
mineral
Garden Quartz (Lodalite)
Silicon Dioxide with various mineral inclusions (SiO2)
AI-generated identification · may be incorrectHardness 7 on Mohs scale; Color is transparent clear with green, brown, or red inclusions; Vitreous luster; Trigonal crystal structure; Conchoidal fracture; Specific gravity 2.65.
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Physical properties
Hardness 7 on Mohs scale; Color is transparent clear with green, brown, or red inclusions; Vitreous luster; Trigonal crystal structure; Conchoidal fracture; Specific gravity 2.65.
Formation & geological history
Formed in hydrothermal veins or pegmatites when quartz crystals grow around other minerals like chlorite, hematite, or feldspar. These inclusions are 'trapped' during the quartz's growth phase millions of years ago.
Uses & applications
Primarily used as a decorative specimen, in lapidary arts for polishing into spheres or 'lenses', and highly valued in the metaphysical and crystal collecting communities.
Geological facts
Also known as 'Lodalite' or 'Scenic Quartz', these stones are often called 'shaman stones' or 'landscape quartz' because the internal inclusions resemble underwater scenes, gardens, or forests.
Field identification & locations
Identify by looking for 3D mineral landscapes inside clear quartz. Unlike synthetic glass with bubbles, natural garden quartz will have complex, irregular mineral structures. Major sources include Minas Gerais, Brazil.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary