Vom Vorkommen Des Apatit Flus Gips Schwerspath Und Strontian in Sachsen

<p><i>Vom Vorkommen Des Apatit Flus Gips Schwerspath Und Strontian in Sachsen</i> Volumes 4-6 by Johann K. Freiesleben and Carl H. Mueller is a detailed exploration of the occurrence of various minerals-Apatite Fluoride Gypsum Barite and Strontian-within the region of Saxony. Published in 1830 this work provides valuable insights into the geological formations and mineral deposits of the area during the early 19th century.</p><p>The authors delve into the specific characteristics and locations of these minerals offering a comprehensive overview for geologists mineralogists and historians of science. The book includes observations and remarks on the Saxonian vein formations related to these minerals making it an essential resource for understanding the region's geological composition. This historical text remains relevant for researchers interested in the historical context of mineralogical studies and the geological history of Saxony.</p><p>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.</p><p>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.</p><p>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.</p>