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COLUMNAR BASALTS by Prof. Palumbo

The columnar basalts are massive basaltic formations whose show in the territory a submarine eruptive activity or the presence of old volcanoes now gone. Other kind of columnar basalts can be admired:
-- In the gorges of Alcantara
-- To Antrim in the Northern Ireland, where they have originated the famous " Pavement of the Giants "
-- To the island of Staffa, in Scotland, inside the cove of Fingal.
-- To Motta S. Anastasia where they form an extraordinary gorge, residual of an old volcano, but now got off.
They are as pentagonal or hexagonal columns and can be disposed:
1) Vertically (like canes of organ), they are situated at the Northeast of the Great Rock where they have a considerable height, near to the old port of Acitrezza placed to southern part of Lachea island.
From the harbour, they are visible from the seafront, only the heads of basalts can be admired because the columns are not emerged; the zone represents a feeding culvert that the bradyseism and the erosion have carried out and it remembers "the pavement of the Giants" of the Irish County of Antrim.

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Heads of columnar basalts
Port of Acitrezza

Heads of columnar basalts
Port of Acitrezza

Columnar basalts like cane of organ – Great Rock

Oblique columnar basalts - the "Faraglionelli"

 

2) Horizontally, like on Scardamiano seafront (ACICASTELLO).

 

3) Fan-shaped, like those placed on the Vamboleri Mount or on the central "faraglione".

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Columnar basalts fan-shaped - Vamboleri Mount

 

The columnar basalts are closely connected to the pillows because they constitute the culvert of feed where the magma came out creating a fracture that happened during the submarine eruption. The characteristic fissure that they show it is due by the contraction that the magma is subject during the cooling. Usually, the pillows are situated at the top of columnar basalts. In Acitrezza at the top of columnar basalts, the pillows are absent because of the sea that has removed them, while they are present in the zones where resisted to the marine abrasion.

Copyright© 2000-2002 Grasso Giovanni - Antonio Guarnera. Tradotto da Mario Grasso. Translated by Mario Grasso. Tutti i diritti sono riservati. All rights reserved. Vietata la riproduzione anche parziale

Renewed: 04-02-02 .