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Central United Methodist Church was one of the first Protestant congregations in Michigan. The church was organized in 1810, incorporated in 1822, and the church building was built in 1865 ( with modifications to the sanctuary in 1867 ) .
cultivate our difference / cultiver notre difference
Serie... See the world
Olympus EP2 + Voigtlander Nokton 50 1.1
My pretty trinity of vintage 2nd generation Liccas. ^o^
You can see the subtle and not so subtle differences between the headmolds and face designs as Licca's looks evolved within the generation. They're all 2nd gen Liccas (1972 - 1980) but don't look the same. The one on the right is closest to 3rd gen Licca.
They're named (left to right): Appley, Glass and Mopsy. Glass and Mopsy have had their hair fixed and looks refreshed and restored by the Japanese customizer Osharebox (Mikiko). ♥
The middle dress is by Button Arcade, the rest of the clothes are Licca Castle and playline Licca coordinates you can buy separately for mixing and matching. Love the pink top + stripey t-shirt combo, the two are sewn together like that as one piece and look very nice with all kinds of summer bottoms.
The Batmobile resumes its journey,* speeding west along Highway 35. The encounter with Bond had been startlingly enlightening. Dreamwalkers. Dreamweavers.**
"Batcomputer. Scan for boundaries in Paprihaven along theta lines. Cross with phantasmal energies across all levels of subatomic translucence."
"Working."
He's missing something. There's not a known formula to scan for dream energy but this should give a starting point. Still...
Something has been bothering him since he and Bond were hit by the... what to call it? If his theory is correct, it was akin to a REM ripple.***
At first Batman was sure he had returned to his previous form. But, then, Bond had been just as sure. He had noticed Bond's difference though. He had to know for sure.
KLIK!
"Hey, Batman!"
"Canary, turn on your video. Look at me."
"Mmooookay! And... Okay, I see you."
"And?"
"Aaaannd, It sounds like I should be noticing something? But I'm missing it."
"Good."
"What was I-"
KLIK!
"Selena."
"Hello, handsome. Oh, and a video call no less. Want me to-"
"How do I look?"
"-get... How do you look? What a fascinatingly un-Batman question. You look luscious. You look entirely-"
"Bond is on his way to meet all of you at the Boogaloo. My Batcomputer places you there."
"Why is your computer tracking m-"
"When he arrives, look at him, contact me, and tell me how he looks."
"... ... Are you wanting me to tell you which of you is more yummy?? I never knew you-"
KLIK!
"Superman."
"Batman, give me some news. We need a solution. The way this conflict has scaled up, even if we win, Paprihaven will be destroyed."
"Hrn. I'm tracking on new information now. I may have a solution soon. I'm going to be out of play and out of contact for a while."
"What's a while?"
"Hard to tell. And I'll need Diana."
"Diana is our heaviest hitter second only to me."
"She beat you once."
"I was mind controlled. If you need power, take Mary Marvel. Or Power Girl. I'd offer Kara but she's out of dimension with Barbara on a mission of the Queen."****
"Out of dimension? Alice sent them? I didn't okay Batgirl leaving."
"I'm just surprised I knew something you didn't."
"No, I need Diana. It's not just the power, it's her experience. Everything may hinge on this, Kal. We don't want to cut corners here."
"Have you asked Diana?"
"I wanted to speak with you first. Keep you in the loop. So you don't throw another super-fit."*****
"I didn't... Okay, contact her. If Diana's good with it, I'm good with it, but do it on open channel so everyone knows she's off the field. We'll need to get a reinforcement to take her place.
Maybe Shazam. She's heavily involved with someone called Juggernaut at the moment."******
"Hrn. I have one more thing to check. Then I'll let Diana know on open channel."
"Sounds good. Be careful, friend."
KLIK!
The Batman settles in and brings his mind into sharp focus. He believes he now knows what Alice is keeping in the castle. And, if so, and he can reach it, then the next steps will mean life or death of Paprihaven.
He pushes aside the uneasiness of 'other Batmen'. There was no evidence any of them had breached or remained in Paprihaven.
⋅•⋅⋅•⋅⋅•⋅⊰⋅•⋅⋅•⋅⋅•⋅⋅•⋅⋅•⋅⋅•⋅⋅•⋅⋅•⋅⋅•⋅⋅•⋅⋅•⋅∙∘☽༓☾∘∙•⋅⋅•⋅⋅•⋅⋅•⋅⋅•⋅⋅•⋅⋅•⋅⋅•⋅⋅⋅•⋅⋅⊰⋅•⋅⋅•⋅⋅•⋅⋅•⋅
A year of the shows and performers of the Bijou Planks Theater.
Legends of Batman
Batmobile
1994, Kenner
Mafex
Batman v Superman
Batman
2016, Medicom Toy
* A journey begun back in episode 1583!
www.flickr.com/photos/paprihaven/50132187992/
** Discussed in detail last episode!
www.flickr.com/photos/paprihaven/53520187275/
*** The REM Ripple smacked them both silly in episode 1625!
www.flickr.com/photos/paprihaven/53496872258/
**** Hinted at in episode 1210! To be shown in full, action-packed glory when we get there!
www.flickr.com/photos/paprihaven/37511434634/
***** In fairness it was a Bat-fit as well! Seen in episode 1526!
www.flickr.com/photos/paprihaven/48407842352/
****** Last seen manhandling Green Lantern, Lina, and Space Ghost back in 1356! Don't worry! We're planning to get back to that!
My 2013 Classic Rapunzel Doll has been completely deboxed. She is standing, supported by a Kaiser doll stand (not included with the doll), and is photographed from various angles.
The 2013 Classic Rapunzel doll has many differences from the 2012 model, and is a greatly improved doll. She is both more attractive and more movie accurate. The major changes are to her head and face, her dress and her legs. There are a minor changes to her hair and she is now barefoot. The only features that haven't changed are her torso and arms. I still prefer the 2011 Classic Rapunzel doll's face. Of course the original 2010 Classic Rapunzel doll has a far superior dress and hair and several accessories. The 2010 doll is still available, repackaged as the 2011 Parks Rapunzel doll, in Disneyland Anaheim as of June 23, 2013.
Her head has been redesigned to be rounder than last year's doll. She has a larger forehead, larger eyes, more pronounced cheekbones, fuller cheeks, wider mouth that still has a smirk, and a smaller chin. Her small nose is slightly straighter, so there is no pronounced knob at the end.
Her face is similar to last years, but with many small changes. Her eyes are wider than before, so they are larger and more oval. Her big green eyes are still glancing to her right, but the pupils are larger, the color is darker, and the whites are larger. She no longer looks like she is glancing to the right but still staring straight ahead (which was a creepy look for the 2012 doll to have). Instead, she looks like she is gracefully looking towards her right. She has two short, thick lashes over the corner of her right eye and three over her left. She has no eyeshadow. Her light brown eyebrows are slightly lighter in color, and closer to her eyes. Her freckles are in a slightly different pattern, and are slightly darker. The rouge on her face is a little darker, and also extends across the middle of her nose. Her closed mouth is a little wider and forms a smirk as before, but her pink lips are now darker and more purple. Overall, her face is much more attractive, feminine and lively, as well as being more movie accurate.
Her golden blonde hair is about 11 inches long, so doesn't quite reach the floor. It is about an inch shorter than the hair on the 2012 Rapunzel, which actually dragged on the floor. It is still straight and free flowing. Right out of the box it is easy to make even by shaking it out, but isn't quite as smooth as the 2012 doll. But it was very easy to comb it to make it smoother and more even. There is a pronounced ridge of hair over her forehead that is fixed in place with gel, so it is quite stiff. The ridge makes her face more open than the 2012 doll, which also helps her appearance. The rest of her hair is soft, smooth and shiny.
The dress is similar in design as the 2012 doll, but is now much more attractive and movie accurate. Her satin bodice is now pink rather than dark purple, with pink corset lacing and a V-shaped waist. She has short puffy satin sleeves with pink and purple stripes. Her purple satin skirt is overlayed with a glittering floral pattern, with a center section that is plain purple satin. This is a switch from the movie version, where the floral pattern was in the central pink panel. However, it is much improved over the purple satin skirt of the 2012 doll, with no central panel, and the glitter in a random spray pattern. The skirt is the same length as before, a couple of inches off the floor. Missing are the sheer pink sleeve extensions on the dresses of the 2012 and earlier versions.
Her body is fully articulated in the arms, but now has the rubber legs of 2011 and earlier dolls, which has internal knee joints and fixed angled feet. Her hip joints allow her to sit down with her legs together and her back straight up, unlike the 2012 doll with the fully articulated but defective legs. But her knees can only bend about 40 degrees, so her legs stick out when she is sitting. The leg joints are also much stiffer, so she is in a much more natural position when placed standing in a Kaiser doll stand. Her angled rubber feet also make her about 1/4 inch taller than the 2012 doll, who had flat feet. I'm glad that she is now barefoot, as she was throughout the original movie. I'd say that the rubber legs are definitely a big improvement, except that glitter tends to stick to them.
The packaging for the dolls is much improved. The box art has been completely redesigned, with beautiful decorations unique to each Princess (actually for each movie), and a cameo of the animated movie character. Rapunzel's artwork has a purple background and includes images of the Sun and her hairbrush. The boxes are the same height and width, but are 1/2'' flatter, making them smaller and lighter.
The 2013 Disney Princess Classic Doll Collection, released on June 10, 2013. They consist of 11-12'' articulated dolls of the 11 official Disney Princesses, from Snow White to Merida, as well as Princes, Villains and Sidekicks. I now have all 11 Princesses, Queen Elinor, Charlotte and Gaston. I will photograph them boxed, during deboxing and fully deboxed. I will also post reviews and comparative photos.
Classic Disney Princess Rapunzel Doll - 12''
US Disney Store
Released online June 10, 2013.
Purchased online June 13, 2013.
Received June 24, 2013.
$14.95 (was on sale for $10 at time of purchase).
The 2013 Classic Snow White Doll is photographed new in her unopened box.
The 2013 Classic Snow White doll has many differences from the 2012 model, many of which are improvements in my view. The biggest changes are to her hairdo, her skirt and her legs, and the addition of a cape. There were also minor changes to her bow, collar, shoes and painted on underwear. Her head, face, arms and upper torso have remained the same. I like this doll much better than last year, and she represents the movie character much more faithfully.
Her face has remained the same, but I think she is beautiful, lively and very movie accurate. She has a round face, big brown eyes glancing to her right. She has three short thick black lashes over each eye, and short thin black eyebrows. She has small button nose, small full dark pink lips in a sweet open mouthed smile. She has pale flesh colored skin, and her cheeks are lightly rouged.
Her hair is greatly improved over the 2012 doll, mostly due to the redesign of her side curls. She is jet black shoulder length hair, in a bobbed hairdo. The main curls on each side of her head are now much larger, and the upper curls now curve in the same direction (clockwise) as the main curls. The upper side curls are now sewn to her hair, keeping them in place, as was done in the Snow White dolls before 2012. Her hair looks very movie accurate, and is much neater than the old style. There is a bit of gel in the curls, both on the sides and in the back, but the hair is still fairly soft to the touch.
Her dress is yet another version of her iconic blue, yellow and red gown. And with the addition of a red satin cape, her outfit is much closer to the movie character than any Disney Store Classic Snow White doll in recent years. Her bodice is the same as last year. It is dark blue satin covered in blue glitter, with puffy short blue satin sleeves. On her sleeves are oval bright red appliques. Her high white satin collar is rounded looks much better and movie accurate than last year's square cornered collar. Her newly added red satin cape is half-length (about four inches long), and is unfortunately sewn to the back of her dress. It is shorter than the movie cape, but matches the doll's shorter skirt. Her yellow satin skirt has changed a bit from last year. It is a couple of inches shorter, less full, and stiffer with the addition of a golden glitter floral pattern. It's color is more golden than last year. The width of last year's skirt was wasted as there was no petticoat underneath to keep it full. This year's skirt keeps its shape much better due to its stiffness. The glitter does tend to shed, finding its way in the dolls body, legs, face and hair, as well as your hands and the general neigborhood of the doll.
Her shoes are pale yellow flats that are shorter and slighter darker in color than last year's. Their soles are also rounded upwards at the toes, similar to the flats that the Mulan doll always wears. This design looks better on a doll with angled feet, than would the 2012 style flats, which had very flat soles. The red satin ribbon in her hair is thinner than last year's, with a much smaller bow. Last year's ribbon and bow were much prettier, but her bow was placed halfway down the right side of her head. Now the bow is in the center, at the top of her head, where it belongs.
Her body is fully articulated in the arms, but now has the rubber legs of 2011 and earlier dolls, which has internal knee joints and fixed angled feet. I would rather that they fixed the problems with the fully articulated 2012 legs, but when exposed the rubber legs do look a lot better, with the disadvantage of being much less posable. Also the glitter tends to stick to the rubber legs, and it cannot simply be brushed off. Although both dolls are wearing flats, the 2013 doll is about 1/4 inch taller since she has angled feet, wearas the 2012 doll has flat feet.
The packaging for the dolls is much improved. The box art has been completely redesigned, with beautiful decorations unique to each Princess (actually for each movie), and a cameo of the animated movie character. Also the way the dolls are packaged is much simplified, making it much easier and quicker to remove them from the box. Greatly reduced or eliminated are the tiny plastic T-bar fasteners, which secured the outfits to the backing and left little holes and sometimes runs in the fabric. There are still large T-bar fasteners tacking the back of the doll's head to the backing. Also the dolls with free flowing hair no longer have them flattened and sectioned into two parts, making it hard to even out the back of their hair after deboxing. Instead, their hair is gathered up and placed to one side of the doll, and secured by thread. It looks good as is in the box. Or if the doll is deboxed, it is easy to shake out the hair and even it out using just your fingers.
The 2013 Disney Princess Classic Doll Collection, released on June 10, 2013. They consist of 11-12'' articulated dolls of the 11 official Disney Princesses, from Snow White to Merida, as well as Princes, Villains and Sidekicks. I now have all 11 Princesses, Queen Elinor, Charlotte and Gaston. I will photograph them boxed, during deboxing and fully deboxed. I will also post reviews and comparative photos.
Classic Disney Princess Snow White Doll - 12''
US Disney Store
Released online June 10, 2013.
Purchased online June 13, 2013.
Received June 24, 2013.
$14.95 (was on sale for $10 at time of purchase).
As usually happens someone didn't agree with what this fellow was saying and chose to show their displeasure by hoisting their own thought of what we deserved. In the end the police passed judgement on both and had them go their separate ways.
I returned to Kings Heath one day after taking an initial shot of All Saints Church since it snowed.
What a difference a day makes! The Farmers Market is gone. The new square is covered with snow.
Is Grade II listed.
Anglican Church of All Saints, Birmingham
997/0/10420 VICARAGE ROAD
08-JUL-03 KINGS HEATH
Anglican Church of All Saints
(Formerly listed as:
VICARAGE ROAD
KINGS HEATH
ALL SAINTS)
II
An Anglican church, dating from 1859-60, with a spire added in 1866, all by Frederick Preedy (1820-1898). The north aisle was added in 1883 by Julius Alfred Chatwin (1830-1907). The west end was enlarged in 1899 by J P Sharp (d.1915).
MATERIALS: The walls are constructed from brick with Bromsgrove stone cladding, under plain clay tile roofs.
PLAN: The plan has a chancel with north organ chamber, choir vestry and boiler room, and a five-bay nave, with north and south aisles. There is a Lady Chapel at the east end of the south aisle. The south-west tower houses the present entrance. The north aisle contains a projecting main entrance (not used) and the baptistery is situated in the west end of the church. The westernmost bay of the nave and aisles is divided from the body of the church by a modern screen, beyond which the vestries have been converted to office space.
EXTERIOR: The exterior is eight bays long, and is arranged around an off-centre tower, above the entrance. To the left of the tower, at ground floor level, are the former vestries. The ground floor entrance is framed by buttresses and the tower stair, which is built into the south-west corner of the tower. A Gothic-arched entrance projects forward as a sharp gable, with coping on the parapet. The tower is in three stages: a deep base with buttresses; a belfry section, rich in detail; and a tall broach spire. Detail is most concentrated on the belfry, with its clustered colonnettes dying into a deeply splayed base picked out in a lighter stone. The clustered colonnettes support coupled Gothic arches, with recessed plate tracery, with quatrefoils. The broach spire has gabled dormers, or openings, also in a lighter stone. To the right of the tower is the south aisle, of three bays with buttresses supporting a low roof. Deeply recessed beyond the aisle is the chancel, with a plain elevation of two window bays and a central door.
INTERIOR: The nave has north and south arcades of pointed arches on octagonal piers. The arches and piers are picked out in alternating bands of reddish and cream stone, with the wall elevations plastered. The piers have simple moulded capitals. The roof is an exposed arched-braced construction, with alternating arched braces resting on carved stone corbels and all braces rising to collars. The aisles are of a lean-to construction, with exposed timber roofing, and wainscoting on the walls. The east end of the south aisle has a Lady Chapel. The carved wood pulpit, with ogival arch motif on facets, sits on a carved stone base with engaged colonnettes. The church's foundation stone is housed at the back of the pulpit, which is accessed by an integrated stone stair. The chancel arch is supported on engaged columns with naturalistically-carved capitals and adjacent headstops. The rood screen wrought-ironwork is of some complexity. The north side of chancel has a screen of coupled Gothic arches springing from a freestanding central pier, with a naturalistically-carved capital - a feature repeated on the engaged piers to either side. The deep relief capitals in this section of the church have fine and crisply-realised detail. A reredos dating from 1892 features wainscoting and much ornament such as crocketing over miniature ogival arches. The south wall of the chancel is wainscoted. The servers' vestry has original very deep cupboards.
HISTORY: The railway arrived in King's Heath in 1840, resulting in gradual development of the area from that date onwards. In 1857 Frederick Preedy was chosen to design a low-budget church for the burgeoning area. The builder, Isaac Clulee, managed to pare down the quotation to £1,945.10.0. Building began in early 1859 and the church was consecrated in July 1860. The church was contemporaneously described as being 'in the early decorated style' and was intended to be extended as to when funds became available. A new parish for All Saints was created out of part of the parishes of St Nicolas, King's Norton and St Mary, Moseley, in 1863. In 1866, the spire was added at a cost of about £1,200 and in 1883 the north aisle was added by Julius Alfred Chatwin. In 1892, a new reredos was erected and in 1899 the church was enlarged at the west end to the designs of J P Sharp & Co., Architects of Martineau Street, Birmingham. At the time of inspection (February 2009), the church was being extended to the west, to connect it to the newly-built church centre at the east of the plot in which the church stands.
SOURCES: Budd, S A, The Parish Church of All Saints', King's Heath, Birmingham - 1860-1960 (1960)
Pevsner, N and Wedgwood, A, The Buildings of England, Warwickshire (1966), 187
REASONS FOR DESIGNATION: The Anglican Church of All Saints, King's Heath, is designated at Grade II, for the following principal reasons:
* The church is a pleasing asymmetrical design of 1857 by the recognised C19 architect, Frederick Preedy
* The exterior shows impressive massing, and demonstrates good detailing, showing a high degree of quality in design and execution
* Its interior has good-quality stonework and interesting roof structures, complemented by high-quality, crisp carving
* Preedy's church is enhanced by additions by J A Chatwin and J P Sharp, which create a cohesive and handsome ensemble
Was quite misty with the church here.
The last photo I posted was taken of our last big tree decorated.
This photo is what we have now. It has one string of lights and hand-carved Santa icicle ornaments.
City Palace, Udaipur, is a palace complex in Udaipur, in the Indian state Rajasthan. It was built over a period of nearly 400 years being contributed by several kings of the dynasty, starting by the Maharana Udai Singh as the capital of the Sisodia Rajput clan in 1559, after he moved from Chittor. It is located on the east bank of the Lake Pichola and has several palaces built within its complex. Udaipur was the historic capital of the former kingdom of Mewar in the Rajputana Agency and its last capital.
The City Palace in Udaipur was built in a flamboyant style and is considered the largest of its type in Rajasthan, a fusion of the Rajasthani and Mughal architectural styles, and was built on a hill top that gives a panoramic view of the city and its surrounding, including several historic monuments such as the Lake Palace in Lake Pichola, the Jag Mandir on another island in the lake, the Jagdish Temple close to the palace, the Monsoon Palace on top of an overlooking hillock nearby and the Neemach Mata temple. These structures are linked to the filming of the James Bond movie Octopussy, which features the Lake Palace and the Monsoon Palace. The subsequent publicity has resulted in the epithet of Udaipur as "Venice of the East". In 2009, Udaipur was rated the top city in the World's Best Awards by Travel + Leisure.
HISTORY
The city Palace was built concurrently with establishment of the Udaipur city by Maharana Udai Singh, in 1559 and his successor Maharanas over a period of the next 300 years. It is considered the largest royal complex in Rajasthan and is replete with history. Founding of the city and building of the palace complex can not be looked in isolation as the Maharanas lived and administered their kingdom from this palace.
Prior to moving their capital from Udaipur to Chittor≤≥, the Mewar kingdom had flourished initially in Nagda (30 kilometres to the north of Udaipur), established in 568 AD by Guhil, the first Mewar Maharana. In the 8th century, the capital was moved to Chittor, a hill top fort from where the Sisodias ruled for 80 years. Maharana Udai Singh II inherited the Mewar kingdom at Chittor in 1537 but by that time there were signs of losing control of the fort in wars with the Mughals. Udai Singh II, therefore, chose the site near Lake Pichola for his new kingdom because the location was well protected on all sides by forests, lakes and the Aravalli hills. He had chosen this site for his new capital, much before the sacking of Chittor by Emperor Akbar, on the advice of a hermit he had met during one of his hunting expeditions.
At his capital Udaipur, Maharana Udai Singh soon faced defeat at the hands of Mughal Emperor Akbar. He soon moved to Udaipur to the chosen location to establish his new capital. The earliest royal structure he built here was the Royal courtyard or 'Rai Angan', which was the beginning of the building of the City Palace complex, at the place where the hermit had advised Maharana to build his Capital.
After Udai Singh’s death in 1572, his son Maharana Pratap took the reins of power at Udaipur. He was successful in defeating Akbar at the battle of Haldighati in 1576 and thereafter Udaipur was peaceful for quite some years. With this, prosperity of Udaipur ensued, palaces were built on the shore and in the midst of the Pichola lake. Concurrently art, particularly miniature painting, also flourished.
But in 1736, the marauding Marathas attacked Udaipur and by the end of the century the Mewar state was in dire straits and in ruins. However, the British came to Mewar’s rescue in the 19th century and soon the State of Mewar got re-established and prospered under British protection, under a treaty signed with the British. However, the British were not allowed to replace them. Once India got independence in 1947, the Mewar Kingdom, along with other princely states of Rajasthan, merged with the Democratic India, in 1949. The Mewar Kings subsequently also lost their special royal privileges and titles. However, the successor Maharanas have enjoyed the trust of their people and also retained their ownership of the palaces in Udaipur. They are now running the palaces by creating a trust, called the Mewar Trust, with the income generated from tourism and the heritage hotels that they have established in some of their palaces. With the fund so generated they are running charitable hospitals, educational institutions and promoting the cause of environmental preservation.
LEGEND
Historical legend narrated to the selection of the site for the palace is about a hermit meeting Maharana Udai Singh when he was on a hunting trail in the Udaipur hills. The Maharana met the hermit who was meditating on top of a hill above the Pichola Lake and sought the hermit’s blessings. The hermit advised the Maharana to build his palace at that very spot and that is where the palace complex came to be established at Udaipur.
GEOGRAPHY
The city palace located in Udaipur city at 24.576°N 73.68°E, which is set with an average elevation of 598 metres.
CLIMATE
The climate of Udaipur reflects the climate at the city palace. It is tropical, with the mercury recording between a maximum of 38.3 °C and a minimum of 28.8 °C during summers. Winter is cold with the maximum temperature rising to 28 °C and the minimum dipping to 11.6 °C. The average annual rainfall is 64 cm.
STRUCTURES
The series of palaces packed in the city palace complex, facing east (as customarily appropriate for the Maharana dynasty – the Sun dynasty), behind an exquisite facade of 244 metres length and 30.4 metres height, were built on a ridge on the east of lake Pichola. They were built over a long period, from 1559 onwards, by 76 generations of Sisodia Rajputs or Suryavanshi Rajputs (worshippers of Sun god). Several Maharanas (the title Maharana is distinctly different from Maharajah, as the former connotes a warrior and the latter a ruler or a king) starting with Udai Mirza Singh II, have richly contributed to this edifice, which comprises an agglomeration of structures, including 11 small separate palaces. The unique aspect of this conglomeration is that the architectural design (a rich blend of Rajasthani, Mughal, Medieval, European and Chinese Architecture) is distinctly homogeneous and eye catching. The palace complex has been built entirely in granite and marble. The interiors of the palace complex with its balconies, towers and cupolas exhibit delicate mirror-work, marble-work, murals, wall paintings, silver-work, inlay-work and leftover of colored glass. The complex provides a fine view of the lake and the Udaipur city from its upper terraces.
Located with the picturesque backdrop of rugged mountains, beside the Pichola lake on its shore, the city palace complex painted in gleaming white color has been compared to the Greek islands, such as the Mykonos.
The famous structures or palaces viewed from the Lake Palace appear like a fort. They are interlinked inside the complex through a number of chowks or quadrangles with zigzag corridors (planned in this fashion to avoid surprise attacks by enemies). Erected in the complex, after entering through the main Tripolia (triple) gate, are the Suraj Gokhda (public address facade), the Mor-chowk (Peacock courtyard), the Dilkhush Mahal (heart’s delight), the Surya Chopar, the Sheesh Mahal (Palace of glass and mirrors), the Moti Mahal (Palace of Pearls), the Krishna Vilas (named after Lord Krishna), Shambu Niwas (royal residence now), the Bhim Vilas, the Amar Vilas (with a raised garden) that faces the Badi Mahal (the big palace), the Fateprakash Palace and the Shiv Niwas Palace (the latest addition to the complex); the last two have been converted into heritage hotels. Details of all these structures are elaborated. The vast collection of structures are termed to form ‘a city within a city’ set with facilities of post office, bank, travel agency, numerous craft shops and also an Indian boutique belonging to the World Wildlife Fund (WWF) for Nature. The entire complex is the property of the Mewar royal family and a number of trusts take care of the running and maintenance of the structures. The earliest royal structure built in the complex was the Royal courtyard or Rai Angan.
GATEWAYS
Gateways, colloquially called Pols, are set to the east of Udaipur city that was established by Maharana Udai Singh II, concurrently with the City Palace. A number of impressive gateways provide access to the palace complex.
The main entry from the city is through the 'Bara Pol' (Great Gate), which leads to the first courtyard. Bara Pol (built in 1600) leads to the ‘Tripolia Pol', a triple arched gate built in 1725, which provides the northern entry. The road between this gate and the palace is lined with shops and kiosks owned by craftsmen, book-binders, miniature painters, textile dealers and antique shops. Between these two gates, eight marble arches or Toranas are erected. It is said that the Maharanas used to be weighed here with gold and silver, which was then distributed among the local people. Following the Tripolia gate is an arena in front of the Toran Pol and the facade palace, where elephant fights were staged in the past to test their prowess before starting on war campaigns.
The main block of the city palace at Udaipur is approached through a modest door from the Ganesha Deodhi terrace. The door is flanked by whitewashed walls vibrantly painted with martial animals in the traditional Rajput style.
AMAR VILAS
Amar Vilas is the uppermost court inside the complex, which is a raised garden. It provides entry to the Badi Mahal. It is a pleasure pavilion built in Mughal style. It has cussed arcades enclosing a square marble tub. Amar Vilas' is the highest point of the City palace and has wonderful hanging gardens with fountains, towers and terraces.
BADI MAHAL
Badi Mahal (Great Palace) also known as Garden Palace and is the exotic central garden palace that is situated on a 27 metres high natural rock formation bis-a-bis the rest of the palace. The rooms on the ground floor appear to be at the level of the fourth floor in view of the height difference to its surrounding buildings. There is a swimming pool here, which was then used for Holi festival (festival of colors) celebration. In an adjoining hall, miniature paintings of 18th and 19th centuries are displayed. In addition, wall paintings of Jag Mandir (as it appeared in the 18th century), Vishnu of Jagdish temple, the very courtyard and an elephant fight scene are depicted.
The elephant fight depicted in a painting on the wall was a representation of the real elephant fights, which used to be organized by the Maharanas. It is mentioned that the elephants used to be fed hashish (opium) before arranging the fights. An interesting observation is that the word ‘assassin’ is a derivative of the word ‘hashish’. The last such fight was reported in 1995.
BHIM VILAS
Bhim Vilas has a gallery of a remarkable collection of miniature paintings that depict the real life stories of Radha-Krishna.
CHINI CHITRASHALA
Chini Chitrashala (Chinese art place) depicts Chinese and Dutch ornamental tiles.
CHOTI CHITRASHALI
Choti Chitrashali or 'Residence of Little Pictures', built in early 19th century, has pictures of peacocks.
DILKHUSHA MAHAL
Dilkhusha Mahal or ‘Palace of Joy’ was built in 1620.
DURBAR HALL
Durbar Hall was built in 1909 within the Fatepraksh Palace (now a heritage hotel) Official functions such as State banquets and meetings were held here. The gallery of the hall was used by the Royal ladies to observe the Durbar proceedings. This hall has luxuriant interior with some unusually large chandeliers. Weapons of the maharanas and also some of their unique portraits are also depicted here. The foundation stone for this hall was laid by Lord Minto, the Viceroy of India, in 1909, during the rule of Maharana Fateh Singh and was then called Minto Hall.
FATEPRAKASH PALCE
Fateprakash Palace, which is now run as a luxury hotel, has a crystal gallery that consists of crystal chairs, dressing tables, sofas, tables, chairs and beds, crockery, table fountains which were never used. There is also a unique jewel studded carpet here. Maharaja Sajjan Singh had ordered these rare items in 1877 from F& C Osler & Co of London but he died before they arrived here. It is said that the packages containing these crystals remained unopened for 110 years.
JAGDISH MANDIR
Jagdish Mandir, located 150 metres north of the city palace, was built in 1652 in Indo-Aryan architectural style. It is a large and aesthetically elegant temple where an idol of Lord Jagannath, a form of Lord Vishnu made in black stone is deified in the sanctum. The temple walls and the sikhara or tower are decorated with carvings of Vishnu, scenes from Lord Krishna’s life and figurines of nymphs or apsaras. A brass image of Garuda (half-bird, half-man image, which is Lord Vishnu’s vehicle), is placed in a separate shrine in front of the temple. Flanking the steps up the temple decoration of statues of elephants are seen. The street square, where the temple is located, is also known as Jagdish Chowk from where several roads radiate in different directions.
KRISHNA VILAS
Krishna Vilas is another chamber, which has rich collection of miniature paintings that portray royal processions, festivals and games of the Maharanas. However, there is tragic story linked to this wing of the City Palace. In the 19th century, a royal princess was unable to choose from two suitors seeking her hand in marriage, one from the royal family of Jaipur and another from Jodhpur, and hence in a state of dilemma, she poisoned herself to death.
LAXMI VILAS CHOWK
Laxmi Vilas Chowk is an art gallery with a distinctive collection of Mewar paintings.
MANAK MAHAL
The Manek mahal approached from the Manak Chowk is an enclosure for formal audience for the Udaipur rulers. It has a raised alcove inlaid completely in mirror glass. Sun-face emblems, in gleaming brass, religious insignia of the Sisodia dynasty are a recurring display at several locations in the City Palace; one of these prominent emblems is depicted on the façade of the Manak Chowk, which can also be seen from the outermost court below. The largest of such an emblem is also seen on the wall of the Surya Chopar, a reception centre at the lower level. Surya or Sun emblem of the Mewar dynasty depicts a Bhil, the Sun, Chittor Fort and a Rajput with an inscription in Sanskrit of a quotation from the Bhagavad Gita (Hindu holy scripture), which means “God Helps those who do their duty". It was customary for the Maharanas to offer obeisance to the Sun facing east, every morning before taking breakfast.
MOR CHOK
Mor Chok or Peacock square is integral to the inner courts of the palace. The elaborate design of this chamber consists of three peacocks (representing the three seasons of summer, winter and monsoon) modeled in high relief and faced with coloured glass mosaic, built into successive niches in the wall area or jharoka, These were built during Maharana Sajjan Singh’s reign, 200 years after the palace was established. The peacocks have been crafted with 5000 pieces of glass, which shine in green, gold and blue colours. The apartments in front of the Chowk are picturesquely depicted with scenes of Hindu god Lord Krishna’s legends. At the upper level, there is a projecting balcony, which is flanked by inserts of coloured glass. In an adjoining chamber, called the Kanch-ki-Burj, mosaic of mirrors adorn the walls. The Badi Charur Chowk within this chowk is a smaller court for private use. Its screen wall has painted and inlaid compositions depicting European men and Indian women. Proceeding further from the Mor-Chowk, in the Zenana Mahal or women’s quarters exquisitely designed alcoves, balconies, colored windows, tiled walls and floors are seen.
MUSEUM
n 1974, a part of the city palace and the 'Zenana Mahal' (Ladies Chamber) were converted into a museum. The museum is open for public. There is an interesting exhibit of a freaky monkey holding a lamp and also portraits of maharajas displaying a spectacular array of mustaches. ‘Lakshmi Chowk' is an elegant white pavilion in the same precinct.
RANG BHAWAN
Rang Bhawan is the palace that used to contain royal treasure. There are temples of Lord Krishna, Meera Bai and Shiva, located here.
SHEESH MAHAL
Sheess Mahal or Palace of Mirrors and glasses was built in 1716.
A shrine of Dhuni Mata is also located in the complex. This location is considered as the oldest part of the Palace, where a sage spent his entire life meditating.
THE PALACE IN FILM & TELEVISION
The palace was used as a hotel in the 1985 James Bond film Octopussy, where Bond (played by Roger Moore) stayed as he began his quest to apprehend the villainous Kamal Khan (Louis Jordan).
A 1991 documentary film directed for television by Werner Herzog is called Jag Mandir and consists of footage of an elaborate theatrical performance for the Maharana Arvind Singh Mewar at the City Palace staged by André Heller.
The palace was used for filming part of Goliyon Ki Raasleela Ram-Leela (English: A Play of Bullets: Ram-Leela) 2013 directed by Sanjay Leela Bhansali.
WIKIPEDIA
46521 leads 78018 away from Quorn - the black BR Standard loco being based on the design of the the green LMS design in front. Saturday of the GCR Winter Gala.
The age difference between the two vessels is not as great as one would think by looking at them. The Gato Class Submarine USS Cobia, on display at the Maritime Museum, was constructed in late 1943 while the Kaye Barker across the river started life as the Edward B. Greene a mere eight years and two months later in January of 1952.
A lot to upload today. xD
I noticed a different level of brightness in the colour. I guess the left ones were just getting to much sun. ^^
/°°/~~/°/~~~~/°°~~~~~~~~~~~~~~
Music was my first love-------------
www.youtube.com/watch?v=t2Wj6bdEozo
All rights are reserved, pls do not use my photos without my permission. Thanks
Thanks for all comments, faves and invites !
Look at my two index toes and compare them... See how my left one is really swollen and there's some bruising? Well yesterday, I was laying on the couch and had to get up to spit out some flemy stuff that I coughed out of my lungs, because I'm pretty sure I've got the H1N1 virus, anyway.. Everytime I would sit up my head would start throbbing, so I figured if I rolled off the couch and then stood up from there my head wouldn't start throbbing like crazy... But what ended up happening was my left foot hit the floor REALLY HARD and my index toe was what came in contact with the floor first, resulting in A LOT of sudden pain and a popping noise... Its not broken, but it is either sprained or I have a hairline fracture, cause it got really swollen and there's A LOT of bruising... Just wait till you see the next picture I upload. Now I have to limp around everywhere... =(
I welcome advice from anyone who might know about this sort of thing.
Well east of Decatur IL. these NS horses gallop past horses of a different nature that could care less of the passing eastbound.
'Wait, this thing is falling in my eyes!'
'You wanted to wear the thing darling so don't complain'.
'But I can't take pictures like this!'
'We have 15 minutes to get to the London Eye'.
Put your powers of observation to the test as you compare two nearly identical pictures and try to spot the differences!
Today is "Red nose day" in the U.K. it's a big charity event lasting all day, this years slogan is "Do something funny for money" you can see more info here
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)
Ã…rdal (around the Ã…rdalsfjord)
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
LÃ¥nefjorden
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
Ã…rdalsfjorden
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 HÃ¥rfagre and then as heirs of Olav the Holy . The Norwegian kings, and their subjects, now professed Christianity . In the time around HÃ¥kon HÃ¥konsson , 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 HÃ¥logaland'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, the national assembly was completed at the earliest at the battle of Stiklestad in 1030 and the introduction of Christianity was probably a significant factor in the establishment of Norway as a state. Håkon I the good Adalsteinsfostre introduced the leasehold system where the "coastal land" (as far as the salmon went up the rivers) was divided into ship raiders who were to provide a longship with soldiers and supplies. The leidange was probably introduced as a defense against the Danes. The border with the Danes was traditionally at the Göta älv and several times before and after Harald Hårfagre the Danes had control over central parts of Norway.
Christianity was known and existed in Norway before Olav Haraldson's time. The spread occurred both from the south (today's Denmark and northern Germany) and from the west (England and Ireland). Ansgar of Bremen , called the "Apostle of the North", worked in Sweden, but he was never in Norway and probably had little influence in the country. Viking expeditions brought the Norwegians of that time into contact with Christian countries and some were baptized in England, Ireland and northern France. Olav Tryggvason and Olav Haraldson were Vikings who returned home. The first Christians in Norway were also linked to pre-Christian local religion, among other things, by mixing Christian symbols with symbols of Odin and other figures from Norse religion.
According to Sverre Steen, the introduction of Christianity in Norway should not be perceived as a nationwide revival. At Mostratinget, Christian law was introduced as law in the country and later incorporated into the laws of the individual jurisdictions. Christianity primarily involved new forms in social life, among other things exposure and images of gods were prohibited, it was forbidden to "put out" unwanted infants (to let them die), and it was forbidden to have multiple wives. The church became a nationwide institution with a special group of officials tasked with protecting the church and consolidating the new religion. According to Sverre Steen, Christianity and the church in the Middle Ages should therefore be considered together, and these became a new unifying factor in the country. The church and Christianity linked Norway to Roman Catholic Europe with Church Latin as the common language, the same time reckoning as the rest of Europe and the church in Norway was arranged much like the churches in Denmark, Sweden and England. Norway received papal approval in 1070 and became its own church province in 1152 with Archbishop Nidaros .
With Christianity, the country got three social powers: the peasants (organized through the things), the king with his officials and the church with the clergy. The things are the oldest institution: At allthings all armed men had the right to attend (in part an obligation to attend) and at lagthings met emissaries from an area (that is, the lagthings were representative assemblies). The Thing both ruled in conflicts and established laws. The laws were memorized by the participants and written down around the year 1000 or later in the Gulationsloven , Frostatingsloven , Eidsivatingsloven and Borgartingsloven . The person who had been successful at the hearing had to see to the implementation of the judgment themselves.
Early Middle Ages (1050s–1184)
The early Middle Ages is considered in Norwegian history to be the period between the end of the Viking Age around 1050 and the coronation of King Sverre in 1184 . The beginning of the period can be dated differently, from around the year 1000 when the Christianization of the country took place and up to 1100 when the Viking Age was over from an archaeological point of view. From 1035 to 1130 it was a time of (relative) internal peace in Norway, even several of the kings attempted campaigns abroad, including in 1066 and 1103 .
During this period, the church's organization was built up. This led to a gradual change in religious customs. Religion went from being a domestic matter to being regulated by common European Christian law and the royal power gained increased power and influence. Slavery (" servitude ") was gradually abolished. The population grew rapidly during this period, as the thousands of farm names ending in -rud show.
The urbanization of Norway is a historical process that has slowly but surely changed Norway from the early Viking Age to today, from a country based on agriculture and sea salvage, to increasingly trade and industry. As early as the ninth century, the country got its first urban community, and in the eleventh century we got the first permanent cities.
In the 1130s, civil war broke out . This was due to a power struggle and that anyone who claimed to be the king's son could claim the right to the throne. The disputes escalated into extensive year-round warfare when Sverre Sigurdsson started a rebellion against the church's and the landmen's candidate for the throne , Magnus Erlingsson .
Emergence of cities
The oldest Norwegian cities probably emerged from the end of the 9th century. Oslo, Bergen and Nidaros became episcopal seats, which stimulated urban development there, and the king built churches in Borg , Konghelle and Tønsberg. Hamar and Stavanger became new episcopal seats and are referred to in the late 12th century as towns together with the trading places Veøy in Romsdal and Kaupanger in Sogn. In the late Middle Ages, Borgund (on Sunnmøre), Veøy (in Romsdalsfjorden) and Vågan (in Lofoten) were referred to as small trading places. Urbanization in Norway occurred in few places compared to the neighboring countries, only 14 places appear as cities before 1350. Stavanger became a bishopric around 1120–1130, but it is unclear whether the place was already a city then. The fertile Jæren and outer Ryfylke were probably relatively densely populated at that time. A particularly large concentration of Irish artefacts from the Viking Age has been found in Stavanger and Nord-Jæren.
It has been difficult to estimate the population in the Norwegian medieval cities, but it is considered certain that the cities grew rapidly in the Middle Ages. Oscar Albert Johnsen estimated the city's population before the Black Death at 20,000, of which 7,000 in Bergen, 3,000 in Nidaros, 2,000 in Oslo and 1,500 in Tunsberg. Based on archaeological research, Lunden estimates that Oslo had around 1,500 inhabitants in 250 households in the year 1300. Bergen was built up more densely and, with the concentration of exports there, became Norway's largest city in a special position for several hundred years. Knut Helle suggests a city population of 20,000 at most in the High Middle Ages, of which almost half in Bergen.
The Bjarkøyretten regulated the conditions in cities (especially Bergen and Nidaros) and in trading places, and for Nidaros had many of the same provisions as the Frostating Act . Magnus Lagabøte's city law replaced the bjarkøretten and from 1276 regulated the settlement in Bergen and with corresponding laws also drawn up for Oslo, Nidaros and Tunsberg. The city law applied within the city's roof area . The City Act determined that the city's public streets consisted of wide commons (perpendicular to the shoreline) and ran parallel to the shoreline, similarly in Nidaros and Oslo. The roads were small streets of up to 3 cubits (1.4 metres) and linked to the individual property. From the Middle Ages, the Norwegian cities were usually surrounded by wooden fences. The urban development largely consisted of low wooden houses which stood in contrast to the relatively numerous and dominant churches and monasteries built in stone.
The City Act and supplementary provisions often determined where in the city different goods could be traded, in Bergen, for example, cattle and sheep could only be traded on the Square, and fish only on the Square or directly from the boats at the quayside. In Nidaros, the blacksmiths were required to stay away from the densely populated areas due to the risk of fire, while the tanners had to stay away from the settlements due to the strong smell. The City Act also attempted to regulate the influx of people into the city (among other things to prevent begging in the streets) and had provisions on fire protection. In Oslo, from the 13th century or earlier, it was common to have apartment buildings consisting of single buildings on a couple of floors around a courtyard with access from the street through a gate room. Oslo's medieval apartment buildings were home to one to four households. In the urban farms, livestock could be kept, including pigs and cows, while pastures and fields were found in the city's rooftops . In the apartment buildings there could be several outbuildings such as warehouses, barns and stables. Archaeological excavations show that much of the buildings in medieval Oslo, Trondheim and Tønsberg resembled the oblong farms that have been preserved at Bryggen in Bergen . The land boundaries in Oslo appear to have persisted for many hundreds of years, in Bergen right from the Middle Ages to modern times.
High Middle Ages (1184–1319)
After civil wars in the 12th century, the country had a relative heyday in the 13th century. Iceland and Greenland came under the royal authority in 1262 , and the Norwegian Empire reached its greatest extent under Håkon IV Håkonsson . The last king of Haraldsätten, Håkon V Magnusson , died sonless in 1319 . Until the 17th century, Norway stretched all the way down to the mouth of Göta älv , which was then Norway's border with Sweden and Denmark.
Just before the Black Death around 1350, there were between 65,000 and 85,000 farms in the country, and there had been a strong growth in the number of farms from 1050, especially in Eastern Norway. In the High Middle Ages, the church or ecclesiastical institutions controlled 40% of the land in Norway, while the aristocracy owned around 20% and the king owned 7%. The church and monasteries received land through gifts from the king and nobles, or through inheritance and gifts from ordinary farmers.
Settlement and demography in the Middle Ages
Before the Black Death, there were more and more farms in Norway due to farm division and clearing. The settlement spread to more marginal agricultural areas higher inland and further north. Eastern Norway had the largest areas to take off and had the most population growth towards the High Middle Ages. Along the coast north of Stad, settlement probably increased in line with the extent of fishing. The Icelandic Rimbegla tells around the year 1200 that the border between Finnmark (the land of the Sami) and resident Norwegians in the interior was at Malangen , while the border all the way out on the coast was at Kvaløya . From the end of the High Middle Ages, there were more Norwegians along the coast of Finnmark and Nord-Troms. In the inner forest and mountain tracts along the current border between Norway and Sweden, the Sami exploited the resources all the way down to Hedmark.
There are no censuses or other records of population and settlement in the Middle Ages. At the time of the Reformation, the population was below 200,000 and only in 1650 was the population at the same level as before the Black Death. When Christianity was introduced after the year 1000, the population was around 200,000. After the Black Death, many farms and settlements were abandoned and deserted, in the most marginal agricultural areas up to 80% of the farms were abandoned. Places such as Skien, Veøy and Borgund (Ålesund) went out of use as trading towns. By the year 1300, the population was somewhere between 300,000 and 560,000 depending on the calculation method. Common methods start from detailed information about farms in each village and compare this with the situation in 1660 when there are good headcounts. From 1300 to 1660, there was a change in the economic base so that the coastal villages received a larger share of the population. The inland areas of Eastern Norway had a relatively larger population in the High Middle Ages than after the Reformation. Kåre Lunden concludes that the population in the year 1300 was close to 500,000, of which 15,000 lived in cities. Lunden believes that the population in 1660 was still slightly lower than the peak before the Black Death and points out that farm settlement in 1660 did not reach the same extent as in the High Middle Ages. In 1660, the population in Troms and Finnmark was 6,000 and 3,000 respectively (2% of the total population), in 1300 these areas had an even smaller share of the country's population and in Finnmark there were hardly any Norwegian-speaking inhabitants. In the High Middle Ages, the climate was more favorable for grain cultivation in the north. Based on the number of farms, the population increased 162% from 1000 to 1300, in Northern and Western Europe as a whole the growth was 200% in the same period.
Late Middle Ages (1319–1537)
Due to repeated plague epidemics, the population was roughly halved and the least productive of the country's farms were laid waste. It took several hundred years before the population again reached the level before 1349 . However, those who survived the epidemics gained more financial resources by sharing. Tax revenues for the state almost collapsed, and a large part of the noble families died out or sank into peasan