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I found this one within my backlog, totally frustrated that the puffin was facing the wrong way.
Statistics
Length: 26-29cm
Wingspan: 47-63cm
Weight: 320-480g
Average lifespan: 18 years
Conservation status
Classified in the UK as Red under the Birds of Conservation Concern 5: the Red List for Birds (2021). Listed as Vulnerable on the global IUCN Red List of Threatened Species.
When to see
March to August
Puffins are unmistakable birds with their black back and white underparts, distinctive black head with large pale cheeks and their tall, flattened, brightly-coloured bill. Its comical appearance is heightened by its red and black eye-markings and bright orange legs.
Used as a symbol for books and other items, this clown among seabirds is one of the world's favourite birds. With half of the UK population at only a few sites it is an Red List species.
Three Million.... wow! I recall when I had 300,000 views on Flickr and thought that was quite impressive. I am so honored to have such wonderful Flickr contacts. I, in turn, love to see the images you post of this incredibly beautiful world. Thanks to all!
Flickr statistics reported that my picture of a turkey had 211k views yesterday. And Google was the referrer. That could make sense since it is a Thanksgiving photo. But it feels like either a mistake or a testament to the power of Google search. Given that today Google continues to refer to that photo but at more normal levels, I suspect a glitch.
Has anyone experienced a similar thing?
Created for the WPC Week 354
Beautiful Rhino with kind thanks to ~Pegazuz66
Boy with kind thanks to ~iquitcountingstock
*** The rhino is being hunted into extinction and could disappear forever unless we act now. Shocking new statistics show 440 rhinos were brutally killed last year in South Africa alone -- a massive increase on five years ago when just 13 had their horns hacked off. European nations could lead the world to a new plan to save these amazing creatures but they need to hear from us first! ***
You can help the billions of animals across the world who suffer everyday, if you care enough ,
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Whew. The year is ending and went through all my published Flickr photos published this year.
From those I selected 52 photos and created separate photo album of those.
Please check out the Year 2014 album.
As a statistical information, I processed and published 387 photos in Flickr this year. Nowadays it seems that the post-process eats at least the same amount of time than the actual shooting... but that also means it increases the time spent on learning as the selection of photos and how to process them are as infinite subject to study as the shooting.
According to Flickr statistics, my photos have been viewed 380 000 times. Thank you all for that!
Let's hope next year will be at least so awesome as this year for all of us =)
Long exposures of moving water create interesting effects, instead of seeing the water, we see a visual representation of the statistical distribution of where the water has been during that period of time.
It was so exciting getting my first photo in Explore (Dec 1, 2012). People from all over were faving and commenting. I really enjoyed it.
So, I set out to figure out how to do it again. I found advice in the FAQ: take good photos, add tags and location, limit the number of groups to 5 - 15. I also found advice that said to avoid Award Groups. I have done that, but I also see photos in both Explore and Award Groups.
I actively joined the Flickr community ranging far and wide in Flickr groups adding comments and faves where they seemed to fit. If someone gave me a fave or a comment, I always visit their photostream and find a way to interact with them. I have built good Flickr friendships with people who provided good feedback and inspiration.
And it happened! I got into Explore again. And it was exciting all over again.
Over time, I started noticing some patterns. The biggest pattern is the lock out period. Flickr seems to allow 7 or 8 photos into Explore in any 60 day period. You can clearly see it in the chart.
I am still working on what makes the difference between low and high. Some photos just seem to catch fire. Others get into Explore down in the 400s and then drop. But I have not noticed a dramatic difference in the early levels of comments and faves. But once a photo gets upward momentum, it often gets many faves and comments.
I enjoy Explore, but understand that it is only a machine algorithm. I much prefer the interaction with real people. But if you are interested in Explore, here is what I have found.
Also, here is a good resource for info on Explore:
As I've just hit 10 million and have been screenshotting my data regularly, I thought I'd quickly look a the pattern between uploads and explores over time.
It seems that after hitting the 7-8 million views mark, a lot more of my photos started making it onto Explore.
CSV data in case I ever need it again:
Milestone,Date,Totaluploads,Totalexplrs
0,01/12/2009,0,0
0.5,16/10/2014,647,2
1,16/06/2015,686,3
2,10/12/2016,866,9
3,15/02/2018,1046,13
4,21/10/2018,1082,19
5,20/02/2019,1127,19
6,03/09/2019,1195,21
7,07/08/2022,1224,23
8,17/04/2023,1307,38
9,07/05/2024,1426,54
10,01/01/2025,1575,69
Some data from Strava:
112.21 miles (not including get to, or from the starting locations)
2,846 calories burnt
11.6 average miles per hour
09h 42m moving time
16h 07m elapsed time
4,449 ft elevation gain
386 ft max elevation
32.9 mph Max speed
Total over the 2 days: 123.09 miles
Ride time: 10h 49m
The last 30 miles or so was hard work. We completed this ride 5 times now. Every time it was has been a different experience - easier, harder. We've arrived much earlier, and a little later. I always like riding in the pitch black, which doesn't long at in the middle of summer.
The Dunwich Dynamo is a turn-up-and-go challenging free-entry overnight 120 mile bicycle ride on-tarmac from London Fields in Hackney to the lonely Suffolk beach at Dunwich. It’s not a race. It’s unsupported. There’s no van following. It’s a long way.
Minolta SRT 101 + Rokkor 50mm + Fuji Superia XTRA 400
We always think about cities as saturated and disorganized places. In this serie, I´m looking for the minimal, clean and simple expressions that hide among city chaos.
Siempre pensamos en las ciudades como espacios saturados y desordenados. En esta serie busco las expresiones mínimas, limpias y simples que se esconden entre el caos de la ciudad.
Thanks to all the friends who take the time to look at my pictures!
10 million 2018-12-01
11 million 2019-02-08, 1.735 views / public image
12 million 2019-04-23, 1,878 views / public image
13 million 2019-09-17, 1.907 views / public image
14 million 2020-01-20, 1,960 views / public image
15 million 2020-07-06, 2,104 views / public image
16 million 2021-04-16, 2,152 views / public image
17 million 2022-01-11 2,330 views / public image
19 million 2023-08-23 2,631 views / public image
20 million 2024-04-29 2,727 views / public image
Summary of properties of Comet 67P/Churyumov–Gerasimenko, as determined by Rosetta’s instruments during the first few months of its comet encounter. The full range of values are presented and discussed in a series of papers published in the 23 January 2015 issue of the journal Science.
More information: Getting to know Rosetta’s comet: www.esa.int/Our_Activities/Space_Science/Rosetta/Getting_...
Credits for individual results:
Shape model, rotation properties, volume and porosity: OSIRIS
Mass: RSI
Density: RSI/OSIRIS
Dust/Gas ratio: GIADA, MIRO and ROSINA
D/H ratio: ROSINA
Surface temperature: VIRTIS
Subsurface temperature and water vapour production rate: MIRO
Albedo: OSIRIS and VIRTIS
Comet images: NavCam
And now for some 'navel-gazing,' as it were.
As of 26 August 2023, my images on Flickr have been viewed twelve million times. To put that in perspective, I joined Flickr seventeen years ago, in 2006. Since then, I have uploaded 24,841 images for public view. That averages to approximately 705,000 views per year of the 1,460 images I upload per year.
When I began posting photographs and images to Flickr, most of my uploads were 'beer-centric' (often for use at my blog). Since 2016 or so, however, my emphasis has shifted toward nature, 'artsy,' and street photography, if not always successfully so. And, concurrently, the number of my images featuring 'good fermentables' has dropped precipitously.
All of these statistics and observations may be components of a dubious milestone but, nonetheless, I thank all who have visited my Flickr site and all who have 'faved' and/or commented upon my images.
PS. The PRO designation? It means that I pay Flickr for the privilege of posting images there.
***************
▶ HOW I GOT THERE.
☞ Eleven million views on 31 January 2023.
☞ Ten million views on 13 July 2022.
☞ Nine million views on 1 December 2021.
☞ Eight million on 27 April 2021.
☞ Seven million on 25 October 2020.
☞ Six million on 26 April 2020.
☞ Five million on 27 October 2019.
☞ Four million on 7 July 2018.
☞ Three million views on 22 Jun 2016.
☞ My first upload was in 2006.
***************
▶ THE CAMERAS I'VE USED.
Since 2006, I primarily have used six digital cameras —excluding cell phones, 'disposable' film cameras, Palm PDAs, and 'loaners.' They were (are), in order, beginning with my current camera:
4. Canon PowerShot SD400Digital ELPH
5. Canon PowerShot SD980 IS Digital ELPH
***************
▶ Image uploaded by Yours For Good Fermentables.com.
▶ For a larger image, type 'L' (without the quotation marks).
— Follow on Facebook: YoursForGoodFermentables.
— Follow on Instagram: @tcizauskas.
▶ Commercial use requires explicit permission, as per Creative Commons.
The trend line is showing a month on month decrease in graffiti incidents. The peak in mid year was due to school holidays.
I bought a Nikon Z fc in February, so my good, old D800 and my favourite lenses (Sigma 35mm & Sigma 105mm) were not used that much.
Lord Pembrokes Bugatti Veyron and Wilton House. Minus the wrap, but including a new Quiksilver Exhaust...
Comments and Criticisms would be really appreciated! :)
Please like my Facebook Page! :) - www.facebook.com/TPhippsPhotography
Please follow my Instagram Page! :D - www.instagram.com/tphipps_photography
Tom :D
As a software engineer and a hobbyist graphics designer I was terribly disappointed in the #MyFlickrYear highlight card that the Flickr team came up with.
There is so much interesting data stored on this website to draw interesting metrics and conclusions from, but they just went the boring way, repeating what you could mostly check on the stats page anyways.
With that in mind, and with the email linking to my highlight card never arriving in my inbox, I decided to assemble this extended recap of my last year instead.
I also selected my top 25 favourite moments captured in 2021, which you can check out on my profile page or in this album.
To check out all my pictures taken last year, follow this link.
Enjoy!
Have you checked out Google Analytics? I have been using it for about two months on my blog, and it is very interesting to track...
Sure, it's not about quantity, but I do like the graphs :)
The Map Overlay may be my favorite of all! how many people visited the site from Sri Lanka? you can find it out with Google Analytics!
Have you checked out Google Analytics? I have been using it for about two months on my blog, and it is very interesting to track...
Sure, it's not about quantity, but I do like the graphs :)
Flåm is a village in Aurland municipality in Vestland county. Flåm lies deep in the Aurlandsfjorden .
Flåm has 257 inhabitants (SSB, 2022), and mostly consists of scattered wooden buildings. Through the Flåmsdalen flows the Flåmselvi , which originates from the Omnsbreen north of the Hardangerjøkulen. According to Statistics Norway's definition, the conurbation is 0.4 km 2 .
The author Per Sivle was born in Flåm on a farm near Flåm church . There is a memorial to Sivle.
Commercial activities
In 2016, Flåm received 240,000 cruise passengers on day visits, which makes the place one of Norway's largest cruise ports. Some of the world's largest cruise ships have been in Flåm, such as "Queen Mary 2" and "Independence of The Seas" .
In 2017, it was reported that 1.4 million tourists visit Flåm in the course of a year, 90% of these are foreign and 40% from Asia. In 2017, over 250,000 visitors came by cruise ship. For 2018, 153 cruise ship calls with at least the same number of passengers have been reported. In 2018, it was estimated that over 1 million visited Flåm during the year. The tourism industry then had a turnover of around NOK 700 million, up from NOK 80 million in 1998. On some days, the large number of tourists has created congestion and it is being discussed whether it can withstand a larger scale.
Infrastructure
Flåm is particularly famous for the Flåm Railway , which runs between Flåm by the fjord and Myrdal station on the Bergen Railway . Flåmsbana is known for its steep ascent. It rises from 2 m. Flåm station to 870 m above sea level. Myrdal station at 17 kilometers. There is a rise of 5.1%, the maximum rise is south of Dalsbotn, 5.5%. [ needs reference ] From the course there is a view of Flåmsdalen. At Berekvam station there are crossing tracks where the trains from Flåm and Myrdal can cross each other. The train makes a stop at Kjosfossen .
Famous people and demonym
Flåm is also the birthplace of the Norwegian poet and writer Per Sivle .
The Sognefjord is Norway's longest and deepest fjord with its 205 km and 1303 m at its deepest (SNL states 1308), including Sognesjøen which is at the far end towards the North Sea. The Sognefjord has the deepest point on Norway's coast. The fjord is 176–180 km from the innermost Lusterfjorden ( Skjolden ) to Sognefest , and 206 km to the outermost reef (then Lake Sognesjøen is also included). The width varies from around 1 to 2 km in Lusterfjorden to 4–5 km from Leikanger and beyond. Measured from the threshold to Skjolden, the fjord is 174 km. The middle part of the fjord is surrounded by mountains of around 1000 meters and in the inner part the height difference between the bottom of the fjord and the mountain tops is 3500 metres. The highest peak right by the fjord is Bleia at 1,721 metres, which gives a 2,850 meter height difference. Around the inner part of the fjord, the landscape is alpine with pointed mountain peaks, steep mountain sides and glaciers. As an extension of the fjord arms, long and deep valleys extend in all directions, including Jostedalen , Lærdalen and Årdal with Utladalen . The Sognefjord is the world's longest open (ice-free) fjord. The Sognefjord is the world's third longest fjord.
It is located in the middle of Vestland county (formerly Sogn og Fjordane county to which it helped give its name) and stretches from Solund on the coast in the west to Skjolden at the foot of Jotunheimen in the east (northeast), where the fjord arm is called Lustrafjorden . The fjord and the land around it make up the Sogn region, often divided into Outer, Midtre and Indre Sogn. The length from Rutletangen to Skjolden is 186 km . Sogn makes up almost 60% of the area in Sogn and Fjordane, or around 11,000 km 2 . The twelve municipalities in Sogn have a total area of 10,671.55 km² and 37,063 inhabitants (1 January 2014). The land around the inner part of the fjord is called Indre Sogn and includes the long fjord arms. From Leikanger onwards, the country is called Ytre Sogn . The outer part of the fjord has few and small fjord arms. The fjord arms are like hanging valleys under water in that the bottom in the side fjords is often much shallower than the main fjord with a height difference of over 1,000 meters in some cases. The main fjord has a threshold at its mouth to the sea, while several of the side fjords have thresholds at the mouth of the main fjord.
The Sognefjord cuts so deeply into the country that it is only 15 km from the innermost arm at Skjolden to mountain peaks such as Store Skagastølstind in Jotunheimen. The water flow usually exits the fjord. The rivers create sandbanks where they run into the fjord, for example at Gudvangen, in Lærdal and in Gaupne. These sandbars are constantly expanding and changing shape.
The Sognefjord, especially the inner part, is surrounded by mountain massifs which are alpine in the inner part and more rounded in the outer part. The innermost arms of the fjord continue as deep and sometimes long valleys, including Lærdal , Årdal with Utladalen , Nærøydalen , Sogndalsdalen , Fjærland , Fortunsdalen , Aurlandsdalen and Jostedalen . The transition between the fjord and these valleys is determined by sea level, and the boundary has moved outwards at the uplift. Some of the side valleys, such as Vik and Fresvik, would have been hanging valleys in the same way as the Feigedalen if the Sognefjord was drained.
Name
Amund Helland writes " The Sognefjord's real name is Sogn , while Sogn is now used only for the surrounding landscape, and was thus already used in the Middle Ages. As a landscape name, the name is a masculine word and has undoubtedly been so as a fjord name as well." The name is connected to the word "suction", which probably refers to the suction or the difficult current conditions that are created when the water flows through the fjord mouth and over the threshold.
Geography
Large parts of the fjord are surrounded by steep mountains. Kvamsøy at Balestrand is a small island separated from the mainland by a short, shallow strait. Outside Balestrand there are small fjord arms and at Veganes ( Dragsvik ferry quay ) there is a significant branching with the Fjærlandsfjorden .
Municipalities
Municipalities with shoreline to the fjord, counted from west to east:
Solund
Hyllestad (north side)
Gulen (south side)
Høyanger (on both sides of the main fjord)
Vik (south side)
Sogndal (north side)
Aurland (south side, around the Aurlandsfjord)
Lærdal (south side)
Luster (north side, around Lustrafjorden)
Årdal (around the Årdalsfjord)
Depths
The Sognefjord has only one threshold which is at the mouth and the threshold is around 165 meters deep. The area beyond the threshold is called Sognesjøen , which is sheltered by islands to the north and south; there is no threshold outside Sognesjøen that has free circulation towards the ocean.
From the inner parts at Årdal or Skjolden, the fjord gradually deepens outwards (westwards). Between Fodnes-Mannheller and Rutledal-Rysjedalsvika, the bottom is at least 800 metres. The deepest part is approximately at Åkrestrand and Vadheim. The outer part of the fjord (at Losna and Sula ) has a marked threshold with depths of 100 to 200 metres, where the fjord bed rises abruptly from a depth of 1,200 meters to around 100 meters over a stretch of 5 km at Rutledal. In Lake Sognesjøen there are several small troughs (with depths down to 400-500 metres) with thresholds between them. Across the fjord, the bottom is partly completely flat with less than 1 meter variation in depth over a 2 km cross-section. The bottom is covered by fine material (clay) which at Vangsnes is up to 300 meters thick. Seismic shows that the greatest depth to the bedrock is approximately 1,600 m, but loose masses with a thickness of 200–400 m mean that the fjord bottom is nevertheless flat. Seismic surveys at Vangsnes have revealed a 300 meter thick layer of clay at the bottom.
Between 50 and 180 km from the mouth, the fjord bed is relatively flat. Almost all side fjords form hanging valleys to the main fjord. For example, the mouth of the Fjærlandsfjord is well over 400 meters deep, while the main fjord is close to 1,200 meters deep just outside the mouth. Vadheimfjord's mouth is 400 meters deep, here the greatest depth is over 1300 m. Ikjefjord's mouth is only 50 meters deep close to where the main fjord is at its deepest. In large parts of the fjord, it is "abruptly deep" in that the steep mountain sides continue just as steeply underwater.
In contrast to a number of other fjords, not every single part of the Sognefjord has its own name. Only the outermost part has its own name - Sognesjøen . However, there are many fjord arms. From west to east these are:
Sognesjøen
Straumsfjorden
Bjørnefjorden
Nessefjord
The Sognefjord
Lifjorden
Bøfjorden
The Risnefjord
The Ikjefjord
Vadheimsfjorden
Fuglsetfjorden
Høyangsfjorden
Lånefjorden
The Finnafjord
The Arnafjord
The Inner Fjord
Framfjorden
Vikbukti
The Esefjord
Fjærlandsfjorden
The Vetlefjord
Sværefjorden
The Norafjord
Sogndalsfjorden
Barsnes Fjord
The Eidsfjord
Aurlandsfjorden
The Nærøyfjord
Amla Bay
Lærdalsfjorden
Årdalsfjorden
The Lustrafjord
The Gaupnefjord
Climate and fresh water
The fjord colored by meltwater from the glacier.
Terrain formations and distance to the sea lead to great variations in climate along the fjord. The outer part has a mild and humid coastal climate, while the innermost part has an inland climate with cold and dry winters.
The amount of precipitation decreases strongly inwards into the fjord. Lærdal lies in the rain shadow and has very little rainfall, while west-facing slopes further out have a lot of rainfall and there the rainfall often increases with altitude. Brekke and Takle in Ytre Parish are among the places in Norway with the most rainfall. North of the Sognefjord lies the Jostedalsbreen, Norway's largest glacier, and parts of the meltwater drain into the Sognefjord. Wind conditions are strongly influenced by terrain formations. In winter, the dominant wind direction is out the fjord or out the side valleys in the form of so-called downwinds . Fall winds can be very strong and have a major impact on cooling and icing. The slopes and valleys along the inner parts of the fjord have a partially mild climate and are fertile, which makes the area suitable for growing fruit and berries, among other things. The slopes along the fjord partly have large conifer forests, including in the roadless area of Frønningen .
The fjord receives fresh water mainly from the rivers and very little precipitation directly on the fjord's water surface. In the inner part of the Sognefjord, the total supply of fresh water during one year corresponds to a depth of 33 meters if it were distributed over the entire area of the fjord. In spring and partly in autumn, the top 2-3 meters of the fjord are brackish water , especially in the side fjords. The salt content in the surface is lowest in summer and autumn. In June 1954, for example, 5 ‰ salt was measured in the uppermost meters of the Lustrafjord, while at great depths it was 34.5 ‰. Regulation of the waterways for power production has led to a larger proportion of fresh water flowing into the fjord in the winter. The most extensive regulation is in Aurland, Lærdal, Årdal and Jostedal. Regulations affect temperature in the surface layer and icing. In the inner part of the fjord, the rivers are fed by high mountains and glaciers.
The rivers Lærdalselvi , Aurlandselvi , Flåmselvi , Mørkridselvi , Henjaelvi , Grindselvi , Hamreelvi , Njøsaelvi , Kvinnafossen , Sogndalselvi and Jostedøla flow into the Sognefjord and normally have spring floods in June. [3] Lærdalselva has the largest catchment, followed by Jostedøla and Aurlandselva, and these three have roughly the same water flow (around 40 m 3 /second). The Årdalsvatnet drains to the Sognefjord through the short Åreidselva or Hæreidselvi through the Årdalstangen . The Eidsvatnet in Luster drains into the Sognefjord just by Mørkridselvi in Skjolden . Regulation of the waterways for hydropower has resulted in a more steady supply of fresh water throughout the year. Without regulation, 92% of the fresh water would have been supplied in the summer half-year from May to October. Several of the large rivers flow into fjord arms.
Geology
The bedrock along the outer and middle part of the fjord consists mostly of Precambrian gneiss with orientation east-west and northeast-southwest. The islands of Solund consist mostly of Devonian sandstone and conglomerates , while the interior (eastern part) consists mostly of Caledonian gabbro , anorthosite , granite and phyllite .
Jostedøla's material transport (in the form of sludge) involves sedimentation in the Gaupnefjord of 10 to 20 cm/year near the river basin, and 1 cm/year 2 km from the river basin. The river transports 50,000 to 100,000 tonnes of silt annually. The sludge concentration from Jostedøla is at most 1 g/litre. It is particularly at Gaupne that the meltwater from the glaciers is marked by the color of the water.
Icing
According to Helland, it was common for the ice to settle on several of the fjord arms every winter, including on Aurlandsfjorden, Nærøyfjorden and Årdalsfjorden. In the winter of 1888–1889, Lusterfjorden was iced over for six months straight. In the deepest parts of the Sognefjord, there is a year-round temperature of around 6.5 °C, according to Helland. Outer parts are almost never iced over, not even the side fjords. The inner parts can be frozen for several weeks at a stretch. Among other things, inner parts of the Aurlandsfjorden and the Nærøyfjorden freeze easily. Lærdalsfjorden is usually ice-free except for the very innermost part, while it has happened that Årdalsfjorden has been iced up to Ofredal and has been an obstacle to ship traffic. Historically, Lustrafjorden has often been iced over as far as Urnes. The Barsnesfjorden has often been covered with ice. In the Nærøyfjord it happened (among other things in the 1920s and in 1962) that the liner was unable to enter the fjord due to ice and had to dispatch at the ice edge.
Streams
In the Sognefjord, incoming current is hardly noticeable and is most noticeable in strong westerly winds. Outgoing current dominates and is particularly strong in spring and summer. At strong tides, the tidal flow can reach over 1 m/s (2 knots ) around the pier and headland. The Sognefjord is covered by a layer or stream of brackish water of up to 10 meters (varying with the seasons and supply from the rivers). Beneath the brackish water, a current or intermediate layer at a depth of 150 meters goes in and out of the fjord and below this lies the main basin, which has some connection with the ocean beyond the threshold. Together, these three currents contribute to the fact that the water in the fjord is replaced on average within 8-10 years, so that the fjord has life right down to the bottom. The brackish water layer has less density and therefore does not mix easily with the deeper layers. The brackish water that flows out of the fjord slowly mixes with the layer below so that the salt content increases at the same time as the brackish water layer increases up to 10 times the amount of fresh water supplied. The brackish water that flows towards the mouth must be replaced and sets up an incoming current in a slightly deeper layer.
Fish
The Sognefjord has herring and good sprat fishing . In the outer parts of the fjord, salmon has traditionally been fished with wedge nets . Salmon warp or "sitjenet" is a traditional method of salmon fishing and skilled players could catch a lot of fish with this method. Hook nets and drift nets have dominated in modern times and do not require the same active fishing as warp . The salmon's migration in the fjord is controlled by currents on the surface and the warps are placed where there are favorable current conditions where, due to the current, the salmon are driven close to land on their way into the fjord. In Leikanger and Balestrand there are many good places for sitejnot with Suppham being by far the best. Good salmon rivers such as Lærdalselva, Aurlandselva and Årøyelva flow into the Sognefjorden.
In the outer part of the fjord (Gulen and Solund) there is some fish farming. Several of the waterways are known for good salmon and sea trout fishing , and five of the rivers have been designated as national salmon rivers. Lærdalselva has a salmon-carrying stretch and has had by far the largest population. Aurlandselva has historically had a good catch of sea trout. The Sognefjord is among the most important in Norway for anadromous fish species. Norwegian spring-spawning herring are fished in the fjord, especially in the outer parts, as well as some coastal sprat.
In the Sognefjord there are plankton algae which in other Norwegian waters and the occurrence follows the seasons. In general, there is little occurrence in winter due to low light, diatoms bloom in March-April and are dependent on the supply of nutrient salts, in May-June diatoms and flagellates bloom in connection with the spring flood, in summer there is a varying population, new blooms in the autumn in connection with, among other things, floods, and married species can occur all year round.
Tourism
The Sognefjord was established as a tourist destination in the 19th century, among other things, with the establishment of Fylkesbåtane. One of the targets was Gudvangen, which in 1889 received 79 large tourist ships with a total of over 10,000 passengers. In 1889, 4,500 travelers came with the county boats. The German Emperor Wilhelm visited the Sognefjord and Balestrand for the first time in 1890. The emperor subsequently visited the Sognefjord 25 times. The fjord itself and the surrounding area with Jotunheimen, Jostedalsbreen and several stave churches have made the Sognefjord one of Norway's most prominent tourist destinations. Balestrand, Vangsnes, Aurland and Fjærland were among the early destinations for English tourists in the 19th century.
History
It has been the Guest of Death
It has sailed on a Torden
It is christened in Rædsler vorden
that has plowed the Sognefjord
from Forthun to Sognefæst.
If you have forgotten your Lord's Prayer,
do you remember a prayer to pray:
learn it from the wrath of God!
imagine, Sinder, then present
in a Bath on Sognefjord!
Henrik Wergeland
The Sognefjord has been an important transport artery since ancient times. The gulation was probably held near the mouth of the Sognefjord and probably because it was practical to hold the meeting where the ship lay along the coast met the great fjord. From the innermost arms of the fjord it is a relatively short distance to the inland villages of Eastern Norway, particularly through Lærdal to Valdres over the moderate mountain pass Filefjell . Lærdalsøyri was from the 17th century an important market and meeting place. There, farmers from Valdres, Hallingdal and Gudbrandsdalen sold slaughter, tar and other products from the interior and bought fish, salt, hemp and iron from the fjords and from Bergen. Around 1300, the authorities established a shuttle station at Maristova at the entrance to Filefjell. The first drivable road between east and west was built over Filefjell in 1792. From 1843 the paddle steamer "Constitutionen" plyed the route between Bergen and Lærdal, the county boats took over the route in 1857. The road over the Sognefjellet was built as a carriageway in 1938. The Flåmsbana connected the Sognefjord to the railway network in 1940. Stalheimskleivi , between Voss and Sogn, was built in 1850 and turned into a road in 1937. It has made it possible to transport agricultural products , fruit , berries and fish between the villages in Sogn and Bergen .
From 1785, the Trondhjem postal route crossed the Sognefjord by boat between Rutledal and Leirvik in Hyllestad . In 1647, a postal route was established between Bergen and Christiania. The post then took 7-8 days via Gudvangen, Lærdal and Valdres.
It was difficult to get to the Sognefjord by sailboat and the yachts could lie for many days or several weeks at the mouth waiting for favorable wind conditions. East wind was favorable out of the fjord, while south to Bergen, wind from the north or north-west was needed. To enter the fjord, a wind from the west was necessary. The steam and motor boats revolutionized transport on the fjord and these had completely taken over in the early 20th century The county boats were established in 1858 with boat routes on the Sognefjord and to Bergen as an important activity.
In 1934, a ferry route was established along the fjord from Vadheim to Lærdal. From 1939 until the Lærdal tunnel opened, there was a car ferry between Gudvangen and Lærdal - first the ferry went to Lærdalsøyri itself, from 1966 to Revsnes when a road was built there to shorten the ferry route. In the 1990s, the ferry connection Revsnes-Kaupanger was replaced by Mannheller-Fodnes , and after this Kaupanger has only been used by the tourist route Gudvangen-Kaupanger-Lærdal. The road system between Sogndal and Jølster on national highway 5 , including the Fjærlands tunnel , created a ferry-free road connection on the north side of the fjord.
Norway , officially the Kingdom of Norway , is a Nordic , European country and an independent state in the west of the Scandinavian Peninsula . Geographically speaking, the country is long and narrow, and on the elongated coast towards the North Atlantic are Norway's well-known fjords . The Kingdom of Norway includes the main country (the mainland with adjacent islands within the baseline ), Jan Mayen and Svalbard . With these two Arctic areas, Norway covers a land area of 385,000 km² and has a population of approximately 5.5 million (2023). Mainland Norway borders Sweden in the east , Finland and Russia in the northeast .
Norway is a parliamentary democracy and constitutional monarchy , where Harald V has been king and head of state since 1991 , and Jonas Gahr Støre ( Ap ) has been prime minister since 2021 . Norway is a unitary state , with two administrative levels below the state: counties and municipalities . The Sami part of the population has, through the Sami Parliament and the Finnmark Act , to a certain extent self-government and influence over traditionally Sami areas. Although Norway has rejected membership of the European Union through two referendums , through the EEA Agreement Norway has close ties with the Union, and through NATO with the United States . Norway is a significant contributor to the United Nations (UN), and has participated with soldiers in several foreign operations mandated by the UN. Norway is among the states that have participated from the founding of the UN , NATO , the Council of Europe , the OSCE and the Nordic Council , and in addition to these is a member of the EEA , the World Trade Organization , the Organization for Economic Co-operation and Development and is part of the Schengen area .
Norway is rich in many natural resources such as oil , gas , minerals , timber , seafood , fresh water and hydropower . Since the beginning of the 20th century, these natural conditions have given the country the opportunity for an increase in wealth that few other countries can now enjoy, and Norwegians have the second highest average income in the world, measured in GDP per capita, as of 2022. The petroleum industry accounts for around 14% of Norway's gross domestic product as of 2018. Norway is the world's largest producer of oil and gas per capita outside the Middle East. However, the number of employees linked to this industry fell from approx. 232,000 in 2013 to 207,000 in 2015.
In Norway, these natural resources have been managed for socially beneficial purposes. The country maintains a welfare model in line with the other Nordic countries. Important service areas such as health and higher education are state-funded, and the country has an extensive welfare system for its citizens. Public expenditure in 2018 is approx. 50% of GDP, and the majority of these expenses are related to education, healthcare, social security and welfare. Since 2001 and until 2021, when the country took second place, the UN has ranked Norway as the world's best country to live in . From 2010, Norway is also ranked at the top of the EIU's democracy index . Norway ranks third on the UN's World Happiness Report for the years 2016–2018, behind Finland and Denmark , a report published in March 2019.
The majority of the population is Nordic. In the last couple of years, immigration has accounted for more than half of population growth. The five largest minority groups are Norwegian-Poles , Lithuanians , Norwegian-Swedes , Norwegian-Syrians including Syrian Kurds and Norwegian-Pakistani .
Norway's national day is 17 May, on this day in 1814 the Norwegian Constitution was dated and signed by the presidency of the National Assembly at Eidsvoll . It is stipulated in the law of 26 April 1947 that 17 May are national public holidays. The Sami national day is 6 February. "Yes, we love this country" is Norway's national anthem, the song was written in 1859 by Bjørnstjerne Bjørnson (1832–1910).
Norway's history of human settlement goes back at least 10,000 years, to the Late Paleolithic , the first period of the Stone Age . Archaeological finds of settlements along the entire Norwegian coast have so far been dated back to 10,400 before present (BP), the oldest find is today considered to be a settlement at Pauler in Brunlanes , Vestfold .
For a period these settlements were considered to be the remains of settlers from Doggerland , an area which today lies beneath the North Sea , but which was once a land bridge connecting today's British Isles with Danish Jutland . But the archaeologists who study the initial phase of the settlement in what is today Norway reckon that the first people who came here followed the coast along what is today Bohuslân. That they arrived in some form of boat is absolutely certain, and there is much evidence that they could easily move over large distances.
Since the last Ice Age, there has been continuous settlement in Norway. It cannot be ruled out that people lived in Norway during the interglacial period , but no trace of such a population or settlement has been found.
The Stone Age lasted a long time; half of the time that our country has been populated. There are no written accounts of what life was like back then. The knowledge we have has been painstakingly collected through investigations of places where people have stayed and left behind objects that we can understand have been processed by human hands. This field of knowledge is called archaeology . The archaeologists interpret their findings and the history of the surrounding landscape. In our country, the uplift after the Ice Age is fundamental. The history of the settlements at Pauler is no more than fifteen years old.
The Fosna culture settled parts of Norway sometime between 10,000–8,000 BC. (see Stone Age in Norway ). The dating of rock carvings is set to Neolithic times (in Norway between 4000 BC to 1700 BC) and show activities typical of hunters and gatherers .
Agriculture with livestock and arable farming was introduced in the Neolithic. Swad farming where the farmers move when the field does not produce the expected yield.
More permanent and persistent farm settlements developed in the Bronze Age (1700 BC to 500 BC) and the Iron Age . The earliest runes have been found on an arrowhead dated to around 200 BC. Many more inscriptions are dated to around 800, and a number of petty kingdoms developed during these centuries. In prehistoric times, there were no fixed national borders in the Nordic countries and Norway did not exist as a state. The population in Norway probably fell to year 0.
Events in this time period, the centuries before the year 1000, are glimpsed in written sources. Although the sagas were written down in the 13th century, many hundreds of years later, they provide a glimpse into what was already a distant past. The story of the fimbul winter gives us a historical picture of something that happened and which in our time, with the help of dendrochronology , can be interpreted as a natural disaster in the year 536, created by a volcanic eruption in El Salvador .
In the period between 800 and 1066 there was a significant expansion and it is referred to as the Viking Age . During this period, Norwegians, as Swedes and Danes also did, traveled abroad in longships with sails as explorers, traders, settlers and as Vikings (raiders and pirates ). By the middle of the 11th century, the Norwegian kingship had been firmly established, building its right as descendants of Harald Hårfagre and then as heirs of Olav the Holy . The Norwegian kings, and their subjects, now professed Christianity . In the time around Håkon Håkonsson , in the time after the civil war , there was a small renaissance in Norway with extensive literary activity and diplomatic activity with Europe. The black dew came to Norway in 1349 and killed around half of the population. The entire state apparatus and Norway then entered a period of decline.
Between 1396 and 1536, Norway was part of the Kalmar Union , and from 1536 until 1814 Norway had been reduced to a tributary part of Denmark , named as the Personal Union of Denmark-Norway . This staff union entered into an alliance with Napoléon Bonaparte with a war that brought bad times and famine in 1812 . In 1814, Denmark-Norway lost the Anglophone Wars , part of the Napoleonic Wars , and the Danish king was forced to cede Norway to the king of Sweden in the Treaty of Kiel on 14 January of that year. After a Norwegian attempt at independence, Norway was forced into a loose union with Sweden, but where Norway was allowed to create its own constitution, the Constitution of 1814 . In this period, Norwegian, romantic national feeling flourished, and the Norwegians tried to develop and establish their own national self-worth. The union with Sweden was broken in 1905 after it had been threatened with war, and Norway became an independent kingdom with its own monarch, Haakon VII .
Norway remained neutral during the First World War , and at the outbreak of the Second World War, Norway again declared itself neutral, but was invaded by National Socialist Germany on 9 April 1940 .
Norway became a member of the Western defense alliance NATO in 1949 . Two attempts to join the EU were voted down in referendums by small margins in 1972 and 1994 . Norway has been a close ally of the United States in the post-war period. Large discoveries of oil and natural gas in the North Sea at the end of the 1960s led to tremendous economic growth in the country, which is still ongoing. Traditional industries such as fishing are also part of Norway's economy.
Stone Age (before 1700 BC)
When most of the ice disappeared, vegetation spread over the landscape and due to a warm climate around 2000-3000 BC. the forest grew much taller than in modern times. Land uplift after the ice age led to a number of fjords becoming lakes and dry land. The first people probably came from the south along the coast of the Kattegat and overland into Finnmark from the east. The first people probably lived by gathering, hunting and trapping. A good number of Stone Age settlements have been found which show that such hunting and trapping people stayed for a long time in the same place or returned to the same place regularly. Large amounts of gnawed bones show that they lived on, among other things, reindeer, elk, small game and fish.
Flintstone was imported from Denmark and apart from small natural deposits along the southern coast, all flintstone in Norway is transported by people. At Espevær, greenstone was quarried for tools in the Stone Age, and greenstone tools from Espevær have been found over large parts of Western Norway. Around 2000-3000 BC the usual farm animals such as cows and sheep were introduced to Norway. Livestock probably meant a fundamental change in society in that part of the people had to be permanent residents or live a semi-nomadic life. Livestock farming may also have led to conflict with hunters.
The oldest traces of people in what is today Norway have been found at Pauler , a farm in Brunlanes in Larvik municipality in Vestfold . In 2007 and 2008, the farm has given its name to a number of Stone Age settlements that have been excavated and examined by archaeologists from the Cultural History Museum at UiO. The investigations have been carried out in connection with the new route for the E18 motorway west of Farris. The oldest settlement, located more than 127 m above sea level, is dated to be about 10,400 years old (uncalibrated, more than 11,000 years in real calendar years). From here, the ice sheet was perhaps visible when people settled here. This locality has been named Pauler I, and is today considered to be the oldest confirmed human traces in Norway to date. The place is in the mountains above the Pauler tunnel on the E18 between Larvik and Porsgrunn . The pioneer settlement is a term archaeologists have adopted for the oldest settlement. The archaeologists have speculated about where they came from, the first people in what is today Norway. It has been suggested that they could come by boat or perhaps across the ice from Doggerland or the North Sea, but there is now a large consensus that they came north along what is today the Bohuslän coast. The Fosna culture , the Komsa culture and the Nøstvet culture are the traditional terms for hunting cultures from the Stone Age. One thing is certain - getting to the water was something they mastered, the first people in our country. Therefore, within a short time they were able to use our entire long coast.
In the New Stone Age (4000 BC–1700 BC) there is a theory that a new people immigrated to the country, the so-called Stone Ax People . Rock carvings from this period show motifs from hunting and fishing , which were still important industries. From this period, a megalithic tomb has been found in Østfold .
It is uncertain whether there were organized societies or state-like associations in the Stone Age in Norway. Findings from settlements indicate that many lived together and that this was probably more than one family so that it was a slightly larger, organized herd.
Finnmark
In prehistoric times, animal husbandry and agriculture were of little economic importance in Finnmark. Livelihoods in Finnmark were mainly based on fish, gathering, hunting and trapping, and eventually domestic reindeer herding became widespread in the Middle Ages. Archaeological finds from the Stone Age have been referred to as the Komsa culture and comprise around 5,000 years of settlement. Finnmark probably got its first settlement around 8000 BC. It is believed that the coastal areas became ice-free 11,000 years BC and the fjord areas around 9,000 years BC. after which willows, grass, heather, birch and pine came into being. Finnmarksvidda was covered by pine forest around 6000 BC. After the Ice Age, the land rose around 80 meters in the inner fjord areas (Alta, Tana, Varanger). Due to ice melting in the polar region, the sea rose in the period 6400–3800 BC. and in areas with little land elevation, some settlements from the first part of the Stone Age were flooded. On Sørøya, the net sea level rise was 12 to 14 meters and many residential areas were flooded.
According to Bjørnar Olsen , there are many indications of a connection between the oldest settlement in Western Norway (the " Fosnakulturen ") and that in Finnmark, but it is uncertain in which direction the settlement took place. In the earliest part of the Stone Age, settlement in Finnmark was probably concentrated in the coastal areas, and these only reflected a lifestyle with great mobility and no permanent dwellings. The inner regions, such as Pasvik, were probably used seasonally. The archaeologically proven settlements from the Stone Age in inner Finnmark and Troms are linked to lakes and large watercourses. The oldest petroglyphs in Alta are usually dated to 4200 BC, that is, the Neolithic . Bjørnar Olsen believes that the oldest can be up to 2,000 years older than this.
From around 4000 BC a slow deforestation of Finnmark began and around 1800 BC the vegetation distribution was roughly the same as in modern times. The change in vegetation may have increased the distance between the reindeer's summer and winter grazing. The uplift continued slowly from around 4000 BC. at the same time as sea level rise stopped.
According to Gutorm Gjessing, the settlement in Finnmark and large parts of northern Norway in the Neolithic was semi-nomadic with movement between four seasonal settlements (following the pattern of life in Sami siida in historical times): On the outer coast in summer (fishing and seal catching) and inland in winter (hunting for reindeer, elk and bear). Povl Simonsen believed instead that the winter residence was in the inner fjord area in a village-like sod house settlement. Bjørnar Olsen believes that at the end of the Stone Age there was a relatively settled population along the coast, while inland there was less settlement and a more mobile lifestyle.
Bronze Age (1700 BC–500 BC)
Bronze was used for tools in Norway from around 1500 BC. Bronze is a mixture of tin and copper , and these metals were introduced because they were not mined in the country at the time. Bronze is believed to have been a relatively expensive material. The Bronze Age in Norway can be divided into two phases:
Early Bronze Age (1700–1100 BC)
Younger Bronze Age (1100–500 BC)
For the prehistoric (unwritten) era, there is limited knowledge about social conditions and possible state formations. From the Bronze Age, there are large burial mounds of stone piles along the coast of Vestfold and Agder, among others. It is likely that only chieftains or other great men could erect such grave monuments and there was probably some form of organized society linked to these. In the Bronze Age, society was more organized and stratified than in the Stone Age. Then a rich class of chieftains emerged who had close connections with southern Scandinavia. The settlements became more permanent and people adopted horses and ard . They acquired bronze status symbols, lived in longhouses and people were buried in large burial mounds . Petroglyphs from the Bronze Age indicate that humans practiced solar cultivation.
Finnmark
In the last millennium BC the climate became cooler and the pine forest disappears from the coast; pine forests, for example, were only found in the innermost part of the Altafjord, while the outer coast was almost treeless. Around the year 0, the limit for birch forest was south of Kirkenes. Animals with forest habitats (elk, bear and beaver) disappeared and the reindeer probably established their annual migration routes sometime at that time. In the period 1800–900 BC there were significantly more settlements in and utilization of the hinterland was particularly noticeable on Finnmarksvidda. From around 1800 BC until year 0 there was a significant increase in contact between Finnmark and areas in the east including Karelia (where metals were produced including copper) and central and eastern Russia. The youngest petroglyphs in Alta show far more boats than the earlier phases and the boats are reminiscent of types depicted in petroglyphs in southern Scandinavia. It is unclear what influence southern Scandinavian societies had as far north as Alta before the year 0. Many of the cultural features that are considered typical Sami in modern times were created or consolidated in the last millennium BC, this applies, among other things, to the custom of burying in brick chambers in stone urns. The Mortensnes burial ground may have been used for 2000 years until around 1600 AD.
Iron Age (c. 500 BC–c. 1050 AD)
The Einangsteinen is one of the oldest Norwegian runestones; it is from the 4th century
Simultaneous production of Vikings
Around 500 years BC the researchers reckon that the Bronze Age will be replaced by the Iron Age as iron takes over as the most important material for weapons and tools. Bronze, wood and stone were still used. Iron was cheaper than bronze, easier to work than flint , and could be used for many purposes; iron probably became common property. Iron could, among other things, be used to make solid and sharp axes which made it much easier to fell trees. In the Iron Age, gold and silver were also used partly for decoration and partly as means of payment. It is unknown which language was used in Norway before our era. From around the year 0 until around the year 800, everyone in Scandinavia (except the Sami) spoke Old Norse , a North Germanic language. Subsequently, several different languages developed in this area that were only partially mutually intelligible. The Iron Age is divided into several periods:
Early Iron Age
Pre-Roman Iron Age (c. 500 BC–c. 0)
Roman Iron Age (c. 0–c. AD 400)
Migration period (approx. 400–600). In the migration period (approx. 400–600), new peoples came to Norway, and ruins of fortress buildings etc. are interpreted as signs that there has been talk of a violent invasion.
Younger Iron Age
Merovingian period (500–800)
The Viking Age (793–1066)
Norwegian Vikings go on plundering expeditions and trade voyages around the coastal countries of Western Europe . Large groups of Norwegians emigrate to the British Isles , Iceland and Greenland . Harald Hårfagre starts a unification process of Norway late in the 8th century , which was completed by Harald Hardråde in the 1060s . The country was Christianized under the kings Olav Tryggvason , fell in the battle of Svolder ( 1000 ) and Olav Haraldsson (the saint), fell in the battle of Stiklestad in 1030 .
Sources of prehistoric times
Shrinking glaciers in the high mountains, including in Jotunheimen and Breheimen , have from around the year 2000 uncovered objects from the Viking Age and earlier. These are objects of organic material that have been preserved by the ice and that elsewhere in nature are broken down in a few months. The finds are getting older as the melting makes the archaeologists go deeper into the ice. About half of all archaeological discoveries on glaciers in the world are made in Oppland . In 2013, a 3,400-year-old shoe and a robe from the year 300 were found. Finds at Lomseggen in Lom published in 2020 revealed, among other things, well-preserved horseshoes used on a mountain pass. Many hundreds of items include preserved clothing, knives, whisks, mittens, leather shoes, wooden chests and horse equipment. A piece of cloth dated to the year 1000 has preserved its original colour. In 2014, a wooden ski from around the year 700 was found in Reinheimen . The ski is 172 cm long and 14 cm wide, with preserved binding of leather and wicker.
Pytheas from Massalia is the oldest known account of what was probably the coast of Norway, perhaps somewhere on the coast of Møre. Pytheas visited Britannia around 325 BC. and traveled further north to a country by the "Ice Sea". Pytheas described the short summer night and the midnight sun farther north. He wrote, among other things, that people there made a drink from grain and honey. Caesar wrote in his work about the Gallic campaign about the Germanic tribe Haruders. Other Roman sources around the year 0 mention the land of the Cimbri (Jutland) and the Cimbri headlands ( Skagen ) and that the sources stated that Cimbri and Charyds lived in this area. Some of these peoples may have immigrated to Norway and there become known as hordes (as in Hordaland). Sources from the Mediterranean area referred to the islands of Scandia, Scandinavia and Thule ("the outermost of all islands"). The Roman historian Tacitus wrote around the year 100 a work about Germania and mentioned the people of Scandia, the Sviones. Ptolemy wrote around the year 150 that the Kharudes (Hordes) lived further north than all the Cimbri, in the north lived the Finnoi (Finns or Sami) and in the south the Gutai (Goths). The Nordic countries and Norway were outside the Roman Empire , which dominated Europe at the time. The Gothic-born historian Jordanes wrote in the 5th century about 13 tribes or people groups in Norway, including raumaricii (probably Romerike ), ragnaricii ( Ranrike ) and finni or skretefinni (skrid finner or ski finner, i.e. Sami) as well as a number of unclear groups. Prokopios wrote at the same time about Thule north of the land of the Danes and Slavs, Thule was ten times as big as Britannia and the largest of all the islands. In Thule, the sun was up 40 days straight in the summer. After the migration period , southern Europeans' accounts of northern Europe became fuller and more reliable.
Settlement in prehistoric times
Norway has around 50,000 farms with their own names. Farm names have persisted for a long time, over 1000 years, perhaps as much as 2000 years. The name researchers have arranged different types of farm names chronologically, which provides a basis for determining when the place was used by people or received a permanent settlement. Uncompounded landscape names such as Haug, Eid, Vik and Berg are believed to be the oldest. Archaeological traces indicate that some areas have been inhabited earlier than assumed from the farm name. Burial mounds also indicate permanent settlement. For example, the burial ground at Svartelva in Løten was used from around the year 0 to the year 1000 when Christianity took over. The first farmers probably used large areas for inland and outland, and new farms were probably established based on some "mother farms". Names such as By (or Bø) show that it is an old place of residence. From the older Iron Age, names with -heim (a common Germanic word meaning place of residence) and -stad tell of settlement, while -vin and -land tell of the use of the place. Farm names in -heim are often found as -um , -eim or -em as in Lerum and Seim, there are often large farms in the center of the village. New farm names with -city and -country were also established in the Viking Age . The first farmers probably used the best areas. The largest burial grounds, the oldest archaeological finds and the oldest farm names are found where the arable land is richest and most spacious.
It is unclear whether the settlement expansion in Roman times, migrations and the Iron Age is due to immigration or internal development and population growth. Among other things, it is difficult to demonstrate where in Europe the immigrants have come from. The permanent residents had both fields (where grain was grown) and livestock that grazed in the open fields, but it is uncertain which of these was more important. Population growth from around the year 200 led to more utilization of open land, for example in the form of settlements in the mountains. During the migration period, it also seems that in parts of the country it became common to have cluster gardens or a form of village settlement.
Norwegian expansion northwards
From around the year 200, there was a certain migration by sea from Rogaland and Hordaland to Nordland and Sør-Troms. Those who moved settled down as a settled Iron Age population and became dominant over the original population which may have been Sami . The immigrant Norwegians, Bumen , farmed with livestock that were fed inside in the winter as well as some grain cultivation and fishing. The northern border of the Norwegians' settlement was originally at the Toppsundet near Harstad and around the year 500 there was a Norwegian settlement to Malangsgapet. That was as far north as it was possible to grow grain at the time. Malangen was considered the border between Hålogaland and Finnmork until around 1400 . Further into the Viking Age and the Middle Ages, there was immigration and settlement of Norwegian speakers along the coast north of Malangen. Around the year 800, Norwegians lived along the entire outer coast to Vannøy . The Norwegians partly copied Sami livelihoods such as whaling, fur hunting and reindeer husbandry. It was probably this area between Malangen and Vannøy that was Ottar from the Hålogaland area. In the Viking Age, there were also some Norwegian settlements further north and east. East of the North Cape are the scattered archaeological finds of Norwegian settlement in the Viking Age. There are Norwegian names for fjords and islands from the Viking Age, including fjord names with "-anger". Around the year 1050, there were Norwegian settlements on the outer coast of Western Finnmark. Traders and tax collectors traveled even further.
North of Malangen there were Norse farming settlements in the Iron Age. Malangen was considered Finnmark's western border until 1300. There are some archaeological traces of Norse activity around the coast from Tromsø to Kirkenes in the Viking Age. Around Tromsø, the research indicates a Norse/Sami mixed culture on the coast.
From the year 1100 and the next 200–300 years, there are no traces of Norwegian settlement north and east of Tromsø. It is uncertain whether this is due to depopulation, whether it is because the Norwegians further north were not Christianized or because there were no churches north of Lenvik or Tromsø . Norwegian settlement in the far north appears from sources from the 14th century. In the Hanseatic period , the settlement was developed into large areas specialized in commercial fishing, while earlier (in the Viking Age) there had been farms with a combination of fishing and agriculture. In 1307 , a fortress and the first church east of Tromsø were built in Vardø . Vardø became a small Norwegian town, while Vadsø remained Sami. Norwegian settlements and churches appeared along the outermost coast in the Middle Ages. After the Reformation, perhaps as a result of a decline in fish stocks or fish prices, there were Norwegian settlements in the inner fjord areas such as Lebesby in Laksefjord. Some fishing villages at the far end of the coast were abandoned for good. In the interior of Finnmark, there was no national border for a long time and Kautokeino and Karasjok were joint Norwegian-Swedish areas with strong Swedish influence. The border with Finland was established in 1751 and with Russia in 1826.
On a Swedish map from 1626, Norway's border is indicated at Malangen, while Sweden with this map showed a desire to control the Sami area which had been a common area.
The term Northern Norway only came into use at the end of the 19th century and administratively the area was referred to as Tromsø Diocese when Tromsø became a bishopric in 1840. There had been different designations previously: Hålogaland originally included only Helgeland and when Norse settlement spread north in the Viking Age and the Middle Ages, Hålogaland was used for the area north approximately to Malangen , while Finnmark or "Finnmarken", "the land of the Sami", lay outside. The term Northern Norway was coined at a cafe table in Kristiania in 1884 by members of the Nordlændingernes Forening and was first commonly used in the interwar period as it eventually supplanted "Hålogaland".
State formation
The battle in Hafrsfjord in the year 872 has long been regarded as the day when Norway became a kingdom. The year of the battle is uncertain (may have been 10-20 years later). The whole of Norway was not united in that battle: the process had begun earlier and continued a couple of hundred years later. This means that the geographical area became subject to a political authority and became a political unit. The geographical area was perceived as an area as it is known, among other things, from Ottar from Hålogaland's account for King Alfred of Wessex around the year 880. Ottar described "the land of the Norwegians" as very long and narrow, and it was narrowest in the far north. East of the wasteland in the south lay Sveoland and in the north lay Kvenaland in the east. When Ottar sailed south along the land from his home ( Malangen ) to Skiringssal, he always had Norway ("Nordveg") on his port side and the British Isles on his starboard side. The journey took a good month. Ottar perceived "Nordveg" as a geographical unit, but did not imply that it was a political unit. Ottar separated Norwegians from Swedes and Danes. It is unclear why Ottar perceived the population spread over such a large area as a whole. It is unclear whether Norway as a geographical term or Norwegians as the name of a ethnic group is the oldest. The Norwegians had a common language which in the centuries before Ottar did not differ much from the language of Denmark and Sweden.
According to Sverre Steen, it is unlikely that Harald Hårfagre was able to control this entire area as one kingdom. The saga of Harald was written 300 years later and at his death Norway was several smaller kingdoms. Harald probably controlled a larger area than anyone before him and at most Harald's kingdom probably included the coast from Trøndelag to Agder and Vestfold as well as parts of Viken . There were probably several smaller kingdoms of varying extent before Harald and some of these are reflected in traditional landscape names such as Ranrike and Ringerike . Landscape names of "-land" (Rogaland) and "-mark" (Hedmark) as well as names such as Agder and Sogn may have been political units before Harald.
According to Sverre Steen, 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 t
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