generated from Jaysyn/ModuleTemplate
116 lines
3.3 KiB
JSON
116 lines
3.3 KiB
JSON
{
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"__data_type": "UTI ",
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"Comment": {
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"type": "cexostring",
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"value": "Quartz is one of the most common minerals in the Earth's continental crust. It has a hexagonal crystal structure made of trigonal crystallized silica (silicon dioxide, SiO2), with a hardness of 7 on the Mohs scale. Density is 2.65 g/cm³. The typical shape is a six-sided prism that ends in six-sided pyramids, although these are often twinned, distorted, or so massive that only part of the shape is apparent from a mined specimen. Additionally a bed is a common form, particularly for varieties such as amethyst, where the crystals grow up from a matrix and thus only one termination pyramid is present. A quartz geode consists of a hollow rock (usually with an approximately spherical shape) with a core lined with a bed of crystals.\r\n"
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},
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"type": "cexolocstring",
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"value": {
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"0": "Quartz is one of the most common minerals in the Earth's continental crust. It has a hexagonal crystal structure made of trigonal crystallized silica (silicon dioxide, SiO2), with a hardness of 7 on the Mohs scale. Density is 2.65 g/cm³. The typical shape is a six-sided prism that ends in six-sided pyramids, although these are often twinned, distorted, or so massive that only part of the shape is apparent from a mined specimen. Additionally a bed is a common form, particularly for varieties such as amethyst, where the crystals grow up from a matrix and thus only one termination pyramid is present. A quartz geode consists of a hollow rock (usually with an approximately spherical shape) with a core lined with a bed of crystals.",
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"id": 83789
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}
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"LocalizedName": {
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"type": "cexolocstring",
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"value": {
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"0": "Faceted, Quartz",
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"id": 83788
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"PropertiesList": {
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{
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"Stolen": {
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"Tag": {
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"type": "cexostring",
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"value": "ct_quartz4"
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"TemplateResRef": {
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"type": "resref",
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"value": "ct_quartz4"
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