Fandango Pass
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Fandango Pass
The Fandango Pass (previously Lassen Pass; variants Lassen Cut-off, Lassen Horn) is a gap in the Warner Mountains of Modoc County, California, USA. Located in the Modoc National Forest, its elevation is above sea level. It is approximately southwest of Fort Bidwell. Fandango Pass was historically notable for its location as the convergence of two trails, the Applegate and the Lassen, that were traveled by emigrant pioneers between 1846 and 1850. The pass can now be traversed on a section of graded gravel, 1.5 lanes wide. It is closed during winter storms. History The mountain pass was located at a convergence of two trails, the Applegate and the Lassen, that were traveled by emigrant pioneers between 1846 and 1850. The Applegate Trail, originally intended as a less dangerous route to the Oregon Territory, was established in 1846 by the Applegate brothers and Levi Scott, and ran through today's U.S. states of Idaho, Nevada, California, and Oregon. The Lassen Horn Trail was ...
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Modoc National Forest
Modoc National Forest is a U.S. national forest in Northeastern California. Geography The Modoc National Forest protects parts of Modoc (82.9% of acreage), Lassen (9.4%), and Siskiyou (7.7%) counties. Most of the forest was covered by immense lava flows occurring over the last 500,000 years. The eastern part of the forest east of Alturas contains the Warner Mountains. The Warner Mountains drop steeply on the eastern slopes, whereas the western flank has a more gentle topography. Ecology Due to the elevation and precipitation differences, the forests hosts a large number of plant species. The western side of the brushy foothills consist mostly of bitterbrush and curl-leaf mahogany. As elevation increases, forests of ponderosa pine, white and red firs, incense cedar, and aspen give way to lodgepole and western white pines sprinkle towards the summit. Some of the forest have been identified as old growth, with lodgepole pine, ponderosa pine, white fir, incense cedar, and ...
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Goose Lake (Oregon-California)
Goose Lake may refer to: Canada Lakes *Goose Lake (Cape Breton), Nova Scotia *Goose Lakes, Halifax, Nova Scotia *Goose Lake (Argyle), Nova Scotia *Goose Lake (Barrington), Nova Scotia *Goose Lake (District of Chester), Nova Scotia *Goose Lake (Cumberland), Nova Scotia *Goose Lake (Guysborough), Nova Scotia *East Goose Lake, Nova Scotia Other places *Goose Lake, Alberta, aka ''Lone Pine'', a hamlet Russia *Lake Gusinoye (Goose Lake), Buryatia, Russia United States Lakes *Goose Lake (Anchorage), Alaska *Goose Lake (Oregon–California) *Goose Lake (Clinton County, Iowa) *Goose Lake (Marquette County, Michigan) *Goose Lake (South Dakota) *Goose Lake (Washington) Other places *Goose Lake, Iowa, a town *Goose Lake Township, Grundy County, Illinois *Goose Lake Valley, a valley in Oregon *Goose Lake National Forest, Oregon *Goose Lake State Recreation Area, Oregon *Goose Lake Prairie State Natural Area, Illinois See also

*Anderson Goose Lake, Iowa *Goose Harbour Lake, Nova Scotia * ...
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Mountain Passes Of California
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Landforms Of Modoc County, California
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ...
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California Historical Landmark
A California Historical Landmark (CHL) is a building, structure, site, or place in California that has been determined to have statewide historical landmark significance. Criteria Historical significance is determined by meeting at least one of these criteria: # The first, last, only, or most significant of its type in the state or within a large geographic region (Northern California, Northern, Central California, Central, or Southern California); # Associated with an individual or group having a profound influence on the history of California; or # An outstanding example of a period, style, architectural movement or construction; or is the best surviving work in a region of a pioneer architect, designer, or master builder. Other designations California Historical Landmarks numbered 770 and higher are automatically listed in the California Register of Historical Resources. A site, building, feature, or event that is of local (city or county) significance may be designated as a ...
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Fandango
Fandango is a lively partner dance originating from Portugal and Spain, usually in triple meter, traditionally accompanied by guitars, castanets, or hand-clapping. Fandango can both be sung and danced. Sung fandango is usually bipartite: it has an instrumental introduction followed by "variaciones". Sung fandango usually follows the structure of "cante" that consist of four or five octosyllabic verses (coplas) or musical phrases (tercios). Occasionally, the first copla is repeated. The meter of fandango is similar to that of the bolero and seguidilla. It was originally notated in time, of slow tempo, mostly in the minor, with a trio in the major; sometimes, however, the whole was in a major key. Later it took the 3-4 tempo, and the characteristic Spanish rhythm. Origins The earliest fandango melody is found in the anonymous "Libro de diferentes cifras de guitarra" from 1705, and the earliest description of the dance itself is found in a 1712 letter by Martín Martí, a Span ...
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List Of Indian Massacres
In the history of the European colonization of the Americas, an Indian massacre is any incident between European settlers and indigenous peoples wherein one group killed a significant number of the other group outside the confines of mutual combat in war. Overview "Indian massacre" is a phrase whose use and definition has evolved and expanded over time. The phrase was initially used by European colonists to describe attacks by indigenous Americans which resulted in mass colonial casualties. While similar attacks by colonists on Indian villages were called "raids" or "battles", successful Indian attacks on white settlements or military posts were routinely termed "massacres". Knowing very little about the native inhabitants of the American frontier, the colonists were deeply fearful, and often, European Americans who had rarely – or never – seen a Native American read Indian atrocity stories in popular literature and newspapers. Emphasis was placed on the depredations of ...
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Surprise Valley (Modoc County, California)
Surprise Valley is a valley in extreme northeastern California, about 60 miles in length from north to south. Locals refer to the area as the Tricorner Region because of the region's location at the intersection of California, Oregon, and Nevada state lines. The valley is east of the Modoc County seat of Alturas. The area is part of the Great Basin which extends across most of the northern half of Nevada. Terrain Most of the valley is over 4,000 feet above mean sea level (AMSL), and could be characterized as a high altitude desert valley. A series of alkaline lakes occupy low-lying areas. Forested mountains mark the west side of the valley. The Hays Canyon Range, (mostly east of the Nevada state line) is to the east, and the Warner Mountains border the west. The valley is considered part of the Great Basin, a desert region roughly covering the geographic majority of Nevada and extending into Utah; also regions of southeast Oregon, and southern California, in the east. Communities i ...
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Black Rock Desert
__NOTOC__ The Black Rock Desert is a semi-arid region (in the Great Basin shrub steppe eco-region) of lava beds and playa, or alkali flats, situated in the Black Rock Desert–High Rock Canyon Emigrant Trails National Conservation Area, a silt playa north of Reno, Nevada that encompasses more than of land and contains more than of historic trails. It is in the northern Nevada section of the Great Basin with a lakebed that is a dry remnant of Pleistocene Lake Lahontan. The Great Basin, named for the geography in which water is unable to flow out and remains in the basin, is a rugged land serrated by hundreds of mountain ranges, dried by wind and sun, with spectacular skies and scenic landscapes. The average annual precipitation ''(years 1971-2000)'' at Gerlach, Nevada (extreme south-west of the desert) is . The region is notable for its paleogeologic features, as an area of 19th-century Emigrant Trails to California, as a venue for rocketry, and as an alternative to the ...
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California Trail
The California Trail was an emigrant trail of about across the western half of the North American continent from Missouri River towns to what is now the state of California. After it was established, the first half of the California Trail followed the same corridor of networked river valley trails as the Oregon Trail and the Mormon Trail, namely the valleys of the Platte, North Platte, and Sweetwater rivers to Wyoming. The trail has several splits and cutoffs for alternative routes around major landforms and to different destinations, with a combined length of over . Introduction By 1847, two former fur trading frontier forts marked trailheads for major alternative routes through Utah and Wyoming to Northern California. The first was Jim Bridger's Fort Bridger (est. 1842) in present-day Wyoming on the Green River, where the Mormon Trail turned southwest over the Wasatch Range to the newly established Salt Lake City, Utah. From Salt Lake the Salt Lake Cutoff (est. 1848) ...
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California Gold Rush
The California Gold Rush (1848–1855) was a gold rush that began on January 24, 1848, when gold was found by James W. Marshall at Sutter's Mill in Coloma, California. The news of gold brought approximately 300,000 people to California from the rest of the United States and abroad. The sudden influx of gold into the money supply reinvigorated the American economy; the sudden population increase allowed California to go rapidly to statehood, in the Compromise of 1850. The Gold Rush had severe effects on Native Californians and accelerated the Native American population's decline from disease, starvation and the California genocide. The effects of the Gold Rush were substantial. Whole indigenous societies were attacked and pushed off their lands by the gold-seekers, called "forty-niners" (referring to 1849, the peak year for Gold Rush immigration). Outside of California, the first to arrive were from Oregon, the Sandwich Islands (Hawaii) and Latin America in late 1848. Of th ...
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