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Geological Formation

Dyngjujökull

Glaciers and Ice Formations

Dyngjujökull is an outlet glacier of the Vatnajökull glacier in Vatnajökull National Park, in the Icelandic Highlands, situated between the volcanic features Bárðarbunga, Holuhraun and Kverkfjöll. Its meltwater flows into Jökulsá á Fjöllum, Iceland second-longest river. On 6 September 2014 scientists discovered depressions in the glacier surface that prompted speculation of eruptions occurring beneath it, associated with seismic activity at the Bárðarbunga caldera that lies beneath the ice. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Facts
Classification
Protected Status
National Park or Reserve 1
Connections

Caused By

Glaciation, Processes

Wikidata P31 formation-type mapped to formative process Glaciation via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Dyngjujökull

In Discipline

Wikidata P31 formation-type mapped to discipline Glaciology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Dyngjujökull
In the Other Atlases
Sources
1. Dyngjujökull (Wikipedia)
Entity description, protection designation
Quote, Entity description, protection designation
Dyngjujökull is an outlet glacier of the Vatnajökull glacier in Vatnajökull National Park, in the Icelandic Highlands, situated between the volcanic features Bárðarbunga, Ho
View the Source
Wikidata: Dyngjujökull
Wikidata Q1269176, class allow-list match (w-wdresolver-0926)View the Source
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