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– Jan Erik Waider
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Cracked Mud

Námafjall geothermal area, Iceland

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ID: ICE-CM-01 / Licensing
Aerial view of abstract mud cracks and sand in Námafjall, Iceland
ID: ICE-CM-02 / Licensing
Cracked mud formations in the geothermal field of Námafjall, Iceland
ID: ICE-CM-03 / Licensing
Patterns of cracked mud formations in Námafjall geothermal area, Iceland
ID: ICE-CM-04 / Licensing
Aerial view of intricate mud cracks in Námafjall geothermal field, Iceland
ID: ICE-CM-05 / Licensing
Abstract Aerial Landscape Photography by Northlandscapes, Jan Erik Waider
ID: ICE-CM-06 / Licensing
Aerial imagery of dried mud cracks in Námafjall geothermal area (Iceland)
ID: ICE-CM-07 / Licensing
Aerial Fine Art Photography of Iceland by Northlandscapes, Jan Erik Waider
ID: ICE-CM-08 / Licensing
Textured landscapes: Aerial imagery of dried mud cracks in Námafjall, Iceland
ID: ICE-CM-09 / Licensing
Mud pool in Námafjall geothermal area, Iceland
ID: ICE-CM-10 / Licensing
Abstract patterns formed by dried mud cracks in Námafjall, Iceland
ID: ICE-CM-11 / Licensing
Abstract patterns formed by dried mud cracks and water in Námafjall, Iceland
ID: ICE-CM-12 / Licensing
Aerial view of abstract mud cracks in Námafjall geothermal field, Iceland

Cracked Mud

The Hverir geothermal area at the foot of Mount Námafjall is located in the northeast of Iceland, on the east side of Lake Mývatn. Námafjall is a still active volcano that belongs to the Krafla volcanic system. In this area, there are numerous smoking fumaroles and boiling mud pots surrounded by bright yellow sulfur crystals.

The cracks in the mud are formed due to the expansion and contraction of the mud caused by the heating and cooling of the ground. As the hot geothermal water rises to the surface and cools down, it creates a layer of solid crust over the mud. When the underlying mud contracts as it cools, it creates tension in the crust, which eventually cracks and breaks.

Published October 2022

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