Skip to main content

Sedimentary Collection (page 3)

Background imageSedimentary Collection: Protaxocrinus tuberculatus (Miller)

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

Background imageSedimentary Collection: Myedactylus flecheri (Salter)

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

Background imageSedimentary Collection: Common rock types

Common rock types
A collection of common rock types - left to right - Igneous (granite), sedimentary (sandstone) and metamorphic (schist)

Background imageSedimentary Collection: Asteroxylon mackiei, clubmoss

Asteroxylon mackiei, clubmoss
A wax model reconstruction of the Early Devonian plant Asteroxylon mackiei, a clubmoss, approximately 10cm tall. Original specimen discovered at Rhynie Chert, Scotland

Background imageSedimentary Collection: Piltdown flake implement

Piltdown flake implement
Piltdown, Sussex item E.612 held at The Natural History Museum, London

Background imageSedimentary Collection: Piltdown flints

Piltdown flints
Collection of Piltdown flints held at The Natural History Museum, London

Background imageSedimentary Collection: Piltdown Eolithic flint

Piltdown Eolithic flint
Piltdown, Sussex item E.614 held at The Natural History Museum, London

Background imageSedimentary Collection: Piltdown rolled flake

Piltdown rolled flake
Piltdown, Sussex item E.613 held at The Natural History Museum, London

Background imageSedimentary Collection: Piltdown flint implement

Piltdown flint implement
Piltdown, Sussex item E.605 held at The Natural History Museum, London

Background imageSedimentary Collection: Piltdown Palaeolith flint

Piltdown Palaeolith flint
Piltdown, Sussex item E.685 held at The Natural History Museum, London

Background imageSedimentary Collection: Trigonocarpus parkinsoni

Trigonocarpus parkinsoni
Large nutlike seeds (about 2.5cm long) from the coal measures of England dating from Upper Carboniferous. Specimen held at the Natural History Museum, London

Background imageSedimentary Collection: Harry Morris Flint

Harry Morris Flint

Background imageSedimentary Collection: Ripple-marked sandstone

Ripple-marked sandstone
Tide formed, symmetrical, ripple marks shown here in this specimen of fossilised in sandstone

Background imageSedimentary Collection: Foraminiferal limestone

Foraminiferal limestone
Nummulitic limestone made up of the hard parts of billions of foraminiferans

Background imageSedimentary Collection: Homo neanderthalensis (calpicus) cranium (Gibraltar 1)

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

Background imageSedimentary Collection: Anorthosite breccia, moon rock

Anorthosite breccia, moon rock
Specimen 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

Background imageSedimentary Collection: Raper drawing No. 5

Raper drawing No. 5
View of SW coast of the Isle of Wight, 1. St Catherines Point; 2. the Needle Point. Painting by George Raper, 1789

Background imageSedimentary Collection: Charcoal

Charcoal
Specimen of commercial charcoal produced from wood. Charcoal is created by burning organic substances such as wood in the absence of oxygen

Background imageSedimentary Collection: Tillite

Tillite
This 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

Background imageSedimentary Collection: Septarian nodule

Septarian nodule

Background imageSedimentary Collection: Coccoliths magnified a thousand times

Coccoliths magnified a thousand times
An illustration of Coccoliths magnified a thousand times. Coccoliths are micro-fossils and feature heavily in the composition of chalk

Background imageSedimentary Collection: Neanderthal artifacts

Neanderthal artifacts
Stone tools believed to once have belonged to Neanderthal Man (Homo neanderthalensis) who lived in Gorhams Cave, Gibraltar

Background imageSedimentary Collection: Dinosaur egg

Dinosaur egg
Found at the Kallankurichi Limestone Mine, India. Was V26861

Background imageSedimentary Collection: Lower Chalk

Lower Chalk

Background imageSedimentary Collection: 6 million year old fossiliferous sandstones

6 million year old fossiliferous sandstones

Background imageSedimentary Collection: Actinopora disticha, bryozoan

Actinopora disticha, bryozoan
Scanning electron micrograph of a fossil cyclostome bryozoan from the Cretaceous Chalk, Santonian, Kent

Background imageSedimentary Collection: Coal

Coal

Background imageSedimentary Collection: Ripple marks

Ripple marks
This sedimentary rock displays fossilised ripple marks which are evidence of flowing waters

Background imageSedimentary Collection: Banded iron formation

Banded iron formation
3, 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

Background imageSedimentary Collection: Sedimentary layer of rock

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

Background imageSedimentary Collection: Puddingstone

Puddingstone is a conglomerate or mixture of different, irregular sized grains and pebbles held together by a finer matrix

Background imageSedimentary Collection: Shale

Shale
Compacted platy clay particles give shales their typical laminated structure. Shale is a sedimentry rock which is composed of many fine-grained clay particles

Background imageSedimentary Collection: Sandstone

Sandstone is formed by loose grains of quartz compacted and cemented together

Background imageSedimentary Collection: Flint hand-axe

Flint hand-axe
Late Palaeolithic from Farnham, Surrey, England

Background imageSedimentary Collection: Flint nodule

Flint nodule
This flint nodule originates from the Cretaceous rocks of the North Downs, England

Background imageSedimentary Collection: Dalmanites myops, trilobite

Dalmanites myops, trilobite
A Silurian fossil trilobite from the Wenlock Limestone, Dudley, Worcestershire. This specimen measures 40mm head to tail

Background imageSedimentary Collection: Hones for sharpening metal edges

Hones for sharpening metal edges
The 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

Background imageSedimentary Collection: Rhynchosaurus footprints

Rhynchosaurus footprints
Fossil 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

Background imageSedimentary Collection: Lonsdaleia, coral

Lonsdaleia, coral
Shown here is the Carboniferous coral, Lonsdaleia. Corals comprise a soft bodied animal called a polyp. Each polyp inhabits a calcareous skeleton called a corallum

Background imageSedimentary Collection: Slate

Slate
Cambrian slate from North Wales. Slate is metamorphosed shale

Background imageSedimentary Collection: Hyolithes, primitive mollusc

Hyolithes, primitive mollusc
Shown 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

Background imageSedimentary Collection: Sandstones

Sandstones
A 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

Background imageSedimentary Collection: Quartzite

Quartzite

Background imageSedimentary Collection: Rhynia major, fossilised plant

Rhynia major, fossilised plant
A 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

Background imageSedimentary Collection: Coal, from the late carboniferous

Coal, from the late carboniferous
Coal 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

Background imageSedimentary Collection: Turquoise vein in shale

Turquoise vein in shale
Turquoise (hydrated copper aluminum phosphate) vein in shale, from Victoria, Australia. Turquoise is perhaps the most valuable non-transparent mineral



All Professionally Made to Order for Quick Shipping