Vatnajökull National Park (Iceland) – Location, History, Facts
Vatnajökull National Park is a protected area in Iceland that preserves the Vatnajökull ice cap and adjacent highlands.

Vatnajökull National Park, Iceland.
- Country
- Iceland
- Coordinates
- 64.5000° N, 17.0000° W
Vatnajökull National Park overview
Vatnajökull National Park is a protected area in Iceland that preserves the Vatnajökull ice cap and adjacent highlands. It covers an area of roughly 14,200 square kilometres, making it one of the largest national parks in Europe by area. The park encompasses major glacial and volcanic landscapes that are important for earth sciences, biodiversity, and national heritage. Its extent includes extensive ice, outlet glaciers, volcanic systems, and dynamic fluvial landforms.
Vatnajökull National Park coordinates
Vatnajökull National Park is commonly mapped at approximately 64.5000° N, 17.0000° W, or 64.5000, -17.0000 in decimal degrees.
Degrees: 64.5000° N, 17.0000° W
Decimal: 64.5000, -17.0000
Where Vatnajökull National Park is located
Vatnajökull National Park occupies a broad sector of southeastern Iceland, extending from coastal lowlands to interior highlands. The park’s approximate geographic centre lies near 64.5°N latitude and 16.7°W longitude. Administratively the park spans multiple municipalities and parts of Iceland’s southeastern and eastern districts, crossing jurisdictional boundaries. It is bounded to the south by Atlantic coastal plains and to the north by the volcanic highlands, with surrounding features that include glacial outwash plains, mountain ranges, and volcanic systems.
Why Vatnajökull National Park is important
Vatnajökull National Park matters for glaciology because it contains Iceland’s largest ice cap and numerous outlet glaciers that illustrate ice dynamics. The park is scientifically important for studying interactions between glaciers and active volcanic systems, including subglacial eruptions that produce jökulhlaups. Ecologically, it supports specialized Arctic flora and fauna adapted to cold, dynamic substrates. Culturally and symbolically, the landscapes appear in Icelandic literature and national identity, while its geological variety distinguishes it from parks dominated by a single landform type.
History of Vatnajökull National Park
The landscapes now within Vatnajökull National Park were sculpted by repeated glacial activity and volcanic construction over geological time, producing layered lava plains, calderas, and glacial valleys. Human recognition of these landscapes led to protection measures that combined previously protected areas into a single park entity, uniting coastal, glacial, and highland zones under shared governance. Volcanic activity beneath the ice and large-scale glacial floods have repeatedly reshaped landforms, altering drainage patterns and sediment deposition across the park’s terrain. Scientific exploration and long-term monitoring programs established the park’s contemporary conservation rationale.
Natural features of Vatnajökull National Park
Vatnajökull National Park’s dominant physical element is the Vatnajökull ice cap, with outlet glaciers forming long tongues that descend toward coastal plains. Ice thickness reaches up to about one thousand metres in interior sectors, and crevassed glacier fronts, moulins, and icefalls are common observable features. Beneath and around the ice are basaltic lava fields, tephra layers, and volcanic edifices including calderas and central volcanoes. Proglacial rivers carve extensive sandur plains, while mountain peaks and nunataks puncture the ice at the glacier margin.
Environment, protection, and monitoring of Vatnajökull National Park
Vatnajökull National Park is managed as a national protected area by an Icelandic park administration under national environmental authorities. The park’s protection framework prioritises conservation of geomorphological values, biodiversity, and scientific monitoring of glacial and volcanic processes. Long-term management includes systematic observation of ice mass balance, geological hazard surveillance, habitat protection, and coordination with research institutions. Land-use regulation and scientific stewardship aim to maintain the park’s natural systems and support data collection for climate and geohazard research.
Vatnajökull National Park facts
- The park encompasses a mixture of volcanic systems and glacier ice that regularly interact through subglacial eruptions and resultant glacial floods. The Vatnajökull ice cap is the largest ice mass in Iceland by surface area and feeds numerous named outlet glaciers. Local place names and landmark features in the park are referenced in Icelandic sagas and traditional narratives. The park contains volcanic systems that have produced extensive basaltic lava fields and distinctive hyaloclastite formations. Vatnajökull National Park is inscribed on the UNESCO World Heritage List for its outstanding geological and glacial phenomena.
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Frequently Asked Questions
What are the coordinates of Vatnajökull National Park?
Vatnajökull National Park is commonly mapped at approximately 64.5000° N, 17.0000° W, or 64.5000, -17.0000 in decimal degrees.