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“Some offer their wealth, their austerity, and their practice of yoga as sacrifice, while the ascetics with strict vows offer their study of scriptures and knowledge as sacrifice.”
(Bhagavad Gita)
Since a few weeks those sadhus are staying at Darabhanga Ghat along the Ganges in Varanasi (Benaras).
The building of this ghat is a palace which was made by the king of Darabhanga from the Indian state of Bihar, it is now being restored into a luxurious hotel.
Beneath its wall several paintings showing a few gods and saints are preventing people to use this place as a bathroom and allowed this ghat to become clean again.
There is a kind of irony to see those men living there now...
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Today offered five movements through Rotherham Masborough of note in a twenty minute period, the highlight probably being the nearly passing of 56081 with a triple headed light engine move of Colas 56s. In the end I think these probably crossed at Primrose Bridge. The heavy rain showers even stopped for the movement and the sun popped out. 56302 leads 56087 and 56113 northbound on the 0C52 Washwood Heath to Doncaster movement, presumably for weekend engineering works.
Die Endfertigung des "red dot" fand in Köln als limitiertes Einzelstück statt, auf Grund günstiger Lohnstückkosten liegt der Schätzpreis des "dot" bei 12.600 €.
Die Zorki 4-K, Jupiter 8, Voigtländer VC Meter II und Tasche sind im Preis enthalten :-).
The final production of the "red dot" took place in Cologne/Germany as a limited single piece, due to cheaper labor costs is the estimate of the "dot" at € 12,600.
The Zorki 4-K, Jupiter 8, Voigtlander VC Meter II and bag are included in the Price :-)
"Postyrium" is an offer on wheels for children from the Royal danish Theatre. Three 40' containers represent the three arts: Ballet, theater and music. The children get a short story about the theatre's history, and then there are experiences on their own in the containers (which are equipped with light, sound and activities). I was allowed to follow a 1st class, and although there were good photos in all categories, I like the ones from the theater container's wardrobe the best.
Postyrium, parking lot behind the City Hall, Ballerup.
All images available for licensing via me. I offer commercial and editorial pet photography on a commissioned basis. And with a pet picture database with thousands of hand-picked images of dogs, cats, as well as horses, I might already have what you are looking for. All pictures here can be licensed.
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French postcard by Edition P.I., offered by Les Carbones Korès, no. 353. Photo: Warner Bros, 1953. Errol Flynn in Adventures of Don Juan (Vincent Sherman, 1948).
Australian-born actor Errol Flynn (1909-1959) achieved fame in Hollywood with his suave, debonair, devil-may-care attitude. He was known for his romantic Swashbuckler roles in films like Captain Blood (1935) and The Adventures of Robin Hood (1938), often co-starring Olivia de Havilland. In 1942, the tall, athletic and exceptionally handsome, Flynn became an American citizen. He developed a reputation for womanising, hard-drinking, and for a time in the 1940s, narcotics abuse. He was linked romantically with Lupe Vélez, Marlene Dietrich, and Dolores del Río, among many others.
Errol Leslie Thomson Flynn was born in a suburb of Hobart, Tasmania, in 1909. His father, Theodore, was a lecturer and later professor of biology at the University of Tasmania. His mother was Lily Mary Young. After early schooling in Hobart, from 1923 to 1925 Flynn was educated at the South West London College, a private boarding school in Barnes, London, and in 1926 returned to Australia to attend Sydney Church of England Grammar School (Shore School) where he was the classmate of a future Australian prime minister, John Gorton. His formal education ended with his expulsion from Shore for theft. After being dismissed from a job as a junior clerk with a Sydney shipping company for pilfering petty cash, he went to Papua New Guinea at the age of eighteen, seeking his fortune in tobacco planting and metals mining. He spent the next five years oscillating between the New Guinea frontier territory and Sydney. In early 1933, Flynn appeared as an amateur actor in the low-budget Australian film In the Wake of the Bounty (Charles Chauvel, 1933), in the lead role of Fletcher Christian. Later that year he returned to Britain to pursue a career in acting and soon secured a job with the Northampton Repertory Company at the town's Royal Theatre, where he worked and received his training as a professional actor for seven months. In 1934 Flynn was dismissed from Northampton Rep. reportedly after he threw a female stage manager down a stairwell. He returned to Warner Brothers' Teddington Studios in Middlesex where he had worked as an extra in the film I Adore You (George King, 1933) before going to Northampton. With his newfound acting skills, he was cast as the lead in Murder at Monte Carlo (Ralph Ince, 1935), now considered a lost film. During its filming, he was spotted by a talent scout for Warner Bros. and Flynn emigrated to the U.S. as a contract actor.
In Hollywood, Errol Flynn was first cast in two insignificant films, but then he got his great chance. He could replace Robert Donat in the title role of Captain Blood (Michael Curtiz, 1935). Flynn's natural athletic talent and good looks rocketed him overnight to international stardom. Over the next six years, he was typecast as a dashing adventurer in The Charge of the Light Brigade (Michael Curtiz, 1936), The Prince and the Pauper (William Keighley, 1937), The Adventures of Robin Hood (Michael Curtiz, William Keighley, 1938; his first Technicolor film), The Dawn Patrol (Edmund Goulding, 1938) with David Niven, Dodge City (Michael Curtiz, 1939), The Private Lives of Elizabeth and Essex (Michael Curtiz, 1939) and The Sea Hawk (Michael Curtiz, 1940). His striking good looks and screen charisma won him millions of fans. Flynn played an integral role in the re-invention of the action-adventure genre. In collaboration with Hollywood's best fight arrangers, Flynn became noted for fast-paced sword fights. He demonstrated an acting range beyond action-adventure roles in light, contemporary social comedies, such as The Perfect Specimen (Michael Curtiz, 1937) and Four's a Crowd (Michael Curtiz, 1938), and melodrama The Sisters (Anatole Litvak, 1938). During this period Flynn published his first book, 'Beam Ends' (1937), an autobiographical account of his sailing experiences around Australia as a youth. He also travelled to Spain, in 1937, as a war correspondent during the Spanish Civil War. Flynn co-starred with Olivia de Havilland a total of eight times, and together they made the most successful on-screen romantic partnership in Hollywood in the late 1930s-early 1940s in eight films. Flynn's relationship with Bette Davis, his co-star in The Private Lives of Elizabeth and Essex (Michael Curtiz, 1939), was quarrelsome. Davis allegedly slapped him across the face far harder than necessary during one scene.
In 1940, at the zenith of his career, Erroll Flynn was voted the fourth most popular star in the US. Flynn became a naturalised American citizen in 1942. As the United States had by then entered the Second World War, he attempted to enlist in the armed services but failed the physical exam due to multiple heart problems and other diseases. This created an image problem for both Flynn, the supposed paragon of male physical prowess, and for Warner Brothers, which continued to cast him in athletic roles, including such patriotic productions as Dive Bomber (Michael Curtiz, 1941), Desperate Journey (Raoul Walsh, 1942) and Objective, Burma! (Raoul Walsh, 1945). His womanizing lifestyle caught up with him in 1942 when two underage girls, Betty Hansen and Peggy Satterlee, accused him of statutory rape at the Bel Air home of Flynn's friend Frederick McEvoy, and onboard Flynn's yacht, respectively. The scandal received immense press attention. Many of Flynn's fans, assuming that his screen persona was a reflection of his actual personality, refused to accept that the charges were true. Flynn was acquitted, but the trial's widespread coverage and lurid overtones permanently damaged his carefully cultivated screen image as an idealised romantic leading player. In 1946, Flynn published an adventure novel, 'Showdown', and earned a reported $184,000. In 1947 he signed a 15-year contract with Warner Bros. for $225,000 per film. After the Second World War, the taste of the American film-going audience changed from European-themed material and the English history-based escapist epics in which Flynn excelled to more gritty, urban realism and film noir, reflecting modern American life. Flynn tried unsuccessfully to make the transition in Uncertain Glory (Raoul Walsh, 1944) with Paul Lukas and Cry Wolf (Peter Godfrey, 1947) with Barbara Stanwyck, and then increasingly passé Westerns such as Silver River (Raoul Walsh, 1948) and Montana (Ray Enright, 1950). Flynn's behaviour became increasingly disruptive during filming; he was released from his contract in 1950 by Jack L. Warner as part of a stable-clearing of 1930s glamour-generation stars. His Hollywood career over at the age of 41, Flynn entered a steep financial and physical decline.
In the 1950s, Errol Flynn became a parody of himself. He lost his savings from the Hollywood years in a series of financial disasters, including The Story of William Tell (Jack Cardiff, 1954) with Waltraut Haas. Aimlessly he sailed around the Western Mediterranean aboard his yacht Zaca. Heavy alcohol abuse left him prematurely aged and overweight. He staved off financial ruin with roles in forgettable productions such as Hello God (William Marshall, 1951), Il maestro di Don Giovanni/Crossed Swords (Milton Krims, 1954) opposite Gina Lollobrigida and King's Rhapsody (Herbert Wilcox, 1955) with Anna Neagle. He performed in such also-ran Hollywood films as Mara Maru (Gordon Douglas, 1952) and Istanbul (Joseph Pevney, 1957) with Cornell Borchers, and made occasional television appearances. As early as 1952 he had been seriously ill with hepatitis resulting in liver damage. In 1956 he presented and sometimes performed in the television anthology series The Errol Flynn Theatre which was filmed in Britain. He enjoyed a brief revival of popularity with The Sun Also Rises (Henry King, 1957); The Big Boodle (Richard Wilson, 1957), filmed in Cuba; Too Much, Too Soon (Art Napoleon, 1958); and The Roots of Heaven (John Huston, 1958) with Juliette Gréco. In these films, he played drunks and washed-out bums and brought a poignancy to his performances that had not been there during his glamorous heydays. He met with Stanley Kubrick to discuss a role in Lolita, but nothing came of it. Flynn went to Cuba in late 1958 to film the self-produced B film Cuban Rebel Girls (Barry Mahon, 1959), where he met Fidel Castro and was initially an enthusiastic supporter of the Cuban Revolution. He wrote a series of newspaper and magazine articles for the New York Journal American and other publications documenting his time in Cuba with Castro. Many of these pieces were lost until 2009 when they were rediscovered in a collection at the University of Texas at Austin's Center for American History. He narrated a short film titled Cuban Story: The Truth About Fidel Castro Revolution (1959), his last known work as an actor. He published his autobiography, My Wicked Wicked Ways. In 1959, Errol Flynn died of a heart attack in Vancouver, Canada. Flynn was married three times. His first wife was actress Lili Damita (1935-1942). They had one son, actor and war correspondent Sean Flynn (1941-1971). Sean and his colleague Dana Stone disappeared in Cambodia in 1970, during the Vietnam War, while both were working as freelance photojournalists for Time magazine. It is generally assumed that they were killed by Khmer Rouge guerrillas. Errol was married a second time to Nora Eddington from 1943 to 1949. They had two daughters, Deirdre (1945) and Rory (1947). His third wife was actress Patrice Wymore from 1950 until his death. They had one daughter, Arnella Roma (1953–1998). In 1980, author Charles Higham published a controversial biography, 'Errol Flynn: The Untold Story', in which he alleged that Flynn was a fascist sympathiser who spied for the Nazis before and during the Second World War and that he was bisexual and had multiple gay affairs. Later Flynn biographers were critical of Higham's allegations and found no evidence to corroborate them.
Sources: Charles Culbertson (IMDb), Wikipedia, and IMDb.
And, please check out our blog European Film Star Postcards.
"What's this?" Norman asks... "This safe contains very dangerous weaponry. It can only be opened by the code '1228'. I will offer it to you for $4,000. I wouldn't offer this to anyone, but because we are friends, you can have it. Do you accept?" Kingpin replies... Norman frowns for a second, but then smiles... "Indeed I do." He answers. "Excellent. Oh, and one more thing... I have someone in mind for using the weaponry. Old mercenary friend of mine... His name is Herman Schultz." Kingpin explains...
~Scarecrow
All images available for licensing via me. I offer commercial and editorial pet photography on a commissioned basis. And with a pet picture database with thousands of hand-picked images of dogs, cats, as well as horses, I might already have what you are looking for. All pictures here can be licensed.
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Aston Martin Residences offer breathtaking views of the Miami River, Biscayne Bay, and Brickell skyline. Additionally, Aston Martin Residences will be within walking distance of Whole Foods, Brickell City Centre, and Mary Brickell Village.
Aston Martin’s design team will design the building’s interior common spaces including the two private lobbies, the two-level fitness center with ocean views, and a full-service spa among other shared spaces within the development.
Each of the building’s common areas will feature “signature items” showcasing the car brand’s trademark colors, stitching style, and materials—from polished wood and supple leather to carbon fiber with an emphasis on comfort.
Credit for the data above is given to the following websites:
www.emporis.com/buildings/1386750/aston-martin-residences...
www.paraninternational.com/new-development/aston-martin
© All Rights Reserved - you may not use this image in any form without my prior permission.
Thank You, dear friends, for the immense joys and pleasures you offered with your fantastic work, to me and untold others. This is the first of my "Thank You 'Quilts' - and if you can't find your photos here yet, wait patiently, I shall do more...
It's such fun too and I can think of every single one while hunting THE picture!
Please VISIT the streams of my friends. They are SO talented and deserve each and every visit!
1. amazing grace, Hello, Guten Tag, liebe Rafaela! I still can hardly believe that I've found you this year... :)
2. autumnal still life, Merci, one of my most beloved ones, chère Isabelle....
3. Petit matin Early morning., Michelle, another one of my French spoken and ever so faithful friends!
4. www.flickr.com/photos/brartist/1848327794/, Ola, liebe Petra, you are a relative newcomer to my friends' circle - aber du fühlst dich total wohl, nicht! :)
5. Light in the Forest, Alex, my all-time 'misty and fog' master works 'provider'. If I didn't already love England, I would after visiting his stream...
6. Essence of tutu!, another 2007 'acquisition', my dear, dear friend Catherine, Cathy who comes home every so often.... :)
7. Into light and under shadow, Gina, I have found you, lost you and luckily found you again! Thank You....
8. Soft and Sunny, Angie, what a pleasure to visit you!
9. Petal Pink, The Queen of Hearts.... Jan, you are surely the only flickrite who get's groups called after you.... I LOVE your work and your comments :)
10. golden morning hour.........., Horst, you are another one who got lost and luckily was re-found!!! Thank You so much for being a great friend
11. Dedicated to my Dad, who passed away, five years ago yesterday... My probably first Flickr buddy, dearest Lauri. Her photos come straight from her heart, Thank You my love!
12. Sunbathing…!!! / Bain de soleil!!! :))) Jet another 2007 newcomer to my cercle of amis, mon cher Denis - je suis ravie d'avoir faite ta connaissance!!
13. apple Here my last but by no means least my dear friend Barbara, one of the few I've met in flesh - in real life! Great artist, thank you
Kindly add a little comment to YOUR picture, so that other viewers can just click on your photo and get straight to your photo stream... :))) That should get you some additional comments and faves!
© all rights/copyright reserved by © Kiki Vol-au-Vent
Aston Martin Residences offer breathtaking views of the Miami River, Biscayne Bay, and Brickell skyline. Additionally, Aston Martin Residences will be within walking distance of Whole Foods, Brickell City Centre, and Mary Brickell Village.
Aston Martin’s design team will design the building’s interior common spaces including the two private lobbies, the two-level fitness center with ocean views, and a full-service spa among other shared spaces within the development.
Each of the building’s common areas will feature “signature items” showcasing the car brand’s trademark colors, stitching style, and materials—from polished wood and supple leather to carbon fiber with an emphasis on comfort.
Credit for the data above is given to the following websites:
www.emporis.com/buildings/1386750/aston-martin-residences...
www.paraninternational.com/new-development/aston-martin
© All Rights Reserved - you may not use this image in any form without my prior permission.
Oceana's atrium offers a real 'wow' as soon as you step on board, with its palm trees and glass-fronted lifts. Her diverse and flexible dining and entertainment options offer great choice day and night - from 2 main restaurants, an Italian restaurant by Marco Pierre White and a poolside grill to 10 places to drink, a nightclub, a casino, 2 pools and a champagne bar, plus fun facilities for children of all ages. Also many weddings were carried out at this location.
Another look at this ensemble. Just me sitting on the stairs in isolation. I think its important at this time to post a few pics and try and put a smile on peoples faces and to distract us from whats happening around us
The photograph offers a view of Prague, taken from Letná Plain. In the foreground, there is a railing with tree leaves framing the city's view. In the center of the image, the Vltava River stretches across with Štefánik Bridge spanning it. On the right side, a prominent building with a dome, the Ministry of Industry and Trade, is part of the city's architectural panorama. The background reveals a densely built-up city with distinct buildings, and in the distance, the Žižkov Television Tower is visible. The sky is dramatic with colorful clouds and a possible hint of a rainbow. Overall, the image captures the beauty and atmosphere of Prague at sunset.
_Z725591_LN_HDR_W
Elsevier now offers a series of derivative works based on the acclaimed Meylers Side Effect of Drugs, 15th Edition. These individual volumes are grouped by specialty to benefit the practicing physician or health care clinician.
Endocrine and metabolic diseases are common, includes diseases such as diabetes, thyroid disease, and obesity. Endocrinologists, including diabetes professionals, internal medicine and primary care practitioners, obstetricians and gynecologists, and others will find this book useful when treating endocrine or metabolic diseases.
The material is drawn from the 15th edition of the internationally renowned encyclopedia, Meyler's Side Effects of Drugs, and the latest volumes in the companion series, Side Effects of Drugs Annuals. Drug names have usually been designated by their recommended or proposed International Non-proprietary Names (rINN or pINN); when those are not available, clinical names have been used. In some cases, brand names have been used.
This volume is critical for any health professional involved in the administration of endocrine and metabolics mediations.
Dr Jeffrey K. Aronson is a consultant clinical pharmacologist and physician in the Department of Primary Health Care in the University of Oxford and a consultant physician in the Oxford Radcliffe Hospitals Trust. He has been associated with the Meyler series since 1977 and has published many research papers on adverse drug reactions. He is also the editor of Meyler's Side Effects of Drugs and the Side Effects of Drugs Annual series. He is President of the British Pharmacological Society and serves on many committees concerned with drug therapy, including the Technology Appraisal Committee of the UK's National Institute for Health and Clinical Excellence (NICE) and the Joint Formulary Committees of the British National Formulary and the British National Formulary for Children.
Entrance on the corner of River and Lake Streets.
Description
Council Rock is situated at the corner of Lake and River Streets within the Village of Cooperstown. It is a 1.25 acre site on the west bank of the mouth of the Susquehanna River. Stone steps lead from the street to the Lake.
Not only does the park offer a magnificent view of the lake, but it is also an important site in the history of Cooperstown [Council Rock and Clinton/Sullivan Expedition of August 9, 1779]. Its entrance is marked by two stone columns with Historical Markers and a large painted arrow which indicates true North.
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The 1779 Sullivan Expedition, also known as the Sullivan-Clinton Expedition, or Sullivan Campaign was an extended systematic military campaign during the American Revolutionary War against Loyalists ("Tories") and the four Nations of the Haudenosaunee which had sided with the British. It has been described by some historians as a genocide due to the magnitude and totality of its violence towards and destruction of the Haudenosaunee.
The campaign ordered and organized by George Washington and his staff was conducted chiefly in the lands of the Iroquois Confederacy (also known as the Longhouse Confederacy) "taking the war home to the enemy to break their morale", and the expedition was largely successful in that goal as they destroyed more than 40 Iroquois villages and stores of winter crops, breaking the power of the six nations in New York all the way to the Great Lakes, as the terrified Indian families relocated to Canada seeking protection of the British. Today this area is the heartland of Upstate New York, and with the military power of the Iroquois vanquished, the events also opened up the vast Ohio Country, the Great Lakes regions, Western Pennsylvania, West Virginia, and Kentucky to post-war settlements.
Led by Major General John Sullivan and Brigadier General James Clinton, the expedition was conducted during the summer of 1779, beginning June 18 when the army marched from Easton, Pennsylvania, to October 3 when it abandoned Fort Sullivan, built at Tioga, to return to George Washington's main camp in New Jersey. While the campaign had only one major battle, at Newtown (since the tribes evacuated ahead of the large military force) along the Chemung River in western New York, the expedition severely damaged the Iroquois nations' economies by burning their crops, villages, and chattels, thus ruining the Iroquois technological infrastructure. With the Native Americans' shelter gone and food supplies destroyed, thereafter the strength of the Iroquois Confederacy was broken. The death toll from exposure and starvation dwarfed the casualties received in the Battle of Newtown, in which about 1,000 Iroquois and Loyalists were decisively defeated by an army of 3,200 Continental soldiers.
Sullivan's army carried out a scorched earth campaign, methodically destroying at least forty Iroquois villages throughout the Finger Lakes region of western New York, to put an end to Iroquois and Loyalist attacks against American settlements as had occurred the previous year of 1778, such as the Cobleskill, Wyoming Valley and Cherry Valley massacres. The survivors fled to British regions in Canada and the Niagara Falls and Buffalo areas. The devastation created great hardships for the thousands of Iroquois refugees who fled the region to shelter under British military protection outside Fort Niagara that winter, and many starved or froze to death, despite strenuous attempts by the British authorities to import food and provide shelter via their limited resources.
The Sullivan Expedition devastated the Iroquois crops and towns and left them dependent upon the mercy of the British for the harsh winter of 1779. With the Iroquois population decimated by disease and battle, the Indian morale never fully recovered, and the Iroquois thereafter mostly limited their incursions into the new United States to isolated hunting parties, the main populations having permanently migrated north of the border.
When the American Revolutionary War began, British officials as well as the colonial Continental Congress sought the allegiance (or at least the neutrality) of the influential Iroquois Confederacy. The Six Nations divided over what course to pursue. Most Mohawks, Cayugas, Onondagas, and Senecas chose to ally themselves with the British. But the Oneidas and Tuscaroras, thanks in part to the influence of Presbyterian missionary Samuel Kirkland, joined the American revolutionaries. For the Iroquois, the American Revolution became a civil war.
The Iroquois homeland lay on the frontier between the Province of Quebec and the provinces of New York and Pennsylvania. After a British army surrendered after the Battles of Saratoga in upstate New York in 1777, Loyalists and their Iroquois allies raided American Patriot settlements in the region, as well as the villages of American-allied Iroquois. Working out of Fort Niagara, men such as Loyalist commander Colonel John Butler, Sayenqueraghta, Mohawk military leader Joseph Brant, and Seneca chief Cornplanter led the British-Indian raids. Commander-in-chief General George Washington never allocated more than minimal Continental Army troops for the defense of the frontier and he told the frontier settlements to use local militia for their own defense.
On June 10, 1778, the Board of War of the Continental Congress concluded that a major Indian war was in the offing. Since a defensive war would prove to be inadequate the board called for a major expedition of 3,000 men against Fort Detroit and a similar thrust into Seneca country to punish the Iroquois. Congress designated Major General Horatio Gates to lead the campaign and appropriated funds for the campaign. In spite of these plans, the expedition did not occur until the following year.
On July 3, 1778, Loyalist commander Colonel Butler led his Rangers accompanied by a force of Senecas and Cayugas (led by Sayenqueraghta) in an attack on Pennsylvania's Wyoming Valley (a rebel granary and settlement along the Susquehanna River near Wilkes-Barre), practically annihilating 360 armed Patriot defenders lured out of their defenses at Forty Fort.
In September 1778, revenge for the Wyoming defeat was taken by American Colonel Thomas Hartley who, with 200 soldiers, burned nine to twelve Seneca, Delaware and Mingo villages along the Susquehanna River in northeast Pennsylvania, including Tioga and Chemung. At the same time, Butler's Rangers attacked German Flatts in the Mohawk Valley, destroying all the houses and fields in the area. Further American retaliation was soon taken by Continental Army units under William Butler (no relation to John Butler) and John Cantine, burning the substantial Indian villages at Unadilla and Onaquaga on the Susquehanna River.
On November 11, 1778, Loyalist Captain Walter Butler (the son of John Butler) led two companies of Butler's Rangers along with about 320 Iroquois led by Cornplanter, including 30 Mohawks led by Joseph Brant, on an assault at Cherry Valley in New York. While the fort was surrounded, Indians began to massacre civilians in the village, killing and scalping 16 soldiers and 32 civilians, mostly women and children, and taking 80 captive, half of whom were never returned. In vain, Brant, who was blamed for the attack, actually tried to stop the rampage. The town was plundered and destroyed.
The Cherry Valley Massacre convinced the American colonists that they needed to take action. In April 1779, American Colonel Van Schaick led an expedition of over 500 soldiers against the Onondaga, destroying several villages. When the British began to concentrate their military efforts on the southern colonies in 1779, Washington used the opportunity to launch a larger planned offensive towards Fort Niagara. His initial impulse was to assign the expedition to Major General Charles Lee, but he, Major General Philip Schuyler, and Major General Israel Putnam were all disregarded for various reasons. Washington first offered command of the expedition to Horatio Gates, the "Hero of Saratoga," but Gates turned down the offer, ostensibly for health reasons. Major General John Sullivan, fifth on the seniority list, was offered command on March 6, 1779, and accepted. Washington's orders to Sullivan made it clear that he wanted the Iroquois threat completely eliminated:
Orders of George Washington to General John Sullivan, at Head-Quarters (Wallace House, New Jersey) May 31, 1779
The Expedition you are appointed to command is to be directed against the hostile tribes of the Six Nations of Indians, with their associates and adherents. The immediate objects are the total destruction and devastation of their settlements, and the capture of as many prisoners of every age and sex as possible. It will be essential to ruin their crops now in the ground and prevent their planting more.
I would recommend, that some post in the center of the Indian Country, should be occupied with all expedition, with a sufficient quantity of provisions whence parties should be detached to lay waste all the settlements around, with instructions to do it in the most effectual manner, that the country may not be merely overrun, but destroyed.
But you will not by any means listen to any overture of peace before the total ruinment of their settlements is effected. Our future security will be in their inability to injure us and in the terror with which the severity of the chastisement they receive will inspire them.[5]
Washington instructed Gen. Sullivan and three brigades to march from Easton, Pennsylvania to the Susquehanna River in central Pennsylvania and to follow the river upstream to Tioga, now known as Athens, Pennsylvania. He ordered Gen. James Clinton to assemble a fourth brigade at Schenectady, New York, move westward up the Mohawk River Valley to Canajoharie, and cross overland to Otsego Lake as a staging point. When Sullivan so ordered, Clinton's New York Brigade was to march down the Susquehanna to meet Sullivan at Tioga, destroying all Indian villages on his route. Sullivan's army was to have totaled 15 regiments and 5,000 men, but his Pennsylvania brigade entered the campaign more than 750 men short, and promised enlistments never materialized. In addition, the third regiment of the brigade, the German Battalion, had shrunk by casualties, sickness, and desertion (the three-year term of enlistment of its soldiers had expired on June 27) to only 100 men, and was parceled out in 25-man companies as flank protection for the expedition. Armand's Legion was recalled by Washington to the Main Army before the campaign began. Because of these and other shortages, Sullivan's army, including two companies of local militia totaling only 70 men, never exceeded 4,000 troops.
The main army left Easton on June 18, marching 58 miles to an encampment on the Bullock farm in the Wyoming Valley, which it reached on June 23. There they awaited provisions and supplies that had not been sent forward, remaining in the Wyoming Valley until July 31. The army marched slowly, paced by both the mountainous terrain and the flatboats carrying the army's supplies up the Susquehanna, and arrived at Tioga on August 11. They began construction of a temporary fort at the confluence of the Chemung and Susquehanna Rivers they called Fort Sullivan.
Sullivan sent one of his guides, Lt. John Jenkins, who had been captured while surveying the area in November 1777, with a scouting party to reconnoiter Chemung. He reported that the village was active and unaware of his presence. Sullivan marched the greater part of the army all night over two high defiles and attacked out of a thick fog just after dawn only to find the town deserted. Brig. Gen. Edward Hand reported a small force fleeing towards Newtown and received permission to pursue. Despite flankers, he had gone only a mile when his advance guard was ambushed with six dead and nine wounded. The entire brigade assaulted but the ambushers escaped with minimal if any casualties. Sullivan's men spent the day burning the town and destroyed all of its grain and vegetable crops. During the afternoon the 1st New Hampshire Regiment of Poor's brigade was fired on, either from ambush or possibly by fire from other troops, inflicting another soldier killed and five wounded. Ambushes also occurred on August 15 and August 17, with combined casualties of two killed and two wounded. On August 23, the accidental discharge of a rifle in camp resulted in one captain killed and one man wounded.
After two-weeks' portage of supplies, Clinton's brigade set up camp on June 30 at the south end of Otsego Lake (now Cooperstown, New York), where he waited for orders that did not arrive until August 6. The next day he began his destructive march of 154 miles (248 km) to Tioga along the upper Susquehanna, taking all of his supplies with him in 250 bateaux. The actions at Chemung made Sullivan suspicious that the Iroquois might be trying to defeat in detail his split forces, and the next day he sent 1,084 picked men under Brig. Gen. Enoch Poor north to locate Clinton and escort him to Fort Sullivan. The entire army assembled on August 22.
On August 26, the combined army of approximately 3,200 men and 250 pack horse teamsters left Fort Sullivan, garrisoned by 300 troops taken from across the army and left behind under Col. Israel Shreve of the 2nd New Jersey Regiment. Marching slowly north into the Six Nations territory in central western New York, the campaign had only one major battle, the Battle of Newtown, fought on August 29. It was a complete victory for the Continental Army. Later a 25-man detachment of the Continental Army was ambushed, and all but five captured and killed at the Boyd and Parker ambush. On September 1 Captain John Combs died of an illness.
Sullivan's forces reached their deepest penetration at the Seneca town of Chenussio (also called Little Beard's town, Beardstown, Chinefee, Genesee, and Geneseo), near the present Cuylerville, New York, on September 15, inflicting total destruction on the Iroquois villages before returning to Fort Sullivan at the end of the month. Three days later the army abandoned the fort to return to Morristown, New Jersey, and go into winter quarters. By Sullivan's account, forty Iroquois villages were destroyed, including Catherine's Town, Goiogouen, Chonodote, and Kanadaseaga, along with all the crops and orchards of the Iroquois.
Appointed the British governor of Quebec in 1778, Frederick Haldimand, while kept informed of Sullivan's invasion by Butler and Fort Niagara, did not supply sufficient troops for his Iroquois allies' defense. Late in September, he dispatched a force of about 600 Loyalists and Iroquois, but by then the expedition had successfully ended.
Further west, a concurrent expedition was undertaken by Colonel Daniel Brodhead. Brodhead left Fort Pitt on August 14, 1779, with a contingent of 600 men, regulars of his 8th Pennsylvania Regiment and militia, marching up the Allegheny River into the Seneca and Munsee country of northwestern Pennsylvania and southwestern New York. Since most native warriors were away to confront Sullivan's army, Brodhead met little resistance and destroyed about 10 villages, including Conewango. Although initial plans called for Brodhead to eventually link up with Sullivan at Chenussio for an attack against Fort Niagara, Brodhead turned back after destroying villages near modern-day Salamanca, New York, never linking up with the main force. Washington's letters indicate that the cross-country trek east to the Finger Lakes region was considered too dangerous, limiting this smaller expedition to a raid north.
The final operation of the campaign occurred September 27. Sullivan sent a portion of Clinton's brigade directly back to winter quarters by way of Fort Stanwix, under Colonel Peter Gansevoort of the 3rd New York Regiment. Two days after leaving Stanwix, near their origination point of Schenectady, the detachment stopped at Teantontalago, the "Lower Mohawk Castle" (also known as Thienderego, Tionondorage and Tiononderoga) and carried out orders to arrest every male Mohawk. Gansevoort wrote "It is remarked that the Indians live much better than most of the Mohawk River farmers, their houses [being] very well furnished with all [the] necessary household utensils, great plenty of grain, several horses, cows, and wagons". The male population was incarcerated at Albany until 1780 and then released.
The action dispossessed the Mohawks of their homes. Local white settlers, homeless after Iroquois raids, asked Gansevoort to turn the homes over to them. Both actions were criticized by Philip Schuyler, then a New York representative to the Continental Congress, because all the Mohawks of Lower Mohawk castle had rejected fighting with the British, and many supported the Patriot cause. Ironically, Schuyler had been Washington's personal preference for command of the expedition, but his relief of command of the Continental Army's Northern Department had led to private service with the army until he could resign his commission, which he did in April 1779.
Exhausted from carrying heavy military equipment, Sullivan's horses reached the end of their endurance on their return route home. Just north of Elmira, New York, Sullivan euthanized his pack horses. A few years later, the skulls of these horses were lined along the trail as a warning to settlers. The area became known as "the Valley of Horses Heads" and is now known as the village and town of Horseheads, New York.
Sullivan, whose illness had slowed the expedition at times, resigned his commission in 1780 when his health continued to worsen.
More than 5,000 Iroquois refugees went to Canada (modern Ontario) for the British to feed. A report from 1778 by John Butler on the Haudenosaunee: "The Indians in this part of the Country are so ill off for Provisions that many have nothing to subsist upon but the roots and greens they gather in the woods" in May, 1778 – i.e., before the expedition. Fearing attack, many Tuscarora and Oneida defected to the British cause. The British granted the Indians 675,000 acres of land in Canada. About 1450 Iroquois and 400 allies lived at one new reserve at Grand River.
In February 1780, retired General Schuyler, now in the Congress, sent a party of pro-rebellion Indians to Fort Niagara to appeal for peace with the British-allied Iroquois. Suspecting a trick by Schuyler, those Iroquois rejected the proposal. The four messengers were imprisoned where one of them died.
Despite widespread dispersion, Washington was disappointed by the lack of a decisive battle and the failure to capture Fort Niagara. Although in truth, Washington's guidance to Sullivan had been that he take Ft Niagara, "if possible," an option not easily within Sullivan's means given the limitations of his artillery (no guns bigger than six inch field howitzers) and his logistics. Iroquois warriors and Loyalists continued to periodically raid the Mohawk and Schoharie Valleys during 1780 and 1781, causing widespread devastation of property and crops, and killing more than 200 settlers. The destruction of Minden on August 2, 1780 was the most destructive raid of property in the course of the four-year civil war. The last significant raid devastated a 20-mile swath of the lower Mohawk Valley in October 1781, but was defeated at the Battle of Johnstown on October 25, 1781. Walter Butler was killed in battle on October 30 at West Canada Creek during the Tory retreat.
The homelands and infrastructure of Iroquois life had been devastated by the campaign. In the long term, it became clear that the expedition broke the Iroquois Confederacy's power to maintain their former crops and utilize many town locations; the expedition appeared to have caused little more than famine and dispersion of the Iroquois people.
Following the war much of the Iroquois land was secured by the United States government in the peace Treaty of Fort Stanwix (1784) agreed to by the six nations of the Iroquois League. This land was later absorbed by treaties with the State of New York.
Much of the native population of these lands would move to Canada, Oklahoma, and Wisconsin. In the wake of the Treaty of Paris (1783), European-Americans began settling the newly vacant areas in relative safety, eventually isolating the remaining pockets of demoralized Iroquois into villages and towns cut off under land treaties with New York State (Wikipedia).
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Corgi offered a less extensive range of commercial vehicles than rival Dinky Toys. The initial range, as far as I can determine, comprised Commer QX, ERF KV and Bedford S-Type cabs with a variety of body styles, plus the Bedford CA in van and Utilicon form. All were attractive and accurate models with the added advantage of glazing at a time when Corgi was promoting its products as ‘the Ones with Windows’. This is an approximate real-life representation of No 456, which utilised the ERF KV cab. The dropside body isn’t quite right (being of steel rather than timber construction) but the colours have been matched to the model. The same chassis/cab also appeared with flatbed, box van, cement truck and tipper bodies; and also as a gift set with a drawbar trailer (22-Oct-22).
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A gift placed on a stone monument enshrining the "Fuji Sengen Daibosatsu".
This picture was taken at the summit of Kozukue Fuji (41m above sea level) in the forest of Kozukue Castle Remains in Kozukue-cho, Kohoku Ward, Yokohama, and Kanagawa.
Our weekend offer is ready and waiting for you at Addams Mainstore, while Victoria Outfit is not a new release this set comes in our new palettes and have the latest Lara X and Legacy Bombshell fitting!
Make sure to check them out but also to try a demo before your purchase!
Available for the following bodies:
- Maitreya X
- Petite X
- Ebody Reborn
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The man on the picture is a Surma warrior. He is ready to fight with the stick he's got in his right hand. The fight is very impressive to watch, and dangerous too as they just do not care about what's happening around! On his left hand, he has a shield to protect the fingers. I saw a warrior who had 10 fingers broken... They must not show any pain during the fight. On the left hand too, you can see some necklaces: they have been offered by girls to him. You can count: he has many girlfriends! Surma can have sex with girls before wedding, as much as they want, and can, but atfer wedding, girls must remain with their husband only while the man can marry many women.
The less the warrior wears some protection (like this one has an helmet on his head), the more he's strong. So we can say this one is not strong!
Mursi tribe also have the same tradition.
One of the main Surma / Suri customs is stick fighting. This ritual and sport is called Donga or Sagenai (Saginay). Donga is both the name of the sport and the stick, whereas sagenai is the name of the stick-fighting session. Stick fighting is central in Suri culture. In most cases, stick fighting is a way for warriors to find girlfriends, it can also be a way to settle conflicts. On this occasion men show their courage, their virility and their resistance to pain, to the young women. The fights are held between Suri villages, and begin with 20 to 30 people on each side, and can end up with hundreds of warriors involved. Suri are famous for stick fighting, but they are not the only ones to respect such a custom, as the neighbor tribe, the Mursi, also practice these traditional fights
The day before the sagenai, fighters have to purge themselves. They do it by drinking a special preparation, called dokai, which is made of the bark of a special tree, which is mixed with water. After taking it, warriors make themselves vomiting the drink. The water is supposed to bring with it many of the body’s impurities. After this ritual they don’t eat until the following morning. Warriors walk kilometers to come fighting at Sagenai, which takes place in a clearing. They stop when crossing a river in order to wash themselves, before decorating their bodies for the fight. They decorate themselves by sliding the fingers full of clay on the warrior’s bodies. This dressing up and decoration is meant to show their beauty and virility and thus catch the women’s attention. The phallic shape ending the sticks contributes to that virile demonstration.
Fighters arrive on the Donga field all together, carrying the strongest man,dancing and singing. Some fighters wear colourful headdresses sometimes with feathers on it, and also knee-protectors. But most of them use no protection at all and fight completely naked in order to show their bravery. They also wear strings of decorative coloured beads around their necks given by the girls and waist, but their genitals are most of the time uncovered and they are barefoot.
All of them get a chance to fight one on one, against someone from the other side. In the beginning each fighter looks for an opponent of the same stature, and exchanges a few held back blows with him in order to test him. If both fighters feel they have found a match, they suddendly throw themselves into the fight, hitting ferocious fast strokes with their sticks. If one of the warriors knocked out or puts paid to his opponent, he immediately declares himself the winner. Sagenai consists in qualifying rounds, each winner fighting the winner of a previous fight, until two finalists are left.
It is strictly forbidden to hit a man when he is down on the ground. During these fights there are referees present to make sure all rules are being followed. Many stick fights end within the first couple of hits. Nevertheless the fights are really violent, and it is quite usual to see men bleeding. Stick fighting has proven to be dangerous because people have died from being hit in the stomach. Loosing an eye or a leg during the fight is quite common, although it is strictly forbidden for a fighter to kill his opponent, and if a fighter gets killed during the fight, his opponent and all his family are banned from the village for life.
For the other locals, especially teenagers, sagenai is a great outing. Girls watch the fights, but it is also the occasion to check out the men, and to meet in order to chat or even gossip.
At the end of the fights, the winners point their phallic sticks in direction of the girls they want to date with, if the girl put a necklace around the stick, it means she is willing to date the champion. Sometimes a group of girls is presented to the champion, who previously which one of them would date the him.
Since stick fighting draws a large audience, it becomes dangerous. For the audience the risk of being hit, is not to be underestimated. Shooting can also easily break out and this seems to be the new trend for young Suri men using AK-47 (Kalashnikov) instead of sticks. The risk of being shot is all the higher as spectators and participants drink gesso, a thick local beer made from fermented maize, and are often quite drunk during the Sagenai.
It’s quite common to see men carrying weapons which are part of the daily life. Their remote homeland has always been a place of traditional rivalries with the neighbouring tribes such as the Bume (Nyangatom) or the Toposa. who regurlarly team up to raid the Suri’s cattle. These fights, and even sometimes battles, have become quite bloody since automatic firearms have become available from the parties in the Sudanese Civil War. This conflict has pushed neighboring tribes into Suri’s land and is a constant competition to keep and protect their territory and their cattle. A battle even ended up with the death of hundreds of Suri, including women and children.
© Eric Lafforgue
Vyšehrad is the oldest seat of Czech princes; in fact, the local settlement was established in the mid-10 th century. Situated on a rocky promontory above the Vltava River, it offers stunning views of the city, and the park area holds hidden architectural treasures including the rare Romanesque Rotunda of St Martin, the neo-Gothic Church of Sts Peter and Paul, the national cemetery Slavín, and the underground casements housing the some of the original Baroque statues from the Charles Bridge.
The trail to Angels Landing offers drop dead, gorgeous views of Zion National Park's valley, thousands of feet below. In late October, the colors of autumn creep thru this magical place while the Virgin River, just a trickle at this time of year, winds its way thru the park. The hike to Angels Landing, while quite strenuous, and not for the faint hearted, is one of the most breathtaking experiences I've found in any of our country's national parks. I can't recommend it enough to anyone who enjoys a challenge with potentially great rewards. Late October is the ideal time to enjoy cool weather, light crowds and spectacular colors throughout the park.
Zion National Park, Utah.
View on black or gray / B l a c k M a g i c
View my photo stream on Flickr Hive Mind</a
The Phoenix metro area is still filled with empty lots, once farms, as the property owners hold out for higher prices to sell out. View large.
Minolta XG-M with Fujichrome Tungsten ISO64 (T64) 35mm slide film, cross-processed.
Dorset Mela offers a unique experience to people in Dorset as it brings various communities together. This event offers a unique dining experience with variety of food, dance, music, live performances, handicraft, henna painting and many more activities.
The Trango Towers are a group of dramatic granite spires located on the north side of the Baltoro Glacier, in Baltistan, a district of the Gilgit-Baltistan region of Pakistan (formerly Northern Areas). They are part of the Baltoro Muztagh, a subrange of the Karakoram range. The Towers offer some of the largest cliffs and most challenging rock climbing in the world. The highest point in the group is the summit of Great Trango Tower, 6,286 m (20,608 ft). (Note: all elevations in this article are subject to significant uncertainty: it is not clear if they have ever been determined precisely, and sources vary.) The east face of the Great Trango Tower features the world's greatest nearly vertical drop.
Harbour at New River is a 36-story high-rise building. It is a multi-family tower with 337 apartment units. The building also includes ground-floor retail spaces and a 7th-floor amenity deck.
Harbour at New River is a luxury waterfront apartment community in Fort Lauderdale, Florida. It is located on the south side of the New River in the downtown Tarpon River neighborhood, offering residents a balance of tranquility and urban vibrancy.
Key features
Waterfront Living: The apartments offer panoramic water views and are situated along the Fort Lauderdale Riverwalk, giving residents direct access to the river.
Location: The property is within walking distance of Las Olas Boulevard and its upscale dining, shopping, and entertainment options. Downtown Fort Lauderdale, with its arts, culture, and beaches, is also nearby.
Residences: The building offers studio, one, two, and three-bedroom apartments with luxury finishes, including Italian cabinetry, quartz countertops, and high-end stainless-steel appliances. Select units feature private terraces and walk-in closets.
Amenities: Residents have access to resort-style amenities, which include a riverside pool deck with cabanas, hot tub, and grilling station. There is also a state-of-the-art fitness center, a spa treatment room, a clubroom with billiards, and a rooftop lounge with a fireplace.
Pet-Friendly: The complex is pet-friendly and includes a dog walk area.
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This sexy bra is designed by :: ANTAYA :: and called :: ANTAYA :: Coral bra. The hud offers 18 color options and 6 pearl options. It's rigged for Maitreya, Perky, Reborn and Legacy. You will find this at the :: ANTAYA :: mainstore: maps.secondlife.com/secondlife/Veles/215/147/21
The next item is this really super cool necklace designed by SFU called SFU - Hecate Slip Chain. It's original mesh with a texture hud for 9 metals. It has a scripted option for Peanut, Whim. Rigged for eBODY Reborn, LaraX, and Legacy Female. Available at the Uber event! Here is your ride: maps.secondlife.com/secondlife/Uber/87/202/22
Lastly but certainly not least is this amazing sexy pose designed by TOUCH MIA called TOUCH MIA - Pin-Up Girl - Legs. This is a set that includes 6 poses with mirror options and a bonus pose. This is available In-World & on Marketplace! maps.secondlife.com/secondlife/Arbor%20Lake/117/86/2223 and
marketplace.secondlife.com/stores/93006
Bon Jovi - Bad Medicine
www.youtube.com/watch?v=eOUtsybozjg
Your love is like bad medicine
Bad medicine is what I need
Oh-oh-oh, shake it up, just like bad medicine
There ain't no doctor that can cure my disease
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:: ANTAYA ::
:: ANTAYA :: Coral bra
Available at the :: ANTAYA :: mainstore: maps.secondlife.com/secondlife/Veles/215/147/21
More information about :: ANTAYA :: :
FLICKR
www.flickr.com/groups/antaya-store/
MP: marketplace.secondlife.com/stores/53899
MAINSTORE: maps.secondlife.com/secondlife/Veles/215/147/21
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SFU - Six Feet Under
SFU - Hecate Slip Chain
Available at the Uber event! Here is your ride: maps.secondlife.com/secondlife/Uber/87/202/22
More information about Six Feet Under:
Flickr: www.flickr.com/photos/xmayze/
Flickr Group: www.flickr.com/groups/sixfeetunder/
Facebook: www.facebook.com/sixfeetundersl/
Instagram: www.instagram.com/sl.sixfeetunder/
Marketplace: marketplace.secondlife.com/stores/45890
In World Store: maps.secondlife.com/secondlife/Indian%20Paradise/38/164/22
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TOUCH MIA
TOUCH MIA - Pin-Up Girl - Legs
Available at the TOUCH MIA store: maps.secondlife.com/secondlife/Kindred%20Soul/192/196/3501
More information about the TOUCH MIA Store:
Mainstore: maps.secondlife.com/secondlife/Arbor%20Lake/117/86/2223
Flickr: www.flickr.com/groups/touchmia-slstore/
www.flickr.com/photos/196350343@N06/
MP: marketplace.secondlife.com/stores/93006
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Other information, items/accessories in picture:
HAIR
S-CLUB UMA FATPACK HAIR
JEWELRY
RAWR! Regina Set
UNHOLY REGAL EARRINGS
ACCESSORIES
cinphul // salacia [crown]
Void - Flutter Lashes
Violent Seduction - Madame Chungking Stole (Black)
AURORA Haneul Stockings
NAILS
Pure Poison - Diamond French Nails
TATTOO
.:Vegas:. Tattoo
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Odda is a town and administrative center in Ullensvang municipality in Vestland county in Norway. The town is located deep in the Sørfjorden in Hardanger , and has 4,764 inhabitants as of 1 January 2023 . Odda was the administrative center of Odda municipality , which on 1 January 2020 was merged with Jondal and Ullensvang to form the new Ullensvang municipality.
In 2009 , the industrial heritage in Odda-Tyssedal was listed on Norway's tentative list for UNESCO's World Heritage List , together with the Rjukan–Notodden industrial heritage .
Public services
Odda hospital is a local hospital for the municipalities of Eidfjord, Jondal, Odda and Ullensvang.
Odda secondary school offers both vocational and study specialist educations.
Business
Odda is known as an industrial location, with companies such as Odda Smelteverk , Boliden Odda (formerly Norzink ) and Tinfos Titan & Iron (TTI).
History
Tourism and hotel management
Before industrial activity in Odda began around 1910, Odda was a popular tourist destination which, among other things, attracted many foreigners who wanted to experience the scenic area with glaciers, fjords and waterfalls. This laid the foundation for several people to start hotel operations on the site.
Some of the most popular destinations for tourists visiting Odda were Låtefossen and Espelandsfossen .
Shuttle station, steamship wharf and steamship expedition
Baard Jakobsen Aga (1812–1895) received a merchant license in Odda in 1861, and in 1864 took over the shuttle station that was in operation in Odda. Then he secured a new plot of land where he built a hotel which was called alternately Prestegårds Hotel and Agas Hotel. In 1868 he became a post opener and steamship dispatcher, and he then had a steamship wharf and dispatch house built at Almerket. He had previously expanded the hotel business, but in 1888 he inaugurated a new hotel building, the "new Agas Hotel". In the 20th century, the large hotel building was used for other purposes, including Rita's bakery, which led to the building being called "Ritagården" colloquially. Agas Hotel/Ritagården was demolished in 1978.
From guest house to Hotel Hardanger
The start of hotel operations at Odda occurred around 1845, when a man named Monsen started an inn on the site. Monsen went bankrupt in the 1860s, and the inn was bought by a man named Wetshus. He continued to run the hotel business. After Wetshus had died, the two brothers Sven and Mikal Tollefsen became his successors in the early 1880s, with financial support from a rich Englishman. The Tollefsen brothers carried out a major renovation of the former guest house. When Sven Tollefsen died, Mikal Tollefsen became the hotel's sole owner.
Tollefsen also bought Agas Hotel, which Baard Jakobsen Aga had started.
On 9 August 1895, the then Hotel Hardanger was completely damaged in a fire. The fire started in Hotel Hardanger, but 7–8 neighboring buildings also caught fire. It was said that the fire was caused by the maid of an English hotel guest having left a candle or a kerosene lamp by an open window, and that the curtain had caught fire - as it was very hot most of the windows in the hotel were open, and this caused the fire to spread with great speed. The fire started at 12 o'clock in the morning.
The commander and crew of the steamship "Vega" - which happened to be docked in Odda when the fire started - managed to put out the fire(s) within three hours using fire-fighting equipment from the ship. Among other things, they managed to save the post office, while the telegraph building was lost. The competing Jordals Hotel, which was run by Jacob Jordal, was also saved.
Hotel Hardanger was insured, and Bergens Tidende wrote that the insurance sum was NOK 90,000, but also published an anonymous source's assessment that the hotel complex was worth NOK 200,000–250,000, and that the owner - Mikal Tollefsen - had probably suffered a significant financial loss due to underinsurance. No people were injured in the fire.
Shortly after the fire in 1895, Tollefsen started building a new and larger hotel on the site of the fire. The new hotel was completed on 24 June 1896, and had 170 hotel beds in 110 guest rooms. Architecturally, it was a mixture of Swiss style and dragon style, with towers and projections.
Hardanger Hotel is mentioned, among other things, in a French travelogue published in 1897.
In 1913, the owner of Hotel Hardanger filed a claim for damages against the two factories - a cyanamide factory and a carbide factory - which had started up in Odda a few years earlier, because the factory operation caused such great pollution and bad odors that it affected the hotel operation. The provisions of the Neighborhood Act were the legal basis for the lawsuit. The court agreed with the plaintiff that the two factories were obliged to pay compensation for inconvenience and losses that the hotel had suffered after 2 August 1911, but not because Odda had become less idyllic and thus attractive to tourists. The compensation sum was to be determined after an appraisal had been carried out , and the result of the appraisal was not available until 1922. By then both factories had gone bankrupt, and hotel owner Mikal Tollefsen had died.
Hotel Hardanger becomes a town hall
In 1917, the municipality bought the Hotel Hardanger, to convert the building into a town hall . The hotel had then been almost empty all year round, because the industrial activity on the site had meant that the tourists did not show up. [9]
The hotel's so-called "Kongerom" was converted into a chairman's office and lord's boardroom. Eventually, the new town hall also accommodated a number of other businesses, such as a cinema, police station, doctor's office and bank. The old hotel was in use as Odda Town Hall until a new building was inaugurated in 1957; from then on, the former Hotel Hardanger was referred to as Odda old town hall . This building was demolished in 1976.
Jordals Hotel becomes Hardanger Hotel
In 1917, Jordals Hotel was bought by the Melkeraaen family, who continued to run the hotel for 68 years. Along the way, they changed the name of the hotel to Hardanger Hotel.
The Hardanger Hotel, which was a wooden Swiss-style building, was demolished in 1962, and a new five-story hotel building was inaugurated on 1 July 1963.
From tourism to industrial site
Factories and smelters
At the beginning of the 20th century, two factories were started in Odda. On one, cyanamide was produced, and on the other, carbide was produced .
In 1908, the operation of the first factory that was to be part of Odda Smelteverk , a carbide factory owned by a British company, began. In 1909, another British company started production of calcium cyanamide in the same area as the first factory. The reason why Odda was interesting for the foreign companies was the access to large amounts of hydropower and ice-free ports.
Both factories went bankrupt in 1921 , in connection with the worldwide economic crisis that occurred in the early 1920s. The bankruptcies led to thousands of people becoming unemployed. Both factories started up again in 1924, with Odda Smelteverk A/S as the new owner. This operating company was established by the power company Tyssefaldene and the Hafslund/Meraker group.
The cyanamide factory was built on in the 1930s.
At the smelter, the so-called Odda process was developed by chief chemist Erling Johnson in 1927–1928; it is a chemical process based on nitric acid for the industrial production of three-sided artificial fertilizer with the sub-components nitrogen , phosphorus and potassium .
Preservation decision and dispute over conservation value
In 2011 , the National Archives decided to protect several of the smelter's buildings and facilities, and to include the smelter in the Norwegian application to UNESCO for world heritage status for Norwegian industrial monuments. In 2013, however, the Ministry of the Environment decided that the series nomination should be split into two phases, 1. application for Rjukan/Notodden to be submitted to UNESCO in January 2014, and phase 2, that work be continued on expanding the nomination to include Odda/ Tyssedal with eventual submission to UNESCO in January 2016.
The owners of the smelter site objected to the conservation decision made in 2011, but the decision was upheld in 2012. The conservation included the cyanamide factory, the cable car, the Linde house (named after the German inventor Carl von Linde ) and the limestone silo on the import quay. Over the years, there has been much controversy in Odda about whether the smelter's buildings and facilities should be preserved or removed.
Cultural life
Music and theater
Tyssedalkoret and Odda Songlag are two choirs that come from Odda municipality. The water power and industrial history of the area here was documented in the performance and the DVD ``Arven'', performed by Tyssedalkoret with band and soloists in autumn 2004 and released on DVD in Christmas 2005. In addition these two choirs have the bands Odda Musikklag , Odda Skolekorps and Røldal Skolemusiklag. The blues team Lokst Utøve has 272 members. The Blueslaget received the culture award for 2009 for their great work as concert/festival organisers, volunteer workers and inspirers for bands and soloists. In 2011, Erlend Garatun Huus published the book Rock og Røyk , which is about the history of rock in Odda.
At the closed smelter (2001), the old "Lindehuset" has been used for theater and concert activities. The theater play Bikebubesong , based on the Oddingen Frode Grytten's novel Bikubesong , was performed in this venue in 2003 with great success. The play's performance in Oslo has been the most watched contemporary drama in Norwegian history.
A key cultural player in Odda is the company Oddakonsertene, led by Gunn Gravdal Elton. In April 2019, the Odda concerts staged the musical Albert og Leonie , a story about how Odda arose as an industrial community. The musical was a huge success with sold-out houses. 2,600 people queued to see and hear the story. The director was Martine Bakken Lundberg. The main roles were played by André Søfteland and Lene Kokai Flage. Over 60 amateurs were on stage. Albert and Leonie was planned to be staged again in 2020 and 2021, but had to be canceled due to the corona pandemic .
The odd concerts started in 2005 and as of 2019 have staged more than 60 concerts. All have been sold out. The most popular concerts are the annual Christmas concerts, which gather over 1,000 listeners. The traditional Christmas concert in Odda church with a large ensemble and two to three concerts in a row officially ended in 2019, but a simplified version was arranged in 2020, with concerts in Skare and Odda churches.
The Literature Symposium
From 2005, a festival called the Literature Symposium in Odda has been organized every autumn . The Linden house at the defunct Smelteverket, Odda cinema, Sentralbadet, Odda church are some of the venues at the symposium. Previously, there was every year "Bikubegang" with Frode Grytten , where he told about the story behind the book "Bikubesong", while he wandered around Odda. The literary symposium also has concerts, often in connection with an author/musician or individual artists. During the Literary Symposium 2011, the Sentralbadet Litteraturhus opened in the old bathroom at the closed Smelteverket, and this has become headquarters for the symposium, as well as a permanent house for literary events all year round.
As of 2010, a major rehabilitation/remodeling of Lindehuset was planned, so that the building would be better suited for events such as concerts and theater performances.
The National Antiquities' "Value creation project"
Odda is one of the pilot projects in the Value Creation Project for the National Archives.
TV shows
The actions in the TV series RIP Henry and Ragnarok have been added to Odda, and are recorded there. In Ragnarok, on the other hand, the city goes by the name Edda .
Known oddities
Samson Isberg (1795–1873), sharpshooter
Knud Knudsen (photographer) (1832–1915)
Gro Holm , born Prestgarden (1878–1949), writer
Alfred Hagn (1882–1958), painter, writer and spy.
Claes Gill (1910–1973), writer, actor and theater manager
Torbjørn Mork (1928–1992), doctor, politician ( Ap ), director of health 1972–1992
Walther Aas (1928–1990), artist
Roger Albertsen , (1957–2003), footballer
Anne B. Ragde (born 1957), writer, (raised in Trondheim)
Arne Borgstrøm (born 1959), elite long-distance swimmer
Frode Grytten (born 1960), author
Lars Ove Seljestad (born 1961), author
Bjørn Ingvaldsen (born 1962), author, leader of Norwegian Children's and Young People's Book Writers
Hallgeir Opedal (born 1965), writer and journalist
Børge Brende (born 1965), politician ( H ), former secretary general of the Norwegian Red Cross , minister of foreign affairs
Ida Melbo Øystese (born 1968), chief of police in Oslo from 2023.
Knut Olav Åmås (born 1968), author, editor, director of the foundation Fritt Ord
Leif Einar Lothe (born 1969), entrepreneur, singer, TV profile
Marit Eikemo (born 1971), writer
Tore Aurstad (born 1972), author
Ingvill Måkestad Bovim (born 1981), athlete
Håkon Opdal (born 1982), footballer
Ingvild Skare Thygesen (born 1993), TV profile
The Sognefjord is Norway's longest and deepest fjord with its 205 km and 1303 m at its deepest (SNL states 1308), including Sognesjøen which is at the far end towards the North Sea. The Sognefjord has the deepest point on Norway's coast. The fjord is 176–180 km from the innermost Lusterfjorden ( Skjolden ) to Sognefest , and 206 km to the outermost reef (then Lake Sognesjøen is also included). The width varies from around 1 to 2 km in Lusterfjorden to 4–5 km from Leikanger and beyond. Measured from the threshold to Skjolden, the fjord is 174 km. The middle part of the fjord is surrounded by mountains of around 1000 meters and in the inner part the height difference between the bottom of the fjord and the mountain tops is 3500 metres. The highest peak right by the fjord is Bleia at 1,721 metres, which gives a 2,850 meter height difference. Around the inner part of the fjord, the landscape is alpine with pointed mountain peaks, steep mountain sides and glaciers. As an extension of the fjord arms, long and deep valleys extend in all directions, including Jostedalen , Lærdalen and Årdal with Utladalen . The Sognefjord is the world's longest open (ice-free) fjord. The Sognefjord is the world's third longest fjord.
It is located in the middle of Vestland county (formerly Sogn og Fjordane county to which it helped give its name) and stretches from Solund on the coast in the west to Skjolden at the foot of Jotunheimen in the east (northeast), where the fjord arm is called Lustrafjorden . The fjord and the land around it make up the Sogn region, often divided into Outer, Midtre and Indre Sogn. The length from Rutletangen to Skjolden is 186 km . Sogn makes up almost 60% of the area in Sogn and Fjordane, or around 11,000 km 2 . The twelve municipalities in Sogn have a total area of 10,671.55 km² and 37,063 inhabitants (1 January 2014). The land around the inner part of the fjord is called Indre Sogn and includes the long fjord arms. From Leikanger onwards, the country is called Ytre Sogn . The outer part of the fjord has few and small fjord arms. The fjord arms are like hanging valleys under water in that the bottom in the side fjords is often much shallower than the main fjord with a height difference of over 1,000 meters in some cases. The main fjord has a threshold at its mouth to the sea, while several of the side fjords have thresholds at the mouth of the main fjord.
The Sognefjord cuts so deeply into the country that it is only 15 km from the innermost arm at Skjolden to mountain peaks such as Store Skagastølstind in Jotunheimen. The water flow usually exits the fjord. The rivers create sandbanks where they run into the fjord, for example at Gudvangen, in Lærdal and in Gaupne. These sandbars are constantly expanding and changing shape.
The Sognefjord, especially the inner part, is surrounded by mountain massifs which are alpine in the inner part and more rounded in the outer part. The innermost arms of the fjord continue as deep and sometimes long valleys, including Lærdal , Årdal with Utladalen , Nærøydalen , Sogndalsdalen , Fjærland , Fortunsdalen , Aurlandsdalen and Jostedalen . The transition between the fjord and these valleys is determined by sea level, and the boundary has moved outwards at the uplift. Some of the side valleys, such as Vik and Fresvik, would have been hanging valleys in the same way as the Feigedalen if the Sognefjord was drained.
Name
Amund Helland writes " The Sognefjord's real name is Sogn , while Sogn is now used only for the surrounding landscape, and was thus already used in the Middle Ages. As a landscape name, the name is a masculine word and has undoubtedly been so as a fjord name as well." The name is connected to the word "suction", which probably refers to the suction or the difficult current conditions that are created when the water flows through the fjord mouth and over the threshold.
Geography
Large parts of the fjord are surrounded by steep mountains. Kvamsøy at Balestrand is a small island separated from the mainland by a short, shallow strait. Outside Balestrand there are small fjord arms and at Veganes ( Dragsvik ferry quay ) there is a significant branching with the Fjærlandsfjorden .
Municipalities
Municipalities with shoreline to the fjord, counted from west to east:
Solund
Hyllestad (north side)
Gulen (south side)
Høyanger (on both sides of the main fjord)
Vik (south side)
Sogndal (north side)
Aurland (south side, around the Aurlandsfjord)
Lærdal (south side)
Luster (north side, around Lustrafjorden)
Årdal (around the Årdalsfjord)
Depths
The Sognefjord has only one threshold which is at the mouth and the threshold is around 165 meters deep. The area beyond the threshold is called Sognesjøen , which is sheltered by islands to the north and south; there is no threshold outside Sognesjøen that has free circulation towards the ocean.
From the inner parts at Årdal or Skjolden, the fjord gradually deepens outwards (westwards). Between Fodnes-Mannheller and Rutledal-Rysjedalsvika, the bottom is at least 800 metres. The deepest part is approximately at Åkrestrand and Vadheim. The outer part of the fjord (at Losna and Sula ) has a marked threshold with depths of 100 to 200 metres, where the fjord bed rises abruptly from a depth of 1,200 meters to around 100 meters over a stretch of 5 km at Rutledal. In Lake Sognesjøen there are several small troughs (with depths down to 400-500 metres) with thresholds between them. Across the fjord, the bottom is partly completely flat with less than 1 meter variation in depth over a 2 km cross-section. The bottom is covered by fine material (clay) which at Vangsnes is up to 300 meters thick. Seismic shows that the greatest depth to the bedrock is approximately 1,600 m, but loose masses with a thickness of 200–400 m mean that the fjord bottom is nevertheless flat. Seismic surveys at Vangsnes have revealed a 300 meter thick layer of clay at the bottom.
Between 50 and 180 km from the mouth, the fjord bed is relatively flat. Almost all side fjords form hanging valleys to the main fjord. For example, the mouth of the Fjærlandsfjord is well over 400 meters deep, while the main fjord is close to 1,200 meters deep just outside the mouth. Vadheimfjord's mouth is 400 meters deep, here the greatest depth is over 1300 m. Ikjefjord's mouth is only 50 meters deep close to where the main fjord is at its deepest. In large parts of the fjord, it is "abruptly deep" in that the steep mountain sides continue just as steeply underwater.
In contrast to a number of other fjords, not every single part of the Sognefjord has its own name. Only the outermost part has its own name - Sognesjøen . However, there are many fjord arms. From west to east these are:
Sognesjøen
Straumsfjorden
Bjørnefjorden
Nessefjord
The Sognefjord
Lifjorden
Bøfjorden
The Risnefjord
The Ikjefjord
Vadheimsfjorden
Fuglsetfjorden
Høyangsfjorden
Lånefjorden
The Finnafjord
The Arnafjord
The Inner Fjord
Framfjorden
Vikbukti
The Esefjord
Fjærlandsfjorden
The Vetlefjord
Sværefjorden
The Norafjord
Sogndalsfjorden
Barsnes Fjord
The Eidsfjord
Aurlandsfjorden
The Nærøyfjord
Amla Bay
Lærdalsfjorden
Årdalsfjorden
The Lustrafjord
The Gaupnefjord
Climate and fresh water
The fjord colored by meltwater from the glacier.
Terrain formations and distance to the sea lead to great variations in climate along the fjord. The outer part has a mild and humid coastal climate, while the innermost part has an inland climate with cold and dry winters.
The amount of precipitation decreases strongly inwards into the fjord. Lærdal lies in the rain shadow and has very little rainfall, while west-facing slopes further out have a lot of rainfall and there the rainfall often increases with altitude. Brekke and Takle in Ytre Parish are among the places in Norway with the most rainfall. North of the Sognefjord lies the Jostedalsbreen, Norway's largest glacier, and parts of the meltwater drain into the Sognefjord. Wind conditions are strongly influenced by terrain formations. In winter, the dominant wind direction is out the fjord or out the side valleys in the form of so-called downwinds . Fall winds can be very strong and have a major impact on cooling and icing. The slopes and valleys along the inner parts of the fjord have a partially mild climate and are fertile, which makes the area suitable for growing fruit and berries, among other things. The slopes along the fjord partly have large conifer forests, including in the roadless area of Frønningen .
The fjord receives fresh water mainly from the rivers and very little precipitation directly on the fjord's water surface. In the inner part of the Sognefjord, the total supply of fresh water during one year corresponds to a depth of 33 meters if it were distributed over the entire area of the fjord. In spring and partly in autumn, the top 2-3 meters of the fjord are brackish water , especially in the side fjords. The salt content in the surface is lowest in summer and autumn. In June 1954, for example, 5 ‰ salt was measured in the uppermost meters of the Lustrafjord, while at great depths it was 34.5 ‰. Regulation of the waterways for power production has led to a larger proportion of fresh water flowing into the fjord in the winter. The most extensive regulation is in Aurland, Lærdal, Årdal and Jostedal. Regulations affect temperature in the surface layer and icing. In the inner part of the fjord, the rivers are fed by high mountains and glaciers.
The rivers Lærdalselvi , Aurlandselvi , Flåmselvi , Mørkridselvi , Henjaelvi , Grindselvi , Hamreelvi , Njøsaelvi , Kvinnafossen , Sogndalselvi and Jostedøla flow into the Sognefjord and normally have spring floods in June. [3] Lærdalselva has the largest catchment, followed by Jostedøla and Aurlandselva, and these three have roughly the same water flow (around 40 m 3 /second). The Årdalsvatnet drains to the Sognefjord through the short Åreidselva or Hæreidselvi through the Årdalstangen . The Eidsvatnet in Luster drains into the Sognefjord just by Mørkridselvi in Skjolden . Regulation of the waterways for hydropower has resulted in a more steady supply of fresh water throughout the year. Without regulation, 92% of the fresh water would have been supplied in the summer half-year from May to October. Several of the large rivers flow into fjord arms.
Geology
The bedrock along the outer and middle part of the fjord consists mostly of Precambrian gneiss with orientation east-west and northeast-southwest. The islands of Solund consist mostly of Devonian sandstone and conglomerates , while the interior (eastern part) consists mostly of Caledonian gabbro , anorthosite , granite and phyllite .
Jostedøla's material transport (in the form of sludge) involves sedimentation in the Gaupnefjord of 10 to 20 cm/year near the river basin, and 1 cm/year 2 km from the river basin. The river transports 50,000 to 100,000 tonnes of silt annually. The sludge concentration from Jostedøla is at most 1 g/litre. It is particularly at Gaupne that the meltwater from the glaciers is marked by the color of the water.
Icing
According to Helland, it was common for the ice to settle on several of the fjord arms every winter, including on Aurlandsfjorden, Nærøyfjorden and Årdalsfjorden. In the winter of 1888–1889, Lusterfjorden was iced over for six months straight. In the deepest parts of the Sognefjord, there is a year-round temperature of around 6.5 °C, according to Helland. Outer parts are almost never iced over, not even the side fjords. The inner parts can be frozen for several weeks at a stretch. Among other things, inner parts of the Aurlandsfjorden and the Nærøyfjorden freeze easily. Lærdalsfjorden is usually ice-free except for the very innermost part, while it has happened that Årdalsfjorden has been iced up to Ofredal and has been an obstacle to ship traffic. Historically, Lustrafjorden has often been iced over as far as Urnes. The Barsnesfjorden has often been covered with ice. In the Nærøyfjord it happened (among other things in the 1920s and in 1962) that the liner was unable to enter the fjord due to ice and had to dispatch at the ice edge.
Streams
In the Sognefjord, incoming current is hardly noticeable and is most noticeable in strong westerly winds. Outgoing current dominates and is particularly strong in spring and summer. At strong tides, the tidal flow can reach over 1 m/s (2 knots ) around the pier and headland. The Sognefjord is covered by a layer or stream of brackish water of up to 10 meters (varying with the seasons and supply from the rivers). Beneath the brackish water, a current or intermediate layer at a depth of 150 meters goes in and out of the fjord and below this lies the main basin, which has some connection with the ocean beyond the threshold. Together, these three currents contribute to the fact that the water in the fjord is replaced on average within 8-10 years, so that the fjord has life right down to the bottom. The brackish water layer has less density and therefore does not mix easily with the deeper layers. The brackish water that flows out of the fjord slowly mixes with the layer below so that the salt content increases at the same time as the brackish water layer increases up to 10 times the amount of fresh water supplied. The brackish water that flows towards the mouth must be replaced and sets up an incoming current in a slightly deeper layer.
Fish
The Sognefjord has herring and good sprat fishing . In the outer parts of the fjord, salmon has traditionally been fished with wedge nets . Salmon warp or "sitjenet" is a traditional method of salmon fishing and skilled players could catch a lot of fish with this method. Hook nets and drift nets have dominated in modern times and do not require the same active fishing as warp . The salmon's migration in the fjord is controlled by currents on the surface and the warps are placed where there are favorable current conditions where, due to the current, the salmon are driven close to land on their way into the fjord. In Leikanger and Balestrand there are many good places for sitejnot with Suppham being by far the best. Good salmon rivers such as Lærdalselva, Aurlandselva and Årøyelva flow into the Sognefjorden.
In the outer part of the fjord (Gulen and Solund) there is some fish farming. Several of the waterways are known for good salmon and sea trout fishing , and five of the rivers have been designated as national salmon rivers. Lærdalselva has a salmon-carrying stretch and has had by far the largest population. Aurlandselva has historically had a good catch of sea trout. The Sognefjord is among the most important in Norway for anadromous fish species. Norwegian spring-spawning herring are fished in the fjord, especially in the outer parts, as well as some coastal sprat.
In the Sognefjord there are plankton algae which in other Norwegian waters and the occurrence follows the seasons. In general, there is little occurrence in winter due to low light, diatoms bloom in March-April and are dependent on the supply of nutrient salts, in May-June diatoms and flagellates bloom in connection with the spring flood, in summer there is a varying population, new blooms in the autumn in connection with, among other things, floods, and married species can occur all year round.
Tourism
The Sognefjord was established as a tourist destination in the 19th century, among other things, with the establishment of Fylkesbåtane. One of the targets was Gudvangen, which in 1889 received 79 large tourist ships with a total of over 10,000 passengers. In 1889, 4,500 travelers came with the county boats. The German Emperor Wilhelm visited the Sognefjord and Balestrand for the first time in 1890. The emperor subsequently visited the Sognefjord 25 times. The fjord itself and the surrounding area with Jotunheimen, Jostedalsbreen and several stave churches have made the Sognefjord one of Norway's most prominent tourist destinations. Balestrand, Vangsnes, Aurland and Fjærland were among the early destinations for English tourists in the 19th century.
History
It has been the Guest of Death
It has sailed on a Torden
It is christened in Rædsler vorden
that has plowed the Sognefjord
from Forthun to Sognefæst.
If you have forgotten your Lord's Prayer,
do you remember a prayer to pray:
learn it from the wrath of God!
imagine, Sinder, then present
in a Bath on Sognefjord!
Henrik Wergeland
The Sognefjord has been an important transport artery since ancient times. The gulation was probably held near the mouth of the Sognefjord and probably because it was practical to hold the meeting where the ship lay along the coast met the great fjord. From the innermost arms of the fjord it is a relatively short distance to the inland villages of Eastern Norway, particularly through Lærdal to Valdres over the moderate mountain pass Filefjell . Lærdalsøyri was from the 17th century an important market and meeting place. There, farmers from Valdres, Hallingdal and Gudbrandsdalen sold slaughter, tar and other products from the interior and bought fish, salt, hemp and iron from the fjords and from Bergen. Around 1300, the authorities established a shuttle station at Maristova at the entrance to Filefjell. The first drivable road between east and west was built over Filefjell in 1792. From 1843 the paddle steamer "Constitutionen" plyed the route between Bergen and Lærdal, the county boats took over the route in 1857. The road over the Sognefjellet was built as a carriageway in 1938. The Flåmsbana connected the Sognefjord to the railway network in 1940. Stalheimskleivi , between Voss and Sogn, was built in 1850 and turned into a road in 1937. It has made it possible to transport agricultural products , fruit , berries and fish between the villages in Sogn and Bergen .
From 1785, the Trondhjem postal route crossed the Sognefjord by boat between Rutledal and Leirvik in Hyllestad . In 1647, a postal route was established between Bergen and Christiania. The post then took 7-8 days via Gudvangen, Lærdal and Valdres.
It was difficult to get to the Sognefjord by sailboat and the yachts could lie for many days or several weeks at the mouth waiting for favorable wind conditions. East wind was favorable out of the fjord, while south to Bergen, wind from the north or north-west was needed. To enter the fjord, a wind from the west was necessary. The steam and motor boats revolutionized transport on the fjord and these had completely taken over in the early 20th century The county boats were established in 1858 with boat routes on the Sognefjord and to Bergen as an important activity.
In 1934, a ferry route was established along the fjord from Vadheim to Lærdal. From 1939 until the Lærdal tunnel opened, there was a car ferry between Gudvangen and Lærdal - first the ferry went to Lærdalsøyri itself, from 1966 to Revsnes when a road was built there to shorten the ferry route. In the 1990s, the ferry connection Revsnes-Kaupanger was replaced by Mannheller-Fodnes , and after this Kaupanger has only been used by the tourist route Gudvangen-Kaupanger-Lærdal. The road system between Sogndal and Jølster on national highway 5 , including the Fjærlands tunnel , created a ferry-free road connection on the north side of the fjord.
Norway , officially the Kingdom of Norway , is a Nordic , European country and an independent state in the west of the Scandinavian Peninsula . Geographically speaking, the country is long and narrow, and on the elongated coast towards the North Atlantic are Norway's well-known fjords . The Kingdom of Norway includes the main country (the mainland with adjacent islands within the baseline ), Jan Mayen and Svalbard . With these two Arctic areas, Norway covers a land area of 385,000 km² and has a population of approximately 5.5 million (2023). Mainland Norway borders Sweden in the east , Finland and Russia in the northeast .
Norway is a parliamentary democracy and constitutional monarchy , where Harald V has been king and head of state since 1991 , and Jonas Gahr Støre ( Ap ) has been prime minister since 2021 . Norway is a unitary state , with two administrative levels below the state: counties and municipalities . The Sami part of the population has, through the Sami Parliament and the Finnmark Act , to a certain extent self-government and influence over traditionally Sami areas. Although Norway has rejected membership of the European Union through two referendums , through the EEA Agreement Norway has close ties with the Union, and through NATO with the United States . Norway is a significant contributor to the United Nations (UN), and has participated with soldiers in several foreign operations mandated by the UN. Norway is among the states that have participated from the founding of the UN , NATO , the Council of Europe , the OSCE and the Nordic Council , and in addition to these is a member of the EEA , the World Trade Organization , the Organization for Economic Co-operation and Development and is part of the Schengen area .
Norway is rich in many natural resources such as oil , gas , minerals , timber , seafood , fresh water and hydropower . Since the beginning of the 20th century, these natural conditions have given the country the opportunity for an increase in wealth that few other countries can now enjoy, and Norwegians have the second highest average income in the world, measured in GDP per capita, as of 2022. The petroleum industry accounts for around 14% of Norway's gross domestic product as of 2018. Norway is the world's largest producer of oil and gas per capita outside the Middle East. However, the number of employees linked to this industry fell from approx. 232,000 in 2013 to 207,000 in 2015.
In Norway, these natural resources have been managed for socially beneficial purposes. The country maintains a welfare model in line with the other Nordic countries. Important service areas such as health and higher education are state-funded, and the country has an extensive welfare system for its citizens. Public expenditure in 2018 is approx. 50% of GDP, and the majority of these expenses are related to education, healthcare, social security and welfare. Since 2001 and until 2021, when the country took second place, the UN has ranked Norway as the world's best country to live in . From 2010, Norway is also ranked at the top of the EIU's democracy index . Norway ranks third on the UN's World Happiness Report for the years 2016–2018, behind Finland and Denmark , a report published in March 2019.
The majority of the population is Nordic. In the last couple of years, immigration has accounted for more than half of population growth. The five largest minority groups are Norwegian-Poles , Lithuanians , Norwegian-Swedes , Norwegian-Syrians including Syrian Kurds and Norwegian-Pakistani .
Norway's national day is 17 May, on this day in 1814 the Norwegian Constitution was dated and signed by the presidency of the National Assembly at Eidsvoll . It is stipulated in the law of 26 April 1947 that 17 May are national public holidays. The Sami national day is 6 February. "Yes, we love this country" is Norway's national anthem, the song was written in 1859 by Bjørnstjerne Bjørnson (1832–1910).
Norway's history of human settlement goes back at least 10,000 years, to the Late Paleolithic , the first period of the Stone Age . Archaeological finds of settlements along the entire Norwegian coast have so far been dated back to 10,400 before present (BP), the oldest find is today considered to be a settlement at Pauler in Brunlanes , Vestfold .
For a period these settlements were considered to be the remains of settlers from Doggerland , an area which today lies beneath the North Sea , but which was once a land bridge connecting today's British Isles with Danish Jutland . But the archaeologists who study the initial phase of the settlement in what is today Norway reckon that the first people who came here followed the coast along what is today Bohuslân. That they arrived in some form of boat is absolutely certain, and there is much evidence that they could easily move over large distances.
Since the last Ice Age, there has been continuous settlement in Norway. It cannot be ruled out that people lived in Norway during the interglacial period , but no trace of such a population or settlement has been found.
The Stone Age lasted a long time; half of the time that our country has been populated. There are no written accounts of what life was like back then. The knowledge we have has been painstakingly collected through investigations of places where people have stayed and left behind objects that we can understand have been processed by human hands. This field of knowledge is called archaeology . The archaeologists interpret their findings and the history of the surrounding landscape. In our country, the uplift after the Ice Age is fundamental. The history of the settlements at Pauler is no more than fifteen years old.
The Fosna culture settled parts of Norway sometime between 10,000–8,000 BC. (see Stone Age in Norway ). The dating of rock carvings is set to Neolithic times (in Norway between 4000 BC to 1700 BC) and show activities typical of hunters and gatherers .
Agriculture with livestock and arable farming was introduced in the Neolithic. Swad farming where the farmers move when the field does not produce the expected yield.
More permanent and persistent farm settlements developed in the Bronze Age (1700 BC to 500 BC) and the Iron Age . The earliest runes have been found on an arrowhead dated to around 200 BC. Many more inscriptions are dated to around 800, and a number of petty kingdoms developed during these centuries. In prehistoric times, there were no fixed national borders in the Nordic countries and Norway did not exist as a state. The population in Norway probably fell to year 0.
Events in this time period, the centuries before the year 1000, are glimpsed in written sources. Although the sagas were written down in the 13th century, many hundreds of years later, they provide a glimpse into what was already a distant past. The story of the fimbul winter gives us a historical picture of something that happened and which in our time, with the help of dendrochronology , can be interpreted as a natural disaster in the year 536, created by a volcanic eruption in El Salvador .
In the period between 800 and 1066 there was a significant expansion and it is referred to as the Viking Age . During this period, Norwegians, as Swedes and Danes also did, traveled abroad in longships with sails as explorers, traders, settlers and as Vikings (raiders and pirates ). By the middle of the 11th century, the Norwegian kingship had been firmly established, building its right as descendants of Harald Hårfagre and then as heirs of Olav the Holy . The Norwegian kings, and their subjects, now professed Christianity . In the time around Håkon Håkonsson , in the time after the civil war , there was a small renaissance in Norway with extensive literary activity and diplomatic activity with Europe. The black dew came to Norway in 1349 and killed around half of the population. The entire state apparatus and Norway then entered a period of decline.
Between 1396 and 1536, Norway was part of the Kalmar Union , and from 1536 until 1814 Norway had been reduced to a tributary part of Denmark , named as the Personal Union of Denmark-Norway . This staff union entered into an alliance with Napoléon Bonaparte with a war that brought bad times and famine in 1812 . In 1814, Denmark-Norway lost the Anglophone Wars , part of the Napoleonic Wars , and the Danish king was forced to cede Norway to the king of Sweden in the Treaty of Kiel on 14 January of that year. After a Norwegian attempt at independence, Norway was forced into a loose union with Sweden, but where Norway was allowed to create its own constitution, the Constitution of 1814 . In this period, Norwegian, romantic national feeling flourished, and the Norwegians tried to develop and establish their own national self-worth. The union with Sweden was broken in 1905 after it had been threatened with war, and Norway became an independent kingdom with its own monarch, Haakon VII .
Norway remained neutral during the First World War , and at the outbreak of the Second World War, Norway again declared itself neutral, but was invaded by National Socialist Germany on 9 April 1940 .
Norway became a member of the Western defense alliance NATO in 1949 . Two attempts to join the EU were voted down in referendums by small margins in 1972 and 1994 . Norway has been a close ally of the United States in the post-war period. Large discoveries of oil and natural gas in the North Sea at the end of the 1960s led to tremendous economic growth in the country, which is still ongoing. Traditional industries such as fishing are also part of Norway's economy.
Stone Age (before 1700 BC)
When most of the ice disappeared, vegetation spread over the landscape and due to a warm climate around 2000-3000 BC. the forest grew much taller than in modern times. Land uplift after the ice age led to a number of fjords becoming lakes and dry land. The first people probably came from the south along the coast of the Kattegat and overland into Finnmark from the east. The first people probably lived by gathering, hunting and trapping. A good number of Stone Age settlements have been found which show that such hunting and trapping people stayed for a long time in the same place or returned to the same place regularly. Large amounts of gnawed bones show that they lived on, among other things, reindeer, elk, small game and fish.
Flintstone was imported from Denmark and apart from small natural deposits along the southern coast, all flintstone in Norway is transported by people. At Espevær, greenstone was quarried for tools in the Stone Age, and greenstone tools from Espevær have been found over large parts of Western Norway. Around 2000-3000 BC the usual farm animals such as cows and sheep were introduced to Norway. Livestock probably meant a fundamental change in society in that part of the people had to be permanent residents or live a semi-nomadic life. Livestock farming may also have led to conflict with hunters.
The oldest traces of people in what is today Norway have been found at Pauler , a farm in Brunlanes in Larvik municipality in Vestfold . In 2007 and 2008, the farm has given its name to a number of Stone Age settlements that have been excavated and examined by archaeologists from the Cultural History Museum at UiO. The investigations have been carried out in connection with the new route for the E18 motorway west of Farris. The oldest settlement, located more than 127 m above sea level, is dated to be about 10,400 years old (uncalibrated, more than 11,000 years in real calendar years). From here, the ice sheet was perhaps visible when people settled here. This locality has been named Pauler I, and is today considered to be the oldest confirmed human traces in Norway to date. The place is in the mountains above the Pauler tunnel on the E18 between Larvik and Porsgrunn . The pioneer settlement is a term archaeologists have adopted for the oldest settlement. The archaeologists have speculated about where they came from, the first people in what is today Norway. It has been suggested that they could come by boat or perhaps across the ice from Doggerland or the North Sea, but there is now a large consensus that they came north along what is today the Bohuslän coast. The Fosna culture , the Komsa culture and the Nøstvet culture are the traditional terms for hunting cultures from the Stone Age. One thing is certain - getting to the water was something they mastered, the first people in our country. Therefore, within a short time they were able to use our entire long coast.
In the New Stone Age (4000 BC–1700 BC) there is a theory that a new people immigrated to the country, the so-called Stone Ax People . Rock carvings from this period show motifs from hunting and fishing , which were still important industries. From this period, a megalithic tomb has been found in Østfold .
It is uncertain whether there were organized societies or state-like associations in the Stone Age in Norway. Findings from settlements indicate that many lived together and that this was probably more than one family so that it was a slightly larger, organized herd.
Finnmark
In prehistoric times, animal husbandry and agriculture were of little economic importance in Finnmark. Livelihoods in Finnmark were mainly based on fish, gathering, hunting and trapping, and eventually domestic reindeer herding became widespread in the Middle Ages. Archaeological finds from the Stone Age have been referred to as the Komsa culture and comprise around 5,000 years of settlement. Finnmark probably got its first settlement around 8000 BC. It is believed that the coastal areas became ice-free 11,000 years BC and the fjord areas around 9,000 years BC. after which willows, grass, heather, birch and pine came into being. Finnmarksvidda was covered by pine forest around 6000 BC. After the Ice Age, the land rose around 80 meters in the inner fjord areas (Alta, Tana, Varanger). Due to ice melting in the polar region, the sea rose in the period 6400–3800 BC. and in areas with little land elevation, some settlements from the first part of the Stone Age were flooded. On Sørøya, the net sea level rise was 12 to 14 meters and many residential areas were flooded.
According to Bjørnar Olsen , there are many indications of a connection between the oldest settlement in Western Norway (the " Fosnakulturen ") and that in Finnmark, but it is uncertain in which direction the settlement took place. In the earliest part of the Stone Age, settlement in Finnmark was probably concentrated in the coastal areas, and these only reflected a lifestyle with great mobility and no permanent dwellings. The inner regions, such as Pasvik, were probably used seasonally. The archaeologically proven settlements from the Stone Age in inner Finnmark and Troms are linked to lakes and large watercourses. The oldest petroglyphs in Alta are usually dated to 4200 BC, that is, the Neolithic . Bjørnar Olsen believes that the oldest can be up to 2,000 years older than this.
From around 4000 BC a slow deforestation of Finnmark began and around 1800 BC the vegetation distribution was roughly the same as in modern times. The change in vegetation may have increased the distance between the reindeer's summer and winter grazing. The uplift continued slowly from around 4000 BC. at the same time as sea level rise stopped.
According to Gutorm Gjessing, the settlement in Finnmark and large parts of northern Norway in the Neolithic was semi-nomadic with movement between four seasonal settlements (following the pattern of life in Sami siida in historical times): On the outer coast in summer (fishing and seal catching) and inland in winter (hunting for reindeer, elk and bear). Povl Simonsen believed instead that the winter residence was in the inner fjord area in a village-like sod house settlement. Bjørnar Olsen believes that at the end of the Stone Age there was a relatively settled population along the coast, while inland there was less settlement and a more mobile lifestyle.
Bronze Age (1700 BC–500 BC)
Bronze was used for tools in Norway from around 1500 BC. Bronze is a mixture of tin and copper , and these metals were introduced because they were not mined in the country at the time. Bronze is believed to have been a relatively expensive material. The Bronze Age in Norway can be divided into two phases:
Early Bronze Age (1700–1100 BC)
Younger Bronze Age (1100–500 BC)
For the prehistoric (unwritten) era, there is limited knowledge about social conditions and possible state formations. From the Bronze Age, there are large burial mounds of stone piles along the coast of Vestfold and Agder, among others. It is likely that only chieftains or other great men could erect such grave monuments and there was probably some form of organized society linked to these. In the Bronze Age, society was more organized and stratified than in the Stone Age. Then a rich class of chieftains emerged who had close connections with southern Scandinavia. The settlements became more permanent and people adopted horses and ard . They acquired bronze status symbols, lived in longhouses and people were buried in large burial mounds . Petroglyphs from the Bronze Age indicate that humans practiced solar cultivation.
Finnmark
In the last millennium BC the climate became cooler and the pine forest disappears from the coast; pine forests, for example, were only found in the innermost part of the Altafjord, while the outer coast was almost treeless. Around the year 0, the limit for birch forest was south of Kirkenes. Animals with forest habitats (elk, bear and beaver) disappeared and the reindeer probably established their annual migration routes sometime at that time. In the period 1800–900 BC there were significantly more settlements in and utilization of the hinterland was particularly noticeable on Finnmarksvidda. From around 1800 BC until year 0 there was a significant increase in contact between Finnmark and areas in the east including Karelia (where metals were produced including copper) and central and eastern Russia. The youngest petroglyphs in Alta show far more boats than the earlier phases and the boats are reminiscent of types depicted in petroglyphs in southern Scandinavia. It is unclear what influence southern Scandinavian societies had as far north as Alta before the year 0. Many of the cultural features that are considered typical Sami in modern times were created or consolidated in the last millennium BC, this applies, among other things, to the custom of burying in brick chambers in stone urns. The Mortensnes burial ground may have been used for 2000 years until around 1600 AD.
Iron Age (c. 500 BC–c. 1050 AD)
The Einangsteinen is one of the oldest Norwegian runestones; it is from the 4th century
Simultaneous production of Vikings
Around 500 years BC the researchers reckon that the Bronze Age will be replaced by the Iron Age as iron takes over as the most important material for weapons and tools. Bronze, wood and stone were still used. Iron was cheaper than bronze, easier to work than flint , and could be used for many purposes; iron probably became common property. Iron could, among other things, be used to make solid and sharp axes which made it much easier to fell trees. In the Iron Age, gold and silver were also used partly for decoration and partly as means of payment. It is unknown which language was used in Norway before our era. From around the year 0 until around the year 800, everyone in Scandinavia (except the Sami) spoke Old Norse , a North Germanic language. Subsequently, several different languages developed in this area that were only partially mutually intelligible. The Iron Age is divided into several periods:
Early Iron Age
Pre-Roman Iron Age (c. 500 BC–c. 0)
Roman Iron Age (c. 0–c. AD 400)
Migration period (approx. 400–600). In the migration period (approx. 400–600), new peoples came to Norway, and ruins of fortress buildings etc. are interpreted as signs that there has been talk of a violent invasion.
Younger Iron Age
Merovingian period (500–800)
The Viking Age (793–1066)
Norwegian Vikings go on plundering expeditions and trade voyages around the coastal countries of Western Europe . Large groups of Norwegians emigrate to the British Isles , Iceland and Greenland . Harald Hårfagre starts a unification process of Norway late in the 8th century , which was completed by Harald Hardråde in the 1060s . The country was Christianized under the kings Olav Tryggvason , fell in the battle of Svolder ( 1000 ) and Olav Haraldsson (the saint), fell in the battle of Stiklestad in 1030 .
Sources of prehistoric times
Shrinking glaciers in the high mountains, including in Jotunheimen and Breheimen , have from around the year 2000 uncovered objects from the Viking Age and earlier. These are objects of organic material that have been preserved by the ice and that elsewhere in nature are broken down in a few months. The finds are getting older as the melting makes the archaeologists go deeper into the ice. About half of all archaeological discoveries on glaciers in the world are made in Oppland . In 2013, a 3,400-year-old shoe and a robe from the year 300 were found. Finds at Lomseggen in Lom published in 2020 revealed, among other things, well-preserved horseshoes used on a mountain pass. Many hundreds of items include preserved clothing, knives, whisks, mittens, leather shoes, wooden chests and horse equipment. A piece of cloth dated to the year 1000 has preserved its original colour. In 2014, a wooden ski from around the year 700 was found in Reinheimen . The ski is 172 cm long and 14 cm wide, with preserved binding of leather and wicker.
Pytheas from Massalia is the oldest known account of what was probably the coast of Norway, perhaps somewhere on the coast of Møre. Pytheas visited Britannia around 325 BC. and traveled further north to a country by the "Ice Sea". Pytheas described the short summer night and the midnight sun farther north. He wrote, among other things, that people there made a drink from grain and honey. Caesar wrote in his work about the Gallic campaign about the Germanic tribe Haruders. Other Roman sources around the year 0 mention the land of the Cimbri (Jutland) and the Cimbri headlands ( Skagen ) and that the sources stated that Cimbri and Charyds lived in this area. Some of these peoples may have immigrated to Norway and there become known as hordes (as in Hordaland). Sources from the Mediterranean area referred to the islands of Scandia, Scandinavia and Thule ("the outermost of all islands"). The Roman historian Tacitus wrote around the year 100 a work about Germania and mentioned the people of Scandia, the Sviones. Ptolemy wrote around the year 150 that the Kharudes (Hordes) lived further north than all the Cimbri, in the north lived the Finnoi (Finns or Sami) and in the south the Gutai (Goths). The Nordic countries and Norway were outside the Roman Empire , which dominated Europe at the time. The Gothic-born historian Jordanes wrote in the 5th century about 13 tribes or people groups in Norway, including raumaricii (probably Romerike ), ragnaricii ( Ranrike ) and finni or skretefinni (skrid finner or ski finner, i.e. Sami) as well as a number of unclear groups. Prokopios wrote at the same time about Thule north of the land of the Danes and Slavs, Thule was ten times as big as Britannia and the largest of all the islands. In Thule, the sun was up 40 days straight in the summer. After the migration period , southern Europeans' accounts of northern Europe became fuller and more reliable.
Settlement in prehistoric times
Norway has around 50,000 farms with their own names. Farm names have persisted for a long time, over 1000 years, perhaps as much as 2000 years. The name researchers have arranged different types of farm names chronologically, which provides a basis for determining when the place was used by people or received a permanent settlement. Uncompounded landscape names such as Haug, Eid, Vik and Berg are believed to be the oldest. Archaeological traces indicate that some areas have been inhabited earlier than assumed from the farm name. Burial mounds also indicate permanent settlement. For example, the burial ground at Svartelva in Løten was used from around the year 0 to the year 1000 when Christianity took over. The first farmers probably used large areas for inland and outland, and new farms were probably established based on some "mother farms". Names such as By (or Bø) show that it is an old place of residence. From the older Iron Age, names with -heim (a common Germanic word meaning place of residence) and -stad tell of settlement, while -vin and -land tell of the use of the place. Farm names in -heim are often found as -um , -eim or -em as in Lerum and Seim, there are often large farms in the center of the village. New farm names with -city and -country were also established in the Viking Age . The first farmers probably used the best areas. The largest burial grounds, the oldest archaeological finds and the oldest farm names are found where the arable land is richest and most spacious.
It is unclear whether the settlement expansion in Roman times, migrations and the Iron Age is due to immigration or internal development and population growth. Among other things, it is difficult to demonstrate where in Europe the immigrants have come from. The permanent residents had both fields (where grain was grown) and livestock that grazed in the open fields, but it is uncertain which of these was more important. Population growth from around the year 200 led to more utilization of open land, for example in the form of settlements in the mountains. During the migration period, it also seems that in parts of the country it became common to have cluster gardens or a form of village settlement.
Norwegian expansion northwards
From around the year 200, there was a certain migration by sea from Rogaland and Hordaland to Nordland and Sør-Troms. Those who moved settled down as a settled Iron Age population and became dominant over the original population which may have been Sami . The immigrant Norwegians, Bumen , farmed with livestock that were fed inside in the winter as well as some grain cultivation and fishing. The northern border of the Norwegians' settlement was originally at the Toppsundet near Harstad and around the year 500 there was a Norwegian settlement to Malangsgapet. That was as far north as it was possible to grow grain at the time. Malangen was considered the border between Hålogaland and Finnmork until around 1400 . Further into the Viking Age and the Middle Ages, there was immigration and settlement of Norwegian speakers along the coast north of Malangen. Around the year 800, Norwegians lived along the entire outer coast to Vannøy . The Norwegians partly copied Sami livelihoods such as whaling, fur hunting and reindeer husbandry. It was probably this area between Malangen and Vannøy that was Ottar from the Hålogaland area. In the Viking Age, there were also some Norwegian settlements further north and east. East of the North Cape are the scattered archaeological finds of Norwegian settlement in the Viking Age. There are Norwegian names for fjords and islands from the Viking Age, including fjord names with "-anger". Around the year 1050, there were Norwegian settlements on the outer coast of Western Finnmark. Traders and tax collectors traveled even further.
North of Malangen there were Norse farming settlements in the Iron Age. Malangen was considered Finnmark's western border until 1300. There are some archaeological traces of Norse activity around the coast from Tromsø to Kirkenes in the Viking Age. Around Tromsø, the research indicates a Norse/Sami mixed culture on the coast.
From the year 1100 and the next 200–300 years, there are no traces of Norwegian settlement north and east of Tromsø. It is uncertain whether this is due to depopulation, whether it is because the Norwegians further north were not Christianized or because there were no churches north of Lenvik or Tromsø . Norwegian settlement in the far north appears from sources from the 14th century. In the Hanseatic period , the settlement was developed into large areas specialized in commercial fishing, while earlier (in the Viking Age) there had been farms with a combination of fishing and agriculture. In 1307 , a fortress and the first church east of Tromsø were built in Vardø . Vardø became a small Norwegian town, while Vadsø remained Sami. Norwegian settlements and churches appeared along the outermost coast in the Middle Ages. After the Reformation, perhaps as a result of a decline in fish stocks or fish prices, there were Norwegian settlements in the inner fjord areas such as Lebesby in Laksefjord. Some fishing villages at the far end of the coast were abandoned for good. In the interior of Finnmark, there was no national border for a long time and Kautokeino and Karasjok were joint Norwegian-Swedish areas with strong Swedish influence. The border with Finland was established in 1751 and with Russia in 1826.
On a Swedish map from 1626, Norway's border is indicated at Malangen, while Sweden with this map showed a desire to control the Sami area which had been a common area.
The term Northern Norway only came into use at the end of the 19th century and administratively the area was referred to as Tromsø Diocese when Tromsø became a bishopric in 1840. There had been different designations previously: Hålogaland originally included only Helgeland and when Norse settlement spread north in the Viking Age and the Middle Ages, Hålogaland was used for the area north approximately to Malangen , while Finnmark or "Finnmarken", "the land of the Sami", lay outside. The term Northern Norway was coined at a cafe table in Kristiania in 1884 by members of the Nordlændingernes Forening and was first commonly used in the interwar period as it eventually supplanted "Hålogaland".
State formation
The battle in Hafrsfjord in the year 872 has long been regarded as the day when Norway became a kingdom. The year of the battle is uncertain (may have been 10-20 years later). The whole of Norway was not united in that battle: the process had begun earlier and continued a couple of hundred years later. This means that the geographical area became subject to a political authority and became a political unit. The geographical area was perceived as an area as it is known, among other things, from Ottar from Hålogaland's account for King Alfred of Wessex around the year 880. Ottar described "the land of the Norwegians" as very long and narrow, and it was narrowest in the far north. East of the wasteland in the south lay Sveoland and in the north lay Kvenaland in the east. When Ottar sailed south along the land from his home ( Malangen ) to Skiringssal, he always had Norway ("Nordveg") on his port side and the British Isles on his starboard side. The journey took a good month. Ottar perceived "Nordveg" as a geographical unit, but did not imply that it was a political unit. Ottar separated Norwegians from Swedes and Danes. It is unclear why Ottar perceived the population spread over such a large area as a whole. It is unclear whether Norway as a geographical term or Norwegians as the name of a ethnic group is the oldest. The Norwegians had a common language which in the centuries before Ottar did not differ much from the language of Denmark and Sweden.
According to Sverre Steen, it is unlikely that Harald Hårfagre was able to control this entire area as one kingdom. The saga of Harald was written 300 years later and at his death Norway was several smaller kingdoms. Harald probably controlled a larger area than anyone before him and at most Harald's kingdom probably included the coast from Trøndelag to Agder and Vestfold as well as parts of Viken . There were probably several smaller kingdoms of varying extent before Harald and some of these are reflected in traditional landscape names such as Ranrike and Ringerike . Landscape names of "-land" (Rogaland) and "-mark" (Hedmark) as well as names such as Agder and Sogn may have been political units before Harald.
According to Sverre Steen
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[HOOK]
My dear Prince and Princess
Your offer is meaningless
Don't give a damn 'bout your rank
The gold in your sack, well it isn't worth jack
I should make you fools go walk the plank
Your riches would fill other pirates with glee
But none of those pirates are me!
[PIRATES]
They're not he!
[HOOK]
Sing a yo ho, keep your jewels divine
[HOOK & PIRATES]
Yo ho
[HOOK]
And your manners refined
'Cause even more precious than rum in a stein is
Revenge, revenge, revenge, and it's gonna be mine!
[HOOK & PIRATES]
Revenge, revenge, revenge
[HOOK]
Is gonna be mine!
[SNOW WHITE, spoken]
Revenge? On whom?
[HOOK, spoken]
Just wait for the second verse, love.
[HOOK]
I've savaged and pillaged and pilfered each village
My conquests I'm justly proud of
[PIRATES]
He's proud of!
[HOOK]
Each town that I plunder, I leave torn asunder
A pirate's life is one to love
[PIRATES]
Lots to love!
[HOOK]
And yet my heart's hardened as hard as a rock
Won't rest 'til I've skinned me a croc!
[PIRATES]
Gonna skin him a croc!
[HOOK]
Sing a yo ho, you can beg, plead, and whine
But yo ho – you are wasting your time
That croc got my hand – wanna tear out his spine
Revenge, revenge, revenge is gonna be mine
[PIRATES & HOOK]
Revenge, revenge, revenge
[HOOK]
Is gonna be mine
[PRINCE CHARMING, spoken]
Let's go.
[SNOW WHITE, spoken]
Wait, you want revenge, on a crocodile? For taking your hand?
[HOOK, spoken]
I'm afraid he did more than that.
[HOOK]
Once I sailed toward a horizon
[PIRATES]
Horizon
[HOOK]
Where I might find happiness waiting
Until that croc
[HOOK & PIRATES]
Destroyed my life
[HOOK]
And filled me with hate unabating
Some say
[HOOK & PIRATES]
"Let it go",
[HOOK]
But I say
[HOOK & PIRATES]
"Hell no",
[HOOK]
I'm finally on the right path
Soon the Dark One will feel
[PIRATES]
He will feel
[HOOK]
The fire of this pirate's wrath!
[PIRATES]
Feel the fire of his,
Feel the fire of his
[SNOW WHITE, spoken]
Wait - did you say the Dark One?
[PRINCE CHARMING, spoken]
I think I know why you can't find him. We have him in our dungeon.
[HOOK, spoken]
Bloody hell.
[SNOW WHITE, spoken]
Captain, if you give us safe passage to the Queen's castle, you've got yourself a crocodile.
[HOOK, spoken]
Aye, luv, you've got a deal.
Have one last drink, mates. Then we've got a date with destiny!
[HOOK]
Sing a
[HOOK & PIRATES]
Yo ho
[HOOK]
I'll slaughter the swine
[HOOK & PIRATES]
Yo ho, must be fate's design
[HOOK]
At last our tales will again intertwine
Revenge, revenge, revenge is gonna be mine!
[PIRATES]
(Revenge, revenge, revenge)
[HOOK]
Oh, it's gonna be,
Oh, it's gonna be
[PIRATES]
(Revenge, revenge, revenge)
[HOOK]
Oh, it's gonna be mine!
[PIRATES]
(Revenge, revenge, revenge
It's gonna be)
[HOOK]
Oh, it's gonna be,
Oh, it's gonna be
[PIRATES]
(Revenge, revenge, revenge)
[HOOK]
Oh, it's gonna be mine!
After 7 year long hiatus I finally finished watching "Once Upon a Time", one of my all-time favorite TV series! It's about a modern city where everyone actually is a fairytale character, with a lot of twists, cliffhangers, magic and drama. I stopped watching after season 4, because the next seasons weren't broadcasted on TV where I live, and when I got the opportunity to watch in on local streaming, I postponed it, because right since 2014 I knew I was going to give the series my Lego treatment, like I did in the same year with Doctor Who, by making all my favorite characters (too many in Doctor, too many in OUAT) as minifigures. And I needed way too much time for that.
In the middle of February I read that all Disney-owned and/or Disney-distributed titles will disappear from the streaming at midnight March 1st, and later I realised that included ABC titles as well. So the penultimate week of the month I was watching some Disney/Pixar/Marvel stuff I missed during pandemic, and the last week I was staying up to 4 am to be able to watch last 3 seasons of 22 episodes each right in time (actually I made it in 5 days of 6 I have left, but only because 4 of them were holidays/weekends, and I was exremely exhausted), with no chance to rewatch the first 4 seasons before it, like I originally intended. It was totally worth it! The ending was good (especially for my most favorite character of the series, Regina), though I have some questions, because it implies right now in the same... world there are more than one... version of the same person for a... couple of people... at the least. It's not a plot hole, it was explained, I just not sure how many there are and I don't think it's good for some characters, so I'm not sure it was good in-universe decision.
Anyway, I'm hoping to gradually make tributes to all my favorite characters, but it will take a lot of time, because for some I need parts which were announced, but not released in sets yet, and for some I'm not sure how big a background I can build or what scene should I take (because these characters had more interesting scenes in the first seasons, and I barely remember it).
This is a tribute to Captain Hook/Killian Jones, a villain turned hero, and quite a cool character (because pirates are cool). By the way, I think that the idea that Peter Pan is evil, and Hook was not bad compared to him even when Hook WAS a villain - is one of the most genius creative decisions in this series. I never liked the book about Peter even when I was a kid because I always felt something is very off with him, very creepy, like if something horribly bad was happening. But I never could quite explain it. With OUAT I finally understood what was wrong, and I'm so happy this dark interpretation of the book exists.
For the character tributes I decided to pick a few (best) songs from the episode, where the wish upon a star accidentally made everyone in the Enchanted forest to sing (and it was both hilarious and epic). Hook's song was awesome, the best choreography!
You can watch the scene (with an official karaoke lines) here:
Captain Hook's Song: Revenge Is Gonna Be Mine - Once Upon A Time (Season 6, Episode 20 "The Song in Your Hearts" aka The Musical Episode)
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I offer private street photography workshops in Brighton Beach all year around and I have the occasional group workshop www.shootnewyorkcity.com/workshops there.
I revisited this magnificent nature reserve today 10th August 2018, many visitors to our city miss its glorious offerings, thinking all we have to offer is the beach front at the main boulevard , its a pity as this reserve is a short drive from the main tourist area and has its own charm, attraction and wealth of nature on offer, I love it .
Donmouth Local Nature Reserve is a beach site in the historic Old Aberdeen part of the City where the River Don meets the sea.
A great place to see seals and a range of interesting birds. The beach area has changed over time as the river has changed its course. There are lots of interesting plants in the dunes and beach area. Bird hide is an excellent shelter from which to watch the wildlife. The paths run across King Street to the Brig 'o Balgownie., the original bridge in to the City from the North, then down the other side of the river to the sea.
The site was designated a Local Nature Reserve in 1992
Paths are good although wheelchair access to the beach would be difficult as the boardwalk can get covered with sand.
There is plenty of free car parking on the Beach Esplanade and at the car park in Donmouth Road. There are cycle racks on Beach Esplanade
Bridge Of Don has five spans of dressed granite, and rounded cutwaters that carry up to road level to form pedestrian refuges. The spans are 75 feet (23 m), with a rise of 25 feet (7.6 m).
It was widened in 1958-59, from 24 feet (7.3 m), to 66 feet (20 m) by the construction of a new concrete bridge adjacent to the old one.
It now carries four lanes of the A956 road, and is the last bridge on the River Don before it meets the sea. The bridge is just downstream from a substantial island in the river. Around the area of the bridge is the Donmouth Local Nature Reserve, designated as a LNR in 1992.
Near to the bridge are a number of World War II era coastal defences, including a pill box.
Mudflats
Mudflats are formed when fine particles carried downstream by the river are deposited as it slows down before entering the sea, and to a lesser extent by fine particles washed in by the tide. The sand spit at the mouth of the Don provides shelter from the wind and waves allowing this material to build up. The mud flats are a very rich and fertile environment. Despite their rather barren appearance they support a surprisingly diverse invertebrate fauna which includes; worms, molluscs and crustacea. These invertebrates are vitally important to wildfowl and wading birds within the estuary.
Salt marsh
Along the upper shore of the south bank saltmarsh has developed. This habitat would once have been much more extensive prior to the tipping of domestic and other refuse in the area and the formation in 1727 of an artificial embankment to prevent flooding of the river into the Links. This habitat is now reduced to a narrow strip of vegetation along the river margins upstream from the Powis Burn.
The species composition of the salt marsh varies according to the salinity of the water i.e. the proximity to the sea. Close to the Powis Burn this habitat is dominated by reed sweet-grass (Glyceria maxima) with reed canary-grass (Phalaris arundinacea), sea club-rush (Scirpus maritimus), spike-rush (Eleocharis palustris), hemlock water-dropwort (Oenanthe crocata) and common scurvygrass (Chochlearia officinalis).
Further inland reed sweet-grass continues to dominate but hemlock water-dropwort is more abundant with meadowsweet (Filipendula ulmaria) and valarian (Valariana officinalis),
Sand dunes
Sand dunes are found in the more exposed parts of the estuary at the river mouth. Again, this habitat was once much more extensive in this locality with dune grasslands stretching from Aberdeen Beach inland as far as King Street, southwards from the estuary of the Dee, northwards to the Sands of Forvie and beyond. Many of the dunes formed part of Seaton Tip, and following tipping the area was grassed over. Other areas have been formally landscaped to form golf courses or planted with native trees in 2010 to create a new woodland area.
Some remnants of the natural dune flora can be seen in the 'roughs' on the Kings Links golf course and near the mouth of the river.
Above the high water mark, fore dunes with thick clumps of the pioneer grass species including sea lyme grass (Elymus arenarius) and marram grass (Ammophila arenaria) occur. Few other species are able to cope with the shifting sand. The largest area of these young dunes is to the north and west of the headland. Further inland where the dunes are sheltered from the actions of the wind and waves, and soils are more developed, more stable dunes are present supporting a more diverse grassland habitat.
Strand line plants which are able to tolerate occasional coverage by sea water include sea rocket (Cakile maritima), frosted orache (Atriplex laciniata), sea sandwort (Honkenya peploides) and knotgrass (Polygonum aviculare). Bur-reed (Sparganium sp.) has been recorded; presumably washed down by the river.
Marram grass (Ammophila arenaria) and sea lyme grass (Elymus arenarius) dominate the fore dunes. The latter species is not native to this area but appeared in 1802. It is thought to have been unintentionally introduced into the area by fishing boats. For a number of years it remained uncommon but from 1870 onwards it spread rapidly along the coastline (Marren, 1982).
In the more stable dunes red fescue (Festuca rubra), sand sedge (Carex arenaria), yellow rattle (Rhinanthus minor), wild pansy (Viola tricolour), harebell (Campanula rotundifolia), bird's-foot-trefoil (Lotus corniculatus) and lesser meadow-rue (Thalictrum minus) are abundant. Small amounts of kidney vetch (Anthyllis vulneraria), valerian (Valeriana officinalis) and spring vetch (Vicia lathyroides) are present.
Scattered willows (Salix sp.) and sycamore (Acer pseudoplantanus) have seeded into this area. Gorse (Ulex europaeus) scrub has colonised the dunes in some areas and appears to be spreading.
Scrub
This habitat is almost entirely artificial with only the gorse scrub on the inner dunes being a semi-natural habitat. Alder and willow were planted along the south bank of the river in about 1970 and these shrubs are now generally well established. Further shrub planting on the south bank was carried out in 1990.
Willow (Salix sp.) and alder (Alnus glutinosa) were planted in the 1970's along the south bank of the River Don eastwards of the Bridge of Don. The trees to the west of this strip are doing considerably better than those to the east. More recent planting was carried out in 1990 with hawthorn (Crataegus monogyna), blackthorn (Prunus spinosa) elder (Sambucus nigra), goat willow (Salix caprea) and alder.
Underneath the scrub neutral grassland is present with cocksfoot (Dactylis glomerata), false oat-grass (Arrhenatherum elatius), cow parsley (Anthriscus sylvestris), sweet cicely (Myrrhis odorata), hedge woundwort (Stachys sylvatica) and hedge bindweed (Calystegia sepium).
Grassland
Much of the grassland within the reserve is formed on imported soil and is intensively managed. This includes grassland on the north and south sides of the Esplanade. Daffodils are present in the grassland on the north side of the road. On the north bank to the east of the Bridge of Don is rank grassland on a steep south-facing slope. This is unmanaged and contains some patches of scrub.
Rough grassland is present on the headland. This area has been modified by tipping, with rubble to the east and with grass cuttings to the west. The grassland contains a mixture of neutral grassland, dune grassland, ruderal, and introduced garden species. This area attracts flocks of seed eating birds in late summer and autumn.
Improved grassland is present on the headland and along the south bank of the estuary downstream from the bridge of Don. Much of this vegetation has developed on imported soil and contains a high proportion of ruderal species and garden escapes. On the headland, broadleaved dock (Rumex obtusifolius), nettle (Urtica dioica), coltsfoot (Tussilago farfara), spear thistle (Cirsium vulgare), cow parsley (Anthriscus sylvestris), hemlock (Conium maculatum) and hogweed (Heracleum sphondylium) are abundant. Sweet cicely (Chaerophyllum bulbosum) is widespread and in late summer fills the air with the scent of aniseed.
To the south of the Esplanade the grassland is managed with an annual cut.. The grassland does flood to form pools. Early in the year cuckoo flower (Cardamine pratensis) is common, meadow foxtail (Alopecuris pratensis)is known to occur around the margins of these pools.
Woodland
Semi-mature woodland is present on the steep sided south bank of the river upstream from the Bridge of Don. Most of this woodland has been planted in the mid 1930's though some older oak and elm trees are present. These may be relicts of former woodland cover. The woodland in the reserve is part of a strip of woodland along the River Don corridor which continues upstream from the Brig 'o' Balgownie.
Woodland is present on the south bank upstream from the Bridge of Don.
Much of the woodland consists of even aged stands with willow (Salix sp.), sycamore (Acer pseudoplatanus), ash (Fraxinus excelsior), beech (Fagus sylvatica) and alder (AInus glutinosa). At the top of the slope mature oak (Quercus sp.) and elm (Ulmus glabra) are present. The ground flora contains tufted hair-grass (Deschampsia caespitosa), red campion (Silene dioica), ramsons (Allium ursinum) and lady fern (Athyrium felix-femina) .In a few areas dense shading is caused by the trees and in these areas the ground flora is poor.
On the north bank scattered trees are present, mainly willow and sycamore with some scrub.
Call me Snake offers an optimistic provocation – ‘imagine what could be here’ by Judy Millar. On a walk into the city October 3, 2015 Christchurch New Zealand.
The work is comprised of vibrant graphics of Millar’s looped paintings, which are adhered to five intersecting flat planes, and draws inspiration from the forms found in pop-up books. The colourful piece will add a dramatic and rhythmic counterpoint to the city’s current urban landscape — a mix of flattened sites, construction zones and defiant buildings that have stood through the quakes. The work employs theatricality, playfulness and visual trickery, whereby the viewer is unsure about the work’s flatness or three-dimensionality; and it has been designed to offer a different perspective from each angle. The bright colours interrupt the grey of the work’s surrounds, and as buildings pop up around it,
SCAPE 8, New Intimacies curated by Rob Garrett was a contemporary art event which mixed new artworks with existing legacy pieces, an education programme, and a public programme of events. The SCAPE 8 artworks were located around central Christchurch and linked via a public art walkway. All aspects of SCAPE 8 were free-to-view.
The title for the 2015 Biennial – New Intimacies – came from the idea that visually striking and emotionally engaging public art works can create new connections between people and places. Under the main theme of New Intimacies there are three other themes that artists responded to: Sight-Lines, Inner Depths and Shared Strengths.
For more Info: www.scapepublicart.org.nz/scape-8-judy-millar
Ocean Terminal offers a great opportunity to observe different bus stock and it's a quiet and safe place to take photographs. I have always felt this to be one of my favourite locations for bus photography.
Working on Service 22 Volvo B7TL / Wright Eclipse Gemini, number 721 (SN55 BLX) is in the company of Omni City Scania number 988 (SN57 DBO).
This small group of Polish buses were for a time the only buses Lothian had that were not made in Great Britain and the photograph provides a chance to compare two designs. Note how immaculate both of these vehicles are.