524:
40:
509:
539:
582:
389:. It is about 25 km (9.7 sq mi) and includes the Reykjanes volcanic system that extends in a linear fashion up its centre continuing to the north-east as the hill of Sýrfell at 93 m (305 ft) high. Other volcanic systems of the Reykjanes volcanic belt could affect the Reykjanes region and have erupted as recently as 2024. Other hills associated with the system are Skálafell (Grindavíkurbær) with a height of 76 m (249 ft) in the south-west near the sea and Bæjarfell at 69 m (226 ft) high to its north.
183:
551:
456:
Ridge. Volcanic rock production has kept pace with rift extension and subsidence with at least ten eruptions in the 14,500 years since the area became ice free after the end of the last ice age. Within the volcanic system there are active NE–SW dip-slip faults. There are two main fissure swarm zones being in the north (Stampar) and south (Sýrfell). They are separated by about 2 km (1.2 mi), and their western parts have been active in the last three eruptive periods of the
Reykjanes area.
176:
570:
450:
and the two volcanic systems are very similar, even though they have separate geothermal systems,and lava composition. Recent studies tend to classify the
Reykjanes volcanic system as a separate fissure volcano of the Reykjanes volcano belt. This volcanic system marks the transition from the mainly
438:
layers in the region. The volcano erupted for a 30 odd year period ending in 1240 CE. In 1226 CE an explosive eruption off
Reykjanes produced about 0.1 km (0.024 cu mi) of tephra with deposits up to 100 km (62 mi) away. It also has lava dated to 2150 years ago and
455:
of the
Atlantic mid-oceanic ridge to a trans-tensional plate boundary in the Reykjanes Peninsula. The 5–6 km (3.1–3.7 mi) wide Reykjanes volcanic system is in a rift zone, which extends 45 km (28 mi), including at least 9 km (5.6 mi) out to sea towards the Reykjanes
471:
characteristics. While the active volcanism on the peninsula has been a major source for the geothermal activity in the area, there is evidence that the volcanism can fuel geothermal systems up to 30 kilometers away, as far as Hvalfjörður. On the
Reykjanes Peninsula itself, the system has had its
239:
Selected geological features near the
Reykjanes volcanic system (approximate outline in red as part of system is ill defined). This is not the Reykjanes headland region which is smaller. Clicking on the image enables mouse-over with more detail where shading also shows: other
523:
581:
538:
508:
978:. Icelandic Meteorological Office, Institute of Earth Sciences at the University of Iceland, Civil Protection Department of the National Commissioner of the Iceland Police
1024:
550:
869:
569:
80:
440:
489:
1284:
175:
1017:
870:"Structure and activity of the geothermal field of Hvalfjörður (Iceland) from brittle tectonic, geothermal and paleostress analysis"
923:
Sæmundsson, K.; Sigurgeirsson, M.Á.; Friðleifsson, G.Ó. (2020). "Geology and structure of the
Reykjanes volcanic system, Iceland".
386:
39:
1289:
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416:
308:, giving the main peninsula its name. Volcanic action is responsible for forming the entire peninsula. The nearest town is
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1010:
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are typically more than 4500 years old, but towards the south there are more recent eruptive fissures, with crater rows,
1034:
494:
195:
73:
475:
Most of the
Reykjanes area is at risk of disruption from future eruptions and susceptibility maps have been published.
1269:
226:
24:
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953:
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as well as parts of tuff cones near the south-west shoreline. The offshore volcanoes have produced 15 different
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49:
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749:
747:
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587:
Map of volcanic systems on the
Reykjanes Peninsula. The Reykjanes system is marked here as number 1
356:
301:
1259:
955:
Volcanic hazard and risk assessment at
Reykjanes, vulnerability of infrastructure. Masters thesis
292:
157:
20:
1050:
889:
427:
661:
659:
657:
439:
3200 years ago. The Reykjanes volcano has been classified historically with the active as of
940:
881:
1202:
452:
1171:
1060:
868:
Bergerat, Françoise; Sæmundsson, Kristjan; Fourel, Loïc; Angelier, Jacques (2013-07-01).
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431:
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volcano to its south-east as its rift system intersects this to the east in the
678:
1197:
976:"Catalogue of Icelandic Volcanoes - Reykjanes and Svartsengi volcanic systems"
396:
lighthouse is on Bæjarfell and is fairly frequently visited by tourists.. The
997:
975:
893:
95:
82:
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Reykjanesviti lighthouse with steam from the geothermal area of Gunnuhver
309:
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1123:
1081:
305:
199:
1104:
460:
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63:
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View from Reykjanestá to south-west with Eldey in the far background
843:
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665:
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611:
355:; there are also many other uses of this name in Iceland, e.g. the
1099:
1065:
472:
geothermal potential exploited, producing up to 176 MW of energy.
351:. It is named this due to the continuing volcanic activity of the
1075:
1006:
1234:
Note: Volcanoes listed here have "central volcanoes" unless a
764:
762:
532:
lighthouse on Bæjarfell with lighthouse keeper's residence
403:
Valahnúkamöl is its south western cliff coast leading to
974:
Sigurgeirsson, Magnús Á.; Einarsson, Sigmundur (2019).
268:
subglacial terrain above 1,100 m (3,600 ft),
831:
807:
780:
753:
738:
1238:is place after name, in that case the volcano is a
1211:
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225:
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163:
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19:This article is about the geographical end of the
844:Sæmundsson, Sigurgeirsson & Friðleifsson 2020
820:Sæmundsson, Sigurgeirsson & Friðleifsson 2020
666:Sæmundsson, Sigurgeirsson & Friðleifsson 2020
649:Sæmundsson, Sigurgeirsson & Friðleifsson 2020
630:Sæmundsson, Sigurgeirsson & Friðleifsson 2020
400:is inland from the lighthouse to its north-east.
182:
612:"National Land Survey of Iceland : Sýrfell"
337:
322:
316:
961:(Thesis). University of Iceland. pp. 1–89
925:Journal of Volcanology and Geothermal Research
275:seismically active areas between 1995 to 2007.
1018:
810:, 1. Geological setting and tectonic context.
8:
998:Catalogue of Icelandic Volcanoes - Reykjanes
906:
855:
792:
768:
726:
714:
702:
422:The basaltic low relief lava shields of the
874:Bulletin de la Société Géologique de France
407:, the most south-western cape of the area.
1025:
1011:
1003:
29:
16:Geographic feature in Southwestern Iceland
614:. Landmælingar Íslands. 28 December 2023.
451:extensional structure of the underwater
415:For broader coverage of this topic, see
598:
501:
490:List of volcanic eruptions in Iceland
371:The region is about nine kilometres (
291:
7:
606:
604:
602:
514:Valahnúkamöl coast to south towards
832:Sigurgeirsson & Einarsson 2019
808:Sigurgeirsson & Einarsson 2019
781:Sigurgeirsson & Einarsson 2019
756:, 4. Eruption history and pattern.
754:Sigurgeirsson & Einarsson 2019
739:Sigurgeirsson & Einarsson 2019
14:
952:Andrésdóttir, Þóra Björg (2018).
321:, translates to "smoking point,”
945:10.1016/j.jvolgeores.2018.11.022
632:, The Reykjanes volcanic system.
580:
568:
549:
537:
522:
507:
300:on the south-western end of the
181:
174:
136:25 km (9.7 sq mi)
38:
23:of Iceland. For other uses, see
741:, 2. Morphology and topography.
387:Iceland's international airport
417:Geology of Reykjanes Peninsula
1:
886:10.2113/gssgfbull.184.4-5.451
783:, 11. Largest known eruption.
128:5–6 km (3.1–3.7 mi)
1186:Snæfellsjökull Volcanic Zone
495:List of volcanoes in Iceland
1285:Volcanic systems of Iceland
1306:
414:
48:Lighthouse and beyond the
25:Reykjanes (disambiguation)
18:
1232:
1212:Öræfajökull Volcanic Zone
424:Reykjanes volcanic system
235:
189:Reykjanes volcanic system
168:
37:
33:Reykjanes volcanic system
683:Global Volcanism Program
398:geothermal power station
289:Icelandic pronunciation:
1290:Reykjanes Volcanic Belt
1116:Reykjanes Volcanic Belt
561:Reykjanes Power Station
459:The volcanic rocks are
448:Reykjanes volcanic belt
385:miles) to the south of
353:Reykjanes volcanic belt
120:45 km (28 mi)
68:93 m (305 ft)
50:Reykjanes Power Station
44:Reykjanes with view of
1092:Northern Volcanic Zone
338:
323:
317:
293:[ˈreiːcaˌnɛːs]
1164:Western Volcanic Zone
1043:Eastern Volcanic Zone
96:63.82000°N 22.69000°W
1280:Volcanoes of Iceland
1265:Headlands of Iceland
1035:volcanoes of Iceland
834:, Short Description.
563:) with cooling ponds
485:Volcanism of Iceland
937:2020JVGR..39106501S
432:hyaloclastite hills
357:Reykjanes Peninsula
302:Reykjanes Peninsula
254:central volcanoes,
146:English translation
101:63.82000; -22.69000
92: /
1270:Black sand beaches
1147:Eldvörp–Svartsengi
503:Reykjanes' scenery
444:Eldvörp–Svartsengi
196:Southern Peninsula
58:Highest point
21:Southern Peninsula
1247:
1246:
1129:Brennisteinsfjöll
909:, pp. 69–73.
907:Andrésdóttir 2018
856:Andrésdóttir 2018
793:Andrésdóttir 2018
769:Andrésdóttir 2018
727:Andrésdóttir 2018
715:Andrésdóttir 2018
705:, pp. 54–55.
703:Andrésdóttir 2018
557:Suðurnesjavirkjun
282:
281:
1297:
1056:Eyjafjallajökull
1027:
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1004:
987:
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970:
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880:(4–5): 451–465.
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359:or Reykjanes in
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154:Language of name
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668:, Introduction.
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453:Reykjanes Ridge
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1275:Rift volcanoes
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1193:Snæfellsjökull
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992:External links
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848:
836:
824:
822:, Conclusions.
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797:
785:
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758:
743:
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717:, pp. 57.
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858:, p. 48.
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795:, p. 30.
794:
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771:, p. 32.
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729:, p. 28.
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530:Reykjanesviti
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394:Reykjanesviti
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227:Last eruption
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217:Mountain type
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149:smoking point
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77:
75:
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52:to north-east
51:
47:
46:Reykjanesviti
41:
36:
31:
26:
22:
1235:
1172:Prestahnúkur
1152:
980:. Retrieved
963:. Retrieved
954:
928:
924:
902:
877:
873:
863:
851:
839:
827:
815:
788:
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734:
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698:
686:. Retrieved
682:
673:
556:
474:
458:
423:
421:
402:
391:
370:
314:
284:
283:
1219:Öræfajökull
1177:Hveravellir
1051:Bárðarbunga
982:29 December
965:28 December
846:, Faulting.
679:"Reykjanes"
651:, Abstract.
516:Reykjanestá
405:Reykjanestá
99: /
74:Coordinates
1254:Categories
1203:Ljósufjöll
1198:Helgrindur
1033:Monitored
931:(106501).
593:References
315:The name,
112:Dimensions
87:22°41′24″W
84:63°49′12″N
1260:Reykjanes
1224:Esjufjöll
1153:Reykjanes
1061:Grímsvötn
894:1777-5817
469:tholeiite
367:Geography
318:Reykjanes
285:Reykjanes
261:calderas
164:Geography
158:Icelandic
64:Elevation
1135:Krýsuvík
688:6 August
479:See also
310:Keflavik
298:headland
1240:fissure
1124:Hengill
1082:Surtsey
933:Bibcode
917:Sources
465:picrite
463:, with
461:basalts
428:tindars
411:Geology
380:⁄
331:smoking
306:Iceland
231:1240 CE
211:Geology
200:Iceland
1105:Krafla
892:
436:tephra
336:, and
324:reykja
273:
271:
266:
264:
259:
257:
252:
250:
245:
243:
141:Naming
117:Length
1242:only.
1100:Askja
1071:Katla
1066:Hekla
959:(PDF)
467:, or
346:point
125:Width
1076:Laki
984:2023
967:2023
890:ISSN
690:2023
441:2024
430:and
392:The
133:Area
1236:(f)
1155:(f)
1149:(f)
1143:(f)
1137:(f)
1131:(f)
1107:(f)
1078:(f)
941:doi
929:391
882:doi
878:184
339:nes
304:in
1256::
939:.
927:.
888:.
876:.
872:.
800:^
761:^
746:^
681:.
656:^
637:^
620:^
601:^
363:.
312:.
198:,
1026:e
1019:t
1012:v
986:.
969:.
947:.
943::
935::
896:.
884::
692:.
559:(
419:.
382:2
378:1
375:+
373:5
349:'
343:'
334:'
328:'
287:(
27:.
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