Aerial view of Skútustaðagígar pseudocraters beside Lake Mývatn in North Iceland, showing circular grassy explosion craters formed over 2,000 years ago.

    Skútustaðagígar pseudocraters on the southern shore of Lake Mývatn, North Iceland.

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    Lake Mývatn Pseudocraters

    Landmark

    Lake Mývatn Pseudocraters are a series of low volcanic formations along the southern shoreline of Lake Mývatn in North Iceland. The circular mounds formed when lava flowed over wet ground, creating steam-driven explosions without direct magma vents. Their clustered shapes create a composition structured by repetition, gentle curvature, and open water backdrop.

    65.60150, -17.00150

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    Quick Facts

    Access

    Short Walk

    5–15 min

    Elevation Gain

    300 m

    Best Light

    Golden Hour
    Overcast

    Light works best when low-angle sun grazes across the crater rims because angled illumination enhances curvature and separates the mounds from the lake surface.

    Why This Light

    Low-Angle Relief
    Reflections

    Season

    Year-Round Stable

    In summer, grass-covered crater rims contrast with the surrounding lake surface. In winter, snow outlines circular forms while maintaining separation between land and water.

    Crowds

    Often Busy

    Photography Notes

    The pseudocraters read strongest from slightly elevated positions where circular forms can be layered against the water. Diagonal framing emphasizes repetition across the shoreline. Avoid flattening the mounds against distant terrain by keeping horizon placement deliberate.

    Nearby Places

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