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This type belongs to a different mineral family, the amphiboles, here, instead of forming sheets, the silica tetrahedra lock into rigid, ladder-like chains,
and amosite, iron and magnesium ions, along with hydroxyl groups embedded in the structure, bind those chains together, forming these long, needle-like fibers,
but tweak that chemistry just slightly so that now iron and sodium ions bind the chains, and you get this, blue asbestos or crocidolite.
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