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Leidolf is, or rather was, the other camera maker from Wetzlar. The Lordomat C35 was developed from the Lordomat by addition of a non-coupled light meter. The meter has a selenium cell and therefore does not need batteries. Mine miraculously still works.
They did not manufacture their own lenses, but had them made by the Enna company in Munich. The Lordonar appears to be a Tessar.
I got mine from ebay. The seller had it from a house clearance. There still is a film inside. I don't know how long it's been there, but I will shoot it to the end of the roll and then have it developed. If it's dud, too bad. The camera was sold as "defective", because the seller didn't know anything about cameras and probably didn't know how to make it go click.
Before receiving it I thought it was about in the same class as the Braun Paxette, but now that I have it and can see and feel the build quality, I rank it significantly higher. About on the same level as a Contaflex III. Not yet in the realm of Leica and Contax.
Technically, it lags somewhat behind the Leica M3 and it has some design quirks. It has a double stroke film advance that, unusually, rotates clockwise, it does not have a self-timer nor does it have a frame in the viewfinder for 50 mm focal length The entire frame corresponds to the FOV of 35 mm focal length and there are added frames for 90 and 135 mm, but you have to guess the frame for 50 mm. That is a bit inconvenient.
There is a second peephole for the ranging, so you have to peer through that while focusing and then switch to the viewfinder window for composing. That is akin to the Leica II and III, though here the two peepholes are not directly next to each other.
There is a manual parallax correction, You focus, read off the range and then set a dial in front of the viewfinder. That means you will have to be moving the camera away from your face and back again to your eye several times. It's not a camera for fast action.
The camera has a leaf shutter with settings between 1 and 300, plus B. There is the usual M-X-V flash synchronisation.
The shutter release button is on the side of the lens mount, Probably the seller didn't find it there and instead pressed on some of the dials on the top deck which didn't lead to anything.
Mine is in very good shape. No dings, bumps or scratches except for a slightly bent filter ring on the lens. The case also looks good. Clearly, the previous owner took good care of it.
Shot with:
Canon EOS600D
Leica Bellows R (16860)
Leica 100mm f/4 Macro Elmar-R, bellows version (11230)
A new addition for Nicolsons of Cunningsburgh is this ex Bus Na Comahairle (Western Isles Council) of Stornoway Mercedes 0813D Plaxton Beaver 3. Seen here at Cunningsburgh yesterday evening in the poor light due to the fog which doesn't make for great quality shots
In addition to the magnificent architecture, the mosaics in San Vitale are the main attractions. These are considered the largest and best-preserved Byzantine mosaics outside modern-day Istanbul.
Original mosaics from late antiquity still cover the whole apsis and altar area. The intrados of the triumphal arch features fifteen figures, including Christ and the twelve apostles.
The Basilica of San Vitale is a highlight of any visit to see the Byzantine wall mosaics in Ravenna, a town popular with day trippers from Venice and Bologna. San Vitale in Ravenna has the largest Byzantine mosaics outside Istanbul and is the best example of Justinian church architecture in existence.
Ravenna in Italy is famous for its Late Antiquity and Byzantine wall and ceiling mosaics in early Christian monuments and churches, which are the top UNESCO World Cultural Heritage-listed sites to see when visiting this interesting town.
This is a Class B industrial type building located in downtown West Palm Beach. The Property Size is 190,727 Sqft on a 1 Acre lot. This building is used as a phone switching center.
This structure was originally built as a 6-story building. A 3-story addition and microwave enclosure were added in 1974. The building went under the names of Southern Bell Dial & Toll Building before it became known as the AT&T Building.
Credit for the data above is given to the following websites:
www.emporis.com/buildings/130862/at-t-building-west-palm-...
www.commercialcafe.com/commercial-property/us/fl/west-pal...
© All Rights Reserved - you may not use this image in any form without my prior permission.
We have had a cold front roll through here in Florida and have had morning temps in the mid to low 30s. The Eagles have been adding additional nest material to keep the Eaglet/Eaglets warmer. We had a perfect shooting alley into the nest to photograph the young, but that has been blocked off to keep the wind out of the nest. Will post photos when I see another head.
5 November is Bonfire night in England.
Here, now, it is like living in a war-zone...
I looked at flowers I had photographed and that reminded me of natural fireworks= flowerworks? Lol.
This was after some more manipulation and another addition...how this image was 'made' click here
Thank you for your time, so very much appreciated! Magda, (*_*)
For more of my other work visit here: www.indigo2photography.co.uk
IT IS STRICTLY FORBIDDEN (BY LAW!!!) TO USE ANY OF MY image or TEXT on websites, blogs or any other media without my explicit permission. © All rights reserved
Laura.
The land around the small town of Laura was originally part of Booyoolee sheep station based in Gladstone which was leased by Herbert Bristow Hughes and Bristow Herbert Hughes from 1843. They soon had a run of 200 square miles and the partnership split with Herbert Hughes retaining Booyoolee and Bristow Hughes developing Bundaleer sheep run from 1846. After the passing of the credit selection land acts of 1869 and 1872 large areas of Booyoolee station were resumed by the government for closer settlement and the arrival of grain farmers rather than pastoralists. But a clerical error in the Lands Office in 1871 meant the Hundred of Booyoolie was declared rather than the Hundred of Booyoolee. Herbert Bristow Hughes married Laura White of Wirrabara run and so the governor of SA named the new township Laura after Herbert Hughes’ wife. The first town lots were offered for sale in 1872 with the first school, the Wesleyan Church, the former Laura Hotel (now a shop) and the brewery all opening in 1873. Of these buildings the Laura Hotel was the first stone building erected in the town. It closed in 1998. Based beside the Rocky River in well-watered country the town grew rapidly. A local land owner Mr H Walter had a private town named North Laura subdivided but it was soon amalgamated into the government town of Laura. However just to the north of North Laura the land was purchased from the original land owner by the state government in 1893 at considerable cost to create a number of Working Men’s Blocks as part of the Cotton government scheme to assist working men to live on small blocks of around 10 acres. This area just north of the town is still known as Laura Blocks and the properties are all around 10 to 20 acres. In the 1890s at a time of great depression the blocks allowed working men to lease the land cheaply from the government in order to grow vegetables, plant fruit trees, keep a cow and a pig, perhaps some bees and poultry to supplement their waged incomes. The land was eventually offered for sale to the blockers or to other settlers.
Like all agricultural areas the grain farmers wanted access to good transport. The first wheat crops were carted by bullock teams or horses and drays through Hughes Gap near Crystal Brook down to the port at Port Pirie. But this need was redundant once the train line was extended from Gladstone to Laura in 1884. A fine stone gable ended railway station was built in Laura shortly after 1884 but alas it has now been demolished and the rail tracks torn up. But Laura did not remain a rail terminus. The rail lines were extended to Booleroo Centre in 1910 and then on to Melrose and Wilmington in 1919. Some of the finest buildings in the town are the Old Court House (now the art gallery) which was built in 1877, the old post office first built around 1874 and the former Police Station in the Main Street built in in 1878 and closed in 1968. The old Institute was built in 1875 but later demolished to make way for an ugly Civic Centre in 1968. In front of that Civic Centre is a bust of Clarence J. Dennis whilst there is a larger than life statue of him in the Main Street. C. J Dennis the famous poet and story writer was born in Auburn in 1876 but lived for most of his childhood and youth years in Laura before he eventually moved to Melbourne. In 1890 C.J. Dennis began work at the solicitor’s office in the Main Street as a junior law clerk. Dennis left Laura in 1898 when he fell out with his father the publican of one of the Laura Hotels. Between the Civic Centre and the old Courthouse is the fine Masonic Lodge which was built in 1908 but is now used by the local history society as an archive. The Masonic Lodge was formed in Laura in 1878. Other buildings of note are the classical style single room fronted Solicitors Offices in the Main Street near Bristow Street where C.J Dennis was employed and the former Bank of South Australia on the corner of White Street. The main chamber on the Main Street was built late in 1922 but walk down White Street and you can see the old bank with half rounded windows behind it. That part of the bank was built in 1878. It is opposite the former Laura hotel which is now the soap shop.
After erecting the first hotels and churches country towns looked to education facilities. In Laura a school opened in 1874 in a small church before the first state school was built in 1877. Additional classrooms were added to the 1877 building in 1883. More buildings have opened since the 1950s. In the 1870s churches were often built of pine and pug with thatched rooves and they were demolished within a couple of decades. The Wesleyan Methodists built the first church in Laura in 1873 opposite the location of the current school. They replaced this structure with their grand stone church in the Main Street in 1888. It is still in use in the Main Street but it is now Redeemer Lutheran Church. The Lutherans purchased this building in the year 2000. The Lutherans also purchased the Primitive Methodist Church in Samuel Street in Laura which was built in 1876. They bought it in 1904, demolished it in 1908 and opened their Easter Lutheran Church on the site in 1909. The Baptist congregation in Laura was strong and they built their church in 1875 and it is still in use by the Baptists. The Catholics built an early church in 1877 with a nearby convent at the same time on land on the outskirts of Laura which was donated by a local farmer Mr Rollison. Both were demolished in 1929 to make way for the current fine Catholic Church. The Anglicans built a church in Laura in 1875 and because Herbert Bristow Hughes of Booyoolee and his family worshiped there he donated funds for the addition of the chancel. The chancel was built in 1883 to the design of Adelaide architect Daniel Garlick.
The town had an important flour mill from 1874 which burnt down in 1878 and was then immediately re-built. The mill machinery was manufactured in the May Brothers foundry at Gawler. New machinery was added to the mill in 1893 and it was eventually taken over by the Laura Milling Company in 1915. Extensive improvements such as roller mills were installed and the mill for many years produced and marketed the BEST Laura flour which was known across SA and in Broken Hill. To supplement revenue a chaff mill was also operated in conjunction with the flourmill. The flourmill finally closed in the 1970s and much of it was destroyed in a 2015 arson attack. A butter factory also opened in Laura in 1891 and operated for some years as butter could by then be refrigerated and shipped to England but a lot of it was railed to the growing silver city of Broken Hill. The local area dairy cooperative was established in 1891 to ensure a reliable local milk supply for the factory. During the big droughts around 1900 milk production declined and the factory became a chaff factory. The old milk factory operated as a chaff mill until 1924. But milk processing in Laura did not cease entirely as in 1923 Laura became the home of Golden North. In that year the Laura Ice Company was formed, primarily to supply the local and the Broken Hill trade and the regional city of Port Pirie with ice, milk and ice cream. From 1938 milk was pasteurised at the factory. The brand name Golden North was adopted in 1948. In 1961 the head office was moved from Laura to Clare and the company was taken over by Farmers Union in 1972 which was in turn taken over by National Foods in 1991. Then in 2001 a group of local investors bought the business back from the large companies and they have since expanded production, including the famous Golden North honey ice cream. You can buy Golden North ice cream from the shops in the main street. The company was awarded a state heritage icon award in 2006 and it is a major employer in the town. The old Laura Brewery operated from 1873 until it was purchased by the South Australian Brewing Company in 1893. They promptly closed it down in 1894 as they centralised all their operations in Adelaide by buying and closing country breweries. During World War Two Laura was declared one of four major flax growing areas and it had a flax mill. Ninety two farmers cultivated flax near Laura and almost two thousand acres were sown to flax during the period of the War time shortages. The flax was stored in the old Showgrounds stone Pavilion to the east of the town before it was milled. The flax mill closed in 1947 after opening in 1942. Like many agricultural towns Laura has several blacksmiths and agricultural implement makers such as Silby and Craig, Adamson Brothers and the foundry of Thomas Forsaith which later became Keipert foundry. Laura was also one of the few towns that had its own newspaper the Laura Standard. The Laura Standard was founded in 1888 and their building still remains named in the Main Street. C.J. Dennis had his first verses published in the newspaper in 1895. The Laura Standard was taken over by the Jamestown newspaper in 1942 and disappeared as an independent publication. It became part of the Northern Review newspaper.
Day 92- In addition to the cake smashed in my face two days ago, were these glorious wonders of sugary deliciousness.
Oh yes, I do love a delicious cupcake baked into a flat-bottomed ice cream cone. YUM!!!
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10 things people may not know about me and my birthday.
1) I LOVE BIRTHDAYS!!!!
2) I prefer to celebrate for a week. Why have a single day when you can have a week, right?
3) I'm not a fan of belated celebrations though. I want to celebrate before or on the day because afterward seems like an afterthought and it kind of bums me out to be honest.
Then again, I won't walk away from a party or a present because it's late. I'm picky, not stupid.
4) BTW, I love everything that comes along with birthday celebrations. Bring on the cake, balloons, flowers, presents, cards...you name it. I say, "Rock on with the treats!" :)
5) Yes, my favorite number is 5. Duh?
6) I don't count numbers other than that one. I find a lot of people are deeply ageist and I won't feed into anyone's prejudice. I AM AS OLD AS I FEEL.
7) Seriously, don't ask. It's not really all that relavent. Besides, it's rude to ask someone their age. That's what I was taught by my grandparents when I was a small child and I agree with them completely.
8) Speaking of being a child, I always associate my birthday with Easter because they were often celebrated together with my family. As a result, I have a fondness for bunnies and all things trinket-like.
9) Best birthday presents have always been vacations. I've gone to Europe, Mexico and across the USA as part of three different birthday presents.
10) Any birthday you can celebrate where you are healthy and happy is a good birthday.
The Muses have definitely taken over at my house..............I bought very few dolls from other lines this year, as my focus has definitely shifted to the Muses.
The Ribblehead Viaduct or Batty Moss Viaduct carries the Settle–Carlisle railway across Batty Moss in the Ribble Valley at Ribblehead, in North Yorkshire, England. The viaduct, built by the Midland Railway, is 28 miles (45 km) north-west of Skipton and 26 miles (42 km) south-east of Kendal. It is a Grade II* listed structure. Ribblehead Viaduct is the longest and the third tallest structure on the Settle–Carlisle line.
The viaduct was designed by John Sydney Crossley, chief engineer of the Midland Railway, who was responsible for the design and construction of all major structures along the line. The viaduct was necessitated by the challenging terrain of the route. Construction began in late 1869. It necessitated a large workforce, up to 2,300 men, most of whom lived in shanty towns set up near its base. Over 100 men lost their lives during its construction. The Settle to Carlisle line was the last main railway in Britain to be constructed primarily with manual labour.
By the end of 1874, the last stone of the structure had been laid; on 1 May 1876, the Settle–Carlisle line was opened for passenger services. During the 1980s, British Rail proposed closing the line. In 1989, after lobbying by the public against closure, it was announced that the line would be retained. Since the 1980s, the viaduct has had multiple repairs and restorations and the lines relaid as a single track. The land underneath and around the viaduct is a scheduled ancient monument; the remains of the construction camp and navvy settlements (Batty Wife Hole, Sebastopol, and Belgravia) are located there.
In the 1860s, the Midland Railway, keen to capitalise on the growth in rail traffic between England and Scotland, proposed building a line between Settle and Carlisle. The line was intended to join the Midland line between Skipton and Carnforth to the city of Carlisle. On 16 July 1866, the Midland Railway (Settle to Carlisle) Act was passed by Parliament, authorising the company "to construct Railways from Settle to Hawes, Appleby, and Carlisle; and for other Purposes".
After the Act passed, the Midland Railway came to an agreement with the London & North Western Railway, to run services on the LNWR line via Shap. The company applied for a bill of abandonment for its original plan but Parliament rejected the bill on 16 April 1869 and the Midland Railway was compelled to build the Settle to Carlisle line.
The line passed through difficult terrain that necessitated building several substantial structures. The company's chief engineer, John Sydney Crossley and its general manager, James Joseph Allport, surveyed the line. Crossley was responsible for the design and construction of the major works, including Ribblehead Viaduct.
On 6 November 1869, a contract to construct the Settle Junction (SD813606) to Dent Head Viaduct section including Ribblehead Viaduct was awarded to contractor John Ashwell. The estimated cost was £343,318 and completion was expected by May 1873. Work commenced at the southern end of the 72-mile (116 km) line.
By July 1870, work had started on the foundations for Ribblehead Viaduct. On 12 October 1870, contractor's agent William Henry Ashwell laid the first stone. Financial difficulties came to greatly trouble John Ashwell; on 26 October 1871, his contract was cancelled by mutual agreement. From this date, the viaduct was constructed by the Midland Railway who worked on a semi-contractual basis overseen by William Ashwell.
The viaduct was built by a workforce of up to 2,300 men. They lived, often with their families, in temporary camps, named Batty Wife Hole, Sebastopol, and Belgravia on adjacent land. More than a hundred workers lost their lives in construction-related accidents, fighting, or from outbreaks of smallpox. According to Church of England records, there are around 200 burials of men, women, and children in the graveyard at Chapel-le-Dale and the church has a memorial to the railway workers.
In December 1872, the design for Ribblehead Viaduct was changed from 18 arches to 24, each spanning 45 feet (13.7 m). By August 1874, the arches had been keyed and the last stone was laid by the end of the year. A single track was laid over the viaduct and on 6 September 1874 the first train carrying passengers was hauled across by the locomotive Diamond. On 3 August 1875, the viaduct was opened for freight traffic and on 1 May 1876, the whole line opened for passenger services, following approval by Colonel F. H. Rich from the Board of Trade.
Ribblehead Viaduct is 440 yards (400 m) long, and 104 feet (32 m) above the valley floor at its highest point, it was designed to carry a pair of tracks aligned over the sleeper walls. The viaduct has 24 arches of 45 feet (14 m) span, the foundations of which are 25 feet (7.6 m) deep. The piers are tapered, roughly 13 feet (4 m) across at the base and 5 feet 11 inches (1.8 m) thick near the arches and have loosely-packed rubble-filled cores. Every sixth pier is 50 per cent thicker, a mitigating measure against collapse should any of the piers fail. The north end is 13 feet (4 m) higher in elevation than the south, a gradient of 1:100.
The viaduct is faced with limestone masonry set in hydraulic lime mortar and the near-semicircular arches are red brick, constructed in five separate rings, with stone voussoirs. Sleeper walls rise from the arches to support the stone slabs of the viaduct's deck and hollow spandrels support plain solid parapet walls. In total, 1.5 million bricks were used; some of the limestone blocks weigh eight tons.
Ribblehead Viaduct is 980 feet (300 m) above sea level on moorland exposed to the prevailing westerly wind. Its height, from foundation to rails is 55 yards (50.3 m). It is 442.7 yards (404.8 m) long on a lateral curve with a radius of 0.85 miles (1.37 km).
The viaduct is the longest structure on the Settle–Carlisle Railway which has two taller viaducts, Smardale Viaduct at 131 feet (40 m) near Crosby Garrett, and Arten Gill at 117 feet (36 m). Ribblehead railway station is less than half a mile to the south and to the north is Blea Moor Tunnel, the longest on the line, near the foot of Whernside.
During 1964, several Humber cars were blown off their wagons while being carried over the viaduct on a freight train.
By 1980, the viaduct was in disrepair and many of its piers had been weakened by water ingress. Between 1981 and 1984, repairs were undertaken as a cost of roughly £100,000. Repairs included strengthening the piers by the addition of steel rails and concrete cladding. For safety reasons, the line was reduced to single track across the viaduct to avoid the simultaneous loading from two trains crossing and a 20mph speed limit was imposed. During 1988, minor repairs were carried out and trial bores were made into several piers. In 1989, a waterproof membrane was installed.
In the 1980s, British Rail proposed closing the line, citing the high cost of repairs to its major structures. Vigorous campaigning by the Friends of the Settle-Carlisle Line, formed during 1981, garnered and mobilised public support against the plan. In 1989, the line was saved from closure. According to Michael Portillo, who took the decision in his capacity as Minister of State for Transport, the economic arguments for closing it had been weakened by a spike in passenger numbers, and further studies by engineers had determined that restoration work would not be nearly as costly as estimated.
In November 1988, Ribblehead Viaduct was Grade II* listed. The surrounding land where the remains of its construction camps are located has been recognised as a scheduled monument.
Between 1990 and 1992, Ribblehead Viaduct underwent major restoration. Between September 1999 and March 2001, a programme of improvements was implemented involving renewal of track, replacement of ballast and the installation of new drainage. Restoration has allowed for increased levels of freight traffic assuring the line's viability.
The Settle–Carlisle Line is one of three north–south main lines, along with the West Coast Main Line through Penrith and the East Coast Main Line via Newcastle. During 2016, the line carried seven passenger trains from Leeds to Carlisle per day in each direction, and long-distance excursions, many hauled by preserved steam locomotives.
Regular heavy freight trains use the route avoiding congestion on the West Coast Main Line. Timber trains, and stone from Ingleton quarry, pass over the viaduct when they depart from the yard opposite Ribblehead railway station. The stone from Ingleton is ferried to the terminal at Ribblehead by road. Limestone aggregate trains from Arcow quarry sidings (near Horton-in-Ribblesdale) run to various stone terminals in the Leeds and Manchester areas on different days – these trains reverse in the goods loop at Blea Moor signal box because the connection from the quarry sidings faces north.
Major restoration work started in November 2020 as a £2.1 million project to re-point mortar joints and replace broken stones got underway. Network Rail released a timelapse video of the works in June 2021.
Building the viaduct was the inspiration behind the ITV period drama series Jericho. The viaduct appears in the 1970 film No Blade of Grass and also in the 2012 film Sightseers. A number of other films and television programmes have also included the viaduct.
North Yorkshire is a ceremonial county in the Yorkshire and the Humber and North East regions of England. It borders County Durham to the north, the North Sea to the east, the East Riding of Yorkshire to the south-east, South Yorkshire to the south, West Yorkshire to the south-west, and Cumbria and Lancashire to the west. Northallerton is the county town.
The county is the largest in England by land area, at 9,020 km2 (3,480 sq mi), and has a population of 1,158,816. The largest settlements are Middlesbrough (174,700) in the north-east and the city of York (152,841) in the south. Middlesbrough is part of the Teesside built-up area, which extends into County Durham and has a total population of 376,663. The remainder of the county is rural, and the largest towns are Harrogate (73,576) and Scarborough (61,749). For local government purposes the county comprises four unitary authority areas — York, Middlesbrough, Redcar and Cleveland, and North Yorkshire — and part of a fifth, Stockton-on-Tees.
The centre of the county contains a wide plain, called the Vale of Mowbray in the north and Vale of York in the south. The North York Moors lie to the east, and south of them the Vale of Pickering is separated from the main plain by the Howardian Hills. The west of the county contains the Yorkshire Dales, an extensive upland area which contains the source of the River Ouse/Ure and many of its tributaries, which together drain most of the county. The Dales also contain the county's highest point, Whernside, at 2,415 feet (736 m).
North Yorkshire non-metropolitan and ceremonial county was formed on 1 April 1974 as a result of the Local Government Act 1972. It covered most of the North Riding of Yorkshire, as well as northern parts of the West Riding of Yorkshire, northern and eastern East Riding of Yorkshire and the former county borough of York. Northallerton, as the former county town for the North Riding, became North Yorkshire's county town. In 1993 the county was placed wholly within the Yorkshire and the Humber region.
Some areas which were part of the former North Riding were in the county of Cleveland for twenty-two years (from 1974 to 1996) and were placed in the North East region from 1993. On 1 April 1996, these areas (Middlesbrough, Redcar and Cleveland and Stockton borough south of the River Tees) became part of the ceremonial county as separate unitary authorities. These areas remain within the North East England region.
Also on 1 April 1996, the City of York non-metropolitan district and parts of the non-metropolitan county (Haxby and nearby rural areas) became the City of York unitary authority.
On 1 April 2023, the non-metropolitan county became a unitary authority. This abolished eight councils and extended the powers of the county council to act as a district council.
The York and North Yorkshire Combined Authority held its first meeting on 22 January 2024, assumed its powers on 1 February 2024 and the first mayor is to be elected in May 2024.
The geology of North Yorkshire is closely reflected in its landscape. Within the county are the North York Moors and most of the Yorkshire Dales, two of eleven areas in England and Wales to be designated national parks. Between the North York Moors in the east and the Pennine Hills. The highest point is Whernside, on the Cumbrian border, at 2,415 feet (736 m). A distinctive hill to the far north east of the county is Roseberry Topping.
North Yorkshire contains several major rivers. The River Tees is the most northerly, forming part of the border between North Yorkshire and County Durham in its lower reaches and flowing east through Teesdale before reaching the North Sea near Redcar. The Yorkshire Dales are the source of many of the county's major rivers, including the Aire, Lune, Ribble, Swale, Ure, and Wharfe.[10] The Aire, Swale, and Wharfe are tributaries of the Ure/Ouse, which at 208 km (129 mi) long is the sixth-longest river in the United Kingdom. The river is called the Ure until it meets Ouse Gill beck just below the village of Great Ouseburn, where it becomes the Ouse and flows south before exiting the county near Goole and entering the Humber estuary. The North York Moors are the catchment for a number of rivers: the Leven which flows north into the Tees between Yarm and Ingleby Barwick; the Esk flows east directly into the North Sea at Whitby as well as the Rye (which later becomes the Derwent at Malton) flows south into the River Ouse at Goole.
North Yorkshire contains a small section of green belt in the south of the county, which surrounds the neighbouring metropolitan area of Leeds along the North and West Yorkshire borders. It extends to the east to cover small communities such as Huby, Kirkby Overblow, and Follifoot before covering the gap between the towns of Harrogate and Knaresborough, helping to keep those towns separate.
The belt adjoins the southernmost part of the Yorkshire Dales National Park, and the Nidderdale AONB. It extends into the western area of Selby district, reaching as far as Tadcaster and Balne. The belt was first drawn up from the 1950s.
The city of York has an independent surrounding belt area affording protections to several outlying settlements such as Haxby and Dunnington, and it too extends into the surrounding districts.
North Yorkshire has a temperate oceanic climate, like most of the UK. There are large climate variations within the county. The upper Pennines border on a Subarctic climate. The Vale of Mowbray has an almost Semi-arid climate. Overall, with the county being situated in the east, it receives below-average rainfall for the UK. Inside North Yorkshire, the upper Dales of the Pennines are one of the wettest parts of England, where in contrast the driest parts of the Vale of Mowbray are some of the driest areas in the UK.
Summer temperatures are above average, at 22 °C. Highs can regularly reach up to 28 °C, with over 30 °C reached in heat waves. Winter temperatures are below average, with average lows of 1 °C. Snow and Fog can be expected depending on location. The North York Moors and Pennines have snow lying for an average of between 45 and 75 days per year. Sunshine is most plentiful on the coast, receiving an average of 1,650 hours a year. It reduces further west in the county, with the Pennines receiving 1,250 hours a year.
The county borders multiple counties and districts:
County Durham's County Durham, Darlington, Stockton (north Tees) and Hartlepool;
East Riding of Yorkshire's East Riding of Yorkshire;
South Yorkshire's City of Doncaster;
West Yorkshire's City of Wakefield, City of Leeds and City of Bradford;
Lancashire's City of Lancaster, Ribble Valley and Pendle
Cumbria's Westmorland and Furness.
The City of York Council and North Yorkshire Council formed the York and North Yorkshire Combined Authority in February 2024. The elections for the first directly-elected mayor will take place in May 2024. Both North Yorkshire Council and the combined authority are governed from County Hall, Northallerton.
The Tees Valley Combined Authority was formed in 2016 by five unitary authorities; Middlesbrough, Redcar and Cleveland Borough both of North Yorkshire, Stockton-on-Tees Borough (Uniquely for England, split between North Yorkshire and County Durham), Hartlepool Borough and Darlington Borough of County Durham.
In large areas of North Yorkshire, agriculture is the primary source of employment. Approximately 85% of the county is considered to be "rural or super sparse".
Other sectors in 2019 included some manufacturing, the provision of accommodation and meals (primarily for tourists) which accounted for 19 per cent of all jobs. Food manufacturing employed 11 per cent of workers. A few people are involved in forestry and fishing in 2019. The average weekly earnings in 2018 were £531. Some 15% of workers declared themselves as self-employed. One report in late 2020 stated that "North Yorkshire has a relatively healthy and diverse economy which largely mirrors the national picture in terms of productivity and jobs.
Mineral extraction and power generation are also sectors of the economy, as is high technology.
Tourism is a significant contributor to the economy. A study of visitors between 2013 and 2015 indicated that the Borough of Scarborough, including Filey, Whitby and parts of the North York Moors National Park, received 1.4m trips per year on average. A 2016 report by the National Park, states the park area gets 7.93 million visitors annually, generating £647 million and supporting 10,900 full-time equivalent jobs.
The Yorkshire Dales have also attracted many visitors. In 2016, there were 3.8 million visits to the National Park including 0.48 million who stayed at least one night. The parks service estimates that this contributed £252 million to the economy and provided 3,583 full-time equivalent jobs. The wider Yorkshire Dales area received 9.7 million visitors who contributed £644 million to the economy. The North York Moors and Yorkshire Dales are among England's best known destinations.
York is a popular tourist destination. A 2014 report, based on 2012 data, stated that York alone receives 6.9 million visitors annually; they contribute £564 million to the economy and support over 19,000 jobs. In the 2017 Condé Nast Traveller survey of readers, York rated 12th among The 15 Best Cities in the UK for visitors. In a 2020 Condé Nast Traveller report, York rated as the sixth best among ten "urban destinations [in the UK] that scored the highest marks when it comes to ... nightlife, restaurants and friendliness".
During February 2020 to January 2021, the average property in North Yorkshire county sold for £240,000, up by £8100 over the previous 12 months. By comparison, the average for England and Wales was £314,000. In certain communities of North Yorkshire, however, house prices were higher than average for the county, as of early 2021: Harrogate (average value: £376,195), Knaresborough (£375,625), Tadcaster (£314,278), Leyburn (£309,165) and Ripon (£299,998), for example.
This is a chart of trend of regional gross value added for North Yorkshire at current basic prices with figures in millions of British pounds sterling.
Unemployment in the county was traditionally low in recent years, but the lockdowns and travel restrictions necessitated by the COVID-19 pandemic had a negative effect on the economy during much of 2020 and into 2021. The UK government said in early February 2021 that it was planning "unprecedented levels of support to help businesses [in the UK] survive the crisis". A report published on 1 March 2021 stated that the unemployment rate in North Yorkshire had "risen to the highest level in nearly 5 years – with under 25s often bearing the worst of job losses".
York experienced high unemployment during lockdown periods. One analysis (by the York and North Yorkshire Local Enterprise Partnership) predicted in August 2020 that "as many as 13,835 jobs in York will be lost in the scenario considered most likely, taking the city's unemployment rate to 14.5%". Some critics claimed that part of the problem was caused by "over-reliance on the booming tourism industry at the expense of a long-term economic plan". A report in mid June 2020 stated that unemployment had risen 114 per cent over the previous year because of restrictions imposed as a result of the pandemic.
Tourism in the county was expected to increase after the restrictions imposed due the pandemic are relaxed. One reason for the expected increase is the airing of All Creatures Great and Small, a TV series about the vet James Herriot, based on a successful series of books; it was largely filmed within the Yorkshire Dales National Park. The show aired in the UK in September 2020 and in the US in early 2021. One source stated that visits to Yorkshire websites had increased significantly by late September 2020.
The East Coast Main Line (ECML) bisects the county stopping at Northallerton,Thirsk and York. Passenger service companies in the area are London North Eastern Railway, Northern Rail, TransPennine Express and Grand Central.
LNER and Grand Central operate services to the capital on the ECML, Leeds Branch Line and the Northallerton–Eaglescliffe Line. LNER stop at York, Northallerton and on to County Durham or spur over to the Tees Valley Line for Thornaby and Middlesbrough. The operator also branch before the county for Leeds and run to Harrogate and Skipton. Grand Central stop at York, Thirsk Northallerton and Eaglescliffe then over to the Durham Coast Line in County Durham.
Northern operates the remaining lines in the county, including commuter services on the Harrogate Line, Airedale Line and York & Selby Lines, of which the former two are covered by the Metro ticketing area. Remaining branch lines operated by Northern include the Yorkshire Coast Line from Scarborough to Hull, York–Scarborough line via Malton, the Hull to York Line via Selby, the Tees Valley Line from Darlington to Saltburn via Middlesbrough and the Esk Valley Line from Middlesbrough to Whitby. Last but certainly not least, the Settle-Carlisle Line runs through the west of the county, with services again operated by Northern.
The county suffered badly under the Beeching cuts of the 1960s. Places such as Richmond, Ripon, Tadcaster, Helmsley, Pickering and the Wensleydale communities lost their passenger services. Notable lines closed were the Scarborough and Whitby Railway, Malton and Driffield Railway and the secondary main line between Northallerton and Harrogate via Ripon.
Heritage railways within North Yorkshire include: the North Yorkshire Moors Railway, between Pickering and Grosmont, which opened in 1973; the Derwent Valley Light Railway near York; and the Embsay and Bolton Abbey Steam Railway. The Wensleydale Railway, which started operating in 2003, runs services between Leeming Bar and Redmire along a former freight-only line. The medium-term aim is to operate into Northallerton station on the ECML, once an agreement can be reached with Network Rail. In the longer term, the aim is to reinstate the full line west via Hawes to Garsdale on the Settle-Carlisle line.
York railway station is the largest station in the county, with 11 platforms and is a major tourist attraction in its own right. The station is immediately adjacent to the National Railway Museum.
The main road through the county is the north–south A1(M), which has gradually been upgraded in sections to motorway status since the early 1990s. The only other motorways within the county are the short A66(M) near Darlington and a small stretch of the M62 motorway close to Eggborough. The other nationally maintained trunk routes are the A168/A19, A64, A66 and A174.
Long-distance coach services are operated by National Express and Megabus. Local bus service operators include Arriva Yorkshire, Stagecoach, Harrogate Bus Company, The Keighley Bus Company, Scarborough & District (East Yorkshire), Yorkshire Coastliner, First York and the local Dales & District.
There are no major airports in the county itself, but nearby airports include Teesside International (Darlington), Newcastle and Leeds Bradford.
The main campus of Teesside University is in Middlesbrough, while York contains the main campuses of the University of York and York St John University. There are also two secondary campuses in the county: CU Scarborough, a campus of Coventry University, and Queen's Campus, Durham University in Thornaby-on-Tees.
Colleges
Middlesbrough College's sixth-form
Askham Bryan College of agriculture, Askham Bryan and Middlesbrough
Craven College, Skipton
Middlesbrough College
The Northern School of Art, Middlesbrough
Prior Pursglove College
Redcar & Cleveland College
Scarborough Sixth Form College
Scarborough TEC
Selby College
Stockton Riverside College, Thornaby
York College
Places of interest
Ampleforth College
Beningbrough Hall –
Black Sheep Brewery
Bolton Castle –
Brimham Rocks –
Castle Howard and the Howardian Hills –
Catterick Garrison
Cleveland Hills
Drax Power Station
Duncombe Park – stately home
Eden Camp Museum –
Embsay & Bolton Abbey Steam Railway –
Eston Nab
Flamingo Land Theme Park and Zoo –
Helmsley Castle –
Ingleborough Cave – show cave
John Smith's Brewery
Jorvik Viking Centre –
Lightwater Valley –
Lund's Tower
Malham Cove
Middleham Castle –
Mother Shipton's Cave –
National Railway Museum –
North Yorkshire Moors Railway –
Ormesby Hall – Palladian Mansion
Richmond Castle –
Ripley Castle – Stately home and historic village
Riverside Stadium
Samuel Smith's Brewery
Shandy Hall – stately home
Skipton Castle –
Stanwick Iron Age Fortifications –
Studley Royal Park –
Stump Cross Caverns – show cave
Tees Transporter Bridge
Theakston Brewery
Thornborough Henges
Wainman's Pinnacle
Wharram Percy
York Castle Museum –
Yorkshire Air Museum –
The Yorkshire Arboretum
The San Juan fiestas are the main festivities of Tolosa and take place around June 24th.
Following old traditions, the festivities of San Juan have kept up the Bordon-dantza (dance with military origins) and the jump over the fire, and they have strengthened and updated the parade of arms (riflemen).
The Bordon-dantza, the dance that has its origins in the Battle of Beotibar between Navarre and Gipuzkoa, offers the public a unique spectacle. In addition to this dance, the Zortziko of San Juan and the Aurresku are also performed.
The parade of arms, which initially only involved 20 riflemen, now has 14 crews, of between 40 and 60 riflemen and riflewomen, each equipped with bright clothing, drums and Txistus (type of fipple flute). In the morning, they fire salvoes in Plaza Vieja, Plaza Santa María and Plaza Triangulo, among others. In the afternoon, the riflemen and riflewomen parade towards the Basilica of San Juan de Arramele, which is the main church, and Plaza Triangulo, together with the municipal plenary and male and female dancers of the Bordon-dantza.
Las fiestas de San Juan en Tolosa, celebradas en torno al 24 de junio, son sus fiestas patronales principales, destacando por tradiciones como la Bordon-dantza (danza de la Batalla de Beotibar), el salto sobre la hoguera y el multitudinario Alarde de Armas con escopeteros. Es una celebración vibrante con música, verbenas y actividades tradicionales.
In addition to our refrigerator conking out, we got a more pleasant (but still problematic...) surprise from the pregnant stray cat that has been hanging around recently, sneaking food here and there. She had disappeared for a couple of weeks, and we thought perhaps something had happened to her. Well, clearly....something did! 😉
It seems she had a litter of kittens under our tool shed...and they just popped their little heads out last week. As if we didn't have enough trouble right now! 😲
Yeah they are undeniably cute as the dickens....but we simply can't handle that many cats. 🙀 Mom is very friendly and we're pretty sure she is currently unowned, so as soon as she is finished nursing her little fuzzballs, she is going to the vet to be spayed....and we will have to find homes for at least two of her babies. I've already decided to keep the cream colored one, and maybe one more if push comes to shove...but no more. Any takers??? Yeah...I already know the answer....😉
The Kremlin (Moscow, Russia).
The Kremlin is the historical, spiritual and political heart of Moscow and the city's most famous landmark and tourist attraction. It's an intriguing ensemble of buildings with an architectural variety that reveals a long and fascinating history. The Kremlin stands at the confluence of the Moscow and Neglinaya Rivers on Borovitsky Hill, named after the pine forests (bor in Russian) that used to cover it. Legend has it that while hunting in the forest a group of boyars (Russian nobles) saw an enormous two-headed bird swoop down on a boar, carry it away and deposit it on the top of what was to become Borovitsky Hill. That night the boyars dreamt of a city of tents, spires and golden domes and resolved the next morning to build a settlement on the hill. History sees it a little differently and attributes the founding of the Kremlin to Prince Yury Dolgoruky, who built the first wooden fort on the hill in 1147 AD, although historians believe that the site may have been inhabited as long ago as 500 BC. The word "kremlin" means simply "fortification" or "citadel" in Russian, and is thought to derive from either the Ancient Greek words kremn or kremnos, meaning a steep hill above a ravine, or the Slavonic term kremnik, meaning thick coniferous forest, that being the likely material from which the original fort was constructed. As the fortress was enlarged and developed, the city of Moscow rapidly sprung up around it. During the 14th century, when Moscow became the center of a Grand Principality, the fortress was for the first time perceived as a separate citadel and a principle part of the city and in 1331 was given the title "Kremlin". Between 1339 and 1340 the fortress was rebuilt with new walls and towers of oak, but due to the constant threat of fire damage, in 1366 the Moscow Prince Dmitry Ivanovich (later Donskoy) ordered the construction of a large white-stone wall around the fortress to protect it.
As Moscow struggled with the Khanate of the Golden Horde, repeated attacks by the Grand Prince Olgerd of Lithuania and political rivalry with the city of Tver, building work within the Kremlin continued and by the end of the 14th century the fortress was filled with churches, monasteries and manors housing the Grand Prince's retainers and the local nobility. The 15th century saw the unification of the Russian feudal principalities under the authority of the Grand Prince Ivan III of Moscow and to celebrate he ordered the reconstruction of the Kremlin on a grand scale. Architects, builders and craftsmen were drafted in from Pskov, Novgorod and Vladimir and the Italian architects Alberti Fioravante, Marco Bono and Pietro Antonio Solari began work on the Kremlin's ramparts and cathedrals. The new Cathedral of the Assumption was the first to be reconstructed, followed by the Cathedral of the Annunciation and the Church of the Deposition of the Robe in the 1480s and finally the Cathedral of the Archangel in the early 16th century. The Bell Tower of Ivan the Great, built between 1505 and 1508, completed the Cathedral Square ensemble and new Kremlin walls and towers were constructed simultaneously from 1485 onwards.
Successive rulers left their mark on the Kremlin and its architectural ensemble grew more and more varied throughout the centuries. The 15th century saw the addition of the Faceted Palace, the oldest secular building in the Kremlin complex. The 16th century ruler Ivan the Terrible further embellished the Kremlin's cathedrals and ramparts and constructed the enormous Tsar Canon and the Old English Embassy, for the purpose of accommodating English merchants and facilitating duty-free trade. At the start of the 17th century Mikhail Romanov assumed power and rebuilt and restored much of the fortress, adding the Terem Palace and the Patriarch's Palace and in 1655 Tsar Alexei's reign saw the casting of the impressive Tsar Bell. Although Peter the Great preferred St. Petersburg as his capital, he commissioned the construction of the Kremlin Arsenal in the 1730s for the storage of weapons and military equipment. Catherine the Great added the Senate building later that century and in the 1840s Nicholas I commissioned the Russo-Byzantine-style Armory and the Great Kremlin Palace. With the Bolshevik storming of the Kremlin during the 1917 Revolution the fortress was closed to the public for the next 50 years and the only architectural additions made by the Soviet regime were the 1934 Presidium and the modernistic State Kremlin Palace (previously the Palace of Congresses) in 1961. Today approximately two-thirds of the Kremlin is off-limits to visitors, including the Arsenal, the Presidium, the Terem, Faceted and Great Kremlin Palaces and most of the buildings in the northern half of the fortress. Tourists do, however, have access to all the cathedrals, the unmissable and priceless collections of the Armory, the Patriarch's Palace and the State Kremlin Palace, which hosts regular concerts and gala performances.
New year, new addition to Glasgow’s Mural Trail (www.citycentremuraltrail.co.uk) - and this one is very Glaswegian, being the eponymous lowlife sitcom character that is Rab C. Nesbitt - the ultimate headbanger’s headbanger - the string vest and bandaged headband-wearing street philosopher and occasional Buckfast-imbiber.
The lifelike painting has taken over the shopfront of Safe Hands on the corner of Argyle Street and Miller Street - next door to Cairns Bar, which Rab C. himself would surely approve of me offering up a pub as a street marker! - and painted by the prolific Australian-born, Glasgow-based contemporary street artist Smug (aka Sam Bates - beyondwalls.org/artists/smug/), was revealed only in mid-December 2023.
The cult BBC series (www.comedy.co.uk/tv/rab_c_nesbitt/), written by Ian Pattison, spanned the 1990s with a few returns in the 2010s. It followed the trials and tribulations of Rab C., (brilliantly portrayed by Gregor Fisher), and his put-upon wife Mary Doll (the equally brilliant Elaine C Smith) and their crazy life misadventures in Govan, with his decision to pursue unemployment as a lifestyle choice.
The only thing missing in this mural was a rolled-up copy of a tattered Evening Times in Rab’s outstretched hand, and a sound box ranting his catchphrase “I’ll tell you this boy. I’ll tell you this….”
Canon RP & Canon RF 24-105mm f/4-7.1
"It was from my own early experience that I decided there was no use to which money could be applied so productive of good to girls and boys who have good within them and ability and ambition to develop it as the founding of a public library." –Andrew Carnegie
The Carnegie library in Sauk Center was constructed in 1904 with funds from a $10,000 grant from Andrew Carnegie. Originally called the Bryant Public Library, it was named in honor of William Cullen Bryant, an American poet. The building continues to house the city’s library in addition to the Sauk Centre Historical Society Museum.
This is part of a continuing project to photograph the remaining 48 Carnegie library buildings in Minnesota.
I felt like I needed some more rolling stock to start off the new year.
Boxcars from BMR and Tankers from BTD
Decals by OKBrickworks
Looking southeast towards the tower of St. Bartholomew's Church.
"Sommerhausen is a market in the Würzburg district of Lower Franconia and a member of the Eibelstadt administrative community. Apart from the main town there are no other parts of the municipality.
Sommerhausen is located on the right bank of the Main, 13 kilometers south of Würzburg. In addition to viticulture, tourism and the art scene play a major role. Sommerhausen is surrounded by Ochsenfurt in the east and south, and Eibelstadt borders the municipality in the north. Directly opposite Sommerhausen, on the west bank of the Main, is the town of Winterhausen. The curious names of the two towns have their origins in the church patrons. The Sommerhäuser church patron Bartholomew has his memorial day in the summer (August 24th), the Winterhäuser church patron Nicholas in the winter (December 6th).
Sommerhausen has been an important community on the Main since the Middle Ages. It was not subordinate to the Prince-Bishop of Würzburg. The Limpurg taverns came to Sommerhausen in 1413 through the marriage of the tavern Friedrich and Elisabetha von Hohenlohe. As part of the Speckfeld rule of the heirs of Counts Schenk von Limpurg (first Counts Pückler, then Counts Rechteren-Limpurg), which was mediated by Bavaria, Sommerhausen belonged to the Franconian Imperial Circle from 1500. From 1540 onwards, the Reformation was introduced in the Limpurg region, so that Sommerhausen became a Protestant enclave in the predominantly Catholic Main Franconia.
In 1810 it came to the Grand Duchy of Würzburg during territorial consolidation, with which it returned to Bavaria in 1814. As part of the administrative reforms in Bavaria, today's municipality was created with the municipal edict of 1818. In 1896/1897 the community had a Main bridge built.
The place, nestled in the valley of the Main under vineyards, has been the flagship of Franconian romanticism for decades. The medieval city wall has been preserved. All the buildings in the town center in the narrow, winding streets look back on several hundred years of history. The town hall dates back to the 16th century.
Lower Franconia (German: Unterfranken) is one of seven districts of Bavaria, Germany. The districts of Lower, Middle and Upper Franconia make up the region of Franconia. It consists of nine districts and 308 municipalities (including three cities).
After the founding of the Kingdom of Bavaria the state was totally reorganised and, in 1808, divided into 15 administrative government regions (German: Regierungsbezirke, singular Regierungsbezirk), in Bavaria called Kreise (singular: Kreis). They were created in the fashion of the French departements, quite even in size and population, and named after their main rivers.
In the following years, due to territorial changes (e. g. loss of Tyrol, addition of the Palatinate), the number of Kreise was reduced to 8. One of these was the Untermainkreis (Lower Main District). In 1837 king Ludwig I of Bavaria renamed the Kreise after historical territorial names and tribes of the area. This also involved some border changes or territorial swaps. Thus the name Untermainkreis changed to Lower Franconia and Aschaffenburg, but the city name was dropped in the middle of the 20th century, leaving just Lower Franconia.
From 1933, the regional Nazi Gauleiter, Otto Hellmuth, (who had renamed his party Gau "Mainfranken") insisted on renaming the government district Mainfranken as well. He encountered resistance from Bavarian state authorities but finally succeeded in having the name of the district changed, effective 1 June 1938. After 1945 the name Unterfranken was restored.
Franconia (German: Franken, pronounced [ˈfʁaŋkŋ̍]; Franconian: Franggn [ˈfrɑŋɡŋ̍]; Bavarian: Frankn) is a region of Germany, characterised by its culture and Franconian dialect (German: Fränkisch).
Franconia is made up of the three Regierungsbezirke of Lower, Middle and Upper Franconia in Bavaria, the adjacent, Franconian-speaking, South Thuringia, south of the Thuringian Forest—which constitutes the language boundary between Franconian and Thuringian— and the eastern parts of Heilbronn-Franconia in Baden-Württemberg.
Those parts of the Vogtland lying in Saxony (largest city: Plauen) are sometimes regarded as Franconian as well, because the Vogtlandian dialects are mostly East Franconian. The inhabitants of Saxon Vogtland, however, mostly do not consider themselves as Franconian. On the other hand, the inhabitants of the Hessian-speaking parts of Lower Franconia west of the Spessart (largest city: Aschaffenburg) do consider themselves as Franconian, although not speaking the dialect. Heilbronn-Franconia's largest city of Heilbronn and its surrounding areas are South Franconian-speaking, and therefore only sometimes regarded as Franconian. In Hesse, the east of the Fulda District is Franconian-speaking, and parts of the Oden Forest District are sometimes regarded as Franconian for historical reasons, but a Franconian identity did not develop there.
Franconia's largest city and unofficial capital is Nuremberg, which is contiguous with Erlangen and Fürth, with which it forms the Franconian conurbation with around 1.3 million inhabitants. Other important Franconian cities are Würzburg, Bamberg, Bayreuth, Ansbach and Coburg in Bavaria, Suhl and Meiningen in Thuringia, and Schwäbisch Hall in Baden-Württemberg.
The German word Franken—Franconians—also refers to the ethnic group, which is mainly to be found in this region. They are to be distinguished from the Germanic people of the Franks, and historically formed their easternmost settlement area. The origins of Franconia lie in the settlement of the Franks from the 6th century in the area probably populated until then mainly by the Elbe Germanic people in the Main river area, known from the 9th century as East Francia (Francia Orientalis). In the Middle Ages the region formed much of the eastern part of the Duchy of Franconia and, from 1500, the Franconian Circle. The restructuring of the south German states by Napoleon, after the demise of the Holy Roman Empire, saw most of Franconia awarded to Bavaria." - 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.
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.
I introduce you to one of my newest paper garbage trucks! This is a 2023 Refurb Scorpion ASL. I have shown my small fleet of trucks on YT but not here!
"Shed" addition most likely put on when the store became a plumbing supply business.
================= Opened in 1967 as a classic Acme "Pitched roof" store and closed in 1979, when a new store was built on Island Avenue to replace it (now Shoprite).
After Acme moved out Thriftway opened here and remained in business until high crime forced it's closure (among other things the store apparently suffered a firebomb attack). From what I read online a plumbing supply house took over for a while until they too closed.
Today the building is tagged up with evidence of makeshift skate ramps set up. Inside, the store is stripped almost bare but the small "balcony" containing the offices, breakroom, restrooms, and electrical equipment is still intact. Also the Thriftway sign is still up at the front.
When I went I saw piles of dirt and heavy equipment on site so this structure might not be too long for this world....
their first evening of summer vacation. remember how awesome that feeling was? so much to anticipate and look forward to. :-)
my niece (on the left) graduated from kindergarten yesterday, which was in addition to my nephew graduating high school and my oldest niece graduating from college... 2012 has been a triple milestone year.
i've been so crazy busy (i think everybody must be... Flickr activity has been really slow lately).
Happy Friday everyone!
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Any suggestions on a name? This little one was wild ( someone threw out a mama cat with kittens). We've tamed him slowly, now he can't be petted enough.lol
The deep archway, dating from 1570, describes the joining of three houses into one. Huntly House, the mansion at the east end displays inscribed stone tablets; the means by which locals were rebuked for opposing its construction at this time.
The present name comes from the bakehouse on the west side. This comprised the quarters of the bakers and hammermen (metalsmiths) in addition to the Acheson family - household staff to James VI and Charles I. Huntly House, purchased in 1924, is now a principal City Museum.
Bakehouse Close leads to Holyrood Road.
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The Old Town of Edinburgh, Scotland, consisted originally of the main street, now known as the Royal Mile, and a large number of small alleyways that led off it to the north and south. Some of these lead to open courtyards and are therefore called “courts”. Others are open thoroughfare wide enough for a horse and cart, and are called “wynds”, a reference to the way they wind along. But most of these alleyways are called “closes”, because they lead to private property and are hence gated and closed to the public.
Bald eagles are carnivorous (piscivorous) and feed mainly upon fish. Their diet includes also small species of birds, rabbits, reptiles, crabs, and amphibians. In addition, they can eat the eggs of other birds.