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Plate 51 from Mineralogie
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Plate 51 from Mineralogie
Or natif en dendriet sur du quartz de Mr. Forster. From Recuille complet de Mineralogie? vol.6 (1790) by F.L. Swebach Desfontaines
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Media ID 20160435
© Bubblepunk / Natural History Museum
1769 Crystal Francois Geological Geology Mineral Mineralogie Mineralogy Observation Quartz Silicate Specimen Study Swebach Tectosilicate Desfontaines
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Plate 51 from Mineralogie, or Native on Quartz of Mr. Forster, is an exquisite illustration from the comprehensive work "Recueil complet de Mineralogie" (Complete Collection of Mineralogy) by F.L. Swebach Desfontaines, published in volume 6 in 1790. This mineralogical masterpiece showcases a stunning specimen of quartz adorned with intricate crystals. The crystals, forming in a dendritic pattern, are reminiscent of the branches of a tree, adding an organic element to the inorganic mineral. Francois Louis Swebach Desfontaines, a renowned French mineralogist, curated this collection to provide an accurate and comprehensive record of minerals known during his time. The observation and documentation of such specimens were essential for the scientific community, as the study of minerals was crucial to the burgeoning field of geology. Quartz, a common silicate mineral, is a tectosilicate, meaning its structure is characterized by a three-dimensional framework of silicon dioxide tetrahedra. The yellow coloration of this particular specimen is due to the presence of impurities, most likely iron or titanium. The illustration, painted with great precision and attention to detail, captures the beauty and complexity of the natural world. This plate serves as a testament to the importance of mineralogical observations and the role they play in our understanding of the Earth's geological history. The Plate 51 from Mineralogie is a valuable addition to any collection focused on the history of mineralogy, geology, or natural history. It offers a glimpse into the past, showcasing the intricacies of a mineral specimen as observed and documented during the late 18th century.
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