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Tufa rock specimens which are calcium carbonate rich, sponge-like rock with fossil remains. Believed to be from the Quaternary period, particularly, the Flandrian epoch the specimens come from Caerwys, North Wales. Available in various sizes and supplied in a card tray with labels.
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Tufa is a variety of limestone, formed by the precipitation of carbonate minerals from ambient temperature water bodies. This rock specimen is from the Quaternary period, particularly, the Flandrian epoch and comes from Caerwys, North Wales. It forms in fluvial channels or lacustrine environments & subterranian passages (dripstone, stalagmites & stalactites). Geothermally heated hot springs sometimes produce similar (but less porous) carbonate deposits known as travertine. Tufa from this deposit contains organic build-ups (phytoherms) of living vegetation, such as reed and willow, although mosses and liverworts are the most common. All have been preserved as casts and moulds. These plants have been cemented and bonded during life by freshwater carbonate precipitation. This rock specimen is a classic tufa, light in weight, spongy, and containing many plant, preserved in the rock. Samples are available in optional sizes and come supplied card tray.
Weight | 120 g |
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Specimen Size | 2" x 2", 3" x 2", 4" x 3" |
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Travertine is a form of limestone which has been precipitated from carbonate rich hot springs. These examples are from Yorkshire, UK and are supplied in a labelled card tray.
39 in stock
Tufa thin section slide. Tufa is a variety of limestone, formed by the precipitation of carbonate minerals from ambient temperature water bodies. This particular material is from the Flandrian epoch of the Quaternary Period and it was collected in Caerwys, North Wales.
5 in stock
Devonian lower Old Red Desert Sandstone from Gloucestershire available in card trays with a label.
198 in stock
Oolitic limestone from the middle Jurassic of Gloucestershire. Traditional building stone throughout the Cotswolds. Available in a range of sizes.
300 in stock
Specimens of fault breccia found in Great Langdale, Cumbria, UK. These specimens are fault breccia meaning that unlike other breccia they were formed by tectonic forces. Specimens are supplied in a white card tray with a information label.
Out of stock
Dark grey Shale from the Jurassic of the Yorkshire coast. Originally deposited in a deep water marine environment. Occasionally fossiliferous.
199 in stock
Banded mudstone, know locally as the Moughton Whetstone from the Silurian deposits Crummackdale, West Yorkshire.
20 in stock
Carboniferous coral limestone from Anglesey, North Wales. Composed largely of well preserved Lithostrotion corals
50 in stock
Conglomerate with well rounded clasts from Faringdon, UK. A good example of the lithotype as opposed to a Breccia which would contain predominantly angular to sub-angular clasts.
200 in stock
A Triassic red millet seed sandstone of aeolian (wind blown) desert origin.
188 in stock
Salt Pseudomorphs on a limy marl matrix collected from the Triassic Aust Cliff in Avon. Numerous cubic imprints can be identified on the limy marl substrate of these specimens; they serve as interesting educational pieces.
20 in stock
Ribbon banded mudstone, Silurian in age, collected from the Denbigh grits in Wales, UK. Available in various sizes.
300 in stock
Lower Carboniferous crinoidal limestone from Derbyshire, U.K.
297 in stock
Rhaetic bone bed, Upper Triassic in age. Rich in marine fossils such as bones, scales & teeth from marine reptiles. From Aust Cliff, Gloucestershire.
40 in stock
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