Earth Record
Mineralogy and formation
Basalt meets atmosphere and loses everything it was. Lava stone is not a mineral. It is the husk of eruption, a vesicular basite riddled with gas pockets that froze open when molten rock hit air faster than dissolved volatiles could escape. The composition varies with whatever magma source fed the flow. Most lava stone in commerce is from Icelandic or Indonesian basaltic fields, tumbled smooth and sold as grounding talismans.
Geologically it is frozen chaos. The vesicles that make it light enough to sometimes float are the same voids that make it structurally weak. It absorbs essential oils because it is literally full of holes. That is not metaphysical porosity. That is igneous texture doing what physics dictates. Every piece records the exact moment liquid rock became solid in open air.
Polymineralic rock structure
Chemical FormulaBasalt (variable silicates)Crystal SystemPolymineralic rockMohs Hardness5Specific Gravity2.8-3.0LusterDull to matteColorBlack to dark gray, porousIMA StatusrockIMA Numberpre-IMA Worldwide (volcanic regions)
Telling it apart
Lava stone (basalt) beads are among the most heavily substituted products in the mass-market crystal trade. Dyed pumice, ceramic, slag, and even molded concrete are all sold as lava stone. Genuine basalt has a characteristic vesicular (porous) texture with irregular gas bubble holes of varying sizes, fine-grained dark gray to black matrix, and a Mohs hardness around 3 to 3. 5 for the matrix.
The porosity is natural and irregular; if every pore is the same size and evenly distributed, the material may be manufactured. Ceramic fakes often feel smoother and more uniform than natural basalt, which has a rough, gritty texture. Genuine lava stone should feel heavier than pumice (which is essentially glass foam and floats in water) with specific gravity of 2. 8 to 3. 0. The popularity of lava beads for essential oil diffusion has driven massive demand, and the cheapest sources supply dyed or manufactured material.
A simple test: genuine basalt does not fizz in acid, but concrete and some slag do. The pores in real basalt are interconnected and absorbent, which is why they work for oil diffusion, while glazed ceramic beads resist absorption despite looking porous on the surface.
Spotting the real thing
Lava stone is one of the most commonly faked stones in the crystal market, primarily because black round beads are cheap to manufacture from dyed materials. Four tests, no equipment needed. The pore test. Real lava stone has visible, irregular pores (vesicles) across its entire surface. These holes vary in size, are randomly distributed, and have rough edges. Fake lava stone (often dyed howlite or ceramic) either has no pores, has pores that are too uniform, or has surface texture that was mechanically applied.
The weight test. Real lava stone is lightweight for its size due to its vesicular structure. Pick up a lava bead and a glass bead of the same size. The lava stone should feel noticeably lighter. If it feels as heavy as glass or ceramic, it is not basalt. The water absorption test. Drop water on the surface.
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