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Indurated Chalk Capped By the Plateau Basalts, Whitewell Qua
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Indurated Chalk Capped By the Plateau Basalts, Whitewell Qua
Indurated Chalk Capped By the Plateau Basalts, Whitewell Quarry, Belfast - a close in view of rock strata. (Location: Northern Ireland: County Antrim: Belfast). Date: circa early 1900s
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Media ID 14356178
© National Museums NI / Mary Evans
Antrim Belfast Capped Chalk Close Plateau Quarry Strata Whitewell
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EDITORS COMMENTS
Indurated Chalk Capped By the Plateau Basalts: A Geological Marvel at Whitewell Quarry, Belfast, Northern Ireland This photograph, taken in the early 1900s, showcases the stunning geological formation at Whitewell Quarry in Belfast, Northern Ireland. The image reveals a close-up view of the intricately layered rock strata, where indurated chalk is capped by the plateau basalts. Indurated chalk, a type of hardened limestone, is formed when sedimentary chalk undergoes high-pressure metamorphosis. The chalk in this photograph displays a beautiful, smooth, and uniform surface, contrasting the rough and textured appearance of the plateau basalts. The plateau basalts, a type of volcanic rock, were formed during the Paleocene epoch, around 60 million years ago. They were created through volcanic eruptions that covered the region with a thick layer of molten rock. Over time, the basalts cooled and solidified, forming the cap that now rests atop the indurated chalk. The juxtaposition of these two distinct rock types in this photograph is a testament to the dynamic geological history of Northern Ireland. The Whitewell Quarry, located in County Antrim, has long been a source of fascination for geologists and visitors alike, offering a glimpse into the Earth's past and the processes that shaped our planet. This photograph, with its rich history and scientific significance, serves as a reminder of the natural wonders that lie hidden beneath our feet, waiting to be discovered and appreciated.
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