{"title":"Septaria","description":"\u003cp\u003eSeptaria, better known to collectors as septarian nodules or septarian concretions, are not a single mineral species but calcium-rich sedimentary concretions that grew around a core of decaying marine organic matter, most often shells. Their formation required water, bentonite mud, and calcium-rich organic matter, such as shells. As the surrounding mud dried and shrank, each nodule cracked into a network of angular voids, and the term \"Septarian\" is derived from the Latin word \"septum,\" meaning partition or boundary, referring to these divisions. Groundwater later carried dissolved minerals into the cracks, and most septarian nodules contain siderite, aragonite and calcite, along with barite crystals, pyrite, and marcasite, producing the honeycomb of golden veins that make polished septaria so distinctive on the collector market.\u003c\/p\u003e\u003cp\u003eThe two classic sources dominate the trade. In Utah, septarian nodules are mined from the Late Cretaceous, roughly 90-100 million years old, Frontier Formation near Orderville in Kane County, with additional material from Muddy Creek and the \u003cstrong\u003eBear Lake\u003c\/strong\u003e district; Utah septarian is known for its distinctive and sometimes fairly large honey-yellow calcite crystals, and is often brightly fluorescent and phosphorescent under UV light. In \u003cstrong\u003eMadagascar\u003c\/strong\u003e, large quantities of septarian are mined near Tsaramandroso on the northern end of the island, of Middle to Late Jurassic age around 160 million years old, tending to display smaller crystals and much darker black or brown colors than the septarian from Utah, with further deposits near \u003cstrong\u003eMahajanga\u003c\/strong\u003e. Both localities yield the paired \u003cstrong\u003ecalcite\u003c\/strong\u003e and \u003cstrong\u003earagonite\u003c\/strong\u003e infill that defines top-grade specimens, occasionally accompanied by \u003cstrong\u003ebarite\u003c\/strong\u003e, \u003cstrong\u003ecelestite\u003c\/strong\u003e or \u003cstrong\u003egypsum\u003c\/strong\u003e in hollow cavities.\u003c\/p\u003e\u003cp\u003eBeyond these two giants, fine septaria are recovered from the Kimmeridge Clay Formation in England along the Jurassic Coast, from \u003cstrong\u003eMorocco\u003c\/strong\u003e, from the \u003cstrong\u003eBearpaw Shale\u003c\/strong\u003e of Alberta and the \u003cstrong\u003eRed River Formation\u003c\/strong\u003e of Manitoba in Canada, and from the Waipara River area in Canterbury, New Zealand. Because of their scaly, cracked surface pattern, septarian nodules are sometimes marketed as \"Dragon Stones,\" a name that dates back to a Malagasy legend that dragons once roamed the area. Collectors prize septaria for the rare combination of sedimentary origin and true crystallized mineral infill: each cut and polished nodule reveals a unique, one-of-a-kind pattern of \u003cstrong\u003ecalcite\u003c\/strong\u003e and \u003cstrong\u003earagonite\u003c\/strong\u003e crystallization, making Septaria a favorite crossover piece for both mineral cabinets and lapidary display.\u003c\/p\u003e","products":[],"url":"https:\/\/www.italmineral.com\/collections\/septaria.oembed","provider":"ITALMINERAL","version":"1.0","type":"link"}