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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.

View On Black

Zion National Park is an American national park located in southwestern Utah near the town of Springdale. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park has a unique geography and a variety of life zones that allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches. The lowest point in the park is 3,666 ft (1,117 m) at Coalpits Wash and the highest peak is 8,726 ft (2,660 m) at Horse Ranch Mountain. A prominent feature of the 229-square-mile (590 km2) park is Zion Canyon, which is 15 miles (24 km) long and up to 2,640 ft (800 m) deep. The canyon walls are reddish and tan-colored Navajo Sandstone eroded by the North Fork of the Virgin River.

 

Human habitation of the area started about 8,000 years ago with small family groups of Native Americans, one of which was the semi-nomadic Basketmaker Ancestral Puebloans (who used to be called Anasazi by early non-indigenous archeologists)(c. 300 CE). Subsequently, what has been called the Virgin Anasazi culture (c. 500) and the Parowan Fremont group developed as the Basketmakers settled in permanent communities. Both groups moved away by 1300 and were replaced by the Parrusits and several other Southern Paiute subtribes. Mormons came into the area in 1858 and settled there in the early 1860s.

 

In 1909, President William Howard Taft named the area Mukuntuweap National Monument in order to protect the canyon. In 1918, the acting director of the newly created National Park Service, Horace Albright, drafted a proposal to enlarge the existing monument and change the park's name to Zion National Monument, Zion being a term used by the Mormons. According to historian Hal Rothman: "The name change played to a prevalent bias of the time. Many believed that Spanish and Indian names would deter visitors who, if they could not pronounce the name of a place, might not bother to visit it. The new name, Zion, had greater appeal to an ethnocentric audience." On November 19, 1919, Congress redesignated the monument as Zion National Park, and the act was signed by President Woodrow Wilson. The Kolob section was proclaimed a separate Zion National Monument in 1937, but was incorporated into the national park in 1956. Congress designated 85% of the park a wilderness area in 2009.

 

The geology of the Zion and Kolob canyons area includes nine formations that together represent 150 million years of mostly Mesozoic-aged sedimentation. At various periods in that time warm, shallow seas, streams, ponds and lakes, vast deserts, and dry near-shore environments covered the area. Uplift associated with the creation of the Colorado Plateau lifted the region 10,000 feet (3,000 m) starting 13 million years ago.

 

As stated in the foundation document:

 

The purpose of Zion National Park is to preserve the dramatic geology including Zion Canyon and a labyrinth of deep and brilliantly colored Navajo sandstone canyons formed by extraordinary processes of erosion at the margin of the Colorado Plateau; to safeguard the park's wilderness character and its wild and scenic river values; to protect evidence of human history; and to provide for scientific research and the enjoyment and enlightenment of the public.

 

The park is located in southwestern Utah in Washington, Iron and Kane counties. Geomorphically, it is located on the Markagunt and Kolob plateaus, at the intersection of three North American geographic provinces: the Colorado Plateau, the Great Basin, and the Mojave Desert. The northern part of the park is known as the Kolob Canyons section and is accessible from Interstate 15, exit 40.

 

The 8,726-foot (2,660 m) summit of Horse Ranch Mountain is the highest point in the park; the lowest point is the 3,666-foot (1,117 m) elevation of Coal Pits Wash, creating a relief of about 5,100 feet (1,600 m).

 

Streams in the area take rectangular paths because they follow jointing planes in the rocks. The stream gradient of the Virgin River, whose North Fork flows through Zion Canyon in the park, ranges from 50 to 80 feet per mile (9.5 to 15.2 m/km) (0.9–1.5%)—one of the steepest stream gradients in North America.

 

The road into Zion Canyon is 6 miles (9.7 km) long, ending at the Temple of Sinawava, which is named for the coyote god of the Paiute Indians. The canyon becomes more narrow near the Temple and a hiking trail continues to the mouth of The Narrows, a gorge only 20 feet (6 m) wide and up to 2,000 feet (610 m) tall. The Zion Canyon road is served by a free shuttle bus from early April to late October and by private vehicles the other months of the year. Other roads in Zion are open to private vehicles year-round.

 

The east side of the park is served by Zion-Mount Carmel Highway (SR-9), which passes through the Zion–Mount Carmel Tunnel and ends at US 89 at Mount Carmel Junction. Park features on the east side of the park include Checkerboard Mesa and The East Temple.

 

The Kolob Terrace area, northwest of Zion Canyon, features a slot canyon called The Subway, and a panoramic view of the entire area from Lava Point. The Kolob Canyons section, further to the northwest near Cedar City, features Tucupit Point and one of the world's longest natural arches, Kolob Arch.

 

Other notable geographic features of Zion Canyon include Angels Landing, The Great White Throne, the Court of the Patriarchs, The Sentinel, The West Temple, Towers of the Virgin, the Altar of Sacrifice, The Watchman, Weeping Rock, and the Emerald Pools.

 

Spring weather is unpredictable, with stormy, wet days being common, mixed with occasional warm, sunny weather. Precipitation is normally heaviest in March. Spring wildflowers bloom from April through June, peaking in May. Fall days are usually clear and mild; nights are often cool. Summer days are hot (95 to 110 °F; 35 to 43 °C), but overnight lows are usually comfortable (65 to 70 °F; 18 to 21 °C). Afternoon thunderstorms are common from mid-July through mid-September. Storms may produce waterfalls as well as flash floods. Autumn tree-color displays begin in September in the high country; in Zion Canyon, autumn colors usually peak in late October. Winter in Zion Canyon is fairly mild. Winter storms bring rain or light snow to Zion Canyon and heavier snow to the higher elevations. Clear days may become quite warm, reaching 60 °F (16 °C); nights are often 20 to 40 °F (−7 to 4 °C). Winter storms can last several days and make roads icy. Zion roads are plowed, except the Kolob Terrace Road which is closed when covered with snow. Winter driving conditions last from November through March.

 

Archaeologists have divided the long span of Zion's human history into three cultural periods: the Archaic, Protohistoric and Historic periods. Each period is characterized by distinctive technological and social adaptations.

 

Archaic period

The first human presence in the region dates to 8,000 years ago when family groups camped where they could hunt or collect plants and seeds. About 2,000 years ago, some groups began growing corn and other crops, leading to an increasingly sedentary lifestyle. Later groups in this period built permanent villages called pueblos. Archaeologists call this the Archaic period and it lasted until c. 500. Baskets, cordage nets, and yucca fiber sandals have been found and dated to this period. The Archaic toolkits included flaked stone knives, drills, and stemmed dart points. The dart points were attached to wooden shafts and propelled by throwing devices called atlatls.

 

By c. 300, some of the archaic groups developed into an early branch of seminomadic Anasazi, the Basketmakers. Basketmaker sites have grass- or stone-lined storage cists and shallow, partially underground dwellings called pithouses. They were hunters and gatherers who supplemented their diet with limited agriculture. Locally collected pine nuts were important for food and trade.

 

Both the Virgin Anasazi and the Parowan Fremont disappeared from the archaeological record of southwestern Utah by c. 1300. Extended droughts in the 11th and 12th centuries, interspersed with catastrophic flooding, may have made horticulture impossible in this arid region.

 

Tradition and archaeological evidence hold that their replacements were Numic-speaking cousins of the Virgin Anasazi, such as the Southern Paiute and Ute. The newcomers migrated on a seasonal basis up and down valleys in search of wild seeds and game animals. Some, particularly the Southern Paiute, also planted fields of corn, sunflowers, and squash to supplement their diet. These more sedentary groups made brownware vessels that were used for storage and cooking.

 

The Historic period begins in the late 18th century with the exploration of southern Utah by padre Silvestre Vélez de Escalante and padre Francisco Atanasio Domínguez. The padres passed near what is now the Kolob Canyons Visitor Center on October 13, 1776, becoming the first people of European descent known to visit the area. In 1825, trapper and trader Jedediah Smith explored some of the downstream areas while under contract with the American Fur Company.

 

In 1847, Mormon farmers from the Salt Lake area became the first people of European descent to settle the Virgin River region. In 1851, the Parowan and Cedar City areas were settled by Mormons who used the Kolob Canyons area for timber, and for grazing cattle, sheep, and horses. They prospected for mineral deposits, and diverted Kolob water to irrigate crops in the valley below. Mormon settlers named the area Kolob which in Mormon scripture is the heavenly place nearest the residence of God.

 

Settlements had expanded 30 miles (48 km) south to the lower Virgin River by 1858. That year, a Southern Paiute guide led young Mormon missionary and interpreter Nephi Johnson into the upper Virgin River area and Zion Canyon.[28] Johnson wrote a favorable report about the agricultural potential of the upper Virgin River basin, and returned later that year to found the town of Virgin. In 1861 or 1862, Joseph Black made the arduous journey to Zion Canyon and was very impressed by its beauty.

 

The floor of Zion Canyon was settled in 1863 by Isaac Behunin, who farmed corn, tobacco, and fruit trees. The Behunin family lived in Zion Canyon near the site of today's Zion Lodge during the summer, and wintered in Springdale. Behunin is credited with naming Zion, a reference to the place of peace mentioned in the Bible. Two more families settled Zion Canyon in the next couple of years, bringing with them cattle and other domesticated animals. The canyon floor was farmed until Zion became a Monument in 1909.

 

The Powell Geographic Expedition of 1869 entered the area after their first trip through the Grand Canyon. John Wesley Powell visited Zion Canyon in 1872 and named it Mukuntuweap, under the impression that that was the Paiute name. Powell Survey photographers John K. Hillers and James Fennemore first visited the Zion Canyon and Kolob Plateau region in the spring of 1872. Hillers returned in April 1873 to add more photographs to the "Virgin River Series" of photographs and stereographs. Hillers described wading the canyon for four days and nearly freezing to death to take his photographs.

 

Paintings of the canyon by Frederick S. Dellenbaugh were exhibited at the Saint Louis World's Fair in 1904, followed by a favorable article in Scribner's Magazine the next year. The article and paintings, along with previously created photographs, paintings, and reports, led to President William Howard Taft's proclamation on July 31, 1909, that created Mukuntuweap National Monument. In 1917, the acting director of the newly created National Park Service visited the canyon and proposed changing its name from the locally unpopular Mukuntuweap to Zion, a name used by the local Mormon community. The United States Congress added more land and established Zion National Park on November 19, 1919. A separate Zion National Monument, the Kolob Canyons area, was proclaimed on January 22, 1937, and was incorporated into the park on July 11, 1956.

 

Travel to the area before it was a national park was rare due to its remote location, lack of accommodations, and the absence of real roads in southern Utah. Old wagon roads were upgraded to the first automobile roads starting about 1910, and the road into Zion Canyon was built in 1917 leading to the Grotto, short of the present road that now ends at the Temple of Sinawava.

 

Touring cars could reach Zion Canyon by the summer of 1917. The first visitor lodging in Zion Canyon, called Wylie Camp, was established that same year as a tent camp. The Utah Parks Company, a subsidiary of the Union Pacific Railroad, acquired Wylie Camp in 1923, and offered ten-day rail/bus tours to Zion, nearby Bryce Canyon, the Kaibab Plateau, and the North Rim of the Grand Canyon. The Zion Lodge complex was built in 1925 at the site of the Wylie tent camp. Architect Gilbert Stanley Underwood designed the Zion Lodge in a rustic architectural style, while the Utah Parks Company funded the construction.

 

Work on the Zion Mount Carmel Highway started in 1927 to enable reliable access between Springdale and the east side of the park. The road opened in 1930 and park visit and travel in the area greatly increased. The most famous feature of the Zion – Mount Carmel Highway is its 1.1-mile (1.8 km) tunnel, which has six large windows cut through the massive sandstone cliff.

 

In 1896, local rancher John Winder improved the Native American footpath up Echo Canyon, which later became the East Rim Trail. Entrepreneur David Flanigan used this trail in 1900 to build cableworks that lowered lumber into Zion Canyon from Cable Mountain. More than 200,000 board feet (470 m3) of lumber were lowered by 1906. The auto road was extended to the Temple of Sinawava, and a trail built from there 1 mile (1.6 km) to the start of the Narrows. Angel's Landing Trail was constructed in 1926 and two suspension bridges were built over the Virgin River. Other trails were constructed by the Civilian Conservation Corps during the 1930s.

 

Zion National Park has been featured in numerous films, including The Deadwood Coach (1924), Arizona Bound (1927), Nevada (1927), Ramrod (1947) and Butch Cassidy and the Sundance Kid (1969).

 

Zion Canyon Scenic Drive provides access to Zion Canyon. Traffic congestion in the narrow canyon was recognized as a major problem in the 1990s and a public transportation system using propane-powered shuttle buses was instituted in the year 2000. As part of its shuttle fleet, Zion has two electric trams each holding up to 36 passengers. Usually from early April through late October, the scenic drive in Zion Canyon is closed to private vehicles and visitors ride the shuttle buses. The National Park Service has contracted the management of the shuttle bus system to transit operator RATP Dev.

 

On April 12, 1995, heavy rains triggered a landslide that blocked the Virgin River in Zion Canyon. Over a period of two hours, the river carved away part of the only exit road from the canyon, trapping 450 guests and employees at the Zion Lodge. A one-lane, temporary road was constructed within 24 hours to allow evacuation of the Lodge. A more stable albeit temporary road was completed on May 25, 1995, to allow summer visitors to access the canyon. This road was replaced with a permanent road during the first half of 1996.

 

The Zion–Mount Carmel Highway can be travelled year-round. Access for oversized vehicles requires a special permit, and is limited to daytime hours, as traffic through the tunnel must be one way to accommodate large vehicles. The 5-mile (8.0 km)-long Kolob Canyons Road was built to provide access to the Kolob Canyons section of the park. This road often closes in the winter.

 

In March 2009, President Barack Obama signed into law the Omnibus Public Land Management Act of 2009, which designated and further protected 124,406 acres (50,345 ha) of park land, about 85% of the park, as the Zion Wilderness.

 

In September 2015, flooding trapped a party of seven in Keyhole Canyon, a slot canyon in the park. The flash flood killed all seven members of the group, whose remains were located after a search lasting several days.

 

In 2017, some scenes from the TV series Extinct were shot in the park.

 

The nine known exposed geologic formations in Zion National Park are part of a super-sequence of rock units called the Grand Staircase. Together, these formations represent about 150 million years of mostly Mesozoic-aged sedimentation in that part of North America. The formations exposed in the Zion area were deposited as sediment in very different environments:

 

The warm, shallow (sometimes advancing or retreating) sea of the Kaibab and Moenkopi formations

Streams, ponds, and lakes of the Chinle, Moenave, and Kayenta formations

The vast desert of the Navajo and Temple Cap formations

The dry near-shore environment of the Carmel Formation

 

Uplift affected the entire region, known as the Colorado Plateaus, by slowly raising these formations more than 10,000 feet (3,000 m) higher than where they were deposited. This steepened the stream gradient of the ancestral Virgin and other rivers on the plateau.

 

The faster-moving streams took advantage of uplift-created joints in the rocks. Eventually, all Cenozoic-aged formations were removed and gorges were cut into the plateaus. Zion Canyon was cut by the North Fork of the Virgin River in this way. During the later part of this process, lava flows and cinder cones covered parts of the area.

 

High water volume in wet seasons does most of the downcutting in the main canyon. These flood events are responsible for transporting most of the 3 million short tons (2.7 million metric tons) of rock and sediment that the Virgin River transports yearly. The Virgin cuts away its canyon faster than its tributaries can cut away their own streambeds, so tributaries end in waterfalls from hanging valleys where they meet the Virgin. The valley between the peaks of the Twin Brothers is a notable example of a hanging valley in the canyon.

 

The Great Basin, Mojave Desert, and Colorado Plateau converge at Zion and the Kolob canyons. This, along with the varied topography of canyon–mesa country, differing soil types, and uneven water availability, provides diverse habitat for the equally diverse mix of plants and animals that live in the area. The park is home to 289 bird, 79 mammals, 28 reptiles, 7 fish, and 6 amphibian species. These organisms make their homes in one or more of four life zones found in the park: desert, riparian, woodland, and coniferous forest.

 

Desert conditions persist on canyon bottoms and rocky ledges away from perennial streams. Sagebrush, prickly pear cactus, and rabbitbrush, along with sacred datura and Indian paintbrush, are common. Utah penstemon and golden aster can also be found. Milkvetch and prince's plume are found in pockets of selenium-rich soils.

 

Common daytime animals include mule deer, rock squirrels, pinyon jays, and whiptail and collared lizards. Desert cottontails, jackrabbits, and Merriam's kangaroo rats come out at night. Cougars, bobcats, coyotes, badgers, gray foxes, and ring-tail cats are the top predators.

 

Cooler conditions persist at mid-elevation slopes, from 3,900 to 5,500 feet (1,200 to 1,700 m). Stunted forests of pinyon pine and juniper coexist here with manzanita shrubs, cliffrose, serviceberry, scrub oak, and yucca. Stands of ponderosa pine, Gambel oak, manzanita and aspen populate the mesas and cliffs above 6,000 feet (1,800 m).

 

Golden eagles, red-tailed hawks, peregrine falcons, and white-throated swifts can be seen in the area. Desert bighorn sheep were reintroduced in the park in 1973. California condors were reintroduced in the Arizona Strip and in 2014 the first successful breeding of condors in the park was confirmed. Nineteen species of bat also live in the area.

 

Boxelder, Fremont cottonwood, maple, and willow dominate riparian plant communities. Animals such as bank beavers, flannel-mouth suckers, gnatcatchers, dippers, canyon wrens, the virgin spinedace, and water striders all make their homes in the riparian zones.

 

Activities

Rangers at the visitor centers in Zion Canyon and Kolob Canyons can help visitors plan their stay. Guided horseback riding trips, nature walks, and evening programs are available from late March to early November. The Junior Ranger Program for children ages 4 and up is active year-round at the Nature Center, Human History Museum, and the visitor centers.[65] A bookstore attached to the Zion Canyon visitor center offers books, maps, and souvenirs. The Grotto in Zion Canyon, the visitor center, and the viewpoint at the end of Kolob Canyons Road have the only designated picnic sites.

 

Seven trails with round-trip times of half an hour (Weeping Rock) to 4 hours (Angels Landing) are found in Zion Canyon. Two popular trails, Taylor Creek (4 hours round trip) and Kolob Arch (8 hours round trip), are in the Kolob Canyons section of the park, near Cedar City. Hiking up into The Narrows from the Temple of Sinawava is popular in summer, but hiking beyond Big Springs requires a permit. The entire Narrows from Chamberlain's Ranch is a 16-mile one way trip that typically takes 12 hours of strenuous hiking. A shorter alternative is to enter the Narrows via Orderville Canyon. Both Orderville and the full Narrows require a back country permit. Entrance to the Parunuweap Canyon section of the park downstream of Labyrinth Falls is prohibited. Other often-used backcountry trails include the West Rim and LaVerkin Creek. The more primitive sections of Zion include the Kolob Terrace and the Kolob Canyons. A network of trails totaling 50 miles in distance connect Zion's northwest corner of the park (Lee Pass Trailhead) to its southeast section (East Rim Trailhead). Popularly known as the Zion Traverse, the route offers backpackers a diverse experience of the park.

 

Zion is a center for rock climbing, with short walls like Spaceshot, Moonlight Buttress, Prodigal Son, Ashtar Command, and Touchstone being the most popular, highly rated routes.

 

Lodging in the park is available at Zion Lodge, located halfway through Zion Canyon. Just outside the park more lodging is available in Springdale.

 

Zion has three campgrounds: South and Watchman at the far southern side of the park, and a primitive site at Lava Point in the middle of the park off Kolob Terrace Road. Overnight camping in the backcountry requires permits.

 

Utah is a landlocked state in the Mountain West subregion of the Western United States. It borders Colorado to its east, Wyoming to its northeast, Idaho to its north, Arizona to its south, and Nevada to its west. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin.

 

Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo, and Ute. The Spanish were the first Europeans to arrive in the mid-16th century, though the region's difficult geography and harsh climate made it a peripheral part of New Spain and later Mexico. Even while it was Mexican territory, many of Utah's earliest settlers were American, particularly Mormons fleeing marginalization and persecution from the United States via the Mormon Trail. Following the Mexican–American War in 1848, the region was annexed by the U.S., becoming part of the Utah Territory, which included what is now Colorado and Nevada. Disputes between the dominant Mormon community and the federal government delayed Utah's admission as a state; only after the outlawing of polygamy was it admitted in 1896 as the 45th.

 

People from Utah are known as Utahns. Slightly over half of all Utahns are Mormons, the vast majority of whom are members of the Church of Jesus Christ of Latter-day Saints (LDS Church), which has its world headquarters in Salt Lake City; Utah is the only state where a majority of the population belongs to a single church. A 2023 paper challenged this perception (claiming only 42% of Utahns are Mormons) however most statistics still show a majority of Utah residents belong to the LDS church; estimates from the LDS church suggests 60.68% of Utah's population belongs to the church whilst some sources put the number as high as 68%. The paper replied that membership count done by the LDS Church is too high for several reasons. The LDS Church greatly influences Utahn culture, politics, and daily life, though since the 1990s the state has become more religiously diverse as well as secular.

 

Utah has a highly diversified economy, with major sectors including transportation, education, information technology and research, government services, mining, multi-level marketing, and tourism. Utah has been one of the fastest growing states since 2000, with the 2020 U.S. census confirming the fastest population growth in the nation since 2010. St. George was the fastest-growing metropolitan area in the United States from 2000 to 2005. Utah ranks among the overall best states in metrics such as healthcare, governance, education, and infrastructure. It has the 12th-highest median average income and the least income inequality of any U.S. state. Over time and influenced by climate change, droughts in Utah have been increasing in frequency and severity, putting a further strain on Utah's water security and impacting the state's economy.

 

The History of Utah is an examination of the human history and social activity within the state of Utah located in the western United States.

 

Archaeological evidence dates the earliest habitation of humans in Utah to about 10,000 to 12,000 years ago. Paleolithic people lived near the Great Basin's swamps and marshes, which had an abundance of fish, birds, and small game animals. Big game, including bison, mammoths and ground sloths, also were attracted to these water sources. Over the centuries, the mega-fauna died, this population was replaced by the Desert Archaic people, who sheltered in caves near the Great Salt Lake. Relying more on gathering than the previous Utah residents, their diet was mainly composed of cattails and other salt tolerant plants such as pickleweed, burro weed and sedge. Red meat appears to have been more of a luxury, although these people used nets and the atlatl to hunt water fowl, ducks, small animals and antelope. Artifacts include nets woven with plant fibers and rabbit skin, woven sandals, gaming sticks, and animal figures made from split-twigs. About 3,500 years ago, lake levels rose and the population of Desert Archaic people appears to have dramatically decreased. The Great Basin may have been almost unoccupied for 1,000 years.

 

The Fremont culture, named from sites near the Fremont River in Utah, lived in what is now north and western Utah and parts of Nevada, Idaho and Colorado from approximately 600 to 1300 AD. These people lived in areas close to water sources that had been previously occupied by the Desert Archaic people, and may have had some relationship with them. However, their use of new technologies define them as a distinct people. Fremont technologies include:

 

use of the bow and arrow while hunting,

building pithouse shelters,

growing maize and probably beans and squash,

building above ground granaries of adobe or stone,

creating and decorating low-fired pottery ware,

producing art, including jewelry and rock art such as petroglyphs and pictographs.

 

The ancient Puebloan culture, also known as the Anasazi, occupied territory adjacent to the Fremont. The ancestral Puebloan culture centered on the present-day Four Corners area of the Southwest United States, including the San Juan River region of Utah. Archaeologists debate when this distinct culture emerged, but cultural development seems to date from about the common era, about 500 years before the Fremont appeared. It is generally accepted that the cultural peak of these people was around the 1200 CE. Ancient Puebloan culture is known for well constructed pithouses and more elaborate adobe and masonry dwellings. They were excellent craftsmen, producing turquoise jewelry and fine pottery. The Puebloan culture was based on agriculture, and the people created and cultivated fields of maize, beans, and squash and domesticated turkeys. They designed and produced elaborate field terracing and irrigation systems. They also built structures, some known as kivas, apparently designed solely for cultural and religious rituals.

 

These two later cultures were roughly contemporaneous, and appear to have established trading relationships. They also shared enough cultural traits that archaeologists believe the cultures may have common roots in the early American Southwest. However, each remained culturally distinct throughout most of their existence. These two well established cultures appear to have been severely impacted by climatic change and perhaps by the incursion of new people in about 1200 CE. Over the next two centuries, the Fremont and ancient Pueblo people may have moved into the American southwest, finding new homes and farmlands in the river drainages of Arizona, New Mexico and northern Mexico.

 

In about 1200, Shoshonean speaking peoples entered Utah territory from the west. They may have originated in southern California and moved into the desert environment due to population pressure along the coast. They were an upland people with a hunting and gathering lifestyle utilizing roots and seeds, including the pinyon nut. They were also skillful fishermen, created pottery and raised some crops. When they first arrived in Utah, they lived as small family groups with little tribal organization. Four main Shoshonean peoples inhabited Utah country. The Shoshone in the north and northeast, the Gosiutes in the northwest, the Utes in the central and eastern parts of the region and the Southern Paiutes in the southwest. Initially, there seems to have been very little conflict between these groups.

 

In the early 16th century, the San Juan River basin in Utah's southeast also saw a new people, the Díne or Navajo, part of a greater group of plains Athabaskan speakers moved into the Southwest from the Great Plains. In addition to the Navajo, this language group contained people that were later known as Apaches, including the Lipan, Jicarilla, and Mescalero Apaches.

 

Athabaskans were a hunting people who initially followed the bison, and were identified in 16th-century Spanish accounts as "dog nomads". The Athabaskans expanded their range throughout the 17th century, occupying areas the Pueblo peoples had abandoned during prior centuries. The Spanish first specifically mention the "Apachu de Nabajo" (Navaho) in the 1620s, referring to the people in the Chama valley region east of the San Juan River, and north west of Santa Fe. By the 1640s, the term Navaho was applied to these same people. Although the Navajo newcomers established a generally peaceful trading and cultural exchange with the some modern Pueblo peoples to the south, they experienced intermittent warfare with the Shoshonean peoples, particularly the Utes in eastern Utah and western Colorado.

 

At the time of European expansion, beginning with Spanish explorers traveling from Mexico, five distinct native peoples occupied territory within the Utah area: the Northern Shoshone, the Goshute, the Ute, the Paiute and the Navajo.

 

The Spanish explorer Francisco Vázquez de Coronado may have crossed into what is now southern Utah in 1540, when he was seeking the legendary Cíbola.

 

A group led by two Spanish Catholic priests—sometimes called the Domínguez–Escalante expedition—left Santa Fe in 1776, hoping to find a route to the California coast. The expedition traveled as far north as Utah Lake and encountered the native residents. All of what is now Utah was claimed by the Spanish Empire from the 1500s to 1821 as part of New Spain (later as the province Alta California); and subsequently claimed by Mexico from 1821 to 1848. However, Spain and Mexico had little permanent presence in, or control of, the region.

 

Fur trappers (also known as mountain men) including Jim Bridger, explored some regions of Utah in the early 19th century. The city of Provo was named for one such man, Étienne Provost, who visited the area in 1825. The city of Ogden, Utah is named for a brigade leader of the Hudson's Bay Company, Peter Skene Ogden who trapped in the Weber Valley. In 1846, a year before the arrival of members from the Church of Jesus Christ of latter-day Saints, the ill-fated Donner Party crossed through the Salt Lake valley late in the season, deciding not to stay the winter there but to continue forward to California, and beyond.

 

Members of the Church of Jesus Christ of Latter-day Saints, commonly known as Mormon pioneers, first came to the Salt Lake Valley on July 24, 1847. At the time, the U.S. had already captured the Mexican territories of Alta California and New Mexico in the Mexican–American War and planned to keep them, but those territories, including the future state of Utah, officially became United States territory upon the signing of the Treaty of Guadalupe Hidalgo, February 2, 1848. The treaty was ratified by the United States Senate on March 10, 1848.

 

Upon arrival in the Salt Lake Valley, the Mormon pioneers found no permanent settlement of Indians. Other areas along the Wasatch Range were occupied at the time of settlement by the Northwestern Shoshone and adjacent areas by other bands of Shoshone such as the Gosiute. The Northwestern Shoshone lived in the valleys on the eastern shore of Great Salt Lake and in adjacent mountain valleys. Some years after arriving in the Salt Lake Valley Mormons, who went on to colonize many other areas of what is now Utah, were petitioned by Indians for recompense for land taken. The response of Heber C. Kimball, first counselor to Brigham Young, was that the land belonged to "our Father in Heaven and we expect to plow and plant it." A 1945 Supreme Court decision found that the land had been treated by the United States as public domain; no aboriginal title by the Northwestern Shoshone had been recognized by the United States or extinguished by treaty with the United States.

 

Upon arriving in the Salt Lake Valley, the Mormons had to make a place to live. They created irrigation systems, laid out farms, built houses, churches, and schools. Access to water was crucially important. Almost immediately, Brigham Young set out to identify and claim additional community sites. While it was difficult to find large areas in the Great Basin where water sources were dependable and growing seasons long enough to raise vitally important subsistence crops, satellite communities began to be formed.

 

Shortly after the first company arrived in the Salt Lake Valley in 1847, the community of Bountiful was settled to the north. In 1848, settlers moved into lands purchased from trapper Miles Goodyear in present-day Ogden. In 1849, Tooele and Provo were founded. Also that year, at the invitation of Ute chief Wakara, settlers moved into the Sanpete Valley in central Utah to establish the community of Manti. Fillmore, Utah, intended to be the capital of the new territory, was established in 1851. In 1855, missionary efforts aimed at western native cultures led to outposts in Fort Lemhi, Idaho, Las Vegas, Nevada and Elk Mountain in east-central Utah.

 

The experiences of returning members of the Mormon Battalion were also important in establishing new communities. On their journey west, the Mormon soldiers had identified dependable rivers and fertile river valleys in Colorado, Arizona and southern California. In addition, as the men traveled to rejoin their families in the Salt Lake Valley, they moved through southern Nevada and the eastern segments of southern Utah. Jefferson Hunt, a senior Mormon officer of the Battalion, actively searched for settlement sites, minerals, and other resources. His report encouraged 1851 settlement efforts in Iron County, near present-day Cedar City. These southern explorations eventually led to Mormon settlements in St. George, Utah, Las Vegas and San Bernardino, California, as well as communities in southern Arizona.

 

Prior to establishment of the Oregon and California trails and Mormon settlement, Indians native to the Salt Lake Valley and adjacent areas lived by hunting buffalo and other game, but also gathered grass seed from the bountiful grass of the area as well as roots such as those of the Indian Camas. By the time of settlement, indeed before 1840, the buffalo were gone from the valley, but hunting by settlers and grazing of cattle severely impacted the Indians in the area, and as settlement expanded into nearby river valleys and oases, indigenous tribes experienced increasing difficulty in gathering sufficient food. Brigham Young's counsel was to feed the hungry tribes, and that was done, but it was often not enough. These tensions formed the background to the Bear River massacre committed by California Militia stationed in Salt Lake City during the Civil War. The site of the massacre is just inside Preston, Idaho, but was generally thought to be within Utah at the time.

 

Statehood was petitioned for in 1849-50 using the name Deseret. The proposed State of Deseret would have been quite large, encompassing all of what is now Utah, and portions of Colorado, Idaho, Nevada, Wyoming, Arizona, Oregon, New Mexico and California. The name of Deseret was favored by the LDS leader Brigham Young as a symbol of industry and was derived from a reference in the Book of Mormon. The petition was rejected by Congress and Utah did not become a state until 1896, following the Utah Constitutional Convention of 1895.

 

In 1850, the Utah Territory was created with the Compromise of 1850, and Fillmore (named after President Fillmore) was designated the capital. In 1856, Salt Lake City replaced Fillmore as the territorial capital.

 

The first group of pioneers brought African slaves with them, making Utah the only place in the western United States to have African slavery. Three slaves, Green Flake, Hark Lay, and Oscar Crosby, came west with this first group in 1847. The settlers also began to purchase Indian slaves in the well-established Indian slave trade, as well as enslaving Indian prisoners of war. In 1850, 26 slaves were counted in Salt Lake County. Slavery didn't become officially recognized until 1852, when the Act in Relation to Service and the Act for the relief of Indian Slaves and Prisoners were passed. Slavery was repealed on June 19, 1862, when Congress prohibited slavery in all US territories.

 

Disputes between the Mormon inhabitants and the federal government intensified after the Church of Jesus Christ of Latter-day Saints' practice of polygamy became known. The polygamous practices of the Mormons, which were made public in 1854, would be one of the major reasons Utah was denied statehood until almost 50 years after the Mormons had entered the area.

 

After news of their polygamous practices spread, the members of the LDS Church were quickly viewed by some as un-American and rebellious. In 1857, after news of a possible rebellion spread, President James Buchanan sent troops on the Utah expedition to quell the growing unrest and to replace Brigham Young as territorial governor with Alfred Cumming. The expedition was also known as the Utah War.

 

As fear of invasion grew, Mormon settlers had convinced some Paiute Indians to aid in a Mormon-led attack on 120 immigrants from Arkansas under the guise of Indian aggression. The murder of these settlers became known as the Mountain Meadows massacre. The Mormon leadership had adopted a defensive posture that led to a ban on the selling of grain to outsiders in preparation for an impending war. This chafed pioneers traveling through the region, who were unable to purchase badly needed supplies. A disagreement between some of the Arkansas pioneers and the Mormons in Cedar City led to the secret planning of the massacre by a few Mormon leaders in the area. Some scholars debate the involvement of Brigham Young. Only one man, John D. Lee, was ever convicted of the murders, and he was executed at the massacre site.

 

Express riders had brought the news 1,000 miles from the Missouri River settlements to Salt Lake City within about two weeks of the army's beginning to march west. Fearing the worst as 2,500 troops (roughly 1/3rd of the army then) led by General Albert Sidney Johnston started west, Brigham Young ordered all residents of Salt Lake City and neighboring communities to prepare their homes for burning and evacuate southward to Utah Valley and southern Utah. Young also sent out a few units of the Nauvoo Legion (numbering roughly 8,000–10,000), to delay the army's advance. The majority he sent into the mountains to prepare defenses or south to prepare for a scorched earth retreat. Although some army wagon supply trains were captured and burned and herds of army horses and cattle run off no serious fighting occurred. Starting late and short on supplies, the United States Army camped during the bitter winter of 1857–58 near a burned out Fort Bridger in Wyoming. Through the negotiations between emissary Thomas L. Kane, Young, Cumming and Johnston, control of Utah territory was peacefully transferred to Cumming, who entered an eerily vacant Salt Lake City in the spring of 1858. By agreement with Young, Johnston established the army at Fort Floyd 40 miles away from Salt Lake City, to the southwest.

 

Salt Lake City was the last link of the First Transcontinental Telegraph, between Carson City, Nevada and Omaha, Nebraska completed in October 1861. Brigham Young, who had helped expedite construction, was among the first to send a message, along with Abraham Lincoln and other officials. Soon after the telegraph line was completed, the Deseret Telegraph Company built the Deseret line connecting the settlements in the territory with Salt Lake City and, by extension, the rest of the United States.

 

Because of the American Civil War, federal troops were pulled out of Utah Territory (and their fort auctioned off), leaving the territorial government in federal hands without army backing until General Patrick E. Connor arrived with the 3rd Regiment of California Volunteers in 1862. While in Utah, Connor and his troops soon became discontent with this assignment wanting to head to Virginia where the "real" fighting and glory was occurring. Connor established Fort Douglas just three miles (5 km) east of Salt Lake City and encouraged his bored and often idle soldiers to go out and explore for mineral deposits to bring more non-Mormons into the state. Minerals were discovered in Tooele County, and some miners began to come to the territory. Conner also solved the Shoshone Indian problem in Cache Valley Utah by luring the Shoshone into a midwinter confrontation on January 29, 1863. The armed conflict quickly turned into a rout, discipline among the soldiers broke down, and the Battle of Bear River is today usually referred to by historians as the Bear River Massacre. Between 200 and 400 Shoshone men, women and children were killed, as were 27 soldiers, with over 50 more soldiers wounded or suffering from frostbite.

 

Beginning in 1865, Utah's Black Hawk War developed into the deadliest conflict in the territory's history. Chief Antonga Black Hawk died in 1870, but fights continued to break out until additional federal troops were sent in to suppress the Ghost Dance of 1872. The war is unique among Indian Wars because it was a three-way conflict, with mounted Timpanogos Utes led by Antonga Black Hawk fighting federal and Utah local militia.

 

On May 10, 1869, the First transcontinental railroad was completed at Promontory Summit, north of the Great Salt Lake. The railroad brought increasing numbers of people into the state, and several influential businessmen made fortunes in the territory.

 

Main article: Latter Day Saint polygamy in the late-19th century

During the 1870s and 1880s, federal laws were passed and federal marshals assigned to enforce the laws against polygamy. In the 1890 Manifesto, the LDS Church leadership dropped its approval of polygamy citing divine revelation. When Utah applied for statehood again in 1895, it was accepted. Statehood was officially granted on January 4, 1896.

 

The Mormon issue made the situation for women the topic of nationwide controversy. In 1870 the Utah Territory, controlled by Mormons, gave women the right to vote. However, in 1887, Congress disenfranchised Utah women with the Edmunds–Tucker Act. In 1867–96, eastern activists promoted women's suffrage in Utah as an experiment, and as a way to eliminate polygamy. They were Presbyterians and other Protestants convinced that Mormonism was a non-Christian cult that grossly mistreated women. The Mormons promoted woman suffrage to counter the negative image of downtrodden Mormon women. With the 1890 Manifesto clearing the way for statehood, in 1895 Utah adopted a constitution restoring the right of women's suffrage. Congress admitted Utah as a state with that constitution in 1896.

 

Though less numerous than other intermountain states at the time, several lynching murders for alleged misdeeds occurred in Utah territory at the hand of vigilantes. Those documented include the following, with their ethnicity or national origin noted in parentheses if it was provided in the source:

 

William Torrington in Carson City (then a part of Utah territory), 1859

Thomas Coleman (Black man) in Salt Lake City, 1866

3 unidentified men at Wahsatch, winter of 1868

A Black man in Uintah, 1869

Charles A. Benson in Logan, 1873

Ah Sing (Chinese man) in Corinne, 1874

Thomas Forrest in St. George, 1880

William Harvey (Black man) in Salt Lake City, 1883

John Murphy in Park City, 1883

George Segal (Japanese man) in Ogden, 1884

Joseph Fisher in Eureka, 1886

Robert Marshall (Black man) in Castle Gate, 1925

Other lynchings in Utah territory include multiple instances of mass murder of Native American children, women, and men by White settlers including the Battle Creek massacre (1849), Provo River Massacre (1850), Nephi massacre (1853), and Circleville Massacre (1866).

 

Beginning in the early 20th century, with the establishment of such national parks as Bryce Canyon National Park and Zion National Park, Utah began to become known for its natural beauty. Southern Utah became a popular filming spot for arid, rugged scenes, and such natural landmarks as Delicate Arch and "the Mittens" of Monument Valley are instantly recognizable to most national residents. During the 1950s, 1960s, and 1970s, with the construction of the Interstate highway system, accessibility to the southern scenic areas was made easier.

 

Beginning in 1939, with the establishment of Alta Ski Area, Utah has become world-renowned for its skiing. The dry, powdery snow of the Wasatch Range is considered some of the best skiing in the world. Salt Lake City won the bid for the 2002 Winter Olympics in 1995, and this has served as a great boost to the economy. The ski resorts have increased in popularity, and many of the Olympic venues scattered across the Wasatch Front continue to be used for sporting events. This also spurred the development of the light-rail system in the Salt Lake Valley, known as TRAX, and the re-construction of the freeway system around the city.

 

During the late 20th century, the state grew quickly. In the 1970s, growth was phenomenal in the suburbs. Sandy was one of the fastest-growing cities in the country at that time, and West Valley City is the state's 2nd most populous city. Today, many areas of Utah are seeing phenomenal growth. Northern Davis, southern and western Salt Lake, Summit, eastern Tooele, Utah, Wasatch, and Washington counties are all growing very quickly. Transportation and urbanization are major issues in politics as development consumes agricultural land and wilderness areas.

 

In 2012, the State of Utah passed the Utah Transfer of Public Lands Act in an attempt to gain control over a substantial portion of federal land in the state from the federal government, based on language in the Utah Enabling Act of 1894. The State does not intend to use force or assert control by limiting access in an attempt to control the disputed lands, but does intend to use a multi-step process of education, negotiation, legislation, and if necessary, litigation as part of its multi-year effort to gain state or private control over the lands after 2014.

 

Utah families, like most Americans everywhere, did their utmost to assist in the war effort. Tires, meat, butter, sugar, fats, oils, coffee, shoes, boots, gasoline, canned fruits, vegetables, and soups were rationed on a national basis. The school day was shortened and bus routes were reduced to limit the number of resources used stateside and increase what could be sent to soldiers.

 

Geneva Steel was built to increase the steel production for America during World War II. President Franklin D. Roosevelt had proposed opening a steel mill in Utah in 1936, but the idea was shelved after a couple of months. After the attack on Pearl Harbor, the United States entered the war and the steel plant was put into progress. In April 1944, Geneva shipped its first order, which consisted of over 600 tons of steel plate. Geneva Steel also brought thousands of job opportunities to Utah. The positions were hard to fill as many of Utah's men were overseas fighting. Women began working, filling 25 percent of the jobs.

 

As a result of Utah's and Geneva Steels contribution during the war, several Liberty Ships were named in honor of Utah including the USS Joseph Smith, USS Brigham Young, USS Provo, and the USS Peter Skene Ogden.

 

One of the sectors of the beachhead of Normandy Landings was codenamed Utah Beach, and the amphibious landings at the beach were undertaken by United States Army troops.

 

It is estimated that 1,450 soldiers from Utah were killed in the war.

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Historicamente, a Pateira deve ser considerada como um antigo braço marinho onde desaguavam, independentemente uns dos outros, os rios Cértima, Águeda e Vouga, antes da constituição da Ria de Aveiro. Aquele braço que os aluviões dos três rios fecharam originou um só curso de água - o rio Vouga - passando a foz a situar-se muito mais a noroeste, como actualmente (Almeida, 2006).

 

Pinho et al. (1988) cit Gomes Andrade escreve, em relação à Pateira, que o vale do Certoma, naquele ponte era dantes terreno firme, coberto de espessos arvoredos, por entre os quais o rio mansamente deslizava.

 

Também Morais em Sousa Batista (1945) cita um excerto de uma carta do almoxarife de Aveiro a D. Manuel em que fala da Mata de Perrães (eventualmente compreendida entre Perrães e a frente da freguesia de Fermentelos) dizendo que esta sempre fora coutada para nela se colherem porcos (provavelmente javalis) e veados, referindo ainda que era apaúlada.

 

Aliás, segundo Pinho et al, 1988, parece admissível supor que se trataria de uma zona bastante rica do ponto de vista faunístico e florístico, muito embora as referências à flora e fauna sejam escassas.

 

A Pateira ter-se-ia começado a formar em finais do século XV, provavelmente ainda na Idade Média, devido às sucessivas inundações dos rios Certoma e Águeda, e alagamento dos campos ribeirinhos.

 

Presentemente, a Pateira corresponde ao assoreamento e espraiamento do rio Cértima, perto do local onde desagua no rio Águeda.

 

A maior lagoa natural da Península Ibérica ocupa actualmente uma área de superfície e profundidade variáveis, de acordo com a estação do ano, que, no seu expoente máximo, atinge mais de 5 Km2. Estes, estendem-se, maioritariamente, pelo concelho de Águeda, abrangendo também o concelho de Aveiro e Oliveira do Bairro.

 

O termo “Pateira” encerra a especificidade da região do Vouga e afluentes designando, por si só, abundância de patos.

 

Em termos hidrográficos, a lagoa está compreendida na bacia hidrográfica do rio Cértima a qual, por sua vez, se insere na bacia hidrográfica do rio Águeda e esta, na bacia do rio Vouga.

 

A lagoa é alimentada pelo rio Cértima (a montante), pela ribeira do Pano (a poente), pontualmente por outras escorrências, e por água subterrânea (sistema aquífero Cretácico de Aveiro), sendo o rio Cértima o principal curso a condicionar a hidrologia.

 

No que diz respeito ao relevo, a zona envolvente da Pateira apresenta um relevo suave, a oeste, registando-se uma zona com altitude superior a 50 metros em Fermentelos (concelho de Águeda).

 

A este, na zona de Espinhel, ocorre uma elevação que atinge os 78 metros, revelando declives com relativo significado dadas as características da área envolvente. A noroeste, sensivelmente entre a Oliveirinha e Requeixo (concelho de Aveiro) destaca-se uma faixa com altitude entre os 50 e os 70 metros, com declive suave em direcção à Pateira.

 

A sudoeste, as áreas de cultivo, na margem esquerda do rio Cértima e de Perrães ladeiam a Pateira com relevos suaves de cotas mínimas.

  

Estatatuto de Protecção

 

A Pateira de Fermentelos apresenta características de um sistema semi-lêntico que integra a Zona de Protecção Especial da Ria de Aveiro (PTZPE0004) e, como tal, incluída na Rede Natura 2000.

   

Protegida pela Directiva Aves, está ainda classificada como “Zona Sensível” de acordo com o Decreto-lei n.º 152/97, de 19 de Julho, Anexo II, tratando-se de uma importante e extensa zona húmida (cit. ICN, 2006).

   

Por definição as Zonas Húmidas (ZH) são áreas de sapal, paul, turfeiras ou águas, naturais ou artificiais, permanentes ou temporárias, estáticas ou correntes, doces , salobras ou salgadas, incluindo extensões de água do mar, cuja profundidade na maré baixa não exceda os 6 metros e zonas costeiras e ribeirinhas (Convenção Ramsar).

   

Estas ZH, onde se inclui a Pateira, desempenham importantes funções nos ecossistemas como a regularização hídrica e climática, a purificação da água, contrariam o efeito de estufa, protegem a costa, alimentam reservatórios naturais subterrâneos, suportando uma elevada biodiversidade, entre outras.

   

As zonas húmidas são, aliás, áreas de grande produtividade primária da Terra (a par com as florestas tropicais), suportando assim uma fauna e flora riquíssimas.

   

Biodiversidade Faunística

No que diz respeito à diversidade faunística, a Pateira e zonas envolventes destacam-se, particularmente, pela importante componente ornitológica. Nestas áreas ocorrem espécies com estatutos de protecção a nível nacional e internacional — classificadas pela Directiva Aves (Directiva 79/409/CEE), Convenção de Bona, Convenção de Berna.

 

Surgem espécies de importância comunitária, como:

 

O Garçote (Ixobrychus minutus) frequenta normalmente zonas com abundante vegetação palustre, sendo difícil a sua observação. Não necessita de grandes áreas para nidificar, sendo uma espécie essencialmente solitária durante a reprodução. Os ninhos são construídos no meio do caniçal, acima da água. Alimenta-se essencialmente de insectos e por vezes de pequenos peixes, anfíbios, moluscos, crustáceos, ovos e crias de outras aves, entre outros.

 

A Garça-vermelha (Ardea purpurea) prefere zonas húmidas com áreas de vegetação densa de caniçais, procurando águas ricas em nutrientes (eutróficas), pouco profundas, paradas ou com pouca corrente. Os ninhos são construídos junto ou sobre a água, geralmente em caniçais inundados, não voltando a ocupar ninhos de anos anteriores. Alimenta-se principalmente de peixes e insectos (larvas e adultos). Segundo observações realizadas ao longo dos últimos anos, a população de Garça-vermelha tem aumentado na Pateira.

 

A Águia-sapeira (Circus aeruginosus) também designada como Tartaranhão-ruivo-dos-pauis, nidifica em zonas húmidas onde ocorra uma vegetação aquática emergente abundante, preferencialmente manchas de caniçal, onde são construídos os ninhos. Nestas áreas procura ainda alimento, bem como em águas pouco profundas e com vegetação aquática, caçando frequentemente em campos agrícolas nas imediações. Alimenta-se de animais de pequeno e médio porte, nomeadamente aves, mamíferos (roedores), e, em menor proporção, insectos, sapos, cobras e peixes.

 

O Milhafre-preto (Milvus migrans) frequenta um número diversificado de habitats embora apareça, principalmente, associado a massas de água. Nidifica nos pinhais e matas ripícolas associadas à lagoa, construindo o ninho nas árvores. Procura alimento em áreas abertas ou semi-abertas, alimentando-se de presas de pequeno porte, como roedores, lagomorfos, aves terrestres e ouriços-cacheiros, especialmente indivíduos jovens, doentes ou feridos mas também répteis, peixes, anfíbios e insectos.

 

Ocorrem ainda espécies como o Perna-longa (Himantopus himantopus), o Guarda-rios (Alcedo athis), a Petinha-dos-campos (Anthus campestris), a Garça-branca-pequena (Egretta garzetta), entre outras, incluídas no Anexo I da Directiva 79/409/CEE.

 

Estas e outras espécies, ocorrem na ZPE da Ria de Aveiro, fazendo a Pateira, assim, parte do sistema que “suporta, regularmente, mais de 1% da população biogeográfica de Alfaiate (Recurvirostra avosetta), de Negrola (Melanitta nigra), de Borrelho-grande-de-coleira (Charadrius hiaticula) e de Borrelho-de-coleira-interrompida (Charadrius alexandrinus)” (ICN, 2006).

 

Refere-se ainda a ocorrência de vários passeriformes migradores de matos e bosques, assim como passeriformes de caniçais e galerias ripícolas. A diversidade de biótopos é propícia à reprodução, refúgio e alimento de aves invernantes, nidificantes e migradoras, sendo a Pateira cada vez mais procurada pelos observadores de aves - Birdwatching - e amantes da natureza para a realização de actividades.

 

As condições biofísicas propiciam também a diversidade de peixes que se encontra na Pateira. Inserida na bacia hidrográfica do Rio Vouga, ocorrem, ou têm potencial para ocorrer, espécies como o Barbo-do-Norte (Barbus bocagei), a Boga (Chondrostoma polylepis), a Boga–portuguesa (Chondrostoma lusitanicum), o Ruivaco (Rutilus macrolepidotus ), o Bordalo (Rutilus alburnoides ) - com estatuto de protecção comunitário (pelo Anexo II e/ou V da Directiva Habitats).

 

Ocorrem ainda espécies como a Tainha (Chelon labrosus), a Carpa (Cyprinius carpio), o Escalo-do-norte (Leucistus carolitertii), o Lúcio (Esox lucius), a Enguia (Anguilla anguilla), a Pardelha (Cobitis calderoni), o Achigã (Micropterus salmoides ), etc.

 

Tratam-se de animais sobretudo nocturnos e que, alimentando-se de larvas de insectos, crustáceos e peixes mortos, podem atingir cerca de 1 metro.

 

A fauna piscícola encontra na Pateira e sistema hídrico adjacente as condições ecológicas que permitem a vitalidade e subsistência das diversas comunidades, condições que permitem o refúgio e a desova em tempo de reprodução. Surgem então na lagoa áreas que são identificadas, pelas gentes locais, como “verdadeiras maternidades” de peixe.

 

Entre as várias espécies de bivalves que se observam na Bacia Hidrográfica do Vouga, ocorre na lagoa um, cujas dimensões o transformam numa espécie emblemática - a Anodonta.

 

Este molusco bivalve de água doce, comummente designado como Mexilhão-do-rio, passa despercebido à maioria da população, devido aos seus hábitos ecológicos discretos, que privilegiam o substrato lodoso, onde se enterram.

 

É muito importante para o ecossistema, uma vez que se alimenta através da filtração de um grande volume de água (de que retira detritos e plâncton), sendo apontada como um indicador da qualidade da água. A degradação das condições ambientais afecta negativamente a população destes bivalves.

 

Associada aos habitats de zonas húmidas está também uma elevada diversidade de répteis e anfíbios, característicos destes sistemas e que se localizam sobretudo no interface terra-água e cuja ocorrência potencial se lista de seguida.

 

Ainda neste interface, bem como nas zonas mais secas adjacentes à lagoa, ocorrem diversas espécies de mamíferos. Destas, destaca-se a Lontra (Lutra lutra), emblemática pelos afectos (e desafectos) que provoca na população, mas também por se tratar de uma espécie protegida pelos anexos II e IV do Decreto-lei nº 49/2005 de 24 de Fevereiro.

 

A Lontra (Lutra lutra) procura de forma selectiva os locais de descanso e abrigo, sendo possível encontrar os seus refúgios nas margens mais tranquilas da lagoa e onde abunda vegetação. Esta espécie solitária alimenta-se sobretudo de fauna piscícola, embora possa alimentar-se também de anfíbios e crustáceos (como o lagostim-do-Louisiana). Pode reproduzir-se durante todo o ano, dependendo da disponibilidade de recursos alimentares, nascendo as crias (uma a quatro) ao fim de 61—63 dias em tocas dissimuladas na vegetação.

 

Surgem ainda espécies como o Ouriço-cacheiro (Erinaceus europaeus), a Raposa (Vulpes vulpes), o Coelho-bravo (Oryctolagus cuniculus), o Javali (Sus scrofa), vários roedores, entre outras, que encontram protecção no Direito Comunitário, e Nacional.

 

Assim, a diversidade de biótopos existentes na região (juncais, caniçais, arrozais, margens com vegetação ripícola, etc.) transforma esta região num complexo ecossistema e, por conseguinte, num importante refúgio para a vida animal..

 

Biodiversidade Florística

Na zona húmida, que engloba as águas livres e a vegetação alagada das margens e linhas, dominam habitats com povoamentos de Caniço (Phragmites communis), juntamente com a Tabúa (Typha sp.) e o Bunho (Scirpus lacustris). Ocorrem ainda comunidades (ou mosaicos de comunidades) de plantas vasculares com macrófitas flutuantes, enraizadas ou suspensas entre o fundo e a superfície: a Erva-pinheirinha (Myriophyllum sp.), os Nenúfares (Nymphaea sp., Nuphar luteo ) ou mesmo o Jacinto-de-água (Eichhornia crassipes).

 

Em algumas zonas marginais ao longo da Pateira, verifica-se a ocorrência de diversas espécies arbóreas e arbustivas como:

 

Salgueiros (Salix alba, Salix sp.), Choupos (Populus canescens, Populus nigra, Populus sp.), Amieiros (Alnus glutinosa), Amieiro-negro (Frangula alnus), Freixos (Fraxinus angustifolia), Pilriteiros (Crataegus monogyna), Sabugueiros (Sambucus nigra), Borrazeiras (Salix atrocinerea ), pontualmente Carvalhos (Quercus robur), Loureiros (Laurus nobilis ), Ulmeiros (Ulmus sp.) ...

 

Entre as espécies alóctones encontra-se o Eucalyptus globulus (predominante no coberto florestal das áreas adjacentes à lagoa), e outras árvores dos géneros Acacia e Hakea , estas com comportamento infestante e que se encontram disseminadas pelas imediações da lagoa.

 

Do grupo das herbáceas e sub-arbustivas refere-se apenas a presença do Lírio-amarelo-dos-pântanos (Íris pseudacorus), do Agrião (Nasturtium officinale), do Embude (Oenanthe crocata), da Erva-pessegueira (Polygonum persicaria), Hortelã-de-água (Mentha aquatica), entre tantas outras. Ocorrem espécies com estatuto de protecção como a Gilbardeira (Ruscus aculeatus ) pelo anexo V, e a Marsilea quadrifolia.

 

Peculiar, e pouco divulgado, é o facto de, em áreas adjacentes à lagoa, ocorrerem ainda espécies de plantas carnívoras como a Pinguicula lusitanica; potencialmente poderão ocorrer ainda outras espécies, embora sejam cada vez mais difíceis de encontrar.

 

Esta carnívora ocorre sobretudo em sítios húmidos, por vezes turfosos das margens da lagoa (e rios), florescendo entre Março e Maio. É nas folhas que é libertado o muco adesivo que aprisiona os insectos, que se aproximam atraídos pelo odor libertado. Assim que detectam a presa, as folhas começam a enrolar-se de forma a envolver a presa nas enzimas digestivas libertadas.

 

Um aspecto que se encontra ainda pouco desenvolvido diz respeito à diversidade micológica. Assim, a variedade de fungos que ocorre começa agora a ser inventariada e estudada de forma mais exaustiva, apresentando-se nas imagens laterais alguns exemplos.

 

Na breve resenha biológica apresentada, ainda que incompleta, fica patente a vasta diversidade biológica e potencial natural (e conservacionista) da Pateira, como é referido para as demais Zonas Húmidas. Não obstante, são alguns os problemas que afectam esta área, entre os quais a infestação com Jacinto-de-água.

 

Jacinto-de-água

O jacinto-de-água (Eichhornia crassipes) é uma espécie infestante originária da bacia do Amazonas (Brasil), encontrando-se actualmente disseminado nos cinco continentes. Alastra-se pelos sistemas aquáticos de climas tropicais e temperados, causando rapidamente a ruptura dos sistemas naturais infestados. É considerada por muitos autores como “uma das piores pragas de plantas aquáticas a nível global” (HOLM et al., 1977).

 

Como tal, a ocorrência e disseminação desta espécie exótica infestante na Pateira constitui um dos principais factores que contribui para a degradação das condições ecológicas, económicas e sociais desta zona húmida que urge recuperar e preservar.

 

A ceifeira-aquática

Dada a área em questão e a dimensão da infestação, as metodologias a adoptar e tecnologias de apoio foram seleccionadas de acordo com a avaliação do risco sobre a ZPE, do efeito ambiental das diferentes metodologias e a eficácia da remoção a curto, médio e longo prazo.

 

A gravidade do problema da infestação de sistemas aquáticos ao nível global levou ao desenvolvimento de tecnologia específica para a sua resolução e/ou controlo.

 

Assim sendo, recorreu-se à remoção mecânica, sendo a extracção feita com recurso a uma máquina – ceifeira-aquática – que começou a laborar na lagoa a 13 de Dezembro de 2006.

 

Com um tapete incorporado, e movido por um motor, extrai as massas de jacintos-de-água. Controlada por um operador, a ceifeira-aquática possui um sistema simples e eficaz: duas rodas de pás com um funcionamento hidráulico independente que garantem a grande manobrabilidade do equipamento.

 

Em apenas dois meses e meio, foi possível melhorar as condições ecológicas e hidrológicas do sistema aquático, recuperar o espelho de água, melhorar a capacidade para suportar actividades lúdicas e de lazer na área, bem como melhorar as condições para a prática das actividades tradicionais no espelho da lagoa.

 

Requalificação Ambiental e Paisagística da Pateira

A remoção do jacinto-de-água da lagoa foi apenas a 1ª fase de um vasto e complexo processo, que engloba várias outras medidas e acções que visam o desenvolvimento sustentável, a conservação e protecção da Natureza e, consequentemente, a Requalificação Ambiental e Paisagística da maior lagoa natural da Península Ibérica, a Pateira de Fermentelos.

 

Após o levantamento topo-hidrográfico realizado, concluiu-se que o leito da lagoa se encontra fortemente assoreado, em particular na zona mais a jusante da Pateira.

 

Desta forma, ficou patente a necessidade de, a curto prazo, se proceder à normalização do leito natural da Pateira, pela remoção (dragagem) do excesso de sedimentos entretanto acumulados, bem como à reconstrução do pequeno açude localizado na confluência da Pateira e rio Águeda.

 

Numa área classificada como a Pateira, englobada numa importante bacia hidrográfica (bacia hidrográfica do Rio Vouga), com valores paisagísticos e a nível da conservação da natureza, que se traduzem na elevada diversidade biológica, alguma com estatuto de protecção a nível nacional e internacional, é importante dotar o espaço com infra-estruturas adequadas que permitam a conservação, mas também a observação e a interpretação da natureza.

 

Neste âmbito, são desenvolvidas várias acções de educação ambiental, como a organização de palestras e acções de sensibilização ambiental, observação de aves, realização de percursos interpretativos, workshops para a construção de ninhos, entre outras actividades promovidas pela Autarquia ou por outras entidades como a SPEA (Sociedade Portuguesa para o Estudo das Aves), a UA (Universidade de Aveiro), a QUERCUS (Associação Nacional de Conservação da Natureza).

 

A definição de percursos com temas e finalidades várias (educação ambiental, prática de desporto, observação de aves, etc.) está a ser estudada numa perspectiva intermunicipal.

 

A Pateira é, desta forma, vista como um todo, onde o objectivo é conduzir o visitante pelo espaço natural dando-lhe a conhecer os valores naturais da área (com descritores de paisagem, de espécies), bem como dotar estes percursos do mobiliário adequado (observatórios de aves, pontos de encontro e descanso, material de apoio à prática desportiva, etc) e que dê ao visitante o conforto, a segurança e o equilíbrio natural que procura neste local.

 

São várias as propostas de actividades que o visitante encontra ao seu dispor na lagoa ou nas áreas adjacentes e que o levam ao contacto quer com a natureza, quer com as dinâmicas culturais e tradições locais. Desde os momentos de descontracção que pode passar nos parques de lazer, a uma travessia nas tradicionais bateiras, a uma viagem nas bicicletas aquáticas, de um passeio a cavalo, de bicicleta ou a pé, a uma tarde de pesca, um dia desportivo, ou simplesmente um momento de pausa a vislumbrar a paisagem, só ou em família, são algumas das ideias já praticáveis na Pateira de Fermentelos.

 

Considerações finais

Numa época em que o ambiente se assume no contexto nacional e internacional como tema prioritário e se procura evitar a continuação da degradação dos recursos hídricos, surge a Directiva-Quadro da Água (DQA) – 2000/60/CE – transposta para a ordem jurídica nacional pela Lei nº 58/2005, de 29 de Dezembro. Esta vem estabelecer como objectivo a alcançar, até 2015, “o bom estado ecológico ou o bom potencial ecológico e químico de todas as massas de água”.

Como tal, “proteger e melhorar o estado dos ecossistemas aquáticos e também dos ecossistemas terrestres e zonas húmidas, directamente dependentes dos ecossistemas aquáticos”, constitui uma atribuição das entidades públicas e um dever dos particulares.

 

Não obstante, e tal como referido no início deste documento, além da dimensão ambiental, prevalece uma forte componente social, sendo incalculável a importância que a Pateira e ecossistemas associados representam para as populações limítrofes desta área.

 

Assim, torna-se premente assegurar a continuidade deste projecto, com o desenvolvimento e implementação das acções previstas para a requalificação ambiental e paisagística da Pateira. Pretende-se pois que a Pateira de Fermentelos volte a ser um ex libris natural da região, motivo de referência e orgulho nacional.

  

Texto retirado do livro

Pateira de Fermentelos: Paisagem a proteger

Célia Laranjeira (CMA) www.cm-agueda.pt/PageGen.aspx?WMCM_PaginaId=28901

At the summit of Mount Lee.

 

The landscape is nice and green from the recent record rains.

 

The Hollywood Sign (formerly the Hollywoodland Sign) is a landmark and American cultural icon located in Los Angeles, California. It is situated on Mount Lee, in the Hollywood Hills area of the Santa Monica Mountains. The sign overlooks Hollywood, Los Angeles.

 

"HOLLYWOOD" is spelled out in 45-foot (13.7 m)-tall white capital letters and is 350 feet (106.7 m) long. It was originally created in 1923 as an advertisement for a local real estate development, but it garnered increasing recognition after the sign was left up. The sign was a frequent target of pranks and vandalism, but it has since undergone restoration, including the installation of a security system to deter vandalism. The sign is protected and promoted by The Trust For Public Land, a nonprofit organization, while its site and the surrounding land are part of Griffith Park.

 

The sign was erected in 1923 and originally read "HOLLYWOODLAND." Its purpose was to advertise the name of a new segregated housing development in the hills above the Hollywood district of Los Angeles.

 

The sign was officially dedicated in 1923. It was intended only to last a year and a half, but after the rise of American cinema in Los Angeles during the Golden Age of Hollywood, the sign became an internationally recognized symbol and was left there.

 

In 1949, the Hollywood Chamber of Commerce began a contract with the City of Los Angeles Parks Department to repair and rebuild the sign. The contract stipulated that "LAND" be removed to spell "Hollywood" and reflect the district, not the "Hollywoodland" housing development. The Parks Department dictated that all subsequent illumination would be at the Chamber's expense, so the Chamber opted not to replace the lightbulbs. The 1949 effort gave it new life, but the sign's unprotected wood and sheet metal structure continued to deteriorate. By the 1970s, the first O had splintered and broken, resembling a lowercase u, and the third O had fallen down completely, leaving the severely dilapidated sign reading "HuLLYWO D."

 

In 1978, in large part because of the public campaign to restore the landmark by Hugh Hefner, founder of Playboy magazine, the Chamber set out to replace the severely deteriorated sign with a more permanent structure. Nine donors gave US$27,777.77 each (totaling US$249,999.93) to sponsor replacement letters, made of steel supported by steel columns on a concrete foundation.

Replacing an earlier scanned photo with a better version 30-Aug-22 (DeNoise AI).

 

JAL's 50th Anniversary Pink 'Dream Express' logojet, 'Friends'. Right Side.

 

The Boeing 747-400D was built for the Japanese Domestic market and had no winglets. They didn't do anything for fuel efficiency on short sectors and omitting them saved weight. Only 19 were built for Japan Air Lines and All Nippon Airways, they had a maximum passenger capacity of 660.

 

This aircraft was delivered to JAL Japan Air Lines as JA8904 in Nov-92. When JAS Japan Air System was merged into JAL in Apr-04, they created two divisions, Domestic and International. This aircraft was part of Japan Airlines - Domestic until the Domestic Division was merged into International in Oct-06.

 

It was retired in Jun-10 after almost 18 years in service and sold to AerSale Inc (USA) as N894DB and permanently retired at Roswell, NM, USA. The registration was cancelled in May-15. Updated 30-Aug-22.

One of my photographs is include in the permanent exhibition at this mini-museum.

 

The Diving Bell is the first project in Dublin Port’s plan to create a ‘distributed museum’ of attractions across the Dublin docklands and into Dublin Port to preserve the port’s industrial heritage and history.

 

The Diving Bell was designed by the port engineer Bindon Blood Stoney (1828 to 1907) and built by Grendon and Co., Drogheda. It was delivered to the Port in 1866, entered service in 1871 and was used in the building of the Port’s quay walls until 1958. Stoney was a prodigious engineer and among his achievements were the building of the Boyne Viaduct in Drogheda, the construction of O’Connell Bridge and the building of many of the Port’s quay walls including Sir John Rogerson’s Quay and North Wall Quay Extension.

 

The Diving Bell was used in the building of the Port’s quay walls from the Victorian era right up until almost the 1960s. It was a ground-breaking piece of engineering innovation in its day.

An old photograph of Birmingham Corporation Tramways (BCT) rail scrubber/grinder No. 8, also referred to as No. PW8, PW meant it was a 'Permanent Way Car'.

 

The photo reverse is annotated as having been taken in "Witton Depot" and stamped as it having been taken by S. N. J. White.

 

No. 8 was originally City of Birmingham Tramways car No. 158, built as a double deck open top car in 1901 by the 'Electric Railway and Tramway Carriage Works' and running on a Peckham 9A Cantilever truck. When the system was taken over by BCT the car was renumbered as 505 and in 1913 retrucked with a Brill 21E.

 

In Dec 1920 No. 505 was withdrawn from service and converted into a single deck rail scrubber/grinder and allocated fleet No. 8, in Nov 1929 the body was removed at the Kyotts Lake Road Works (KLRW) and replaced with the body of car No. 266 which had been used as an illuminated tram. This was another open top double deck car, but built in 1907 by the 'United Electric Car Co.', as well as being cut down to single deck and fitted with vestibules it was retrucked with a Brush Conaty (Radial) truck, returning to service in Mar 1930.

 

Towards the end of the system No. 8 was used in KLRW to shunt around the withdrawn cars, because of this it was the last car to run operationally on the BCT system, as well as being the last car broken up by W. T. Bird & Sons in Aug 1953.

 

The parts of the Birmingham tramways system that had not already been withdrawn or transferred to trolleybus/bus operation closed in Jul 1953.

  

📷 Any photograph I post on Flickr is an original in my possession, nothing is ever copied/downloaded from another location. 📷

 

-------------------------------------------------

 

If there are any errors in the above description please let me know. Thanks.

 

Any photograph, ephemera, etc I post on Flickr is in my possession, nothing is copied from another location. The original photographer may have taken copies from their original negative and passed them out (sold them?) so there may be other copies out there of your (and my) 'original' transport photo, although occasionally there may be 'holiday snaps' type photos where there are not any other photos exactly the same in existence.

 

If you wish to use this image (bearing in mind it may not be my copyright) or obtain a full size version (most of my uploads are small size) please contact me.

HISTORY UPDATED - Permanently retired.

 

Photo taken from the Templeton Bridge.

 

Fleet No: '206'.

 

First flown with the Airbus test registration F-WWIU, this aircraft was delivered to Air Canada as C-FDSN in Nov-90. It was sold to GECAS in Dec-01 and leased back to Air Canada. Now 30 years old, the aircraft was stored at Kansas City, MO, USA in Sep-20 due to the COVID-19 Pandemic. It was ferried to Greenwood, MS, USA in Nov-20 and permanently retired after 30 years in service. Updated (Nov-20).

Contrasting with the known very short life-spans of insects like gnats and flies, these caught in amber are permanently caught for humans thousands of years later to see and marvel at. This macro of amber was taken at an outdoor vendor display at the Tucson Rock and Gem Show. There is a set for many of the photos I took at the February, 2007 show, here.

 

SNCF 'Infra' liveried BB 67000 class diesel loco 667623 seen here about to leave Clermont-Ferrand yard.

The famous Puy de Dome can just be seen in the distance, obviously my intention all the time to include it in the picture! 😉

Sony A6300 + Zeiss Vario-Tessar T* E 4/16-70

 

Mont Blanc, Chamonix, France

 

Young Woo Park - All Rights Reserved.

Unpacking seems endless for this old suitcase that has been left behind in an abandoned workers house at Amiantos Asbestos Mine.

Permanent closure..

Toronto, Ontario

 

Panasonic Lumix G 14mm f2.5

Olympus OM-D E-M5

HISTORY UPDATED - Permanently retired.

 

Updated 'new' livery!

 

First flown with the Airbus test registration D-AUAF, this aircraft was delivered to Air France as F-GUGB in Nov-03.

 

After 18 years in service the aircraft was ferried from Paris-deGaulle to Blytheville, AR, USA in Oct-21 and permanently retired. Updated 01-Nov-21.

Criado em 1929, o Parque Doutor Fernando Costa, conhecido como Parque da Água Branca, é um espaço de 137 mil metros quadrados que abriga atrações para todas as idades. O Museu Geológico, por exemplo, tem exposições permanentes que são mantidas pelo Instituto Geológico. A Casa de Caboclo é uma réplica das residências da zona rural, onde o visitante pode experimentar a Cavaca, uma broa de milho assada na chapa do fogão a lenha.

Além dessas atrações, quem visita o parque pode conhecer as espécies mais importantes das bacias hidrográficas do estado no Aquário. O Relógio do Sol é outra atração interessante. Ele marca a passagem do tempo nos diversos países, por meio da observação da posição do sol. Para os amantes dos animais, o parque é ótimo para ter contato direto com diversas espécies, como as carpas e as tartarugas, que ficam em tanques espalhados pelo local, ou com os pavões, galinhas, pintinhos e gatos que ficam soltas pelo parque. Às vezes, é possível ver saguis pelas árvores. O local também possui um aquário com as principais espécies da bacia hidrográfica do Estado, com valor de entrada a R$ 2,0 por visitante.

A terceira idade também possui espaço no parque, como a Praça do Idoso, um local com aparelhos para a prática de ginástica, que é bastante frequentado. Diversas atividades também são desenvolvidas ao longo do ano, como ginástica ante estresse e yoga – a programação deve ser consultada diretamente no parque.

Opções para todos os gostos

O parque sedia várias feiras, como a de produtos orgânicos que acontece todos os sábados, também há outras feiras, como as de artesanato e comida que ocorrem nas cocheiras do parque ou as feiras de exposição de animais de pequeno e médio porte.

O piquenique é outro programa que pode de ser feito no parque, que possui um espaço com mesas e bancos, para os mais tradicionais é possível estender a toalha no chão, embaixo de uma árvore, lugar geralmente escolhido pelos casais para fazer um lanche romântico. Outro espaço muito procurado é o dedicado à leitura, com diversas opções de livros e mesas que só podem ser usadas para estudar ou para ler. É um lugar bem confortável em meio ao verde e às sombras das árvores.

A Casa do Caboclo é uma ótima escolha para quem gosta do interior, um cenário típico da fazenda com fogão a lenha e mesas de madeira. O ambiente rústico é inspirado nas casas da zona rural e serve café típico do interior, entre as iguarias servidas, está a famosa cavaca – broa de milho assada na chapa do fogão a lenha. Aos finais de semana, o café é servido com música ao vivo, moda de viola e sertaneja. Também há outros ambientes do parque que remetem à fazenda, como as cocheiras e a Arena, que ainda são usados para a prática de equitação.

Um passeio bastante requisitado não só pelas crianças, mas também pelo público em geral, é o de trenzinho, onde as pessoas se divertem passeando pelas ruas e dependências do parque, custa R$ 3 por pessoa. Outro atrativo do parque é O Relógio do Sol, que marca a passagem do tempo nos diversos países por meio da observação da posição do sol. O parque também abriga um museu de geologia, o Mugeu; um Centro de Referência em Educação Ambiental; e diversos espaços para exposições.

Mais informações

Parque da Água Branca

Av. Professor Francisco Matarazzo, 455 – Água Branca - Zona Oeste

São Paulo - SP

Fone: (0xx11) 3865 4131/ 3865 4130

 

Left

 

Arlington Memorial Bridge

 

The Arlington Memorial Bridge is a Neoclassical masonry, steel, and stone arch bridge with a central bascule (or drawbridge) that crosses the Potomac River, linking Washington, D.C., with the U.S. state of Virginia. First proposed in 1886, the bridge went unbuilt for decades thanks to political quarrels over whether the bridge should be a memorial, and to whom or what. Traffic problems associated with the dedication of the Tomb of the Unknown Soldier in November 1921 and the desire to build a bridge in time for the bicentennial of the birth of George Washington led to its construction in 1932.

 

Designed by the architectural firm McKim, Mead, and White, Arlington Memorial Bridge defines the western end of the National Mall and is decorated with monumental statues depicting valor and sacrifice by sculptor Leo Friedlander. The bridge's draw span was permanently closed in 1961. The bridge has received minor repairs, but as of 2013, never a major overhaul and is deteriorating.

 

See: Arlington Memorial Bridge

 

Memorial Bridge

 

Arlington Memorial Bridge and its related architectural, engineering, sculptural, and landscape features are significant as important elements in the Neo-classical urban design of the National Capital as it evolved during the first third of the 20th century. Successfully integrated with Washington's grand plan, the bridge composition enhances the monumental city as well as the riverscape.

 

Widely regarded as Washington's most beautiful bridge, Memorial Bridge symbolically links North and South in its alignment between the Lincoln Memorial and Arlington House, the Robert E. Lee Memorial. The adjacent Rock Creek and Potomac Parkway terminus, the Watergate steps, and monumental equestrian statuary join with the bridge in constituting a formal western terminus of the great Washington Mall composition at the edge of the Potomac. The bridge axis, angled southwesterly from the east-west Mall axis, is carried on Memorial Avenue across the Boundary Channel Bridge to the Virginia shore. There it terminates at the Arlington Hemicycle, keystone of the grand renaissance gateway to Arlington National Cemetery and now the location of the Women in Military Service for America Memorial. This Memorial and museum, located in the Hemicycle, was designed in 1989 by Marion Weiss and Michael Manfredi, and is now open to the public. The project has restored the Hemicycle in a very sensitive manner. Arlington House rises as the focal point on the hill above.

 

The entire composition was designed by the prominent architectural firm of McKim, Mead and White. The low, Neo-classical bridge is 2,163 feet long; nine broad arches carry the bridge across the river. Except for the draw span, the bridge is of reinforced concrete construction faced with dressed North Carolina granite ashlar.

 

Flanking the eastern ends of the bridge and parkway are two pairs of monumental Neo-classical equestrian sculpture on identical pedestals. "The Arts of War" by Leo Friedlander stands at the end of the bridge. In "Valor" on the left, the male equestrian is accompanied by a female striding forward with a shield; in "Sacrifice" a standing female symbolizing the earth looks up to the rider Mars. "The Arts of Peace" by James Earle Fraser flanks the end of the parkway. "Music and Harvest" consists of a winged horse, Pegasus, between a male figure with a bundle of wheat and a sickle and a woman with a harp. In "Aspiration and Literature," another Pegasus is flanked by figures holding a book and a bow. The statues, approximately 17 feet tall are of gilded bronze. They were commissioned in 1925, but were not erected until 1951.

 

Memorial Bridge runs across the Potomac River from the Lincoln Memorial to Arlington House in Virginia.

 

See: Memorial Bridge Equestrian sculptures

 

Arlington House, The Robert E. Lee Memorial

 

Arlington House, The Robert E. Lee Memorial, formerly named the Custis-Lee Mansion, is a Greek revival style mansion located in Arlington, Virginia, USA that was once the home of Confederate General Robert E. Lee. It overlooks the Potomac River and the National Mall in Washington, D.C. During the American Civil War, the grounds of the mansion were selected as the site of Arlington National Cemetery, in part to ensure that Lee would never again be able to return to his home. However, the United States has since designated the mansion as a National Memorial to Lee, a mark of widespread respect for him in both the North and South. Arlington Woods, located behind Arlington House, contains the oldest and largest tract of climax eastern hardwood forest that still exists in Arlington County.

 

See: Arlington House

 

Center

 

Potomac River

 

The Potomac River flows into the Chesapeake Bay, located along the mid-Atlantic coast of the United States. The river (main stem and North Branch) is approximately 652 km long, with a drainage area of about 38,000 km². In terms of area, this makes the Potomac River the fourth largest river along the Atlantic coast of the United States and the 21st largest in the United States. Over 5 million people live within the Potomac watershed.

 

See: Potomac River

 

Right

 

Arlington County, Virginia

 

The county is situated in Northern Virginia on the south bank of the Potomac River directly across from Washington, D.C. Arlington is also bordered by Fairfax County and the City of Falls Church to the southwest, and the City of Alexandria to the southeast. With a land area of 67 km2, Arlington is the geographically smallest self-governing county in the United States and has no other incorporated towns within its borders. Given these unique characteristics, for statistical purposes the county is included as a municipality within the Washington Metropolitan Area by the United States Census Bureau. As of 2012, Arlington County had a population of 220,565 residents. It would be the fourth-largest city in the state if it were incorporated as such.

 

Given the county's proximity to Washington, D.C., Arlington is headquarters to many departments and agencies of the federal government of the United States, including the Department of Defense, the United States Drug Enforcement Administration, and the Defense Advanced Research Projects Agency (DARPA). The many federal agencies, government contractors, and service industries contribute to Arlington's stable economy, which has made it one of the highest-income counties in the United States. Arlington is also the location of national memorials and museums, including Arlington National Cemetery, the Pentagon Memorial, the Marine Corps War Memorial, and the United States Air Force Memorial.

 

See: Arlington

Permanently closed

Permanently closed as a hotel.

Permanent bunting at Getliffes Yard arcade, Leek, Staffordshire

Riders grab some thrills, at Haverfordwest skate park.

 

Tripod-mounted. AF.

 

Take a break at Pelcomb Portraits.

Moscow. July 2009

All-Russian Exhibition Centre (Всероссийский выставочный центр) is a permanent general-purpose trade show in Moscow, Russia.

 

The "All-Russia Exhibition Centre" is a state joint-stock company, officially abbreviated as GAO "VVC", which stands for "Gosudarstvennoye Aktsionernoye Obshchestvo 'Vserossiyskiy Vystavochny Centr'".

 

VVC is a member of exhibition associations: IUEF (since 1991) and UFI (since 1997).

History

 

1935-1939 Construction

This section is based on Soviet public documents, available in Russian at www.bcxb.ru

 

The exhibition was established February 17, 1935 as the All-Union Agricultural Exhibition (VSKhV) (Russian: Всесоюзная Сельско-Хозяйственная Выставка Vsesoyuznaya Selsko-Khozyaystvennaya Vystavka). Existing site (then known as Ostankino Park, a country territory recently incorporated into city limits), was approved in August, 1935. Master plan by Vyacheslav Oltarzhevsky was approved in April, 1936, and the first show season was announced to begin in July, 1937.

 

However, plans didn't materialize, and 3 weeks before the deadline Stalin personally postponed the exhibition by one year (to August 1938). It seemed that this time everything would be ready on time, and again the builders failed to complete their work, and regional authorities failed to select and deliver proper exhibits. Some pavilions and the 1937 entrance gates by Oltarzhevsky were torn down to be replaced with more appropriate structures (most pavilions were criticized for having no windows). According to Oltarzhevsky's original plan, all of the pavilions were to be constructed from wood. In 1938, a government commission examined the construction and decided that it did not suit the ideological direction of the moment. The exhibition was considered too modest and too temporary. Oltarzhevsky was arrested, together with the Comissar for Agriculture and his staff, and eventually released in 1943. Later, he worked on the 1947-1953 Moscow skyscraper project.

 

As a result, in August 1938 Nikita Khrushchev, speaking at the Supreme Soviet assembly, declared that the site is not ready, and the opening was extended to August, 1939. It opened indeed August 1, 1939, and worked in 8AM - 11PM mode until October 25 (40,000 daily attendance). 1940 and 1941 seasons followed; after the German invasion, July 1, 1941 the exhibition was closed - until the end of World War II.

 

1948-1959 Renovation

 

Statue by Vera Mukhina over the northern entrance to the VDNKHIn October, 1948 the State ordered to renew the Exhibition, starting with the 1950 season. Again, the opening was postponed more than once; the first post-war season opened in 1954 (still as Agricultural exhibition). In 1956 season the planners set aside an Industrial area within the main territory; more restructuring and rebuilding followed. In 1959 the park was renamed Exhibition of Achievements of the National Economy (Russian: Выставка Достижений Народного Хозяйства Vystavka Dostizheniy Narodnovo Khozyaystva) or ВДНХ/VDNKh.

  

Space pavillon, 1980By 1989 the exhibition had 82 pavilions with the exhibition area of 700,000 square metres. Each pavilion (including the 1939 "regions") had been dedicated to a particular industry or a field: the Engineering Pavilion (1954), the Space Pavilion (1966), the Atomic Energy Pavilion (1954), the People's Education Pavilion (1954), the Radioelectronics Pavilion (1958), the Soviet Culture Pavilion (1964).

 

During the Soviet times, each year VDNKh hosted more than 300 national and international exhibitions and many conferences, seminars and meetings of scientists and industry professionals. These events attracted about 11 million visitors annually, including 600,000 guests from outside the Soviet Union. The "Radioelectronics" exhibition hall for some years housed the working (and unique) prototypes of the most advanced ES EVM computers to date, which were time-shared by many research organizations right on the premises.

 

The most memorable feature of the exhibition site was the statue Worker and Kolkhoz Woman (Rabochiy i Kolkhoznitsa), featuring the gigantic figures of a man and woman holding together the famous "hammer and sickle". The sculpture, which reaches 25 meters toward the sky, was created by Vera Mukhina and originally crowned the 35-meter-tall Soviet pavilion at the Exposition Internationale des Arts et Techniques dans la Vie Moderne (1937). The statue was featured on a logo of Mosfilm, Russia's largest movie studio.

  

[edit] Present Day

 

Space Pavilion. The Tupolev Tu-154 (reg. no. SSSR-85005, prod. no. 70M005, 1970 year of production, Model 005) in front of the pavilion was dismantled on September 14, 2008. This Tupolev Tu-154 was used as a flight testbed.In 1992, VDNKh was renamed, receiving its current name VVC. It occupies 2,375,000 square metres of which 266,000 square metres are used for indoor exhibits. The territory of VVC is greater than that of the Principality of Monaco and has approximately 400 buildings. Inadequate maintenance of Vera Mukhina's statue caused such disrepair that the statue was disassembled (see 2006 photographs of what's left). It was slated to be refurbished and installed on the top of the new pavilion by 2008[1], but funding shortages lead to dragged-out restoration. Now it is to be installed back by the end of 2010.

 

The term "VDNKh" is still in use, including the name of a nearby subway station.

 

Wikipedia

I have highlighted this issue previously. I realise that the fishermen have a dangerous job and from time to time incidents do occur. These plastic boxes are easily lost overboard but when they are washed ashore they should be removed from the beach. I must have removed dozens over the years.

In fact a few years ago I had found one just like this one and filled it with smaller plastic items, As I was carrying the box back up from the sea a couple of French men came over to chat and noticing immediately that I was English told me that it was not my job and I should leave the box and contents there. I think that they meant that as a tourist I should not have to clear such problems on their behalf.

The local authorities do employ teams of people to clean the beaches of such things now on a regular basis, an endless task, I feel.

Ugh, hate this flat perm look.

So sad, Tommy Bartlett show has been permanently closed.

 

After losing the 2020 season to the COVID-19 pandemic, the Tommy Bartlett Show portion of the business will be permanently closing after a 68-year run. The Wisconsin Dells won't be the same without it.

Fred was evidently too sexy for his sign :P Of course I took a photo of the whole thing also (lying on the bottom of a shelf no less), but then noticed the rather ironic lettering in the lower right corner.

____________________________________

Fred's, 1977-built, closed June 2019, Northwest Dr. near Main St., Southaven MS

permanent marker on paper, 11 x 9 inches, hbt14-p002, 2014

Originals - Reproductions

permanent marker on paper, 11 x 9 inches, hbt13-p010, 2013

Originals - Reproductions

The Royal Courts of Justice was opened by Queen Victoria in 1882 and became the permanent home of the Supreme Court. The history of the administration of justice in England and Wales spans many centuries. By the mid-19th century‚ a number of separate courts had come into existence at different times and to meet different needs. Many anomalies and archaisms had arisen and it was recognised that this state of affairs was unacceptable‚ and‚ in consequence‚ the Judicature Acts of 1873-75 reconstituted all the higher courts. The Judicature Acts abolished the former courts and established in their place a Supreme Court of Judicature‚ the name of which was changed in 1981 to the Supreme Court of England and Wales.

 

The Supreme Court consists of two courts: the High Court of Justice and the Court of Appeal. The High Court consists of three Divisions dealing mainly with civil disputes: the Chancery Division (which took over the work of the old High Court of Chancery)‚ the Queen’s Bench Division (which incorporated the jurisdiction of the three former common law courts: the Court of King’s Bench‚ the Court of Common Pleas and the Court of Exchequer) and the Probate‚ Divorce and Admiralty Division which took over the former Court of Admiralty‚ Court of Probate and Court for Divorce. This last division has itself been replaced by the Family Division which was created in 1970.

 

When Queen Victoria opened the Royal Courts of Justice on 4th December 1882 she was drawing a line under a long and difficult effort to achieve a home for the Supreme Court for England and Wales.

 

Before 1875‚ courts had been housed in Westminster Hall‚ Lincoln’s Inn and various other buildings around London and pressure had been mounting for a grand new building and in 1866 Parliament announced a competition for the design.

 

The eleven architects competing for the contract for the Law Courts each submitted alternative designs with the view of the possible placing of the building on the Thames Embankment. The present site was chosen only after much debate.

 

In 1868 it was finally decided that George Edmund Street‚ R.A. was to be appointed the sole architect for the Royal Courts of Justice and it was he who designed the whole building from foundation to varied carvings and spires.? Building was started in 1873 by Messrs. Bull & Sons of Southampton.

 

There was a serious strike of masons at an early stage which threatened to extend to other trades and caused a temporary stoppage of the works. In consequence‚ foreign workmen were brought in - mostly Europeans. This aroused bitter hostility on the part of the men on strike and the newcomers had to be specially protected by the police and were housed and fed in the building.? However‚ these disputes were eventually settled and the building took eight years to complete and was officially opened by Queen Victoria on the 4th of December‚ 1882. Sadly‚ Street died before the building was opened.

 

Parliament paid ?1‚453‚000 for the 7.5 acre site. It was reported that 4‚175 people lived in 450 houses. In two houses in Robin Hood Court 52 people had their abode‚ in Lower Serle’s Place 189 people slept in 9 houses. The site also housed the Kit Kat Club.

 

The building was paid for by cash accumulated in court from the estates of the intestate to the sum of ?700‚000. Oak work and fittings in the courts cost a further ?70‚000 and with decoration and furnishing the total cost for the building came to under a million pounds.

 

The dimensions of the building (in round figures) are: 470 feet (approx.143 metres) from East to West; 460 feet (approx.140 metres) from north to south; 245 (approx 74 metres) feet from the Strand level to the tip of the fleche.

 

Entering through the main gates in the Strand one passes under two elaborately carved porches fitted with iron gates. The carving over the outer porch consists of heads of the most eminent Judges and Lawyers. Over the highest point of the upper arch is a figure of Jesus Christ; to the left and right at a lower level are figures of Solomon and Alfred; that of Moses is at the northern front of the building. Also at the northern front‚ over the Judges entrance are a stone cat and dog representing fighting litigants in court.

 

The walls and ceilings (of the older‚ original Courts) are panelled in oak which in many cases is elaborately carved. In Court 4‚ the Lord Chief Justice’s court‚ there is an elaborately carved wooden royal Coat of Arms.? Each court has an interior unique to itself; they were each designed by different architects.

 

There are‚ in addition to the Waiting Rooms‚ several Arbitration and Consultation Chambers together with Robing Rooms for the members of the Bar.

  

www.flaneurphoto.com

From the vintage "sexploitation" collection of Richard Perez, relating to "Permanent Obscurity" at: RichardPerez.net

Permanent exhibition at Thun Castle

My unique style, captured by my adorable identical twin sister, June

Situated next to the famous Tottori Sand Dunes in Tottori Prefecture. Each yearly exhibit starts in April and lasts until January of the following year. The sand sculptures are then deliberately destroyed and a new exhibit is prepared from January to April. The sand sculptor Katsuhiko Chaen is the chief sculptor. Despite the museum's close proximity to the sand dunes, that sand cannot be used because the sand dunes are part of a protected national park. The sand comes from a road building project, and the same sand is reused each year, only sand and water is used to create the sculptures. The museum's motto is "Travel around the World in Sand", and the exhibit is themed around a different country or geographical area each year. 　Wikipedia

Mit permanent Make up sind Sie in jeder Lebenslage perfekt geschminkt!

Die meisten Frauen legen großen Wert auf ihr Äußeres und verbringen jeden Morgen nicht unbeträchtliche Zeit im Bad, um sich zu stylen. Ist dann der Tag vorüber, geht es ans Abschminken, was wiederum Zeit in Anspruch nimmt. In ...

 

swiss-beauty-studio.ch/permanent-make-up-in-zuerich/

woman getting a perm done

It's a candle holder. Or something.

Oumarou Ganou (centre), Permanent Representative of Burkina Faso, presents his credentials to Secretary-General António Guterres.

 

The Secretary-General hands the credentials to Beatrix Kania, Chief of the United Nations Protocol and Liaision Service.

 

UN Photo/Manuel Elías

28 April 2023

New York, United States of America

Photo # UN7983008