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I grew up in this town, my poetry was born between the hill and the river, it took its voice from the rain, and like the timber, it steeped itself in the forests.
Pablo Neruda
We came on this little trip to see Burney falls which we had heard about and here's a bit of the history of it according to Wikipedia
The park is within the Cascade Range and Modoc Plateau natural region, with 910 acres (4 km²) of forest and five miles (8 km) of streamside and lake shoreline, including a portion of Lake Britton.
The park's centerpiece is the 129 foot (39 m) Burney Falls, which is not the highest or largest waterfall in the state, but arguably the most beautiful. Additional water comes from springs, joining to create a mist-filled basin. Burney Creek originates from the park's underground springs and flows to Lake Britton, getting larger along the way to the falls.
The park's landscape was created by volcanic activity as well as erosion from weather and streams. This volcanic region is surrounded by mountain peaks and is covered by black volcanic rock, or basalt. Created over a million years ago, the layered, porous basalt retains rainwater and snow melt, which forms a large underground reservoir.
Within the park, the water emerges as springs at and above Burney Falls, where it flows at 100 million gallons every day (4.4 m³/s).
Teddy Roosevelt named it the eighth wonder of the world...
view on black it looks kind of cool I promise!
Original poster - 'Blowing in the Mind/ Mister Tambourine Man', colour screen-print from multiple stencils on gold foil paper, designed by Martin Sharp, London, 1968. It is a complex multi-stencil design in red and black inks screen-printed on gold foil paper, the design featuring multiple radiating circular motifs with two portraits of Bob Dylan, the large central frontal profile with reflecting dark glasses and caption 'Blowing in the Mind', the smaller side profile placed in front of an entwined 'Mister Tambourine Man'. Lyrics of the song are written within letters and circles. This was the first "serious" poster I bought.
Yesterday was so chilly in Toronto (-18C with windchill), I decided to capture my cactus rather than shooting outdoor. I have this gift in December 2009, which is from my friend Katherine.
"This is a very popular house plants known by a variety of names including Christmas Cactus, Thanksgiving Cactus, Crab Cactus and Holiday Cactus, which are Schlumbergera cultivars, and flower in white, pink, yellow, orange, red or purple."
after all that plagiarism and copying others work discussions that float around flickr right now, i felt really bad about last weeks picture...
i mean, i am often inspired by other peoples work but usually i try to make my pictures really mine by doing things differently than the stuff i got my inspiration from... but last weeks picture really is nothing more than a copy with minor differences to the original. that's why i'm feeling bad and i wanted to at least use the techniques i learned copying that work in this weeks picture so that i can say i copied for a reason...
so here you go, using last weeks method i created this (and no, the concept is not very original, i've seen it around a few times but at least this time i feel like it really is my work...)...
anyway, sorry for the rant but reading all those discussion really made me feel bad about some of my work...
oh, and for those who want to know what's going on in my life:
a photography school in vienna accepted me (finally!!) so i'm gonna start studying photography starting in 2 weeks... plus, since that program is not very elaborate, i also enrolled at university again and am starting to study comparative literature starting from next week... on the other hand, i am still looking for a job but so far no one wanted me... :(
at least studying will keep me busy until i can apply at the academy of advertising...
scout says this appeared in explore!! thank you guys!! :)
In the quiet corners of the bookshop, he traced the spines of old novels, each one stirring a memory he thought he’d long since shelved.... then kindly posed for this photo.
Another from my smoke session. This is a combination of two images duplicated and flipped in photoshop plus a little saturation painting and sharpening.
All exposed at 160th sec, f11, ISO 100 at 70mm focal length. I used a slave flash slightly behind and below the smoke and used a home made snoot on my speedlight set at 50% power. With black card at the rear and also a nightlight candle on the floor hopefully to help the smoke form more interesting swirls from the rising heat.
Thanks for looking and I hope you like it. Please press L to view on black and full size (recommended).
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Copyright © MiqsPixImaging 2013
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No part of this picture may be reproduced or transmitted in any form or by any means (on websites, blogs) without prior permission.
Will be busy printing and framing in nice large, matted formats and frames and museum glass! Five of these photos will be printed on 40" x 60" floating wall mounted metal sheets! I think I know which--will share photos of the photos hanging on the walls!
And I am mounting some on plexiglass/acryllic--front mounting them! Some I am printing on lossy fuji-crystal archival paper too, and then front mounting 40"x60" versions to plexiglass--will send photos!
The secret to HDR photography is that you want people to say, "Woe dude--that's unreal!" And not, "Dude--that's not real!" "Unreal" is the word they use when they're trying to figure out the photo--what makes it cool--is it a photo? Is it painted? How'd it come to be--how'd you bend the light that way? "That's not real," is what they say if you have the saturation/HDR/ etc. turned up too high. :)
Some (almost) final edits for my Los Angeles Gallery Show! Printing them on metallic paper at 13" x 19" and mounting and framing them on a 4mm 18x24 white mat and 2" dark wood frame. Also printing some 40" x 70" whihc is over three feet by five feet! Wish you all could come (and hang out with the goddesses)!
Let me know your favs.!
New Instagram!
Videos!
Nikon D800E / D800 HDR Anelope Valley Ghosts in Slot Canyonfor Gallery Show!
Yay! I booked a major photography show at a major LA gallery in December! Will also be giving some lectures on the story--the Hero's Journey Mythology--behind the photography!
Join/like my facebook!
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Preparing for some gallery shows this fall to celebrate 300,000,000 views! Printing a few dozen photographs in ~ 30"x40" formats and mounting/framing. Here are some close-to-final edits. HDR photography 7 exposures shot at 1EV and combined in photomatix: 36 megapixel Nikon D800E with the awesome Nikon 14-24mm f/2.8G ED AF-S Nikkor Wide Angle Zoom Lens. 45SURF Hero's Journey Mythology Photography!
Epic Scenic HDR Landscaps Shot with Nikon D800E: Hero's Journey Mythology Photography!
Shot with the Nikon Nikkor wide-angle 14-24 mm 2.8 lens!
Seven exposures @ 1EV finished in photomatix.
Enjoy the Hero's Journey Mythology Photography, and all the best on a hero's journey of your own making!
These were shot with Nikon's best D800 with the 14-24mm wide-angle Nikkor lens. 7 exposures were taken at 1 EV intervals, and combined in photomatix to bring out the shadows and highlights.
Rather large HDR (high dynamic range) photo--you can see great detail both near and far! View the detail at full size!
The Nikon 14-24mm f/2.8G ED AF-S Nikkor Wide Angle Zoom Lens rocks!
High Dynamic Range (HDR) photos rock in capturing the full dynamic range of the scene!
All the best on your epic hero's journey from Johnny Ranger McCoy!
The Delicate Arch in Arches National Park Utah! Nikon D800E Dr. Elliot McGucken Fine Art Landscape & Nature Photography for Los Angeles Fine Art Gallery Show !
Zion National Park Utah! Nikon D800E Dr. Elliot McGucken Fine Art Landscape & Nature Photography for Los Angeles Fine Art Gallery Show !
Yosemite! Nikon D800E Dr. Elliot McGucken Fine Art Landscape & Nature Photography for Los Angeles Fine Art Gallery Show !
Yosemite El Capitan Reflected in the Merced River! Nikon D800E Dr. Elliot McGucken Fine Art Landscape & Nature Photography for Los Angeles Fine Art Gallery Show !
Yosemite El Capitan Reflected in the Merced River! Nikon D800E Dr. Elliot McGucken Fine Art Landscape & Nature Photography for Los Angeles Fine Art Gallery Show !
In diesen Augenblicken wird eine nichtige Kreatur, ein Hund, eine Ratte, ein Käfer, ein verkrümmter Apfelbaum, ein sich über den Hügel schlängelnder Karrenweg, ein moosbewachsener Stein mir mehr als die schönste hingebendste Geliebte der glücklichsten Nacht mir je gewesen ist. Diese stummen und manchmal unbelebten Kreaturen heben sich mir mit einer solchen Fülle, einer solchen Gegenwart der Liebe entgegen, daß mein beglücktes Auge auch ringsum auf keinen toten Fleck zu fallen vermag.
Es erscheint mir alles, was es gibt, alles, dessen ich mich entsinne, alles, was meine verworrensten Gedanken berühren, etwas zu sein.
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In these moments an insignificant creature - a dog, a rat, a beetle, a crippled apple tree, a lane winding over the hill, a moss-covered stone, mean more to me than the most beautiful, abandoned mistress of the happiest night. These mute and, on occasion, inanimate creatures rise toward me with such an abundance, such a presence of love, that my enchanted eye can find nothing in sight void of life.
Everything that exists, everything I can remember, everything touched upon by my confused thoughts, has a meaning.
Hugo von Hofmannsthal, Brief des Lord Chandos an Francis Bacon / The Letter of Lord Chandos
"Surgeons' Hall in Edinburgh, Scotland, is the headquarters of the Royal College of Surgeons of Edinburgh (RCSED). It houses the Surgeons' Hall Museum, and the library and archive of the RCSED. The present Surgeons' Hall was designed by William Henry Playfair and completed in 1832, and is a category A listed building.
Surgeons' Hall Museum is the major medical museum in Scotland, and one of Edinburgh's many tourist attractions. The museum is recognised as a collection of national significance by the Scottish Government.
The museum reopened in September 2015, after being closed for an eighteen-month period of redevelopment.
The Royal College of Surgeons of Edinburgh was incorporated in 1505, when it received its Seal of Cause or charter and became styled as 'The Incorporation of Surgeons and Barbers of Edinburgh'. The Museum at Surgeons Hall, Edinburgh dates from 1699 when the Incorporation announced that they were making a collection of ‘natural and artificial curiosities’. and advertised for these in the first edition of a local paper, the Edinburgh Gazette. Daniel Defoe, an early visitor in 1726, wrote in his Tour thro' the whole Island of Great Britain that the 'chamber of rarities' contained many curious things too numerous for him to describe. Much of this early collection was given to the University of Edinburgh in the 1760s.
By the early years of the 19th Century, the Incorporation had received a Royal Charter to become the Royal College of Surgeons of Edinburgh. The College saw its primary role as the teaching of anatomy and surgery, the training of surgeons, and examination of their acquired knowledge. Anatomy and pathology specimens were crucial to that function. The museum expanded dramatically with the acquisition of two large collections. John Barclay, a successful anatomy demonstrator in the extramural school of medicine donated his collection, while Sir Charles Bell, Professor of Surgery in the University of London and latterly in the University of Edinburgh sold his collection to the museum. These collections were much too large to be housed in the original 1697 Surgeons' Hall, and so the surgeons commissioned the leading Edinburgh architect William Playfair to build the present day Surgeons Hall, which opened in 1832. At first the entire upper floor of the building was devoted to the museum collections, which were open to the public and attracted large visitor numbers. Throughout the 19th and early 20th century the collection expanded as it became customary for surgeons and pathologists to donate not only specimens which they regarded as interesting or instructive, but surgical instruments and equipment. With the great scientific and technical advances of the time, the museum began to acquire anaesthetic equipment, histology slides, X-rays and photographs.
Edinburgh (/ˈɛdɪnbərə/; Scots: Edinburgh; Scottish Gaelic: Dùn Èideann [ˈt̪uːn ˈeːtʲən̪ˠ]) is the capital of Scotland and one of its 32 council areas. Historically part of the county of Midlothian (interchangeably Edinburghshire before 1921), it is located in Lothian on the Firth of Forth's southern shore.
Recognised as the capital of Scotland since at least the 15th century, Edinburgh is the seat of the Scottish Government, the Scottish Parliament and the supreme courts of Scotland. The city's Palace of Holyroodhouse is the official residence of the monarch in Scotland. The city has long been a centre of education, particularly in the fields of medicine, Scots law, literature, philosophy, the sciences and engineering. It is the second largest financial centre in the United Kingdom (after London) and the city's historical and cultural attractions have made it the United Kingdom's second most visited tourist destination attracting 4.9 million visits including 2.4 million from overseas in 2018.
Edinburgh is Scotland's second most populous city and the seventh most populous in the United Kingdom. The official population estimates are 488,050 (2016) for the Locality of Edinburgh (Edinburgh pre 1975 regionalisation plus Currie and Balerno), 518,500 (2018) for the City of Edinburgh, and 1,339,380 (2014) for the city region. Edinburgh lies at the heart of the Edinburgh and South East Scotland city region comprising East Lothian, Edinburgh, Fife, Midlothian, Scottish Borders and West Lothian.
The city is the annual venue of the General Assembly of the Church of Scotland. It is home to national institutions such as the National Museum of Scotland, the National Library of Scotland and the Scottish National Gallery. The University of Edinburgh, founded in 1582 and now one of four in the city, is placed 20th in the QS World University Rankings for 2020. The city is also known for the Edinburgh International Festival and the Fringe, the latter being the world's largest annual international arts festival. Historic sites in Edinburgh include Edinburgh Castle, the Palace of Holyroodhouse, the churches of St. Giles, Greyfriars and the Canongate, and the extensive Georgian New Town built in the 18th/19th centuries. Edinburgh's Old Town and New Town together are listed as a UNESCO World Heritage site, which has been managed by Edinburgh World Heritage since 1999." - info from Wikipedia.
Summer 2019 I did a solo cycling tour across Europe through 12 countries over the course of 3 months. I began my adventure in Edinburgh, Scotland and finished in Florence, Italy cycling 8,816 km. During my trip I took 47,000 photos.
Now on Instagram.
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Benjamin Sheares Bridge right
Opened in 1981, the Benjamin Sheares Bridge ( 薛尔思桥) is the longest bridge in Singapore, spanning 1.8 km, and the tallest, at 20m. It is named after Dr Benjamin Henry Sheares, the 2nd president of the Republic. The bridge was once part of the East Coast Parkway, but it is currently downgraded to an arterial road, Sheares Avenue. The cost of construction was S$177 million.
Built over reclaimed land by construction company Sato Kogyo, the bridge is made of pre-stressed concrete and links East Coast Parkway on the east coast to Marina Bay on the west coast.
Bayfront Bridge left
The Bayfront Bridge (海湾桥) is a vehicular bridge part of the Bayfront Avenue which links the Marina Bay Sands Integrated Resort to Raffles Avenue at the junction with Temasek Avenue, next to the Singapore Flyer.
Its simple design blends in with the existing Benjamin Sheares Bridge to form a backdrop to The Helix Bridge.
This new road will provide a direct connection between Temasek Avenue and Central Boulevard as well as Marina Boulevard. The opening of this new road network will provide road access to the upcoming developments in the Marina Bay area, such as the Marina Bay Sands Integrated Resort (MBSIR), Gardens by the Bay and the Marina Bay Financial Centre (MBFC).
Location: Singapore
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a wee bit of a trek to a lesser know location provides awesome reflections of El Capitan in the Merced River. Once again making our own paths through priistine snow. It seems like a sin to walk oin such untouched snow.
Monday will mark the first day of Spring. I can’t believe it’s here already! I figure I better share these photos of my winter adventure to Yosemite before they become completely irrelevant!
In Nature, I find peace and spiritual guidance…the forest is my temple…When you loose what you have you reinvent yourself!
A quiet portrait captured in a moment of deep reflection. The red hoodie, soft shadows, and cinematic tones draw the eye toward the subtle emotion in his profile. This image blends fine art portraiture with a moody, urban atmosphere, highlighting the intensity of youth, identity, and stillness. It is a study in colour, character, and contemplative expression, a simple moment that reveals something fragile, honest, and real. Perfect light, raw emotion, and a strong visual narrative bring this portrait to life.
Santa Maria in Campitelli or Santa Maria in Portico is a church dedicated to the Virgin Mary on the Piazza di Campitelli, Rome, Italy.
The church contains a 25 cm-high icon of the Virgin Mary dated by style and dendrochronology to the 11th century, though it had previously been claimed by tradition to have appeared miraculously in 524 at the table of Galla, a Roman woman who was helping the poor, and then carried in processions since 590. It was previously housed in the now-demolished Oratory of Santa Gala, sited at what is now the piazza's far end near the Porticus Octaviae (giving the church and icon its name of "Madonna of the Portico").
The icon was believed to have saved the city from plague in 1656 (or 1658), when it was carried in procession through the streets. On account of this, the earlier church on this site was replaced by Pope Alexander VII between 1659 and 1667 with the present one, designed by Carlo Rainaldi in the high Baroque style.
The present church has a travertine façade with large columns against (but not attached to) it, thus giving it strong vertical lines. The original design included statues which were however never executed.
Metro
Beijing, China
July 2012
Candid shots in and around Public Transport
Ricoh GRD IV
Please do not reproduce or use this picture without my explicit permission.
If you ask nicely I will probably say yes, just ask me first!
If you happen to be in one of my frames and have any objections to this.
Please contact me!
Please no glossy awards, scripted comments and big thumbnails back to your own work.
I will remove them...
In 'South Yorkshire Passenger Transport Executive' livery / markings, Class 114 DMU, No's E54004 and E53045 pass Edale on a possible Sheffield to Manchester train (could be New Mills as per destination screen). 9 November 1985. (037.003)
Copyright: Doug Birmingham (8A Rail)
In the American cities, the main church is located in the central square, but in the case of the San Gabriel village, it is located at a block of distance from the main plaza and reproducing what the Indian laws (Leyes de Indias) mentioned in the case of the main temple: "In Mediterranean places the temple is not build in the square, but somewhat distant from it, .... and that it can be seen of all parts and better venerated.
This is the only church in Ecuador that has been build that way.
Thanks for taking the time to comment, I really appreciate it and
will always try to reciprocate with a visit back to your stream.
© Henri Leduc - All of my images are protected by copyright
Some of my images are for sale via Getty Images and 500px
the technology that has been used to produce nuclear power has been atomic fission. in this process neutrons are used to bombard uranium atoms thus leading to the nucleus fission. it is such fission that generates the heat necessary to produce electric power in the same way as inside a conventional gas or coal-fired thermal power station. a side-effect of atomic fission is the release of radiation. to proceed well this process needs several parameters inside the nuclear reactor being balanced. when it is mismanaged it can get out of control generating huge radioactive leakages.
the alternative which has been studied to nuclear fission is nuclear fusion, a process through which two hydrogen atoms fuse. the advantage of this process, which reproduces what happens inside the sun, is that no radioactive emission occurs. the problem however is that typically atoms repulse each other. so to get them together there is the need of an extremely high amount of energy. for this reason hot fusion has also been called high energy fusion. currently several nations are building together ITER, a research facility aiming to develop this technology (see www.iter.org/). this big science has still a long way ahead before it gets to the commercial stage, if it will ever. the pay back for society would however be extremely high, as people across the planet would get access to a non-polluting and non-exhaurible source of energy.
over the last couple of years or so much has been written about another technology, so-called cold fusion or low-energy fusion. the same basic process of hot fusion happens here, but what induces it is not the energy imposed externally on the atoms to merge. several accounts of the process have been provided in scientific articles, but cold fusion remains outside mainstream physics as it can not be accounted for by current theories. cold fusion scientists have described several circumstances in which it has happened, but attempts to reproduce their experiments elsewhere have not been that successful. the tide seems however to be changing with organizations like NASA showing interest in cold fusion and investing in its research.
cold fusion has certainly been the most interesting scientific saga over recent years. if its proponents claims prove true, this could be the beginning of a new era. a live account of what's getting on, from the cold fusion scientists side, can be found here www.e-catworld.com/. as a former student of mine who is an expert on these issues pointed out a couple of weeks ago, cold fusion development has been a "real-world soap opera of innovation management, with patents claims, trade secrets, mad scientists, competition and a great deal of controversy peppered with conspiracy".
Mallards in Flight - a Photo Essay
Click on this link to access photo album: flic.kr/s/aHBqjzHLHH
In the depth of the winter months, mallard ducks can often be found in large numbers in and around water holes dotting the frozen waters of the Kingston Inner Harbour. Because it is the most common duck in the world, this water fowl is often ignored by photographers.
However, with their irradiant head (male) and blue wing patches, mallard ducks are colorful, accessible and approachable subjects that I use to sharpen my bird-in-flight photography skills. Falling or fallen snow make for ideal backgrounds to isolate and highlight the bird’s features which are particularly captivating during the landing process.
To get from Nice to London, I opted to fly on British Airways. A decade earlier, I was a BA Gold Card member. I booked this NCE-LHR without much enthusiasm, aware that the cheeseparing regime of former CEO Alex Cruz had imposed draconian cuts to the airline’s standards of comfort and service. The Economy Class seat-pitch had been tightened to an unacceptable 29 inches (Ryanair offers better) and food was strictly buy-on-board. So I forked out $672 for a 1-way Club Class ticket for a 31-inch seat pitch and free scoff. This was the food offering - OK, but nothing to excite the palate. The service was OK, but ditto: BA cabin staff can be friendly or totally aloof and even perfunctory. The flight was punctual and I had no issues with checked-in luggage. I give it a 7/10 rating, but I won’t rushing back to BA anytime soon.
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.