Fingal's Cave, Sea cave in Inner Hebrides, Scotland.
Fingal's Cave reaches about 1130 meters into Staffa island, displaying geometric columns of dark basalt formed by cooling volcanic rock. The sea enters deep into the opening, making the hexagonal pillars appear like organ pipes along both walls.
Joseph Banks described the formation in 1772 after an expedition to the Hebrides, bringing it to scientific attention. His reports led to numerous visits by artists and writers throughout the 19th century.
The Gaelic name Uamh-Binn means cave of melody, describing the echoing sounds created when waves strike the basalt walls. Visitors still hear this natural music today with each wave rolling through the columns.
Boat tours depart from Oban and Iona, allowing access to Staffa island when calm seas permit safe landing. Spring and autumn often offer more favorable conditions than summer, when the sea can become rougher.
The hexagonal basalt columns are part of the same geological events that created the North Atlantic volcanic fields around 60 million years ago. This formation connects with similar structures beneath the sea to the Northern Irish coast.
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