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ICELAND

FALLS

Discover Your favorite waterfall

There are over 10,000 + waterfalls in Iceland! Some of them are iconic, while others are less known. Discover your favorite!
Litlanesfoss Featured Image

Litlanesfoss

Litlanesfoss is the smaller sister to Hengifoss. The waterfall is surrounded by iconic basalt columns, similar to Svartifoss and Aldeyarfoss.

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hraunfossar p3

Hraunfossar

Hraunfossar is a uniquely beautiful series of waterfalls located on the Hallmundarhraun lava field. This lava field was created when a volcano under the Langjokull glacier erupted shortly after the settlement of Iceland. Hraunfossar is formed as several small streams flow from the lava field into the Hvitá river. The name Hraunfossar appropriately means “Lava Falls,” it is also known as “Girdingar cascade.”

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Gullfoss from the walking trail

Gullfoss

Gullfoss is the largest waterfall in Europe with an average flow of water is around 49,441 ft³/s. Gullfoss is fed from the wide Hvítá river.

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Djupavikurfoss featured

Djúpavíkurfoss 

Djúpavíkurfoss is a hidden gem nestled in the rugged landscape of the Westfjords region of Iceland. This breathtaking waterfall tumbles down over a cliff, ending approximately 160 meters below before it flows into the Atlantic Sea. From the seaside at Djúpavík, you can get a stunning view of the waterfall with the small town of Djúpavík in the foreground. The river Djúpavíkurá, which feeds the falls, originates from a plateau with several small lakes and mountains reaching up to 524 meters. Djúpavíkurfoss is located directly on road 643 in the village of Djúpavík, near the Reykjarfjörður fjord. If you’re looking for a unique and off-the-beaten-path destination, Djúpavíkurfoss is definitely worth a visit.

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þórufoss in summer

Þórufoss

ABOUT þórufoss: þórufoss is a little-known waterfall standing at 54 ft (16 m). It’s tucked away on the edge of the Capital Region. Still, it

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Tröllafoss

Tröllafoss

Tröllafoss, or Troll Waterfall, is a beautiful hidden waterfall in the Capital Region on the Leirvogsá river.

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