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Dark room print on Fomabrom 111 in Ilford MG developer. Intensive toning (15 min) in Foma Selenium 1+19, although it doesn't show easily in the scan.
SM Mall of Asia (MOA) is a shopping mall owned and developed by SM Prime Holdings, the largest mall developer and owner in the Philippines. SM Mall of Asia is the second largest shopping mall in the Philippines and the 4th largest shopping mall in the world. It has a land area of 42 hectares and has a gross floor area of an approximate 390,193 m² (4.2 million square feet)[1] and 407,101 m² of total area. The mall is located at Bay City, Pasay City, Philippines just near the SM Central Business Park, the Manila Bay and the southern end of EDSA (Epifanio de los Santos Avenue)
For Processing BW Film - Not For Drinking!
The FPP’s new Caffenol Developer for Black and White Processing at home! CUP O’ JOE is a powder solution in a handy pouch that when mixed with water produces 1 Liter of BW Home Developing solution that will process up to 4 rolls of 35mm, 120 or 8 4x5 sheets of BW film.
filmphotographystore.com/products/darkroom-supplies-caffe...
Chamonix 45F-2 view camera, 75mm Grandagon Lens, taken on Ilford FP-4+ film developed in Pyrocat HD formula developer
For Processing BW Film - Not For Drinking!
The FPP’s new Caffenol Developer for Black and White Processing at home! CUP O’ JOE is a powder solution in a handy pouch that when mixed with water produces 1 Liter of BW Home Developing solution that will process up to 4 rolls of 35mm, 120 or 8 4x5 sheets of BW film.
filmphotographystore.com/products/darkroom-supplies-caffe...
The Film Photography Project now brings you D96 B/W negative developer. Long used in the motion picture industry as the standard B/W developer, but previously only available in very large quantities. We now have it available in powder to make 1 US Gallon.
D96 is a lower contrast film developer with the ability to increase the contrast by increasing your developing times or agitation. We have tested this developer with not only cinema films like X2 (Eastman Double-X), ORWO Cinema Films and FPP LOW ISO BW, but with standard B/W films like Kodak Tri-X. T-Max and Ilford FP4 an HP5 films.
Hindmarsh Island.
Our access to Hindmarsh Island from Goolwa is via the bridge which opened in 2001. The bridge is 319 metres long and 19 metres high. Hindmarsh Island leads to the Murray River Mouth beside Mundoo Island and the start of the Coorong. It is 15 kms long and about 6 kms wide and roughly one third of the island is now part of the Coorong National Park. In 1990 the SA government passed an act of parliament allowing the developers to construct a bridge so that the developers could create a marina and housing development on the island. But the SA government accepted legal liability for the financing of the bridge. The bridge became one of the great fiascos and controversies in South Australian history. Some members of the Ngarrindjeri people objected to the proposed bridge in 1994 on the basis of the water channel being part of “secret women’s business” and it being a sacred site. The controversy ended in a Royal Commission and the decision that “secret women’s business” was a fabrication. The Ngarrindjeri group then took their case to the Supreme Court in Canberra which doubted that “secret women’s business” was a fabrication but did not endorse it. The Keating federal government then banned construction of the bridge because of this Supreme Court finding. A few years later the Howard Federal government legislated for the bridge to be constructed. The controversy became a conflict point with much conflict and many competing interests. It involved state and federal governments, locals and outsiders, white and non-white Australians, men and feminists, developers and anti-development people, lawyers for and against it, anthropologists for and against it and much secrecy about the significance or otherwise of the bridge site. This conflict point mainly had direct impacts on the local people – the town of Goolwa was divided over the issue as were the inhabitants of Hindmarsh Island, the Ngarrindjeri women were divided as some opposed the concept of “secret women’s business” and others said it was nonsense. The main people to gain were the developers who had eventual success with their marina and housing estate. The “outsiders” including professors, archaeologists, anthropologists, politicians, bankers and lawyers all made gains – in monetary, publicity or humanitarian rights terms. Their moments of glory seldom acknowledged the difficulties the whole controversy had caused for the Ngarrindjeri people. Ngarrindjeri people have accepted the outcome of the conflict point and whilst they still maintain that the area is a sacred site for Ngarrindjeri women and their “secret business” they allow their people to use the bridge to gain access to their cultural lands.
Captain Charles Sturt on his epic voyage down and up the Murray River in 1829/30 named Point McLeay after one of his officers on their rowing boat and Point Sturt after himself both on the edges of Lake Alexandrina. The large island near the Murray Mouth was named later by Captain John Blenkinsop after the first SA Governor Sir John Hindmarsh. Captain Charles Sturt later became an early settler in Adelaide. After he resigned his commission with the British Military Service he was granted 5,000 acres in NSW in 1835 near what was to become Canberra much later. He purchased a further 1,950 acres in NSW at Mittagong. Two years later he purchased a further 1,000 acres near Sydney where he intended to make a new home. He then overlanded cattle from NSW to South Australia in 1838 to revive his fortunes. This did not work but he was feted in Adelaide as a hero and so he sold all his lands in NSW to accept a government appointment as Commissioner of Lands in South Australia in 1839. He was soon after demoted by the Governor to Assistant Registrar. In 1844 Sturt led an expedition to the Barrier Range area of NSW and he went further trying to cross what was named Sturts Stony Desert. When he returned in 1846 he was made Colonial Treasurer which was a much higher paying position. He returned to England in 1847 to receive the gold medal of the Royal Geographical Society in London for his inland explorations. Sturt returned to SA and lived on his 380 acre farm and orchard on the Port River near Grange Beach. This was where he had built Grange cottage in 1841. He returned to England permanently in 1853 so his children could be educated in England. The Grange was sold by members of his family in 1877 to finalise his estate as Sturt had died in 1869.
Early pastoralists recognised the value of Hindmarsh Island as a well-watered spot surrounded by water supplies so Dr John Rankine of Strathalbyn took out occupational licenses on most of Hindmarsh Island in 1844. He had a boat as a ferry at Clayton to cart his sheep back and forth across the channel. But in 1851 the Hundred of Alexandrina was declared and surveyed into 80 acre sections for sale to farmers. The land was quickly taken up when made available for sale in 1854 and the wealthy of Strathalbyn including the Rankins, Gollans and Maidment family bought some land. One of the early farming settlers was Charles Price. Price and his family arrived in Melbourne in 1853 when he was aged 48 but he decided he did not like Melbourne and he voyaged to Port Adelaide. From here he took up land on Hindmarsh Island in 1853 against the wishes of Dr Rankine and he was the first to import cattle from his home county Hereford in 1866. He was also the first to import Shropshire sheep from the neighbouring county of Hereford earlier in 1855. He ran his Hereford cattle stud on the island from 1867 till his death in 1886 and during this time he sold prized stud cattle to George Fife Angas and John Riddoch. His 983 acres were sold at £5 per acre and his son moved on to Eyre Peninsula. Charles Price was buried in the Island Cemetery. Not far away is the Hindmarsh Island School which started in 1880 and closed in 1954. The building is now a part time café of sorts. Next to that is the island butter factory with grand buttresses. It operated from the late 19th century until 1936. Not far away is the Murray Mouth. There was also a Wesleyan Methodist Church on the island which opened in 1857 and closed around 1887 and was then demolished.
The local residents erected a stone cairn memorial to Captain Charles Sturt on the island in 1930 one hundred years after his discovery of the island in 1830. It is also a memorial to the other early explorer of these parts Captain Collet Barker (1784-1831) who explored here in 1831 just after Sturt. As a military officer he had served in India and explored areas in WA including King George Sound where Albany is located. Here he was in charge of the settlement at Raffles Bay with a group of convicts to control. His name was later used for the inland settlement of Mt Barker north of Albany. He was recalled to Sydney with the convicts in 1831 and Raffles Bay settlement was closed down. The Governor of NSW told him to explore the Fleurieu Peninsula region on his way back to Sydney. In SA he climbed Mt Lofty which had been named by Captain Matthew Flinders in 1802. Barker named the Sturt River which he discovered. Collet Barker then explored areas from Cape Jervis to the mouth of the Murray River. Here he was speared by local Aboriginal people. There is a fine memorial to Collet Barker in St. James Anglican Church in Sydney from his fellow officers. Barker’s journals were especially important as they convinced Sturt that the mountain he had seen from Lake Alexandrina was not Mt Lofty but another mountain. Sturt altered his maps and charts and named the second mountain after Collet Barker. This was done by Sturt in 1834.
Oct. 21, 2021: Route 66 El Trovatore Motel in Kingman, Arizona. Developer John F. Miller from 1937-40, built the motel, gas station, and cafe. Celebrities staying at the motel included Jeff Chandler, Charles Bronson, Jane Russell, James Dean, Marilyn Monroe, Clark Gable, and Don Knotts. Unfortunately, in later years, the motel fell into disrepair.
But about a decade ago, the rundown property was closed and facing foreclosure. Sam and Monica Frisher took over the motel in 2012 and renovated it - twenty rooms became Hollywood-themed rooms. In addition, workers repaired old signs and murals. Painters added new murals. A 206-foot Route 66 map decorates one side of the main motel building.
2020-08-20
Nikon F90X
Nikon Ais 85mm f/1.4 lens
Kodak Tri-X 400 (800-push) 35mm film
Adox Rodinal (1+50) developer
20ºC - 17min
Canyonlands National Park is an American national park located in southeastern Utah near the town of Moab. The park preserves a colorful landscape eroded into numerous canyons, mesas, and buttes by the Colorado River, the Green River, and their respective tributaries. Legislation creating the park was signed into law by President Lyndon Johnson on September 12, 1964.
The park is divided into four districts: the Island in the Sky, the Needles, the Maze, and the combined rivers—the Green and Colorado—which carved two large canyons into the Colorado Plateau. While these areas share a primitive desert atmosphere, each retains its own character. Author Edward Abbey, a frequent visitor, described the Canyonlands as "the most weird, wonderful, magical place on earth—there is nothing else like it anywhere."
In the early 1950s, Bates Wilson, then superintendent of Arches National Monument, began exploring the area to the south and west of Moab, Utah. After seeing what is now known as the Needles District of Canyonlands National Park, Wilson began advocating for the establishment of a new national park that would include the Needles. Additional explorations by Wilson and others expanded the areas proposed for inclusion into the new national park to include the confluence of Green and Colorado rivers, the Maze District, and Horseshoe Canyon.
In 1961, Secretary of the Interior Stewart Udall was scheduled to address a conference at Grand Canyon National Park. On his flight to the conference, he flew over the Confluence (where the Colorado and Green rivers meet). The view apparently sparked Udall's interest in Wilson's proposal for a new national park in that area and Udall began promoting the establishment of Canyonlands National Park.
Utah Senator Frank Moss first introduced legislation into Congress to create Canyonlands National Park. His legislation attempted to satisfy both nature preservationists' and commercial developers' interests. Over the next four years, his proposal was struck down, debated, revised, and reintroduced to Congress many times before being passed and signed into creation.
In September, 1964, after several years of debate, President Lyndon B. Johnson signed Pub.L. 88–590, which established Canyonlands National Park as a new national park. Bates Wilson became the first superintendent of the new park and is often referred to as the "Father of Canyonlands."
The Colorado River and Green River combine within the park, dividing it into three districts called the Island in the Sky, the Needles, and the Maze. The Colorado River flows through Cataract Canyon below its confluence with the Green River.
The Island in the Sky district is a broad and level mesa in the northern section of the park, between the Colorado and Green rivers. The district has many viewpoints overlooking the White Rim, a sandstone bench 1,200 feet (370 m) below the Island, and the rivers, which are another 1,000 feet (300 m) below the White Rim.
The Needles district is located south of the Island in the Sky, on the east side of the Colorado River. The district is named for the red and white banded rock pinnacles which are a major feature of the area. Various other naturally sculpted rock formations are also within this district, including grabens, potholes, and arches. Unlike Arches National Park, where many arches are accessible by short to moderate hikes, most of the arches in the Needles district lie in backcountry canyons, requiring long hikes or four-wheel drive trips to reach them.
The Ancestral Puebloans inhabited this area and some of their stone and mud dwellings are well-preserved, although the items and tools they used were mostly removed by looters. The Ancestral Puebloans also created rock art in the form of petroglyphs, most notably on Newspaper Rock along the Needles access road.
The Maze district is located west of the Colorado and Green rivers. The Maze is the least accessible section of the park, and one of the most remote and inaccessible areas of the United States.
A geographically detached section of the park located north of the Maze district, Horseshoe Canyon contains panels of rock art made by hunter-gatherers from the Late Archaic Period (2000-1000 BC) pre-dating the Ancestral Puebloans. Originally called Barrier Canyon, Horseshoe's artifacts, dwellings, pictographs, and murals are some of the oldest in America. The images depicting horses date from after 1540 AD, when the Spanish reintroduced horses to America.
Since the 1950s, scientists have been studying an area of 200 acres (81 ha) completely surrounded by cliffs. The cliffs have prevented cattle from ever grazing on the area's 62 acres (25 ha) of grassland. According to the scientists, the site may contain the largest undisturbed grassland in the Four Corners region. Studies have continued biannually since the mid-1990s. The area has been closed to the public since 1993 to maintain the nearly pristine environment.
Mammals that roam this park include black bears, coyotes, skunks, bats, elk, foxes, bobcats, badgers, ring-tailed cats, pronghorns, desert bighorn sheep, and cougars. Desert cottontails, kangaroo rats and mule deer are commonly seen by visitors.
At least 273 species of birds inhabit the park. A variety of hawks and eagles are found, including the Cooper's hawk, the northern goshawk, the sharp-shinned hawk, the red-tailed hawk, the golden and bald eagles, the rough-legged hawk, the Swainson's hawk, and the northern harrier. Several species of owls are found, including the great horned owl, the northern saw-whet owl, the western screech owl, and the Mexican spotted owl. Grebes, woodpeckers, ravens, herons, flycatchers, crows, bluebirds, wrens, warblers, blackbirds, orioles, goldfinches, swallows, sparrows, ducks, quail, grouse, pheasants, hummingbirds, falcons, gulls, and ospreys are some of the other birds that can be found.
Several reptiles can be found, including eleven species of lizards and eight species of snake (including the midget faded rattlesnake). The common kingsnake and prairie rattlesnake have been reported in the park, but not confirmed by the National Park Service.
The park is home to six confirmed amphibian species, including the red-spotted toad, Woodhouse's toad, American bullfrog, northern leopard frog, Great Basin spadefoot toad, and tiger salamander. The canyon tree frog was reported to be in the park in 2000, but was not confirmed during a study in 2004.
Canyonlands National Park contains a wide variety of plant life, including 11 cactus species,[34] 20 moss species, liverworts, grasses and wildflowers. Varieties of trees include netleaf hackberry, Russian olive, Utah juniper, pinyon pine, tamarisk, and Fremont's cottonwood. Shrubs include Mormon tea, blackbrush, four-wing saltbush, cliffrose, littleleaf mountain mahogany, and snakeweed
Cryptobiotic soil is the foundation of life in Canyonlands, providing nitrogen fixation and moisture for plant seeds. One footprint can destroy decades of growth.
According to the Köppen climate classification system, Canyonlands National Park has a cold semi-arid climate ("BSk"). The plant hardiness zones at the Island in the Sky and Needles District Visitor Centers are 7a with an average annual extreme minimum air temperature of 4.0 °F (-15.6 °C) and 2.9 °F (-16.2 °C), respectively.
The National Weather Service has maintained two cooperative weather stations in the park since June 1965. Official data documents the desert climate with less than 10 inches (250 millimetres) of annual rainfall, as well as hot, mostly dry summers and cold, occasionally wet winters. Snowfall is generally light during the winter.
The station in The Neck region reports an average January temperature of 29.6 °F and an average July temperature of 79.3 °F. Average July temperatures range from a high of 90.8 °F (32.7 °C) to a low of 67.9 °F (19.9 °C). There are an average of 45.7 days with highs of 90 °F (32 °C) or higher and an average of 117.3 days with lows of 32 °F (0 °C) or lower. The highest recorded temperature was 105 °F (41 °C) on July 15, 2005, and the lowest recorded temperature was −13 °F (−25 °C) on February 6, 1989. Average annual precipitation is 9.33 inches (237 mm). There are an average of 59 days with measurable precipitation. The wettest year was 1984, with 13.66 in (347 mm), and the driest year was 1989, with 4.63 in (118 mm). The most precipitation in one month was 5.19 in (132 mm) in October 2006. The most precipitation in 24 hours was 1.76 in (45 mm) on April 9, 1978. Average annual snowfall is 22.8 in (58 cm). The most snowfall in one year was 47.4 in (120 cm) in 1975, and the most snowfall in one month was 27.0 in (69 cm) in January 1978.
The station in The Needles region reports an average January temperature of 29.7 °F and an average July temperature of 79.1 °F.[44] Average July temperatures range from a high of 95.4 °F (35.2 °C) to a low of 62.4 °F (16.9 °C). There are an average of 75.4 days with highs of 90 °F (32 °C) or higher and an average of 143.6 days with lows of 32 °F (0 °C) or lower. The highest recorded temperature was 107 °F (42 °C) on July 13, 1971, and the lowest recorded temperature was −16 °F (−27 °C) on January 16, 1971. Average annual precipitation is 8.49 in (216 mm). There are an average of 56 days with measurable precipitation. The wettest year was 1969, with 11.19 in (284 mm), and the driest year was 1989, with 4.25 in (108 mm). The most precipitation in one month was 4.43 in (113 mm) in October 1972. The most precipitation in 24 hours was 1.56 in (40 mm) on September 17, 1999. Average annual snowfall is 14.4 in (37 cm). The most snowfall in one year was 39.3 in (100 cm) in 1975, and the most snowfall in one month was 24.0 in (61 cm) in March 1985.
National parks in the Western US are more affected by climate change than the country as a whole, and the National Park Service has begun research into how exactly this will effect the ecosystem of Canyonlands National Park and the surrounding areas and ways to protect the park for the future. The mean annual temperature of Canyonlands National Park increased by 2.6 °F (1.4 °C) from 1916 to 2018. It is predicted that if current warming trends continue, the average highs in the park during the summer will be over 100 °F (40 °C) by 2100. In addition to warming, the region has begun to see more severe and frequent droughts which causes native grass cover to decrease and a lower flow of the Colorado River. The flows of the Upper Colorado Basin have decreased by 300,000 acre⋅ft (370,000,000 m3) per year, which has led to a decreased amount of sediment carried by the river and rockier rapids which are more frequently impassable to rafters. The area has also begun to see an earlier spring, which will lead to changes in the timing of leaves and flowers blooming and migrational patterns of wildlife that could lead to food shortages for the wildlife, as well as a longer fire season.
The National Park Service is currently closely monitoring the impacts of climate change in Canyonlands National Park in order to create management strategies that will best help conserve the park's landscapes and ecosystems for the long term. Although the National Park Service's original goal was to preserve landscapes as they were before European colonization, they have now switched to a more adaptive management strategy with the ultimate goal of conserving the biodiversity of the park. The NPS is collaborating with other organizations including the US Geological Survey, local indigenous tribes, and nearby universities in order to create a management plan for the national park. Right now, there is a focus on research into which native plants will be most resistant to climate change so that the park can decide on what to prioritize in conservation efforts. The Canyonlands Natural History Association has been giving money to the US Geological Survey to fund this and other climate related research. They gave $30,000 in 2019 and $61,000 in 2020.
A subsiding basin and nearby uplifting mountain range (the Uncompahgre) existed in the area in Pennsylvanian time. Seawater trapped in the subsiding basin created thick evaporite deposits by Mid Pennsylvanian. This, along with eroded material from the nearby mountain range, became the Paradox Formation, itself a part of the Hermosa Group. Paradox salt beds started to flow later in the Pennsylvanian and probably continued to move until the end of the Jurassic. Some scientists believe Upheaval Dome was created from Paradox salt bed movement, creating a salt dome, but more modern studies show that the meteorite theory is more likely to be correct.
A warm shallow sea again flooded the region near the end of the Pennsylvanian. Fossil-rich limestones, sandstones, and shales of the gray-colored Honaker Trail Formation resulted. A period of erosion then ensued, creating a break in the geologic record called an unconformity. Early in the Permian an advancing sea laid down the Halgaito Shale. Coastal lowlands later returned to the area, forming the Elephant Canyon Formation.
Large alluvial fans filled the basin where it met the Uncompahgre Mountains, creating the Cutler red beds of iron-rich arkose sandstone. Underwater sand bars and sand dunes on the coast inter-fingered with the red beds and later became the white-colored cliff-forming Cedar Mesa Sandstone. Brightly colored oxidized muds were then deposited, forming the Organ Rock Shale. Coastal sand dunes and marine sand bars once again became dominant, creating the White Rim Sandstone.
A second unconformity was created after the Permian sea retreated. Flood plains on an expansive lowland covered the eroded surface and mud built up in tidal flats, creating the Moenkopi Formation. Erosion returned, forming a third unconformity. The Chinle Formation was then laid down on top of this eroded surface.
Increasingly dry climates dominated the Triassic. Therefore, sand in the form of sand dunes invaded and became the Wingate Sandstone. For a time climatic conditions became wetter and streams cut channels through the sand dunes, forming the Kayenta Formation. Arid conditions returned to the region with a vengeance; a large desert spread over much of western North America and later became the Navajo Sandstone. A fourth unconformity was created by a period of erosion.
Mud flats returned, forming the Carmel Formation, and the Entrada Sandstone was laid down next. A long period of erosion stripped away most of the San Rafael Group in the area, along with any formations that may have been laid down in the Cretaceous period.
The Laramide orogeny started to uplift the Rocky Mountains 70 million years ago and with it, the Canyonlands region. Erosion intensified and when the Colorado River Canyon reached the salt beds of the Paradox Formation the overlying strata extended toward the river canyon, forming features such as The Grabens. Increased precipitation during the ice ages of the Pleistocene quickened the rate of canyon excavation along with other erosion. Similar types of erosion are ongoing, but occur at a slower rate.
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.
*Somehow* I have 377 pictures from a road trip to Chicago & Wisconsin that I took with a friend in May 2013... that never got posted until now.
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History of the Polo Inn Motel - Located next door to the McDonald's Museum on Lee Street, the Polo Inn Motel, was known as Drury Northwestern Motel from 1951-2005, and was used as Northwestern Hospital 1931-1951. Originally built as a bank in 1929, (but never operated as a bank as a result of the stock market crash). Facade has since been entirely painted and made ugly. Still, restorable. The columns painted green here are supposed to be dark blue. This spray paint is a good argument for why there should be some restrictions over what you can do to a visible public building.
(Copied research from BWChicago) - "It was built for use as a bank with offices above in 1929, but never opened because of the stock market crash. It then served as Northwestern Hospital, the Northwest suburbs' sole hospital, for 20 years until Resurrection and Holy Family opened, and was then converted to the Drury Northwestern Motel, back when River and Rand were travel routes. It turned into the Polo Inn in about 2003. It's pretty unusual architecture for a bank - I guess you'd call it Egyptian-Moorish Art Deco? I've never been able to turn up information on its architect, nor what bank it was intended for.
Oddly, the building was built a few blocks out of downtown proper, and was the only substantial building around besides the subdivision in the blocks behind it built by the same developer, H. Roy Berry.
I can't imagine it will remain a flophouse too much longer. I hope it can be turned into a McDonald's museum, or else have the facade reused in the actual downtown, maybe as an annex to the Des Plaines Theatre. Paint is removable, especially from terra cotta.
A few years ago, the Des Plaines Historical Society was floating the idea of a "history campus", since they need more room for offices, exhibits, archives, and events. The proposal calls for tearing down this historic building, putting up a new, larger building, and moving the 1906 Queen Anne Kinder House to this location next to the flashing lights of McDonald's and the roar of traffic, in a place where no houses existed in 1906. I don't think they'll ever have the money to pull off such an ambitious and ill-considered plan, although I hope they can find a suitable home in a historic building.
Further research indicates that it was designed by architects Rowe, Dillard, & Rowe in late 1927, with terra cotta by Midland Terra Cotta. Rowe usually designed in tudor style, but this is clearly more Egyptian. It looks like it was originally meant as two stores with apartments above, the bank concept must have come somewhat later.
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(See links) -
March 14 2013 -
Man Dies after Stabbing at Des Plaines Motel
Des Plaines Police Wednesday night surrounded the Polo Inn near the “5 Corners” area of Rand and Rivers roads responding to a report of a stabbing. They cordoned off the small two-story motel with yellow police tape.
Police were tight-lipped about details of the incident yesterday (Thursday) morning citing an ongoing investigation.
Deputy Police Chief Nick Treantafeles said there was a stabbing connected to a domestic dispute that occurred at the Polo Inn at 374 Lee St. at around 5:30 p.m.
"Police say a woman who fatally stabbed her boyfriend at a Des Plaines motel won’t be charged in the killing, adding the act may have been self-defense.
Des Plaines police responded to the Polo Inn, 374 S. Lee St., at 5:28 p.m. on March 6 to find Charles McGinnis, 51, with a single stab wound to the heart area, police said." -- Chicago Tribune, 3/12/1013
June 13, 2013 - 6 Tossed From ‘Unfit’ Polo Inn.
Six people were tossed out from allegedly squatting inside Polo Inn. & When police removed six inhabitants from the structurally unsound Polo Inn last month they left eight elusive residents behind. But three weeks later, police have caught at least seven of the eight cats that were still roaming the aging building. City officials declared the building unfit for occupancy. There was extensive flood damage, fire safety concerns and other issues with the aging building that made it dangerous to live. The ordeal dates back to the April flood when the area near River and Rand roads was underwater for several days. Ever since the epic April flood, the Polo Inn in Des Plaines has been unlivable & suffered damage during that flood and was deemed unfit for occupancy by city inspectors. However, at least six people continued to live in the second floor of the building, until police raided the structure in the early morning hours of June 13, removing those residents from the property.
However, one woman, Darcy Brisco, was tending to eight cats in her unit that she had to leave behind when police came. Brisco told The Journal she worked out an arrangement with city building inspectors to enter the building once a day and feed the cats.
July 5 2013 -
7 Felines Rounded Up At Polo Inn.
March 27 2014 -
City Seeks Demolition Of Polo Inn
April 7 2015 -
Des Plaines Looks To Demolish old Polo Inn
February 3 2016 -
End Seems Near For ‘Five Corners’ Inn. Located near Five Corners and River and Rand roads, the Polo Inn was at one time a hospital.The days of a worn out two-story building in the “Five Corners” area of Rand and River roads appear to be numbered as the city of Des Plaines is preparing to file in Skokie court this week a complaint to force the demolition of the former Polo Inn motel. Ever since the 2013 devastating flood that hit Five Corners and neighborhoods along the Des Plaines River, the city has had its eye on having the building demolished.
October 28 2016 -
Wrecking equipment stands ready to spring into action next to the long shuttered Polo Inn building on Lee Street near River and Rand roads in Des Plaines Friday. After lengthy condemnation court proceedings, the once former motel and hospital will be demolished today (Friday). It has been damaged many times by water when the River-Rand intersection has flooded.
August 30 2020 - Google street view of 374 Lee St
374 Lee St. Des Plaines, IL. 052813.
67 Park Place, Bloomfield, New Jersey, October, 2024
Chamonix 4x5 view camera, 150 mm Symmar S lens on FFP Frankenstein film developed in Pyrocat HD developer
The High Level Bridge is a road and railway bridge spanning the River Tyne between Newcastle upon Tyne and Gateshead in North East England. It is considered the most notable historical engineering work in the city. It was built by the Hawks family from 5,050 tons of iron. George Hawks, Mayor of Gateshead, drove in the last key of the structure on 7 June 1849, and the bridge was officially opened by Queen Victoria later that year.
It was designed by Robert Stephenson to form a rail link towards Scotland for the developing English railway network; a carriageway for road vehicles and pedestrians was incorporated to generate additional revenue. The main structural elements are tied cast-iron arches.
Notwithstanding the considerable increase in the weight of railway vehicles since it was designed, it continues to carry rail traffic, although the King Edward bridge nearby was opened in 1906 to ease congestion. The roadway is also still in use, although with a weight restriction. It is a Grade I listed structure.
In 1835, the Newcastle and Carlisle Railway (N&CR) Act authorised the line to approach Newcastle to a terminus at Redheugh, on the south bank of the River Tyne, close to the end of the present-day New Redheugh Bridge. The Act also authorised a crossing of the Tyne there, giving rail access to the north shore quays. The river was shallow at this point, and the bridge would have been at a low level, only 20 ft (6.1 m) above high water. The line would then have climbed to a terminus at the Spital, near Neville Street and the east end of the present-day Newcastle Central station. The climb was to be at a gradient of 1 in 22 and would have been operated by a stationary steam engine with rope haulage.
Hitherto railways in the region had had a local focus, but now the Great North of England Railway (GNER) obtained authorising Acts to build from Newcastle to York, forming part of a continuous trunk railway network to connect to London; the project was controlled by George Hudson, the so-called Railway King. At first the GNER was content to get access to the N&CR Newcastle terminus, by connecting with the N&CR at Redheugh and running over its line across the Tyne and up to the Spital. This had the advantage of avoiding a separate, and expensive, crossing of the river, but would have meant a steep descent to Redheugh as the GNER line approached on high ground from the Team Valley, only to climb once again to the Spital. Moreover, William Brandling had made known his intention to reach Newcastle from his line by running at a high level through Gateshead. On 25 April 1837, the N&CR decided to build to their south side, low-level terminus at Redheugh, but to leave the issue of the Tyne crossing open.
Richard Grainger was a developer in Newcastle, and had acquired lands at Elswick (on the north bank of the Tyne west of the proposed Redheugh crossing). In 1836, he published a pamphlet recommending a crossing of the Tyne there, and the formation of spacious railway terminal accommodation there. Drawing attention to the limited scope for extending eastwards from the Spital, and "in the event of an Edinburgh Railway also terminating in this situation, the interchange of passengers, goods, and cattle would be greatly increased".
Grainger's plan was not adopted, and the Brandling Junction Railway reached Gateshead in 1839. The GNER ran out of money and it was superseded in Hudson's railway empire by the Newcastle and Darlington Junction Railway, which opened its line using the Brandling Junction Railway from the south east instead of through the Team Valley. The Brandling Junction line had a terminus in Gateshead at Greenesfield at a high level, and the N&CR line was built climbing on an inclined plane at a gradient of 1 in 23 from Redheugh to reach that. The Newcastle and Darlington Junction Railway opened its line from the south to Pelaw, allowing its trains to reach Gateshead over the Brandling Junction line, in 1844. The tables had been turned, and indeed for a while Greenesfield was the de facto main station for the conurbation of Newcastle and Gateshead.
John and Benjamin Green were a father and son architectural practice active in Newcastle. In 1841 Benjamin Green had proposed a high level bridge for road traffic, substantially on the alignment of the actual High Level Bridge; and sensing the commercial climate he explained how it could be adapted for railway use. He failed to get any financial support, but in 1843 George Hudson was looking for ways to extend his railway network northwards, and the Greens' scheme fitted with his takeover of the Newcastle and Darlington Junction Railway; the line got its authorising Act on 22 May 1844, and the Act included the road bridge.
The Newcastle and North Shields Railway had opened in 1839 from its own terminus at Carliol Square, on the north-east edge of Newcastle. As a purely local concern, the disconnection was not important, but interest gathered in a railway to central Scotland; the "Edinburgh Railway" foreseen by Grainger. A Scottish concern, the North British Railway, had got its Act of Parliament the previous year to build as far south as Berwick (later known as Berwick-upon-Tweed.
Now Hudson was intent on capturing the line to Edinburgh for his empire, and he encouraged the development of railway plans to get there; the route such a line might take continued to generate considerable controversy. There was still ambiguity about Hudson's intentions for the bridge—an easier crossing point at Bill Quay, two miles downstream had been considered—and Newcastle Town Council sought undertakings from him. In addition, he promised a footway crossing; this was apparently not a sweetener to the Town Council, but a commercial decision, expected to bring in £250 a week. The footway crossing was later extended to include horse-drawn vehicles.
Finally, the Newcastle and Berwick Railway was authorised by Act of Parliament of 31 July 1845. The line would cross the Greens' high level bridge, starting from the Gateshead Greenesfield station, and commitments made to the building of a bridge by the Newcastle and Darlington Junction Railway were transferred to the Newcastle and Berwick Railway.
The bridge was to be designed by Robert Stephenson; T E Harrison did the detailed design work.
The height of the railway, at about 120 ft (37 m) above high water, was determined by the level of the Brandling Junction line in Gateshead. A double-deck configuration was selected because of road levels on the approaches, and to avoid the excess width of foundations which a side-by-side arrangement would require. The deck width was determined by the useful roadway width plus the width of structural members, which gave the railway deck the width for three tracks.
The foundations were to be difficult because of the poor ground conditions in the river, and this ruled out an all-masonry structure, so cast iron or wrought iron was inevitable for the superstructure. A tied arch (or bow-string) design was favoured because the outward thrust imposed by an arch is contained by the tie; no abutments capable of resisting the thrust could be provided here.
Stephenson had used this configuration before; he recorded that, "The earliest railway bridge on the bowstring principle is that over the Regent's Canal, near Chalk Farm, on the London and Birmingham Railway".
The arch would consist of iron ribs. Fawcett says, "The reasons for not using wrought iron was due to some engineers' distrust of rivetting, the relatively small size of wrought iron plates then available, and the higher cost… On 1 October 1845 when the Newcastle and Berwick Board instructed T E Harrison for their bridges, none of the uses of wrought iron had been developed far enough to be considered as an alternative to cast iron for the High Level Bridge. A tubular bridge might have been considered by Robert Stephenson but the distance between solid and reasonably shallow foundations would have given a span much larger than the Britannia Bridge."
The depth of rock in the riverbed resulted in a height of 140 ft (43 m) from there to the superstructure. Three river piers were permitted by the Tyne Improvement Commissioners, and therefore four river spans of 125 ft (38 m) were decided on; there were additional subsidiary spans on the shore.
The cast iron arch ribs are 3 ft 6 in (1.07 m) deep at the crown, increasing to 3 ft 9 in (1.14 m) at the springing, with 12-inch (30 cm) flanges; the flanges and webs were three inches thick; in the case of the inner ribs, and two inches for the outer ribs. The rise was 17 ft 6 in (5.33 m), determined by the desired geometry to confine the horizontal thrust within bounds. Each arch was cast in five sections, bolted together.
Stephenson described the tie bars:
The ties consist of flat wrought-iron bars, 7 inches by 1 inch of best scrap iron, with eyes of 3½ inches diameter, bored out of the solid, and pins turned and fitted closely. Each external rib is tied by four of these bars, and each internal rib by eight. The sectional area of each external tie is 28 [square] inches, and of each internal tie 56 [square] inches, giving a total area of 168 square inches. These bars were all tested to 9 tons on the square inch.
The rail deck is supported above the arches by twelve 14-inch (360 mm) square columns at 9 feet 11 inches (3.02 m) centres. Suspension rods supported the road deck, and both decks had two layers of diagonally laid three-inch deck timbers on suitable wrought iron cross girders (and rail-bearers in the case of the rail deck).
The main contractors for the ironwork were Hawks, Crawshay, and Sons, who were assisted by John Abbot and Co., of Gateshead Park Works, and Losh Wilson and Bell, of Walker Ironworks, in the production of the castings. The tender was accepted at £112,000. The contract for the bridge piers and land arches and for the Newcastle Viaduct were won by John Rush and Benjamin Lawton of York for £94,000 and £82,500 respectively. The total cost of the contracts at 1999 prices would be over £30 million.
The first masonry was laid on 12 January 1847. A temporary timber viaduct on the east side was ready on 20 August 1848.
Timber coffer dams were constructed; they were 76 ft 6 in (23.32 m) by 29 ft (8.8 m) with two skins, the space between being filled with puddle clay. James Nasmyth had a novel design of steam pile driver; it had first been used in Devonport Docks in 1845; it could deliver 60 to 70 blows a minute; the cycle time with the hand-operated pile drivers formerly in use was four minutes. The drop weight was 1½ tons and its stroke was 2 ft 9 in (0.84 m); one was purchased from Nasmyth.
The ground gave considerable trouble during construction; Stephenson recorded:
Many difficulties occurred in driving the piles which considerably retarded the progress of the work, and, among others, the peculiar effect of ebb and flow during this operation is worthy of note. At flood-tide, the sand became so hard as almost totally to resist the utmost efforts of driving, while at ebb the sand was quite loose, and allowed of doing so with facility. It was therefore found necessary to abandon the driving on many occasions during high water. The difference between high and low water is 11 feet 6 inches. Another difficulty arose from the quicksands beneath the foundations. Although the piles were driven to the rock bottom, the water forced its way up, baffling the attempts to fill in between them; this, however, was remedied by using a concrete made of broken stone and Roman cement, which was continually thrown in until the bottom was found to be secure.
The arch ribs were erected in section by travelling crane; each arch was temporarily erected at the contractor’s works. The first was placed on 10 July 1848, and the erection of the ironwork was quick.
Already on 29 August 1848, it was possible to pass a special train over the first arch, and over a temporary structure for the rest of the crossing:
The High Level Bridge Over the Tyne: This important junction between the York and Newcastle and the Newcastle and Berwick Railway has been completed, and the event was celebrated on Tuesday last. In the afternoon of that day, a train of [specially invited] passengers passed along the temporary timber viaduct from the station at Gateshead to the station at Newcastle. Mr Hudson and several other Directors of the York, Newcastle, and Berwick line, who had been visiting Sunderland ... proceeded in a special train from that town to Gateshead... Several carriages were then added to the special train, and an open truck placed at each end, in which bands of music were stationed. The shrill sound of the whistle gave the signal for a royal salute, under the booming of which the train passed along the line, the band playing, and the thousands assembled to witness the event, rending the air with joyous acclamation Upon reaching the bridge, the bands struck up the well-known local air of "The Keel Row" which they continued till the train had reached the solid ground on the northern side of the river... The train proceeded to the Newcastle and Berwick station, where the company alighted and walked in procession to the Queen’s Head Inn, where a magnificent entertainment had been provided for the Directors and their friends, by the Mayor of Newcastle.
[From the south abutment of the High Level Bridge] and the river pier on the south side, the cast iron arch and road-way are nearly completed, and the second arch will be in progress in the course of a few weeks. From the middle of the first arch, the line curves to a temporary timber viaduct erected along the west side of the intended bridge. The height of this viaduct is one hundred and twenty feet to the level of the rails; it is built upon piles, which are driven between thirty and forty feet into the bed of the river. Its stability was sufficiently tested on Monday, when Captain Leffan (sic), the Government Inspector of Railways, examined it preparatory to the opening. On that day, two powerful engines weighing upwards of seventy tons, traversed it at different degrees of speed for between two and three hours; the weight would be about one ton to a foot, being four or five times greater than the temporary structure will ever be required to bear, and the result was, in the highest degree, satisfactory.
Among the company in the train were four ladies, who are deserving of honourable mention, from the courage they displayed in accompanying it, namely, Mrs Nichs. Wood, and Miss F. Wood, Mrs I. L. Bell, and her sister, Miss Pattinson of Washington. As the train passed steadily over the bridge the anxiety of the immense multitude seemed intense, and the scene was truly exciting, yet fearful—not only from the lofty eminence occupied by the train but, from the apparent narrowness and nakedness of the platform on which it rolled along. It seemed from its noiselessness, rather an aerial flight, than the rattling sweep of the iron horse.
Ordinary traffic appears to have used the temporary single line structure after this date.
The eastern track was ready for an inspection by Captain Laffan, Inspecting Office for the Board of Trade, when he visited on 11 August 1849; a load test with four tender locomotives and eighteen wagons loaded with ballast, a total weight of 200 tons. Laffan approved the bridge:
I believe all the works of the bridge are completed, and that I believe it to be perfectly secure and safe. The Company have as yet only laid one line of rails over this structure, and I beg to recommend that permission be given to open that one line.
The first passenger train crossed the completed structure on the morning of 15 August 1849.
Queen Victoria formally inaugurated the bridge on passing through by train on 28 September 1849.
The Queen at Newcastle: Her Majesty yesterday honoured this ancient borough with her presence. The event was one of universal and all-engrossing interest... The morning, unfortunately, was dull and the weather unsettled, giving forebodings of a wet and uncomfortable day... Notwithstanding, however, the unfavourable weather dense crowds assembled at every spot in this locality, where a view of the royal carriage could be obtained, and many remained for hours exposed to the weather in order that they might retain the places which at an earlier period of the morning they had secured. The bridge was densely lined with people, and the platform was well covered, though not inconveniently crowded. A profusion of banners were displayed on this elegant and substantial structure, and from nearly all the public and many of the private buildings both in Newcastle and Gateshead. The vessels in the river hoisted their flags mast-high on the occasion, and the church bells of the two towns rung many a merry peal in honour of the royal visit... Pursuant to a request issued by the Mayor, most of the shops were closed about 11 o’clock, and the manufacturers were desired by our worthy chief magistrate "not to produce smoke between that hour and one," with which we believe, they generally complied... At precisely twenty minutes past twelve, the royal carriage appeared in sight, and when it reached the Spital, a splendid locomotive, built by the celebrated house of Stephenson and Co., gaily decorated and bearing on its front "God save the Queen" surmounted by a crown, and a suitable inscription encircling the boiler, was attached to the train. It then slowly proceeded to the centre of the colossal fabric, amidst bursts of loud and rapturous cheering from the assembled thousands, her Majesty repeatedly acknowledging these marked demonstrations of loyalty and affection from her faithful and attached subjects.
The Mayors of Newcastle and Gateshead presented a formal address. The queen travelled in the royal carriage belonging to the London and North Western Railway.
In other carriages were members of her Majesty’s suite and the directors of the York, Newcastle, and Berwick Railway. The engine drawing the royal train was under the direction of Mr T. E. Harrison, the resident engineer, and driven by Mr Thos. Carr... After staying altogether from five to ten minutes, the train was again put in motion, and amidst firing of artillery and rapturous plaudits from the dense throng, proceeded en route to Darlington.
The bridge and its immediate approaches had cost £243,000.
The road deck was re-opened only in a southbound (towards Gateshead) direction and carries only buses and taxis; the one-way operation is required because of width considerations after protection to the structural members was inserted. Pedestrians and cyclists use the bridge freely. Railway traffic continues in full use of the bridge, although the majority of mainline trains use the King Edward VII bridge for reasons of convenience.
Anybody living in the Midwest of the US right now will tell you this couldn't have been taken this year. Here as 2015 comes to a close, we're being hit with very warm weather, leaving many of us with a brown XMAS. At the beginning of the year, however, we did have a bit of snow to shoot. By the time I got around to processing that film, it was already melting. If there was ever a time I'd like to think about snow, it's XMAS Eve.
Tachihara 8x10 Double Extension
Nikkor T 600 ED
1/2 sec @ f/32ish + front rise
Ilford HP5+ @ ASA 200
Pyrocat HD 1:1.5:100
Canyonlands National Park is an American national park located in southeastern Utah near the town of Moab. The park preserves a colorful landscape eroded into numerous canyons, mesas, and buttes by the Colorado River, the Green River, and their respective tributaries. Legislation creating the park was signed into law by President Lyndon Johnson on September 12, 1964.
The park is divided into four districts: the Island in the Sky, the Needles, the Maze, and the combined rivers—the Green and Colorado—which carved two large canyons into the Colorado Plateau. While these areas share a primitive desert atmosphere, each retains its own character. Author Edward Abbey, a frequent visitor, described the Canyonlands as "the most weird, wonderful, magical place on earth—there is nothing else like it anywhere."
In the early 1950s, Bates Wilson, then superintendent of Arches National Monument, began exploring the area to the south and west of Moab, Utah. After seeing what is now known as the Needles District of Canyonlands National Park, Wilson began advocating for the establishment of a new national park that would include the Needles. Additional explorations by Wilson and others expanded the areas proposed for inclusion into the new national park to include the confluence of Green and Colorado rivers, the Maze District, and Horseshoe Canyon.
In 1961, Secretary of the Interior Stewart Udall was scheduled to address a conference at Grand Canyon National Park. On his flight to the conference, he flew over the Confluence (where the Colorado and Green rivers meet). The view apparently sparked Udall's interest in Wilson's proposal for a new national park in that area and Udall began promoting the establishment of Canyonlands National Park.
Utah Senator Frank Moss first introduced legislation into Congress to create Canyonlands National Park. His legislation attempted to satisfy both nature preservationists' and commercial developers' interests. Over the next four years, his proposal was struck down, debated, revised, and reintroduced to Congress many times before being passed and signed into creation.
In September, 1964, after several years of debate, President Lyndon B. Johnson signed Pub.L. 88–590, which established Canyonlands National Park as a new national park. Bates Wilson became the first superintendent of the new park and is often referred to as the "Father of Canyonlands."
The Colorado River and Green River combine within the park, dividing it into three districts called the Island in the Sky, the Needles, and the Maze. The Colorado River flows through Cataract Canyon below its confluence with the Green River.
The Island in the Sky district is a broad and level mesa in the northern section of the park, between the Colorado and Green rivers. The district has many viewpoints overlooking the White Rim, a sandstone bench 1,200 feet (370 m) below the Island, and the rivers, which are another 1,000 feet (300 m) below the White Rim.
The Needles district is located south of the Island in the Sky, on the east side of the Colorado River. The district is named for the red and white banded rock pinnacles which are a major feature of the area. Various other naturally sculpted rock formations are also within this district, including grabens, potholes, and arches. Unlike Arches National Park, where many arches are accessible by short to moderate hikes, most of the arches in the Needles district lie in backcountry canyons, requiring long hikes or four-wheel drive trips to reach them.
The Ancestral Puebloans inhabited this area and some of their stone and mud dwellings are well-preserved, although the items and tools they used were mostly removed by looters. The Ancestral Puebloans also created rock art in the form of petroglyphs, most notably on Newspaper Rock along the Needles access road.
The Maze district is located west of the Colorado and Green rivers. The Maze is the least accessible section of the park, and one of the most remote and inaccessible areas of the United States.
A geographically detached section of the park located north of the Maze district, Horseshoe Canyon contains panels of rock art made by hunter-gatherers from the Late Archaic Period (2000-1000 BC) pre-dating the Ancestral Puebloans. Originally called Barrier Canyon, Horseshoe's artifacts, dwellings, pictographs, and murals are some of the oldest in America. The images depicting horses date from after 1540 AD, when the Spanish reintroduced horses to America.
Since the 1950s, scientists have been studying an area of 200 acres (81 ha) completely surrounded by cliffs. The cliffs have prevented cattle from ever grazing on the area's 62 acres (25 ha) of grassland. According to the scientists, the site may contain the largest undisturbed grassland in the Four Corners region. Studies have continued biannually since the mid-1990s. The area has been closed to the public since 1993 to maintain the nearly pristine environment.
Mammals that roam this park include black bears, coyotes, skunks, bats, elk, foxes, bobcats, badgers, ring-tailed cats, pronghorns, desert bighorn sheep, and cougars. Desert cottontails, kangaroo rats and mule deer are commonly seen by visitors.
At least 273 species of birds inhabit the park. A variety of hawks and eagles are found, including the Cooper's hawk, the northern goshawk, the sharp-shinned hawk, the red-tailed hawk, the golden and bald eagles, the rough-legged hawk, the Swainson's hawk, and the northern harrier. Several species of owls are found, including the great horned owl, the northern saw-whet owl, the western screech owl, and the Mexican spotted owl. Grebes, woodpeckers, ravens, herons, flycatchers, crows, bluebirds, wrens, warblers, blackbirds, orioles, goldfinches, swallows, sparrows, ducks, quail, grouse, pheasants, hummingbirds, falcons, gulls, and ospreys are some of the other birds that can be found.
Several reptiles can be found, including eleven species of lizards and eight species of snake (including the midget faded rattlesnake). The common kingsnake and prairie rattlesnake have been reported in the park, but not confirmed by the National Park Service.
The park is home to six confirmed amphibian species, including the red-spotted toad, Woodhouse's toad, American bullfrog, northern leopard frog, Great Basin spadefoot toad, and tiger salamander. The canyon tree frog was reported to be in the park in 2000, but was not confirmed during a study in 2004.
Canyonlands National Park contains a wide variety of plant life, including 11 cactus species,[34] 20 moss species, liverworts, grasses and wildflowers. Varieties of trees include netleaf hackberry, Russian olive, Utah juniper, pinyon pine, tamarisk, and Fremont's cottonwood. Shrubs include Mormon tea, blackbrush, four-wing saltbush, cliffrose, littleleaf mountain mahogany, and snakeweed
Cryptobiotic soil is the foundation of life in Canyonlands, providing nitrogen fixation and moisture for plant seeds. One footprint can destroy decades of growth.
According to the Köppen climate classification system, Canyonlands National Park has a cold semi-arid climate ("BSk"). The plant hardiness zones at the Island in the Sky and Needles District Visitor Centers are 7a with an average annual extreme minimum air temperature of 4.0 °F (-15.6 °C) and 2.9 °F (-16.2 °C), respectively.
The National Weather Service has maintained two cooperative weather stations in the park since June 1965. Official data documents the desert climate with less than 10 inches (250 millimetres) of annual rainfall, as well as hot, mostly dry summers and cold, occasionally wet winters. Snowfall is generally light during the winter.
The station in The Neck region reports an average January temperature of 29.6 °F and an average July temperature of 79.3 °F. Average July temperatures range from a high of 90.8 °F (32.7 °C) to a low of 67.9 °F (19.9 °C). There are an average of 45.7 days with highs of 90 °F (32 °C) or higher and an average of 117.3 days with lows of 32 °F (0 °C) or lower. The highest recorded temperature was 105 °F (41 °C) on July 15, 2005, and the lowest recorded temperature was −13 °F (−25 °C) on February 6, 1989. Average annual precipitation is 9.33 inches (237 mm). There are an average of 59 days with measurable precipitation. The wettest year was 1984, with 13.66 in (347 mm), and the driest year was 1989, with 4.63 in (118 mm). The most precipitation in one month was 5.19 in (132 mm) in October 2006. The most precipitation in 24 hours was 1.76 in (45 mm) on April 9, 1978. Average annual snowfall is 22.8 in (58 cm). The most snowfall in one year was 47.4 in (120 cm) in 1975, and the most snowfall in one month was 27.0 in (69 cm) in January 1978.
The station in The Needles region reports an average January temperature of 29.7 °F and an average July temperature of 79.1 °F.[44] Average July temperatures range from a high of 95.4 °F (35.2 °C) to a low of 62.4 °F (16.9 °C). There are an average of 75.4 days with highs of 90 °F (32 °C) or higher and an average of 143.6 days with lows of 32 °F (0 °C) or lower. The highest recorded temperature was 107 °F (42 °C) on July 13, 1971, and the lowest recorded temperature was −16 °F (−27 °C) on January 16, 1971. Average annual precipitation is 8.49 in (216 mm). There are an average of 56 days with measurable precipitation. The wettest year was 1969, with 11.19 in (284 mm), and the driest year was 1989, with 4.25 in (108 mm). The most precipitation in one month was 4.43 in (113 mm) in October 1972. The most precipitation in 24 hours was 1.56 in (40 mm) on September 17, 1999. Average annual snowfall is 14.4 in (37 cm). The most snowfall in one year was 39.3 in (100 cm) in 1975, and the most snowfall in one month was 24.0 in (61 cm) in March 1985.
National parks in the Western US are more affected by climate change than the country as a whole, and the National Park Service has begun research into how exactly this will effect the ecosystem of Canyonlands National Park and the surrounding areas and ways to protect the park for the future. The mean annual temperature of Canyonlands National Park increased by 2.6 °F (1.4 °C) from 1916 to 2018. It is predicted that if current warming trends continue, the average highs in the park during the summer will be over 100 °F (40 °C) by 2100. In addition to warming, the region has begun to see more severe and frequent droughts which causes native grass cover to decrease and a lower flow of the Colorado River. The flows of the Upper Colorado Basin have decreased by 300,000 acre⋅ft (370,000,000 m3) per year, which has led to a decreased amount of sediment carried by the river and rockier rapids which are more frequently impassable to rafters. The area has also begun to see an earlier spring, which will lead to changes in the timing of leaves and flowers blooming and migrational patterns of wildlife that could lead to food shortages for the wildlife, as well as a longer fire season.
The National Park Service is currently closely monitoring the impacts of climate change in Canyonlands National Park in order to create management strategies that will best help conserve the park's landscapes and ecosystems for the long term. Although the National Park Service's original goal was to preserve landscapes as they were before European colonization, they have now switched to a more adaptive management strategy with the ultimate goal of conserving the biodiversity of the park. The NPS is collaborating with other organizations including the US Geological Survey, local indigenous tribes, and nearby universities in order to create a management plan for the national park. Right now, there is a focus on research into which native plants will be most resistant to climate change so that the park can decide on what to prioritize in conservation efforts. The Canyonlands Natural History Association has been giving money to the US Geological Survey to fund this and other climate related research. They gave $30,000 in 2019 and $61,000 in 2020.
A subsiding basin and nearby uplifting mountain range (the Uncompahgre) existed in the area in Pennsylvanian time. Seawater trapped in the subsiding basin created thick evaporite deposits by Mid Pennsylvanian. This, along with eroded material from the nearby mountain range, became the Paradox Formation, itself a part of the Hermosa Group. Paradox salt beds started to flow later in the Pennsylvanian and probably continued to move until the end of the Jurassic. Some scientists believe Upheaval Dome was created from Paradox salt bed movement, creating a salt dome, but more modern studies show that the meteorite theory is more likely to be correct.
A warm shallow sea again flooded the region near the end of the Pennsylvanian. Fossil-rich limestones, sandstones, and shales of the gray-colored Honaker Trail Formation resulted. A period of erosion then ensued, creating a break in the geologic record called an unconformity. Early in the Permian an advancing sea laid down the Halgaito Shale. Coastal lowlands later returned to the area, forming the Elephant Canyon Formation.
Large alluvial fans filled the basin where it met the Uncompahgre Mountains, creating the Cutler red beds of iron-rich arkose sandstone. Underwater sand bars and sand dunes on the coast inter-fingered with the red beds and later became the white-colored cliff-forming Cedar Mesa Sandstone. Brightly colored oxidized muds were then deposited, forming the Organ Rock Shale. Coastal sand dunes and marine sand bars once again became dominant, creating the White Rim Sandstone.
A second unconformity was created after the Permian sea retreated. Flood plains on an expansive lowland covered the eroded surface and mud built up in tidal flats, creating the Moenkopi Formation. Erosion returned, forming a third unconformity. The Chinle Formation was then laid down on top of this eroded surface.
Increasingly dry climates dominated the Triassic. Therefore, sand in the form of sand dunes invaded and became the Wingate Sandstone. For a time climatic conditions became wetter and streams cut channels through the sand dunes, forming the Kayenta Formation. Arid conditions returned to the region with a vengeance; a large desert spread over much of western North America and later became the Navajo Sandstone. A fourth unconformity was created by a period of erosion.
Mud flats returned, forming the Carmel Formation, and the Entrada Sandstone was laid down next. A long period of erosion stripped away most of the San Rafael Group in the area, along with any formations that may have been laid down in the Cretaceous period.
The Laramide orogeny started to uplift the Rocky Mountains 70 million years ago and with it, the Canyonlands region. Erosion intensified and when the Colorado River Canyon reached the salt beds of the Paradox Formation the overlying strata extended toward the river canyon, forming features such as The Grabens. Increased precipitation during the ice ages of the Pleistocene quickened the rate of canyon excavation along with other erosion. Similar types of erosion are ongoing, but occur at a slower rate.
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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Developer Console (Free camera) | Hud Toggle
Original Photo 5k (15Mp)
Reshade
Photoshop Edit
2019-02-09
Pentax Spotmatic II
Fujinon EBC 55mm f/1.8 lens
Kodak Tri-X 400 (1600-push) 35mm film
Adox Rodinal (1+50) developer
20ºC - 19min
On the way to Presido, had to stop for this. Warning, subject in photo is much farther away appears!
Homemade coffee based film developer.
My formula:
Dissolve 5tbs instant coffee in 6oz water.
Dissolve 4tbs washing soda in 2oz of water. Stir until uniform.
Add soda solution to coffee.
Dissolve 1000mg Vitamin C in 2oz water. Dissolves fast.
Add Vitamin C solution to coffee/washing soda mixture.
Put in freezer until temp lowers to 20C.
I developed for 15 minutes, agitating 15 seconds for every minute of development.
Fujifilm X-M1, XC16-50mmF3.5-5.6 OIS, all pre-production, RAW / Iridient Developer & Apple Aperture
Read the X-Pert Corner article about using the X-M1 and the two new lenses (XF27mmF2.8 & XC16-50mmF3.5-5.6 OIS) on June 27th.
Free PDF reading samples from my current book on the X-Pro1 (also suitable for X-E1 users):
English: Mastering the Fujifilm X-Pro1 (reading samples, 65 pages, PDF)
German: Das Fujifilm X-Pro1 Handbuch (65 Seiten Leseproben, PDF)
Film: Kodak TRI-X 400
Camera: Nikon F100
Developer: Rodinal R09 1+50 for 13min @20C
Scanner: Plustek OpticFilm 7600i
identical developer and toner as previously described, but different results of course
left: bleach 1+50 40 secs, MT5 Sepia 1+10 50 secs
middle: MT5 Sepia 1+10 4 mins
right: MT5 Sepia 1+10 4 mins, bleach 1+50 1 min, MT5 30 secs
Contax RTS III. Sigma Zoom Master 35~70 mm 1:2.8~4. Película Argenti Reporter Film 400 ISO forzado a /pushed to 1600 ISO. Reveladore feitoaman / handmade developer Patapalo Puxador 1+9, 15 minutos, 25ºC. Papel Forte Fortezo FN3. Reveladores feitosaman / handmade developers Patapalo Caldolith (1+1+5) + Patapalo Fastone (1+30). Virado al selenio con / Selenium toned with Gago Selentoner. Original 30 x 40 cm.
Soportales da Ferrería, Pontevedra. Outono 2011
Camera Canon EOS 7D
Exposure 0.1 sec (1/10)
Aperture f/9.0
Focal Length 11 mm
Flash fired to the left and one to the right. Set off with a remote
Print developed in coffee.
Developer: 2 teespoons Nesskaffee Espresso, 3 Teespoons soda (natriumcarbonate), 200ml water
Paper: AGFA MCP 24x30
Film: Fuji Neopan Acros in Moersch Tanol Speed
Camera: Hasselblad 500C/M
Lens: Zeiss Distagon CF 60mm f/3.5
Film: Ilford HP5+
Developer: Kodak HC-110 (1+49, 8 mins) Development details on FilmDev
Scanner: Epson 4180
3409