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Glass Frame : Plate 4, fig 2 Puddingstone - from Mineralienbuch
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Plate 4, fig 2 Puddingstone - from Mineralienbuch
An illustration of a polished section of puddingstone. Puddingstone is a conglomerate sedimentary rock. Plate 4, fig 2 from Mineralienbuch by F. A. Schmidt, Stuttgart 1855
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Media ID 8617681
© Mary Evans Picture Library 2015 - https://copyrighthub.org/s0/hub1/creation/maryevans/MaryEvansPictureID/10706048
Abstract Conglomerate Irregular Matrix Mineral Pebble Polished Schmidt Section Sedimentary Sedimentary Rock Plate 4
7"x5" Glass Mount
Wall mounted or free-standing, these black edged glass frames feature a smooth chamfered edge and a stylish black border (on back face of the glass). Manufactured from 4mm thick glass, Glass Mounts are a durable, professional way of displaying and protecting your prints. Your 7x5 print is slotted into the back of the frame so can easily be changed if needed.
Tempered Glass Mounts are ideal for wall display, plus the smaller sizes can also be used free-standing via an integral stand
Estimated Image Size (if not cropped) is 12.7cm x 17.7cm (5" x 7")
Estimated Product Size is 16.2cm x 20.3cm (6.4" x 8")
These are individually made so all sizes are approximate
Artwork printed orientated as per the preview above, with portrait (vertical) orientation to match the source image.
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EDITORS COMMENTS
Plate 4, Figure 2: A Polished Section of Puddingstone from Mineralienbuch by F.A. Schmidt (1855) This illustration is a close-up view of Plate 4, Figure 2 from Mineralienbuch by F.A. Schmidt, published in Stuttgart, Germany, in 1855. The image showcases a polished section of puddingstone, a unique and intriguing sedimentary rock. Puddingstone, also known as breccia, is a conglomerate rock characterized by its irregular, rounded clasts or pebbles, which are set in a fine-grained matrix. The name "puddingstone" is derived from the English word "pudding," which refers to the rock's appearance, resembling a pudding with its distinct, rounded pebbles suspended in a fine-grained, often calcareous, matrix. The illustration provides a detailed view of the various components of this sedimentary rock. The larger, rounded pebbles, which can range from pebbles to boulders in size, are interspersed within the fine-grained matrix. The matrix itself is typically composed of calcareous material, such as limestone or chalk, and may contain minute fossils and other mineral inclusions. The polished section reveals the intricate textures and structures of the puddingstone, providing a glimpse into the geological processes that formed this fascinating rock. The irregular shapes and sizes of the pebbles suggest that they were transported and deposited in a watery environment, possibly during a catastrophic event such as a flood or a landslide. This illustration, a testament to the meticulous work of F.A. Schmidt, offers a unique perspective on the beauty and complexity of the natural world. It invites us to explore the intricacies of geology and the wonders of the Earth's history, while also showcasing the artistic skill and attention to detail of the illustrator.
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