivers from Long Valley on

6075-529: The western half of the Sierra, while the later plutons formed in the eastern half of the Sierra. At this time, the Sierra Nevada formed the western ramp of a high plateau to the east, the Nevadaplano . During this period, rivers cut deep canyons into the range, generating topographic relief similar to the modern Sierra Nevada. This period of incision was halted approximately 30 million years ago by vast outpourings of pyroclastic flows from Nevada which filled

6156-509: The western side, and the Kawaiisu and Tübatulabal tribes in the southern Sierra. Today, some historic intertribal trade route trails over mountain passes are known artifact locations, such as Duck Pass with its obsidian arrowheads . The California and Sierra Native American tribes were predominantly peaceful, with occasional territorial disputes between the Paiute and Sierra Miwok tribes in

6237-511: The western slope up to the crest, since most of the precipitation has been wrung out at lower elevations. Most parts of the range east of the crest are in a rain shadow , and receive less than 25 inches of precipitation per year. While most summer days are dry, afternoon thunderstorms are common, particularly during the North American Monsoon in mid and late summer. Some of these summer thunderstorms drop over an inch of rain in

6318-470: Was a major center for logging, with operations supplying lumber for the construction of mine structures, such as tunnels, shafts, and buildings, as well as fuel for the mines. Dan DeQuille observed in 1876, "the Comstock Lode may truthfully be said to be the tomb of the forests of the Sierra. Millions upon millions of feet of lumber are annually buried in the mines, nevermore to be resurrected.” In

6399-479: Was discovered, hundreds of miners would collaborate to put up a camp and stake their claims. Because the gold in the California gravel beds was so richly concentrated, the early forty-niners simply panned for gold in California's rivers and streams. However, panning cannot take place on a large scale, and miners and groups of miners graduated to more complex placer mining. Groups of prospectors would divert

6480-440: Was first protected by the federal government in 1864. The Valley and Mariposa Grove were ceded to California in 1866 and turned into a state park. John Muir perceived overgrazing by sheep and logging of giant sequoia to be a problem in the Sierra. Muir successfully lobbied for the protection of the rest of Yosemite National Park: Congress created an Act to protect the park in 1890. The Valley and Mariposa Grove were added to

6561-598: Was their chief food staple and trading article and not the "Mono". This " Kucadikadi Northern Paiute Band ", whose autonym Kutsavidökadö/Kutzadika'a means "eaters of the brine fly pupae", are also known as Mono Lake Paiute or Owens Valley Paiute , a holdover from early anthropological literature, and are often confused with the non-Northern Paiute ethnic group of the Western mono "Mono". The "Eastern Mono" referred to themselves as Numa/Nuumu or Nüümü ("People") in their Mono/Bannock language dialect and to their kin to

#679320