Lysefjord cuts 42 kilometers inland from Stavanger, a glacially carved channel bounded by walls that rise 1,000 metres vertical from saltwater. The fjord formed during the last Ice Age, when ice sheets two kilometres thick ground through Precambrian bedrock, leaving behind a U-shaped trough now flooded by the North Sea. Preikestolen, the plateau that juts 604 metres above the eastern shore, became a pilgrimage site only in the late 20th century; before 1900, locals avoided the cliffs, considering them cursed. The first recorded ascent by a woman occurred in 1883, when a British tourist hired two farmers to guide her up the unmarked scree. Today, Lysefjord anchors a constellation of natural landmarks that draw half a million visitors annually. Kjeragbolten, a boulder wedged in a mountain crevice five kilometres south of Preikestolen, appeared in National Geographic in 1994 and became an Instagram fixture three decades later. Fantahålå, a sea cave accessible only by boat, extends 30 metres into the cliff face; its acoustics amplify engine noise into a cathedral hum. Hengjanefossen, a 400-metre waterfall on the northern shore, flows year-round, fed by snowmelt from the Kjerag plateau. The fjord's ecology is rare: brackish surface water sits atop a saline layer 20 metres down, creating a halocline that supports both freshwater trout and deepwater cod. Electric ferries and RIB boats now ply routes that coal steamers pioneered in the 1860s. Forsand, the village at the fjord's head, served as a timber port until the 1950s; log booms once choked the narrows each spring. The old quay survives, repurposed as a departure point for cruise operators. Stavanger's maritime district, Vågen, lies 25 kilometres west by water, a sheltered harbor that Norse traders used a millennium before oil companies arrived in 1969. The contrast defines the region: Stavanger's cranes and refineries fund the infrastructure that protects Lysefjord's roadless shores, ensuring the cliffs remain as glaciers left them twelve thousand years ago.