Skjaldbreiður (Icelandic pronunciation: [ˈscaltˌpreiːðʏr̥], "broad shield") is an Icelandic lava shield formed in one huge and protracted eruption roughly 9,000 years ago[citation needed]. The extensive lava fields which were produced by this eruption, flowed southwards, and formed the basin of Þingvallavatn, Iceland's largest lake, and Þingvellir, the "Parliament Plains" where the Icelandic national assembly, the Alþing was founded in 930.
This article may be expanded with text translated from the corresponding article in Icelandic. (January 2022) Click [show] for important translation instructions.
|
Skjaldbreiður | |
---|---|
Highest point | |
Elevation | 1,060 m (3,480 ft) |
Coordinates | 64°24′36″N 20°45′44″W |
Naming | |
English translation | broad shield |
Language of name | Icelandic |
Geography | |
Geology | |
Age of rock | 9,000 years |
Mountain type | shield volcano |
The volcano summit is at 1,060 metres, and its crater measures roughly 300 metres in diameter.
Straddling the Mid-Atlantic ridge, the lava fields from Skjaldbreiður have been torn and twisted over the millennia, forming a multitude of fissures and rifts inside the Þingvellir National Park, the best known of which are Silfra, Almannagjá [ˈalˌmanːaˌcauː], Hrafnagjá [ˈr̥apnaˌcauː] and Flosagjá [ˈflɔːsaˌcauː].
Active volcanoes of Iceland | |
---|---|
Eastern Volcanic Zone |
|
Northern Volcanic Zone | |
Reykjanes Volcanic Zone |
|
Note: Volcanoes listed here are "central volcanoes" unless a (f) is place after name, in that case the volcano is a fissure. |