Some 50 to 60 million years ago, during the Paleogene period, Antrim was subject to intense volcanic activity, when highly fluid molten basalt intruded through chalk beds to form an extensive lava plateau. As the lava cooled rapidly, contraction occurred. While contraction in the vertical direction reduced the flow thickness (without fracturing), horizontal contraction could only be accommodated by cracking throughout the flow. The size of the columns is primarily determined by the speed at which lava from a volcanic eruption cools. The extensive fracture network produced the distinctive columns seen today. The basalts were originally part of a great volcanic plateau called the Thulean Plateau which formed during the Paleogene period.
Giclee reproduction canvas prints come on titanum primed genuine artist's canvas. They are waterproof and archival, reproducing excellent fine details and color. Overall canvas size is 16.54" by 11.69" (420mm by 297mm).
We do not compromise on material costs - our canvas is imported from the USA, and prepared in London, England. Reproduction prints come on titanum primed genuine artist's canvas. They are waterproof and archival, reproducing excellent fine details and color. Overall canvas size is 16.54" by 11.69" (420mm by 297mm), and image size is slightly smaller to account for an approximate one inch border. Canvases come unframed and unmounted, and although they may be stretched, this is not at all necessary. These exquisite canvases are suited to traditional framing, and look great with or without glass, depending on personal preference.
- Canvas Ref : tp05095
- 50 Units in Stock
Art
Victorian Britain
England
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