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Granite, collected by Dr Benza from the summit of the Western range of Kaitee Valley
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Granite, collected by Dr Benza from the summit of the Western range of Kaitee Valley
Granite, collected by Dr Benza from the summit of the Western range of Kaitee Valley, Neilgherries, India c.1837. NHM specimen number: BM 651
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Media ID 8623458
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Benza Granite Igneous Intrusion Intrusive Intrusive Rock White Background Neilgherries
EDITORS COMMENTS
This stunning photograph showcases a beautiful specimen of Granite, collected by Dr. Benza from the summit of the Western range of Kaitee Valley in the Neilgherries region of India around 1837. The nineteenth century image, now held in the Natural History Museum in London under the specimen number BM 651, captures the intricacies and raw beauty of this igneous rock. Granite, an intrusive rock, is formed deep within the Earth's crust through the slow cooling and solidification of magma. The Victorian era, known for its fascination with the natural world, saw an increase in the collection and study of such geological specimens. Dr. Benza's acquisition of this granite sample from Kaitee Valley adds to the rich history of geological discoveries made during this period. The photograph, taken against a pristine white background, highlights the intricate patterns and textures of the granite. The image, reminiscent of the nineteenth century, transports us back in time to an era of exploration and discovery. The intrusive nature of this rock, formed through the slow cooling of magma, is evident in the photograph, with its distinct crystalline structure and varied shades of gray and white. This photograph is a testament to the beauty and intrigue of the natural world, and serves as a reminder of the important role that exploration and discovery played in shaping our understanding of the Earth's geology during the nineteenth century. The intrusive granite specimen from Kaitee Valley, collected by Dr. Benza, continues to inspire awe and fascination among geologists and enthusiasts alike, over 180 years after its discovery.
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