A Two-Stage Geological Saw
Gullfoss is not a single plunge but a two-tiered system cutting through ancient rock. The process began at the end of the last ice age, as meltwater from the Langjökull glacier formed the powerful Hvítá river. The river flows across layers of rock formed during warm interglacial periods. These layers consist of hard dolerite (a type of basalt) and softer, sedimentary layers of conglomerate rock, mudstone, and gravel. The water uses these differences in hardness. It carves through the softer materials more easily, creating a stepped descent.
The upper cascade is a drop of 11 meters (36 feet), followed by a second, more dramatic plunge of 21 meters (69 feet). This second drop turns at a near-right angle into a narrow canyon, the Gullfossgjúfur. This canyon is approximately 2.5 kilometers long and up to 70 meters (230 feet) deep. The constant abrasive action of the water continues to lengthen the canyon by an estimated 25 centimeters each year. The primary cause for this rapid excavation is the presence of loose gravel lenses within the sedimentary layers, which the river easily washes away.