94-882: Trinity River may refer to: Trinity River (California) Trinity River (Texas) Trinity River Audubon Center in Texas Trinity River Authority in Texas Trinity River National Wildlife Refuge in Texas Trinity River Project in Texas Trinity River Vision Project in Texas Topics referred to by the same term [REDACTED] This disambiguation page lists articles associated with
188-643: A Tsnungwe community had re-established around the ancient principal village of łe:lding 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
282-486: A historical site maintained by the Forest Service. 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. The Webber family bought
376-517: 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
470-776: A ranch along the Stuart Fork in 1922 and established a resort. Having traveled in Europe, the Webbers thought the area resembled the Austrian Alps, and so named the mountains along the upper Trinity River the "Trinity Alps". During the 1870s, the Southern Pacific Railroad was extended from Sacramento through Redding and would eventually reach Oregon, making travel to the area easier than ever before. Commercial logging had also been operating for years in
564-490: A reduced scale, finally ending in 1959, when the last claim was bought by the federal government in preparation for dam construction of the Central Valley Project . Although most of the miners left, either to return home or settle elsewhere, some stayed to work in the ranching and logging industries that became the economic mainstay of the Trinity River area. Some also continued to search for gold long after
658-626: A reservation here in 1876. They are the only Native American group in California to retain most of their original territory; today, the Hoopa Valley Reservation is the largest and most populous in the state. 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
752-610: 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. Trinity Lake Trinity Lake , previously called Clair Engle Lake ,
846-470: A small creek that flows into the Trinity, was the biggest hydraulic mine in California, covering over 3,000 acres (1,200 ha). Tailings washed from this single mine buried the valley, the creek and the entire town of Oregon Gulch (which had been purchased by the mine owners in anticipation of this) under a staggering 110 million cubic yards (84,000,000 m ) of sediment. This is equal to thirty times
940-600: Is a reservoir on the Trinity River formed by the Trinity Dam and located in Trinity County, California , United States. The dam was built by the U.S. Bureau of Reclamation . The lake's capacity is 2,447,650 acre⋅ft (3,019.13 GL ), making it one of the largest reservoirs in California . The lake's surface is at 2,370 ft (720 m) above MSL. Trinity Lake captures and stores water for
1034-645: 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 km ) in Trinity and Humboldt Counties. Designated a National Wild and Scenic River , along most of its course
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#17327657967991128-546: 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
1222-464: The Central Valley Project , which provides the Central Valley with water for irrigation and produces hydroelectric power. This lake is known for its many small arms, glassy inlets, and good water-skiing conditions. After the death in office of California United States Senator Clair Engle in 1964, the lake was renamed after him. The name change never received wide popularity and the name
1316-549: 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
1410-589: 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
1504-589: The Yurok and Hupa (Hoopa). Both tribes have reservation lands in the area. Trinity Lake is less used by vacationers than the lower Lake Shasta due in part to the lengthy winding road up from the valley floor. Typical drive time from Redding (Interstate 5) to the lake is about 90 minutes along a winding mountain road. This makes it a destination spot for fishing and water sports. Popular fishing includes that of smallmouth and largemouth bass , catfish , kokanee , rainbow and brown trout . Fish remain ample, despite
1598-541: The 1800s. These have declined in part due to increasing environmental regulations. Tourism has been an increasingly important part of the economy especially after the creation of the Trinity Lake reservoir in 1964. 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
1692-407: 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. After World War II commercial dredges continued to operate on the Trinity, but at
1786-520: The 1980s. Many logged areas were on steep mountains, and improper construction of roads and skid trails exposed slopes to erosion and landslides. 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
1880-559: The 20th century, before damming, the fall chinook salmon run was estimated at anywhere between 19,000 and 75,500. The spring chinook and coho salmon runs were about 10,000 each and the annual steelhead run was about 50,000. 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
1974-500: The Central Valley Project came to fruition in 1961 with the completion of Trinity Dam. The lake was renamed Clair Engle Lake from 1964 to 1997. It was eventually renamed Trinity Lake. The lake was completely filled with water from the Trinity River by 1963 and is the third largest lake in California with 145 miles (233 km) of shoreline. The area is the ancestral lands of several Native American tribes, most notably
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#17327657967992068-620: 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
2162-399: The Franciscan assemblage as a "nightmare of rocks" due to its complex and fragmented layers. 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. An archaeological site on the Trinity River at Cox Bar, with spear points dating from 3000–6000 BC, has some of
2256-780: The Gold Rush mining town of Weaverville . The Alpine scenery surrounding the lake makes up the Trinity Alps. The Alps were formed in the late Jurassic Period by volcanic activity in the form of ultramafic and granitic plutons (igneous rock formed from super-heated magma cooling under the surface of the earth), and tectonic activity (the super continent of Pangaea was beginning to pull apart into two separate super-sized continents) and glaciation during frigid climate periods known as ice ages (land surface modified by action of glaciers). The last remaining glaciers are on Thompson’s peak, at more than 9,000 feet (2,700 m). The lake bed
2350-555: The Hayfork Wintu as norelmaq ("south-uphill people"). Many Wintu villages were located along the Trinity River, and were home to up to 150 people. Each village operated as an independent unit led by a chief, although the villagers interacted frequently through trade with each other as well as neighboring tribes, such as the Nomlaki , Achomawi and Shasta . Since about 1000 A.D. the lower Trinity River has been inhabited by
2444-704: 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. Smith and his party traded with the Hupas and Yuroks in
2538-532: The Natinixwe, now known as the Hupa people. 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
2632-413: The Trinity Alps – the highest range in northwest California – were also sculpted by glaciation during successive Ice Ages, the last of which ended roughly 10,000 years ago. Glacial erosion produced numerous granite outcroppings, tarns , cirques and knife-edged ridges. Remnants of these glaciers, or "glacierets", are still extant in the higher valleys. The Coast Ranges pass through the western part of
2726-758: The Trinity Mountains to the Whiskeytown Lake reservoir, and from there it flows 2.4 miles (3.9 km) through the Spring Creek Tunnel to join the Sacramento River at Keswick Dam . Along the way the water drops some 1,500 feet (460 m) through three hydroelectric plants, generating nearly one billion kilowatt hours each year. Water flow data for the Judge Francis Carr hydroelectric station located at
2820-641: The Trinity River Basin and consist of even younger rock formations, chiefly the Franciscan Assemblage . The Franciscan formation consists of more unstable sedimentary and igneous rocks and soils that are highly breakable and prone to erosion. They formed even more recently in geologic history than the Klamath Mountains, primarily due to uplift along the Cascadia subduction zone . The Natural Resources Conservation Service refers to
2914-598: The Trinity River Division of the Central Valley Project. In 1955 Congress authorized an annual diversion of 704,000 acre-feet (0.868 km ) 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 865,000 acre-feet (1.067 km ). Construction of Trinity Dam started in 1956 and
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3008-519: 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
3102-506: The Trinity River area. Their traditional lands included much of the upper (eastern) Trinity River in the present day area of Shasta-Trinity National Forest . There were nine major groups of Wintu spread across the Trinity, Upper Sacramento, and McCloud River valleys as well as parts of the South Fork Trinity River and its tributary Hayfork Creek . The Trinity River Wintu were known as nomsu's ("those being west"), and
3196-807: 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
3290-409: The Trinity River country, but most of the timber produced was used locally. After World War II , logging greatly increased both due to high demand for housing domestically and abroad, and the introduction of more advanced technologies. In 1959 alone, loggers took 439 million board feet from Trinity County. The rate dropped after that, but logging continued at 200–300 million board feet per year well into
3384-524: The Trinity River each year. 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
3478-521: The Trinity River passes the towns of Lewiston and receives another large tributary named Grass Valley Creek, before passing Douglas City and turns west, passing within a few miles of Weaverville , the seat of Trinity County and the main population center of the area. It then turns northwest and receives Browns Creek, passes Junction City , and receives Canyon Creek and the North Fork Trinity River at Helena . Further west it passes
3572-506: The Trinity River turns sharply north, entering Humboldt County . It flows through the wider steep-sided namesake valley of the Hoopa Valley Reservation , past the towns of Willow Creek and Hoopa . It joins the Klamath River at Weitchpec , 44 miles (71 km) above the mouth of the larger river on the Pacific Ocean . The confluence marks the point where the Klamath turns from its generally southwesterly course to flow north towards
3666-467: The Trinity River valley were heavily opposed to the dam, but they had no recourse against eminent domain used by the federal government (although property owners were paid for their land). Many buildings in Trinity Center were moved to a new location on the western shore of the reservoir. The dam blocked salmon runs to 109 miles (175 km) of habitat in the upper Trinity River basin, destroying
3760-563: 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 57 inches (1,400 mm). Precipitation ranges from 37 inches (940 mm) in lowlands around Weaverville and Hayfork, to as high as 85 inches (2,200 mm) in some mountain ranges close to
3854-438: The Trinity River. The lowermost gage, located at Hoopa, measures runoff from 2,853 square miles (7,390 km ), or 97 percent of the Trinity River watershed. The annual discharge , averaged over the 1964–2013 period, was 4,849 cubic feet per second (137.3 m /s). The average discharge between 1912–1960, prior to construction of Trinity and Lewiston Dams, was 5,618 cubic feet per second (159.1 m /s). The maximum flow
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3948-431: The Trinity flows swiftly through tight canyons and mountain meadows. The river is known for its once prolific runs of anadromous fish , notably Chinook salmon and steelhead , which sustained Native American tribes for thousands of years. Due to its remoteness, the Trinity did not feature prominently in the early European colonization of California, but the gold rush in the mid-1800s brought thousands of gold seekers to
4042-597: The West. Cedar Creek is the next major tributary that meets from the East. The river continues to flow in a Southwestern direction picking up numerous tributaries before entering Trinity Lake , a large reservoir created by the Trinity Dam . These tributaries include Picayunne Creek, Nyott Creek, and Sherer Creek, Sunflower Creek, and more. Coffee Creek, the Little Trinity River, Tangle Blue Creek, and Eagle Creek are
4136-461: The Wintu population had been reduced to about 1,000, from an estimated 12,000 prior to European contact. The Chimariko also suffered heavily when European prospectors entered the region in the 19th century searching for gold. After clashing with the Europeans, many members of the tribe were dispersed to Shasta territory or killed. Some returned to the Trinity River in the late 19th century, after
4230-471: 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
4324-502: The area and their encounters were generally friendly. Early maps of the area label the South Fork, the lower Trinity and the lower Klamath as "Smith's River". The name was later applied to the Smith River further north, which Smith also crossed on the same expedition. Harrison Rogers, a member of Smith's party, called the Trinity "Indian Scalp River" although the reason for this name is unknown. The Old Trinity Trail, which crosses
4418-483: The area. The river was named by Major Pierson B. Reading who, upon reaching the river in 1848, mistakenly believed it to flow into the Pacific Ocean at Trinidad Bay . During and after the gold rush, the influx of settlers and miners into the Trinity River country led to conflict with indigenous tribes, many of which saw severe depopulation due to fighting and foreign diseases. In the following decades logging and ranching, combined with mining runoff, significantly changed
4512-410: The beaver furs he can from them", suggesting that beaver were then plentiful on the Trinity or at least in the surrounding area. 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
4606-407: 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
4700-455: The complex "jumble of different rock types" that characterizes the region today. Rocks commonly found in the Trinity River area include gabbro , chert , granite , diorite , limestone , sandstone , serpentine , schist and marble . Gold -bearing quartz veins are widespread in local metamorphic rock formations; the richness of the area made it among the focal points of the California Gold Rush . The Klamath Mountains, which make up
4794-568: The confluence of High Camp Creek and Chilcoot Creek. It flows south through a deep valley between the Trinity Mountains to the east as well as the Salmon Mountains / Trinity Alps and Scott Mountains to the west. The river picks up its first large tributary called Bear Creek near a series of large spring filled meadows roughly one mile from the headwaters. The short but steep Bull Creek comes in just shortly down stream from
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#17327657967994888-528: The dam and contributed to a crest fully 20 feet (6.1 m) higher than the second highest peak, recorded in December 1955. 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 . The Trinity River's 2,936-square-mile (7,600 km ) watershed drains a rugged, forested region of California's North Coast . The highest point in
4982-547: 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
5076-530: 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
5170-438: The eastern part of the watershed are quite young in geologic terms, no more than 2 or 3 million years old. The present shape of the mountains was highly influenced by underground volcanic activity, which created batholiths , domes of igneous rock formed by cooled magma. They raised the elevation of the terrain above and created the widespread granite and diorite formations found in the area today. The higher mountains, including
5264-399: The end of Trinity Tunnel indicates an annual average of 1,257 cubic feet per second (35.6 m /s), or 910,700 acre-feet (1.1233 km ), diverted from the river between 1963 and 2013. The filling of the reservoir flooded the town of Trinity Center, one of the original main population centers of Trinity County, as well as the smaller communities of Stringtown and Minersville. Residents of
5358-477: 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
5452-409: The fishing economy that had sustained local people for generations. 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
5546-580: The former mining settlement of Big Bar and receives Price Creek. It then enters a deep gorge, which provides the route for Highway 299 , the principal road connecting Redding to the Humboldt Bay area. At Burnt Ranch it receives the New River from the north. At Salyer the South Fork , its main tributary, enters from the south, nearly doubling the flow. At the confluence of the South Fork,
5640-455: The gold seekers had left. People of Chimariko ancestry continue to live in the region, although the tribe functionally no longer exists. Because of the geographic isolation of their homeland, the Hupa had few interactions with early European explorers, although they later came in conflict with miners looking for gold. Even after California became a US state in 1850, the Hupa continued to live on their traditional lands and were eventually granted
5734-433: The harder to reach deposits, was feverish. Author James Hilton remarked that Weaverville was a "Shangri-La, that strange and wonderful somewhere which is not a place but a state of mind." 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. The Great Flood of 1862 largely obliterated
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#17327657967995828-500: The lake, visitors enjoy hiking and camping in the pristine wilderness of the Trinity Alps and the Shasta-Trinity National Forest. There has been a dramatic decline in various fish species in the river since the dams were built and the lake created. Spawning steelhead , Chinook and Coho Salmon populations have all been affected by their loss of spawning ground. However, wildlife populations surrounding
5922-507: The largest tributaries above the lake. East Fork and Stuart Fork of the Trinity River also flow into the reservoir along with many other tributaries. Just below Trinity Dam is the smaller Lewiston Dam , which diverts part of the Trinity River through a hydroelectric plant to the Sacramento River Basin as part of the Central Valley Project , providing irrigation water to California's Central Valley . Below Lewiston Dam
6016-514: The local timber industry, whose decline has partly been attributed to more stringent environmental regulations. 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
6110-488: The major deposits were gone; even today, recreational gold panning remains a popular activity along the Trinity. 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. Jorstad's cabin was an important rest stop for miners, hunters, hikers and fishermen along the North Fork for many years; it remains as
6204-460: The mountains between Redding and Weaverville (approximately where State Route 299 is today) was used by Native Americans for generations before Europeans came to the area. Hudson's Bay Company fur trappers may have used this route in search of beaver as early as the 1830s and 1840s; trapping was common in the area until about 1845. The trail pioneered by Smith was also used by fur trappers, including mountain man Ewing Young in 1832. Today part of
6298-587: The negative impact that the dams have had on spawning ground in part due to the Trinity River Fish Hatchery, located just below Lewiston Dam . The California Office of Environmental Health Hazard Assessment (OEHHA) has developed a safe eating advisory for fish caught in Trinity Lake based on levels of mercury or PCBs found in local species. House boating, speed boating, and waterskiing are also popular lake activities. Surrounding
6392-664: The occasional high elevation thunderstorm. The Shasta-Trinity National Forest encompasses nearly the entire Trinity River watershed with the exception of private inholdings and the small area in Humboldt County. 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
6486-406: The oldest evidence of human habitation in Northern California. This site is believed to be part of the early Borax Lake Pattern culture. Archaeological evidence in the Whiskeytown area also indicates human presence as early as 5000 BC, although it is uncertain at what point the ancestors of modern Native American tribes arrived here. The Wintu people are the first recorded indigenous group in
6580-441: The placer mining claims along this part of the Trinity River, 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. Although the river gold petered out by the 1870s, lode gold was discovered in the 1880s in the mountains above the Trinity River country. Because hard rock mining
6674-509: The primary source of flow is snowmelt from the higher elevations of the Klamath Mountains and groundwater base flow . In addition, diversion of water to the Central Valley has greatly reduced the total flow of the river since the 1960s, though conversely, a required minimum dam release for protection of migrating salmon results in a flow rate during the dry season that is higher than it naturally would be. The United States Geological Survey (USGS) operates eight real-time stream gages on
6768-423: The river's ecology and led to the decline of its fish populations. The Trinity River is an important water source for irrigation and hydroelectricity generation, as well as a major center of recreational activities such as gold panning , fishing and whitewater rafting . Since 1964 the Trinity River has been dammed to create Trinity Lake , the third largest man-made lake in the state. As much as 90 percent of
6862-415: The sea. As the crow flies , Weitchpec is situated about 30 miles (48 km) northeast of Eureka . The Trinity River is a predominantly rain-fed river, with the highest flows occurring between December and April and the lowest from August through October. The water level can rise quickly in the winter when large Pacific storms strike California's north coast. Almost no precipitation occurs in summer, when
6956-505: The smallest homelands, if not the smallest, of any distinct linguistic group in North America." The abundant salmon, steelhead and sturgeon runs in the Trinity River were central to the lives of indigenous peoples along the entire length of the river. Fishing provided their primary sustenance as well as goods for trade. Prior to the arrival of Europeans, native peoples took as much as 2,000,000 pounds (910,000 kg) of salmon from
7050-573: The title Trinity River . If an internal link led you here, you may wish to change the link to point directly to the intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Trinity_River&oldid=779712492 " Categories : Disambiguation pages Place name disambiguation pages Hidden categories: Short description is different from Wikidata All article disambiguation pages All disambiguation pages Trinity River (California) The Trinity River ( Yurok : Hoopa or Hupa; Hupa : hun')
7144-668: The trail also forms the route of California State Route 36 . Major Pierson B. Reading (for whom the present city of Redding is named) explored the upper Trinity area in 1845 and is credited with the modern name of the river. Reading mistakenly thought that the Trinity flowed west to empty into the Pacific Ocean at Trinidad Bay . In 1849 prospectors confirmed the actual path of the river to flow into what, twenty years earlier had been called "Smith's River"; however, Reading's name stuck. In July 1848, not too long after James Marshall's famous gold find at Sutter's Mill – which started
7238-466: The upper Trinity River watershed was diverted for agriculture in the Central Valley . In 1991 environmental regulations were enacted, requiring a greater release of water to the Trinity River in order to protect fish. However, the use of Trinity River water remains a contentious issue, especially in years of drought. The Trinity River begins deep in the Scott Mountains , in Trinity County , at
7332-419: The upper Trinity River; Oregon white oak is widespread throughout lower elevations. Fir forests comprise almost 74 percent of the forests in the Trinity River watershed; pine and hardwoods account for 13 percent each. There are also limited amounts of chaparral , brush and grass/rangeland within the basin. Wildfires are common in the dry summers which receive little to no precipitation, aside from
7426-625: 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,
7520-484: The use of pressurized water to demolish hillsides in search of gold bearing ore. This had an enormous impact on the landscape – leveling forests, carving huge gullies and burying streambeds under dozens of feet of sediment – which still characterizes the area today. Elaborate flume, reservoir and tunnel systems were built to supply the massive quantities of water required by these "hydraulicking" operations. The La Grange Mine which began operating in 1862 on Oregon Gulch,
7614-628: The volume of the Great Pyramid of Giza . 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
7708-683: The watershed is 8,888-foot (2,709 m) Sawtooth Peak in the Trinity Alps; the elevation is 190 feet (58 m) 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 52,000 acres (21,000 ha) of farmland. About 80 percent of
7802-534: The watershed, little brown bats being the most common. The area around Trinity Lake has a significant nesting bald eagle population. Beaver also inhabit the Trinity River watershed although their numbers were much higher before fur trappers came to the area. In 1828, the Jedediah Smith expedition was helped across the Trinity River by the Yurok and camped on the east side of the Trinity River. His clerk, Harrison G. Rogers wrote, "Mr. Smith purchases all
7896-419: 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/km ) it is one of the least densely populated counties in California. Only 415 square miles (1,070 km ), or about 14 percent of
7990-676: 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
8084-504: The western part of the basin, is in Humboldt County. The part of the Trinity River watershed in Humboldt County is also sparsely populated, with the exception of the Hoopa Valley Reservation, which was home to 2,930 people as of 2011. Extractive industries such as mining and logging, and to a limited extent farming and ranching, have been the main economic drivers in the Trinity River basin since European settlement in
8178-824: The winter. Many locals remained "so bitter about the dam that they tore down signs and misdirected tourists" for many years after the dam was built. 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 6,000 feet (1,800 m). 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 . Stands of Port Orford cedar are common along
8272-405: The world at its completion in 1962 (it was surpassed by Oroville Dam , also in California, in 1968). Trinity Lake can store a maximum of 2,447,650 acre-feet (3.01913 km ), or about twice the Trinity River's flow at this point. Below Trinity Dam is the much smaller Lewiston Dam , the actual point at which the water is diverted. The 10.7-mile (17.2 km) Clear Creek Tunnel conveys water under
8366-577: Was 231,000 cubic feet per second (6,500 m /s) on December 22, 1964, during the Christmas flood of 1964 , and the lowest was 162 cubic feet per second (4.6 m /s) on October 4, 1931. The peak flow in 1964 was greatly attenuated by the Trinity Dam which had just started reservoir filling at the time, perhaps by as much as 100,000 cubic feet per second (2,800 m /s). However, the record-breaking rains of that winter swelled tributaries below
8460-418: 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 538 feet (164 m) high, was the tallest embankment dam in
8554-522: 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
8648-453: Was originally a series of deep valleys in the Alps. The discovery of gold in 1848 prompted hundreds of miners to move into the area. In 1958, a plan to divert water from Trinity River to California’s Central Valley led to the construction of Trinity Dam and the creation of Trinity Lake. This project was also designed to provide hydroelectric power to the local area. The Trinity River Division of
8742-406: Was required to access the gold bearing veins, new industries such as iron forges and stamp mills prospered in the region. Another profitable way to access gold was hydraulic mining operations, which sprang up across the Trinity River country starting in the 1860s. At one point, there were 307 hydraulic mines in Trinity County alone, of which 145 were "fully operational", all of which depended on
8836-552: Was returned to the original name. The lake is serviced by three marinas: Trinity Alps Marina located on the southern end in view of the Dam; Cedar Stock marina on the Stuart Fork arm on the west end of the lake; and Trinity Center marina at the northern end of the main arm of the lake. Most of the marinas rent houseboats to vacationers year round. Trinity Lake is located northwest of Redding , off of Highway 299 north-northeast of
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