The Info List - Gudbrandsdal

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(English: Gudbrand Valley[1][2][3]) is a valley and traditional district in the Norwegian county of Oppland. The valley is oriented in a north-westerly direction from Lillehammer
and the lake of Mjøsa, extending 230 kilometers (140 mi) toward Romsdalen. The river of Gudbrandsdalslågen
(Lågen) flows through the valley, starting from Lesjaskogsvatnet
and ending at Mjøsa. The Otta river flowing through Otta valley is a major tributary to Lågen. The valleys of the tributary rivers such as Otta and Gausa (Gausdal) are usually regarded as part of Gudbrandsdalen. The total area of the valley is calculated from the areas of the related municipalities.[4] Gudbrandsdalen
is the main valley in a web of smaller valleys. On the western (right hand) side there are long adjacent valleys: Ottadalen stretches 100 km from Otta village, Gausdal
some 50 km from Lillehammer
and Heidal
some 40 km from Sjoa.[5] Together with Glomma
river and Østerdalen, Lågen and the Gudbrand Valley
forms Norway's largest drainage system covering major parts of East Norway. The Gudbrand Valley
is home to Dovre
Line and the E6 road, and is the main land transport corridor through South Norway, from Oslo
and central eastern lowlands to Trondheim
and Møre og Romsdal. The valley is divided into three parts: Norddalen (the municipalities of Lesja, Dovre, Skjåk, Lom, Vågå
and Sel), Midtdalen (the municipalities of Nord-Fron, Sør-Fron
and Ringebu), and Sørdalen (the municipalities of Øyer, Gausdal
and Lillehammer). The valley has two district courts, north and south.[4] Until 2016 the valley was also a police district.[6] The Gudbrandsdalen
district covers about 60 % of Oppland
county.[5] The main character in Henrik Ibsen's play Peer Gynt
Peer Gynt
was inspired by a real or legendary person living in the valley in the 18th or 17th century.[7] Ibsen travelled through the valley in 1862 and collected local stories, legends and poems.[8] Ibsen also made drawings from his trip, including "Elstad in Gudbrandsdalen".[5]


1 Etymology 2 Geography 3 Geology 4 History

4.1 Legendary history 4.2 Older history 4.3 Modern history

5 Towns 6 Mountain areas close to the valley 7 See also 8 References 9 External links


Depiction of King Olaf II speaking to peasants at the thing, Hundorp. Halfdan Egedius, 1899.

The name Gudbrandsdalen
means 'the valley/dale of Gudbrand'. Gudbrand ( Old Norse
Old Norse
Guðbrandr) is an old male name compounded of guð, 'god' and brandr, 'sword'. The name may be derived from a chief (hersir) called Gudbrand. According to Snorri Sturluson
Snorri Sturluson
the district was also referred to as i Dalom ("in the valleys") because of the many valleys.[5] Dale-Gudbrand
settled in Hundorp, Sør-Fron.[9][10] At the time of Halfdan the Black
Halfdan the Black
there was a "chief Gudbrand north in Gubrandsdalen" (Gudbrand herse nord i Dalom). Later Eric Bloodaxe
Eric Bloodaxe
had an opponent called Dale-Gudbrand. According to the sage Olaf II of Norway
met one Dale-Gudbrand, supposedly the last Dale-Gudbrand, in 1021. Historians believe there was a regional centre at Hundorp during the Viking era and that the name Gudbrand was used for many generations by the ruling family. Burial mounds (tumulus) at Hundorp suggest that powerful men are buried there.[5] Geography[edit] Gudbrand Valley
includes the most arid area in Norway. At Skjåk
the average annual precipitation is only 278 mm.[11] Gudbrand Valley sits in the rain shadow of the mountains West (including Jotunheimen), North and East of the valley.[12] The valley is less incised than the valleys of western Norway.[13] Farming is mostly confined to the relatively narrow valleys. Gudbrandsdalen
and adjacent valleys are surrounded by wide uplands and mountain plateaus traditional used as seter or summer farms.[5]

Patchwork farmland created by draining the shallow lake at Lesja
east of the church.

A 1799 hand-drawn map of the valley. The previous lake at Lesja visible.

In July 1789 the Storofsen flood disaster occurred and Gudbrandsdalslågen
overflooded. This is the largest flood recorded in Norway
and the valley was particularly affected. 61 people perished. About 3000 houses were totally damaged and some thousand livestock drowned. All bridges disappeared.[14][15] Lågen rose up to 7 meters above its normal level and covered most of the valley floor.[12] A number of farmers abandoned their damaged farms and settled in Målselv, Troms
county.[15][14] The second largest flood occurred in the summer of 1995 and again the valley floor was largely covered by water. After Storofsen the valley floor upstream from Sel
church changed into bogs and shallow lakes because stone and gravel changed the flow of Lågen. From around 1910 drainage efforts left some 500 hectar dry farmland on what is still known as the Sel
bogs. The toxic cicuta virosa thrived on those bogs before they were drained and are known in Norwegian as selsnepe (literally Sel
turnip). The valley floor in Lesja
(between Dombås and Lora) were originally covered by a shallow lake. Drainage efforts from 1860 abolished the lake and left some 1000 hectar farmland.[14] The central part of the valley is covered by the Losna lake, some 50–60 meters deep. Geology[edit] The valley of Gudbrandsdalen
is of considerable antiquity considering the overall development of the relief of Norway. The valley runs across the height axis of the southern Scandinavian Mountains
Scandinavian Mountains
—a characteristic that could be indicating that the valley formed before the tectonic uplift of Norway.[13] The valley is one of several valleys of southern Norway
that existed already as part of the ancient Paleic relief but had at the time gentler slopes.[16] Gudbrandsdalen formed and developed originally as a valley of fluvial origin. Only millions of year later was the valley re-shaped by glaciers during the Quaternary period.[13] As the Fennoscandian Ice Sheet melted and retreated during the end of the last ice age a large but ephemeral ice-dammed lake formed in the valley.[17] History[edit] The Gudbrand Valley
was shaped by the recent ice age and rivers from the present glacial areas in Jotunheimen
and Dovre. Bones and teeth from mammoths and musk oxen, living in the area at that time, are found in the valley. Several traces of hunters from the Stone Age
Stone Age
are found in the valley (and in the mountain areas around). There is a rock carving of elks in the northern part of Lillehammer.[18] Gudbrandsdalen
has always hosted the main road between Trondheim
and the central eastern lowlands. In Old Norse
Old Norse
known as þjóðvegr (tjodvei), "people's road" or "everybody's road".[5] Legendary history[edit]

The Battle of Kringen, depicted by Georg Nielsen Strømdal (1856-1914)

Raum the Old was the father of Dale-Gudbrand, and he settled in Hundorp. The Gudbrand Valley
is mentioned extensively in the Heimskringla
(Chronicle of the Kings of Norway) by Snorri Sturluson. The account of King Olaf's (A.D. 1015-1021) conversion of Dale-Gudbrand
to Christianity
is popularly recognized. According to the saga Gudbrand built a church there "in the valleys", possibly at Haave farm near Hundorp where archaeological evidence indicates what may have been the first church in the valley.[5] In 1206, the heir to the Norwegian throne, Håkon Håkonsson, was saved by birkebeiners with a ski-run from Lillehammer
to Rena. Until the Black Plague
Black Plague
settlement expanded and new farms were established at outskirts. Farms with names -gard, -rud, -hus, and -li are mostly from this expansion period. During the High Middle Ages about 40 churches existed, most built in wood except for instances masonry churches in Easter Gausdal
and Follebu. Hamar episcopal see was established in 1152 and its jurisdiction included Gudbrandsdalen. Garmo stave church
Garmo stave church
and Ringebu
Stave Church are examples of ancient wooden churches. Fåvang stave church
Fåvang stave church
and Vågå
Church include parts from older churches. The Black Plague
Black Plague
reduced the population in Gudbrandsdal by 50 to 70 % during 1349 to 1350. Saksum, Brekkom, Skåbo, Venabygd and other districts were left largely deserted for centuries. Inhabitants from marginal areas presumably relocated to the main valley and other areas with vacant land. A large number of clergy also perished during the plague and churches fell into disrepair. During the 1600s the population again reached the same level as in 1300. During the 1500s the area had about 6000 inhabitants. No census was taken before 1665 and population figures are based on estimates.[5] This resulted in a temporary improvement for the lower classes as crofters became scarce and the poor were able to rent the better farms.[5] Older history[edit] During the Reformation in 1537, the Church of Norway
was subordinated to the lendmenn or sheriffs. Church property was appropriated by the Crown and the King became the biggest landowner in the Gudbrand Valley. The Battle of Kringen
Battle of Kringen
took place in 1612, near Otta, Norway, and the local "Gudbrandsdøls" defeated a Scottish mercenary army. The legends of this battle live on to this day, including the story of how the peasant girl Prillar-Guri
lured the Scots into an ambush by playing the traditional ram's horn.[citation needed] The 1665 census indicates a population of 13,000.[5]

German Ju-52 shot down at Dombås, April 1940

In 1670 to 1725, most of the royal property was sold off to pay for war debts, first to established property holders, but increasingly to peasant proprietors. A freeholders' era began and a new "upper class" of land holders was formed. Storofsa happened in 1789, and is the greatest flood recorded in the Gudbrand Valley; several farms were devastated, and many people died.[citation needed] Modern history[edit] In 1827, the city of Lillehammer
is established. The paddle steamer Skibladner
on Mjøsa
and Hovedbanen
(the first railroad in Norway) connected the Gudbrand Valley
to Christiania in 1856. The Hamar-Selbanen railway was completed to Tretten in 1894. Hamar-Selbanen changed its name to the Dovre
Line 1921, and the new main railway between Oslo
and Trondheim, was completed through the Gudbrand Valley. The outdoor museum of Maihaugen, exhibiting old houses from all parts of the Gudbrand Valley, opened at Lillehammer
in 1904.[citation needed] From around 1865 the population declined substantially because of emigration to North-America. Until 1946 the majority of inhabitants worked in farming.[5] There was severe fighting in the valley at Tretten and Kvam, as well as in Dombås, during World War II. The Battle of Dombås
Battle of Dombås
was an attempt to stop the German advance. British troops engaged German troops in land battles for the first time in World War 2 after many months of Phoney War.[19] The 1994 Winter Olympics
1994 Winter Olympics
were celebrated at Lillehammer. Towns[edit]

Lillehammer Ringebu Otta

Mountain areas close to the valley[edit]

Jotunheimen Rondane Dovre

See also[edit]

Gudbrandsdalsost Gudbrandsdalsbunad Dølahest
(Dole Gudbrandsdal) Dølafe


^ Jenkins, J Geraint. 1972. The Use of Artifacts and Folk Art in the Folk Museum. In: Richard M. Dorson (ed.), Folklore and Folklife: An Introduction, pp. 497–516. Chicago: University of Chicago Press, p. 513. ^ Hesse, David. 2014. Warrior Dreams: Playing Scotsmen in Mainland Europe. Manchester: Manchester University Press, p. 147. ^ Art of California. 1990. Saint Helena, CA: Greg Saffell Communications. p. 59. ^ a b https://snl.no/Gudbrandsdalen ^ a b c d e f g h i j k l Gudbrandsdalen. Oslo: Gyldendal, 1974. ISBN 8205062846. ^ http://www.nettavisen.no/politikk/direkte-slik-blir-politireformen/3422793443.html ^ Meyer, Michael. 1974. Ibsen: A Biography. Abridged edition. Pelican Biographies ser. Harmondsworth: Penguin. ISBN 0-14-021772-X. ^ Østvedt, Einar (1967). Med Henrik Ibsen
Henrik Ibsen
i fjellheimen. Skien: Oluf Rasmussens forlag. ^ "dialekter i Gudbrandsdalen". snl.no. Retrieved 2 July 2015.  ^ "Gudbrandsdalen". snl.no. Retrieved 2 July 2015.  ^ "Norges våteste og tørreste steder". NRK (in Norwegian). 2013-07-11. Retrieved 2017-01-21.  ^ a b Østmoe, Arne (1985). Stor-ofsen 1789. Værsystemet som førte til den største flomkatastrofen i Norge (in Norwegian). Ski: Oversiktsregisteret. ISBN 8273790010.  ^ a b c Bonow, Johan Mauritz; Lidmar-Bergström, Karna; Näslund, Jens-Ove (2007). "Palaeosurfaces and major valleys in the area of Kjølen Mountains, southern Norway
– a concequence of uplift and climatic change". Norwegian Journal of Geography. 57: 83–101.  ^ a b c Andersen, Bård (1996). Flomsikring i 200 år. [Oslo]: Norges vassdrags- og energiverk. ISBN 8241002637.  ^ a b Mardal, Marius A. "Storofsen". In Godal, Anne Marit. Store norske leksikon (in Norwegian). Oslo: Norsk nettleksikon. Retrieved 20 September 2012.  ^ Lidmar-Bergström, Karna; Ollier, C.D.; Sulebak, J.R. (2000). "Landforms and uplift history of southern Norway". Global and Planetary Change. 24: 211–231.  ^ Garnes, K.; Bergersten, O.F. (1980). "Wastage features of the inland ice sheet in central South Norway". Boreas. 9: 251–269.  ^ https://kulturminnesok.no/minne/?queryString=https://data.kulturminne.no/askeladden/lokalitet/20978 ^ Dirk Levsen: Mikrogeschichte als Besatzungsgeschichte. Der deutsche Feldzug durch das Guldbrandsdal und das Romsdal im Frühjahr 1940. Historiographie und museale Präsentation. In Robert Bohn, (Hrsg.): Die deutsche Herrschaft in den "germanischen" Ländern 1940–1945 (= Historische Mitteilungen der Ranke-Gesellschaft, Beiheft 26). Steiner, Stuttgart 1997 ISBN 3-515-07099-0. S. 113f.

External links[edit]

Information about the Gudbrand Valley

Wikivoyage has a travel guide for Gudbrandsdalen.

Coordinates: 61°08′N 10°21′E / 61.133°N 10.350°E / 61.133; 10.350

v t e

Municipalities of Oppland



Nord-Fron Sør-Fron Ringebu


Dovre Lesja Lom Sel Skjåk Vågå


Gausdal Lillehammer Øyer


Nord-Aurdal Sør-Aurdal Etnedal Vestre Slidre Øystre Slidre Vang

Vest- Oppland



Gran Lunner Jevnaker


Nordre Søndre