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Landscape of St Kilda
Landscape
of St Kilda
Explosive
Beginnings
The dramatic
coastal scenery of the St Kildan islands is a result of their being
formed of resistant crystalline rock. Some 60 million years ago
volcanic activity was a feature of what is now the western coast
of Scotland. A chain of volcanoes stretched from south of Arran
northwards across the continental margin into the Atlantic. Molten
rock, generated by the stretching of the Earth's upper mantle and
overlying crust, ascended through the crust to erupt from large
central volcanoes or elongated fissures.
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St Kilda marks
the site of one of the central volcanoes and the rocks which now
form the spectacular group of islands resulted from the slow cooling
of molten magma deep beneath the erupting volcano. Magmas of different
composition formed the dark grey gabbros which run from Soay, Hirta
and Dun to Boreray, and the light pink granite of Conachair and
Oiseval.
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Photograph: Graham Durant
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two magma types had different compositions, the gabbros being relatively
richer in magnesium and iron and the granites being relatively richer
in silicon. From time to time the two magmas, existing at significantly
different temperatures and densities, mixed together, triggering volcanic
eruptions at the surface. Evidence for this process is preserved in
the rocks and boulders at the western end of Village Bay. |

Photograph: Graham Durant
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| Dark
pillow-like blobs of hot gabbroic magma mixed with cooler lighter-coloured
granite to form this striking rock exposed adjacent to Caolas an Duin.
Elsewhere, more thorough mixing of the two magma types formed a range
of hybrid diorite crystalline rocks. |

Photograph: Graham Durant
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| Thin
inclined sheets and dykes of fine-grained basalt cut through the various
gabbros and granophyres. These are conspicuous features in the granite
cliffs of Oiseval. |

Photograph: Graham Durant
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| Sixty
million years of erosion following the end of volcanic activity has
left the resistant heart of a volcano standing proud close to the
edge of the north-west European continental margin. |

Photograph: Graham Durant
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