{"product_id":"22g-analcime-with-natrolite-pink-seed-specimen","title":"22g Analcime with Natrolite (Pink Seed) Specimen","description":"\u003cp\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\/p\u003e\n\u003cp\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\/p\u003e\n\u003cp\u003eThis piece weighs 22g, measures 4cm x 2cm x 2cm and was collected in the 1970’s in the Flinders area, Victoria, Australia. Most of the Natroltie sprays on this piece has a lovely pink centre, or seed, possible caused by Hematite.\\\u003c\/p\u003e\n\u003cp\u003eThe section of coastline between Cape Schanck and the township of Flinders on the Mornington Peninsula has been the most productive zeolite collecting areas in Victoria. The initial description of minerals in the Flinders area was made back in 1854 by A.R.C. Selwyn, the first Government Mineral Surveyor of Victoria. His report refers to carbonate mineralisation along the Bass Straight coast precisely where the township of Flinders is situated today. The zeolites analcite, chabazite, gmelinite and Natrolite were first mentioned in reports in 1896.\u003c\/p\u003e\n\u003cp\u003eIt is believed that Zeolites forming near the surface of an older basalt flow were covered and reheated by a younger flow (Rew, 1969). The reheating partly dissolved existing Zeolites and redeposited new minerals as the solutions cooled.\u003c\/p\u003e\n\u003cp\u003eNatrolite:-\u003c\/p\u003e\n\u003cp\u003eNamed for the Greek for “sodium,” natrio, in reference to the mineral’s sodium content, and for “stone,” lithos. Natrolite is a mineral that occurs in cavities in basalts and other igneous rocks as one of the last minerals to forms, and also occurs as a filling in seams in granites, gneisses, and syenites.\u003c\/p\u003e\n\u003cp\u003eNatrolite is pyroelectric and piezoelectric, and will generate a charge in response to temperature and pressure changes, respectively. It will commonly fluoresce an orange to yellow under ultraviolet light.\u003c\/p\u003e\n\u003cp\u003eNatrolite is the principal member of a group of zeolite minerals whose molecular structure is predominantly chains of linked silicate and aluminate tetrahedra (four oxygen atoms arranged at the points of a triangular pyramid about a central silicon or aluminium atom); the relative scarcity of lateral bonds between chains results in the characteristic fibrous appearance of the group. Other zeolites in the natrolite group are Mesolite, Scolecite, Thomsonite and Gonnardite; all have similar modes of occurrence, molecular structures, and physical properties, even though they have different crystal symmetries: mesolite and scolecite crystallize in the monoclinic system (three unequal axes with one inclined to the plane of the other two), whereas Natrolite, Thomsonite, and Gonnardite crystallize in the orthorhombic system (three unequal axes at right angles to one another). Mesolite is chemically intermediate between Natrolite and Scolecite.\u003c\/p\u003e\n\u003cp\u003eNatrolite was one of the first zeolite minerals for which cation-exchange properties (dissolved sodium, potassium, calcium, and magnesium readily replacing one another in the molecular structure) were discovered. It is used in softening water.\u003c\/p\u003e\n\u003cp\u003eAnalcime:-\u003c\/p\u003e\n\u003cp\u003eThe name Analcime is derived from the Greek term \"an alkimos\", meaning \"not strong, in allusion to the weak pyroelectricity exhibited by this mineral.\u003c\/p\u003e\n\u003cp\u003eAnalcime or analcite is a white, grey, or colourless tectosilicate mineral. Analcime consists of hydrated sodium aluminium silicate in cubic crystalline form. Its chemical formula is NaAlSi₂O₆·H₂O. Minor amounts of potassium and calcium substitute for sodium.\u003c\/p\u003e\n\u003cp\u003eAnalcime is a member of the Zeolite group and often occurs together with other zeolites. However, it is closely related in structure to the Feldspathoid group and is occasionally also classified as a Feldspathoid together with the similar mineral Leucite. However, most mineralogical sources, including the IMA, classify Analcime only as a Zeolite and not as a feldspathoid.\u003c\/p\u003e\n\u003cp\u003eAlthough the crystal structure of Analcime appears isometric its is usually off by only a fraction of an angle. This technically removes its classification from the isometric crystal system. Analyses of different Analcime crystals have yielded multiple results in crystal symmetry, with the most prevalent symmetry being tetragonal. However, truly isometric examples have been analysed and do exist, thus making this mineral complex in its crystal classification. Due to Analcime's appearance as an isometric mineral, and the fact that isometric examples do exist, we have placed this mineral within the isometric group for classification.\u003c\/p\u003e","brand":"NaturesgiftsByChris","offers":[{"title":"Default Title","offer_id":49616734945557,"sku":null,"price":17.99,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0870\/2453\/3781\/files\/7f459b41-il_fullxfull.6518956876_df34.jpg?v=1765592705","url":"https:\/\/naturesgiftsbychris.com\/products\/22g-analcime-with-natrolite-pink-seed-specimen","provider":"NaturesgiftsByChris","version":"1.0","type":"link"}