Lysefjord (Norway) – Location, Geography & Facts

Lysefjord is a fjord in Norway located in Rogaland county on the country’s southwestern coast.

Lysefjord, Norway.

Country: Norway
Coordinates: 59.0100° N, 6.3590° E

Lysefjord overview

Lysefjord is a fjord in Norway located in Rogaland county on the country’s southwestern coast. The fjord extends roughly 42 kilometres from its mouth at Høgsfjorden inland to the hamlet of Lysebotn, with maximum reported depths exceeding 400 metres; this measurable length and depth mark Lysefjord as a prominent glacial fjord in Norwegian hydrography. The entry identifies its physical form, shoreline features, and regional significance for geology and infrastructure.

Lysefjord coordinates

Lysefjord is commonly mapped at approximately 59.0100° N, 6.3590° E, or 59.0100, 6.3590 in decimal degrees.

Degrees: 59.0100° N, 6.3590° E

Decimal: 59.0100, 6.3590

Where Lysefjord is located

Lysefjord lies in the Ryfylke district of Rogaland in southwestern Norway, positioned east of the urban area around Stavanger. The fjord opens into Høgsfjorden and trends inland to Lysebotn, with its shoreline touching local settlements including Forsand and Lysebotn. Administratively the shoreline falls within Rogaland municipalities and regional planning zones that shape land use and resource management. Surrounding physical features include steep cliff faces, narrow side valleys feeding the fjord, and a rocky mouth framed by skerries and headlands.

Why Lysefjord is important

Lysefjord matters for its textbook example of a glacially carved U-shaped fjord with near-vertical rock walls and a deep marine basin, distinguishing it from shallower coastal inlets. The presence of the Preikestolen plateau on the northern flank, a flat-topped cliff about 604 metres above the fjord, and the Kjerag massif rising above 1,000 metres are distinct cultural and geomorphological markers tied to Lysefjord. Scientific studies of fjord stratification, sediment deposition, and steep-slope rock mechanics often cite Lysefjord because of its well-exposed bedrock and dramatic bathymetry.

History of Lysefjord

Lysefjord’s form results from repeated glacial sculpting during the late Quaternary, when successive ice sheets deepened valleys in the crystalline bedrock and left a steep-walled trough subsequently inundated by rising post-glacial sea levels. Human settlement history centers on small hamlets along sheltered bays and the use of fjord waters for local transport and fishing; settlements at Lysebotn and Forsand developed around these marine resources. In more recent centuries the steep gradients of the Lysefjord watershed were harnessed for hydropower and engineered infrastructure, which altered runoff regimes and introduced tunnels, reservoirs, and intake works specific to this drainage basin.

Natural features of Lysefjord

Lysefjord’s physical structure includes a narrow entrance widening inland to a deep axial basin underlain by Precambrian gneiss and granite. The fjord displays vertical cliffs, scree slopes, and perched rock plateaus formed by jointing and differential weathering of hard bedrock. Notable built features tied to the fjord’s topography include powerstation intakes and pressure tunnels that exploit the long fall from high-elevation catchments to the fjord outlet. Small rocky islets and submerged ledges occur near the mouth, while steep tributary ravines incise the surrounding highlands.

Environment, protection, and monitoring of Lysefjord

Portions of the Lysefjord shoreline and adjacent uplands are subject to municipal landscape protections and national environmental oversight, with management responsibilities shared between local authorities and Norwegian environmental agencies. The fjord sustains deep-water benthic communities and steep-terrain ecosystems that require monitoring for sediment disturbance and water-quality changes linked to land-use and hydropower operations. Long-term stewardship emphasizes scientific monitoring, catchment management to limit erosion, and regulatory frameworks that govern resource extraction and landscape conservation specific to the Lysefjord catchment.

Lysefjord facts

Lysefjord was sculpted by glacial ice that excavated a deep trough through hard Precambrian bedrock, creating its characteristic steep walls.
Lysefjord measures about 42 kilometres in length and reaches depths greater than 400 metres in its central basin.
The Preikestolen plateau on Lysefjord’s northern side rises to approximately 604 metres above the fjord and forms a prominent cliff face.
Kjerag above Lysefjord includes a famous wedged boulder, known as Kjeragbolten, lodged between two rock walls on the mountain’s steep flank.
Hydropower infrastructure in the Lysefjord watershed uses the fjord’s large elevation gradients and has shaped modern engineering within this specific drainage system.

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