mail_outline sales@mediastorehouse.com
Protaxocrinus tuberculatus (Miller)A fossil specimen of Protaxocrinus tuberculatus (Miller), a crinoid, dating back to the Silurian period (440 million years ago), discovered in the Wenlock Limestone bed, Dudley, Worcestershire, UK
Myedactylus flecheri (Salter)A fossil specimen of Myelodactylus fletcheri (Salter) dating back to the Silurian period (440 million years ago), discovered in Wenlock Limestone bed, Dudley, Worcestershire, UK
Common rock typesA collection of common rock types - left to right - Igneous (granite), sedimentary (sandstone) and metamorphic (schist)
Asteroxylon mackiei, clubmossA wax model reconstruction of the Early Devonian plant Asteroxylon mackiei, a clubmoss, approximately 10cm tall. Original specimen discovered at Rhynie Chert, Scotland
Piltdown flake implementPiltdown, Sussex item E.612 held at The Natural History Museum, London
Piltdown flintsCollection of Piltdown flints held at The Natural History Museum, London
Piltdown Eolithic flintPiltdown, Sussex item E.614 held at The Natural History Museum, London
Piltdown rolled flakePiltdown, Sussex item E.613 held at The Natural History Museum, London
Piltdown flint implementPiltdown, Sussex item E.605 held at The Natural History Museum, London
Piltdown Palaeolith flintPiltdown, Sussex item E.685 held at The Natural History Museum, London
Trigonocarpus parkinsoniLarge nutlike seeds (about 2.5cm long) from the coal measures of England dating from Upper Carboniferous. Specimen held at the Natural History Museum, London
Harry Morris Flint
Ripple-marked sandstoneTide formed, symmetrical, ripple marks shown here in this specimen of fossilised in sandstone
Foraminiferal limestoneNummulitic limestone made up of the hard parts of billions of foraminiferans
Homo neanderthalensis (calpicus) cranium (Gibraltar 1)Frontal view of an adult female Neanderthal cranium discovered at Forbes Quarry, Gibraltar. Its discovery was announced by Lieutenant Flint in 1848 and it is believed to be 50, 000 years old
Anorthosite breccia, moon rockSpecimen of anorthosite breccia or moon rock collected on the Apollo 16 mission in April 1972, and mounted in an acrylic block for protection and display
Raper drawing No. 5View of SW coast of the Isle of Wight, 1. St Catherines Point; 2. the Needle Point. Painting by George Raper, 1789
CharcoalSpecimen of commercial charcoal produced from wood. Charcoal is created by burning organic substances such as wood in the absence of oxygen
TilliteThis Tillite specimen is from Kimberley, South Africa. Tillites are the consolidated remains of the rock fragments and powder that are left behind as a glacier melts and retreats
Septarian nodule
Coccoliths magnified a thousand timesAn illustration of Coccoliths magnified a thousand times. Coccoliths are micro-fossils and feature heavily in the composition of chalk
Neanderthal artifactsStone tools believed to once have belonged to Neanderthal Man (Homo neanderthalensis) who lived in Gorhams Cave, Gibraltar
Dinosaur eggFound at the Kallankurichi Limestone Mine, India. Was V26861
Lower Chalk
6 million year old fossiliferous sandstones
Actinopora disticha, bryozoanScanning electron micrograph of a fossil cyclostome bryozoan from the Cretaceous Chalk, Santonian, Kent
Coal
Ripple marksThis sedimentary rock displays fossilised ripple marks which are evidence of flowing waters
Banded iron formation3, 000 million year old specimen of banded iron-rich chert from the Murchison Goldfield, Western Australia. The banding derives from differing amounts and oxidation state of the iron composite
Sedimentary layer of rock shows the effects of drought. A layer of dried-out mud was overlain with darker sediment which filled the cracks - the whole was then compacted and changed to rock
Puddingstone is a conglomerate or mixture of different, irregular sized grains and pebbles held together by a finer matrix
ShaleCompacted platy clay particles give shales their typical laminated structure. Shale is a sedimentry rock which is composed of many fine-grained clay particles
Sandstone is formed by loose grains of quartz compacted and cemented together
Flint hand-axeLate Palaeolithic from Farnham, Surrey, England
Flint noduleThis flint nodule originates from the Cretaceous rocks of the North Downs, England
Dalmanites myops, trilobiteA Silurian fossil trilobite from the Wenlock Limestone, Dudley, Worcestershire. This specimen measures 40mm head to tail
Hones for sharpening metal edgesThe longest hone here dates back to the 12th century and was discovered in Winchester however the rock type matches specimens of schist from quarries in Eidsborg in Norway
Rhynchosaurus footprintsFossil footprints made by Rhynchosaurus on a slab of Triassic, Keuper Sandstone from a quarry in Rathbone Street, Liverpool. Dimensions of slab are 5 inches x 6 inches
Lonsdaleia, coralShown here is the Carboniferous coral, Lonsdaleia. Corals comprise a soft bodied animal called a polyp. Each polyp inhabits a calcareous skeleton called a corallum
SlateCambrian slate from North Wales. Slate is metamorphosed shale
Hyolithes, primitive molluscShown here is Hyolithes, a Cambrian primitive mollusc. Hyolithes had an oval or cone-shaped, elongated shell and often occured in clusters along bedding planes of Cambrian shale
SandstonesA collection if sandstones showing colour variations. Clockwise from the left: green Ightham Stone, brown St Bees, beige L Coal Measures from Derbyshire and striped from Stirling
Quartzite
Rhynia major, fossilised plantA complete soft tissue preservation at the cellular level in Rhynia major. Transverse section through stem, approximately 2mm in diameter. From Rhynie Chert, Scotland, Early Devonian
Coal, from the late carboniferousCoal is formed from fossil plants. The regular pattern on the surface of this 14 cm long piece is the impression of the bark of a fossil tree; Lepidodendron
Turquoise vein in shaleTurquoise (hydrated copper aluminum phosphate) vein in shale, from Victoria, Australia. Turquoise is perhaps the most valuable non-transparent mineral