![The Public Domain Review](/static/pdr-logo_2x-a9aa17abb46a7af84cd791867a6031ec.png)
James Sowerby’s British Mineralogy (1802–17)
On December 13, 1795, a fifty-six-pound meteorite fell from the sky into an English quarry. Wondering if it had “come from some volcano in the Moon”, the landowner turned this lump of multi-colored minerals over to James Sowerby, a well-connected scientific illustrator and naturalist. Sowerby published an extensive account of what became known as the “Yorkshire Meteorite” in his five-part mineralogical handbook, inviting pushback from geologists who thought that including a “Phaëton from the heavens might seem absurd in a work on British Mineralogy”. Since the curious object contained substances commonly found within mines of the British Isles, Sowerby believed the meteorite belonged in a volume primarily devoted to more mundane earthbound subjects, such as table salt and oxygenized carbon.
Comprised of more than four hundred vividly hand-colored engravings of various rocks, minerals, and compounds, British Mineralogy saw the Royal Academy-trained illustrator depart from his focus on botany toward non-living specimens. Pledging to leave “no stone unturned” in communicating to both laypeople — farmers, miners, and surveyors — and a growing class of gentlemanly mineralogists interested in theories of evolutionary transmutation, Sowerby tried to bridge ever-growing cleavages in geological communities during a time when the age of Earth was hotly disputed. Geologists adhering to “Volcanian” and “Neptunian” theories of planetary origin might, at long last, “shake hands together”, if provided with detailed illustrations of every known British “species” of rock and mineral. By referencing these dueling ideologies, which argued that the Earth was born either out of fiery eruption or biblical deluge, Sowerby positioned his work at the center of a debate that held enormous stakes far beyond the realm of geology.
James Sowerby, British Mineralogy, or, Coloured Figures Intended to Elucidate the Mineralogy of Great Britain, Vol. 1 (London: R. Taylor and Co., 1804).
Catastrophism — the idea that the origins of Earth and the transmutation of species have been shaped by sudden, often violent events — dominated early-nineteenth century scientific debates about evolution and extinction. Embraced, by some, as a way of reconciling biblical beginnings with increasingly common discoveries of fossilized bones that pointed to a decidedly non-Christian view of the world, the set of layered theories attempted to integrate mass extinction with ongoing transmutation. Sowerby, who was deeply committed to public scholarship, refused to weigh in on the religious implication of his geological work, saving it for later texts on less “controversial” subjects. Seemingly circumspect in his own beliefs, Sowerby gestured towards, while never fully engaging with, profound conversations between science and religion.
Despite his scientific leanings, James Sowerby was first and foremost an artist. From his intricately detailed accounts of fungi and shells to his 1809 A New Elucidation of Colour Theory (dedicated to none other than Isaac Newton), the naturalist was concerned with translating three-dimensional, colorful, and sometimes ephemeral objects to the flat surface of the page. Adept in describing and demonstrating how complex questions of perspective, scale, and color functioned in individual objects, Sowerby’s observational eyes and deft hands were remarkable for the time and continue to work as standards within scientific illustration. The illustrator’s rocks and minerals were, at once, geometric objects and geological proofs of the Earth’s age.
By the 1830s, geologists had largely replaced catastrophic origin theories with “uniformitarian” ideas of gradual change. These ideas were most clearly articulated in geologist Charles Lyell’s enormously popular and oft-revised Principles of Geology, a scantily illustrated text that formed the sediments of Charles Darwin’s theory of evolution by natural selection. Sowerby, for his part, continued to add natural-historical specimens to his private collections while building a familial legacy of scientific collecting and illustration that lasted for generations. As Sowerby’s disciple John Mawe wrote in his public-facing Familiar Lessons on Mineralogy and Geology, the magic and mystery of mineralogy, from meteorite to table salt, lay in its multiple identities, spanning audiences and consumers. Rocks and minerals, in all of their mundanity, held beautiful and sublime lessons about the world for specialists and non-specialists alike — a beauty that Sowerby was devoted to capturing through illustration, and a beauty that continues to capture illustrators and designers more than two centuries later.
Find below highlights of plates from all five volumes. You can see the first four volumes at the Biodiversity Heritage Library, and the full set at e-rara. Also check out this wonderful hand-copied selection from Sowerby's work made in 1840 by a woman named Martha Proby.
Calcite (Calcareous Spar)
Satin Spar (Calx sericea)
Azure Iron Ore (Ferrum caeruleum)
Crystallized Carbonite of Lime, lenticular-equiaxed (Calx carbonata)
Argilla Marga (Argillaceous Marle)
Sulfate of Iron (Ferrum sulphuratum)
Silky filamentous Sulphate of Iron (Ferrum sulphuratum)
Arseniate of Copper (Cuprum arseniatum)
Siliceous Sandstone (Silex arenacea)
Byssus-like Carbonate of Copper (Cuprum carbonatum)
Oxygenized Carbon (Carbo oxygenizatus)
Argillaceous Iron Ore (Ferrum argillaceum)
Spathose Iron Ore; Lenticular crystallized Carbonate of Lime (Calx carbonata ferrifera, var. lenticularis)
Sulfate of Barytes (Barytes sulphata, var. primitiva)
Sulphuret of Copper (Cuprum sulphuratum)
Variegated Limestone; or Tirie Marble (Calx carbonata, var. petrosa)
Arseniate of Iron (Ferrum arseniatum)
Flint Pebbles, &c. (Silex Quartzum)
Quartzose Pudding Stone (Silex Quartzum, var. aggregatum)
Arseniate of Copper (Cuprum arseniatum)
Carbonate of Copper (Cuprum carbonatum)
Sulphate of Barytes
Arseniate of Iron
Argillaceous Oxide of Iron (Ferrum argillaceum)
Crystallized Carbonate of Barytes (Barytes carbonata)
Stalactitical Oxide of Iron (Ferrum oxygenizatum, var. stalactiticum)
Hydrargillite (Argilla hydrata)
Inverse crystallized Carbonate of Lime (Calx carbonata, var. inversa)
Filamentose Oxide of Copper (Cuprum oxygenizatum)
Crystallized Oxide of Zinc (Zincum oxygenizatum)
Quartz-Jasper (Silex Quartzum, var. Jaspis)
Oxide of Manganese (Manganesium oxygenizatum)
Arseniate of Copper (Cuprum arseniatum)
Talc (Silex Talcum)
Prehnite (Silex Prehnites)
Ferriferous Carbonate of Lime (Calx carbonata, var. ferrifera)
Quartz Septarium (Silex Quartzum)
Feldspar and Petuntse (Silex Petuntse)
Red Jasper (Silex Quartzum, var. Jaspis)
Red and Green Serpentine (Silex steatites, var. induratum)
Indurated Steatite (Silex steatites, var. indurata)
Kaolin (Silex Petuntse)
Quartz, or Agate (Silex Quartzum)
Macle or Chiastolite
Sulphuret of Lead, or Galaena (Plumbum sulphureum)
Peroxide or rather Hydrate of Copper (Cuprum hyperoxygenizatum)
Water, Ice or Hail (Oxygen Aqua)
Hard Carbonate of Lime (Calx carbonata dura)
Coralliform Limestone (Calx carbonata coralliformis)
Sulphate of Barytes (Barytes sulphata)
Sulphate of Barytes (Barytes sulphata)
Crystallized Quartz (Silex Quartzum)
Peroxide or Hydrate of Copper (Cuprum hyperoxgenizatum)
Stellated or radiated Sulphate of Strontian (Strontia sulphata)
Brush-like Sulphate of Strontian (Strontia sulphata)
Cotham Marble — “The fanciful figure to themselves in this something like a boat and men in one part, and hedge-rows in another, with trees in full foliage.”
Calcareous Schist (Calx carbonata)
Siliceous Schistus, Hone-Stone, or Novaculite
Plant-formed Coal (Carbo bituminosus)
Striped Flints (Silex quartzum)
Fire-Stone
Fluor (Calx fluata)
Blistered Sulphuret of Copper (Cuprum sulphureum)
Siliceo-calcareous Oxide of Titanium (Titanium oxygenizatum siliceocalcareum)
Amorphous Quartz or Flint (Silex quartzum)
Vitrified Sand tubes (Quatzum vitrificatum)
Calcedony or Agate (Silex Achates)
Red oxyde of Iron (Ferrum oxygenizatum)
Mar 3, 2022