The Isle of Staffa is a classic geological site, part of the Tertiary volcanics of Scotland part of the Mull volcanic Group. . The lower section with its famous sea-caves consists of columnar basalt, an upper more rubble-like lava forming the upper section. It is also an example of differential cooling of ejected lava materials.
No EXIF information is available
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Keywords:basalt, fingals cave, igneous, isle of mull, isle of staffa, lava-flows, lavas, scotland, sea-caves, tertiary, volcanic
