Lists all names used for mineral substances throughout history which are NOT now considered valid or current. Each mineral today can have only a single name and modern mineralogical science does not recognize gemologically important colour variations with independent names. Designed as a companion to: Fleischer's glossary of mineral species.
1.1 Prologue What is archaeomineralogy? The term has been used at least once before (Mitchell 1985), but this volume is the first publication to lay down the scientific basis and systematics for this subdiscipline. Students sometimes call an introductory archaeology course "stones and bones." Archaeomineralogy covers the stones component of this phrase. Of course, archaeology consists of a great deal more than just stones and bones. Contemporary archaeology is based on stratigraphy, geomorphology, chronometry, behavioral inferences, and a host of additional disciplines in addition to those devoted to stones and bones. To hazard a definition: archaeomineralogy is the study of the minerals and rocks used by ancient societies over space and time, as implements, orna ments, building materials, and raw materials for ceramics and other processed products. Archaeomineralogy also attempts to date, source, or otherwise char acterize an artifact or feature, or to interpret past depositional alteration of archaeological contexts. Unlike geoarchaeology, archaeomineralogy is not, and is not likely to become, a recognized subdiscipline. Practitioners of archaeomineralogy are mostly geoarchaeologists who specialize in geology and have a strong background in mineralogy or petrology (the study of the origin ofrocks).
This work is the critical edition of the catalog of Holy Roman Emperor Leopold’s II mineralogical collection. The volume, unpublished and preserved at the Historical Archives of the University of Firenze Museum System, dates to 1765 and describes 242 mineralogical specimens coming primarily from the current Slovak-Hungarian mining district. This edition gives the transcription of the German manuscript and its translation into English together with an organized system of notation to illustrate the complex history of the text, the characterization of the mineralogical species, and the geographical location of the mineral extraction sites. This work represents to date the only published catalog of a mineralogical collection belonging to a member of the Habsburg-Lorraine family.
The fifth edition of the Glossary of Geology contains nearly 40,000 entries, including 3.600 new terms and nearly 13,000 entries with revised definitions from the previous edition. In addition to definitions, many entries include background information and aids to syllabication. The Glossary draws its authority from the expertise of more than 100 geoscientists in many specialties who reviewed definitions and added new terms.
“Archaeomineralogy” provides a wealth of information for mineralogists, geologists and archaeologists involved in archaeometric studies. The first edition was very well-received and praised for its systematic description of the rocks and minerals used throughout the world by our ancestors and for its excellent list of over 900 references, providing easy access to the fields of archaeomineralogy and geoarchaeology. This second edition of “Archaeomineralogy” takes an updated and expanded look at the human use of rocks and minerals from the Paleolithic through to the 18th century CE. It retains the structure and main themes of the original but has been revised and expanded with more than 200 new references within the text, a bibliography of additional references not included in the text, a dozen new figures (drawings and photos), coverage of many additional important mineral, rock, and gem materials, a broader geographic scope, particularly but not limited to Eastern Europe, and a more thorough review of early contributions to archaeomineralogy, especially those of Agricola. From reviews of the first edition: "... crammed full of useful information, is well-balanced using both new and Old World examples of the archaeomaterials described. It also provides a broad, but of necessity, all too brief overview of the geological raw materials used in antiquity." -- Geoscientist "...provides much interesting discussion of how particular names came to be employed by archaeologists working in different regions of the world.... much to offer for any geologist or archaeologist interested in minerals and rocks and how they have been used in the past." -- Mineralium Deposita "... a gem of a book, it's strength is that it is encyclopedic in content, if not in layout, draws on a wealth of field experience and almost every sentence contains a nugget of information" -- The Holocene
Volume 50 of Reviews in Mineralogy and Geochemistry treats Beryllium and its cosmogenic isotopes. This volume includes an overview of Be studies in the earth sciences and a systematic classification of Be minerals based on their crystal structure. It treats the analysis of these minerals by the secondary ion mass spectroscopy as well as experimental studies of systems involving Be. Moreover, this volume reviews the behavior of Be in the Solar System, with an emphasis on meteorites, the Moon and Mars, and the implications of this behavior for the evolution of the solar system. It gives an overview of the terrestrial geochemistry of Be and discusses the contamination of the environment by this anthropogenic toxin. It reports use of the longer lived Be-10 to assess erosion rates and other surficial processes and how this isotope can yield independent temporal records of geomagnetic field variations for comparison with records obtained by measuring natural remnant magnetization, be a chemical tracer for processes in convergent margins, and can date events in Cenozoic tectonics. It reviews applications of the shorter lived isotope Be-7 in environmental studies as well. Residual phases include acidic plutonic and volcanic rocks, whose geochemistry and evolution are covered, while granitic pegmatites, which are well-known for their remarkable, if localized, Be enrichments and a wide variety of Be mineral assemblages, are reviewed. Not all Be concentrations have obvious magmatic affinities; for example, one class of emerald deposits results from Be being introduced by heated brines. Pelitic rocks are an important reservoir of Be in the Earth's crust and their metamorphism plays a critical role in recycling of Be in subduction zones, eventually, anatectic processes complete the cycle, providing a source of Be for granitic rocks.
An understanding of rocks and the minerals that comprise them lies at the core of every geologist’s education. As more curricula combine mineralogy and petrology into a single course, Raymond and Johnson have responded with a concise introduction to the study of Earth materials. The authors have written at a level that won’t intimidate students encountering fundamental concepts for the first time, yet with enough rigor that they’ll be well prepared for future study. A broad approach to the subject that incorporates fluids and soils will appeal to instructors who teach engineering and environmental science students as well as future geoscientists. Abundant illustrations reinforce all of the ideas in the text. Many images are presented in color, with additional color images available at waveland.com/Raymond-Johnson. Problems appear throughout the book, encouraging a deeper understanding for students. Helpful appendices make it easy for instructors to assign further exercises in rock and mineral identification as well as optical mineralogy and petrography.