Volcanoes & Earthquakes - new app for Android
Départs garantis:
8-16 mai 2021: Montagnes de Feu - du Stromboli à l'Etna - Eoliennes + Etna
: Places libres / : Départ garanti / : Quelques places disponibles / : Groupe fermé
Actualitées:
lun., 28 sept. 2020, 07:15
Depth vs time of recent quakes in Iceland (image: VolcanoDiscovery)
The Icelandic Met Office (IMO) recorded an earthquake with magnitude M 4.8 at 9.1 km depth in Bárðarbunga volcano at 00:06 local time yesterday. Few smaller aftershocks have been detected in the area. Tremor has not shown significant variations. The earthquakes of this magnitude (M 4.8) were detected in April and January this year. lire toutes
mar., 14 juil. 2020, 08:53
Depth vs time of recent quakes in Iceland (image: Volcano Discovery)
On 13 July at 23:41 local time Icelandic Met Office (IMO) recorded an earthquake with magnitude M 3.0 at 2.4 km depth beneath the SE caldera. In one hour later an earthquake M 3.3 occurred in similar location. Last time an M 3.0 or larger earthquake occurred about a month ago. ... lire toutes

Bárdarbunga volcan

Stratovolcano approx. 2000 m / ca. 6,560 ft
Central Iceland, 64.63°N / -17.53°W
Condition actuelle: normal / en sommeil (1 sur 5)
Last update: 28 Sep 2020 (light to moderate earthquake)
Lava fountains from the Holuhraun fissure eruption August 2014

Bardarbunga (Bárðarbunga) is a large central volcano lying underneath Iceland's 500-m thick Vatnajokull glacier in the center of the country. It is located at the junction between the eastern and northern volcanic rift zones in the area where the present-day center of the mantle hot spot beneath Iceland is thought to be.
Bardarbunga has had about 300-400 eruptions during the past 10,000 years which includes only 23 eruptions historic times (approx the past 1000 years), i.e. it seems to erupt currently at rates of approx. twice per century, the last one having occurred in 1910. A massive explosive-effusive eruption (VEI 6) in 1477 resulted in a large ash and pumice fall-out deposit.
Approx 8600 years ago, Bardarbunga produced the largest known lava flow during the past 10,000 years on earth (more than 21 cubic kilometers of volume). The lava was erupted from the Veidivötn fissure system and traveled more than 100 km to the south coast.

Show interactive Map
Style éruptif tipique: Large effusive eruptions, some explosive activity.
Eruptions du volcan Bárdarbunga: 1080(?), 1159(?), ca. 1210, ca. 1270, ca. 1350, ca. 1410(?), 1477 (very large effusive-explosive eruption), 1697, 1702, 1706, 1712, 1716, 1717, 1720, 1726, 1729, 1739, 1750, 1766, 1769, 1797, 1807(?), 1862-64, 1872(?), 1902-03

Latest nearby earthquakes

HeureMag. / ProfondeurDistanceLocation
Fri, 5 Mar 2021 (GMT) (4 earthquakes)
5 Mar 2021 13:09:43 GMT
1.5

14 km - Plus
84 km5.5 Km NNW of Herðubreið, Iceland
5 mars 2021 11:21 (GMT +0) (5 Mar 2021 11:21:22 GMT)
0.6

0.7 km - Plus
28 km2.1 Km WSW of Grímsfjall, Iceland
5 mars 2021 09:36 (GMT +0) (5 Mar 2021 09:36:20 GMT)
0.2

12 km - Plus
76 km2.2 Km N of Herðubreiðartögl, Iceland
5 mars 2021 03:58 (GMT +0) (5 Mar 2021 03:58:41 GMT)
0.5

5.2 km - Plus
56 km16.8 Km NNW of Skaftafell, Iceland
Thu, 4 Mar 2021 (GMT) (1 tremblement de terre)
4 mars 2021 21:11 (GMT +0) (4 Mar 2021 21:11:29 GMT)
0.5

7.6 km - Plus
97 km6.0 Km NNW of Herðubreiðarfjöll, Iceland

Introduction

The volcano is hidden beneath the northwestern part of the Vatnajökull glacier, and contains a 700-m-deep caldera that is hidden beneath ice and has extensive flank fissures, from where eruptions have taken place: the Veidivötn fissure extends for over 100 km to the SW, almost reaching Torfajökull volcano, while the Trollagigar fissure extends 50 km to the NE touching Askja volcano.

A major risk from Bárdarbunga are jökulhlaups (glacier-outburst floods), that can be hazardous for areas in all directions around Bárdarbunga.


See also: Sentinel hub | Landsat 8

Plus sur VolcanoDiscovery

Why is there advertising on this site?
Copyright: VolcanoDiscovery ou autres sources indiquées.
Utilisation des documents: Les textes, les images et les vidéos de ce site internet sont protégées par copyright. Toute reproduction et tout usage sans accord préalable ne sont pas autorisés. Si vous désirez acquérir pour certains documents (photos, vidéos, textes ou autres) le droit de reproduction, d'édition et, plus généralement, de toute utilisation destinée à un usage public, qu'elle soit commerciale ou pas, vous êtes priés de nous contacter.