Gullfoss is one of Iceland's most prominent hydrological features, situated in the upper reaches of the Hvítá River. While the aesthetic and touristic value of the site is well-documented, the structural geology facilitating its existence remains a subject of specific interest. The "Gullfoss Crack" serves as a colloquial term for the deep, narrow gorge into which the waterfall cascades. This draft paper aims to delineate the tectonic origins of this gorge, positing that the feature is a graben-like structure resulting from the extensional forces of the Mid-Atlantic Ridge, rather than a feature formed solely by fluvial erosion.
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This paper presents a preliminary geological and structural analysis of the fracture network dominating the Gullfoss (Golden Falls) region in Southwest Iceland. Referred to herein as the "Gullfoss Crack," this feature is not a singular anomaly but a manifestation of the intense tensile stress regime characteristic of the divergent plate boundary. We examine the interaction between the underlying rifting tectonics of the Western Volcanic Zone (WVZ) and the erosional mechanics of the Hvítá River. By analyzing the orientation, depth, and propagation of the fracture systems, we propose that the waterfall’s location and distinct two-tiered morphology are structurally controlled by pre-existing weaknesses in the tholeiitic basalt, exacerbated by ongoing seismic activity. Gullfoss is one of Iceland's most prominent hydrological
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Brings out masked frequencies that are "hidden" in the mix. This draft paper aims to delineate the tectonic
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