{"product_id":"28g-smithsonite-specimen-from-b14-broken-hill-australia","title":"28g Smithsonite Specimen from B14, Broken Hill, Australia","description":"\u003cp class=\"p1\"\u003e\u003cspan class=\"s1\"\u003e*** All information about the metaphysical properties of the listings on this site is for reference only and is to be understood in this context. It is based on research of opinions and beliefs from different cultures today and throughout history and my own personal beliefs.The information is not to be taken as a replacement for a medical examination, diagnosis, or treatment. For medical advice, please consult a healthcare professional. ***\u003c\/span\u003e\u003c\/p\u003e\n\u003cp class=\"p1\"\u003e\u003cspan class=\"s1\"\u003e\u003cbr\u003ePlease message me prior to completion of your order for details on how to save on shipping costs by purchasing multiple items from my store.\u003c\/span\u003e\u003c\/p\u003e\n\u003cp class=\"p1\"\u003e\u003cspan class=\"s1\"\u003eThis specimen weighs 28g and measures 3.5cm x 3cm x 2cm.\u003c\/span\u003e\u003c\/p\u003e\n\u003cp class=\"p1\"\u003e\u003cspan class=\"s1\"\u003eThis Smithsonite specimen was sourced in the 1980’s from block 14, open cut, South Mine, Broken Hill New South Wales, Australia. The South Mine was established as The Broken Hill South Silver Mining Co Ltd in 1885 and covers the central area of the Broken Hill line of lode, approximately 4 km in length, with the boundaries defined by two roads that connect the main part of the city of Broken Hill with the south district. The South Mine took over the original leases held by BHP when they left in the 1940s and was officially closed in 1972.\u003c\/span\u003e\u003c\/p\u003e\n\u003cp class=\"p1\"\u003e\u003cspan class=\"s1\"\u003e\u003cmeta charset=\"UTF-8\"\u003e\n\u003cspan class=\"rQesXe MPyX\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003e\u003cspan data-subtree=\"aimfl,mfl\"\u003eSmithsonite specimens from the Block 14 Opencut\u003c\/span\u003e\u003c\/span\u003e\u003cspan\u003e (often abbreviated as B14) in Broken Hill, New South Wales, Australia, are famous among mineral collectors for showcasing an incredible diversity of crystal habits.\u003c\/span\u003e\u003cspan\u003e While smithsonite globally is most recognized for its bubbly, globular, or \"botryoidal\" masses, the unique geochemical environment of the Broken Hill oxidized zone allowed it to crystallize into several distinct shapes.\u003c\/span\u003e\u003c\/span\u003e\u003c\/p\u003e\n\u003cdiv class=\"n6owBd awi2gc\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-hveid=\"CAIIAAgACA8QAA\" data-complete=\"true\"\u003eThe most prominent habits found at the \u003cspan class=\"iNqyIf\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003eBlock 14 Opencut\u003c\/span\u003e include:\u003cspan\u003e\u003c\/span\u003e\n\u003c\/div\u003e\n\u003cdiv class=\"n6owBd awi2gc\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-hveid=\"CAIIAAgACA8QAA\" data-complete=\"true\"\u003e\u003c\/div\u003e\n\u003cdiv data-bfc=\"\" class=\"\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-ved=\"2ahUKEwiuhabIqaaXAxUte_UHHWn4Ij8Qi4wTegoIAggACAAIEBAB\" data-hveid=\"CAIIAAgACBAQAQ\" data-complete=\"true\"\u003e\u003cspan class=\"iNqyIf\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003e\u003cstrong class=\"rQesXe MPyX\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003eRice-grain habits:\u003c\/strong\u003e Tiny, elongated, and pointed rhombohedral crystals that resemble individual grains of rice clustered together.\u003c\/span\u003e\u003c\/div\u003e\n\u003cdiv data-bfc=\"\" class=\"\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-ved=\"2ahUKEwiuhabIqaaXAxUte_UHHWn4Ij8Qi4wTegoIAggACAAIEBAB\" data-hveid=\"CAIIAAgACBAQAQ\" data-complete=\"true\"\u003e\u003cspan class=\"iNqyIf\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003e\u003c\/span\u003e\u003c\/div\u003e\n\u003cdiv data-bfc=\"\" class=\"\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-ved=\"2ahUKEwiuhabIqaaXAxUte_UHHWn4Ij8Qi4wTegoIAggACAAIEBAD\" data-hveid=\"CAIIAAgACBAQAw\" data-complete=\"true\"\u003e\u003cspan class=\"iNqyIf\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003e\u003cstrong class=\"rQesXe MPyX\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003eBulbous and rounded habits:\u003c\/strong\u003e Smooth, translucent, droplet-like or \"lightbulb\" shaped crystals that often cluster on top of dark matrices.\u003c\/span\u003e\u003c\/div\u003e\n\u003cdiv data-bfc=\"\" class=\"\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-ved=\"2ahUKEwiuhabIqaaXAxUte_UHHWn4Ij8Qi4wTegoIAggACAAIEBAD\" data-hveid=\"CAIIAAgACBAQAw\" data-complete=\"true\"\u003e\u003cspan class=\"iNqyIf\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003e\u003c\/span\u003e\u003c\/div\u003e\n\u003cdiv data-bfc=\"\" class=\"\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-ved=\"2ahUKEwiuhabIqaaXAxUte_UHHWn4Ij8Qi4wTegoIAggACAAIEBAF\" data-hveid=\"CAIIAAgACBAQBQ\" data-complete=\"true\"\u003e\u003cspan class=\"iNqyIf\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003e\u003cstrong class=\"rQesXe MPyX\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003eDog-tooth scalenohedrons:\u003c\/strong\u003e Sharp, elongated crystals that mimic the classic \"dog-tooth\" calcite habit.\u003c\/span\u003e\u003c\/div\u003e\n\u003cdiv data-bfc=\"\" class=\"\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-ved=\"2ahUKEwiuhabIqaaXAxUte_UHHWn4Ij8Qi4wTegoIAggACAAIEBAF\" data-hveid=\"CAIIAAgACBAQBQ\" data-complete=\"true\"\u003e\u003cspan class=\"iNqyIf\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003e\u003c\/span\u003e\u003c\/div\u003e\n\u003cdiv data-bfc=\"\" class=\"\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-ved=\"2ahUKEwiuhabIqaaXAxUte_UHHWn4Ij8Qi4wTegoIAggACAAIEBAH\" data-hveid=\"CAIIAAgACBAQBw\" data-complete=\"true\"\u003e\u003cspan class=\"iNqyIf\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003e\u003cstrong class=\"rQesXe MPyX\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003eCurved rhombohedrons:\u003c\/strong\u003e Saddle-shaped or slightly warped rhombohedral crystals with a high pearly lustre.\u003c\/span\u003e\u003c\/div\u003e\n\u003cdiv data-bfc=\"\" class=\"\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-ved=\"2ahUKEwiuhabIqaaXAxUte_UHHWn4Ij8Qi4wTegoIAggACAAIEBAH\" data-hveid=\"CAIIAAgACBAQBw\" data-complete=\"true\"\u003e\u003cspan class=\"iNqyIf\" data-sfc-cp=\"\" data-sfc-root=\"ep\" data-epip=\"\" data-complete=\"true\"\u003e\u003c\/span\u003e\u003c\/div\u003e\n\u003cp class=\"p1\"\u003e\u003cspan class=\"s1\"\u003e\u003cspan\u003e\u003cmeta charset=\"UTF-8\"\u003eThese variations typically occur as colorless, white, or pale gray crystals, frequently resting in stark contrast against a dark, contrasting manganese oxide matrix. \u003c\/span\u003e\u003c\/span\u003e\u003c\/p\u003e\n\u003cp class=\"p2\"\u003e \u003c\/p\u003e\n\u003cp class=\"p1\"\u003e\u003cspan class=\"s1\"\u003eSmithsonite:-\u003c\/span\u003e\u003c\/p\u003e\n\u003cp class=\"p2\"\u003e\u003cspan style=\"font-size: 0.875rem;\"\u003eSmithsonite, also sometimes referred to as “Zinc Spar”, is a secondary mineral found in the rocks above and around many important zinc deposits. These smithsonite occurrences are often seen at the surface or at shallow depths. As a result, smithsonite was one of the earliest zinc minerals to be discovered and mined by pioneer metallurgists. Finding smithsonite at the surface has led to the discovery of a major zinc deposit below.\u003c\/span\u003e\u003cbr\u003e\u003cspan class=\"s1\"\u003e\u003c\/span\u003e\u003c\/p\u003e\n\u003cp class=\"p1\"\u003e\u003cspan class=\"s1\"\u003eSmithsonite is almost never found as nice crystals. Botryoidal coatings on rocks and fractures are a common mode of occurrence. Smithsonite can be found in a variety of colors such as yellow, brown, purple, white, green, grey, and most notably, its turquoise-blue shade. This mineral was commonly mistaken for Hemimorphite or Calamine, until 1832 when F.S. Beaudant differentiated it. He named the mineral after the English mineralogist James Smithson, who first identified the crystal in 1802. This is the same James Smithson who was the founding donor of the Smithsonian Institution.\u003c\/span\u003e\u003c\/p\u003e","brand":"NaturesgiftsByChris","offers":[{"title":"Default Title","offer_id":50231753474325,"sku":null,"price":12.99,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0870\/2453\/3781\/files\/IMG_9595_81c24f3b-af0c-4340-a705-4a009c2319ca.jpg?v=1791322145","url":"https:\/\/naturesgiftsbychris.com\/products\/28g-smithsonite-specimen-from-b14-broken-hill-australia","provider":"NaturesgiftsByChris","version":"1.0","type":"link"}