Transverse Dykes Or Sills in Triassic Sandstone, Scrabo
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Transverse Dykes Or Sills in Triassic Sandstone, Scrabo
Transverse Dykes Or Sills in Triassic Sandstone, Scrabo. Newtownards - a view of strata in an exposed section of hillside. (Location: Northern Ireland; County Down; Newtownards). Date: circa early 1900s
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Media ID 14356154
© National Museums NI / Mary Evans
Dykes Exposed Hillside Newtownards Sandstone Scrabo Section Strata Triassic Sills Transverse
EDITORS COMMENTS
1. Title: Transverse Dykes or Sills in Triassic Sandstone, Scrabo: A Glimpse into Geological History 2. Description: This photograph captures an exposed section of the hillside at Scrabo in Newtownards, Northern Ireland, revealing the intriguing presence of transverse dykes or sills in the Triassic Sandstone formation. Dating back to the early 1900s, this image offers a fascinating glimpse into the geological history of this region. 3. Background: The Triassic period, spanning approximately 252 to 201 million years ago, is a critical era in Earth's history, marked by the emergence of dinosaurs and the first reptiles. The Triassic Sandstone formation in County Down, Northern Ireland, is a testament to the diverse geological processes that shaped our planet during this time. 4. Geological Features: Transverse dykes and sills are intrusive igneous formations that cut across the existing rock strata. They are created when magma or molten rock forces its way into existing cracks and fissures in the Earth's crust. In this image, the transverse dykes or sills can be seen as the darker, more distinct bands that cross the lighter Triassic Sandstone layers. 5. Historical Significance: This photograph holds significant historical value, as it provides a rare and intriguing look into the geological past. The presence of these transverse dykes or sills in the Triassic Sandstone formation at Scrabo offers valuable insights into the tectonic activity and geological processes that shaped this region during the Triassic period. 6. Conclusion: This photograph of Transverse Dykes or Sills in Triassic Sandstone at Scrabo, Newtownards, Northern Ireland, is a captivating reminder of the rich geological history that lies beneath our feet. It invites us to explore the fascinating processes that shaped our planet and offers a glimpse into the complex and ever-evolving world of Earth sciences.
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