On the Geological Age of the Ballycastle Coal Field, and Its Relations to the Carboniferous Rocks of the West of Scotland
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"On the Geological Age of the Ballycastle Coal Field, and Its Relations to the Carboniferous Rocks of the West of Scotland" is a detailed exploration of the geological characteristics of the Ballycastle coal field in Ireland and its connection to similar rock formations in western Scotland. Authored by Edward Hull and the Royal Geological Society of Ireland, this work, originally published in 1871, provides valuable insights into the region's geological history. The book offers a comprehensive study of the coal field's age and composition, contributing to a broader understanding of Carbonifero...
"On the Geological Age of the Ballycastle Coal Field, and Its Relations to the Carboniferous Rocks of the West of Scotland" is a detailed exploration of the geological characteristics of the Ballycastle coal field in Ireland and its connection to similar rock formations in western Scotland. Authored by Edward Hull and the Royal Geological Society of Ireland, this work, originally published in 1871, provides valuable insights into the region's geological history. The book offers a comprehensive study of the coal field's age and composition, contributing to a broader understanding of Carboniferous geology. It remains a significant resource for geologists, paleontologists, and historians of science interested in the geological makeup of Ireland and Scotland. This historical scientific work provides a foundational understanding of geological formations and comparative regional geology. This work has been selected by scholars as being culturally important, and is part of the knowledge base of civilization as we know it. This work was reproduced from the original artifact, and remains as true to the original work as possible. Therefore, you will see the original copyright references, library stamps (as most of these works have been housed in our most important libraries around the world), and other notations in the work. This work is in the public domain in the United States of America, and possibly other nations. Within the United States, you may freely copy and distribute this work, as no entity (individual or corporate) has a copyright on the body of the work. As a reproduction of a historical artifact, this work may contain missing or blurred pages, poor pictures, errant marks, etc. Scholars believe, and we concur, that this work is important enough to be preserved, reproduced, and made generally available to the public. We appreciate your support of the preservation process, and thank you for being an important part of keeping this knowledge alive and relevant.
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