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Trinity River (California)

The Trinity River is a major river in northwestern California in the United States and is the principal tributary of the Klamath River. The Trinity flows for 165 miles (266 km) through the Klamath Mountains and Coast Ranges, with a watershed area of nearly 3,000 square miles (7,800 km2) in Trinity and Humboldt Counties. Designated a National Wild and Scenic River, along most of its course the Trinity flows swiftly through tight canyons and mountain meadows.

Course
. The silty South Fork joins the river from below. The Trinity River begins deep in the Scott Mountains, in Trinity County, at the confluence of High Camp Creek and Chilcoot Creek. Streamflow The United States Geological Survey (USGS) operates eight real-time stream gages on the Trinity River. The lowermost gage, located at Hoopa, measures runoff from , or 97 percent of the Trinity River watershed. The annual discharge, averaged over the 1964–2013 period, was . The average discharge between 1912–1960, prior to construction of Trinity and Lewiston Dams, was . The other USGS gages are located at Coffee Creek (above Trinity Lake), below Lewiston Dam, above and below Douglas City, at Junction City, at Helena, and at Burnt Ranch. ==Watershed==
Watershed
The Trinity River's watershed drains a rugged, forested region of California's North Coast. The highest point in the watershed is Sawtooth Peak in the Trinity Alps; the elevation is where the Trinity meets the Klamath River in the town of Salyer. The watershed is almost entirely covered by mountains, with the only level land in a few narrow valleys: the Weaverville basin, and the Hoopa, Hyampom and Hayfork Valleys. The Hayfork Valley is the largest agricultural area in Trinity County, with about of farmland. About 80 percent of the Trinity River watershed is federal land managed by the U.S. Forest Service and the U.S. Bureau of Land Management. The remaining 20 percent are privately owned; about half are owned by logging companies. The overall climate is Mediterranean, with cool, wet winters and hot, dry summers. Annual precipitation over the Trinity River watershed averages . Precipitation ranges from in lowlands around Weaverville and Hayfork, to as high as in some mountain ranges close to the coast. The high rainfall combined with the rugged geography results in extremely fast runoff and a high risk of flooding during winter storms. Large volumes of rocks and sediment carried by floods are spread along the rivers forming wide alluvial channels. In general, human activities such as mining and road construction have increased the rate of erosion within the watershed and consequentially the amount of sediment carried into the rivers. Dam building has had the opposite effect, by blocking natural sediment sources to a long section of the Trinity River. Both have had notable impacts on river geomorphology, altering the development of riparian zones and fish habitat. The Trinity River watershed borders several major California drainage basins; these are the Mad River and Redwood Creek to the west, the Salmon River and Scott River (tributaries of the Klamath River) to the north, and Clear Creek and Cottonwood Creek (both tributaries of the Sacramento River) to the east and south, respectively. Fir, oak, and pine forests cover about 92 percent of the watershed. Chaparral and shrubs account for slightly over 5 percent, and grassland and barren land each cover approximately 1 percent. Riparian zones and wetlands encompass 0.5 percent of the watershed. Less than 2 percent of the watershed is urbanized. About 86 percent of the Trinity River watershed is in Trinity County. As of the 2010 census, the population of Trinity County was 13,786. With a population density of 4.3 people per square mile (1.7/km2) it is one of the least densely populated counties in California. Only , or about 14 percent of the western part of the basin, is in Humboldt County.{{cite web ==Geology==
Geology
The lands that make up the Trinity River basin today began to take shape over 200 million years ago by the collision of several exotic terranes – or crustal fragments of the Pacific Plate – with the North American Plate, causing uplift of the sea floor under what is now northwestern California. During the Jurassic and Cretaceous periods, tectonic movement along the plate boundary produced a range of mountains much higher than those found in the area today. Over millions of years these mountains were eroded, then reformed again as the next oceanic terrane collided with the continental crust. This repeating cycle of erosion and orogeny created the complex "jumble of different rock types" that characterizes the region today.{{cite web|url=https://pubs.usgs.gov/sim/3119/ The Klamath Mountains, which make up the eastern part of the watershed are quite young in geologic terms, no more than 2 or 3 million years old.{{cite web The Coast Ranges pass through the western part of the Trinity River Basin and consist of even younger rock formations, chiefly the Franciscan Assemblage.{{cite book The most common type of rock is greywacke, followed by other types of sandstones and shales. Landslides and mass wasting are common in this region due to erosion as well as earthquakes. ==History==
History
Native Americans An archaeological site on the Trinity River at Cox Bar, with spear points dating from 3000–6000 BC, has some of the oldest evidence of human habitation in Northern California. This site is believed to be part of the early Borax Lake Pattern culture. Natinixwe is an endonym meaning "people of the place where the trails return". Their name for the Trinity River was hun' simply meaning "river". The name "Hupa" or "Hoopa" appears to originate from the Yurok word for the Trinity River country, hopah, which was first recorded by ethnologist George Gibbs in 1852. The Hupa lived in the fertile Hoopa Valley along the Trinity River and the Hyampom Valley on the South Fork – some of the few flat lands in a region otherwise dominated by rugged mountains. A Yurok village called Weitspus stood at the site of present-day Weitchpec at the confluence of the Trinity and Klamath Rivers. The Hupa traded with the coastal Yurok and Karok by using canoes to navigate the Trinity and Klamath Rivers. The trade arrangements with neighboring tribes were complex and involved the use of dentalium shells as currency. The Tsnungwe people, also known as the South Fork Hupa, lived pre-contact in the South Fork of the Trinity River area and Burnt Ranch/New River area. After the Gold Rush of 1849, many years of battles occurred between the Trinity River Indians and the miners/soldiers. Most surviving Tsnungwe were taken to the Hoopa Valley Indian Reservation. By 1900, a Tsnungwe community had re-established around the ancient principal village of at the mouth of the South Fork of the Trinity River. The tribe is still surviving there today and is recognized by both Humboldt County and Trinity County. The federal government considers the Tsnungwe to be a "previously recognized" tribe. The Tsnungwe Council is working towards having their federally recognized tribal status restored. The Chimariko people lived along the Trinity River canyon near its confluence with the New River. They were enemies of the Hupa, but had friendly relations with the Wintu. The now extinct Chimariko language was of Northern Hokan origin, in contrast to the Athabaskan dialect of the Hupa and the Wintuan languages spoken by the Wintu. Carl Waldman describes in Encyclopedia of Native American Tribes (2014) that "the Chimariko occupied one of the smallest homelands, if not the smallest, of any distinct linguistic group in North America." Native peoples also made meal of berries, seeds and acorns, and hunted game animals such as deer and elk that were drawn to the Trinity River. Due to their proximity to trade routes in and around the Central Valley, the Wintu came into frequent contact with European explorers, traders and settlers. These initial meetings were peaceful, but the Wintu population – along with many other Central Valley tribes – were decimated by a malaria epidemic in the 1830s, accidentally introduced by Hudson's Bay Company fur trappers. In the following decades the remaining Wintu became embroiled in conflict as prospectors and settlers occupied their traditional lands. Some of these conflicts ended in deadly massacres. In 1846, one of the bloodiest single encounters occurred when soldiers led by John C. Frémont killed 175 Wintu, Maidu and Yana. In 1850 about 100 Trinity Wintu perished after being given poisoned food by white settlers. By 1910 the Wintu population had been reduced to about 1,000, from an estimated 12,000 prior to European contact. Explorers Jedediah Smith's expedition to northwestern California in 1828 were some of the first Europeans to set foot in the Trinity River country. After departing from the Sacramento Valley Smith passed over the Klamath Mountains and arrived at what is probably now Hayfork Creek on April 18. They followed the creek to the South Fork and from there to the Trinity River and the Klamath River. After following the Klamath to the Pacific, they traveled north towards Oregon, thus becoming the first white men to travel from inland California to coastal Oregon. Gold Rush In July 1848, not too long after James Marshall's famous gold find at Sutter's Mill – which started the California Gold Rush – Major Reading discovered gold on the Trinity River. The find attracted thousands of miners to the area and created boomtowns such as Douglas City, Francis, Hoboken, Lake City, Lewiston, Junction City and Quimby. Weaverville, located at the end of the trail Reading had established from the Sacramento Valley to the Trinity, prospered as the main trade center through which gold was exchanged for imported supplies and services. The initial discoveries were placer deposits, carried by the river to settle in gravel bars. The Trinity River gold rush is also noted for the large number of Chinese miners attracted to the area, as many as 2,500 by 1854. Many of the Chinese were from the Pearl River Delta (Guangdong region). Mining activity was initially concentrated in the eastern (upper) valleys of the Trinity River around Weaverville, as the hostile Native Americans and treacherous gorges around Burnt Ranch precluded the transport of rations and equipment to places further west. For about two decades the area was extremely productive, second only to the Sierra Nevada (the Mother Lode) itself. The rate at which gold was extracted, and new methods pioneered to access the harder to reach deposits, was feverish. The area was soon profiting $1.5 million a year, with hundreds of claims along the Trinity River equipped with flumes, waterwheels and other apparatus to separate fine gold from river gravel. spurring prospectors to push west, establishing a pack trail to the area around the New River and the South Fork of the Trinity. In fact, the New River was named thusly for being a "new" river to explore for gold. Post-Gold Rush settlement In 1884 the California legislature banned hydraulic mining as the flow of tailings from hydraulic mines in the Sierra Nevada was silting up the Sacramento River, making it unnavigable. However, the Trinity hydraulic mines escaped this ban, as the remote and swift flowing Trinity River was not considered a navigable watercourse. Nevertheless, the largest deposits had been played out by the 1920s, and the mining settlements were abandoned or fell into decline. This brought on the last stage of commercial gold mining along the Trinity, as floating dredges (called "doodle-bugs" by the miners) were used to turn over the river bottoms that had been inaccessible by the placer miners a half-century earlier. One Mr. Jorstad who had been mining in the Trinity River country since the 1930s, continued to live in a small cabin at Pfeiffer Flat on the North Fork until his death in 1989. Although settlers had been farming and ranching in the Trinity River valley since the beginning of the gold rush, the number greatly increased after the gold rush when miners decided to settle down and homestead in the area. One of the major ranching areas was the wide valley known as Trinity Meadows, which is now flooded by Trinity Lake. In 1988 several environmentalist groups including the Wilderness Society, Audubon Society and Sierra Club filed a lawsuit against the Forest Service, preventing the cutting of 18.4 million board feet of salvage lumber in an area with particularly high erosion risk. This generated pushback in the local timber industry, whose decline has partly been attributed to more stringent environmental regulations. Central Valley Project As early as the 1930s, the state of California had floated the idea of diverting water from the rainy north to support irrigation in the fertile, but dry San Joaquin Valley. A diversion of the Trinity River was contemplated in order to boost the available water supply for the Central Valley watershed, but planners eventually determined that the extra water was not yet needed. The U.S. Bureau of Reclamation took over the Central Valley Project from the bankrupt state of California during the Great Depression in 1933 as a federal public works project, and in 1942 it began investigations to dam the Trinity River. However, the Trinity River plan was dropped in 1945, after the completion of nearby Shasta Dam. As the 1950s began, demand on the Colorado River – which forms the border of California and Arizona and provided most of Southern California's water – was moving toward unsustainable levels. The Bureau of Reclamation restarted its surveys of the Trinity River basin as part of a larger proposal to move water from northern to southern parts of the state, and compensate for the shortages on the Colorado. The United Western Investigation, in 1951, proposed the damming of nearly every river in the North Coast region of California, chiefly the Trinity, Klamath and Eel. The Ah Pah Dam would have flooded the canyons of the Klamath and Trinity Rivers to form the largest reservoir in California. These grandiose plans culminated in the Pacific Southwest Water Plan of 1964, which sought to comprehensively link the water systems of California and the rest of the Colorado River Basin. One of the key projects was an aqueduct to transport North Coast water to the Imperial Valley, reducing its reliance on water from the Colorado River. However, with the exception of the upper Trinity River project, none of these dam and diversion projects were ever realized. The Trinity River project was first drafted on October 1, 1951, and authorized by Congress on January 2, 1953, as the Trinity River Division of the Central Valley Project. In 1955 Congress authorized an annual diversion of of water (56 percent of total flow) from the Trinity River, stating that the water could be exported "without detrimental effect on the fishery resources" of the Trinity. In 1957 the Bureau of Reclamation revised the export volume to . Construction of Trinity Dam started in 1956 and was completed on December 23, 1963. The reservoir was originally named "Clair Engle Lake" to commemorate United States Senator Clair Engle, who played a crucial role in shepherding the Trinity bill through Congress; however, the name proved unpopular with locals, and it was changed to Trinity Lake in 1997. Trinity Dam, an earth embankment structure high, was the tallest embankment dam in the world at its completion in 1962 (it was surpassed by Oroville Dam, also in California, in 1968). Other residents welcomed the dam project for the economic benefits it would bring via hydropower and tourism, as the gold mining industry that had long supported the region was greatly diminished by the 1950s. By 1986 tourism in the Trinity River country accounted for 50–75 percent of business in the summer and 25 percent in the winter. ==Ecology==
Ecology
With the exception of rocky alpine regions in the highest mountains, the Trinity River watershed is almost entirely forested. Mixed coniferous (fir and pine) forests dominate the landscape at elevations of up to . Common tree species include ponderosa pine, Jeffrey pine, Douglas fir, white fir, red fir, sugar pine, knobcone pine and incense cedar. The watershed also includes some hardwood forests, typically located along canyon bottoms and streams, which are home to California black oak (Quercus kelloggii), madrone, tanbark oak, canyon live oak and bigleaf maple. Oregon white oak is widespread throughout lower elevations. Large mammals found in the national forest include black bear, mountain lion, bobcat, coyote, gray fox, Columbian black-tailed deer (mule deer), and elk. River otters inhabit most streams. Other mammals include ringtails, raccoons, skunks, jackrabbits, martens and many squirrel and rat species including northern flying squirrel. Several species of bats are also found in the watershed, little brown bats being the most common. The area around Trinity Lake has a significant nesting bald eagle population. The Trinity River was once known for its prolific anadromous fish (salmon, steelhead and sturgeon) runs. The actual number of fish returning to the river each year to spawn, prior to European settlement, is uncertain due to the lack of records. During the first half of the 20th century, before damming, the fall chinook salmon run was estimated at anywhere between 19,000 and 75,500. Forest and river habitats in the watershed have been heavily affected by human activities ever since Gold Rush mining began in the 1800s. Commercial logging has caused mountain slopes to become more prone to erosion; even in areas that are no longer logged and have seen secondary forest growth, abandoned logging roads pose a serious erosive threat. Grazing of livestock has also degraded grasslands and exposed soils to runoff. This has resulted in river channels becoming clogged and confined by sediment, harming salmon and steelhead populations by burying gravel bars used by these fish for spawning. Along the South Fork, this problem has been exacerbated by the inherently unstable rocks and soils of the Franciscan formation, causing mass wasting events that dump sediment into streams. After the Trinity and Lewiston Dams were complete, the Bureau of Reclamation did not adhere to the water export limits set in the project's authorization, diverting 72 percent of the total river flow In 2002, 65,000 adult salmon perished in a fish kill on the lower Trinity and Klamath rivers (the fish were mostly of Trinity stock). which contains soils laced with salt and selenium. After the completion of Lewiston Dam in 1963, the Bureau of Reclamation constructed the Trinity River Fish Hatchery to raise young steelhead, coho and chinook salmon. The primary purpose of the hatchery was to compensate for the loss of of anadromous fish habitat above Lewiston Dam. The hatchery is operated by the California Department of Fish and Wildlife to produce returns of 7,500 coho, 6,000 spring chinook, 70,000 fall chinook and 22,000 steelhead each year. In 2014, the California Fish Hatchery Review Project found that Trinity Hatchery raised coho were out-competing wild stocks. The hatchery has since been required to carefully time releases of young fish in order to reduce the risk of competition. The deaths of a dog in 2021 after going swimming occurred due to cyanobacteria in blue-green algae on the river, east of Willow Creek. Algae blooms can occur during times of warm weather and low water flow. Restoration efforts After an environmental impact statement in 1991 the Bureau of Reclamation was required to make greater releases to the Trinity River below Lewiston Dam. On December 19, 2000, the Department of the Interior signed a Record of Decision (ROD) officially re-allocating Central Valley Project water for environmental purposes. This modified flow regime officially began in water year 2005. Prior to this, annual releases to the Trinity River ranged from , or about each year, with the exception of occasional flood water discharges. The ROD increases the minimum dam release to or about , even in "critically dry" years, with even greater releases made during years of normal and above average precipitation. These restrictions would reduce the Trinity River diversions about 28 percent on average; however, the impacts on the Central Valley Project as a whole would be far less, only about 1–4 percent. In addition, the project will periodically release high flows up to to simulate historic flooding and sediment transport conditions. In 2015 Humboldt County won a lawsuit against the Westlands Water District for an extra of water from the Trinity River for in-stream flows. Previously, the Bureau of Reclamation had included this sum in the water released for fishery management. Although this means more water for the Trinity River, no provision was made for commensurately reducing Central Valley Project water diversions, increasing the risk that Trinity Lake could be drained to "dead pool" in drought years. The California Water Impact Network stated channel rehabilitation was "an activity equivalent to a clear-cut on a Wild and Scenic River." Bulldozing of the riverbanks to clear space for juvenile salmon habitat has harmed steelhead spawning grounds, impacted public access and allowed the spread of invasive plant species. Between 2005 and 2011, restoration work cost a total of $36 million. ==Recreation==
Recreation
on the Trinity River The Trinity River and many of its tributaries have been part of the National Wild and Scenic Rivers System since 1981. The main stem is designated from a point below Lewiston Dam to the confluence with the Klamath River. The North Fork and New River are designated from the boundary of the Trinity Alps Wilderness to the mouth, and the South Fork from State Route 36 to the mouth. A total of are classified as "wild", as "scenic" and as "recreational". The South Fork is the largest river in California without a single dam along its length. Although fish populations have declined since the early 1900s, fishing for salmon and steelhead has recovered on many parts of the river. The Trinity is known as one of the best steelhead streams in the western United States and is home to both wild and hatchery fish. The California Office of Environmental Health Hazard Assessment (OEHHA) has developed a safe eating advisory for fish caught in the Trinity River based on levels of mercury or PCBs found in local species. The Trinity is a popular whitewater rafting and kayaking river. Dam releases for fish restoration have incidentally increased the amount of water available for boating year-round. The river has three main whitewater runs, all known for their scenery and wildlife. The Pigeon Point section, alongside Highway 299, contains Class II-III (beginner to intermediate) rapids. Below the takeout at Cedar Flat, the Trinity flows through the extremely hazardous Class V Burnt Ranch Gorge, which was first run in 1971 by three kayakers, one of whom died of a heart attack soon after finishing the run, due to the arduous work of portaging many rapids. This gave the area a bad reputation for many years; it was not until 1983 that commercial trips began on this section of the river. The lower Trinity, much of which flows through the Hoopa Valley Reservation, is a Class II river with gentler and lower gradient despite having a greater volume of water flow. Recreational gold panning is another pastime along the Trinity. However, many streams in the area are located on private property, or are part of existing placer mining claims. Claims in the area are administered by the Bureau of Land Management (BLM). ==See also==
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