Curious Minds

Fancy Jasper Tumblestone Collectable Gemstone (SINGLE UNIT)

Best price from 1 retailer
£1.95
Brand
Curious Minds
Category
Rocks & Fossils
GTIN / Barcode
5060285967318
MPN
C021961
Jasper is an opaque, impure variety of silica, primarily composed of microgranular quartz and/or cryptocrystalline chalcedony. With a density typically ranging from 2.5 to 2.9 g/cm³. It is classified as a sedimentary or, in some cases, volcanic rock, containing 80–95% silica, often with minor amounts of clay or other mineral inclusions. Its composition includes radiolarians cemented in a chalcedony matrix, resulting in a fine-grained, durable structure with a smooth surface when polished. Jasper exhibits a wide range of colours—commonly red, yellow, brown, green, and rarely blue—due to impurities such as iron(III) oxides, which produce the characteristic red hues, or other minerals like epidote for green varieties. Its fracture is typically conchoidal to splintery, and its appearance can be mottled, banded, or spotted, with patterns like orbicular (e.g., leopard skin jasper) or brecciated (fragmented and cemented) forms arising from depositional, hydrothermal, or tectonic processes. Tumble stones are rock specimens that have been mechanically polished in a rock tumbler, a process that rounds and smooths the rough edges, enhancing their aesthetic appeal and revealing internal patterns or colours. The tumbling process involves abrading the stones with progressively finer grits, resulting in a glossy, tactile surface ideal for display or jewellery. Varieties like picture jasper, with scene-like patterns, or orbicular jasper, with distinctive circular markings, are particularly prized after tumbling. Geological Significance Geologists are interested in jasper due to its formation processes and what they reveal about Earths history. Jasper typically forms in sedimentary environments through the precipitation of silica-rich fluids, often associated with volcanic ash or organic-rich sediments, or via hydrothermal circulation where mineral-rich fluids infiltrate fractures. For example, jaspillite, a banded-iron-formation rock, provides evidence of ancient oceanic che

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