View allAll Photos Tagged EXPAND
365/2021 - Expanding Horizons ~ 112/365
Thank you to everyone who pauses long enough to look at my photo. All comments and Faves are very much appreciated
Description: G292.0+1.8 is a young supernova remnant located in our galaxy. This deep Chandra image shows a spectacularly detailed, rapidly expanding shell of gas that is 36 light years across and contains large amounts of oxygen, neon, magnesium, silicon and sulfur. Astronomers believe that this supernova remnant, one of only three in the Milky Way known to be rich in oxygen, was formed by the collapse and explosion of a massive star. Supernovas are of great interest because they are a primary source of the heavy elements believed to be necessary to form planets and life.
Creator/Photographer: Chandra X-ray Observatory
NASA's Chandra X-ray Observatory, which was launched and deployed by Space Shuttle Columbia on July 23, 1999, is the most sophisticated X-ray observatory built to date. The mirrors on Chandra are the largest, most precisely shaped and aligned, and smoothest mirrors ever constructed. Chandra is helping scientists better understand the hot, turbulent regions of space and answer fundamental questions about origin, evolution, and destiny of the Universe. The images Chandra makes are twenty-five times sharper than the best previous X-ray telescope. NASA's Marshall Space Flight Center in Huntsville, Ala., manages the Chandra program for NASA's Science Mission Directorate in Washington. The Smithsonian Astrophysical Observatory controls Chandra science and flight operations from the Chandra X-ray Center in Cambridge, Massachusetts.
Medium: Chandra telescope x-ray
Date: 2006
Persistent URL: www.chandra.harvard.edu/photo/2007/g292/
Repository: Smithsonian Astrophysical Observatory
Collection: X-rays Collection - X-rays are electromagnetic radiations beyond ultra-violet which form a shadow image of the internal structure of the object when passed through a solid object and allowed to act upon a sensitive emulsion.
Gift line: X-ray: NASA/CXC/Penn State/S.Park et al.;
Optical: Pal.Obs. DSS.
Accession number: G292
365/2021 - Expanding Horizons ~ 304/365
Brown, peaty water flowing down our normally quiet little river after a night of heavy rainfall on the moors.
Thank you to everyone who pauses long enough to look at my photo. All comments and Faves are very much appreciated
iss047e061100 (4/16/2016) --- The Bigelow Expandable Activity Module (BEAM) was installed to the International Space Station on April 16, 2016 at 5:36 a.m. EDT. Following extraction from SpaceX's Dragon cargo craft using the Canadarm2 robotic arm, ground controllers installed the expandable module to the aft port of Tranquility. Astronauts will enter BEAM on an occasional basis to conduct tests to validate the module’s overall performance and the capability of expandable habitats.
NASA is investigating concepts for habitats that can keep astronauts healthy during space exploration. Expandable habitats are one such concept under consideration – they require less payload volume on the rocket than traditional rigid structures, and expand after being deployed in space to provide additional room for astronauts to live and work inside.
I had an accident on my ‘ability’ scooter yesterday at Burry Port Harbour. It was very cold and very windy there so we decided to come home which meant crossing a narrow bridge. As I was half way across, I saw a man coming towards me and shouted out “Keep your distance, please!” but he carried on regardless so I went into reverse on my scooter and whether it was driver error on my part, or the fact that I don’t have eyes in the back of my head, I hit a kerb so hard that I got flung out of my scooter down a short but steep embankment. The front basket flew off as did the under basket. An old gent jumped up from a bench to help me up, but Huw who’d already gone ahead came running “Don’t touch her. Leave her alone!” in case I’d broken any bones.
Thankfully I got up of my own accord, unharmed which is nothing short of a miracle. Huw put the scooter pieces back together- they too were unharmed. (Pic of my ‘alternative legs’ in comments )
If there’s a moral to this then please everyone, if you see anyone that is less abled than you , then keep your distance – the person you see might not be able to move out of your way, whether it’s a pedestrian or someone like me who is unable to walk unaided....
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.
Odda is a town and administrative center in Ullensvang municipality in Vestland county in Norway. The town is located deep in the Sørfjorden in Hardanger , and has 4,764 inhabitants as of 1 January 2023 . Odda was the administrative center of Odda municipality , which on 1 January 2020 was merged with Jondal and Ullensvang to form the new Ullensvang municipality.
In 2009 , the industrial heritage in Odda-Tyssedal was listed on Norway's tentative list for UNESCO's World Heritage List , together with the Rjukan–Notodden industrial heritage .
Public services
Odda hospital is a local hospital for the municipalities of Eidfjord, Jondal, Odda and Ullensvang.
Odda secondary school offers both vocational and study specialist educations.
Business
Odda is known as an industrial location, with companies such as Odda Smelteverk , Boliden Odda (formerly Norzink ) and Tinfos Titan & Iron (TTI).
History
Tourism and hotel management
Before industrial activity in Odda began around 1910, Odda was a popular tourist destination which, among other things, attracted many foreigners who wanted to experience the scenic area with glaciers, fjords and waterfalls. This laid the foundation for several people to start hotel operations on the site.
Some of the most popular destinations for tourists visiting Odda were Låtefossen and Espelandsfossen .
Shuttle station, steamship wharf and steamship expedition
Baard Jakobsen Aga (1812–1895) received a merchant license in Odda in 1861, and in 1864 took over the shuttle station that was in operation in Odda. Then he secured a new plot of land where he built a hotel which was called alternately Prestegårds Hotel and Agas Hotel. In 1868 he became a post opener and steamship dispatcher, and he then had a steamship wharf and dispatch house built at Almerket. He had previously expanded the hotel business, but in 1888 he inaugurated a new hotel building, the "new Agas Hotel". In the 20th century, the large hotel building was used for other purposes, including Rita's bakery, which led to the building being called "Ritagården" colloquially. Agas Hotel/Ritagården was demolished in 1978.
From guest house to Hotel Hardanger
The start of hotel operations at Odda occurred around 1845, when a man named Monsen started an inn on the site. Monsen went bankrupt in the 1860s, and the inn was bought by a man named Wetshus. He continued to run the hotel business. After Wetshus had died, the two brothers Sven and Mikal Tollefsen became his successors in the early 1880s, with financial support from a rich Englishman. The Tollefsen brothers carried out a major renovation of the former guest house. When Sven Tollefsen died, Mikal Tollefsen became the hotel's sole owner.
Tollefsen also bought Agas Hotel, which Baard Jakobsen Aga had started.
On 9 August 1895, the then Hotel Hardanger was completely damaged in a fire. The fire started in Hotel Hardanger, but 7–8 neighboring buildings also caught fire. It was said that the fire was caused by the maid of an English hotel guest having left a candle or a kerosene lamp by an open window, and that the curtain had caught fire - as it was very hot most of the windows in the hotel were open, and this caused the fire to spread with great speed. The fire started at 12 o'clock in the morning.
The commander and crew of the steamship "Vega" - which happened to be docked in Odda when the fire started - managed to put out the fire(s) within three hours using fire-fighting equipment from the ship. Among other things, they managed to save the post office, while the telegraph building was lost. The competing Jordals Hotel, which was run by Jacob Jordal, was also saved.
Hotel Hardanger was insured, and Bergens Tidende wrote that the insurance sum was NOK 90,000, but also published an anonymous source's assessment that the hotel complex was worth NOK 200,000–250,000, and that the owner - Mikal Tollefsen - had probably suffered a significant financial loss due to underinsurance. No people were injured in the fire.
Shortly after the fire in 1895, Tollefsen started building a new and larger hotel on the site of the fire. The new hotel was completed on 24 June 1896, and had 170 hotel beds in 110 guest rooms. Architecturally, it was a mixture of Swiss style and dragon style, with towers and projections.
Hardanger Hotel is mentioned, among other things, in a French travelogue published in 1897.
In 1913, the owner of Hotel Hardanger filed a claim for damages against the two factories - a cyanamide factory and a carbide factory - which had started up in Odda a few years earlier, because the factory operation caused such great pollution and bad odors that it affected the hotel operation. The provisions of the Neighborhood Act were the legal basis for the lawsuit. The court agreed with the plaintiff that the two factories were obliged to pay compensation for inconvenience and losses that the hotel had suffered after 2 August 1911, but not because Odda had become less idyllic and thus attractive to tourists. The compensation sum was to be determined after an appraisal had been carried out , and the result of the appraisal was not available until 1922. By then both factories had gone bankrupt, and hotel owner Mikal Tollefsen had died.
Hotel Hardanger becomes a town hall
In 1917, the municipality bought the Hotel Hardanger, to convert the building into a town hall . The hotel had then been almost empty all year round, because the industrial activity on the site had meant that the tourists did not show up. [9]
The hotel's so-called "Kongerom" was converted into a chairman's office and lord's boardroom. Eventually, the new town hall also accommodated a number of other businesses, such as a cinema, police station, doctor's office and bank. The old hotel was in use as Odda Town Hall until a new building was inaugurated in 1957; from then on, the former Hotel Hardanger was referred to as Odda old town hall . This building was demolished in 1976.
Jordals Hotel becomes Hardanger Hotel
In 1917, Jordals Hotel was bought by the Melkeraaen family, who continued to run the hotel for 68 years. Along the way, they changed the name of the hotel to Hardanger Hotel.
The Hardanger Hotel, which was a wooden Swiss-style building, was demolished in 1962, and a new five-story hotel building was inaugurated on 1 July 1963.
From tourism to industrial site
Factories and smelters
At the beginning of the 20th century, two factories were started in Odda. On one, cyanamide was produced, and on the other, carbide was produced .
In 1908, the operation of the first factory that was to be part of Odda Smelteverk , a carbide factory owned by a British company, began. In 1909, another British company started production of calcium cyanamide in the same area as the first factory. The reason why Odda was interesting for the foreign companies was the access to large amounts of hydropower and ice-free ports.
Both factories went bankrupt in 1921 , in connection with the worldwide economic crisis that occurred in the early 1920s. The bankruptcies led to thousands of people becoming unemployed. Both factories started up again in 1924, with Odda Smelteverk A/S as the new owner. This operating company was established by the power company Tyssefaldene and the Hafslund/Meraker group.
The cyanamide factory was built on in the 1930s.
At the smelter, the so-called Odda process was developed by chief chemist Erling Johnson in 1927–1928; it is a chemical process based on nitric acid for the industrial production of three-sided artificial fertilizer with the sub-components nitrogen , phosphorus and potassium .
Preservation decision and dispute over conservation value
In 2011 , the National Archives decided to protect several of the smelter's buildings and facilities, and to include the smelter in the Norwegian application to UNESCO for world heritage status for Norwegian industrial monuments. In 2013, however, the Ministry of the Environment decided that the series nomination should be split into two phases, 1. application for Rjukan/Notodden to be submitted to UNESCO in January 2014, and phase 2, that work be continued on expanding the nomination to include Odda/ Tyssedal with eventual submission to UNESCO in January 2016.
The owners of the smelter site objected to the conservation decision made in 2011, but the decision was upheld in 2012. The conservation included the cyanamide factory, the cable car, the Linde house (named after the German inventor Carl von Linde ) and the limestone silo on the import quay. Over the years, there has been much controversy in Odda about whether the smelter's buildings and facilities should be preserved or removed.
Cultural life
Music and theater
Tyssedalkoret and Odda Songlag are two choirs that come from Odda municipality. The water power and industrial history of the area here was documented in the performance and the DVD ``Arven'', performed by Tyssedalkoret with band and soloists in autumn 2004 and released on DVD in Christmas 2005. In addition these two choirs have the bands Odda Musikklag , Odda Skolekorps and Røldal Skolemusiklag. The blues team Lokst Utøve has 272 members. The Blueslaget received the culture award for 2009 for their great work as concert/festival organisers, volunteer workers and inspirers for bands and soloists. In 2011, Erlend Garatun Huus published the book Rock og Røyk , which is about the history of rock in Odda.
At the closed smelter (2001), the old "Lindehuset" has been used for theater and concert activities. The theater play Bikebubesong , based on the Oddingen Frode Grytten's novel Bikubesong , was performed in this venue in 2003 with great success. The play's performance in Oslo has been the most watched contemporary drama in Norwegian history.
A key cultural player in Odda is the company Oddakonsertene, led by Gunn Gravdal Elton. In April 2019, the Odda concerts staged the musical Albert og Leonie , a story about how Odda arose as an industrial community. The musical was a huge success with sold-out houses. 2,600 people queued to see and hear the story. The director was Martine Bakken Lundberg. The main roles were played by André Søfteland and Lene Kokai Flage. Over 60 amateurs were on stage. Albert and Leonie was planned to be staged again in 2020 and 2021, but had to be canceled due to the corona pandemic .
The odd concerts started in 2005 and as of 2019 have staged more than 60 concerts. All have been sold out. The most popular concerts are the annual Christmas concerts, which gather over 1,000 listeners. The traditional Christmas concert in Odda church with a large ensemble and two to three concerts in a row officially ended in 2019, but a simplified version was arranged in 2020, with concerts in Skare and Odda churches.
The Literature Symposium
From 2005, a festival called the Literature Symposium in Odda has been organized every autumn . The Linden house at the defunct Smelteverket, Odda cinema, Sentralbadet, Odda church are some of the venues at the symposium. Previously, there was every year "Bikubegang" with Frode Grytten , where he told about the story behind the book "Bikubesong", while he wandered around Odda. The literary symposium also has concerts, often in connection with an author/musician or individual artists. During the Literary Symposium 2011, the Sentralbadet Litteraturhus opened in the old bathroom at the closed Smelteverket, and this has become headquarters for the symposium, as well as a permanent house for literary events all year round.
As of 2010, a major rehabilitation/remodeling of Lindehuset was planned, so that the building would be better suited for events such as concerts and theater performances.
The National Antiquities' "Value creation project"
Odda is one of the pilot projects in the Value Creation Project for the National Archives.
TV shows
The actions in the TV series RIP Henry and Ragnarok have been added to Odda, and are recorded there. In Ragnarok, on the other hand, the city goes by the name Edda .
Known oddities
Samson Isberg (1795–1873), sharpshooter
Knud Knudsen (photographer) (1832–1915)
Gro Holm , born Prestgarden (1878–1949), writer
Alfred Hagn (1882–1958), painter, writer and spy.
Claes Gill (1910–1973), writer, actor and theater manager
Torbjørn Mork (1928–1992), doctor, politician ( Ap ), director of health 1972–1992
Walther Aas (1928–1990), artist
Roger Albertsen , (1957–2003), footballer
Anne B. Ragde (born 1957), writer, (raised in Trondheim)
Arne Borgstrøm (born 1959), elite long-distance swimmer
Frode Grytten (born 1960), author
Lars Ove Seljestad (born 1961), author
Bjørn Ingvaldsen (born 1962), author, leader of Norwegian Children's and Young People's Book Writers
Hallgeir Opedal (born 1965), writer and journalist
Børge Brende (born 1965), politician ( H ), former secretary general of the Norwegian Red Cross , minister of foreign affairs
Ida Melbo Øystese (born 1968), chief of police in Oslo from 2023.
Knut Olav Åmås (born 1968), author, editor, director of the foundation Fritt Ord
Leif Einar Lothe (born 1969), entrepreneur, singer, TV profile
Marit Eikemo (born 1971), writer
Tore Aurstad (born 1972), author
Ingvill Måkestad Bovim (born 1981), athlete
Håkon Opdal (born 1982), footballer
Ingvild Skare Thygesen (born 1993), TV profile
The Sognefjord is Norway's longest and deepest fjord with its 205 km and 1303 m at its deepest (SNL states 1308), including Sognesjøen which is at the far end towards the North Sea. The Sognefjord has the deepest point on Norway's coast. The fjord is 176–180 km from the innermost Lusterfjorden ( Skjolden ) to Sognefest , and 206 km to the outermost reef (then Lake Sognesjøen is also included). The width varies from around 1 to 2 km in Lusterfjorden to 4–5 km from Leikanger and beyond. Measured from the threshold to Skjolden, the fjord is 174 km. The middle part of the fjord is surrounded by mountains of around 1000 meters and in the inner part the height difference between the bottom of the fjord and the mountain tops is 3500 metres. The highest peak right by the fjord is Bleia at 1,721 metres, which gives a 2,850 meter height difference. Around the inner part of the fjord, the landscape is alpine with pointed mountain peaks, steep mountain sides and glaciers. As an extension of the fjord arms, long and deep valleys extend in all directions, including Jostedalen , Lærdalen and Årdal with Utladalen . The Sognefjord is the world's longest open (ice-free) fjord. The Sognefjord is the world's third longest fjord.
It is located in the middle of Vestland county (formerly Sogn og Fjordane county to which it helped give its name) and stretches from Solund on the coast in the west to Skjolden at the foot of Jotunheimen in the east (northeast), where the fjord arm is called Lustrafjorden . The fjord and the land around it make up the Sogn region, often divided into Outer, Midtre and Indre Sogn. The length from Rutletangen to Skjolden is 186 km . Sogn makes up almost 60% of the area in Sogn and Fjordane, or around 11,000 km 2 . The twelve municipalities in Sogn have a total area of 10,671.55 km² and 37,063 inhabitants (1 January 2014). The land around the inner part of the fjord is called Indre Sogn and includes the long fjord arms. From Leikanger onwards, the country is called Ytre Sogn . The outer part of the fjord has few and small fjord arms. The fjord arms are like hanging valleys under water in that the bottom in the side fjords is often much shallower than the main fjord with a height difference of over 1,000 meters in some cases. The main fjord has a threshold at its mouth to the sea, while several of the side fjords have thresholds at the mouth of the main fjord.
The Sognefjord cuts so deeply into the country that it is only 15 km from the innermost arm at Skjolden to mountain peaks such as Store Skagastølstind in Jotunheimen. The water flow usually exits the fjord. The rivers create sandbanks where they run into the fjord, for example at Gudvangen, in Lærdal and in Gaupne. These sandbars are constantly expanding and changing shape.
The Sognefjord, especially the inner part, is surrounded by mountain massifs which are alpine in the inner part and more rounded in the outer part. The innermost arms of the fjord continue as deep and sometimes long valleys, including Lærdal , Årdal with Utladalen , Nærøydalen , Sogndalsdalen , Fjærland , Fortunsdalen , Aurlandsdalen and Jostedalen . The transition between the fjord and these valleys is determined by sea level, and the boundary has moved outwards at the uplift. Some of the side valleys, such as Vik and Fresvik, would have been hanging valleys in the same way as the Feigedalen if the Sognefjord was drained.
Name
Amund Helland writes " The Sognefjord's real name is Sogn , while Sogn is now used only for the surrounding landscape, and was thus already used in the Middle Ages. As a landscape name, the name is a masculine word and has undoubtedly been so as a fjord name as well." The name is connected to the word "suction", which probably refers to the suction or the difficult current conditions that are created when the water flows through the fjord mouth and over the threshold.
Geography
Large parts of the fjord are surrounded by steep mountains. Kvamsøy at Balestrand is a small island separated from the mainland by a short, shallow strait. Outside Balestrand there are small fjord arms and at Veganes ( Dragsvik ferry quay ) there is a significant branching with the Fjærlandsfjorden .
Municipalities
Municipalities with shoreline to the fjord, counted from west to east:
Solund
Hyllestad (north side)
Gulen (south side)
Høyanger (on both sides of the main fjord)
Vik (south side)
Sogndal (north side)
Aurland (south side, around the Aurlandsfjord)
Lærdal (south side)
Luster (north side, around Lustrafjorden)
Årdal (around the Årdalsfjord)
Depths
The Sognefjord has only one threshold which is at the mouth and the threshold is around 165 meters deep. The area beyond the threshold is called Sognesjøen , which is sheltered by islands to the north and south; there is no threshold outside Sognesjøen that has free circulation towards the ocean.
From the inner parts at Årdal or Skjolden, the fjord gradually deepens outwards (westwards). Between Fodnes-Mannheller and Rutledal-Rysjedalsvika, the bottom is at least 800 metres. The deepest part is approximately at Åkrestrand and Vadheim. The outer part of the fjord (at Losna and Sula ) has a marked threshold with depths of 100 to 200 metres, where the fjord bed rises abruptly from a depth of 1,200 meters to around 100 meters over a stretch of 5 km at Rutledal. In Lake Sognesjøen there are several small troughs (with depths down to 400-500 metres) with thresholds between them. Across the fjord, the bottom is partly completely flat with less than 1 meter variation in depth over a 2 km cross-section. The bottom is covered by fine material (clay) which at Vangsnes is up to 300 meters thick. Seismic shows that the greatest depth to the bedrock is approximately 1,600 m, but loose masses with a thickness of 200–400 m mean that the fjord bottom is nevertheless flat. Seismic surveys at Vangsnes have revealed a 300 meter thick layer of clay at the bottom.
Between 50 and 180 km from the mouth, the fjord bed is relatively flat. Almost all side fjords form hanging valleys to the main fjord. For example, the mouth of the Fjærlandsfjord is well over 400 meters deep, while the main fjord is close to 1,200 meters deep just outside the mouth. Vadheimfjord's mouth is 400 meters deep, here the greatest depth is over 1300 m. Ikjefjord's mouth is only 50 meters deep close to where the main fjord is at its deepest. In large parts of the fjord, it is "abruptly deep" in that the steep mountain sides continue just as steeply underwater.
In contrast to a number of other fjords, not every single part of the Sognefjord has its own name. Only the outermost part has its own name - Sognesjøen . However, there are many fjord arms. From west to east these are:
Sognesjøen
Straumsfjorden
Bjørnefjorden
Nessefjord
The Sognefjord
Lifjorden
Bøfjorden
The Risnefjord
The Ikjefjord
Vadheimsfjorden
Fuglsetfjorden
Høyangsfjorden
Lånefjorden
The Finnafjord
The Arnafjord
The Inner Fjord
Framfjorden
Vikbukti
The Esefjord
Fjærlandsfjorden
The Vetlefjord
Sværefjorden
The Norafjord
Sogndalsfjorden
Barsnes Fjord
The Eidsfjord
Aurlandsfjorden
The Nærøyfjord
Amla Bay
Lærdalsfjorden
Årdalsfjorden
The Lustrafjord
The Gaupnefjord
Climate and fresh water
The fjord colored by meltwater from the glacier.
Terrain formations and distance to the sea lead to great variations in climate along the fjord. The outer part has a mild and humid coastal climate, while the innermost part has an inland climate with cold and dry winters.
The amount of precipitation decreases strongly inwards into the fjord. Lærdal lies in the rain shadow and has very little rainfall, while west-facing slopes further out have a lot of rainfall and there the rainfall often increases with altitude. Brekke and Takle in Ytre Parish are among the places in Norway with the most rainfall. North of the Sognefjord lies the Jostedalsbreen, Norway's largest glacier, and parts of the meltwater drain into the Sognefjord. Wind conditions are strongly influenced by terrain formations. In winter, the dominant wind direction is out the fjord or out the side valleys in the form of so-called downwinds . Fall winds can be very strong and have a major impact on cooling and icing. The slopes and valleys along the inner parts of the fjord have a partially mild climate and are fertile, which makes the area suitable for growing fruit and berries, among other things. The slopes along the fjord partly have large conifer forests, including in the roadless area of Frønningen .
The fjord receives fresh water mainly from the rivers and very little precipitation directly on the fjord's water surface. In the inner part of the Sognefjord, the total supply of fresh water during one year corresponds to a depth of 33 meters if it were distributed over the entire area of the fjord. In spring and partly in autumn, the top 2-3 meters of the fjord are brackish water , especially in the side fjords. The salt content in the surface is lowest in summer and autumn. In June 1954, for example, 5 ‰ salt was measured in the uppermost meters of the Lustrafjord, while at great depths it was 34.5 ‰. Regulation of the waterways for power production has led to a larger proportion of fresh water flowing into the fjord in the winter. The most extensive regulation is in Aurland, Lærdal, Årdal and Jostedal. Regulations affect temperature in the surface layer and icing. In the inner part of the fjord, the rivers are fed by high mountains and glaciers.
The rivers Lærdalselvi , Aurlandselvi , Flåmselvi , Mørkridselvi , Henjaelvi , Grindselvi , Hamreelvi , Njøsaelvi , Kvinnafossen , Sogndalselvi and Jostedøla flow into the Sognefjord and normally have spring floods in June. [3] Lærdalselva has the largest catchment, followed by Jostedøla and Aurlandselva, and these three have roughly the same water flow (around 40 m 3 /second). The Årdalsvatnet drains to the Sognefjord through the short Åreidselva or Hæreidselvi through the Årdalstangen . The Eidsvatnet in Luster drains into the Sognefjord just by Mørkridselvi in Skjolden . Regulation of the waterways for hydropower has resulted in a more steady supply of fresh water throughout the year. Without regulation, 92% of the fresh water would have been supplied in the summer half-year from May to October. Several of the large rivers flow into fjord arms.
Geology
The bedrock along the outer and middle part of the fjord consists mostly of Precambrian gneiss with orientation east-west and northeast-southwest. The islands of Solund consist mostly of Devonian sandstone and conglomerates , while the interior (eastern part) consists mostly of Caledonian gabbro , anorthosite , granite and phyllite .
Jostedøla's material transport (in the form of sludge) involves sedimentation in the Gaupnefjord of 10 to 20 cm/year near the river basin, and 1 cm/year 2 km from the river basin. The river transports 50,000 to 100,000 tonnes of silt annually. The sludge concentration from Jostedøla is at most 1 g/litre. It is particularly at Gaupne that the meltwater from the glaciers is marked by the color of the water.
Icing
According to Helland, it was common for the ice to settle on several of the fjord arms every winter, including on Aurlandsfjorden, Nærøyfjorden and Årdalsfjorden. In the winter of 1888–1889, Lusterfjorden was iced over for six months straight. In the deepest parts of the Sognefjord, there is a year-round temperature of around 6.5 °C, according to Helland. Outer parts are almost never iced over, not even the side fjords. The inner parts can be frozen for several weeks at a stretch. Among other things, inner parts of the Aurlandsfjorden and the Nærøyfjorden freeze easily. Lærdalsfjorden is usually ice-free except for the very innermost part, while it has happened that Årdalsfjorden has been iced up to Ofredal and has been an obstacle to ship traffic. Historically, Lustrafjorden has often been iced over as far as Urnes. The Barsnesfjorden has often been covered with ice. In the Nærøyfjord it happened (among other things in the 1920s and in 1962) that the liner was unable to enter the fjord due to ice and had to dispatch at the ice edge.
Streams
In the Sognefjord, incoming current is hardly noticeable and is most noticeable in strong westerly winds. Outgoing current dominates and is particularly strong in spring and summer. At strong tides, the tidal flow can reach over 1 m/s (2 knots ) around the pier and headland. The Sognefjord is covered by a layer or stream of brackish water of up to 10 meters (varying with the seasons and supply from the rivers). Beneath the brackish water, a current or intermediate layer at a depth of 150 meters goes in and out of the fjord and below this lies the main basin, which has some connection with the ocean beyond the threshold. Together, these three currents contribute to the fact that the water in the fjord is replaced on average within 8-10 years, so that the fjord has life right down to the bottom. The brackish water layer has less density and therefore does not mix easily with the deeper layers. The brackish water that flows out of the fjord slowly mixes with the layer below so that the salt content increases at the same time as the brackish water layer increases up to 10 times the amount of fresh water supplied. The brackish water that flows towards the mouth must be replaced and sets up an incoming current in a slightly deeper layer.
Fish
The Sognefjord has herring and good sprat fishing . In the outer parts of the fjord, salmon has traditionally been fished with wedge nets . Salmon warp or "sitjenet" is a traditional method of salmon fishing and skilled players could catch a lot of fish with this method. Hook nets and drift nets have dominated in modern times and do not require the same active fishing as warp . The salmon's migration in the fjord is controlled by currents on the surface and the warps are placed where there are favorable current conditions where, due to the current, the salmon are driven close to land on their way into the fjord. In Leikanger and Balestrand there are many good places for sitejnot with Suppham being by far the best. Good salmon rivers such as Lærdalselva, Aurlandselva and Årøyelva flow into the Sognefjorden.
In the outer part of the fjord (Gulen and Solund) there is some fish farming. Several of the waterways are known for good salmon and sea trout fishing , and five of the rivers have been designated as national salmon rivers. Lærdalselva has a salmon-carrying stretch and has had by far the largest population. Aurlandselva has historically had a good catch of sea trout. The Sognefjord is among the most important in Norway for anadromous fish species. Norwegian spring-spawning herring are fished in the fjord, especially in the outer parts, as well as some coastal sprat.
In the Sognefjord there are plankton algae which in other Norwegian waters and the occurrence follows the seasons. In general, there is little occurrence in winter due to low light, diatoms bloom in March-April and are dependent on the supply of nutrient salts, in May-June diatoms and flagellates bloom in connection with the spring flood, in summer there is a varying population, new blooms in the autumn in connection with, among other things, floods, and married species can occur all year round.
Tourism
The Sognefjord was established as a tourist destination in the 19th century, among other things, with the establishment of Fylkesbåtane. One of the targets was Gudvangen, which in 1889 received 79 large tourist ships with a total of over 10,000 passengers. In 1889, 4,500 travelers came with the county boats. The German Emperor Wilhelm visited the Sognefjord and Balestrand for the first time in 1890. The emperor subsequently visited the Sognefjord 25 times. The fjord itself and the surrounding area with Jotunheimen, Jostedalsbreen and several stave churches have made the Sognefjord one of Norway's most prominent tourist destinations. Balestrand, Vangsnes, Aurland and Fjærland were among the early destinations for English tourists in the 19th century.
History
It has been the Guest of Death
It has sailed on a Torden
It is christened in Rædsler vorden
that has plowed the Sognefjord
from Forthun to Sognefæst.
If you have forgotten your Lord's Prayer,
do you remember a prayer to pray:
learn it from the wrath of God!
imagine, Sinder, then present
in a Bath on Sognefjord!
Henrik Wergeland
The Sognefjord has been an important transport artery since ancient times. The gulation was probably held near the mouth of the Sognefjord and probably because it was practical to hold the meeting where the ship lay along the coast met the great fjord. From the innermost arms of the fjord it is a relatively short distance to the inland villages of Eastern Norway, particularly through Lærdal to Valdres over the moderate mountain pass Filefjell . Lærdalsøyri was from the 17th century an important market and meeting place. There, farmers from Valdres, Hallingdal and Gudbrandsdalen sold slaughter, tar and other products from the interior and bought fish, salt, hemp and iron from the fjords and from Bergen. Around 1300, the authorities established a shuttle station at Maristova at the entrance to Filefjell. The first drivable road between east and west was built over Filefjell in 1792. From 1843 the paddle steamer "Constitutionen" plyed the route between Bergen and Lærdal, the county boats took over the route in 1857. The road over the Sognefjellet was built as a carriageway in 1938. The Flåmsbana connected the Sognefjord to the railway network in 1940. Stalheimskleivi , between Voss and Sogn, was built in 1850 and turned into a road in 1937. It has made it possible to transport agricultural products , fruit , berries and fish between the villages in Sogn and Bergen .
From 1785, the Trondhjem postal route crossed the Sognefjord by boat between Rutledal and Leirvik in Hyllestad . In 1647, a postal route was established between Bergen and Christiania. The post then took 7-8 days via Gudvangen, Lærdal and Valdres.
It was difficult to get to the Sognefjord by sailboat and the yachts could lie for many days or several weeks at the mouth waiting for favorable wind conditions. East wind was favorable out of the fjord, while south to Bergen, wind from the north or north-west was needed. To enter the fjord, a wind from the west was necessary. The steam and motor boats revolutionized transport on the fjord and these had completely taken over in the early 20th century The county boats were established in 1858 with boat routes on the Sognefjord and to Bergen as an important activity.
In 1934, a ferry route was established along the fjord from Vadheim to Lærdal. From 1939 until the Lærdal tunnel opened, there was a car ferry between Gudvangen and Lærdal - first the ferry went to Lærdalsøyri itself, from 1966 to Revsnes when a road was built there to shorten the ferry route. In the 1990s, the ferry connection Revsnes-Kaupanger was replaced by Mannheller-Fodnes , and after this Kaupanger has only been used by the tourist route Gudvangen-Kaupanger-Lærdal. The road system between Sogndal and Jølster on national highway 5 , including the Fjærlands tunnel , created a ferry-free road connection on the north side of the fjord.
Norway , officially the Kingdom of Norway , is a Nordic , European country and an independent state in the west of the Scandinavian Peninsula . Geographically speaking, the country is long and narrow, and on the elongated coast towards the North Atlantic are Norway's well-known fjords . The Kingdom of Norway includes the main country (the mainland with adjacent islands within the baseline ), Jan Mayen and Svalbard . With these two Arctic areas, Norway covers a land area of 385,000 km² and has a population of approximately 5.5 million (2023). Mainland Norway borders Sweden in the east , Finland and Russia in the northeast .
Norway is a parliamentary democracy and constitutional monarchy , where Harald V has been king and head of state since 1991 , and Jonas Gahr Støre ( Ap ) has been prime minister since 2021 . Norway is a unitary state , with two administrative levels below the state: counties and municipalities . The Sami part of the population has, through the Sami Parliament and the Finnmark Act , to a certain extent self-government and influence over traditionally Sami areas. Although Norway has rejected membership of the European Union through two referendums , through the EEA Agreement Norway has close ties with the Union, and through NATO with the United States . Norway is a significant contributor to the United Nations (UN), and has participated with soldiers in several foreign operations mandated by the UN. Norway is among the states that have participated from the founding of the UN , NATO , the Council of Europe , the OSCE and the Nordic Council , and in addition to these is a member of the EEA , the World Trade Organization , the Organization for Economic Co-operation and Development and is part of the Schengen area .
Norway is rich in many natural resources such as oil , gas , minerals , timber , seafood , fresh water and hydropower . Since the beginning of the 20th century, these natural conditions have given the country the opportunity for an increase in wealth that few other countries can now enjoy, and Norwegians have the second highest average income in the world, measured in GDP per capita, as of 2022. The petroleum industry accounts for around 14% of Norway's gross domestic product as of 2018. Norway is the world's largest producer of oil and gas per capita outside the Middle East. However, the number of employees linked to this industry fell from approx. 232,000 in 2013 to 207,000 in 2015.
In Norway, these natural resources have been managed for socially beneficial purposes. The country maintains a welfare model in line with the other Nordic countries. Important service areas such as health and higher education are state-funded, and the country has an extensive welfare system for its citizens. Public expenditure in 2018 is approx. 50% of GDP, and the majority of these expenses are related to education, healthcare, social security and welfare. Since 2001 and until 2021, when the country took second place, the UN has ranked Norway as the world's best country to live in . From 2010, Norway is also ranked at the top of the EIU's democracy index . Norway ranks third on the UN's World Happiness Report for the years 2016–2018, behind Finland and Denmark , a report published in March 2019.
The majority of the population is Nordic. In the last couple of years, immigration has accounted for more than half of population growth. The five largest minority groups are Norwegian-Poles , Lithuanians , Norwegian-Swedes , Norwegian-Syrians including Syrian Kurds and Norwegian-Pakistani .
Norway's national day is 17 May, on this day in 1814 the Norwegian Constitution was dated and signed by the presidency of the National Assembly at Eidsvoll . It is stipulated in the law of 26 April 1947 that 17 May are national public holidays. The Sami national day is 6 February. "Yes, we love this country" is Norway's national anthem, the song was written in 1859 by Bjørnstjerne Bjørnson (1832–1910).
Norway's history of human settlement goes back at least 10,000 years, to the Late Paleolithic , the first period of the Stone Age . Archaeological finds of settlements along the entire Norwegian coast have so far been dated back to 10,400 before present (BP), the oldest find is today considered to be a settlement at Pauler in Brunlanes , Vestfold .
For a period these settlements were considered to be the remains of settlers from Doggerland , an area which today lies beneath the North Sea , but which was once a land bridge connecting today's British Isles with Danish Jutland . But the archaeologists who study the initial phase of the settlement in what is today Norway reckon that the first people who came here followed the coast along what is today Bohuslân. That they arrived in some form of boat is absolutely certain, and there is much evidence that they could easily move over large distances.
Since the last Ice Age, there has been continuous settlement in Norway. It cannot be ruled out that people lived in Norway during the interglacial period , but no trace of such a population or settlement has been found.
The Stone Age lasted a long time; half of the time that our country has been populated. There are no written accounts of what life was like back then. The knowledge we have has been painstakingly collected through investigations of places where people have stayed and left behind objects that we can understand have been processed by human hands. This field of knowledge is called archaeology . The archaeologists interpret their findings and the history of the surrounding landscape. In our country, the uplift after the Ice Age is fundamental. The history of the settlements at Pauler is no more than fifteen years old.
The Fosna culture settled parts of Norway sometime between 10,000–8,000 BC. (see Stone Age in Norway ). The dating of rock carvings is set to Neolithic times (in Norway between 4000 BC to 1700 BC) and show activities typical of hunters and gatherers .
Agriculture with livestock and arable farming was introduced in the Neolithic. Swad farming where the farmers move when the field does not produce the expected yield.
More permanent and persistent farm settlements developed in the Bronze Age (1700 BC to 500 BC) and the Iron Age . The earliest runes have been found on an arrowhead dated to around 200 BC. Many more inscriptions are dated to around 800, and a number of petty kingdoms developed during these centuries. In prehistoric times, there were no fixed national borders in the Nordic countries and Norway did not exist as a state. The population in Norway probably fell to year 0.
Events in this time period, the centuries before the year 1000, are glimpsed in written sources. Although the sagas were written down in the 13th century, many hundreds of years later, they provide a glimpse into what was already a distant past. The story of the fimbul winter gives us a historical picture of something that happened and which in our time, with the help of dendrochronology , can be interpreted as a natural disaster in the year 536, created by a volcanic eruption in El Salvador .
In the period between 800 and 1066 there was a significant expansion and it is referred to as the Viking Age . During this period, Norwegians, as Swedes and Danes also did, traveled abroad in longships with sails as explorers, traders, settlers and as Vikings (raiders and pirates ). By the middle of the 11th century, the Norwegian kingship had been firmly established, building its right as descendants of Harald Hårfagre and then as heirs of Olav the Holy . The Norwegian kings, and their subjects, now professed Christianity . In the time around Håkon Håkonsson , in the time after the civil war , there was a small renaissance in Norway with extensive literary activity and diplomatic activity with Europe. The black dew came to Norway in 1349 and killed around half of the population. The entire state apparatus and Norway then entered a period of decline.
Between 1396 and 1536, Norway was part of the Kalmar Union , and from 1536 until 1814 Norway had been reduced to a tributary part of Denmark , named as the Personal Union of Denmark-Norway . This staff union entered into an alliance with Napoléon Bonaparte with a war that brought bad times and famine in 1812 . In 1814, Denmark-Norway lost the Anglophone Wars , part of the Napoleonic Wars , and the Danish king was forced to cede Norway to the king of Sweden in the Treaty of Kiel on 14 January of that year. After a Norwegian attempt at independence, Norway was forced into a loose union with Sweden, but where Norway was allowed to create its own constitution, the Constitution of 1814 . In this period, Norwegian, romantic national feeling flourished, and the Norwegians tried to develop and establish their own national self-worth. The union with Sweden was broken in 1905 after it had been threatened with war, and Norway became an independent kingdom with its own monarch, Haakon VII .
Norway remained neutral during the First World War , and at the outbreak of the Second World War, Norway again declared itself neutral, but was invaded by National Socialist Germany on 9 April 1940 .
Norway became a member of the Western defense alliance NATO in 1949 . Two attempts to join the EU were voted down in referendums by small margins in 1972 and 1994 . Norway has been a close ally of the United States in the post-war period. Large discoveries of oil and natural gas in the North Sea at the end of the 1960s led to tremendous economic growth in the country, which is still ongoing. Traditional industries such as fishing are also part of Norway's economy.
Stone Age (before 1700 BC)
When most of the ice disappeared, vegetation spread over the landscape and due to a warm climate around 2000-3000 BC. the forest grew much taller than in modern times. Land uplift after the ice age led to a number of fjords becoming lakes and dry land. The first people probably came from the south along the coast of the Kattegat and overland into Finnmark from the east. The first people probably lived by gathering, hunting and trapping. A good number of Stone Age settlements have been found which show that such hunting and trapping people stayed for a long time in the same place or returned to the same place regularly. Large amounts of gnawed bones show that they lived on, among other things, reindeer, elk, small game and fish.
Flintstone was imported from Denmark and apart from small natural deposits along the southern coast, all flintstone in Norway is transported by people. At Espevær, greenstone was quarried for tools in the Stone Age, and greenstone tools from Espevær have been found over large parts of Western Norway. Around 2000-3000 BC the usual farm animals such as cows and sheep were introduced to Norway. Livestock probably meant a fundamental change in society in that part of the people had to be permanent residents or live a semi-nomadic life. Livestock farming may also have led to conflict with hunters.
The oldest traces of people in what is today Norway have been found at Pauler , a farm in Brunlanes in Larvik municipality in Vestfold . In 2007 and 2008, the farm has given its name to a number of Stone Age settlements that have been excavated and examined by archaeologists from the Cultural History Museum at UiO. The investigations have been carried out in connection with the new route for the E18 motorway west of Farris. The oldest settlement, located more than 127 m above sea level, is dated to be about 10,400 years old (uncalibrated, more than 11,000 years in real calendar years). From here, the ice sheet was perhaps visible when people settled here. This locality has been named Pauler I, and is today considered to be the oldest confirmed human traces in Norway to date. The place is in the mountains above the Pauler tunnel on the E18 between Larvik and Porsgrunn . The pioneer settlement is a term archaeologists have adopted for the oldest settlement. The archaeologists have speculated about where they came from, the first people in what is today Norway. It has been suggested that they could come by boat or perhaps across the ice from Doggerland or the North Sea, but there is now a large consensus that they came north along what is today the Bohuslän coast. The Fosna culture , the Komsa culture and the Nøstvet culture are the traditional terms for hunting cultures from the Stone Age. One thing is certain - getting to the water was something they mastered, the first people in our country. Therefore, within a short time they were able to use our entire long coast.
In the New Stone Age (4000 BC–1700 BC) there is a theory that a new people immigrated to the country, the so-called Stone Ax People . Rock carvings from this period show motifs from hunting and fishing , which were still important industries. From this period, a megalithic tomb has been found in Østfold .
It is uncertain whether there were organized societies or state-like associations in the Stone Age in Norway. Findings from settlements indicate that many lived together and that this was probably more than one family so that it was a slightly larger, organized herd.
Finnmark
In prehistoric times, animal husbandry and agriculture were of little economic importance in Finnmark. Livelihoods in Finnmark were mainly based on fish, gathering, hunting and trapping, and eventually domestic reindeer herding became widespread in the Middle Ages. Archaeological finds from the Stone Age have been referred to as the Komsa culture and comprise around 5,000 years of settlement. Finnmark probably got its first settlement around 8000 BC. It is believed that the coastal areas became ice-free 11,000 years BC and the fjord areas around 9,000 years BC. after which willows, grass, heather, birch and pine came into being. Finnmarksvidda was covered by pine forest around 6000 BC. After the Ice Age, the land rose around 80 meters in the inner fjord areas (Alta, Tana, Varanger). Due to ice melting in the polar region, the sea rose in the period 6400–3800 BC. and in areas with little land elevation, some settlements from the first part of the Stone Age were flooded. On Sørøya, the net sea level rise was 12 to 14 meters and many residential areas were flooded.
According to Bjørnar Olsen , there are many indications of a connection between the oldest settlement in Western Norway (the " Fosnakulturen ") and that in Finnmark, but it is uncertain in which direction the settlement took place. In the earliest part of the Stone Age, settlement in Finnmark was probably concentrated in the coastal areas, and these only reflected a lifestyle with great mobility and no permanent dwellings. The inner regions, such as Pasvik, were probably used seasonally. The archaeologically proven settlements from the Stone Age in inner Finnmark and Troms are linked to lakes and large watercourses. The oldest petroglyphs in Alta are usually dated to 4200 BC, that is, the Neolithic . Bjørnar Olsen believes that the oldest can be up to 2,000 years older than this.
From around 4000 BC a slow deforestation of Finnmark began and around 1800 BC the vegetation distribution was roughly the same as in modern times. The change in vegetation may have increased the distance between the reindeer's summer and winter grazing. The uplift continued slowly from around 4000 BC. at the same time as sea level rise stopped.
According to Gutorm Gjessing, the settlement in Finnmark and large parts of northern Norway in the Neolithic was semi-nomadic with movement between four seasonal settlements (following the pattern of life in Sami siida in historical times): On the outer coast in summer (fishing and seal catching) and inland in winter (hunting for reindeer, elk and bear). Povl Simonsen believed instead that the winter residence was in the inner fjord area in a village-like sod house settlement. Bjørnar Olsen believes that at the end of the Stone Age there was a relatively settled population along the coast, while inland there was less settlement and a more mobile lifestyle.
Bronze Age (1700 BC–500 BC)
Bronze was used for tools in Norway from around 1500 BC. Bronze is a mixture of tin and copper , and these metals were introduced because they were not mined in the country at the time. Bronze is believed to have been a relatively expensive material. The Bronze Age in Norway can be divided into two phases:
Early Bronze Age (1700–1100 BC)
Younger Bronze Age (1100–500 BC)
For the prehistoric (unwritten) era, there is limited knowledge about social conditions and possible state formations. From the Bronze Age, there are large burial mounds of stone piles along the coast of Vestfold and Agder, among others. It is likely that only chieftains or other great men could erect such grave monuments and there was probably some form of organized society linked to these. In the Bronze Age, society was more organized and stratified than in the Stone Age. Then a rich class of chieftains emerged who had close connections with southern Scandinavia. The settlements became more permanent and people adopted horses and ard . They acquired bronze status symbols, lived in longhouses and people were buried in large burial mounds . Petroglyphs from the Bronze Age indicate that humans practiced solar cultivation.
Finnmark
In the last millennium BC the climate became cooler and the pine forest disappears from the coast; pine forests, for example, were only found in the innermost part of the Altafjord, while the outer coast was almost treeless. Around the year 0, the limit for birch forest was south of Kirkenes. Animals with forest habitats (elk, bear and beaver) disappeared and the reindeer probably established their annual migration routes sometime at that time. In the period 1800–900 BC there were significantly more settlements in and utilization of the hinterland was particularly noticeable on Finnmarksvidda. From around 1800 BC until year 0 there was a significant increase in contact between Finnmark and areas in the east including Karelia (where metals were produced including copper) and central and eastern Russia. The youngest petroglyphs in Alta show far more boats than the earlier phases and the boats are reminiscent of types depicted in petroglyphs in southern Scandinavia. It is unclear what influence southern Scandinavian societies had as far north as Alta before the year 0. Many of the cultural features that are considered typical Sami in modern times were created or consolidated in the last millennium BC, this applies, among other things, to the custom of burying in brick chambers in stone urns. The Mortensnes burial ground may have been used for 2000 years until around 1600 AD.
Iron Age (c. 500 BC–c. 1050 AD)
The Einangsteinen is one of the oldest Norwegian runestones; it is from the 4th century
Simultaneous production of Vikings
Around 500 years BC the researchers reckon that the Bronze Age will be replaced by the Iron Age as iron takes over as the most important material for weapons and tools. Bronze, wood and stone were still used. Iron was cheaper than bronze, easier to work than flint , and could be used for many purposes; iron probably became common property. Iron could, among other things, be used to make solid and sharp axes which made it much easier to fell trees. In the Iron Age, gold and silver were also used partly for decoration and partly as means of payment. It is unknown which language was used in Norway before our era. From around the year 0 until around the year 800, everyone in Scandinavia (except the Sami) spoke Old Norse , a North Germanic language. Subsequently, several different languages developed in this area that were only partially mutually intelligible. The Iron Age is divided into several periods:
Early Iron Age
Pre-Roman Iron Age (c. 500 BC–c. 0)
Roman Iron Age (c. 0–c. AD 400)
Migration period (approx. 400–600). In the migration period (approx. 400–600), new peoples came to Norway, and ruins of fortress buildings etc. are interpreted as signs that there has been talk of a violent invasion.
Younger Iron Age
Merovingian period (500–800)
The Viking Age (793–1066)
Norwegian Vikings go on plundering expeditions and trade voyages around the coastal countries of Western Europe . Large groups of Norwegians emigrate to the British Isles , Iceland and Greenland . Harald Hårfagre starts a unification process of Norway late in the 8th century , which was completed by Harald Hardråde in the 1060s . The country was Christianized under the kings Olav Tryggvason , fell in the battle of Svolder ( 1000 ) and Olav Haraldsson (the saint), fell in the battle of Stiklestad in 1030 .
Sources of prehistoric times
Shrinking glaciers in the high mountains, including in Jotunheimen and Breheimen , have from around the year 2000 uncovered objects from the Viking Age and earlier. These are objects of organic material that have been preserved by the ice and that elsewhere in nature are broken down in a few months. The finds are getting older as the melting makes the archaeologists go deeper into the ice. About half of all archaeological discoveries on glaciers in the world are made in Oppland . In 2013, a 3,400-year-old shoe and a robe from the year 300 were found. Finds at Lomseggen in Lom published in 2020 revealed, among other things, well-preserved horseshoes used on a mountain pass. Many hundreds of items include preserved clothing, knives, whisks, mittens, leather shoes, wooden chests and horse equipment. A piece of cloth dated to the year 1000 has preserved its original colour. In 2014, a wooden ski from around the year 700 was found in Reinheimen . The ski is 172 cm long and 14 cm wide, with preserved binding of leather and wicker.
Pytheas from Massalia is the oldest known account of what was probably the coast of Norway, perhaps somewhere on the coast of Møre. Pytheas visited Britannia around 325 BC. and traveled further north to a country by the "Ice Sea". Pytheas described the short summer night and the midnight sun farther north. He wrote, among other things, that people there made a drink from grain and honey. Caesar wrote in his work about the Gallic campaign about the Germanic tribe Haruders. Other Roman sources around the year 0 mention the land of the Cimbri (Jutland) and the Cimbri headlands ( Skagen ) and that the sources stated that Cimbri and Charyds lived in this area. Some of these peoples may have immigrated to Norway and there become known as hordes (as in Hordaland). Sources from the Mediterranean area referred to the islands of Scandia, Scandinavia and Thule ("the outermost of all islands"). The Roman historian Tacitus wrote around the year 100 a work about Germania and mentioned the people of Scandia, the Sviones. Ptolemy wrote around the year 150 that the Kharudes (Hordes) lived further north than all the Cimbri, in the north lived the Finnoi (Finns or Sami) and in the south the Gutai (Goths). The Nordic countries and Norway were outside the Roman Empire , which dominated Europe at the time. The Gothic-born historian Jordanes wrote in the 5th century about 13 tribes or people groups in Norway, including raumaricii (probably Romerike ), ragnaricii ( Ranrike ) and finni or skretefinni (skrid finner or ski finner, i.e. Sami) as well as a number of unclear groups. Prokopios wrote at the same time about Thule north of the land of the Danes and Slavs, Thule was ten times as big as Britannia and the largest of all the islands. In Thule, the sun was up 40 days straight in the summer. After the migration period , southern Europeans' accounts of northern Europe became fuller and more reliable.
Settlement in prehistoric times
Norway has around 50,000 farms with their own names. Farm names have persisted for a long time, over 1000 years, perhaps as much as 2000 years. The name researchers have arranged different types of farm names chronologically, which provides a basis for determining when the place was used by people or received a permanent settlement. Uncompounded landscape names such as Haug, Eid, Vik and Berg are believed to be the oldest. Archaeological traces indicate that some areas have been inhabited earlier than assumed from the farm name. Burial mounds also indicate permanent settlement. For example, the burial ground at Svartelva in Løten was used from around the year 0 to the year 1000 when Christianity took over. The first farmers probably used large areas for inland and outland, and new farms were probably established based on some "mother farms". Names such as By (or Bø) show that it is an old place of residence. From the older Iron Age, names with -heim (a common Germanic word meaning place of residence) and -stad tell of settlement, while -vin and -land tell of the use of the place. Farm names in -heim are often found as -um , -eim or -em as in Lerum and Seim, there are often large farms in the center of the village. New farm names with -city and -country were also established in the Viking Age . The first farmers probably used the best areas. The largest burial grounds, the oldest archaeological finds and the oldest farm names are found where the arable land is richest and most spacious.
It is unclear whether the settlement expansion in Roman times, migrations and the Iron Age is due to immigration or internal development and population growth. Among other things, it is difficult to demonstrate where in Europe the immigrants have come from. The permanent residents had both fields (where grain was grown) and livestock that grazed in the open fields, but it is uncertain which of these was more important. Population growth from around the year 200 led to more utilization of open land, for example in the form of settlements in the mountains. During the migration period, it also seems that in parts of the country it became common to have cluster gardens or a form of village settlement.
Norwegian expansion northwards
From around the year 200, there was a certain migration by sea from Rogaland and Hordaland to Nordland and Sør-Troms. Those who moved settled down as a settled Iron Age population and became dominant over the original population which may have been Sami . The immigrant Norwegians, Bumen , farmed with livestock that were fed inside in the winter as well as some grain cultivation and fishing. The northern border of the Norwegians' settlement was originally at the Toppsundet near Harstad and around the year 500 there was a Norwegian settlement to Malangsgapet. That was as far north as it was possible to grow grain at the time. Malangen was considered the border between Hålogaland and Finnmork until around 1400 . Further into the Viking Age and the Middle Ages, there was immigration and settlement of Norwegian speakers along the coast north of Malangen. Around the year 800, Norwegians lived along the entire outer coast to Vannøy . The Norwegians partly copied Sami livelihoods such as whaling, fur hunting and reindeer husbandry. It was probably this area between Malangen and Vannøy that was Ottar from the Hålogaland area. In the Viking Age, there were also some Norwegian settlements further north and east. East of the North Cape are the scattered archaeological finds of Norwegian settlement in the Viking Age. There are Norwegian names for fjords and islands from the Viking Age, including fjord names with "-anger". Around the year 1050, there were Norwegian settlements on the outer coast of Western Finnmark. Traders and tax collectors traveled even further.
North of Malangen there were Norse farming settlements in the Iron Age. Malangen was considered Finnmark's western border until 1300. There are some archaeological traces of Norse activity around the coast from Tromsø to Kirkenes in the Viking Age. Around Tromsø, the research indicates a Norse/Sami mixed culture on the coast.
From the year 1100 and the next 200–300 years, there are no traces of Norwegian settlement north and east of Tromsø. It is uncertain whether this is due to depopulation, whether it is because the Norwegians further north were not Christianized or because there were no churches north of Lenvik or Tromsø . Norwegian settlement in the far north appears from sources from the 14th century. In the Hanseatic period , the settlement was developed into large areas specialized in commercial fishing, while earlier (in the Viking Age) there had been farms with a combination of fishing and agriculture. In 1307 , a fortress and the first church east of Tromsø were built in Vardø . Vardø became a small Norwegian town, while Vadsø remained Sami. Norwegian settlements and churches appeared along the outermost coast in the Middle Ages. After the Reformation, perhaps as a result of a decline in fish stocks or fish prices, there were Norwegian settlements in the inner fjord areas such as Lebesby in Laksefjord. Some fishing villages at the far end of the coast were abandoned for good. In the interior of Finnmark, there was no national border for a long time and Kautokeino and Karasjok were joint Norwegian-Swedish areas with strong Swedish influence. The border with Finland was established in 1751 and with Russia in 1826.
On a Swedish map from 1626, Norway's border is indicated at Malangen, while Sweden with this map showed a desire to control the Sami area which had been a common area.
The term Northern Norway only came into use at the end of the 19th century and administratively the area was referred to as Tromsø Diocese when Tromsø became a bishopric in 1840. There had been different designations previously: Hålogaland originally included only Helgeland and when Norse settlement spread north in the Viking Age and the Middle Ages, Hålogaland was used for the area north approximately to Malangen , while Finnmark or "Finnmarken", "the land of the Sami", lay outside. The term Northern Norway was coined at a cafe table in Kristiania in 1884 by members of the Nordlændingernes Forening and was first commonly used in the interwar period as it eventually supplanted "Hålogaland".
State formation
The battle in Hafrsfjord in the year 872 has long been regarded as the day when Norway became a kingdom. The year of the battle is uncertain (may have been 10-20 years later). The whole of Norway was not united in that battle: the process had begun earlier and continued a couple of hundred years later. This means that the geographical area became subject to a political authority and became a political unit. The geographical area was perceived as an area as it is known, among other things, from Ottar from Hålogaland's account for King Alfred of Wessex around the year 880. Ottar described "the land of the Norwegians" as very long and narrow, and it was narrowest in the far north. East of the wasteland in the south lay Sveoland and in the north lay Kvenaland in the east. When Ottar sailed south along the land from his home ( Malangen ) to Skiringssal, he always had Norway ("Nordveg") on his port side and the British Isles on his starboard side. The journey took a good month. Ottar perceived "Nordveg" as a geographical unit, but did not imply that it was a political unit. Ottar separated Norwegians from Swedes and Danes. It is unclear why Ottar perceived the population spread over such a large area as a whole. It is unclear whether Norway as a geographical term or Norwegians as the name of a ethnic group is the oldest. The Norwegians had a common language which in the centuries before Ottar did not differ much from the language of Denmark and Sweden.
According to Sverre Steen, it is unlikely that Harald Hårfagre was able to control this entire area as one kingdom. The saga of Harald was written 300 years later and at his death Norway was several smaller kingdoms. Harald probably controlled a larger area than anyone before him and at most Harald's kingdom probably included the coast from Trøndelag to Agder and Vestfold as well as parts of Viken . There were probably several smaller kingdoms of varying extent before Harald and some of these are reflected in traditional landscape names such as Ranrike and Ringerike . Landscape names of "-land" (Rogaland) and "-mark" (Hedmark) as well as names such as Agder and Sogn may have been political units before Harald.
According to Sverre Steen
My wife made lovely vegetable soup and of course she made some lovely croutons to accompany her soup!
365/2021 - Expanding Horizons ~ 293/365
Stay Safe and Healthy Everyone!
Thanks to everyone who views this photo, adds a note, leaves a comment and of course BIG thanks to anyone who chooses to favourite my photo .... Thanks to you all!
Profilele hidroizolante externe de imbinare pentru colturi se folosesc la rosturi de turnare (constructive ) in constructii de beton, de exemplu: pentru jonctiuni ale peretilor si placilor.
Caracteristici hidroizolatii externe imbinari colturi:
Profilele hidroizolante externe de imbinare pentru colturi se instaleaza usor, nefiind nevoie de modificarea armaturii.
365/2021 - Expanding Horizons - Day 66 Mar 7 - Dinner in Vegas at Gordon Ramsey's Pub and Grill at Caesar's Palace casino - our son always wanted to eat at one of his restaurants so they took us here for dinner awesome food. Was not disappointed with the food, I had fish and chips of course, the rest had steak. I have never had sticky toffee pudding before and I thought it was awesome. www.gordonramsayrestaurants.com/pub-and-grill-las-vegas/
Fine Art Ballet Photography: Nikon D810 Elliot McGucken Fine Art Ballerina Dancer Dancing Ballet Spring Wildflowers! Black leotard!
Dancing for Dynamic Dimensions Theory dx4/dt=ic: The fourth dimension is expanding relative to the three spatial dimensions at the rate of c!
New ballet & landscape instagrams!
www.instagram.com/elliotmcgucken/
Nikon D810 Epic Fine Art Ballerina Goddess Dancing Ballet! Dr. Elliot McGucken Fine Art Ballet!
Marrying epic landscape, nature, and urban photography to ballet!
Nikon D810 with the Nikon MB-D12 Multi Battery Power Pack / Grip for D800 and D810 Digital Cameras allows one to shoot at a high to catch the action FPS! Ballerina Dance Goddess Photos! Pretty, Tall Ballet Swimsuit Bikini Model Goddess! Captured with the AF-S NIKKOR 70-200mm f/2.8G ED VR II from Nikon, and the Sigma 50mm f/1.4 DG HSM Art Lens for Nikon! Love them both!
www.facebook.com/45surfAchillesOdysseyMythology
A pretty goddess straight out of Homer's Iliad & Odyssey!
New Instagram! instagram.com/45surf
New facebook: www.facebook.com/45surfAchillesOdysseyMythology
Join my new fine art ballet facebook page! www.facebook.com/fineartballet/
The 45EPIC landscapes and goddesses are straight out of Homer's Iliad & Odyssey!
I'm currently updating a translation with the Greek names for the gods and goddesses--will publish soon! :)
"RAGE--Sing, O goddess, the anger of Achilles son of Peleus, that brought countless ills upon the Achaeans. Many a brave soul did it send hurrying down to Hades, and many a hero did it yield a prey to dogs and vultures, for so were the counsels of Zeus fulfilled from the day on which the son of Atreus, king of men, and great Achilles, first fell out with one another. " --Homer's Iliad capturing the rage of the 45EPIC landscapes and seascapes! :)
Ludwig van Beethoven: "Music/poetry/art should strike fire from the heart of man, and bring tears from the eyes of woman."
365/2021 - Expanding Horizons - Day 155 June4 - Saw seven eagles yesterday on the beach all in one group, was awesome.
Pretty Blue Eyes Beautiful Swimsuit Bikini Model Goddess! Helen from Homer's Iliad! 45SURF 45EPIC Tall Thin Fit Blonde Athletic Bikini Swimsuit California Beach Venus Goddess! Sony A7R III & Sony FE 70-200mm f/2.8 GM OSS Lens! Epic Bokeh!
All my photography celebrates the physics of light! The McGucken Principle of the fourth expanding dimension: The fourth dimension is expanding at the rate of c relative to the three spatial dimensions: dx4/dt=ic .
Light Time Dimension Theory: The Foundational Physics Unifying Einstein's Relativity and Quantum Mechanics: A Simple, Illustrated Introduction to the Unifying Physical Reality of the Fourth Expanding Dimensionsion dx4/dt=ic !: geni.us/Fa1Q
Epic Art & 45EPIC Eagle Gear exalting golden ratio designs for your Hero's Odyssey -- 45SURF T-shirts & Hoodies & more:
"Between every two pine trees there is a door leading to a new way of life." --John Muir
Epic Stoicism guides my fine art odyssey and photography: geni.us/epicstoicism
“The clearest way into the Universe is through a forest wilderness.” --John Muir
Epic Poetry inspires all my photography: geni.us/9K0Ki Epic Poetry for Epic Landscape Photography: Exalt Fine Art Nature Photography with the Poetic Wisdom of John Muir, Emerson, Thoreau, Homer's Iliad, Milton's Paradise Lost & Dante's Inferno Odyssey
“The mountains are calling and I must go.” --John Muir
Support epic fine art! 45surf ! Bitcoin: 1FMBZJeeHVMu35uegrYUfEkHfPj5pe9WNz
Exalt the goddess archetype in the fine art of photography! My Epic Book: Photographing Women Models!
Portrait, Swimsuit, Lingerie, Boudoir, Fine Art, & Fashion Photography Exalting the Venus Goddess Archetype: How to Shoot Epic ... Epic! Beautiful Surf Fine Art Portrait Swimsuit Bikini Models!
Some of my epic books, prints, & more!
Exalt your photography with Golden Ratio Compositions!
Golden Ratio Compositions & Secret Sacred Geometry for Photography, Fine Art, & Landscape Photographers: How to Exalt Art with Leonardo da Vinci's, Michelangelo's!
Epic Landscape Photography:
A Simple Guide to the Principles of Fine Art Nature Photography: Master Composition, Lenses, Camera Settings, Aperture, ISO, ... Hero's Odyssey Mythology Photography)
All art is but imitation of nature.-- Seneca (Letters from a Stoic - Letter LXV: On the First Cause)
The universe itself is God and the universal outpouring of its soul. --Chrysippus (Quoted by Cicero in De Natura Deorum)
Season of mists and mellow fruitfulness
Close bosom-friend of the maturing sun
Conspiring with him how to load and bless
With fruit the vines that round the thatch-eves run;
To bend with apples the moss'd cottage-trees,
And fill all fruit with ripeness to the core;
To swell the gourd, and plump the hazel shells
With a sweet kernel; to set budding more,
And still more, later flowers for the bees,
Until they think warm days will never cease,
For Summer has o'er-brimm'd their clammy cells. --To Autumn. by John Keats
Fine Art Ballet Photography: Nikon D810 Elliot McGucken Fine Art Ballerina Dancer Dancing Ballet Spring Wildflowers! Black leotard!
Dancing for Dynamic Dimensions Theory dx4/dt=ic: The fourth dimension is expanding relative to the three spatial dimensions at the rate of c!
New ballet & landscape instagrams!
www.instagram.com/elliotmcgucken/
Nikon D810 Epic Fine Art Ballerina Goddess Dancing Ballet! Dr. Elliot McGucken Fine Art Ballet!
Marrying epic landscape, nature, and urban photography to ballet!
Nikon D810 with the Nikon MB-D12 Multi Battery Power Pack / Grip for D800 and D810 Digital Cameras allows one to shoot at a high to catch the action FPS! Ballerina Dance Goddess Photos! Pretty, Tall Ballet Swimsuit Bikini Model Goddess! Captured with the AF-S NIKKOR 70-200mm f/2.8G ED VR II from Nikon, and the Sigma 50mm f/1.4 DG HSM Art Lens for Nikon! Love them both!
www.facebook.com/45surfAchillesOdysseyMythology
A pretty goddess straight out of Homer's Iliad & Odyssey!
New Instagram! instagram.com/45surf
New facebook: www.facebook.com/45surfAchillesOdysseyMythology
Join my new fine art ballet facebook page! www.facebook.com/fineartballet/
The 45EPIC landscapes and goddesses are straight out of Homer's Iliad & Odyssey!
I'm currently updating a translation with the Greek names for the gods and goddesses--will publish soon! :)
"RAGE--Sing, O goddess, the anger of Achilles son of Peleus, that brought countless ills upon the Achaeans. Many a brave soul did it send hurrying down to Hades, and many a hero did it yield a prey to dogs and vultures, for so were the counsels of Zeus fulfilled from the day on which the son of Atreus, king of men, and great Achilles, first fell out with one another. " --Homer's Iliad capturing the rage of the 45EPIC landscapes and seascapes! :)
Ludwig van Beethoven: "Music/poetry/art should strike fire from the heart of man, and bring tears from the eyes of woman."
In the winter of viral discontent, it might be easy to overlook some recent breakthroughs in lifespan expansion.
David Sinclair from Harvard Medical School just published the latest advances in reversing the biological clock and restoring function in the vision system. Full disclosure: after I read his book, he helped with due diligence when we became the largest investor in Cambrian Bio, a company that seeks to reverse the root causes of aging and disease.
Sinclair’s focus in on analog information loss, the epigenetic noise that accumulates in the methylation patterns running along our DNA and disturbing its expression. This degradation is a biological clock of aging, and today’s results “tell us the clock doesn't just represent time—it is time," said Sinclair. "If you wind the hands of the clock back, time also goes backward." (more book quotes below, after the news)
Today’s news: “Harvard Medical School scientists have successfully restored vision in mice by turning back the clock on aged eye cells in the retina to recapture youthful gene function. The achievement represents the first successful attempt to reverse glaucoma-induced vision loss, rather than merely stem its progression, the team said. If replicated through further studies, the approach could pave the way for therapies to promote tissue repair across various organs and reverse aging and age-related diseases in humans.
The team's approach is based on a new theory about why we age. Most cells in the body contain the same DNA molecules but have widely diverse functions. To achieve this degree of specialization, these cells must read only genes specific to their type. This regulatory function is the purview of the epigenome, a system of turning genes on and off in specific patterns without altering the basic underlying DNA sequence of the gene.
This theory postulates that changes to the epigenome over time cause cells to read the wrong genes and malfunction—giving rise to diseases of aging. One of the most important changes to the epigenome is DNA methylation, a process by which methyl groups are tacked onto DNA. Patterns of DNA methylation are laid down during embryonic development to produce the various cell types. Over time, youthful patterns of DNA methylation are lost, and genes inside cells that should be switched on get turned off and vice versa, resulting in impaired cellular function. Some of these DNA methylation changes are predictable and have been used to determine the biologic age of a cell or tissue.
The treatment worked similarly well in elderly, 12-month-old mice with diminishing vision due to normal aging. Following treatment of the elderly mice, the gene expression patterns and electrical signals of the optic nerve cells were similar to young mice, and vision was restored. When the researchers analyzed molecular changes in treated cells, they found reversed patterns of DNA methylation—an observation suggesting that DNA methylation is not a mere marker or a bystander in the aging process, but rather an active agent driving it.”
And from the Nature Paper:
“Ageing is a degenerative process that leads to tissue dysfunction and death. A proposed cause of ageing is the accumulation of epigenetic noise that disrupts gene expression patterns, leading to decreases in tissue function and regenerative capacity. Changes to DNA methylation patterns over time form the basis of ageing clocks… Collectively, these changes cause cells to lose their identity and so to lose the DNA-, RNA- and protein-expression patterns that once promoted their youthful resilience. These data indicate that mammalian tissues retain a record of youthful epigenetic information—encoded in part by DNA methylation—that can be accessed to improve tissue function and promote regeneration in vivo.”
Some of my favorite passages from his recent book, Lifespan:
“Aging, quite simply, is a loss of information. Yes, a singular reason why we age.” (p.20)
“Unlike digital DNA, analog information degrades over time — falling victim to the conspiring forces of magnetic fields, gravity, cosmic rays, and oxygen. Worse still, information is lost as it’s copied.” (p.22)
“Our DNA is constantly under attack. On average, each of our 46 chromosomes is broken in some way every time a cell copies its DNA, amounting to more than 2 trillion breaks in our body per day. And that’s just the breaks that occur during replication. If we didn’t have a way to repair our DNA wouldn’t last long.: (p.44) “Sirtuins stabilize human rDNA and prevent cellular senescence.” (p.43) “Adding more copies of the sirtuin genes increases the health and extends the lifespan of mice, just as adding extra copies does in yeast.” (p.45).
“Aging itself is a disease. Physicians and researchers have been avoiding saying that for a long time. Aging, we’ve long been told, is simply the process of growing old. And growing old has long been seen as an inevitable part of life.” (p.67).
“We know the process of aging begins long before we notice it. Girls who go through puberty earlier than normal, for example, have an accelerated epigenetic clock. The mistakes are there, even as a teenager.” (p.72)
“Your chance of developing a lethal disease increases by a thousandfold between the ages of 20 and 70, so preventing one disease makes little difference to lifespan.” (p.77) “Though smoking increases the risk of getting cancer five fold, being 50 years old increases your cancer risk a hundredfold. By the age of 70, it’s a thousandfold. Such exponentially increasing odds also apply to heart disease. And diabetes. And dementia.” (p.80)
“There’s a reason smokers seem to age fast: they do age faster. Smoking is not a private, victimless activity. The levels of DNA-damaging aromatic amines in cigarette smoke are about 50 to 60 times as high in secondhand as in firsthand smoke. In some places — cities with lots of cars, especially — the simple act of breathing is enough to do extra damage to your DNA.” (p.113)
“NAD boosts the activity of all seven sirtuins. And because NAD is used by over 500 different enzymes, without any NAD, we’d be dead in 30 seconds. NAD acts as a fuel for sirtuins. NAD levels decrease with age throughout the body. Human studies with NAD boosters (NMN and NR) are ongoing. So far, there has been no toxicity, not even a hint of it.” (p.134)
“Once you recognize that there are universal regulators of aging in everything from yeast to roundworms to mice to humans… and once you recognize that these regulators can be changed with a molecule such as NMN or a few hours of vigorous exercise or a few less meals… and once you realize that it’s all just one disease, it all becomes clear: Aging is going to be remarkably easy to tackle. Easier than cancer. I know how that sounds. It sounds crazy.” (p.148)
“Together, all the DNA in our body, if laid end to end, would stretch twice the diameter of the solar system. Unlike a simple DVD, the DNA in our cells is wet and vibrating in three dimensions. No wonder gene reading becomes difficult the older we get; it’s miraculous that any cell finds the right genes in the first place.” (p.159)
“That’s the world’s biggest problem: the future is seen as someone else’s concern. This is what I want to change— more than anything else in the world. I want everyone to expect that they will meet not only their grandchildren but their great-great-grandchildren. We will be accountable — in this life — for the decisions we made in the past that will impact the future. That, more than anything else, is how our understanding of aging and inevitable prolonged vitality is going to change the world. It will compel us to confront the challenges we currently push down the road.” (p.292-3)
Arches National Park is a national park in eastern Utah, United States. The park is adjacent to the Colorado River, 4 miles (6 km) north of Moab, Utah. More than 2,000 natural sandstone arches are located in the park, including the well-known Delicate Arch, as well as a variety of unique geological resources and formations. The park contains the highest density of natural arches in the world.
The park consists of 310.31 square kilometres (76,680 acres; 119.81 sq mi; 31,031 ha) of high desert located on the Colorado Plateau. The highest elevation in the park is 5,653 feet (1,723 m) at Elephant Butte, and the lowest elevation is 4,085 feet (1,245 m) at the visitor center. The park receives an average of less than 10 inches (250 mm) of rain annually.
Administered by the National Park Service, the area was originally named a national monument on April 12, 1929, and was re designated as a national park on November 12, 1971. The park received more than 1.6 million visitors in 2018.
As stated in the foundation document in U.S. National Park Service website:
The purpose of Arches National Park is to protect extraordinary examples of geologic features including arches, natural bridges, windows, spires, and balanced rocks, as well as other features of geologic, historic, and scientific interest, and to provide opportunities to experience these resources and their associated values in their majestic natural settings.
The national park lies above an underground evaporite layer or salt bed, which is the main cause of the formation of the arches, spires, balanced rocks, sandstone fins, and eroded monoliths in the area. This salt bed is thousands of feet thick in places and was deposited in the Paradox Basin of the Colorado Plateau some 300 million years ago (Mya) when a sea flowed into the region and eventually evaporated. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 200 Mya), desert conditions prevailed in the region and the vast Navajo Sandstone was deposited. An additional sequence of stream laid and windblown sediments, the Entrada Sandstone (about 140 Mya), was deposited on top of the Navajo. Over 5,000 feet (1,500 m) of younger sediments were deposited and have been mostly eroded. Remnants of the cover exist in the area including exposures of the Cretaceous Mancos Shale. The arches of the area are developed mostly within the Entrada formation.
The weight of this cover caused the salt bed below it to liquefy and thrust up layers of rock into salt domes. The evaporites of the area formed more unusual "salt anticlines" or linear regions of uplift. Faulting occurred and whole sections of rock subsided into the areas between the domes. In some places, they turned almost on edge. The result of one such 2,500-foot (760 m) displacement, the Moab Fault, is seen from the visitor center.
As this subsurface movement of salt shaped the landscape, erosion removed the younger rock layers from the surface. Except for isolated remnants, the major formations visible in the park today are the salmon-colored Entrada Sandstone, in which most of the arches form, and the buff-colored Navajo Sandstone. These are visible in layer-cake fashion throughout most of the park. Over time, water seeped into the surface cracks, joints, and folds of these layers. Ice formed in the fissures, expanding and putting pressure on surrounding rock, breaking off bits and pieces. Winds later cleaned out the loose particles. A series of free-standing fins remained. Wind and water attacked these fins until, in some, the cementing material gave way and chunks of rock tumbled out. Many damaged fins collapsed. Others, with the right degree of hardness and balance, survived despite their missing sections. These became the famous arches.
Although the park's terrain may appear rugged and durable, it is extremely fragile. More than 1 million visitors each year threaten the fragile high-desert ecosystem. The problem lies within the soil's crust, which is composed of cyanobacteria, algae, fungi, and lichens that grow in the dusty parts of the park. Factors that make Arches National Park sensitive to visitor damage include being a semiarid region, the scarce, unpredictable rainfall, lack of deep freezing, and lack of plant litter, which results in soils that have both a low resistance to and slow recovery from, compressional forces such as foot traffic. Methods of indicating effects on the soil are cytophobic soil crust index, measuring of water infiltration, and t-tests that are used to compare the values from the undisturbed and disturbed areas.
Geological processes that occurred over 300 million years ago caused a salt bed to be deposited, which today lies beneath the landscape of Arches National Park.[ Over time, the salt bed was covered with sediments that eventually compressed into rock layers that have since been named Entrada Standstone. Rock layers surrounding the edge of the salt bed continued to erode and shift into vertical sandstone walls called fins. Sand collected between vertical walls of the fins, then slightly acidic rain combined with carbon dioxide in the air allowed for the chemical formation of carbonic acid within the trapped sand. Over time, the carbonic acid dissolved the calcium carbonate that held the sandstone together. Many of the rock formations have weaker layers of rock on bottom that are holding stronger layers on top. The weaker layers would dissolve first, creating openings in the rock. Gravity caused pieces of the stronger rock layer to fall piece by piece into an arch shape. Arches form within rock fins at points of intense fracturing localization, or weak points in the rock's formation, caused by horizontal and vertical discontinuities. Lastly, water, wind, and time continued this erosion process and ultimately created the arches of Arches National Park. All of the arches in the park are made of Entrada Sandstone, however, there are slight differences in how each arch was developed. This allows the Entrada Sandstone to be categories into 3 groups including Slick rock members, Dewey rock members, and Moab members. Vertical arches can be developed from Slick rock members, a combination of Slick rock members and Moab members, or Slick rock members resting above Dewey rock members. Horizontal arches (also called potholes) are formed when a vertical pothole formation meets a horizontal cave, causing a union into a long arch structure. The erosion process within Arches National Park will continue as time continues to pass. Continued erosion combined with vertical and horizontal stress will eventually cause arches to collapse, but still, new arches will continue to form for thousands of years.
Humans have occupied the region since the last ice age 10,000 years ago. Fremont people and Ancestral Puebloans lived in the area until about 700 years ago. Spanish missionaries encountered Ute and Paiute tribes in the area when they first came through in 1775, but the first European-Americans to attempt settlement in the area were the Mormon Elk Mountain Mission in 1855, who soon abandoned the area. Ranchers, farmers, and prospectors later settled Moab in the neighboring Riverine Valley in the late 1870s. Word of the beauty of the surrounding rock formations spread beyond the settlement as a possible tourist destination.
The Arches area was first brought to the attention of the National Park Service by Frank A. Wadleigh, passenger traffic manager of the Denver and Rio Grande Western Railroad. Wadleigh, accompanied by railroad photographer George L. Beam, visited the area in September 1923 at the invitation of Alexander Ringhoffer, a Hungarian-born prospector living in Salt Valley. Ringhoffer had written to the railroad to interest them in the tourist potential of a scenic area he had discovered the previous year with his two sons and a son-in-law, which he called the Devils Garden (known today as the Klondike Bluffs). Wadleigh was impressed by what Ringhoffer showed him, and suggested to Park Service director Stephen T. Mather that the area be made a national monument.
The following year, additional support for the monument idea came from Laurence Gould, a University of Michigan graduate student (and future polar explorer) studying the geology of the nearby La Sal Mountains, who was shown the scenic area by local physician Dr. J. W. "Doc" Williams.
A succession of government investigators examined the area, in part due to confusion as to the precise location. In the process, the name Devils Garden was transposed to an area on the opposite side of Salt Valley that includes Landscape Arch, the longest arch in the park. Ringhoffer's original discovery was omitted, while another area nearby, known locally as the Windows, was included. Designation of the area as a national monument was supported by the Park Service in 1926 but was resisted by President Calvin Coolidge's Interior Secretary, Hubert Work. Finally, in April 1929, shortly after his inauguration, President Herbert Hoover signed a presidential proclamation creating the Arches National Monument, consisting of two comparatively small, disconnected sections. The purpose of the reservation under the 1906 Antiquities Act was to protect the arches, spires, balanced rocks, and other sandstone formations for their scientific and educational value. The name Arches was suggested by Frank Pinkely, superintendent of the Park Service's southwestern national monuments, following a visit to the Windows section in 1925.
In late 1938, President Franklin D. Roosevelt signed a proclamation that enlarged the Arches to protect additional scenic features and permit the development of facilities to promote tourism. A small adjustment was made by President Dwight Eisenhower in 1960 to accommodate a new road alignment.
In early 1969, just before leaving office, President Lyndon B. Johnson signed a proclamation substantially enlarging the Arches. Two years later, President Richard Nixon signed legislation enacted by Congress, which significantly reduced the total area enclosed, but changed its status. Arches National Park was formally dedicated in May 1972.
In 1980, vandals attempted to use an abrasive kitchen cleanser to deface ancient petroglyphs in the park, prompting park officials to recruit physicist John F. Asmus, who specialized in using lasers to restore works of art, to use his technology to repair the damage. Asmus "zapped the panel with intense light pulses and succeeded in removing most of the cleanser".
Climbing Balanced Rock or any named or unnamed arch in Arches National Park with an opening larger than 3 ft (0.9 m) is banned by park regulations. Climbing on other features in the park is allowed but regulated; in addition, slacklining and BASE jumping are banned parkwide.
Climbing on named arches within the park had long been banned by park regulations, but following Dean Potter's successful free climb on Delicate Arch in May 2006, the wording of the regulations was deemed unenforceable by the park attorney. In response, the park revised its regulations later that month, eventually imposing the current ban on arch climbing in 2014.
Approved recreational activities include auto touring, hiking, bicycling, camping at the Devils Garden campground, backpacking, canyoneering, and rock climbing, with permits required for the last three activities. Guided commercial tours and ranger programs are also available.
Astronomy is also popular in the park due to its dark skies, despite the increasing light pollution from towns such as Moab.
Delicate Arch is the subject of the third 2014 quarter of the U.S. Mint's America the Beautiful Quarters program commemorating national parks and historic sites. The Arches quarter had the highest production of the five 2014 national park quarters, with more than 465 million minted.
American writer Edward Abbey was a park ranger at Arches National Monument in 1956 and 1957, where he kept journals that became his book Desert Solitaire. The success of Abbey's book, as well as interest in adventure travel, has drawn many hikers, mountain bikers, and off-pavement driving enthusiasts to the area. Permitted activities within the park include camping, hiking along designated trails, backpacking, canyoneering, rock climbing, bicycling, and driving along existing roads, both paved and unpaved. The Hayduke Trail, an 812 mi (1,307 km) backpacking route named after one of Edward Abbey's characters, begins in the park.
An abundance of wildlife occurs in Arches National Park, including spadefoot toads, antelope squirrels, scrub jays, peregrine falcons, many kinds of sparrows, red foxes, desert bighorn sheep, kangaroo rats, mule deers, cougars, midget faded rattlesnakes, yucca moths, western rattlesnakes, and collared lizards.
A number of plant species are common in the park, including prickly pear cactus, Indian ricegrass, bunch grasses, cheatgrass, moss, liverworts, Utah juniper, Mormon tea, blackbrush, cliffrose, four-winged saltbrush, pinyon pine, evening primrose, sand verbena, yucca, and sacred datura.
Biological soil crust consisting of cyanobacteria, lichen, mosses, green algae, and microfungi is found throughout southeastern Utah. The fibrous growths help keep soil particles together, creating a layer that is more resistant to erosion. The living soil layer readily absorbs and stores water, allowing more complex forms of plant life to grow in places with low precipitation levels.
Among the notable features of the park are the following:
Balanced Rock – a large balancing rock, the size of three school buses
Courthouse Towers – a collection of tall stone columns
Dark Angel – a free-standing 150 ft-tall (46 m) sandstone pillar at the end of the Devils Garden Trail
Delicate Arch – a lone-standing arch that has become a symbol of Utah and the most recognized arch in the park
Devils Garden – many arches and columns scattered along a ridge
Double Arch – two arches that share a common end
Fiery Furnace – an area of maze-like narrow passages and tall rock columns (see biblical reference, Book of Daniel, chapter 3)
Landscape Arch – a very thin and long arch in the Devils Garden with a span of 290 ft (88 m) (the longest arch in the park)
Petrified Dunes – petrified remnants of dunes blown from the ancient lakes that covered the area
The Phallus – a rock spire that resembles a phallus
Wall Arch – located along the popular Devils Garden Trail; collapsed sometime on August 4/5, 2008
The Three Gossips –a mid-sized sandstone tower located in the Courthouse Towers area.
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.
Fine Art Ballet Photography: Nikon D810 Elliot McGucken Fine Art Ballerina Dancer Dancing Ballet Spring Wildflowers! Black leotard!
Dancing for Dynamic Dimensions Theory dx4/dt=ic: The fourth dimension is expanding relative to the three spatial dimensions at the rate of c!
New ballet & landscape instagrams!
www.instagram.com/elliotmcgucken/
Nikon D810 Epic Fine Art Ballerina Goddess Dancing Ballet! Dr. Elliot McGucken Fine Art Ballet!
Marrying epic landscape, nature, and urban photography to ballet!
Nikon D810 with the Nikon MB-D12 Multi Battery Power Pack / Grip for D800 and D810 Digital Cameras allows one to shoot at a high to catch the action FPS! Ballerina Dance Goddess Photos! Pretty, Tall Ballet Swimsuit Bikini Model Goddess! Captured with the AF-S NIKKOR 70-200mm f/2.8G ED VR II from Nikon, and the Sigma 50mm f/1.4 DG HSM Art Lens for Nikon! Love them both!
www.facebook.com/45surfAchillesOdysseyMythology
A pretty goddess straight out of Homer's Iliad & Odyssey!
New Instagram! instagram.com/45surf
New facebook: www.facebook.com/45surfAchillesOdysseyMythology
Join my new fine art ballet facebook page! www.facebook.com/fineartballet/
The 45EPIC landscapes and goddesses are straight out of Homer's Iliad & Odyssey!
I'm currently updating a translation with the Greek names for the gods and goddesses--will publish soon! :)
"RAGE--Sing, O goddess, the anger of Achilles son of Peleus, that brought countless ills upon the Achaeans. Many a brave soul did it send hurrying down to Hades, and many a hero did it yield a prey to dogs and vultures, for so were the counsels of Zeus fulfilled from the day on which the son of Atreus, king of men, and great Achilles, first fell out with one another. " --Homer's Iliad capturing the rage of the 45EPIC landscapes and seascapes! :)
Ludwig van Beethoven: "Music/poetry/art should strike fire from the heart of man, and bring tears from the eyes of woman."
Been busy expanding my 8th army!
Let me know what you think ;)
PS: Finished model: www.flickr.com/photos/75513482@N08/8722455449/in/photostr...
365/2021 - Expanding Horizons - Day 71 Mar 12 - First day home had to go across the river and caught this ship coming into Astoria in the fog.
Square shape by Angel Ecija Blanco
By looking at the crease pattern, I realized that you can fold other shaped boxes as well. Hexagonal & Octagonal versions calculated by me.
This is the second model that I folded from Angel Ecija Blanco's designs. The first one is the Self-Closing Twist Box (origamitutorials.com/self-closing-origami-twist-box/). Both designs share a few elements and are interesting to fold. You can read more here: origamitutorials.com/expandable-origami-coin-purse/
Fine Art Ballet Photography: Nikon D810 Elliot McGucken Fine Art Ballerina Dancer Dancing Ballet Spring Wildflowers! Black leotard!
Dancing for Dynamic Dimensions Theory dx4/dt=ic: The fourth dimension is expanding relative to the three spatial dimensions at the rate of c!
New ballet & landscape instagrams!
www.instagram.com/elliotmcgucken/
Nikon D810 Epic Fine Art Ballerina Goddess Dancing Ballet! Dr. Elliot McGucken Fine Art Ballet!
Marrying epic landscape, nature, and urban photography to ballet!
Nikon D810 with the Nikon MB-D12 Multi Battery Power Pack / Grip for D800 and D810 Digital Cameras allows one to shoot at a high to catch the action FPS! Ballerina Dance Goddess Photos! Pretty, Tall Ballet Swimsuit Bikini Model Goddess! Captured with the AF-S NIKKOR 70-200mm f/2.8G ED VR II from Nikon, and the Sigma 50mm f/1.4 DG HSM Art Lens for Nikon! Love them both!
www.facebook.com/45surfAchillesOdysseyMythology
A pretty goddess straight out of Homer's Iliad & Odyssey!
New Instagram! instagram.com/45surf
New facebook: www.facebook.com/45surfAchillesOdysseyMythology
Join my new fine art ballet facebook page! www.facebook.com/fineartballet/
The 45EPIC landscapes and goddesses are straight out of Homer's Iliad & Odyssey!
I'm currently updating a translation with the Greek names for the gods and goddesses--will publish soon! :)
"RAGE--Sing, O goddess, the anger of Achilles son of Peleus, that brought countless ills upon the Achaeans. Many a brave soul did it send hurrying down to Hades, and many a hero did it yield a prey to dogs and vultures, for so were the counsels of Zeus fulfilled from the day on which the son of Atreus, king of men, and great Achilles, first fell out with one another. " --Homer's Iliad capturing the rage of the 45EPIC landscapes and seascapes! :)
Ludwig van Beethoven: "Music/poetry/art should strike fire from the heart of man, and bring tears from the eyes of woman."
Follow my Fine Art Ballet instagram!