Tulare Lake | |
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![]() A group of unidentified men and a dog camping at the shores of Tulare Lake | |
Location | San Joaquin Valley Kings County, California |
Coordinates | 36°3′0″N119°47′17″W / 36.05000°N 119.78806°W Coordinates: 36°3′0″N119°47′17″W / 36.05000°N 119.78806°W |
Type | Flat |
Primary inflows | Kaweah River Kern River Kings River Tule River White River |
Primary outflows | Evaporation, historically underground seepage to San Joaquin River, occasional flow to Suisun Bay |
Basin countries | United States |
Max. length | dry bed 130 km (81 mi) |
Surface area | dry bed 1,780 km2 (690 sq mi) |
Average depth | dry |
Surface elevation | 56 m (184 ft) |
Settlements | Hanford, CA Corcoran, CA Alpaugh, CA |
References | U.S. Geological Survey Geographic Names Information System: Tulare Lake |
Tulare Lake ( /tʊˈlɛəri/ ( listen )) (Yokuts: Pah-áh-su, Pah-áh-sē) is a freshwater dry lake with residual wetlands and marshes in the southern San Joaquin Valley, California, United States. Tulare Lake was once the largest freshwater lake west of the Mississippi River, and the second-largest freshwater lake entirely in the United States based upon surface area. For thousands of years, from the Paleolithic onwards, Tulare Lake was a uniquely rich area which supported perhaps the largest population of Native Americans north of Mexico. [1] Tulare Lake dried up after its tributary rivers were diverted for agricultural irrigation and municipal water uses.
The Spanish word tulare refers to a field of tule rush. Spanish captain Pedro Fages led the first excursions to the southern San Joaquin Valley in 1773.
This plain will exceed one hundred and twenty leagues in length and in parts is twenty, fifteen and even less in width. It is all a labyrinth of lakes and tulares, and the river San Francisco, divided into several branches, winding in the middle of the plain, now enters and now flows out of the lakes, until very near to the place where it enters into the estuary of the river.
Tulare ultimately derives from Classical Nahuatl tōllin, "sedge" or "reeds". [2] [3] The name is thus cognate with various Mesoamerican sites, such as Tula and Tultepec.
Before 600,000 years ago, Lake Corcoran covered the Central Valley of California. 600,000 years ago a new outlet formed in the present day San Francisco Bay, rapidly carving an outlet through Carquinez Strait, probably catastrophically, and drained the lake, leaving the Buena Vista, Kern Lake and Tulare Lakes as remnants. The lake was part of a 13,670-square-mile (35,400 km2) partially endorheic basin, at the south end of the San Joaquin Valley, where it received water from the Kern, Tule, and Kaweah Rivers, as well as from southern distributaries of the Kings. It was separated from the rest of the San Joaquin Valley by tectonic subsidence and alluvial fans extending out from Los Gatos Creek in the Coast Ranges and the Kings River in the Sierra Nevada. Above a threshold elevation of 207 to 210 feet, it overflowed into the San Joaquin River. This happened in 19 of 29 years from 1850 to 1878. No overflows occurred after 1878 due to increasing diversions of tributary waters for agricultural irrigation and municipal water uses, and by 1899, the lake was dry except for residual wetlands and occasional floods. [4]
Tulare Lake was the largest of several similar lakes in its lower basin. Most of the Kern River's flow first went into Kern Lake and Buena Vista Lake via the Kern River and Kern River Slough southwest and south of the site of Bakersfield. If they overflowed, it was through the Kern River channel northwest through tule marshland and Goose Lake, into Tulare Lake.
During times of high water, the ridge of high ground separating the upper Chintache basin from the lower Tontache basin became an archipelago in the southern portion of the lake. During times of low water, this ridge created two separate lakes. Today, these former islands make up the Sand Ridge in Kings County. [1]
The largest of these islands, Atwell's Island, was originally known Hog-Root Island or Root Island. It was owned by Allen J. Atwell of Visalia, California, who introduced hogs onto the island. In early historical times, it was the site of the Wowol village, Chawlowin. Today the city of Alpaugh, California, sits on the remnants of Atwell's Island. Atwell Island was the largest of the Tulare Lake archipelago and has the latest recorded habitation by indigenous peoples. A Bird Island is attested in a 1876 map at the tip of Atwell Island's 'teardrop' shape which shows a small, oblate island. [1]
A Wowol village on Atwell's Island was named Chawlowin, occupied later than 1852 by refugee Yokuts natives. Yoimut described semi-traditional life at Chawlowin:
My mother found almost all of her relations there at Chawlowin. Her brother had his family there and two or three of her uncles were there, too. They had all come back to that camp from Tule River Reservation, where the soldiers had taken them from Téjon Ranch. They wanted to stay at their old home. These people did not go back to the old village at the mouth of Deer Creek and White River because they would come back and get them. They were hid in the tules in tumlus (toom-loos) houses at the north side of the Island.
Gull Island was a small islet at the mouth of the Tule River, extending westward from the south bank of the Tule River. It was a narrow bar which was low, muddy, and had no vegetation. It was named for the large number of seagulls which nested at the site.
Pelican Island was formed from deposits of the Kings River as an extension of its east channel, about a mile long and ten to sixty feet wide in 1883. It was named (as with Gull Island) for the vast number of white pelicans that nested on there. Brandt's cormorant also was present.
Skull Island extended between five and six miles and was just over half a mile wide, the highest part being about twenty feet above the lakebed. Skull Island is one of the more locally famous landmarks. Frank F. Latta identifies it with the Calaveres [ sic ] of the early Spanish settlers. [5] [6] Yoimut (Josie Alonzo) described a village, Witi'tsolo wın, probably on or near the site, to Anna Hardwick Gayton, which she visited between 1860 and 1870. [1] [7] Throughout the 19th century it was common for settlers in the Central Valley to raid Skull Island. Dr. William Ferguson Cartmill, who numerous streets are named after in Tulare County, took several skulls from the site and kept them in his house. [6] Local legend holds of a great "Indian battle" that took place at Skull Island. [5] However, it is far more likely that the mass grave on Skull Island was due to an epidemic, probably smallpox.
For many years the tradition was that these unburied skeletons were the results of a great Indian battle. We can well believe upon good authority that [the battle] was really not the case, but that during the pestilence of 1833 this tribe was probably killed by the same plague which almost entirely depopulated the entire San Joaquin Valley.
— Frank F. Latta, Tulare Daily Times Tuesday, 9 June 1931
Native ecosystems of the region ranged from saltbrush scrub and alkali sink to valley grassland and wetland. Today alfalfa is grown on some parts of the southern basin and invasive saltcedar is recorded in natural habitats. [8] Indigenous fauna of the Sand Ridge area include Buena Vista Lake shrew (Sorex ornatus relictus), southwestern pond turtle (Actinemys pallida), fulvous whistling-duck (Dendrocygna bicolor), least bittern (Ixobrychus exilis), California red-legged frog (Rana aurora draytonii) and giant garter snake (Thamnophis gigas). [8] Other species native or present in the area are sandhill cranes and tricolored blackbird. Historically attested species (sometimes present in nearby placenames) like the tule elk and pronghorn antelope were of economic importance to Native American peoples living in the area. Grizzly Adams hunted tule elk on Pelican Island in the 1850s. [5]
The Tulare Lake region has been continually inhabited for more than 10,000 years. The Witt Site, on the shores of Tulare Lake, has yielded fluted and stemmed points from Paleoindian cultures, flaked stone crescents, Pinto points, drills, and limaces or "humpies." Fragmented mineralized bone have been identified as horse ( Equus ), bison ( Bison ), ground sloth ( Paramylodon ), and mammoth ( Mammuthus ) or mastodon ( Mammut ). [9]
The Sand Ridge area has similarly been occupied since at least the late Pleistocene. [10] According to the Bureau of Land Management, Sand Ridge "has yielded artifacts spanning the entire cultural horizon in California." [10] Historical research by William Preston suggests that European-introduced epidemics may have devastated Lake Indians as early as 1500. [11]
At the point of European contact, three Yokuts nations inhabited the Tulare Lake area. The Wowol, to the southern margin, the Chunut to the east, and the Tachi to the north and west. [12]
European exploration into the Tulare Basin area began in 1805 with Fr. Juan Martin, who was the first European to see the lake. He arrived in Wowol territory following a three-day trip from the coast. [12]
In 1816, Luís Antonio Martinez destroyed the rancheria of Bubal, burning the village, scattering their grain, and smashing their grinding stones. He was heavily criticized for his cruelty by Father Juan Cabot, who was present on the expedition. [13]
According to Frank F. Latta, a pandemic around 1833 that wiped out nearly the entire western San Joaquin Valley:
At least three centenarians among my Yokuts informants were children here at that time. They were able to verify the existence of such an occurrence and to give me some account of it: burial of dead bodies until there were not enough survivors to make burials; abandonment of village sites, fleeing to the mountains, and later, studying the general condition of the valley floor and foothills until the Mewalk throught[ sic ] them safe for reoccupation. These centarians were Pahmit, San Joaquin River Dumna; Sahn-e-hat, Tule River Yaudanche, and To-tu-yah, Yosemite Valley Mewalk. Totuyah and Pahmit actually knew of the Mewalk moving down into the vacant Yokuts territory. [14]
Skull Island was probably a result of this epidemic, as Latta’s informants specifically note that bodies were too high in quantity for the living to bury them. [15]
Two Mexican land grants were claimed in 1843, one between Kings River and Cross Creek, and another, Manuel Castro’s Rancho Laguna de Tache on the north bank of the Kings River. John C. Fremont led a United States military expedition across California, including Tulare Lake, immediately before the Mexican-American War.
Anglo-Americans began entering the Tulare Basin in 1826. The first American to enter the San Joaquin Valley was Jedediah Smith. [16] [13]
In 1854, Grizzly Adams hunted on Pelican Island, "where there was said to be elk in abundance." Children from a village on the mouth of the Kings River guided him to the island on a canoe made of tules. In 1858 or 1859, settlers ethnically cleansed Tulare Lake, forcibly moving hundreds of Yokuts to the Fresno River Reservation to the north. Severe floods in 1861 and 1867, killing thousands of cattle, resulted in settlers calling for further dams on the inflows to Tulare Lake. From 1875 to 1877, large numbers of hogs and cattle were carried to Skull Island from the mainland on the Mose Andross. [17]
Presumably the last autonomous Indigenous people lived at the Tulare Lake archipelago in the 1870s. Yoimut detailed white settlers introducing cattle to the island and subsequently forcing the indigenous people out:
While we were at Chawlowin some white men put cattle on the island. The water was low and they drove them across from the east. There were hogs there already, but they were wild. As soon as the white people found out we were there we began to have trouble. The tules were getting dry and we were afraid the white people would burn us out. So we all left. My mother and stepfather took us to Téjon Ranch. We went in his brother's little wagon. [18]
In the wake of the United States Civil War, late 19th-century settlers drained the surrounding marshes for early agriculture. In 1884, Scottish travel writer Constance Gordon-Cumming would warn that "[e]ven the great Tulare lake itself is in danger of being gradually absorbed by the numerous canals and ditches with which the whole country is now being intersected...[t]he poor lakes have simply been left to starve—the rivers, whose surplus waters hitherto fed them, having now been bridled and led away in ditches and canals to feed the great wheat-fields." [19] That same year, Scientific American predicted the "utter absorption" of Tulare Lake. [20] The Kaweah, Kern, Kings, and Tule Rivers were dammed upstream in the Sierra Nevada Mountains, which turned their headwaters into a system of reservoirs. In the San Joaquin Valley, the state and counties built canals to deliver that water and divert the remaining flows for agricultural irrigation and municipal water uses. Tulare Lake was nearly dry by the early 20th century.
Swedish naturalist Gustav Eisen, who crossed the lake by steamboat in 1878 and undertook an excavation of Sand Ridge probably that same year, celebrated the desiccation. [13] He wrote,
In my opinion the drying up of Tulare Lake is a good thing. The land will be good for crops and there will be less sickness in the vicinity. The sloughs and marsh land in the old days used to be full of malaria that will now be a thing of the past. [22]
Skull Island, surrounded by wheat fields, was eventually raided by grave robbers. [22]
Enough water remained so the Alameda Naval Air Station used Tulare Lake as an outlying seaplane base during World War II and the early years of the Cold War. Flying boats could land on Tulare Lake when landing conditions were unsafe on San Francisco Bay. [23] In 1938 and 1955, the lake flooded, which prompted the construction of the Terminus and Success Dams on the Kaweah and Tule Rivers in Tulare County and Pine Flat Dam on the Kings River in Fresno County. [24] The lake bed is now a shallow basin of fertile soil, within the Central Valley of California, the most productive agricultural region of the United States. Farmers have irrigated the area for a century, so soil salination is becoming a concern. The destruction of the terrestrial wetlands and the lake ecosystem habitats resulted in substantial losses of terrestrial animals, plants, aquatic animals, water plants, and resident and migrating birds. Although now dry, the lake occasionally reappears during floods following unusually high levels of rainfall or snow melt, as it did in 1983 and 1997. For this reason, it has been called a "phantom lake," or "the lake that will not die". [25]
In 1938 and 1955, the lake flooded, which prompted the construction of the Terminus and Success Dams on the Kaweah and Tule Rivers in Tulare County and Pine Flat Dam on the Kings River in Fresno County. [24] Although now dry, the lake occasionally reappears during floods following unusually high levels of rainfall or snow melt, as it did in 1969, 1983, [24] 1997 and 2023. [27] [28] [29]
Estimates have found that Tulare Lake could hold twice the water of the proposed Temperance Flat Dam at one-fifth the cost. [30]
Yoimut, who spent a significant portion of her life on the lake, warned ethnographer Frank F. Latta that the lake would return. [1]
In 2023, the communities of Alpaugh and Allensworth were evacuated due to concerns that they might become flooded. [27] Alpaugh was formerly on the site of Chawlowin, a Wowol Yokuts village, which sat on an island in Tulare Lake. [1]
TV personality Huell Howser visited Tulare Lake in an episode of his show, California's Gold, in 1999. [31]
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(help)Tulare County is a county located in the U.S. state of California. As of the 2020 census, the population was 473,117. The county seat is Visalia. The county is named for Tulare Lake, once the largest freshwater lake west of the Great Lakes. Drained for agricultural development, the site is now in Kings County, which was created in 1893 from the western portion of the formerly larger Tulare County.
The Central Valley is a broad, elongated, flat valley that dominates the interior of California. It is 40–60 mi (60–100 km) wide and runs approximately 450 mi (720 km) from north-northwest to south-southeast, inland from and parallel to the Pacific coast of the state. It covers approximately 18,000 sq mi (47,000 km2), about 11% of California's land area. The valley is bounded by the Coast Ranges to the west and the Sierra Nevada to the east.
The San Joaquin River is the longest river of Central California. The 366-mile (589 km) long river starts in the high Sierra Nevada, and flows through the rich agricultural region of the northern San Joaquin Valley before reaching Suisun Bay, San Francisco Bay, and the Pacific Ocean. An important source of irrigation water as well as a wildlife corridor, the San Joaquin is among the most heavily dammed and diverted of California's rivers.
The Kings River is a 132.9-mile (213.9 km) river draining the Sierra Nevada mountain range in central California in the United States. Its headwaters originate along the Sierra Crest in and around Kings Canyon National Park and form the eponymous Kings Canyon, one of the deepest river gorges in North America. The river is impounded in Pine Flat Lake before flowing into the San Joaquin Valley southeast of Fresno. With its upper and middle course in Fresno County, the Kings River diverges into multiple branches in Kings County, with some water flowing south to the old Tulare Lake bed and the rest flowing north to the San Joaquin River. However, most of the water is consumed for irrigation well upstream of either point.
The St. John's River is a distributary of the Kaweah River in the San Joaquin Valley of California in the United States. The river begins at a diversion dam at McKay's Point, about a mile west of Lemon Cove. The distributary flows west along the north side of the city of Visalia, where it joins Elbow Creek, continuing west to Cross Creek.
The Governor Edmund G. Brown California Aqueduct is a system of canals, tunnels, and pipelines that conveys water collected from the Sierra Nevada Mountains and valleys of Northern and Central California to Southern California. Named after California Governor Edmund Gerald "Pat" Brown Sr., the over 400-mile (640 km) aqueduct is the principal feature of the California State Water Project.
The Kern River, previously Rio de San Felipe, later La Porciuncula, is an Endangered, Wild and Scenic river in the U.S. state of California, approximately 165 miles (270 km) long. It drains an area of the southern Sierra Nevada mountains northeast of Bakersfield. Fed by snowmelt near Mount Whitney, the river passes through scenic canyons in the mountains and is a popular destination for whitewater rafting and kayaking. It is the southernmost major river system in the Sierra Nevada, and is the only major river in the Sierra that drains in a southerly direction.
The Mono are a Native American people who traditionally live in the central Sierra Nevada, the Eastern Sierra, 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 a single, unique, unified group of Great Basin tribes.
The Tule River, also called Rio de San Pedro or Rio San Pedro, is a 71.4-mile (114.9 km) river in Tulare County in the U.S. state of California. The river originates in the Sierra Nevada east of Porterville and consists of three forks, North, Middle and South. The North Fork and Middle Fork meet above Springville. The South Fork meets the others at Lake Success. Downstream of Success Dam, the river flows west through Porterville. The river used to empty into Tulare Lake, but its waters have been diverted for irrigation. However, the river does reach Tulare Lake during floods. Tulare Lake is the terminal sink of an endorheic basin that historically also received the Kaweah and Kern Rivers as well as southern distributaries of the Kings.
The Tübatulabal are an indigenous people of Kern River Valley in the Sierra Nevada range of California. They may have been the first people to make this area their permanent home. Today many of them are enrolled in the Tule River Indian Tribe. They are descendants of the people of the Uto-Aztecan language group, separating from Shoshone people about 3000 years ago.
The Kaweah River is a river draining the southern Sierra Nevada in Tulare County, California in the United States. Fed primarily by high elevation snowmelt along the Great Western Divide, the Kaweah begins as four forks in Sequoia National Park, where the watershed is noted for its alpine scenery and its dense concentrations of giant sequoias, the largest trees on Earth. It then flows in a southwest direction to Lake Kaweah – the only major reservoir on the river – and into the San Joaquin Valley, where it diverges into multiple channels across an alluvial plain around Visalia. With its Middle Fork headwaters starting at almost 13,000 feet (4,000 m) above sea level, the river has a vertical drop of nearly two and a half miles (4.0 km) on its short run to the San Joaquin Valley, making it one of the steepest river drainages in the United States. Although the main stem of the Kaweah is only 33.6 miles (54.1 km) long, its total length including headwaters and lower branches is nearly 100 miles (160 km).
Isabella Dam is an embankment dam located in the Kern River Valley, about halfway down the Kern River course, between the towns of Kernville and Lake Isabella in Kern County, California.
Terminus Dam is a dam on the Kaweah River in Tulare County, California in the United States, located near Three Rivers about 15 mi (24 km) from the western boundary of Sequoia National Park and 20 mi (32 km) east of Visalia. The dam forms Lake Kaweah for flood control and irrigation water supply. Completed by the U.S. Army Corps of Engineers (USACE) in 1962, Terminus is an earthfill dam 255 ft (78 m) high and 2,375 ft (724 m) long. The reservoir has a maximum capacity of 185,600 acre⋅ft (0.2289 km3) of water, although it usually sits at much lower levels.
Visalia, California, commonly known in the 1850s as Four Creeks, is the oldest continuously inhabited inland European settlement between Stockton and Los Angeles. The city played an important role in the American colonization of the San Joaquin Valley as the county seat of Old Tulare County, an expansive region comprising most if not all of modern-day Fresno, Kings, and Kern counties.
The Stockton–Los Angeles Road, also known as the Millerton Road, Stockton–Mariposa Road, Stockton–Fort Miller Road or the Stockton–Visalia Road, was established about 1853 following the discovery of gold on the Kern River in Old Tulare County. This route between Stockton and Los Angeles followed by the Stockton–Los Angeles Road is described in "Itinerary XXI. From Fort Yuma to Benicia, California", in The Prairie Traveler: A Hand-book for Overland Expeditions by Randolph Barnes Marcy. The Itinerary was derived from the report of Lieutenant R. S. Williamson on his topographical survey party in 1853, that was in search of a railroad route through the interior of California.
Buena Vista Lake was a fresh-water lake in Kern County, California, in the Tulare Lake Basin in the southern San Joaquin Valley, California.
The Tule River War of 1856 was a conflict where American settlers, and later, California State Militia, and a detachment of the U. S. Army from Fort Miller, fought a six-week war against the Yokuts in the southern San Joaquin Valley.
Yoimut or Yo'yomat was a Yokuts woman who was the last speaker of the Chunut language of central California. Josie Alonzo has also been recorded as the last "full-blooded" Chunut. She was a noted polyglot, speaking 8 different Yokutsan languages along with English and Spanish. She was among the last indigenous inhabitants of Tulare Lake, before being forcibly removed by Anglo-American settlers. She was an informant to anthropologists Frank F. Latta and A. H. Gayton.
Sacramento–San Joaquin is a freshwater ecoregion in California. It includes the Sacramento and San Joaquin river systems of California's Central Valley, which converge in the inland Sacramento–San Joaquin Delta. It also includes the mostly-closed Tulare Lake basin in the southern Central Valley, the rivers and streams that empty into San Francisco Bay, and the Pajaro and Salinas river systems of Central California which empty into Monterey Bay.