Museums and Galleries - Installing Exhibitions
View allAll Photos Tagged install
Buse variable (Buteo buteo)
Perchée sur les installations de la ligne ferroviaire en face de chez moi, elle est à l'affut des souris qui trottent dans le ballast.
Vu depuis mon balcon !
Le musée est installé dans l'édifice gothique monumental qui abritait l'hôpital des Chevaliers de Saint-Jean. Sa construction a été commencée en 1440 et achevée à l'époque du grand maître d'Aubusson (1476-1503).
Il abrite des œuvres d'art de Rhodes et des îles voisines, de l'époque préhistorique à l'époque protobyzantine et jusqu'à l'époque des Chevaliers, qui composent une image d'une culture cosmopolite, vivante et continue.
part of installation at exhibition "Now, the future of the past", In Liemers Museum, Zevenaar (NL) 2018
Installed in the courtyard of MoMA-PS1. "Le Grand Soir" (The Big Night) by artist Yto Barrada
From the museum's website:
Yto Barrada (French-Moroccan, b. 1971) transforms the courtyard with a colorful arrangement of towering sculptures built from stacked concrete blocks, which visitors can sit on and explore. Barrada often mines the hidden histories embedded within architectural and geometric forms, revealing the intersections of material, political, and personal narratives. For Le Grand Soir, Barrada looks to the tradition of constructing human pyramids in Morocco, where their distinctive applications have ranged from martial arts and acrobatics to spiritual practices. Each of Barrada’s structures takes inspiration from an acrobatic formation used by Moroccan acrobats: tqal (weight), bourj tarbaite (tower of four), and bourj benayma ou chebaken (tower lift with net). They also draw on subjects as wide-ranging as Moroccan Brutalism and Barrada’s family lore, weaving together distinct historical moments of shapeshifting, surmounting barricades, and retooling architectures.
La Maison de Nostradamus est un Musée installé, depuis 1992, dans le logis où habita Michel de Notredame, dit Nostradamus (1503-1566), de 1547 à sa mort, et dans lequel il écrivit ses célèbres "Prophéties" (Lyon 1555).
Situé au coeur du centre ancien de la ville de Salon-de-Provence, au pied du Château de l'Empéri, le Musée est construit autour de cet énigmatique personnage qui scruta le passé, le présent… et l'avenir jusqu'en 3797 (!)
L'accent est mis sur l'homme pluriel s'adonnant à la Médecine, la Pharmacie, l'Astrologie, l'Humanisme, côtoyant, dans la foulée, Rabelais, Catherine de Médicis, Charles IX, Marguerite de Navarre et bien d'autres encore… discutant des nouvelles idées de la Réforme, citant la Bible, évoquant la Kabbale hébraïque ou pesant l'intérêt des premières notions d'hygiène mises en pratique lors des grandes épidémies de peste.
A la Renaissance, l'instrument des "Mathématiques" va trouver sa principale application dans le domaine de l'Architecture : " Ainsi, toute mesure doit dériver du corps humain, résumé et microcosme de l'univers créé par Dieu."
L'ascension initiatique de Nostradamus va le conduire vers un savoir universel, tel l'escalier transparent de la cité céleste.
Powerfully emotive bronze sculpture positioned at the front of the National Art Gallery of NSW in Sydney.
It is one of a pair, the other being The Offerings of Peace. Both by British sculptor Gilbert Bayes (1872 – 1953).
In 1915, after the outbreak of World War I, Bayes submitted to the National Art Gallery a pair of 18 inch bronzed plaster figures entitled Offerings of Peace and Offerings of War and the following year he received the commission to produce large bronze versions to flank the museum's main entrance. They were finished in 1923 and installed in 1926.
Both are allegorical sculptures. War holds a staff, a bundle of swords and broken spear shafts.
This statue stands 4. 2 m in height and weights 6 tonnes.
© All rights reserved.
For many years, the Miami-Dade County Courthouse, at an elevation of 360 feet, was reputed to be the tallest building south of Baltimore.
It was the County's first high-rise and is in the National Register of Historic Places. Efforts to refurbish this magnificent structure and restore it to its original grandeur have been underway since 1981 by Architect James W. Piersol, AIA of M.C Harry Associates Architects of Miami.
The restoration and renovations initially stabilized the terra cotta facade and installed new life safety systems. In 1982, the idea of restoring the lobby to its original distinction was the passion of both Architect James Piersol and engineer Don Youatt, of the Miami-Dade Planning and Development Department. With a little less than half of the funding necessary for the lobby restoration project in hand ($300,000 grant approved by the Legislature in 1996), the Dade County Bar Association acted as the fund-raising umbrella and initiate a drive to raise the remainder needed from lawyers and the general public. A few years later, the same team restored Courtroom 6-1, which had been the site of many infamous trials over the years.
Today, the Miami-Dade County Courthouse provides offices, chambers, and courtrooms for the clerks and judiciary assigned to both the Circuit and County Civil Court and the Family Court.
When county government was established following the Civil War, public records were so sparse they could be carried in a carpetbag and most probably were. Therefore, the "courthouse" was wherever the county's chief office holder decided to do business.
In 1890, Dade County's first courthouse stood in the town of Juno, Florida some ten miles north of West Palm Beach. At that time, Dade County covered more territory than it does today, stretching from Bahia Honda Key, in the middle Keys, up to the St. Lucie River, near present-day Port St. Lucie.
Juno was chosen as the "county seat" because of its strategic location at the southern terminus of the Jupiter-Juno railroad. Juno also held the northern terminus of the boat and connecting the stagecoach line to Miami. The courthouse remained in Juno (now no longer in existence) until 1899 when it was moved to Miami down the inland waterway on a barge and was placed on the banks of the Miami River, east of the old Miami Avenue bridge.
The building was two-story wooden frame construction, housing offices and jail cells on the ground floor and a courtroom on the second floor. It has a Neoclassical design, in 1904 this building was replaced by a new courthouse building situated on Flagler Street (then known as Twelfth Street). It was a magnificent building constructed of limestone, having an elegant red-domed top, at the cost of $47,000. It was anticipated that this courthouse would serve the city for at least fifty years; however, no one was prepared for the rapid growth Miami experienced during this period, and by 1924, only twenty years later, there was serious talk of the need for a larger courthouse.
In the early 1920s, architect A. Ten Eyck Brown entered a design competition for Atlanta City Hall, which was rejected. He then made the plans available to Dade County, and City and County officials readily approved them. It was decided by the officials to build the new courthouse at the same location as the existing one on Flagler Street. Construction began in 1925, with workers erecting the new building around the existing structure, which was then dismantled. Community leaders and citizens alike voiced excitement over the new 28 stories "skyscraper" that would soon dominate the skyline.
Unexpectedly, construction was halted when the building reached ten stories. It was discovered that the "high-rise" was sinking into the spongy ground. Engineers consulted with an architect from Mexico City, who had encountered a similar problem while building the city's opera house. The consultant determined that the foundation pilings were not set deep enough. To correct the problem, cement supports were poured, which take up much of the space in the building's basement file room even to this day.
The courthouse was finally completed in 1928 at the cost of $4 million (USD 2013 $54.5 million). Initially, it served as both the Dade County Courthouse and the Miami City Hall. Jail cells occupied the top nine floors because these heights offered "maximum security" and were considered escape-proof. In 1934, a prisoner housed on the twenty-first floor picked the lock of his jail cell window and used a fire hose to lower himself to freedom. In the years following, more than 70 prisoners escaped from this so-called "secure" prison.
Credit for the data above is given to the following websites:
en.wikipedia.org/wiki/Miami-Dade_County_Courthouse
www.emporis.com/buildings/122294/miami-dade-county-courth...
© All Rights Reserved - you may not use this image in any form without my prior permission.
The bridge has been installed after paint and weathering, and scenic elements are getting underway slowly but surely.
This is an installation shot of the painting O Bright Sea combined with a rather explosive wave-like form employing Nnenna Okore's remarkable material. It is currently in the exhibition "La Mére | La Mer" at Saint Mary's College in South Bend. Thanks to Sherrie, Deb Hendriksma Anderson and her mother for help with the installation. .
In the painting the dense field of marks suggests a galaxy, perhaps also suggesting a shift in the significance of an otherwise lowly domestic event (taking a bath). The addition of Nnenna's installation furthers this expansive possibility.
This is the third time Nnenna and I have done joint installations. See more here
IE15 LJ74BPZ at Hastings Road Locksbottom working on route 358 towards Orpington Station.
Some of the new Irizar "ie tram" buses have entered service on the 358, after quite a delay with getting the electrical infrastructure installed, driver training, etc. It is probably one of the oddest bus in terms of design, not quite keen on the designs of the lower windows, could imagine if they get damaged!
Had to reinstall Skyrim cause it crashed for unknown reasons, so I was testing armors after the install, while taking screenshots!
La cité antique de Rhodes est née en 408 av. J.-C.. Son célèbre plan en damier fut réalisé par Hippodamos de Milet.
Pendant les guerres des diadoques, elle résista à un siège fameux par Démétrios Poliorcète en 305 av. J.-C., qu'elle commémora par l'édification du célèbre Colosse de Rhodes, détruit par un tremblement de terre en 226 av. J.-C.
Après l'expulsion des croisés de Terre sainte (1291), l'Ordre s'installe à Chypre avant de conquérir l'île de Rhodes. La ville devint le siège de l'ordre de Saint-Jean de Jérusalem durant plus de deux siècles, jusqu'en 1522. L'Ordre ceint la ville des impressionnants remparts que l'on peut toujours voir.
L'ensemble de l'enceinte fortifiée fait 800m sur 1000m pour un périmètre de 4km², permit de résister à des sièges importants dont celui du Sultan d'Égypte en 1444 et de Mehmet II en 1480. Conservé et entretenu par les Turcs après le xve siècle et restauré au xxe siècle, cet ensemble forme une des plus grandes places fortes médiévales d'Europe.
222:365
Sorry guys, boring shot today. I am worn out, exhausted and going to bed!
I will endeavor for a more interesting shot tomorrow.
On a bright note, I'm getting pretty good and bending my arm around and taking a photo without looking =]
Come to the opening next thurs 2/4! At Manuel Izquierdo Gallery in Sculpture Building at PNCA . Photo by Matt
Craters of the Moon National Monument and Preserve is a U.S. national monument and national preserve in the Snake River Plain in central Idaho. It is along US 20 (concurrent with US 93 and US 26), between the small towns of Arco and Carey, at an average elevation of 5,900 feet (1,800 m) above sea level.
The Monument was established on May 2, 1924. In November 2000, a presidential proclamation by President Clinton greatly expanded the Monument area. The 410,000-acre National Park Service portions of the expanded Monument were designated as Craters of the Moon National Preserve in August 2002. It spreads across Blaine, Butte, Lincoln, Minidoka, and Power counties. The area is managed cooperatively by the National Park Service and the Bureau of Land Management (BLM).
The Monument and Preserve encompass three major lava fields and about 400 square miles (1,000 km2) of sagebrush steppe grasslands to cover a total area of 1,117 square miles (2,893 km2). The Monument alone covers 343,000 acres (139,000 ha). All three lava fields lie along the Great Rift of Idaho, with some of the best examples of open rift cracks in the world, including the deepest known on Earth at 800 feet (240 m). There are excellent examples of almost every variety of basaltic lava, as well as tree molds (cavities left by lava-incinerated trees), lava tubes (a type of cave), and many other volcanic features.
Craters of the Moon is in south-central Idaho, midway between Boise and Yellowstone National Park. The lava field reaches southeastward from the Pioneer Mountains. Combined U.S. Highway 20–26–93 cuts through the northwestern part of the monument and provides access to it. However, the rugged landscape of the monument itself remains remote and undeveloped, with only one paved road across the northern end.
The Craters of the Moon Lava Field spreads across 618 square miles (1,601 km2) and is the largest mostly Holocene-aged basaltic lava field in the contiguous United States. The Monument and Preserve contain more than 25 volcanic cones, including outstanding examples of spatter cones. The 60 distinct solidified lava flows that form the Craters of the Moon Lava Field range in age from 15,000 to just 2,000 years. The Kings Bowl and Wapi lava fields, both about 2,200 years old, are part of the National Preserve.
This lava field is the largest of several large beds of lava that erupted from the 53-mile (85 km) south-east to north-west trending Great Rift volcanic zone, a line of weakness in the Earth's crust. Together with fields from other fissures they make up the Lava Beds of Idaho, which in turn are in the much larger Snake River Plain volcanic province. The Great Rift extends across almost the entire Snake River Plain.
Elevation at the visitor center is 5,900 feet (1,800 m) above sea level.
Total average precipitation in the Craters of the Moon area is between 15–20 inches (380–510 mm) per year. Most of this is lost in cracks in the basalt, only to emerge later in springs and seeps in the walls of the Snake River Canyon. Older lava fields on the plain have been invaded by drought-resistant plants such as sagebrush, while younger fields, such as Craters of the Moon, only have a seasonal and very sparse cover of vegetation. From a distance this cover disappears almost entirely, giving an impression of utter black desolation. Repeated lava flows over the last 15,000 years have raised the land surface enough to expose it to the prevailing southwesterly winds, which help to keep the area dry. Together these conditions make life on the lava field difficult.
Paleo-Indians visited the area about 12,000 years ago but did not leave much archaeological evidence. Northern Shoshone created trails through the Craters of the Moon Lava Field during their summer migrations from the Snake River to the camas prairie, west of the lava field. Stone windbreaks at Indian Tunnel were used to protect campsites from the dry summer wind. No evidence exists for permanent habitation by any Native American group. A hunting and gathering culture, the Northern Shoshone pursued elk, bears, American bison, cougars, and bighorn sheep — all large game who no longer range the area. The most recent volcanic eruptions ended about 2,100 years ago and were likely witnessed by the Shoshone people. Ella E. Clark has recorded a Shoshone legend which speaks of a serpent on a mountain who, angered by lightning, coiled around and squeezed the mountain until liquid rock flowed, fire shot from cracks, and the mountain exploded.
In 1879, two Arco cattlemen named Arthur Ferris and J.W. Powell became the first known European-Americans to explore the lava fields. They were investigating its possible use for grazing and watering cattle but found the area to be unsuitable and left.
U.S. Army Captain and western explorer B.L.E. Bonneville visited the lava fields and other places in the West in the 19th century and wrote about his experiences in his diaries. Washington Irving later used Bonneville's diaries to write the Adventures of Captain Bonneville, saying this unnamed lava field is a place "where nothing meets the eye but a desolate and awful waste, where no grass grows nor water runs, and where nothing is to be seen but lava."
In 1901 and 1903, Israel Russell became the first geologist to study this area while surveying it for the United States Geological Survey (USGS). In 1910, Samuel Paisley continued Russell's work and later became the monument's first custodian. Others followed and in time much of the mystery surrounding this and the other Lava Beds of Idaho was lifted.
The few European settlers who visited the area in the 19th century created local legends that it looked like the surface of the Moon. Geologist Harold T. Stearns coined the name "Craters of the Moon" in 1923 while trying to convince the National Park Service to recommend protection of the area in a national monument.
The Snake River Plain is a volcanic province that was created by a series of cataclysmic caldera-forming eruptions which started about 15 million years ago. A migrating hotspot thought to now exist under Yellowstone Caldera in Yellowstone National Park has been implicated. This hot spot was under the Craters of the Moon area some 10 to 11 million years ago but 'moved' as the North American Plate migrated northwestward. Pressure from the hot spot heaves the land surface up, creating fault-block mountains. After the hot spot passes the pressure is released and the land subsides.
Leftover heat from this hot spot was later liberated by Basin and Range-associated rifting and created the many overlapping lava flows that make up the Lava Beds of Idaho. The largest rift zone is the Great Rift; it is from this 'Great Rift fissure system' that Craters of the Moon, Kings Bowl, and Wapi lava fields were created. The Great Rift is a National Natural Landmark.
In spite of their fresh appearance, the oldest flows in the Craters of the Moon Lava Field are 15,000 years old and the youngest erupted about 2000 years ago, according to Mel Kuntz and other USGS geologists. Nevertheless, the volcanic fissures at Craters of the Moon are considered to be dormant, not extinct, and are expected to erupt again in less than a thousand years. There are eight major eruptive periods recognized in the Craters of the Moon Lava Field. Each period lasted about 1000 years or less and were separated by relatively quiet periods that lasted between 500 and as long as 3000 years. Individual lava flows were up to 30 miles (50 km) long with the Blue Dragon Flow being the longest.
Kings Bowl Lava Field erupted during a single fissure eruption on the southern part of the Great Rift about 2,250 years ago. This eruption probably lasted only a few hours to a few days. The field preserves explosion pits, lava lakes, squeeze-ups, basalt mounds, and an ash blanket. The Wapi Lava Field probably formed from a fissure eruption at the same time as the Kings Bowl eruption. More prolonged activity over a period of months to a few years led to the formation of low shield volcanoes in the Wapi field. The Bear Trap lava tube, between the Craters of the Moon and the Wapi lava fields, is a cave system more than 15 miles (24 km) long. The lava tube is remarkable for its length and for the number of well-preserved lava cave features, such as lava stalactites and curbs, the latter marking high stands of the flowing lava frozen on the lava tube walls. The lava tubes and pit craters of the monument are known for their unusual preservation of winter ice and snow into the hot summer months, due to shielding from the sun and the insulating properties of basalt.
A typical eruption along the Great Rift and similar basaltic rift systems starts with a curtain of very fluid lava shooting up to 1,000 feet (300 m) high along a segment of the rift up to 1 mile (1.6 km) long. As the eruption continues, pressure and heat decrease and the chemistry of the lava becomes slightly more silica rich. The curtain of lava responds by breaking apart into separate vents. Various types of volcanoes may form at these vents: gas-rich pulverized lava creates cinder cones (such as Inferno Cone – stop 4), and pasty lava blobs form spatter cones (such as Spatter Cones – stop 5). Later stages of an eruption push lava streams out through the side or base of cinder cones, which usually ends the life of the cinder cone (North Crater, Watchmen, and Sheep Trail Butte are notable exceptions). This will sometimes breach part of the cone and carry it away as large and craggy blocks of cinder (as seen at North Crater Flow – stop 2 – and Devils Orchard – stop 3). Solid crust forms over lava streams, and lava tubes (a type of cave) are created when lava vacates its course (examples can be seen at the Cave Area – stop 7).
Geologists feared that a large earthquake that shook Borah Peak, Idaho's tallest mountain, in 1983 would restart volcanic activity at Craters of the Moon, though this proved not to be the case. Geologists predict that the area will experience its next eruption some time in the next 900 years with the most likely period in the next 100 years.
All plants and animals that live in and around Craters of the Moon are under great environmental stress due to constant dry winds and heat-absorbing black lavas that tend to quickly sap water from living things. Summer soil temperatures often exceed 150 °F (66 °C) and plant cover is generally less than 5% on cinder cones and about 15% over the entire monument. Adaptation is therefore necessary for survival in this semi-arid harsh climate.
Water is usually only found deep inside holes at the bottom of blow-out craters. Animals therefore get the moisture they need directly from their food. The black soil on and around cinder cones does not hold moisture for long, making it difficult for plants to establish themselves. Soil particles first develop from direct rock decomposition by lichens and typically collect in crevices in lava flows. Successively more complex plants then colonize the microhabitat created by the increasingly productive soil.
The shaded north slopes of cinder cones provide more protection from direct sunlight and prevailing southwesterly winds and have a more persistent snow cover (an important water source in early spring). These parts of cinder cones are therefore colonized by plants first.
Gaps between lava flows were sometimes cut off from surrounding vegetation. These literal islands of habitat are called kīpukas, a Hawaiian name used for older land surrounded by younger lava. Carey Kīpuka is one such area in the southernmost part of the monument and is used as a benchmark to measure how plant cover has changed in less pristine parts of southern Idaho.
Idaho is a landlocked state in the Mountain West subregion of the United States. It shares a small portion of the Canada–United States border to the north, with the province of British Columbia. It borders Montana and Wyoming to the east, Nevada and Utah to the south, and Washington and Oregon to the west. The state's capital and largest city is Boise. With an area of 83,570 square miles (216,400 km2), Idaho is the 14th largest state by land area. With a population of approximately 1.8 million, it ranks as the 13th least populous and the 6th least densely populated of the 50 U.S. states.
For thousands of years, and prior to European colonization, Idaho has been inhabited by native peoples. In the early 19th century, Idaho was considered part of the Oregon Country, an area of dispute between the U.S. and the British Empire. It officially became a U.S. territory with the signing of the Oregon Treaty of 1846, but a separate Idaho Territory was not organized until 1863, instead being included for periods in Oregon Territory and Washington Territory. Idaho was eventually admitted to the Union on July 3, 1890, becoming the 43rd state.
Forming part of the Pacific Northwest (and the associated Cascadia bioregion), Idaho is divided into several distinct geographic and climatic regions. The state's north, the relatively isolated Idaho Panhandle, is closely linked with Eastern Washington, with which it shares the Pacific Time Zone—the rest of the state uses the Mountain Time Zone. The state's south includes the Snake River Plain (which has most of the population and agricultural land), and the southeast incorporates part of the Great Basin. Idaho is quite mountainous and contains several stretches of the Rocky Mountains. The United States Forest Service holds about 38% of Idaho's land, the highest proportion of any state.
Industries significant for the state economy include manufacturing, agriculture, mining, forestry, and tourism. Several science and technology firms are either headquartered in Idaho or have factories there, and the state also contains the Idaho National Laboratory, which is the country's largest Department of Energy facility. Idaho's agricultural sector supplies many products, but the state is best known for its potato crop, which comprises around one-third of the nationwide yield. The official state nickname is the "Gem State."
The history of Idaho is an examination of the human history and social activity within the state of Idaho, one of the United States of America located in the Pacific Northwest area near the west coast of the United States and Canada. Other associated areas include southern Alaska, all of British Columbia, Washington, Oregon, western Montana and northern California and Nevada.
Humans may have been present in Idaho for 16,600 years. Recent findings in Cooper's Ferry along the Salmon River in western Idaho near the town of Cottonwood have unearthed stone tools and animal bone fragments in what may be the oldest evidence of humans in North America. Earlier excavations in 1959 at Wilson Butte Cave near Twin Falls revealed evidence of human activity, including arrowheads, that rank among the oldest dated artifacts in North America. Native American tribes predominant in the area in historic times included the Nez Perce and the Coeur d'Alene in the north; and the Northern and Western Shoshone and Bannock peoples in the south.
Idaho was one of the last areas in the lower 48 states of the US to be explored by people of European descent. The Lewis and Clark expedition entered present-day Idaho on August 12, 1805, at Lemhi Pass. It is believed that the first "European descent" expedition to enter southern Idaho was by a group led in 1811 and 1812 by Wilson Price Hunt, which navigated the Snake River while attempting to blaze an all-water trail westward from St. Louis, Missouri, to Astoria, Oregon. At that time, approximately 8,000 Native Americans lived in the region.
Fur trading led to the first significant incursion of Europeans in the region. Andrew Henry of the Missouri Fur Company first entered the Snake River plateau in 1810. He built Fort Henry on Henry's Fork on the upper Snake River, near modern St. Anthony, Idaho. However, this first American fur post west of the Rocky Mountains was abandoned the following spring.
The British-owned Hudson's Bay Company next entered Idaho and controlled the trade in the Snake River area by the 1820s. The North West Company's interior department of the Columbia was created in June 1816, and Donald Mackenzie was assigned as its head. Mackenzie had previously been employed by Hudson's Bay and had been a partner in the Pacific Fur Company, financed principally by John Jacob Astor. During these early years, he traveled west with a Pacific Fur Company's party and was involved in the initial exploration of the Salmon River and Clearwater River. The company proceeded down the lower Snake River and Columbia River by canoe, and were the first of the Overland Astorians to reach Fort Astoria, on January 18, 1812.
Under Mackenzie, the North West Company was a dominant force in the fur trade in the Snake River country. Out of Fort George in Astoria, Mackenzie led fur brigades up the Snake River in 1816-1817 and up the lower Snake in 1817-1818. Fort Nez Perce, established in July, 1818, became the staging point for Mackenzies' Snake brigades. The expedition of 1818-1819 explored the Blue Mountains, and traveled down the Snake River to the Bear River and approached the headwaters of the Snake. Mackenzie sought to establish a navigable route up the Snake River from Fort Nez Perce to the Boise area in 1819. While he did succeed in traveling by boat from the Columbia River through the Grand Canyon of the Snake past Hells Canyon, he concluded that water transport was generally impractical. Mackenzie held the first rendezvous in the region on the Boise River in 1819.
Despite their best efforts, early American fur companies in this region had difficulty maintaining the long-distance supply lines from the Missouri River system into the Intermountain West. However, Americans William H. Ashley and Jedediah Smith expanded the Saint Louis fur trade into Idaho in 1824. The 1832 trapper's rendezvous at Pierre's Hole, held at the foot of the Three Tetons in modern Teton County, was followed by an intense battle between the Gros Ventre and a large party of American trappers aided by their Nez Perce and Flathead allies.
The prospect of missionary work among the Native Americans also attracted early settlers to the region. In 1809, Kullyspell House, the first white-owned establishment and first trading post in Idaho, was constructed. In 1836, the Reverend Henry H. Spalding established a Protestant mission near Lapwai, where he printed the Northwest's first book, established Idaho's first school, developed its first irrigation system, and grew the state's first potatoes. Narcissa Whitman and Eliza Hart Spalding were the first non-native women to enter present-day Idaho.
Cataldo Mission, the oldest standing building in Idaho, was constructed at Cataldo by the Coeur d'Alene and Catholic missionaries. In 1842, Father Pierre-Jean De Smet, with Fr. Nicholas Point and Br. Charles Duet, selected a mission location along the St. Joe River. The mission was moved a short distance away in 1846, as the original location was subject to flooding. In 1850, Antonio Ravalli designed a new mission building and Indians affiliated with the church effort built the mission, without nails, using the wattle and daub method. In time, the Cataldo mission became an important stop for traders, settlers, and miners. It served as a place for rest from the trail, offered needed supplies, and was a working port for boats heading up the Coeur d'Alene River.
During this time, the region which became Idaho was part of an unorganized territory known as Oregon Country, claimed by both the United States and Great Britain. The United States gained undisputed jurisdiction over the region in the Oregon Treaty of 1846, although the area was under the de facto jurisdiction of the Provisional Government of Oregon from 1843 to 1849. The original boundaries of Oregon Territory in 1848 included all three of the present-day Pacific Northwest states and extended eastward to the Continental Divide. In 1853, areas north of the 46th Parallel became Washington Territory, splitting what is now Idaho in two. The future state was reunited in 1859 after Oregon became a state and the boundaries of Washington Territory were redrawn.
While thousands passed through Idaho on the Oregon Trail or during the California gold rush of 1849, few people settled there. In 1860, the first of several gold rushes in Idaho began at Pierce in present-day Clearwater County. By 1862, settlements in both the north and south had formed around the mining boom.
The Church of Jesus Christ of Latter-Day Saints missionaries founded Fort Lemhi in 1855, but the settlement did not last. The first organized town in Idaho was Franklin, settled in April 1860 by Mormon pioneers who believed they were in Utah Territory; although a later survey determined they had crossed the border. Mormon pioneers reached areas near the current-day Grand Teton National Park in Wyoming and established most of the historic and modern communities in Southeastern Idaho. These settlements include Ammon, Blackfoot, Chubbuck, Firth, Idaho Falls, Iona, Pocatello, Rexburg, Rigby, Shelley, and Ucon.
Large numbers of English immigrants settled in what is now the state of Idaho in the late 19th and early 20th century, many before statehood. The English found they had more property rights and paid less taxes than they did back in England. They were considered some of the most desirable immigrants at the time. Many came from humble beginnings and would rise to prominence in Idaho. Frank R. Gooding was raised in a rural working-class background in England, but was eventually elected as the seventh governor of the state. Today people of English descent make up one fifth of the entire state of Idaho and form a plurality in the southern portion of the state.
Many German farmers also settled in what is now Idaho. German settlers were primarily Lutheran across all of the midwest and west, including Idaho, however there were small numbers of Catholics amongst them as well. In parts of Northern Idaho, German remained the dominant language until World War I, when German-Americans were pressured to convert entirely to English. Today, Idahoans of German ancestry make up nearly one fifth of all Idahoans and make up the second largest ethnic group after Idahoans of English descent with people of German ancestry being 18.1% of the state and people of English ancestry being 20.1% of the state.
Irish Catholics worked in railroad centers such as Boise. Today, 10% of Idahoans self-identify as having Irish ancestry.
York, a slave owned by William Clark but considered a full member of Corps of Discovery during expedition to the Pacific, was the first recorded African American in Idaho. There is a significant African American population made up of those who came west after the abolition of slavery. Many settled near Pocatello and were ranchers, entertainers, and farmers. Although free, many blacks suffered discrimination in the early-to-mid-late 20th century. The black population of the state continues to grow as many come to the state because of educational opportunities, to serve in the military, and for other employment opportunities. There is a Black History Museum in Boise, Idaho, with an exhibit known as the "Invisible Idahoan", which chronicles the first African-Americans in the state. Blacks are the fourth largest ethnic group in Idaho according to the 2000 census. Mountain Home, Boise, and Garden City have significant African-American populations.
The Basque people from the Iberian peninsula in Spain and southern France were traditionally shepherds in Europe. They came to Idaho, offering hard work and perseverance in exchange for opportunity. One of the largest Basque communities in the US is in Boise, with a Basque museum and festival held annually in the city.
Chinese in the mid-19th century came to America through San Francisco to work on the railroad and open businesses. By 1870, there were over 4000 Chinese and they comprised almost 30% of the population. They suffered discrimination due to the Anti-Chinese League in the 19th century which sought to limit the rights and opportunities of Chinese emigrants. Today Asians are third in population demographically after Whites and Hispanics at less than 2%.
Main articles: Oregon boundary dispute, Provisional Government of Oregon, Oregon Treaty, Oregon Territory, Washington Territory, Dakota Territory, Organic act § List of organic acts, and Idaho Territory
On March 4, 1863, President Abraham Lincoln signed an act creating Idaho Territory from portions of Washington Territory and Dakota Territory with its capital at Lewiston. The original Idaho Territory included most of the areas that later became the states of Idaho, Montana and Wyoming, and had a population of under 17,000. Idaho Territory assumed the boundaries of the modern state in 1868 and was admitted as a state in 1890.
After Idaho became a territory, legislation was held in Lewiston, the capital of Idaho Territory at the time. There were many territories acts put into place, and then taken away during these early sessions, one act being the move of the capital city from Lewiston to Boise City. Boise was becoming a growing area after gold was found, so on December 24, 1864, Boise City was made the final destination of the capital for the Territory of Idaho.
However, moving the capital to Boise City created a lot of issues between the territory. This was especially true between the north and south areas in the territory, due to how far south Boise City was. Problems with communicating between the north and south contributed to some land in Idaho Territory being transferred to other territories and areas at the time. Idaho’s early boundary changes helped create the current boundaries of Washington, Wyoming, and Montana States as currently exist.
In a bid for statehood, Governor Edward A. Stevenson called for a constitutional convention in 1889. The convention approved a constitution on August 6, 1889, and voters approved the constitution on November 5, 1889.
When President Benjamin Harrison signed the law admitting Idaho as a U.S. state on July 3, 1890, the population was 88,548. George L. Shoup became the state's first governor, but resigned after only a few weeks in office to take a seat in the United States Senate. Willis Sweet, a Republican, was the first congressman, 1890 to 1895, representing the state at-large. He vigorously demanded "Free Silver" or the unrestricted coinage of silver into legal tender, in order to pour money into the large silver mining industry in the Mountain West, but he was defeated by supporters of the gold standard. In 1896 he, like many Republicans from silver mining districts, supported the Silver Republican Party instead of the regular Republican nominee William McKinley.
During its first years of statehood, Idaho was plagued by labor unrest in the mining district of Coeur d'Alene. In 1892, miners called a strike which developed into a shooting war between union miners and company guards. Each side accused the other of starting the fight. The first shots were exchanged at the Frisco mine in Frisco, in the Burke-Canyon north and east of Wallace. The Frisco mine was blown up, and company guards were taken prisoner. The violence soon spilled over into the nearby community of Gem, where union miners attempted to locate a Pinkerton spy who had infiltrated their union and was passing information to the mine operators. But agent Charlie Siringo escaped by cutting a hole in the floor of his room. Strikers forced the Gem mine to close, then traveled west to the Bunker Hill mining complex near Wardner, and closed down that facility as well. Several had been killed in the Burke-Canyon fighting. The Idaho National Guard and federal troops were dispatched to the area, and union miners and sympathizers were thrown into bullpens.
Hostilities would again erupt at the Bunker Hill facility in 1899, when seventeen union miners were fired for having joined the union. Other union miners were likewise ordered to draw their pay and leave. Angry members of the union converged on the area and blew up the Bunker Hill Mill, killing two company men.
In both disputes, the union's complaints included pay, hours of work, the right of miners to belong to the union, and the mine owners' use of informants and undercover agents. The violence committed by union miners was answered with a brutal response in 1892 and in 1899.
Through the Western Federation of Miners (WFM) union, the battles in the mining district became closely tied to a major miners' strike in Colorado. The struggle culminated in the December 1905 assassination of former Governor Frank Steunenberg by Harry Orchard (also known as Albert Horsley), a member of the WFM. Orchard was allegedly incensed by Steunenberg's efforts as governor to put down the 1899 miner uprising after being elected on a pro-labor platform.
Pinkerton detective James McParland conducted the investigation into the assassination. In 1907, WFM Secretary Treasurer "Big Bill" Haywood and two other WFM leaders were tried on a charge of conspiracy to murder Steunenberg, with Orchard testifying against them as part of a deal made with McParland. The nationally publicized trial featured Senator William E. Borah as prosecuting attorney and Clarence Darrow representing the defendants. The defense team presented evidence that Orchard had been a Pinkerton agent and had acted as a paid informant for the Cripple Creek Mine Owners' Association. Darrow argued that Orchard's real motive in the assassination had been revenge for a declaration of martial law by Steunenberg, which prompted Orchard to gamble away a share in the Hercules silver mine that would otherwise have made him wealthy.
Two of the WFM leaders were acquitted in two separate trials, and the third was released. Orchard was convicted and sentenced to death. His sentence was commuted, and he spent the rest of his life in an Idaho prison.
Mining in Idaho was a major commercial venture, bringing a great deal of attention to the state. From 1860-1866 Idaho produced 19% of all gold in the United States, or 2.5 million ounces.
Most of Idaho's mining production, 1860–1969, has come from metals equating to $2.88 billion out of $3.42 billion, according to the best estimates. Of the metallic mining areas of Idaho, the Coeur d'Alene region has produced the most by far, and accounts for about 80% of the total Idaho yield.
Several others—Boise Basin, Wood River Valley, Stibnite, Blackbirg, and Owyhee—range considerably above the other big producers. Atlanta, Bear Valley, Bay Horse, Florence, Gilmore, Mackay, Patterson, and Yankee Fork all ran on the order of ten to twenty million dollars, and Elk City, Leesburg, Pierce, Rocky Bar, and Warren's make up the rest of the major Idaho mining areas that stand out in the sixty or so regions of production worthy of mention.
A number of small operations do not appear in this list of Idaho metallic mining areas: a small amount of gold was recovered from Goose Creek on Salmon Meadows; a mine near Cleveland was prospected in 1922 and produced a little manganese in 1926; a few tons of copper came from Fort Hall, and a few more tons of copper came from a mine near Montpelier. Similarly, a few tons of lead came from a property near Bear Lake, and lead-silver is known on Cassia Creek near Elba. Some gold quartz and lead-silver workings are on Ruby Creek west of Elk River, and there is a slightly developed copper operation on Deer Creek near Winchester. Molybdenum is known on Roaring River and on the east fork of the Salmon. Some scattered mining enterprises have been undertaken around Soldier Mountain and on Chief Eagle Eye Creek north of Montour.
Idaho proved to be one of the more receptive states to the progressive agenda of the late 19th century and early 20th century. The state embraced progressive policies such as women's suffrage (1896) and prohibition (1916) before they became federal law. Idahoans were also strongly supportive of Free Silver. The pro-bimetallism Populist and Silver Republican parties of the late 1890s were particularly successful in the state.
Eugenics was also a major part of the Progressive movement. In 1919, the Idaho legislature passed an Act legalizing the forced sterilization of some persons institutionalized in the state. The act was vetoed by governor D.W. Davis, who doubted its scientific merits and believed it likely violated the Equal Protection clause of the US Constitution. In 1925, the Idaho legislature passed a revised eugenics act, now tailored to avoid Davis's earlier objections. The new law created a state board of eugenics, charged with: the sterilization of all feebleminded, insane, epileptics, habitual criminals, moral degenerates and sexual perverts who are a menace to society, and providing the means for ascertaining who are such persons.
The Eugenics board was eventually folded into the state's health commission; between 1932 and 1964, a total of 30 women and eight men in Idaho were sterilized under this law. The sterilization law was formally repealed in 1972.
After statehood, Idaho's economy began a gradual shift away from mining toward agriculture, particularly in the south. Older mining communities such as Silver City and Rocky Bar gave way to agricultural communities incorporated after statehood, such as Nampa and Twin Falls. Milner Dam on the Snake River, completed in 1905, allowed for the formation of many agricultural communities in the Magic Valley region which had previously been nearly unpopulated.
Meanwhile, some of the mining towns were able to reinvent themselves as resort communities, most notably in Blaine County, where the Sun Valley ski resort opened in 1936. Others, such as Silver City and Rocky Bar, became ghost towns.
In the north, mining continued to be an important industry for several more decades. The closure of the Bunker Hill Mine complex in Shoshone County in the early 1980s sent the region's economy into a tailspin. Since that time, a substantial increase in tourism in north Idaho has helped the region to recover. Coeur d'Alene, a lake-side resort town, is a destination for visitors in the area.
Beginning in the 1980s, there was a rise in North Idaho of a few right-wing extremist and "survivalist" political groups, most notably one holding Neo-Nazi views, the Aryan Nations. These groups were most heavily concentrated in the Panhandle region of the state, particularly in the vicinity of Coeur d'Alene.
In 1992 a stand-off occurred between U.S. Marshals, the F.B.I., and white separatist Randy Weaver and his family at their compound at Ruby Ridge, located near the small, northern Idaho town of Naples. The ensuing fire-fight and deaths of a U.S. Marshal, and Weaver's son and wife gained national attention, and raised a considerable amount of controversy regarding the nature of acceptable force by the federal government in such situations.
In 2001, the Aryan Nations compound, which had been located in Hayden Lake, Idaho, was confiscated as a result of a court case, and the organization moved out of state. About the same time Boise installed an impressive stone Human Rights Memorial featuring a bronze statue of Anne Frank and quotations from her and many other writers extolling human freedom and equality.
The demographics of the state have changed. Due to this growth in different groups, especially in Boise, the economic expansion surged wrong-economic growth followed the high standard of living and resulted in the "growth of different groups". The population of Idaho in the 21st Century has been described as sharply divided along geographic and cultural lines due to the center of the state being dominated by sparsely-populated national forests, mountain ranges and recreation sites: "unless you're willing to navigate a treacherous mountain pass, you can't even drive from the north to the south without leaving the state." The northern population gravitates towards Spokane, Washington, the heavily Mormon south-east population towards Utah, with an isolated Boise "[being] the closest thing to a city-state that you'll find in America."
On March 13, 2020, officials from the Idaho Department of Health and Welfare announced the first confirmed case of the novel coronavirus COVID-19 within the state of Idaho. A woman over the age of 50 from the southwestern part of the state was confirmed to have the coronavirus infection. She contracted the infection while attending a conference in New York City. Conference coordinators notified attendees that three individuals previously tested positive for the coronavirus. The Idahoan did not require hospitalization and was recovering from mild symptoms from her home. At the time of the announcement, there were 1,629 total cases and 41 deaths in the United States. Five days beforehand, on March 8, a man of age 54 had died of an unknown respiratory illness which his doctor had believed to be pneumonia. The disease was later suspected to be – but never confirmed as – COVID-19.
On March 14, state officials announced the second confirmed case within the state. The South Central Public Health District, announced that a woman over the age of 50 that resides in Blaine County had contracted the infection.[44] Like the first case, she did not require hospitalization and she was recovering from mild symptoms from home. Later on in the day, three additional confirmed cases of COVID-19 were reported in the state by three of the seven health districts in the state, which brought the confirmed total cases of coronavirus to five in Idaho. Officials from Central District Health announced their second confirmed case, which was a male from Ada County in his 50s. He was not hospitalized and was recovering at home. South Central Public Health reported their second confirmed case in a female that is over the age of 70 who was hospitalized. Eastern Idaho Public Health reported a confirmed positive case in a woman under the age of 60 in Teton County. She had contracted the coronavirus from contact with a confirmed case in a neighboring state; she was not hospitalized. The South Central Public Health District announced that a woman over the age of 50 that resides in Blaine County had contracted the infection. Like the first case, she did not require hospitalization and she was recovering from mild symptoms from home.
On March 17, two more confirmed cases of the infection were reported, bringing the total to seven. The first case on this date was by officials from Central District Health reported that a female under the age of 50 in Ada County was recovering at home and was not hospitalized. The second confirmed case was a female over the age of 50 as reported by South Central Public Health officials.
On March 18, two additional confirmed cases were announced by South Central Public Health District officials. One is a male from Blaine County in his 40s and the other a male in his 80s from Twin Falls County. These cases were the first known community spread transmission of the coronavirus in South Central Idaho.