Santa Barbara, CA

Santa Barbara ( es, Santa Bárbara, meaning "Saint Barbara") is a coastal city in Santa Barbara County, California, of which it is also the county seat. Situated on a south-facing section of coastline, the longest such section on the West Coast of the United States, the city lies between the steeply rising Santa Ynez Mountains and the Pacific Ocean. Santa Barbara's climate is often described as Mediterranean, and the city has been dubbed "The American Riviera". According to the 2020 U.S. Census, the city's population was 88,665.

In addition to being a popular tourist and resort destination, the city has a diverse economy that includes a large service sector, education, technology, health care, finance, agriculture, manufacturing, and local government. In 2004, the service sector accounted for 35% of local employment. Education in particular is well represented, with four institutions of higher learning nearby: the University of California, Santa Barbara, Santa Barbara City College, Westmont College, and Antioch University. The city is served by Santa Barbara Airport and train service is provided by Amtrak, which operates the Pacific Surfliner, which runs from San Diego to San Luis Obispo. The Santa Barbara area is connected via U.S. Highway 101 to Los Angeles to the southeast and San Francisco to the northwest. Behind the city, in and beyond the Santa Ynez Mountains, is the Los Padres National Forest, which contains several remote wilderness areas. Channel Islands National Park and Channel Islands National Marine Sanctuary are located approximately offshore.

History

Evidence of human habitation of the area begins at least 13,000 years ago. Evidence for a Paleoindian presence includes a fluted Clovis-like point found in the 1980s along the western Santa Barbara County coast, as well as the remains of Arlington Springs Man, found on Santa Rosa Island in the 1960s. At least 25,000 Chumash natives lived in the region prior to Spanish contact. Five Chumash villages flourished in the area. The present-day area of Santa Barbara City College was the village of ''Mispu''; the site of the Los Baños pool (along west beach) was the village of ''Syukhtun'', chief Yanonalit's large village located between Bath and Chapala streets; ''Amolomol'' was at the mouth of Mission Creek; and ''Swetete'', above the bird refuge.

Spanish era

Spanish explorer Juan Rodríguez Cabrillo, sailing for the Kingdom of Spain, sailed through what is now called the Santa Barbara Channel in 1542, anchoring briefly in the area. In 1602, Spanish maritime explorer Sebastián Vizcaíno gave the name "Santa Barbara" to the channel and also to one of the Channel Islands.

A land expedition led by Gaspar de Portolà visited around 1769, and Franciscan missionary Juan Crespi, who accompanied the expedition, named a large native town "Laguna de la Concepcion". Cabrillo's earlier name, however, is the one that has survived.

The first permanent European residents were Spanish missionaries and soldiers under Felipe de Neve, who arrived in 1782 and constructed the Presidio. They were sent to both secure the Spanish claim to the region and to convert the indigenous peoples to Catholicism. Many of the Spaniards brought their families with them, and those formed the nucleus of the small town – at first just a cluster of adobes – that surrounded the Presidio of Santa Barbara. The Santa Barbara Mission was established on the Feast of Saint Barbara, December 4, 1786. It was the tenth of the California Missions to be founded by the Spanish Franciscans. It was dedicated by Padre Fermín Lasuén, who succeeded Padre Junipero Serra as the second president and founder of the California Franciscan Mission Chain. The Chumash laborers built a connection between the canyon creek and the Santa Barbara Mission water system through the use of a dam and an aqueduct. During the following decades, many of the natives died of diseases such as smallpox, against which they had no natural immunity.

The most dramatic event of the Spanish period was the powerful 1812 earthquake, and tsunami, with an estimated magnitude of 7.1, which destroyed the Mission as well as the rest of the town; water reached as high as present-day Anapamu street, and carried a ship half a mile up Refugio Canyon. The Mission was rebuilt by 1820 after the earthquake. Following the earthquake, the Mission fathers chose to rebuild in a grander manner, and it is this construction that survives to the present day, the best-preserved of the California Missions, and still functioning as an active church by the Franciscans. After the Mexican government secularized the missions in the 1830s, the baptismal, marriage, and burial records of other missions were transferred to Santa Barbara, and now found in the Santa Barbara Mission Archive-Library.

The Spanish period ended in 1822 with the conclusion of the Mexican War of Independence, which terminated 300 years of Spanish colonial rule and transferred control to the newly independent Mexican government.

Santa Barbara street names reflect the influence of the Spanish period. The names ''de le Guerra'' and ''Carrillo'' come from the Guerra family of California and Carrillo family of California. They were instrumental in building up the town, so they were honored by having streets named after them.

Mexican era

After the forced secularization of the Missions in 1833, successive Mexican Governors distributed the large land tracts formerly held by the Franciscan Order to various families in order to reward service or build alliances. These land grants to local notable families mark the beginning of the "Rancho Period" in California and Santa Barbara history. Fernando Tico was one of the first settlers who received land grants for the local area. Fernando led the Native Americans against the Argentinian pirates in the 1800s. The population remained sparse, with enormous cattle operations run by wealthy families. It was during this period that Richard Henry Dana, Jr. first visited Santa Barbara and wrote about the culture and people of Santa Barbara in his book ''Two Years Before the Mast''.

Santa Barbara fell bloodlessly to a battalion of American soldiers under John C. Frémont on December 27, 1846, during the Mexican–American War, and after the Treaty of Guadalupe Hidalgo in 1848 it became part of the expanding United States.

Post-Conquest era

Change came quickly in Santa Barbara following the American Conquest of California. The population doubled between 1850 and 1860. In 1851, land surveyor Salisbury Haley designed the street grid, famously botching the block measurements, misaligning the streets, thereby creating doglegs at certain intersections. Wood construction replaced adobe as American settlers moved in; during the Gold Rush years and following, the town became a haven for bandits and gamblers, and a dangerous and lawless place. Charismatic gambler and highwayman Jack Powers had virtual control of the town in the early 1850s, until driven out by a posse organized in San Luis Obispo. English gradually supplanted Spanish as the language of daily life, becoming the language of official record in 1870. The first newspaper, the ''Santa Barbara Gazette'', was founded in 1855.

While the Civil War had little effect on Santa Barbara, the disastrous drought of 1863 ended the Rancho Period, as most of the cattle died and ranchos were broken up and sold. Mortimer Cook, a wealthy entrepreneur, arrived in 1871 and opened the city's first bank. Cook later served two terms as mayor. Cook founded the first National Gold Bank of Santa Barbara in 1873. The building of Stearns Wharf in 1872 enhanced Santa Barbara's commercial and tourist accessibility; previously goods and visitors had to transfer from steamboats to smaller craft to row ashore. During the 1870s, writer Charles Nordhoff promoted the town as a health resort and destination for well-to-do travelers from other parts of the U.S.; many of them came, and many stayed. The luxurious Arlington Hotel dated from this period. In 1887 the railroad finally went through to Los Angeles, and in 1901 to San Francisco: Santa Barbara was now easily accessible by land and by sea, and subsequent development was brisk. Santa Barbara had a system of street railways that operated from 1875 through 1929. Begun as a single mule-drawn line from the waterfront pier to the Arlington Hotel, over the decades it was incrementally expanded, later electrified, and operated until its closure in June 1929.

Peter J. Barber, an architect, designed many Late Victorian style residences, and served twice as mayor, in 1880 and again in 1890. A year after Barber's term as mayor, President Benjamin Harrison became the first of five presidents to visit Santa Barbara.

Early 20th century to World War II

Just before the turn of the 20th century, oil was discovered at the Summerland Oil Field, and the region along the beach east of Santa Barbara sprouted numerous oil derricks and piers for drilling offshore. This was the first offshore oil development in the world; oil drilling offshore would become a contentious practice in the Santa Barbara area, which continues to the present day.

Santa Barbara housed the world's largest movie studio during the era of silent film. Flying A Studios, a division of the American Film Manufacturing Company, operated on two city blocks centered at State and Mission between 1910 and 1922, with the industry shutting down locally and moving to Hollywood once it outgrew the area, needing the resources of a larger city. Flying A and the other smaller local studios produced approximately 1,200 films during their tenure in Santa Barbara, of which approximately 100 survive.

During this period, the Loughead Aircraft Company was established on lower State Street, and regularly tested seaplanes off of East Beach. This was the genesis of what would later become Lockheed.

The magnitude 6.3 earthquake of June 29, 1925, the first destructive earthquake in California since the 1906 San Francisco quake, destroyed much of downtown Santa Barbara and killed 13 people. The earthquake caused infrastructure to collapse including the Sheffield Dam. The low death toll is attributed to the early hour (6:44 a.m., before most people were out on the streets, vulnerable to falling masonry). While this quake, like the one in 1812, was centered in the Santa Barbara Channel, it caused no tsunami. It came at an opportune time for rebuilding, since a movement for architectural reform and unification around a Spanish Colonial style was already underway. Under the leadership of Pearl Chase, many of the city's famous buildings rose as part of the rebuilding process, including the Santa Barbara County Courthouse, and Naval Reserve Center Santa Barbara at the harbor. Up the coast, west of the city, was the Army's Camp Cooke (the present-day Vandenberg Space Force Base). In the city,
Hoff General Hospital treated servicemen wounded in the Pacific Theatre. On February 23, 1942, not long after the outbreak of war in the Pacific, the Japanese submarine '' I-17'' surfaced offshore and lobbed 16 shells at the Ellwood Oil Field, about west of Santa Barbara, in the first shelling attack by an enemy power on the continental U.S. since the bombardment of Orleans in World War I. Although the shelling was inaccurate and only caused about $500 damage to a catwalk, panic was immediate. Many Santa Barbara residents fled, and land values plummeted to historic lows.

After World War II

After the war many of the servicemen who had seen Santa Barbara returned to stay. The population surged by 10,000 people between the end of the war and 1950. This burst of growth had dramatic consequences for the local economy and infrastructure. Highway 101 was built through town during this period, and newly built Lake Cachuma began supplying water via a tunnel dug through the mountains between 1950 and 1956.

Local relations with the oil industry gradually soured through the period. Production at Summerland had ended, Elwood was winding down, and to find new fields oil companies carried out seismic exploration of the Channel using explosives, a controversial practice that local fishermen claimed harmed their catch. The culminating disaster, and one of the formative events in the modern environmental movement, was the blowout at Union Oil's Platform A on the Dos Cuadras Field, about eight miles (13 km) southeast of Santa Barbara in the Santa Barbara Channel, on January 28, 1969. Approximately of oil surged out of a huge undersea break, fouling hundreds of square miles of ocean and all the coastline from Ventura to Goleta, as well north facing beaches on the Channel Islands. Two legislative consequences of the spill in the next year were the passages of the California Environmental Quality Act (CEQA) and the National Environmental Policy Act (NEPA); locally, outraged citizens formed GOO (Get Oil Out).Baker, pp. 88–89
Santa Barbara's business community strove to attract development until the surge in the anti-growth movement in the 1970s. Many "clean" industries, especially aerospace firms such as Raytheon and Delco Electronics, moved to town in the 1950s and 1960s, bringing employees from other parts of the U.S. UCSB itself became a major employer. In 1975, the city passed an ordinance restricting growth to a maximum of 85,000 residents, through zoning. Growth in the adjacent Goleta Valley could be shut down by denying water meters to developers seeking permits. As a result of these changes, growth slowed down, but prices rose sharply.

When voters approved connection to State water supplies in 1991, parts of the city, especially outlying areas, resumed growth, but more slowly than during the boom period of the 1950s and 1960s. While the slower growth preserved the quality of life for most residents and prevented the urban sprawl notorious in the Los Angeles basin, housing in the Santa Barbara area was in short supply, and prices soared: in 2006, only six percent of residents could afford a median-value house. As a result, many people who work in Santa Barbara commute from adjacent, more affordable areas, such as Santa Maria, Lompoc, and Ventura. The resultant traffic on incoming arteries, in particular the stretch of Highway 101 between Ventura and Santa Barbara, is another problem being addressed by long-range planners.

Notable wildfires

Since the middle of the twentieth century, several destructive fires have affected Santa Barbara: the 1964 Coyote Fire, which burned of backcountry along with 106 homes; the smaller, but quickly moving, Sycamore Fire in 1977, which burned 200 homes; the disastrous 1990 Painted Cave Fire, which incinerated over 500 homes in only several hours, during an intense Sundowner wind event; the November 2008 Tea Fire, which destroyed 210 homes in the foothills of Santa Barbara and Montecito; and the 2009 Jesusita Fire that burned and destroyed 160 homes above the San Roque region of Santa Barbara.

The Thomas Fire burned from its origins in Santa Paula to the east of Santa Barbara and consumed in Santa Barbara and Ventura counties, most of which consisted of rural land and wilderness areas. The fire started December 4, 2017, and was 100% contained by January 12, 2018. 1,050 structures were lost in the Thomas Fire, mostly east of Santa Barbara in Ventura County. The Thomas Fire has been the largest Santa Barbara County fire ever recorded to date.

Geography

Santa Barbara is located about west-northwest of Los Angeles, along the Pacific coast. This stretch of coast along southern Santa Barbara County is sometimes referred to as "The American Riviera", presumably because its geography and climate are similar to that of areas along the northern Mediterranean Sea coast (especially in southern France) known as the Riviera. The Santa Ynez Mountains, an east–west trending range, rise dramatically behind the city, with several peaks exceeding . Covered with chaparral, oaks and sandstone outcrops, they make a scenic backdrop to the town. Sometimes, perhaps once every three years, snow falls on the mountains, but it rarely stays for more than a few days. Nearer to town, directly east and adjacent to Mission Santa Barbara, is an east–west ridge known locally as "the Riviera," traversed by a road called "Alameda Padre Serra" (shortened APS, which translates to "Father Serra's pathway").

According to the United States Census Bureau, the city has a total area of , of which of it is land and of it (53.61%) is water. The high official figures for water is due to the extension of the city limit into the ocean, including a strip of city reaching out into the sea and inland again to keep the Santa Barbara Airport (SBA) within the city boundary.

Climate

Santa Barbara experiences a warm-summer Mediterranean climate ( Köppen: Csb) characteristic of coastal California. Santa Barbara's weather was ranked number 1 in the United States in 2018 by U.S. News & World Report. Because the city lies along the ocean and parallel to the predominant westerly winds, sideshore and light onshore breezes moderate temperatures resulting in warmer winters and cooler summers compared with places farther inland.

In the winter, storms reach California, some of which bring heavy rainfall but the rainshadow effect of the coastal mountains can at times moderate or enhance the rainfall depending on local storm wind flows. Local rainfall totals can be enhanced by orographic lift when storms are accompanied by southerly flow pushing moist air over the Santa Ynez mountains, producing greater rainfall than in other coastal areas. Diurnal temperature variation reaches a maximum in winter due to lower humidity and the absence of summer fog. On average, only 1.7 nights have freezing lows.

Summers in Santa Barbara are mostly rainless due to the presence of a high-pressure area over the eastern Pacific, but summer showers can happen due to tropical hurricane/Monsoonal flows that rarely reach the region; thunderstorms can also occur during the North American Monsoon. In the fall, afternoon or evening downslope winds, locally called " Sundowners", can raise temperatures into the high 90s °F (high 30s °C) and drop humidities into the single digits, increasing the chance due to downed power lines, etc., and severity of wildfires in the foothills north of the city.

Annual rainfall totals are highly variable and in exceptional years like 1940–1941 and 1997–1998 over of rain have fallen in a year, but in dry seasons less than is not unheard of. Snow sometimes covers higher elevations of the Santa Ynez Mountains but is extremely rare in the city itself. The most recent accumulating snow to fall near sea level was in January 1949, when approximately fell in the city.

Geology and soils

The city of Santa Barbara is situated on a coastal plain between the Santa Ynez Mountains and the sea. This coastal plain consists of a complex array of Holocene and Pleistocene alluvial and colluvial deposits, marine terraces, debris flows, and estuarine deposits. Soils are mostly well drained brown fine sandy loam of the Milpitas series. Rapid geologic uplift is characteristic of the entire region, as evidenced by the coastal bluffs and narrow beaches that are present along most of the coastline.

Downtown Santa Barbara occupies a floodplain between two major geologic faults, the Mission Ridge Fault Zone to the north and the Mesa Fault to the south. The Mission Ridge Fault Zone runs along the range of hills known locally as the "Riviera", and the Mesa Fault defines the northern boundary of the band of hills called the "Mesa". These two faults converge near the Five Points Shopping Center at Los Positas and State Streets. Neither is well-exposed, with their locations being inferred from topography, springs, seeps, and well logs. The Mesa Fault continues southeast offshore into the Santa Barbara Channel; the portion of the fault offshore is believed to have been responsible for the destructive earthquake of 1925. The Mission Ridge Fault trends east–west, being named the More Ranch Fault west of Santa Barbara, and forms the northern boundary of the uplands which include Isla Vista, More Mesa, and the Hope Ranch Hills.

Three major sedimentary bedrock units underlie the coastal plain: the Monterey Formation, the Sisquoc Formation, and the Santa Barbara Formation. The Santa Barbara Formation is one of the main units in the aquifer underlying the city. Its coarse-grained freshwater-bearing portion, much of which is below sea level, is protected from seawater intrusion by the More Ranch Fault, which has shielded it by uplifting less-permeable rocks between it and the sea. The majority of water wells in the Santa Barbara-Goleta area pull from this geologic unit.

The Santa Ynez Mountains to the north of the city consist of multiple layers of sandstone and conglomerate units dating from the Jurassic Age to the present, uplifted rapidly since the Pliocene

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