{{short description|Autonomous territory of Denmark}}
{{redirect|Faroe|the 17th century ship|HDMS Færøe|the pony breed|Faroe pony|the sheep breed|Faroe sheep}}
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{{Use dmy dates|date=November 2025}}
{{Use British English|date=February 2026}}
{{Infobox dependency
| name = Faroe Islands
| native_name = {{nobold|{{native name|fo|Føroyar}}}}
{{nobold|{{native name|da|Færøerne}}}}
| type = [[Danish Realm|Autonomous territory in the Kingdom of Denmark]]{{Cite web|url=https://www.government.fo/en/foreign-relations/about-the-faroe-islands|title=About the Faroe Islands|website=Government.fo|access-date=3 June 2026}}
| linking_name = the Faroe Islands
| image_flag = Flag of the Faroe Islands.svg
| flag_size = 125px
| flag_link = Flag of the Faroe Islands
| image_seal = Coat of arms of the Faroe Islands.svg
| seal_size = 80px
| seal_type = Coat of arms
| seal_link = Coat of arms of the Faroe Islands
| nickname =
| nickname_link =
| motto_link =
| motto =
| anthem_link =
| anthem = {{native name|fo|"[[Tú alfagra land mítt]]"|italics=off}}
({{Langx|en|"Thou, fairest land of mine"}})
There are many other islands in the ocean to the north of Britain which can be reached from the northern islands of Britain in a direct voyage of two days and nights with sails filled with a continuously favourable wind. A devout priest told me that in two summer days and the intervening night he sailed in a two-benched boat and entered one of them. There is another set of small islands, nearly all separated by narrow stretches of water; in these for nearly a hundred years hermits sailing from our country, Ireland, have lived. But just as they were always deserted from the beginning of the world, so now because of the Northman pirates they are emptied of [[anchorite]]s, and filled with countless sheep and very many diverse kinds of sea-birds. I have never found these islands mentioned in the authorities.{{Cite book |last=Tierney |first=J.J. |title=Dicuili Liber de mensura orbis terrae |date=1967 |publisher=Dublin Institute for Advances Studies |location=Dublin |pages=75–77|ol=16308328M }}It has been argued that these were likely the eremitic [[Papar]] that had similarly resided in parts of Iceland and Scotland in the same period,{{cite web |title=Chapter 7.2 |url=https://penelope.uchicago.edu/Thayer/L/Roman/Texts/Dicuil/De_mensura_orbis_terrae/text*.html |access-date=14 March 2014 |publisher=Penelope.uchicago.edu |archive-date=26 May 2012 |archive-url=https://archive.today/20120526074859/http://penelope.uchicago.edu/Thayer/L/Roman/Texts/Dicuil/De_mensura_orbis_terrae/text*.html |url-status=live }} with these Papar also being the ones to bring sheep to the islands. A [[Immram|voyage tale]], recorded in the ninth-century, concerning Irish saint [[Brendan the Navigator|Brendan]], who proceeded Dicuil by 3 centuries, details him visiting an unnamed northern group of islands; this has also been argued to be referring to the Faroe Islands, though not nearly as conclusively.{{cite web |title=Navigatio Sancti Brendani Abbatis |url=http://www.hs-augsburg.de/~harsch/Chronologia/Lspost10/Brendanus/bre_navi.html |access-date=28 April 2013 |archive-date=17 October 2017 |archive-url=https://web.archive.org/web/20171017194919/http://www.hs-augsburg.de/~harsch/Chronologia/Lspost10/Brendanus/bre_navi.html |url-status=live }} See translation: {{cite web |title=Nauigatio sancti Brendani abbatis [the Voyage of St Brendan the Abbot] chapter XI, edition by Archbishop P. F. Moran, tr. Denis O'Donoghue, Brendaniana, 1893 |url=http://markjberry.blogs.com/StBrendan.pdf |access-date=28 April 2013 |archive-date=10 January 2015 |archive-url=https://web.archive.org/web/20150110192228/http://markjberry.blogs.com/StBrendan.pdf |url-status=live }} Some toponyms around the islands refer to the Papar and the Irish, such as Paparøkur near [[Vestmanna]] and Papurshílsur near [[Saksun]]. Vestmanna is itself short for {{Lang|fo|Vestmannahøvn|italic=yes}} ({{gloss |harbour of the [[Vestmenn|Westmen]]}}). Tombstones in a churchyard on [[Skúvoy]] display a possible Gaelic origin or influence.Schei, Liv Kjørsvik & Moberg, Gunnie (2003) ''The Faroe Islands''. Birlinn. [[File:Faroe stamps 515-517 everyday life in the viking age.jpg|thumb|400px|Everyday life in the Viking Age]] Old Norse-speaking settlers arrived in the early 9th century, and their Old West Norse dialect would later evolve into the modern [[Faroese language]]. A number of the settlers were [[Norse–Gaels]] who did not come directly from Scandinavia, but rather from Norse communities that spanned the [[Irish Sea]], [[Northern Isles]], and [[Outer Hebrides]] of [[Scotland]], including the [[Shetland]] and [[Orkney]] islands; these settlers also brought thralls of [[Gaels|Gaelic]] origin with them, and this admixture is reflected today in the Faroese genetic makeup and many loanwords from Old Irish. According to ''[[Færeyinga saga]]'', many of the Norwegian settlers in particular were spurred by their disapproval of the monarchy of [[Harald Fairhair]], whose rule was also seen as an inciting factor for the [[Settlement of Iceland]]. The founding date of the [[Løgting]] is not historically documented. However, the saga implies that it was a well-established institution by the middle of the 10th century, when a legal dispute between chieftains Havgrímur and Einar Suðuroyingur, resulting in the [[exile]] of Eldjárn Kambhøttur, is recounted in detail.{{Cite web |title=Færeyinga saga – heimskringla.no |url=https://www.heimskringla.no/wiki/F%C3%A6reyinga_saga |access-date=28 March 2024 |website=Heimskringla.no}} Christianity was introduced to the islands in the late 10th and early 11th centuries by chieftain [[Sigmundur Brestisson]].{{cite web |title=The Faroe Islands, Faroese History – A part of Randburg |url=http://www.randburg.com/fa/general/general_5.html |archive-url=https://archive.today/20120907123238/http://www.randburg.com/fa/general/general_5.html |archive-date=7 September 2012 |publisher=Randburg.com }} Baptised as an adult by then-[[monarchy of Norway|King of Norway]] [[Olaf Tryggvason]], his mission to introduce Christianity was part of a greater plan to seize the islands on behalf of the Norwegian crown.{{Cite EB1911|wstitle=Faeroe|volume=10|pages=123–124}} While Christianity arrived at the same time as in [[Christianization of Iceland|Iceland]], the process was met with much more conflict and violence, and was defined particularly by Sigmundur's conflict with rival chieftain [[Tróndur í Gøtu]], the latter of whom was converted under threat of decapitation. Although their conflict resulted in Sigmundur's murder, the Islands fell firmly under Norwegian rule following Tróndur's death in 1035. ===14th century onwards=== [[File:Faroe Islands, 1767, as seen by Yves de Kerguelen Trémarec.PNG|thumb|upright=1.35|The Faroe Islands as seen by the Breton navigator [[Yves-Joseph de Kerguelen-Trémarec]] in 1767]] In 1380, the Faroe Islands entered a union with [[Denmark]] through the unification of Denmark and Norway, marking the beginning of a prolonged period under Danish influence.{{Cite news |date=21 November 2012 |title=Faroe Islands profile – Timeline |url=https://www.bbc.com/news/world-europe-20427188 |access-date=9 April 2025 |work=BBC News |language=en-GB |archive-date=7 October 2025 |archive-url=https://web.archive.org/web/20251007032801/https://www.bbc.com/news/world-europe-20427188 |url-status=live }} This transition led to significant changes, including the introduction of [[Lutheranism]] in 1538, which had profound effects on the islands' religious practices and cultural identity. The Faroe Islands were subjected to repeated [[Barbary slave trade|slave raids]] by the [[Barbary corsairs]] between the 16th and 18th centuries.Liisberg, H. C. B. (2020). Danmarks søfart og søhandel. Bind 1. Danmark: SAGA Egmont. The most famous slave raid on the Faroe Islands was the [[slave raid of Suðuroy]] in the summer of 1629.{{Cite book |last=Niels Andreas Christian Andersen |url=http://archive.org/details/faererne00andegoog |title=Faerøerne, 1600–1709 |date=1895 |publisher=G. E. C. Gad |others=New York Public Library |pages=234–254 |language=Danish}} The 17th century brought economic challenges as Denmark imposed a trade monopoly, restricting the Faroese economy and limiting their commercial interactions with other nations.{{Cite web |date=February 9, 2026 |title=Faroe Islands {{!}} History, Population, Capital, Map, & Facts {{!}} Britannica |url=https://www.britannica.com/place/Faroe-Islands-Atlantic-Ocean |url-status=live |access-date=April 8, 2026 |website=Encyclopædia Britannica}} This monopoly was eventually lifted in 1856, allowing the islands to develop a modern fishing industry and revitalise their economy.{{cite web |title=CIDOB – Secession and Counter-secession. An International Relations Perspective |url=https://www.cidob.org/en/publications/publication_series/monographs/monographs/secession_and_counter_secession_an_international_relations_perspective |access-date=19 May 2018 |website=CIDOB |page=69 |archive-date=27 January 2018 |archive-url=https://web.archive.org/web/20180127014249/https://www.cidob.org/en/publications/publication_series/monographs/monographs/secession_and_counter_secession_an_international_relations_perspective |url-status=live }} The 19th century was a pivotal era for Faroese cultural and political revival. Lutheran minister [[Venceslaus Ulricus Hammershaimb]] introduced an official orthography for the Faroese language in 1846, reaffirming its cultural significance after centuries of suppression. This linguistic renaissance fuelled the growth of a national movement, leading to the reinstatement of the Løgting in 1852 as an advisory body. [[File:Engelske tropper ankommer til Thorshavn (FHM-17412).jpg|thumb|British troops arrive in [[Tórshavn]], 1940]] The early 20th century saw the emergence of political parties advocating for greater autonomy. The Union Party favoured maintaining ties with Denmark, while the Self-Government Party pushed for full independence. In the first year of the [[Second World War]], on 12 April 1940, [[British occupation of the Faroe Islands|British troops occupied the Faroe Islands in Operation Valentine]]. [[Nazi Germany]] had invaded Denmark and commenced the invasion of Norway on 9 April 1940 under [[Operation Weserübung]]. In 1942–1943, the British [[Royal Monmouthshire Royal Engineers|Royal Engineers]], under the command of Lieutenant Colonel William Law, built the first and only airport in the Faroe Islands, [[Vágar Airport]]. The British refrained from governing Faroese internal affairs, and the islands became effectively self-governing during the war. After the war ended and the British army left, this period and [[Iceland]]'s declaration as a republic in 1944 served as a precedent and a model in the mind of many Faroe Islanders. Independence debates culminated in a 1946 referendum where a slim majority voted for independence; however, the Danish government annulled the results, and the islands remained under Danish sovereignty. The Løgting held an independence referendum on [[1946 Faroese independence referendum|14 September 1946]], resulting in a very narrow majority for independence; 50.73% voted in favour and 49.27% against; the margin was only 161 votes.{{cite web|url=http://www.sudd.ch/event.php?lang=en&id=fo011946|title=Faroe Islands, 14 September 1946: Status|archive-url=https://web.archive.org/web/20201021014332/http://www.sudd.ch/event.php?lang=en&id=fo011946 |archive-date=21 October 2020|website=Database and Search Engine for Direct Democracy|date=14 September 1946 |language=de}} The Løgting subsequently declared independence on 18 September 1946; this declaration was annulled by Denmark on 20 September, arguing that the number of invalid votes (481) being greater than the narrow margin in favour made the result invalid. As a result, [[Christian X of Denmark|King Christian X of Denmark]] ordered that the Faroese Løgting be dissolved on 24 September, with new elections held that November.{{sfnp |Steining |1953 |p=187}} The [[1946 Faroese parliamentary election|Faroese parliamentary election of 1946]] resulted in a majority for parties opposed to independence:{{sfnp |Steining |1953 |p=188}} following protracted negotiations, Denmark granted [[home rule]] to the Faroe Islands on 30 March 1948. This agreement granted the islands a high degree of autonomy, and Faroese finally became the official language in all public spheres.{{cite news|title=Faroe Islands|newspaper=Encyclopedia Britannica |url=https://www.britannica.com/place/Faroe-Islands-Atlantic-Ocean|publisher=[[Britannica]]|access-date=19 April 2021|archive-url=https://archive.today/20210419122910/https://www.britannica.com/place/Faroe-Islands-Atlantic-Ocean|archive-date=19 April 2021}} In 1973, the Faroe Islands declined to join Denmark in entering the [[European Economic Community]] (EEC); as a result, the islands are not part of the European Union (EU) today (although, as Danish citizens, Faroe Islanders are still considered EU citizens). Following the collapse of the fishing industry in the early 1990s, the Faroes experienced considerable economic difficulties.{{Cite journal |last1=Hamilton |first1=Lawrence C. |last2=Colocousis |first2=Chris R. |last3=Johansen |first3=Sámal T. F. |date=May 2004 |title=Migration from Resource Depletion: The Case of the Faroe Islands|journal=Society & Natural Resources |volume=17 |issue=5 |pages=443–453 |doi=10.1080/08941920490430232 |bibcode=2004SNatR..17..443H }} Today, the Faroe Islands are a [[Self-governance|self-governing territory]] within the [[Danish Realm|Kingdom of Denmark]], proud of their cultural heritage, fishing industry, and political autonomy.{{Cite web |last=Travel |first=Times |date=28 February 2019 |title=Best things to do in the Faroe Islands |url=https://www.thetimes.com/travel/destinations/europe-travel/denmark/faroe-islands/things-to-do-in-the-faroe-islands-rl8m9pnwb?region=global |access-date=9 April 2025 |website=Thetimes.com |language=en |archive-date=25 April 2025 |archive-url=https://web.archive.org/web/20250425121347/https://www.thetimes.com/travel/destinations/europe-travel/denmark/faroe-islands/things-to-do-in-the-faroe-islands-rl8m9pnwb?region=global |url-status=live }} ==Geography== {{Main|Geography of the Faroe Islands}} [[File:Faroe Islands by Sentinel-2.jpg|thumb|Satellite image of the Faroe Islands]] The Faroe Islands are an island group consisting of [[List of islands of the Faroe Islands|18 major islands]] (and a total of 779 islands, [[islet]]s, and [[skerry|skerries]]) about {{convert|655|km}} off the coast of Northern Europe, between the [[Norwegian Sea]] and the [[North Atlantic Ocean]], about halfway between [[Iceland]] and [[Norway]], the closest neighbours being the [[Northern Isles]] and the [[Outer Hebrides]] of the [[United Kingdom]]. Its coordinates are {{coord|62|00|N|06|47|W}}. Distance from the Faroe Islands to: * [[North Rona|Rona]] (uninhabited), United Kingdom: {{convert|260|km|mi}} * [[Shetland]] ([[Foula]]), United Kingdom: {{convert|285|km|mi}} * [[Orkney]] ([[Westray]]), United Kingdom: {{convert|300|km|mi}} * [[United Kingdom]] (mainland): {{convert|320|km|mi}} * [[Iceland]]: {{convert|450|km|mi}} * [[Norway]]: {{convert|580|km|mi}} * [[Ireland]]: {{convert|670|km|mi}} * [[Denmark]]: {{convert|990|km|mi}} The islands cover an area of 1,399 square kilometres (540 sq. mi) and have [[List of lakes of the Faroe Islands|small lakes]] and rivers, but no major ones. There are {{convert|1117|km|mi}} of coastline.{{cite web |title=Faroe Islands |url=https://www.cia.gov/the-world-factbook/countries/faroe-islands/ |access-date=6 August 2016 |website=[[The World Factbook]] |publisher=[[CIA]] |archive-date=10 January 2021 |archive-url=https://web.archive.org/web/20210110004755/https://www.cia.gov/the-world-factbook/countries/faroe-islands |url-status=dead }} The only significant uninhabited island is [[Lítla Dímun]]. The islands are rugged and rocky with some low peaks; the coasts are mostly cliffs. The highest point is [[Slættaratindur]] in northern [[Eysturoy]], {{convert|882|m|ft}} [[above sea level]]. The Faroe Islands are made up of an approximately six-kilometres-thick succession of mostly [[basalt]]ic [[lava]] that was part of the great [[North Atlantic Igneous Province]] during the [[Paleogene]] period.{{Cite journal |last1=Geoffroy |first1=Laurent |last2=Bergerat |first2=Francoise |last3=Angelier |first3=Jacques |year=1996 |title=Brittle tectonism in relation to the Palaeogene evolution of the Thulean/NE Atlantic domain: A study in Ulster |journal=Geological Journal |volume=31 |issue=3 |pages=259–269 |doi=10.1002/(SICI)1099-1034(199609)31:3<259::AID-GJ711>3.0.CO;2-8|bibcode=1996GeolJ..31..259G }} The lavas erupted during the opening of the [[North Atlantic Ocean]], which began about 60 million years ago, and what is today the Faroe Islands was then attached to Greenland.{{Cite web|last=Dahrén |first=Börje |date=2016 |title=Magma plumbing architecture in Indonesia and the North Atlantic Igneous Province |url=http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-267764|website=Urn.kb.se}}{{Cite journal |last1=Jolley |first1=David W. |last2=Bell |first2=Brian R. |date=2002 |title=The evolution of the North Atlantic Igneous Province and the opening of the NE Atlantic rift |journal=Geological Society, London, Special Publications |volume=197 |issue=1 |pages=1–13 |bibcode=2002GSLSP.197....1J |doi=10.1144/GSL.SP.2002.197.01.01 }} The lavas are underlain by circa 30 km of unidentified ancient continental crust.{{Cite journal |last1=Richardson |first1=K.R |last2=Smallwood |first2=J.R |last3=White |first3=R.S |last4=Snyder |first4=D.B |last5=Maguire |first5=P.K.H |date=December 1998 |title=Crustal structure beneath the Faroe Islands and the Faroe–Iceland Ridge |journal=Tectonophysics |volume=300 |issue=1–4 |pages=159–180 |bibcode=1998Tectp.300..159R |doi=10.1016/S0040-1951(98)00239-X}}{{Cite journal |last1=Harland |first1=K. E. |last2=White |first2=R. S. |last3=Soosalu |first3=H. |date=April 2009 |title=Crustal structure beneath the Faroe Islands from teleseismic receiver functions |journal=Geophysical Journal International |volume=177 |issue=1 |pages=115–124 |bibcode=2009GeoJI.177..115H |doi=10.1111/j.1365-246X.2008.04018.x |doi-access=free}} ===Climate=== {{See also|Geography of the Faroe Islands#Climate}}[[File:Faroe Islands, Eysturoy, Skipanes and Undir Gøtueiði.jpg|thumb|upright=1.3|The village of [[Skipanes]] on [[Eysturoy]], with murkier weather in the distance]] The climate is classed as [[subpolar oceanic climate]] according to the [[Köppen climate classification]]: [[Oceanic climate|Cfc]], with areas having a [[tundra]] climate, especially in the mountains, although some coastal or low-lying areas may have very mild-winter versions of a tundra climate. The overall character of the climate of the islands is influenced by the strong warming influence of the Atlantic Ocean, which produces the [[North Atlantic Current]]. This, together with the remoteness of any source of landmass-induced warm or cold airflows, ensures that winters are mild (mean temperature 3.0 to 4.0 °C or 37 to 39 °F) while summers are cool (mean temperature 9.5 to 11.2 °C or 49 to 52 °F). The islands are windy, cloudy, and cool throughout the year, with an average of 210 rainy or snowy days per year. The islands lie in the path of depressions moving northeast, making strong winds and heavy rain possible at all times of the year. Sunny days are rare, and overcast days are common. [[Hurricane Faith]] struck the Faroe Islands on 5 September 1966 with sustained winds over 100 mph (160 km/h), and only then did the storm cease to be a tropical system.GHCN Climate data, Thorshavn series 1881 to 2007 The climate varies greatly over small distances due to the altitude, ocean currents, topography, and winds. Precipitation varies considerably throughout the archipelago. In some highland areas, snow cover may last for months, with snowfalls possible for the greater part of the year (on the highest peaks, summer snowfall is by no means rare), while in some sheltered coastal locations, several years pass without any snowfall whatsoever. Tórshavn receives frosts more often than other areas just a short distance to the south. Snow is also seen at a much higher frequency than on outlying islands nearby. The area receives on average 49 frosts a year. The collection of meteorological data on the Faroe Islands began in 1867.{{cite web |title=Plant production on a Faeroese farm 1813–1892, related to climatic fluctuations |url=http://rdgs.dk/djg/pdfs/101/1/06.pdf |archive-url=https://web.archive.org/web/20120317115552/http://rdgs.dk/djg/pdfs/101/1/06.pdf |archive-date=17 March 2012 |access-date=25 August 2013 }} Winter recording began in 1891, and the warmest winter occurred in 2016–17 with an average temperature of 6.1 °C (43 °F).{{cite web |date=3 March 2017 |title=Rekordvarm vinter på Færøerne |url=http://www.dmi.dk/nyheder/arkiv/nyheder-2017/marts/rekordvarm-vinter-paa-faeroeerne/ |archive-url=https://web.archive.org/web/20170307183257/http://www.dmi.dk/nyheder/arkiv/nyheder-2017/marts/rekordvarm-vinter-paa-faeroeerne |archive-date=7 March 2017 |access-date=7 March 2017 |publisher=[[Danish Meteorological Institute]]}} {{Weather box|width=auto |location = Tórshavn (1981–2010 normals, extremes 1961–2010) |metric first = Y |single line = Y |Jan record high C = 11.6 |Feb record high C = 12.0 |Mar record high C = 12.3 |Apr record high C = 18.3 |May record high C = 19.7 |Jun record high C = 20.0 |Jul record high C = 20.2 |Aug record high C = 22.0 |Sep record high C = 19.5 |Oct record high C = 15.2 |Nov record high C = 14.7 |Dec record high C = 13.2 |year record high C = 22.0 |Jan high C = 5.8 |Feb high C = 5.6 |Mar high C = 6.0 |Apr high C = 7.3 |May high C = 9.2 |Jun high C = 11.1 |Jul high C = 12.8 |Aug high C = 13.1 |Sep high C = 11.5 |Oct high C = 9.3 |Nov high C = 7.2 |Dec high C = 6.2 |year high C = 8.8 |Jan mean C = 4.0 |Feb mean C = 3.6 |Mar mean C = 4.0 |Apr mean C = 5.2 |May mean C = 7.0 |Jun mean C = 9.0 |Jul mean C = 10.7 |Aug mean C = 11.0 |Sep mean C = 9.6 |Oct mean C = 7.5 |Nov mean C = 5.5 |Dec mean C = 4.3 |year mean C = 6.8 |Jan low C = 1.7 |Feb low C = 1.3 |Mar low C = 1.7 |Apr low C = 3.0 |May low C = 5.1 |Jun low C = 7.1 |Jul low C = 9.0 |Aug low C = 9.2 |Sep low C = 7.6 |Oct low C = 5.4 |Nov low C = 3.4 |Dec low C = 2.1 |year low C = 4.7 |Jan record low C = -8.8 |Feb record low C = -11.0 |Mar record low C = -9.2 |Apr record low C = -9.9 |May record low C = -3.0 |Jun record low C = 0.0 |Jul record low C = 1.5 |Aug record low C = 1.5 |Sep record low C = -0.6 |Oct record low C = -4.5 |Nov record low C = -7.2 |Dec record low C = -10.5 |year record low C = -11.0 |precipitation colour = green |Jan precipitation mm = 157.7 |Feb precipitation mm = 115.2 |Mar precipitation mm = 131.6 |Apr precipitation mm = 89.5 |May precipitation mm = 63.3 |Jun precipitation mm = 57.5 |Jul precipitation mm = 74.3 |Aug precipitation mm = 96.0 |Sep precipitation mm = 119.5 |Oct precipitation mm = 147.4 |Nov precipitation mm = 139.3 |Dec precipitation mm = 135.3 |year precipitation mm = 1321.3 |humidity colour = |Jan humidity = 89 |Feb humidity = 88 |Mar humidity = 88 |Apr humidity = 87 |May humidity = 87 |Jun humidity = 88 |Jul humidity = 89 |Aug humidity = 90 |Sep humidity = 89 |Oct humidity = 89 |Nov humidity = 88 |Dec humidity = 89 |year humidity = 88 |unit precipitation days = 0.1 mm |Jan precipitation days = 26 |Feb precipitation days = 23 |Mar precipitation days = 26 |Apr precipitation days = 22 |May precipitation days = 19 |Jun precipitation days = 18 |Jul precipitation days = 19 |Aug precipitation days = 20 |Sep precipitation days = 23 |Oct precipitation days = 26 |Nov precipitation days = 26 |Dec precipitation days = 27 |year precipitation days = 273 |Jan snow days = 8.3 |Feb snow days = 6.6 |Mar snow days = 8.0 |Apr snow days = 4.4 |May snow days = 1.5 |Jun snow days = 0.0 |Jul snow days = 0.0 |Aug snow days = 0.0 |Sep snow days = 0.1 |Oct snow days = 1.4 |Nov snow days = 5.5 |Dec snow days = 8.2 |year snow days = 44.0 |Jan sun = 14.5 |Feb sun = 36.7 |Mar sun = 72.8 |Apr sun = 108.6 |May sun = 137.8 |Jun sun = 128.6 |Jul sun = 103.6 |Aug sun = 100.9 |Sep sun = 82.7 |Oct sun = 53.4 |Nov sun = 21.1 |Dec sun = 7.8 |year sun = 868.2 |source 1 = [[Danish Meteorological Institute]] (humidity 1961–1990, precipitation days 1961–1990, snowy days 1961–1990) {{cite web |title=Monthly means and extremes 1961–1990 and 1981–2010 for air temperature, atmospheric pressure, hours of bright sunshine and precipitation–Denmark, The Faroe Islands and Greenland |url=http://www.dmi.dk/fileadmin/Rapporter/TR/tr11-20.pdf |access-date=18 January 2015 |publisher=Danish Meteorological Institute |pages=16–19 |archive-date=18 January 2015 |archive-url=https://web.archive.org/web/20150118104640/http://www.dmi.dk/fileadmin/Rapporter/TR/tr11-20.pdf |url-status=live }} {{cite web |title=DMI Report 18–19: Climatological Standard Normals 1981–2010 Denmark, The Faroe Islands and Greenland Based on Data Published in DMI Reports 18–08, 18–04 and 18–05 |url=https://www.dmi.dk/fileadmin/user_upload/Rapporter/TR/2019/DMIRep18-19.pdf |archive-url = https://web.archive.org/web/20190210040507/https://www.dmi.dk/fileadmin/user_upload/Rapporter/TR/2019/DMIRep18-19.pdf |archive-date=10 February 2019 |access-date=9 February 2019 |publisher=Danish Meteorological Institute }} {{cite web |title=The Climate of The Faroe Islands with Climatological Standard Normals, 1961–1990 |url=https://www.dmi.dk/fileadmin/user_upload/Rapporter/TR/1998/tr98-14.pdf |archive-url = https://web.archive.org/web/20190210162510/https://www.dmi.dk/fileadmin/user_upload/Rapporter/TR/1998/tr98-14.pdf |archive-date=10 February 2019 |access-date=10 February 2019 |publisher=Danish Meteorological Institute }} }} ===Flora=== {{Main|Flora of the Faroe Islands}} [[File:Myrisolja.jpg|thumb|upright=1.2|Marsh marigold (''[[Caltha palustris]]'') is common in the Faroe Islands during May and June.]] The Faroes belong to the [[Faroe Islands boreal grasslands]] ecoregion.{{cite journal |last1=Dinerstein |first1=Eric |last2=Olson |first2=David |last3=Joshi |first3=Anup |last4=Vynne |first4=Carly |last5=Burgess |first5=Neil D. |last6=Wikramanayake |first6=Eric |last7=Hahn |first7=Nathan |last8=Palminteri |first8=Suzanne |last9=Hedao |first9=Prashant |last10=Noss |first10=Reed |last11=Hansen |first11=Matt |last12=Locke |first12=Harvey |last13=Ellis |first13=Erle C |last14=Jones |first14=Benjamin |last15=Barber |first15=Charles Victor |last16=Hayes |first16=Randy |last17=Kormos |first17=Cyril |last18=Martin |first18=Vance |last19=Crist |first19=Eileen |last20=Sechrest |first20=Wes |last21=Price |first21=Lori |last22=Baillie |first22=Jonathan E. M. |last23=Weeden |first23=Don |last24=Suckling |first24=Kierán |last25=Davis |first25=Crystal |last26=Sizer |first26=Nigel |last27=Moore |first27=Rebecca |last28=Thau |first28=David |last29=Birch |first29=Tanya |last30=Potapov |first30=Peter |last31=Turubanova |first31=Svetlana |last32=Tyukavina |first32=Alexandra |last33=de Souza |first33=Nadia |last34=Pintea |first34=Lilian |last35=Brito |first35=José C. |last36=Llewellyn |first36=Othman A. |last37=Miller |first37=Anthony G. |last38=Patzelt |first38=Annette |last39=Ghazanfar |first39=Shahina A. |last40=Timberlake |first40=Jonathan |last41=Klöser |first41=Heinz |last42=Shennan-Farpón |first42=Yara |last43=Kindt |first43=Roeland |last44=Lillesø |first44=Jens-Peter Barnekow |last45=van Breugel |first45=Paulo |last46=Graudal |first46=Lars |last47=Voge |first47=Maianna |last48=Al-Shammari |first48=Khalaf F. |last49=Saleem |first49=Muhammad |title=An Ecoregion-Based Approach to Protecting Half the Terrestrial Realm |journal=BioScience |date=June 2017 |volume=67 |issue=6 |pages=534–545 |doi=10.1093/biosci/bix014 |pmid=28608869 |pmc=5451287 |doi-access=free }} The natural vegetation of the Faroe Islands is dominated by arctic-alpine plants, wildflowers, grasses, moss, and lichen. Most of the lowland area is grassland, and some are heath, dominated by shrubby heathers, mainly [[Calluna|''Calluna vulgaris'']]. Among the herbaceous flora that occurs in the Faroe Islands is the cosmopolitan marsh thistle, ''[[Cirsium palustre]]''.Hogan, C. Michael (2009) [http://www.globaltwitcher.com/artspec_information.asp?thingid=48639 ''Marsh Thistle: Cirsium palustre'', GlobalTwitcher, ed. N. Stromberg] {{webarchive |url=https://web.archive.org/web/20121213144520/http://www.globaltwitcher.com/artspec_information.asp?thingid=48639 |date=13 December 2012 }} Although it is often asserted that the islands are naturally treeless, several tree species, among them shrubby willows (''salix''), junipers (''Juniperus''), and stunted birches, colonised the island after the Ice Age but disappeared later – apparently as a result of grazing impacts, possibly aggravated by a shift to relatively wetter cooler climatic conditions about the same time.{{cite journal |last1=Olsen |first1=Jesper |last2=Björck |first2=Svante |last3=Leng |first3=Melanie J. |last4=Gudmundsdóttir |first4=Esther Ruth |last5=Odgaard |first5=Bent V. |last6=Lutz |first6=Christina M. |last7=Kendrick |first7=Chris P. |last8=Andersen |first8=Thorbjørn J. |last9=Seidenkrantz |first9=Marit-Solveig |title=Lacustrine evidence of Holocene environmental change from three Faroese lakes: a multiproxy XRF and stable isotope study |journal=Quaternary Science Reviews |date=September 2010 |volume=29 |issue=19 |page=2765 |doi=10.1016/j.quascirev.2010.06.029 |bibcode=2010QSRv...29.2764O }} A limited number of species have been successfully introduced to the region, in particular, trees from the [[Magellanic subpolar forests]] region of Chile. Conditions in the Magellanic subpolar forests are similar to those in the Faroe Islands, with cold summers and near-continuous subpolar winds. The following species from [[Tierra del Fuego]], ''[[Drimys winteri]]'', ''[[Nothofagus antarctica]]'', ''[[Nothofagus pumilio]]'', and ''[[Nothofagus betuloides]]'', have been successfully introduced to the Faroe Islands. A non-Chilean species that has been introduced is the [[Populus trichocarpa#Distribution|black cottonwood]], also known as the California poplar (''Populus trichocarpa'').{{citation needed|date=January 2021}} ===Fauna=== {{Main|Fauna of the Faroe Islands}} {{further|List of birds of the Faroe Islands|List of mammals of the Faroe Islands|List of Lepidoptera of the Faroe Islands}} [[File:Dreierprofil.jpg|thumb|upright=1.2|left|[[Atlantic puffin]]s are very common and a part of the local cuisine: [[Faroese puffin]].]] The [[List of birds of the Faroe Islands|bird fauna of the Faroe Islands]] is dominated by [[seabird]]s and birds attracted to open land such as [[Calluna|heather]], probably because of the lack of woodland and other suitable habitats. Many species have developed special Faroese sub-species such as the [[common eider]],{{cite web|url=https://www.oneearth.org/ecoregions/faroe-islands-boreal-grasslands/|title=Faroe Islands Boreal Grasslands|website=One Earth|access-date=1 September 2024|author=((UNEP-WCMC Author Team))|date=15 February 2022|archive-date=5 September 2024|archive-url=https://web.archive.org/web/20240905153246/https://www.oneearth.org/ecoregions/faroe-islands-boreal-grasslands/|url-status=live}} [[common starling]],{{cite web|url=https://www.birdmigrationatlas.dk/uk/species/starling|website=The Faroese Bird Migration Atlas|title=Starling ''Sturnus vulgaris'' Stær Stari|access-date=1 September 2024|year=2024|orig-date=Originally published 2014 by Fróðskapur – Faroe University Press|last1=Hammer|first1=Sjúrður|last2=Madsen|first2=Jadsen J.|last3=Jensen|first3=Jens-Kjeld|last4=Pedersen|first4=Kjeld T.|last5=Bloch|first5=Dorete|last6=Thorup|first6=Kasper}} [[Eurasian wren]],{{cite web|url=https://www.allaboutbirds.org/guide/Eurasian_Wren/id|title=Eurasian Wren: Regional Differences|website=All About Birds|publisher=CornellLab of Ornithology, Cornell University|access-date=1 September 2024|archive-date=2 September 2024|archive-url=https://web.archive.org/web/20240902040635/https://www.allaboutbirds.org/guide/Eurasian_Wren/id|url-status=live}} and [[black guillemot]].{{cite web |title=The Faroese Fauna|url=http://www.mundofree.com/islasferoe/thefaroesefauna.html|archive-url=https://web.archive.org/web/20080228060832/http://www.mundofree.com/islasferoe/thefaroesefauna.html|archive-date=28 February 2008|publisher=Mundofree.com}} The [[pied raven]], a colour morph of the North Atlantic subspecies of the [[common raven]], was [[endemism|endemic]] to the Faroe Islands, but now has become extinct;{{Cite journal |last=van Grouw |first=Hein |date=2014 |title=Some black-and-white facts about the Faeroese white-speckled Common Raven Corvus corax varius |url=https://www.biodiversitylibrary.org/item/252797#page/6/mode/1up |journal=Bulletin of the British Ornithologists' Club |volume=134 |issue=1 |pages=4–13 |archive-date=6 May 2025 |access-date=22 June 2025 |archive-url=https://web.archive.org/web/20250506183702/https://www.biodiversitylibrary.org/item/252797#page/6/mode/1up |url-status=live }} the ordinary, all-black morph remains fairly widespread in the archipelago.{{citation needed|date=January 2024}} Only a few species of wild land mammals are found in the Faroe Islands today, all introduced by humans. Three species are thriving on the islands today: [[mountain hare]] (''Lepus timidus''), [[brown rat]] (''Rattus norvegicus''), and the [[house mouse]] (''Mus musculus''). Recent DNA studies have reveal three independent introductions of the brown rat to the Faroe Islands{{Cite journal |last1=Puckett |first1=Emily E. |last2=Magnussen |first2=Eyðfinn |last3=Khlyap |first3=Liudmila A. |last4=Strand |first4=Tanja M. |last5=Lundkvist |first5=Åke |last6=Munshi-South |first6=Jason |date=2020 |title=Genomic analyses reveal three independent introductions of the invasive brown rat (Rattus norvegicus) to the Faroe Islands |journal=Heredity |language=en |volume=124 |issue=1 |pages=15–27 |doi=10.1038/s41437-019-0255-6 |pmc=6906366 |pmid=31399718 |bibcode=2020Hered.124...15P }} The [[Faroe Islands domestic animals|domestic animals of the Faroe Islands]] are a result of 1,200 years of isolated breeding. As a result, many of the islands' domestic animals are found nowhere else in the world. Faroese domestic breeds include [[Faroe pony]], [[Faroe Islands domestic animals#Faroese cow|Faroe cow]], Faroe sheep, [[Faroese goose]], and [[Faroe Islands domestic animals#Faroese duck|Faroese duck]]. The [[Faroe sheep]] is depicted on the [[Coat of arms of the Faroe Islands|coat of arms]]; there once was a variety of [[feral animal|feral sheep]], which survived on [[Lítla Dímun]] until the mid-nineteenth century.{{Cite journal |last=Ryder |first=M. L. |year=1981 |title=A survey of European primitive breeds of sheep |journal=Ann. Génét. Sél. Anim. |volume=13 |issue=4 |pages=381–418 [p. 400] |doi=10.1186/1297-9686-13-4-381 |pmc=2718014 |pmid=22896215 |doi-access=free }} [[File:Faroese sheep Sumba 1.jpg|thumb|upright=1.2|[[Faroe sheep]] with the town of [[Sumba, Faroe Islands|Sumba]] in the background]] [[Grey seal]]s (''Halichoerus grypus'') are common around the shorelines, away from human habitations.{{cite journal |last1=Haug |first1=Tore |last2=Hammil |first2=Mike |last3=Olafsdottir |first3=Droplaug |title=Grey Seals in the North Atlantic and the Baltic |journal=NAAMCO Scientific Publications |date=23 October 2013 |volume=6 |url=https://septentrio.uit.no/index.php/nammcosp/issue/view/NSP6 |access-date=5 June 2023 |archive-date=6 June 2023 |archive-url=https://web.archive.org/web/20230606054410/https://septentrio.uit.no/index.php/nammcosp/issue/view/NSP6 |url-status=live }} Several species of [[cetacea]] live in the waters around the Faroe Islands. Best known are the [[long-finned pilot whale]]s (''Globicephala melaena''), which still are hunted by the islanders under longstanding local tradition{{cite web | last=Rogers | first=Stephanie | title=Pilot Whales Brutally Slaughtered Annually in the Faroe Islands |url=http://earthfirst.com/pilot-whales-brutally-slaughtered-annually-in-the-faroe-islands |url-status=bot: unknown |archive-url=https://web.archive.org/web/20120522015403/http://earthfirst.com/pilot-whales-brutally-slaughtered-annually-in-the-faroe-islands |archive-date=22 May 2012 |access-date=28 June 2010}} (see [[#Whaling|Whaling]], below). [[Orca]]s (''Orcinus orca'') are regular visitors around the islands. ===Geology=== {{Main|Geology of the Faroe Islands}} [[File:Suðuroy.FaroeIslands.2.jpg|thumb|upright=1.2|Beinisvørð, on the west coast of Suðuroy]] The islands were formed during a period of high volcanic activity in the Early [[Paleogene]], around 50–60 million years ago. The islands are built up in layers of different lava flows (basalt) alternating with thin layers of volcanic ash (tuff). The soft ash and the hard basalt thus lie layer upon layer in narrow and thick strips. The soft tuff or ash zones erode relatively quickly, and the hard lump of basalt above the eroded tuff falls away, forming the first terrace. Volcanic activity has varied over millions of years, with periods of quiescence and various periods of quiet eruptive fissures and explosive volcanism. In a few places, mainly on Suðuroy, thin layers of coal are present, which are the remains of swamp forests from the time between volcanic eruptions. The plateau has, therefore, been divided into different basalt series according to the course of volcanism and the age sequence of the layers. There are major differences in the shapes of the islands' terraces. The lowest and oldest series are thick lava deposits that can be seen on the southern part of Suðuroy, Mykines, Tindhólmur, and the western side of Vágar. The basalts of the lower basalt series are often pillared, which is shown by elongated, angular, and regular pillars in the mountainside. Very regular vertical columns are found on northern Mykines, where they can be up to {{convert|30|m|ft|-1}} high. The middle basalt series consists of thin lava flows with a highly porous interlayer. This series has very little resistance to crumbling and weathering. As these erosion processes are more severe at higher altitudes than lower down, the lowlands are filled with weathering material from the heights, often resulting in a characteristic curved landscape shape. This can be seen in Vágar, the northernmost part of Streymoy, and the northwestern part of Eysturoy. Glacial activity has reduced plateau surfaces, especially on the northern islands, where the surfaces have been reduced to a series of narrower or wider zig-zag rows along the length of the islands: especially on the islands of Kunoy, Kalsoy, and Borðoy, where an eastward and a westward ice mass have eroded the intervening mountain range into a narrow ridge. === Topography === The Faroe Islands have a predominantly mountainous terrain, with elevations rising steeply from the coastline on most islands. The landscape features a series of basaltic plateaus intersected by valleys and fjords, resulting in numerous summits across the archipelago. The highest elevations are located on the larger northern islands, particularly [[Eysturoy]], [[Viðoy]] and [[Kunoy]]. '''The five highest mountain peaks in the Faroe Islands are:''' # [[Slættaratindur]] (Eysturoy) – 880 m{{Cite web |last=PeakVisor |title=Faroe Islands Mountains |url=https://peakvisor.com/adm/faroe-islands.html |access-date=13 November 2025 |website=PeakVisor |language=en |archive-date=27 November 2025 |archive-url=https://web.archive.org/web/20251127122358/https://peakvisor.com/adm/faroe-islands.html |url-status=live }} # [[Gráfelli]] (Eysturoy) – 856 m{{Cite web |title=Gráfelli - Peakbagger.com |url=https://www.peakbagger.com/peak.aspx?pid=31028 |access-date=13 November 2025 |website=Peakbagger.com}} # Villingadalsfjall (Viðoy) – 841 m{{Cite web |last=Fyllgraf |first=Mads |title=Mount Villingadalsfjall • Towering Summit |url=https://guidetofaroeislands.fo/travel-faroe-islands/drive/villingadalsfjall/ |access-date=13 November 2025 |website=Guide to Faroe Islands |language=en-US |archive-date=16 January 2026 |archive-url=https://web.archive.org/web/20260116141757/https://guidetofaroeislands.fo/travel-faroe-islands/drive/villingadalsfjall/ |url-status=live }} # Kúvingafjall (Kunoy) – 830 m{{Cite web |title=Kúvingafjall |url=https://peakery.com/kuvingafjall-faroe-islands/ |access-date=13 November 2025 |website=peakery.com |language=en |archive-date=6 October 2022 |archive-url=https://web.archive.org/web/20221006101031/https://peakery.com/kuvingafjall-faroe-islands/ |url-status=live }} # Teigafjall (Kunoy) – 825 m{{Cite web |title=Teigafjall - Peakbagger.com |url=https://www.peakbagger.com/peak.aspx?pid=123347 |access-date=13 November 2025 |website=Peakbagger.com |archive-date=27 November 2025 |archive-url=https://web.archive.org/web/20251127122359/https://www.peakbagger.com/peak.aspx?pid=123347 |url-status=live }} ''See more at Wikipedia page: [[List of mountains of the Faroe Islands]]'' ==Government and politics== {{Main|Politics of the Faroe Islands}} {{multiple image | align = vertical | total_width = 420 | width1 = 140 | image1 = King Frederik X in 2025.jpg | caption1 = [[Frederik X]],