| 11. | Diffraction spots caused by goethite are diffuse even though the material is well oriented.
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| 12. | :: : : It appears that Goethite becomes magnetic in a reducing flame.
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| 13. | They consist largely of goethite and contain 1-2 % nickel incorporated in goethite.
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| 14. | They consist largely of goethite and contain 1-2 % nickel incorporated in goethite.
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| 15. | Other minerals such as topaz, fluorite and goethite have been found in the area.
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| 16. | Native gold is mostly associated with goethite.
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| 17. | Goethite-like structures are common because goethite is in the same space group as olivine.
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| 18. | Goethite-like structures are common because goethite is in the same space group as olivine.
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| 19. | The Clovis group is especially interesting because the M�ssbauer spectrometer ( MB ) detected goethite in it.
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| 20. | The preferred orientation of olivine and goethite are when they are parallel with their z-axis.
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