Témbongkeun sumber pikeun Eyjafjallajökull

{{pp-move-indef}}
{{Infobox mountain
| name = Eyjafjallajökull
| other_name = Guðnasteinn <br> Hámundur
| photo = Eyjafjallajokull Gigjokull in ash.jpg
| photo_caption = Gígjökull, [[Morfologi glasiér|Saluran kaluar glasiér]] Eyjafjallajökull panglegana nu katutupan ku lebu vulkanis
| elevation_m = 1651
| listing = 
| pronunciation = {{IPA-is|ˈeɪjaˌfjatlaˌjœːkʏtl̥}}
| location = [[Wewengkon Kidul (Islandia)|Suðurland]], [[Islandia]]
| range = 
| map = Iceland
| map_caption = Islandia
| map_size =
| label_position = 
| lat_d = 63 | lat_m = 37 | lat_s = 12 | lat_NS = N
| long_d = 19 | long_m = 36 | long_s = 48 | long_EW = W
| region = IS
| coordinates_ref = <ref name="peakbagger">[http://www.peakbagger.com/peak.aspx?pid=8834 "Eyjafjallajökull, Iceland"]. Peakbagger.com. Retrieved 2013-08-09.</ref>
| topo = 
| type = [[Stratovolkano]]
| age = 
| volcanic_arc/belt = East Volcanic Zone
| last_eruption = Maret tepi ka Juni 2010
| first_ascent = 
| easiest_route = 
}}

[[File:Iceland volcano april 4 2010.JPG|thumb|right|Sawangan ti béh kaléreun  Mýrdalsjökull, Fimmvörðuháls katut Eyjafjallajökull (ti kénca ka katuhu) dina 4 April 2010, dipoto ti luhurna 10,000&nbsp;méter (32,800&nbsp;suku)]]
'''Eyjafjallajökull''' (dikecapkeun {{IPA-is|ˈeɪjaˌfjatlaˌjœːkʏtl̥||Is-Eyjafjallajökull (3).oga}}; [[basa Islandia]] keur "glasiér Eyjafjöll") nyaéta salah sahiji [[lapisan és]] [[Islandia]] nu rada leutik, perenahna di béh kaléreun [[Skógar]], kuloneun [[Mýrdalsjökull]]. Ieu lapisan és téh nutupan [[kaldéra]] [[gunung api]] nu luhur ponclotna 1.651 méter  (5.147 kaki). Ieu gunung api geus bitu rada mindeng ti [[période glasial pangahirna]], pangpandeurina mah bituna téh [[bituna Eyjafjallajökull taun 2010|taun 2010]].<ref>{{cite web |url=http://scienceblogs.com/eruptions/2010/03/increasing_signs_of_activity_a.php |title=Increasing signs of activity at Eyjafjallajökull in Iceland: Eruptions |doi=10.1016/j.jog.2006.09.005 |publisher=Scienceblogs.com |date= |accessdate=2010-04-17 }} {{Webarchive|url=https://web.archive.org/web/20100419024054/http://scienceblogs.com/eruptions/2010/03/increasing_signs_of_activity_a.php |date=2010-04-19 }}</ref><ref name="BBC8621581">{{cite news|url=http://news.bbc.co.uk/2/hi/8622978.stm |title=Iceland's volcanic ash halts flights in northern Europe |date=15 April 2010 |publisher=BBC News |accessdate=15 April 2010}}</ref>

==Géografi==
Eyjafjallajökull ngawengku hiji gunung api nu kabéhanana katutupan ku lapisan és. Ieu lapisan és nutupan hiji wewengkon nu legana kira-kira 100 km<sup>2</sup> (39 mil<sup>2</sup>), nu ngaluarkeun loba [[saluran kaluar glasiér]]. Saluran kaluar glasiér utama nyaéta di béh kalér; Gígjökull, ngalir ka Lónið, jeung Steinholtsjökull, ngalir deui ka Steinholtslón. Ieu glasiér téh panglegana ka-4 di Islandia mah.<ref name="vefur1">{{citation |url=http://iceland.vefur.is/iceland_nature/glaciers_in_iceland/eyjafjallajokull.htm |title= Eyjafjallajokull Glacier}}</ref> Dina taun 1967 aya urug gedé dina bojong glasial. Dina tanggal 16 Januari 1967 jam 13:47:55 (atawa 1:47:55 PM) aya kajadian bitu dina glasiér. Ieu kajadian bisa karékam wancina alatan séismometer-séismometer di Kirkjubæjarklaustur ngamonitor ieu gerakan. Nalika kurang leuwih {{convert|15000000|m3|0|abbr=off}} material nabrak glasier éta, sajumlah gedé udara, és, katut cai mimiti bagerak ti handapeun glasiér kaluar ka laguna nu aya dina suku glasiér.<ref name="vefur1"/>

Gunungna sorangan mah, mangrupa hiji [[stratovolkano]], nu titik pangluhurna mah luhurna {{convert|1651|m|ft}}, tur boga hiji [[Kawah vulkanis|kawah]] nu gurat tengahna {{convert|3|–|4|km|mi}}, muka ka  béh kaler. Biwir kawahna boga tilu punclut, nyaéta (saarah jeung jarum jam ti kalér wétan) Guðnasteinn, {{convert|1500|m|ft}} (kurang leuwih), Hámundur, {{convert|1651|m|ft}} jeung Goðasteinn, {{convert|1497|m|ft}} <!-- ref>[http://atlas.lmi.is/kortasafn_kort/2001-540-qv.jpg Map of area]</ref -->. Beungeut kidul ieu gunung mangrupa hiji bagéan tina [[basisir]] [[Atlantik]] Islandia, nu salila mangrébu-rébu taun, lautna geus mundur {{convert|5|km|mi}}. Basisir saméméhna mah kiwari mangrupa jungkrang nu lewang kalayan sababaraha [[curug]], nu pangkasohorna mah [[Skógafoss]]. Nalika angin kenceng, cai tina curug-curug nu leuwih leutik malah bisa katiup naék deui ka gunung. Wewengkon antara gunung jeung basisir kiwari mangrupa hiji amparan nu rélatif datar, legana {{convert|2|to|5|km|0|abbr=in}}, katelahna Eyjafjöll.

Ieu gunung api eusina hiji [[rohangan magma]] di sahandapeun gunung, nu asalna tina [[wates nu béda|perbédaan]] [[lémpéng téktonik|téktonik]] [[Tonggong Atlantik Tengah]]. Ieu gunung téh bagéan tina ranté pagunungan nu manjang sapanjang Islandia. Tatangga-tatangga pangdeukeutna nu aktif nyaéta [[Gunung api Katla|Katla]], di béh kalér wétan, jeung [[Eldfell]], di [[Heimaey]], di béh kidul kuloneunanan.
Ieu gunung api sacara géologis dianggep boga hubungan jeung Katla, sabab lamun Eyjafjallajökull bitu, biasana dituluykeun ku bituna Katla.
[[File:Iceland Eyjafjallajökull from Sólheimajökull.JPG|thumb|left|Eyjafjallajökull bulan Maret 2006, ditempo to hiji wewengkon wisata di Sólheimajökull, glasiér di gunung api Katla.]]

Gunung api Eyjafjallajökull bitu taun 920, 1612 tuluy ti 1821 tepi ka 1823 nalika nyababkeun [[caah nyebrot situ glasial]] atawa [[jökulhlaup]].<ref>{{cite web |url=http://icelandreview.com/icelandreview/daily_news/?cat_id=16567&ew_0_a_id=360723 |title="Last Eyjafjallajökull Eruption Lasted Two Years", Iceland Review |publisher=Icelandreview.com |date= |accessdate=2010-04-18 }} {{Webarchive|url=https://web.archive.org/web/20110713001426/http://icelandreview.com/icelandreview/daily_news/?cat_id=16567&ew_0_a_id=360723 |date=2011-07-13 }}</ref> [[Bituna Eyjafjallajökull taun 2010|Bitu tilu kali taun 2010]] nyaéta tanggal 20 Maret, April–Méi, sarta Juni. Kajadian bulan Maret mah nyababkeun évakuasi gegedéan kira-kira 500 urang lokal,<ref>{{cite news|url=http://www.guardian.co.uk/travel/gallery/2010/apr/01/iceland-volcano-tourist-trips |title="Iceland's hottest ticket&nbsp;— volcano tourism", The |publisher=Guardian |date= 1 April 2010|accessdate=2010-04-18 | location=London | first=Tom | last=Robbins}}</ref><ref>{{cite news|author=Associated Press |url=http://www.guardian.co.uk/world/2010/mar/21/volacno-erupts-iceland |title="Volcano erupts in Iceland" ''Hundreds of people evacuated from areas near glacier but no immediate reports of damage or injuries'', The |publisher=Guardian |date=2010-03-25 |accessdate=2010-04-18 | location=London}}</ref> tapi bitu tanggal 14 April mah sapuluh tepi ka dua puluh kalieun leuwih kuat sarta nyababkeun [[Gangguan perjalanan udara sanggeus bituna Eyjafjallajökull taun 2010|gangguan gedé kana lalu lintas udara]] di sakabéh [[Éropah]]. Nyababkeun dibolaykeunanan rébuan penerbangan di Éropah katut Islandia.

==Étimologi==
Ieu ngaran hartina "[[glasiér]]" (atawa ciplesna mah hartina "[[tutup és]]") Eyjafjöll. Kecap ''jökull'', nu hartina glasiér atawa tutup és, mangrupa [[basa nu sakulawarga]] jeung kecap [[Basa Inggris Panengah]] ''ikel'' nu aya dina ''-icle'' dina basa Inggris ''[[wikt:icicle|icicle]]'').

''Eyjafjöll'' mangrupa ngaran nu dilélér pikeun sisi kidul gunung katut gunung-gunung leutik nu ngawangun suku gunung.

''Eyjafjöll'' asalna tina kecap ''eyja'' (jamak tina ''ey'', nu hartina ''[[wikt:eyot|eyot]]'' atawa ''[[wikt:island|island]]''), jeung kecap jamak ''fjöll'', hartina ''[[wikt:fell#Etymology 3|fells]]'' atawa ''[[wikt:mountain|pagunungan]]''), lamun dihijikeun sacara literal hartina: "pagunungan di kapuloan". Ieu ngaran meureun nujul kana kapuloan [[Vestmannaeyjar]] nu aya di deukeuteunana.

Kecap ''fjalla'' mangrupa jamak génitif tina ''fjöll'', jadi ''Eyjafjalla'' mangrupa wangun génitif tina ''Eyjafjöll'' nu hartina: "tina Eyjafjöll".
Tarjamah literal bagéan demi bagéan tina ''Eyjafjallajökull'' baris jadi "tutup és Pagunungan di Kapuloan".

Eyjafjallajökull kadang-kadang ditujulkeun kana ''[[numeronym]]'' "E15".<ref>{{cite doi|10.1016/j.atmosenv.2011.05.034|noedit}}</ref>

== Géologi ==
[[File:Volcanic system of Iceland-Map-en.svg|thumb|right|Wewengkon katut sistem vulkanis aktif di Islandia]]

Ieu [[stratovolcano]], nu liang-liangna miturut kana trén wétan-kulon, kawangun ku [[lava]] [[basalt]] tepi ka [[andesite]]. lolobana bitu historisna mangrupa [[bitu éksplosif]].<ref>{{cite gvp|title=Eyjafjallajökull: Eruptive History|vnum= 1702-02=&volpage=erupt|accessdate=2010-04-18}}</ref> Sok sanajan kitu, [[liang nu rengat]] aya dina kadua sisina (utamana béh kulon).<ref>{{cite gvp|title=Eyjafjallajökull: Summary|vnum= 1702-02=|accessdate=2010-04-18}}</ref>

===Bitu taun 1821 tepi ka 1823===
Sababaraha karuksakan disababkeun ku bitu leutik taun 1821.<ref name=larsen>{{cite book|last=Larsen|first=G.|year=1999|title=Gosið í Eyjafjallajökli 1821–1823|trans_title=The eruption of the Eyjafjallajökull volcano in 1821–1823|publisher=Science Institute|id=Research Report RH-28-99|page=13|location=Reykjavík|url=http://www2.hi.is/Apps/WebObjects/HI.woa/swdocument/1015722/RH-28-1999_GLarsen-Eyj%C3%B6kull.pdf|format=PDF|language=Icelandic}} {{Webarchive|url=http://wayback.vefsafn.is/wayback/20101122162525/http://www2.hi.is/Apps/WebObjects/HI.woa/swdocument/1015722/RH-28-1999_GLarsen-Eyjökull.pdf |date=2010-11-22 }}</ref> Hususna, lebu nu kaluar alatan bitu ngandung pecahan [[florida]] nu loba, nu lamun dosisna loba mah bisa ngabahyakeun struktur tulang sato piaraan, kuda, domba, katut manusa. Ieu bitu ogé nyababkeun [[gerakan glasiér]] leutik jeung sedeng sarta caah di walungan [[Markarfljót]] jeung [[Holtsá]] nu aya deukeuteunana. Fase éruptif dimimitian tanggal 19 jeung 20 Désémber 1821 ku ayana bitu éksplosif nu tumuluy tepi ka sababaraha poé. Sumber-sumber nerangkeun yén [[lebu ragragan]] kacida kandelna di wewengkon sabudeureun gunung api, hususna ka béh kidul jeung kulon.<ref name=larsen/>

Sanggeus kajadian éta, runtuyan bitu nu leuwih leutik tumuluy tepi ka bulan Juni 1822.
Ti ahir Juni nepikeun ka awal Agustus 1822, runtuyan bitu lianna nuturkeun. Kolom bituna luhur pisan, kalayan lebu ragragan tepi ka jauh béh kalér nagara, di [[Eyjafjörður]], sarta béh kidul kulon, di bojong [[Seltjarnarnes]] deukeuteun [[Reykjavík]].

Période ti Agustus tepi ka Désémber 1822 katingalina mah leuwih simpé, tapi para patani mah matalikeun paraéhna lembu jeung domba di wewengkon Eyjafjörður jeung karacunan alatan bitu, nu ari analisis modéren mah ngidéntifikasi ieu kajadian téh minangka [[karacunan florida]]. Sababaraha glasiér leutik leupas ka walungan Holtsá. Nu leuwih gedéna mah nyaahan dataran deukeuteun walungan Markarfljót. Sumberna teu netepkeun tanggal pasti.

Dina taun 1823, sababaraha urang lalaki naék ka Eyjafjallajökull pikeun mariksa [[kawah vulkanis|kawah]]na. Maranéhanana manggihan hiji [[liang rengat]] deukeuteun [[kaldéra]] poncot béh kulon deukeuteun ''Guðnasteinn''.

Dina taun 1823 awal, gunung api deukeuteunana, [[gunung api Katla|Katla]] sahandapeun lapisan és [[Mýrdalsjökull]] bitu tur dina wanci nu babarengan, kolom sa'abna katempo dina poncot Eyjafjallajökull.

Lebu tina bitu Eyjafjallajökull taun 1821 kapanggih di sakabéh wewengkon kidul Islandia. Kelirna kulawu kolot, keusik jeung [[koral]]na ngandung [[silikon dioksida]] 28–40%.

===Bitu taun 2010===
{{Main|Bituna Eyjafjallajökull taun 2010|Pangaruh bituna Eyjafjallajökull bulan April 2010|Gangguan angkutan udara sanggeus bituna Eyjafjallajökull taun 2010}}
[[File:Eyjafjallajökull Glacier - 29.8.09.jpg|thumb|alt=A |Poto Eyjafjallajökull, dicokot ti [[Rute 1 (Islandia)|Rute 1]] bulan Agustus 2009]]

Bulan April 2010, [[aktivitas séismik]] katangén di wewengkon ieu gunung api, ku ayana mangrébu-rébu [[lini]] leutik (lolobananana magnitudona 1–2 [[skala magnitudo Richter]], ukur saeutik nu leuwih gedé ti 3 magnitudo) {{convert|7|–|10|km|mi}} di handapeun ieu gunung api.<ref>Pulo-pulo Veðurstofa (5 Maret 2010) {{cite web | title=Jarðskjálftahrina undir Eyjafjallajökli | work=Veðurstofa Ísland (The Meteorological Institute of Iceland)|url=http://www.vedur.is/um-vi/frettir/2010/nr/1831}}</ref> Dina ping 26 Pébruari 2010, peta séismik nu teu wajar dibarengan ku ngalegaanana kulit bumi kacida gancangna nu kadaptar ku [[Institut Météorologi Islandia]].<ref>{{cite web|title=Fasteignaskrá measurement tools|url=http://skra.is/default.aspx?pageid=943}} {{Webarchive|url=https://web.archive.org/web/20150328095226/http://www.skra.is/default.aspx?pageid=943 |date=2015-03-28 }}</ref> Ieu téh ngabuktikeun ka [[ahli géofisika]] yén magma ngocor ti handapeun kulit bumi ka [[rohangan magma]] gunung api Eyjafjallajökull sarta tekananana ngakar tina prosés nu nyababkeun pindahna kulit bumi di daérah pertanian Þorvaldseyri.<ref>Morgublaðið (26.02.2010) {{cite web |title=Innskot undir Eyjafjallajökli|work=Morgunblaðið|url=http://www.mbl.is/frettir/innlent/2010/02/26/innskot_undir_eyjafjallajokli/}}</ref> Aktivitas séismik tumuluy ngagedéan sarta ti saprak 3–5 Maret, ampir 3,000 lini kauukur dina épiséntrum ieu gunung api.
<!--
The eruption is thought to have begun on 20 March 2010, about {{convert|8|km|mi}} east of the top crater of the volcano, on [[Fimmvörðuháls]], the high neck between Eyjafjallajökull and the neighboring icecap, Mýrdalsjökull. This first eruption, in the form of a [[fissure vent]], did not occur under the glacier and was smaller in scale than had been expected by some geologists. The fissure opened on the north side of Fimmvörðuháls, directly across the popular hiking trail between Skógar, south of the pass, and [[Þórsmörk]], immediately to the north.
[[File:Fimmvorduhals 2010 03 27 dawn.jpg|thumb|left|The eruption on 27 March 2010]]
[[File:Eyjafjallajökull crater 2013.jpg|thumb|left|The crater three years post eruption in March 2013]]

On 14 April 2010 Eyjafjallajökull resumed erupting after a brief pause, this time from the top crater in the centre of the glacier, causing [[jökulhlaup]] (also known as [[meltwater]] floods) to rush down the nearby rivers, and requiring 800 people to be evacuated.<ref name="BBC8621581"/> This eruption was explosive in nature, due to melt water getting into the volcanic vent. It was estimated to be ten to twenty times larger than the previous one in [[Fimmvörðuháls]]. This second eruption threw volcanic ash several kilometres up in the atmosphere which led to [[Air travel disruption after the 2010 Eyjafjallajökull eruption|air travel disruption]] in northwest Europe for six days from 15 April to 21 April 2010 and also in May 2010,{{Clarify|date=May 2011}} including the closure of [[airspace]] over many parts of Europe.<ref>[http://news.bbc.co.uk/2/hi/uk_news/8636461.stm BBC: Row grows over airspace shutdown costs, 22 April 2010]</ref> The eruptions also created [[dirty thunderstorm|electrical storms]].<ref>{{cite web|url=http://www.msnbc.msn.com/id/36645958?GT1=43001|title=‘Dirty thunderstorm’: Lightning in a volcano}}</ref> On 23 May 2010, the London Volcanic Ash Advisory Commission declared the eruption to have stopped, but stated that they were continuing to monitor the volcano.<ref>{{cite web|url=http://www.metoffice.gov.uk/aviation/vaac/vaacuk.html|title=Met Office: Volcanic Ash Advisory Centres}}</ref> The volcano continued to have several earthquakes daily, with [[Volcanologist]]s watching the volcano closely.<ref name="en.vedur.is">{{cite web|url=http://en.vedur.is/earthquakes-and-volcanism/earthquakes/myrdalsjokull/ |title=Iceland Meteorological office – Earthquakes Mýrdalsjökull, Iceland |publisher=En.vedur.is |date= |accessdate=2013-03-26}}</ref> As of August 2010, Eyjafjallajökull was considered dormant.<ref>{{cite web|url=http://www.metoffice.gov.uk/news/releases/archive/2010/volcano-pauses |title=Iceland volcano ‘pauses’  |date= |accessdate=2010-07-12}}</ref>-->
<!-- **************************************************************
*                                                                 *
*    Please consider adding new information to the main article   *
*    located at [[2010 eruptions of Eyjafjallajökull]] instead    *
*    of adding it here.                                           *
*                                                                 *
*************************************************************** -->
<!--
===Relationship to Katla===
[[File:Eyjafjallajökull en Katla.png|thumb|400px|right| Cross section through Eyjafjöll and Katla]]

Eyjafjallajökull lies {{convert|25|km|0|abbr=on}} west of another subglacial volcano, [[Katla volcano|Katla]], under the [[Mýrdalsjökull]] ice cap, which is much more active and known for its powerful [[subglacial eruption]]s and its large magma chamber.<ref>{{cite news|url=http://www.economist.com/node/15943975?story_id=15943975&source=features_box2 |title=Green.view: Back into the clouds |publisher=The Economist |date=2010-04-16 |accessdate=2010-04-22}}</ref> Each of the eruptions of Eyjafjallajökull in 920, 1612, and 1821–1823 has preceded an eruption of Katla.<ref name="icelandprepares">{{cite news|title=Iceland prepares for second, more devastating volcanic eruption|publisher=TimesOnline|author=Roger Boyes|accessdate=21 March 2010|url=http://www.timesonline.co.uk/tol/news/world/europe/article7070239.ece | location=London | date=21 March 2010}}</ref> Katla has not displayed any unusual activity (such as expansion of the crust or seismic activity) during the 2010 eruptions of Eyjafjallajökull, though geologists have been concerned about the general instability of Katla since 1999. Some geophysicists in Iceland believe that the Eyjafjallajökull eruption may trigger an eruption of Katla, which would cause major flooding due to melting of glacial ice and send up massive plumes of ash.<ref name="icelandprepares"/><ref>Kastljósið 22.3.2010, Sjónvarpið, "Viðtal við Dr. Pál Einarsson, jarðeðlisfræðing"</ref> On 20 April 2010 Icelandic President [[Ólafur Ragnar Grímsson|Ólafur Grímsson]] said "the time for Katla to erupt is coming close...we [Iceland] have prepared...it is high time for European governments and airline authorities all over the world to start planning for the eventual Katla eruption".<ref>[http://news.bbc.co.uk/2/hi/programmes/newsnight/8631343.stm BBC Newsnight interview with President Grímsson of Iceland, 20 April 2010]</ref>

Volcanologists continue to monitor Katla, aware that any eruption from Katla following an eruption from Eyjafjallajökull has historically occurred within months of an Eyjafjallajökull eruption. The Icelandic Meteorological Office updates its website with reports of quakes both at Eyjafjallajökull and Katla.<ref name="en.vedur.is"/> A small eruption of Katla was confirmed on 8 July 2011 after a harmonic tremor was detected. The event produced cracks on Katla's glacier and a [[jökulhlaup]] that destroyed a bridge on the [[Ring Road (Iceland)|Ring Road]].<ref>{{cite web|url=http://volcano.si.edu/world/volcano.cfm?vnum=1702-03=&volpage=weekly|title=Weekly Reports|work=Katla|publisher=Smithsonian Global Volcanism Program}}</ref>
-->

== Tempo ogé ==
* [[Glaciers of Iceland|Glasiér di Islandia]]
* [[Volcanism of Iceland|Vulkanisme di Islandia]]
* [[Waterfalls of Iceland|Curug di Islandia]]
* [[Ragnar Th. Sigurdsson]] nu moto bituna gunung Eyjafjallajökull taun 2010
{{portal bar|Géografi|Géologi}}

== Rujukan ==
{{Reflist|colwidth=32em}}

== Tumbu kaluar ==
{{Commons category|Eyjafjallajökull}}
{{Wikinews2|Ash from Iceland volcano could affect UK flights|European airspace closed by volcanic ash|Volcanic eruption starts on top of Eyjafjallajökull, Iceland|Icelandic volcanic eruption prompts evacuation, flight diversions|Europe's airline chaos: in depth}}
; Poto
* [http://www.eyjafjallajokull.com/ Poto katut vidio ti Eyjafjallajökull]
* [http://earthobservatory.nasa.gov/IOTD/view.php?id=43252 Gambar satelit nalika bitu taun 2010 yasana NASA]
* [http://www.millhouse.nl/eyjafjallajokull/ Poto bitu taun 2010 yasana Fred Kamphues] {{Webarchive|url=https://web.archive.org/web/20100418185156/http://www.millhouse.nl/eyjafjallajokull/ |date=2010-04-18 }}
* [http://cimss.ssec.wisc.edu/goes/blog/archives/5137 Kumpulan gambar satelit ti Blog Satelit CIMSS]
* [http://lostinstockholm.com/2010/04/16/amazing-photos-from-the-volcanic-eruption-in-iceland/ Koléksi Poto Panghadéna] {{Webarchive|url=https://web.archive.org/web/20120709151026/http://lostinstockholm.com/2010/04/16/amazing-photos-from-the-volcanic-eruption-in-iceland/ |date=2012-07-09 }}
* [http://www.boston.com/bigpicture/2010/04/more_from_eyjafjallajokull.html More from Eyjafjallajökull – Gambar Badag]
* [http://www.raw.is/?cat=4 Poto-poto ku Raw Iceland], hiji organisasi basis Reykjavík nu ngorganisir poto wisata amatir jeung profésional ka ieu gunung api.

; Vidio jeung webcam
* [[2010 eruptions of Eyjafjallajökull#Webcams|Webcam nalika bitu]]
* [http://vimeo.com/11008464 Vidio pondok 17 April 2010. Kurang leuwih 30 menit diputer salila 18 detik.]
* [http://www.flickr.com/photos/iriya/4526241556/ Video bitu munggaran 2010]
* [http://www.vimeo.com/10548285 Video bitu munggaran 2010 yasana Raw Iceland]
* [http://www.helicoptericeland.com/volcano-tour-eyjafjallajokull/ Video sanggeus bituna Eyjafjallajokull. Dicokot 28 Juli 2010] {{Webarchive|url=https://web.archive.org/web/20100718182351/http://www.helicoptericeland.com/volcano-tour-eyjafjallajokull/ |date=2010-07-18 }}
* [http://www.vimeo.com/11122783 Saurang kru pilem badarat di Eyjafjallajokull salila bitu 2010]

; Audio
* [http://www.binauralairwaves.com/2008/12/icelandic-waterfall-in-fall-2008.html Gunung api Eyjafjallajökull: Curug Seljalandsfoss  (rékaman keur dua ceuli optimal keur headpon)]

; Artikel géologis
* [http://www.jardvis.hi.is/page/jheyjafjallajokull Universitas Islandia: Sajarah Eyjafjallajökull] {{Webarchive|url=https://web.archive.org/web/20090907091633/http://www.jardvis.hi.is/page/jheyjafjallajokull |date=2009-09-07 }} {{is icon}}
* [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B7W57-4X83J77-7&_user=713833&_origUdi=B6VCS-4XH0MNS-2&_fmt=high&_coverDate=12%2F31%2F2010&_rdoc=1&_orig=article&_acct=C000039878&_version=1&_urlVersion=0&_userid=713833&md5=905703f9b1f300b531ddaf11e2fc50fa Géologi gunung api Katla jeung Eyjafjallajökull, Universitas Islandia]
* [http://www.vedur.is/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf Jalur magma jeung lini di Eyjafjallajökull, Institut Météorologi Islandia (PDF)]
* [http://www.evropusamvinna.is/solofile/1015933 Institut Élmu Bumi&nbsp;– Bitu di Eyjafjallajökull] {{Webarchive|url=http://wayback.vefsafn.is/wayback/20100809191050/www.evropusamvinna.is/solofile/1015933 |date=2010-08-09 }} (laporan status bitu poéan)
* [http://www.volcano.si.edu/reports/usgs/index.cfm#eyjafjol Laporan Aktivitas Vulkanis Mingguan SI / USGS keur Eyjafjallajökull] {{Webarchive|url=https://web.archive.org/web/20051112102231/http://www.volcano.si.edu/reports/usgs/index.cfm#eyjafjol |date=2005-11-12 }}

; Perkiraan lebu penerbangan
* [http://www.metoffice.gov.uk/aviation/vaac/vaacuk_vag.html Perkiraan Grafis Lebu Vulkanis keur wewengkon Atlantik Kalér]
* [http://www.metoffice.gov.uk/corporate/pressoffice/2010/volcano/ashconcentration/ Peta Konséntrasi Lebu Vulkanis keur wewengkon Atlantik Kalér]

; Peta
* [http://www.lmi.is/Files/Skra_0041261.pdf Peta wewengkon Iceland National Land Survey] {{Webarchive|url=http://wayback.vefsafn.is/wayback/20100813154030/www.lmi.is/Files/Skra_0041261.pdf |date=2010-08-13 }}
* [http://atlas.lmi.is/kortasafn_kort/2001-540-qv.jpg Peta kontur]

{{Glaciers of Iceland}}
{{2010 Eyjafjallajökull eruptions}}

{{DEFAULTSORT:Eyjafjallajokull}}
[[Kategori:Eyjafjallajökull|*]]
[[Kategori:Islandia Kidul]]
[[Kategori:Gunung api di Islandia]]
[[Kategori:Gunung api aktif]]
[[Kategori:Stratovolkano]]
[[Kategori:Gunung api VEI-4]]
[[Kategori:Wewengkon Vulanis Kidul di Islandia]]