This article needs additional citations for verification. (April 2019)
Jönköping County (most of)
Halland County (part of)
Östergötland County (part of)
|• Total||29,400 km2 (11,400 sq mi)|
(31 December 2016)
|• Density||26/km2 (66/sq mi)|
|• Bird||Song thrush|
|Time zone||UTC+1 (CET)|
|• Summer (DST)||UTC+2 (CEST)|
28500-28799, 33000–34999, 35000–36999, 38000–39999, 55000–57999, 59000–59999 (shared with Östergötland)
|Area codes||0370-0372 |
Småland (Swedish pronunciation: [ˈsmǒːland] (listen)) is a historical province (landskap) in southern Sweden. Småland borders Blekinge, Scania (Swedish: Skåne), Halland, Västergötland, Östergötland and the island Öland in the Baltic Sea. The name Småland literally means Small Lands. The Latinized form Smolandia has been used in other languages. The highest point in Småland is Tomtabacken, at 377 metres (1,237 ft). In terms of total area, Småland is of a similar size as Belgium.
The traditional provinces of Sweden no longer serve any governmental purpose, but they do remain important historically and culturally. The province of Småland today is divided almost entirely into the three administrative counties of Jönköping, Kalmar, and Kronoberg. Some few small portions of historic Småland are situated in Halland and Östergötland Counties.
The current coat of arms, granted in 1569, displays a rampant red lion carrying a crossbow, all on a golden background. The arms may be surmounted by a ducal coronet. The blazon in English would be, "Or, a lion rampant gules, langued and armed azure, holding in its front paws a crossbow of the second, bowed and stringed Sable with a bolt argent."
The population of Småland was 754,535 as of 31 December 2016, distributed over five counties as follows:
|Jönköping County, largely||333,923|
|Kalmar County, largely||216,455|
|Kronoberg County, entirely||194,628|
|Halland County, peripherally||7,574|
|Östergötland County, peripherally||1,955|
The land is dominated by a forested high plain in which the soil is mixed with sand and small boulders, making it barren in all but the coastal areas and unsuited for agriculture except in certain locations, most notably the Kalmar plains. The province is rich in lakes and bogs. The coast is marked by bays in the north (with an island archipelago offshore) and cultivated flatlands in the south. In total, cultivated land covers 14%, meadows cover 7%, and forests cover 50% of the surface of the province. Other than lacking deep valleys, the landscape is similar to the Norrland terrain found further north in Sweden.
Småland comprises the central, eastern, and southern parts of the South Swedish highlands. In detail, the topography of Småland is a series of flat surfaces built upon or deformed by a geological dome. The elevated terrain thought to be a buckle formed as result of far-away forces transmitted to Sweden. The main surfaces are the Sub-Cambrian peneplain, the South Småland peneplain and the "200 m peneplain". These surfaces and others are arranged in a stepped sequence called a piedmonttreppen. In eastern Småland, the Sub-Cambrian peneplain dips gently to the sea.[A] To the West, this part of the Sub-Cambrian peneplain terminates along a north–south escarpment (running slightly to the east of Växjö) that separates it from other flat surfaces. Central and northwestern Småland contains strings of isolated hills.
The lakes and rivers of Småland are associated to zones of weak rock, either fractured, weathered, or both. The many lakes in Småland owe their existence to the creation of basins through the stripping of an irregular mantle of weathered rock by glacial erosion. The Lagan and the Nissan drain western Småland, following for most of their courses zones of weak rock associated with the Protogine Zone. Rusken, Rymmen, and Möckeln lakes are aligned with a more eastern branch of the Protogine Zone. Canyons cut into the bedrock are common in central and northern Småland, with the area near Mörlunda containing various particularly narrow (<50 m) canyons.[B]
The climate of Småland is divided between the oceanic climate of coastal areas such as Kalmar and the humid continental climate of the interior higher areas such as Jönköping. Southern interior areas such as Växjö have similar oceanic climates such as the coastline. However, temperature average differences between areas are relatively small, since Småland lies in the continental/oceanic transition zone. Summer daytime averages are similar throughout the province, since all three major urban areas are on average around 22 °C (72 °F) with daytime winter temperatures hovering around the freezing point. The slightly colder nights averaging −5 °C (23 °F) in Jönköping are in keeping with its continental classification. The locality of Målilla has the Swedish and Scandinavian all-time highest-measured temperature with 38 °C (100 °F) on June 1, 1947.
The area was probably populated in the Stone Age from the south, by people moving along the coast up to Kalmar. Småland was populated by Stone Age peoples by at least 6000 BC, since the Alby People are known to have crossed the ice bridge across the Kalmar Strait at that time.
It is named Småland ("small lands") because it was an aggrupation of a dozen little (yet largely independent) territories: Kinda (today a part of Östergötland), Tveta, Vista, Vedbo, Tjust, Sevede, Aspeland, Handbörd, Möre, Värend, Finnveden, and Njudung. Each "small land" had its own law in the Viking age and early Middle Ages and could declare itself neutral in wars that Sweden was involved in — at least if the King had no army present at the parliamentary debate. Around 1350, during the reign of Magnus Eriksson, the first national law code was introduced in Sweden and the historic provinces lost much of their old autonomy.
The city of Kalmar is one of the oldest cities of Sweden. In the medieval period it was the southernmost and the third largest city in Sweden, when it was a center for export of iron, which, in many cases, was handled by German merchants. At that time, Scania and Blekinge were not part of Sweden.
Småland was the center of several peasant rebellions. The most nearly successful was the Dackefejden led by Nils Dacke in 1542 and 1543. When officials of king Gustav Vasa were assaulted and murdered, the king sent small expeditions to pacify the area; but all failed. Dacke was the virtual ruler of large parts of Småland during that Winter, though much troubled by a blockade of supplies, before finally being defeated by larger forces attacking from both Västergötland and Östergötland. He famously defended Kronoberg Castle (now ruined) but was shot while trying to escape to then Danish-ruled Blekinge.
During the 17th and 18 Century Småland saw Christian revival break out, leading to an increase of entrepreneurship, church building and the sending out of missionaries all over the world. To this day, the people of Småland are affected by this activity.
In the 19th century, Småland was afflicted by social and economic turbulence and poverty, and it had substantial emigration to North America. 4,300 Swedish emigrants were recruited to settle in Stamford, Texas, by the family network of the first Swedish emigrant to Texas, Swante M. Swenson, who came from Jönköping.
Overnight between 8 and 9 January 2005 the province suffered serious damage from the storm Gudrun.
Towns with former city status were: Eksjö (chartered around 1400), Gränna (1652), Huskvarna (1911), Jönköping (1284), Kalmar (approximately 1100), Ljungby (1936), Nybro (1932), Nässjö (1914), Oskarshamn (1856), Sävsjö (1947), Tranås (1919), Vetlanda (1920), Vimmerby (approximately 1400), Värnamo (1920), Västervik (approximately 1200), Växjö (1342)
Småland has four national parks:
Compared to much of Sweden, Småland has a higher level of religious intensity and church participation.
Småland is also known for its free churches, although the free church congregations are concentrated in Jönköping County. Most of Kalmar County and Kronoberg County have few or no free church congregations.
Politically Småland is the strongest province for Kristdemokraterna (the Swedish Christian Democratic Party), and both of the last two leaders of the party - Göran Hägglund and Alf Svensson live in Jönköping Municipality in northern Småland.
The Swedish botanist Carl Linnaeus, sw. Carl von Linné (1707–1778), often called the father of taxonomy or "The flower-king", was born in Älmhult in Småland. He gave the twinflower its Latin name based on his own (Latin: Linnaea borealis), because of his particular fondness of it. The flower has become Småland's provincial flower.
The Swedish emigration to North America during the 19th century, is best depicted in a suite of novels by author Vilhelm Moberg, which is also the basis for the musical Kristina from Duvemåla created by Benny Andersson and Björn Ulvaeus of ABBA fame.
In her writing, children's book author Astrid Lindgren often portrayed scenes from her own childhood, growing up on a farm in Småland.
In the 20th century, Småland has been known for its high level of entrepreneurship and low unemployment, especially in the Gnosjö region.
Old Swedish encyclopedia Nordisk familjebok describes the inhabitants of Småland as follows:
- the Smålandian is by nature awake and smart, diligent and hard-working, yet compliant, cunning and crafty, which gives him the advantage of being able to move through life with little means.
A running joke local to Sweden, is that Smålandians are very economical, ranging from modestly frugal to utterly cheap. Ingvar Kamprad, founder of IKEA said that the Smålandians are seen as the Scotsmen of Sweden.
The local language is a Swedish dialect known as Småländska (Smalandian). This may in turn be separated in two main branches, with the northern related to the Götaland dialects and the southern to the Scanian dialects.
For details, see: Districts of Småland
The historical sub-divisions of all Sweden's provinces were through hundreds (Swedish: härad). These were Småland's hundreds:
- Allbo Hundred
- Aspeland Hundred
- Handbörd Hundred
- Kinda Hundred
- Kinnevald Hundred
- Konga Hundred
- Mo Hundred
- Möre Northern Hundred
- Möre Southern Hundred
- Norrvidinge Hundred
- Sevede Hundred
- Stranda Hundred
- Sunnerbo Hundred
- Tjust Northern Hundred
- Tjust Southern Hundred
- Tunalän Hundred
- Tveta Hundred
- Uppvidinge Hundred
- Vedbo Northern Hundred
- Vedbo Southern Hundred
- Vista Hundred
- Västbo Hundred
- Västra Hundred
- Ydre Hundred
- Östbo Hundred
- Östra Hundred
Towns in Småland
Football in the province is administered by Smålands Fotbollförbund.
- "Folkmängd i landskapen den 31 december 2016" (in Swedish). Statistics Sweden. 21 March 2017. Retrieved 26 November 2017.
- Encyclopædia Britannica; Micropaedia Volume IX (1974) p. 278
- This figure is from Nordisk familjebok (see details and link below). A guess would be that meadows have decreased since.
- Lundqvist, Jan (1969). "Landskapet". In Lundqvist, Magnus (ed.). Det Moderna Sverige (in Swedish). Bonniers. pp. 64–67.
- Lidmar-Bergström (1988). "Denudation surfaces of a shield area in southern Sweden". Geografiska Annaler. 70 A (4): 337–350.
- Lidmar-Bergström, Karna; Olvmo, Mats; Bonow, Johan M. (2017). "The South Swedish Dome: a key structure for identification of peneplains and conclusions on Phanerozoic tectonics of an ancient shield". GFF.
- Japsen, Peter; Chalmers, James A.; Green, Paul F.; Bonow, Johan M. (2012). "Elevated, passive continental margins: Not rift shoulders, but expressions of episodic, post-rift burial and exhumation". Global and Planetary Change. 90–91: 73–86. Bibcode:2012GPC....90...73J. doi:10.1016/j.gloplacha.2011.05.004.
- Lidmar-Bergström, K.; Olsson, S.; Roaldset, E. (1999). "Relief features and palaeoweathering remnants in formerly glaciated Scandinavian basement areas". In Thiry, Médard; Simon-Coinçon, Régine (eds.). Palaeoweathering, Palaeosurfaces and Related Continental Deposits. Special publication of the International Association of Sedimentologists. Vol. 27. Blackwell Science Ltd. pp. 275–301. ISBN 0-632 -05311-9.
- Andréasson, Per-Gunnar; Rodhe, Agnes (1992). The Protogine Zone. Geology and mobility during the last 1.5 Ga (PDF) (Report). SKB technical report.
- Persson, Torsten (1977). "Erosion channels and canyons in the central South Swedish Highlands — a short survey" (PDF). Bulletin of the Geological Society of Finland. 49: 11–18. doi:10.17741/bgsf/49.1.003. Retrieved February 18, 2018.
- Olvmo, M. (1992). "Glaciofluvial canyons and their relation to the Late Weiochselian deglaciation in Fennoscandia". Zeitschrift für Geomorphologie. 36 (3): 343–363.
- "Karlmar, Sweden Climate summary". Weatherbase. Retrieved 12 December 2014.
- "Jonkoping, Sweden Climate summary". Weatherbase. Retrieved 12 December 2014.
- "Vaxjo, Sweden Köppen Climate Classification". Weatherbase. Retrieved 12 December 2014.
- "Jonkoping, Sweden temperature averages". Weatherbase. Retrieved 12 December 2014.
- "Hur var vädret?". Swedish Meteorological and Hydrological Institute. Retrieved 12 December 2014.
- "YWAM Småland | Sweden". YWAM Småland. Retrieved 2019-11-13.
- Kulturparken Småland. http://www.kulturparkensmaland.se/22.214.171.124/761/2/ Archived 2016-12-08 at the Wayback Machine;
- Smålänningen är till sin natur vaken och intelligent, flitig och sträfsam, rask och hurtig, men likväl foglig till lynnet, händig och slug, hvilket allt medför åt honom den förmånen, att han äfven med små medel kan taga sig fram i lifvet. . p.62; source as above.
- SSR TSR March 24, 2006
- Visit Småland - Official tourist site (Kronoberg and Jönköping counties)
- Eastern Småland and Öland - Official tourist site (Kalmar County)
- VisitSweden - Sweden's official website for tourism and travel information (in English)
- Travel Smaland