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Specimens of Accretionary Lapilli Tuff collected from Longsleddle in Cumbria, UK. This igneous pyroclastic rock forms when material from volcanic activity ejects into the air. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Aeolian Sandstone collected from Lazonby, near Penrith, Cumbria in the UK. This aeolian sandstone is Triassic in age – approximately 200 Ma. It belongs to the group of rocks known as the New Red Sandstone which date from the Permian (280 Ma) into the Triassic. The composition of this sandstone consists solely of spheroidal (millet seed) quartz grains with an iron oxide cement called haematite. It is the presence of this haematite that contributes to the distinct red – orange colouration of these samples. This lithology is typical of an aeolian (wind blown) hot desert environment. Available in multiple sizes, these specimens come supplied in a white card tray with information label.
We also supply Aeolian Sandstone thin sections for microscope study which are available to buy HERE.
Specimens of Agglomerate collected in Scotland, UK. This volcanic rock has a coarse texture and is fairly hard. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Amygdaloidal Basalt collected from Northern Ireland. This variety of extrusive igneous rock dates from the Tertiary period with it being dark from a low quartz content. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Andesite, collected from Cumbria, UK. Andesite is a fine grain, extrusive igneous rock with a dark grey colouration. These rocks date to the late Ordovician. Specimens are available in multiple sizes and come in white card tray with an information label.
We also supply Andesite thin sections for microscope study which are available to buy HERE.
Specimens of Anorthosite, collected from the Rogaland Province in Norway. Anorthosite is an intrusive igneous that consists predominantly of calcium rich plagioclase feldspar. These specimens date to the Proterozoic age – the most recent part of the Precambrian. Most Anorthosite tends to be coarse in grain size, however some specimens collected from the moon are finely crystalline in nature. Specimens are available in multiple sizes and come in a white card tray with an information label.
We also supply Anorthosite thin sections for microscope study which are available to buy HERE.
Ashford Black Marble samples originate from Ashford-in-the-Water, Derbyshire, UK. Despite its name, this rock surprises many by being classified as a fine-grained Sedimentary Rock instead of a Metamorphic one. This classification is due to its true nature as a dark limestone rather than a genuine marble. Ashford Black Marble earns its reputation for ornamental purposes, showcasing a stunningly shiny black surface when cutting and polishing it. The rock’s origin dates back to the Carboniferous period, and it boasts a generous amount of bitumen, giving rise to its dark grey hue that transforms into a mesmerising glossy black appearance upon polishing. Supplied in various sizes, each specimen comes presented in a white card tray with an accompanying informative label.
Specimens of Augen Gneiss collected from Ross-shire, near Garve, Scotland. This gneiss contains characteristic elliptic feldspar porphyroclasts within the layering of the rock. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Augite Andesite, collected from Thirlmere, Cumbria in the UK. Augite Andesite is a variation of the fine grained igneous rock, Andesite, but containing coarse phenocrysts of augite crystals. This gives the Augite Andesite a speckled appearance. These rocks date to the Ordovician period and are available in multiple sizes. They come in a white card tray with an information label.
We also supply Augite Andesite thin sections for microscope study which are available to buy HERE.
Specimens of Augite Granophyre, collected from Carrock Fell, Cumbria in the UK. Augite Granophyre is a fine to medium grain igneous rock, that typically forms in sub volcanic to intrusive igneous bodies. These specimens mostly consist of quartz and feldspar, but also contain small but visible augite crystals which are dark green to black in colour. These specimens are available in multiple sizes and come in a white card tray with an information label.
Specimens of Banded Tuff, collected from Cumbria in the UK. Tuff is an igenous rock, formed when volcanic ash that is ejected from a vent during an eruption, is deposited and lithified into a solid rock. Tuff is often banded, as larger particles of fall first, with finer particles deposited on top as they fall later. These pieces are in limited stock and pink-brown in colour. Varying levels of banding shown in each piece. Available in three different sizes and come in a white card tray with an information label.
Specimens of Basalt, collected from Northern Ireland. Basalt is a common, extrusive igneous rock, that forms when magma erupts and cools quickly on the Earth’s surface. These specimens are part of the Antrim lava group and date to the Tertiary period, around 60 million years ago. These specimens are available in multiple sizes and come in a white card tray with an information label.
We also supply Basalt thin sections for microscope study which are available to buy HERE.
Specimens of Bauxite collected from Northern Ireland. This red sedimentary rock forms at or near to the Earth’s surface. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Biotite Gneiss collected from Evje in Norway. High contents of both white minerals and black biotite mica result in a black and white banding appearance. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Biotite Gneiss, collected from Blairgowrie, Perthshire in Scotland. This gneiss exhibits a black and white banded appearance. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Biotite Granite, collected from Ballachulish, Scotland. Biotite Granite – like all granites – is a coarse grained, intrusive igenous rock. As the name suggests however, this variety contains much greater quantities of biotite mica. This contrasts with the white colouration of the quartz and plagioclase feldspar to give a striking appearance. These specimens are available in multiple sizes and come in a white card tray with an information label.
Specimens of Biotite Granite collected from Spain. This igneous rock consists of quartz, plagioclase feldspar and biotite mica. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Biotite Muscovite Granite collected from St. Austell in Cornwall, UK. This granite is part of the Cornubian batholith and dates to the Permian period around 280 million years ago. Specimens are available in multiple sizes and comes in a white card tray with an information label.
We also supply Biotite Muscovite Granite thin sections for microscope study which are available to buy HERE.
Specimens of Boulder Clay collected from Yorkshire in the UK. This clay dates to the Pleistocene period and forms due to glacier and ice sheet activity. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Breccia, collected from the Manifold Valley in Staffordshire. Breccia is a term that describes coarse grained sedimentary rocks, with large angular clasts, surrounded by a finer grained matrix. Calcrete binds the clasts in these specimens, forming on calcareous materials in response to climatic fluctuations in arid and semi-arid regions. These specimens are available in multiple sizes and come supplied in a white card tray with information label.
Specimens of Breccia, collected from Yorkshire. Breccia is a term that describes coarse grained sedimentary rocks, with large angular clasts, surrounded by a finer grained matrix. These specimens date to the Holocene period, approximately within the last 11ooo years. These specimens are available in multiple sizes and come supplied in a white card tray with information label.
Brockram Breccia specimens sourced from Hoff, Cumbria, UK. Breccia, a type of clastic sedimentary rock, is characterized by its coarse-grained and poorly sorted nature, containing large angular fragments embedded in a finer-grained matrix.
Brockram is a basal breccia, composed of cemented limestone and sandstone fragments originating from the Permian period. The Permian was the last period of the Paleozoic era and occurred approximately 299 – 251 million years ago.
These samples are available in various sizes and are presented in a white card tray along with accompanying information label.
Specimens of Bunter Sandstone, collected from Knutsford, Cheshire in the UK. This sandstone dates to the lower Triassic, around 252 – 246 Mya. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Bytownite Basalt collected from Cumbria in the UK. This dark, igneous rock is a calcium-rich variation of the common basalt rock. Specimens are available in multiple sizes and comes in a white card tray with an information label.
We also supply Bytownite Basalt thin sections for microscope study which are available to buy HERE.
Specimens of Cannel Coal collected from the Alexander open cast pit, Wigan in Lancashire. This coal dates to the Carboniferous age. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Cannonball Limestone, collected from around the Hartlepool area, in the UK. This is a very distinctive and rare form of limestone known as Cannonball rock. It is part of the Rocker formation; a basin slope deposit which comprises part of the Zechstein Group. This is a highly studied sedimentary formation which dates to the Mid to Late Permian Period. These specimens are available in multiple sizes and come with an information label.
Specimens of Carstone collected from Westcott, Surrey in the UK. This variation of sandstone is Cretaceous in age, dating them between 66 and 145 million years old. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Chalk, collected from Yorkshire, in the UK. Chalk is a soft, white, porous sedimentary carbonate rock and form of limestone. It forms in reasonably deep marine conditions, by the gradual accumulation of minute calcite plates, known as coccoliths, which shed from micro-organisms called coccolithophores. Additionally, it is not uncommon to find flint or chert nodules embedded in chalk. These specimens are Cretaceous in age, available in multiple sizes, and supplied in a white card tray with information label.
We also supply Chalk thin sections for microscope study which are available to buy HERE.
Specimens of Red Chalk collected in the Reighton Gap, North Yorkshire in the UK. This chalk dates to the Albian stage of the early Cretaceous period. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of chert found in Foss mine, Scotland, UK. Specimens are supplied in a white card tray with an information label.
Specimens of Chiastolite Slate collected from Cumbria in the UK. This slate is quite soft and friable unlike classic slate. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Chlorite Schist, collected from Auchtertyre, Ross-shire in Scotland, UK. Chlorite Schist is a foliated metamorphic rock, with a pale green colour. This is due to high quantities of a chlorite. Specimens are available in multiple sizes and come in a white card tray with an information label.
Specimens of Anthracite collected from the coalfields in South Wales. This coal has the highest carbon content out of all the coal types. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Bituminous Coal, collected from the Carboniferous deposits in Yorkshire. Bituminous Coal is an organic sedimentary rock, that forms by diagenetic and sub metamorphic compression of peat bog & swamp material. Its primary constituents are macerals: vitrinite, and liptinite. The carbon content of bituminous coal is around 60-80%. The rest consists of residual water, air, hydrogen, and sulphur. These specimens are available in multiple sizes and come in a white card tray with an information label.
We also supply Bituminous Coal thin sections for microscope study which are available to buy HERE.
Specimens of Conglomerate, collected from Farringdon, Berkshire in the UK. This sedimentary rock features large, well rounded clasts and deposits in a high energy environment, either fluvial, alluvial or shallow marine. Specimens are available in multiple sizes and comes in a white card tray with an information label.
We also supply Conglomerate thin sections for microscope study which are available to buy HERE.
Specimens of fossiliferous conglomerate, collected from Farringdon, Berkshire. The term conglomerate describes a coarse grained, clastic sedimentary rock composed of a substantial proportion of rounded grains. These conglomerate specimens, despite also being from Farringdon, differ from our other clonglomerate (which you can find HERE) due to the prescence of various fossiliferous remains. These different fossil fragments include bryozoa, brachiopods and bivalves. These specimens are cretaceous in age, available in three sizes, and supplied in a white card tray with information label.
Specimens of Connemara Marble collected from Streamstown Quarry in County Galway, Ireland. This rare, green marble dates back to the end of the Pre-Cambrian period, around 700 million years ago. Specimens are available in multiple sizes and comes in a white card tray with an information label.
Specimens of Coral Limestone, collected from Anglesey. Limestone is a common, well known sedimentary rock. It consists of the calcium-rich shells, bones, and skeletons of the fauna that dominated during that period. These specimens date to the Palaeozoic era around 300 million years ago. They were laid down in shallow tropical seas around 300 million years ago, in the Carboniferous. The composition of these specimens is primarily Lithostrotion corals. They are available in multiple sizes and come supplied in a white card tray with an information label.
We also supply Coral Limestone thin sections for microscope study which are available to buy HERE.
Specimens of Cordierite Hornfels collected near Carrock Fell in Cumbria, UK. These hornfels include small cordierite crystals within the significant banding of the rock. Specimens are available in multiple sizes and comes in a white card tray with an information label.
We also supply Cordierite Hornfels thin sections for microscope study which are available to buy HERE.
Specimens of Sandstone, collected from Philpots Quarry, West Sussex, in the UK. This sandstone is from the Wealden Group (Hastings sub-group), which dates it to the Lower Cretaceous. This makes these rocks approximately 110 million years old. This Cretaceous sandstone is yellow to buff in coloured, and particularly fine grained. It exhibits large scale cross bedding, which is indicative of fast flowing tidal currents. It is quite soft , friable and flaggy in places and so is extracted mainly for concreting and building sand. These specimens are available in multiple sizes and come supplied in a white card tray with information label.
We also supply Cretaceous Sandstone thin sections for microscope study which are available to buy HERE.