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The source of Icelandic Glacial – the Ölfus Spring – lies deep beneath an impenetrable layer of lava rock. This natural spring – one of the largest in the world – is continuously replenished from the mountains to the north through the gradual filtration of water from rain, snow and ice melt
The source of Icelandic Glacial – the Ölfus Spring – lies deep beneath an impenetrable layer of lava rock. This natural spring – one of the largest in the world – is continuously replenished from the mountains to the north through the gradual filtration of water from rain, snow and ice melt
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