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KaoliniteScanning electron microscope image of kaolinite (x 4.00K). Its a common phyllosilicate mineral, its structure is composed of silicate sheets bonded to aluminum oxide/hydroxide layers
Smokejacks Brickworks, SurreySmokejacks Brickworks in Ockley, Surrey shows part of the Upper Weald Clay Formation of Lower Cretaceous (Barremian) age
Eocene London clayEli Marsden Wilsons impression of the Eocene (55 to 34 million years ago) London Clay landscape
The Nummulosphere Part I. Front CoverAn account of the organic origin of so-called igneous rocks and of abyssal red clays by Kirkpatrick, Randolph (1863-1950), London. 1913
Mica schist is a rock resulting from the metamorphism of shale. Specimen originates from Grantown-on-Spey, Murrayshire
Hornblende-biotite graniteGeological specimen collected by Scotts British Antarctic Expedition 1910-1913, also known as the Terra Nova expedition. It had a broad scientific programme and collected thousands of geological
Pyrophyllite, green radiating in quartz from Berezovsk, Russia. Close-up of specimen on display in the Mineral Gallery at the Natural History Museum, London
Shale (right) and garnet-mica-schist (left)Shale is sedimentary and garnet-mica-schist is metamorphoc in origin. Specimen held at the Natural History Museum, London
BentoniteA specimen of the mineral Bentonite Reg No. 1926, 216 light grey mass, Range 19, W4, Township 28, Rosedale, Alberta, Canada. Predented by the Canadian Government Exhibition Commision, 1926
Serpentine cupA mottled serpentine ornamental cup or tazza on a black marble base. The mineral serpentine is composed of (magnesium iron silicate hydroxide)
Belemnotheutis antiquusA well-preserved Upper Jurassic squid aged 160 million years. This specimen originates from the famous clay deposits in Wiltshire
Cordierite-biotite-gneissGeological specimen collected by Scotts British Antarctic Expedition 1910-1913, also known as the Terra Nova expedition. It had a broad scientific programme and collected thousands of geological
Antigorite and boweniteGroup of two specimens of antigorite (above) and two specimens of antigorite var. bowenite below. Both these specimens comprise of (magnesium iron silicate hydroxide)
Limacina mercinensis, holoplanktonic molluscFossilised specimens of Holoplaktonic molluscs found in early Eocene, London Clay at Highgate, London. 58 million years old
Chlorite variant clinochloreBooks of clinochlore with hessonite garnet from Piedmont, Italy. Clinochlore (Magnesium Iron Aluminum Silicate Hydroxide) is a common member of the Chlorite group of minerals
Talc
Dancing woman in green serpentine
Insect collection by James Petiver (1663-1)This late 17th century insect collection is unique in that the specimens are mounted and preserved between sheets of the mineral mica
Fossil collecting near Aveley, EssexPalaeontologists collecting the remains of a woolly mammoth and a straight-tusked elephant from a clay pit near Aveley, Essex in 1964
Plate 4a from Histoire naturelle? (1789)Plate 4a Mineralogie, [unfinished] from Histoire naturelle: ou, Exposition des morceaux, les mieux choisis pour servir? (1789) by by Swebach Desfontaines
Lepidolite
Fuchsite specimen
Observing structure of rockLooking at fresh granite under a microscope to study structure, granular composition can clearly be seen
Clay Toy Turtles and spidersWatercolour by Olivia Fanny Tonge (1858-1949). Captioned: Clay Toy Turtles with Heads and Legs that waggle costing one anna. Cawnpore
ShaleCompacted platy clay particles give shales their typical laminated structure. Shale is a sedimentry rock which is composed of many fine-grained clay particles
MuscoviteA specimen of muscovite (Potassium aluminum silicate hydroxide fluoride) with hematite and limonite inclusions, from Adelaide Australia