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Untersuchungen über die versteinerungsführenden Diluvialgeschiebe des norddeutschen Flachlandes, mit besonderer Berücksichtigung der Mark Brandenburg (Investigations on the Fossil-Bearing Diluvial Deposits of the North German Plain, with Special Consideration of the Margraviate of Brandenburg) by Adolf Remelé, published in 1882, offers a detailed exploration of the geological formations and paleontological finds in the North German Plain, focusing particularly on the region of Brandenburg. This historical work delves into the study of glacial deposits, known as Diluvialgeschiebe, and their significance in understanding the geological history of the area. Remelé’s investigations provide valuable insights into the types of fossils discovered within these deposits, shedding light on the ancient flora and fauna that once inhabited the region. This book is an important resource for geologists, paleontologists, and historians of science interested in the early research on glacial geology and the natural history of Northern Germany.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.