Mineralogy
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In our eReader you can find the full English version of the book. Read Mineralogy Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Mineralogy
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MICA- may be conveniently separated into CRYSTAL.
i i i j ji i -i Basal plane- M two broad subdivisions: the white or prism- A clino- light-coloured. And the black or dark- pinacoid;'*, clino- dome.
coloured varieties. Chief among the former is muscovite, or potash-mica, which is essenti- ally a hydrated silicate of alumina and potash. This variety of mica is not attacked by hydrochloric acid. It is generally pale-coloured to silvery white, with pearly lustre on the cleavage surfaces. It occurs... in flakes, scales, and laminae, in many granites, gneisses, and phyllites. Fragments are often present in sand- stones and shales (derived, no doubt, originally from granitic rocks) ; and by their parallel arrangement impart to these rocks a fissile character.
100 DESCRIPTIVE MINERALOGY Less common than muscovite are the following light- coloured micas : Paragonite, or soda-mica. Lepidolite, or lithia-mica.
Biotite. The most important dark mica ; essentially a hydrated ferro-magnesian and aluminous silicate.
What to read after Mineralogy?
You can find similar books in the "Read Also" column, or choose other free books by F H Frederick Henry Hatch to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
MICA- may be conveniently separated into CRYSTAL.
i i i j ji i -i Basal plane- M two broad subdivisions: the white or prism- A clino- light-coloured. And the black or dark- pinacoid;'*, clino- dome.
coloured varieties. Chief among the former is muscovite, or potash-mica, which is essenti- ally a hydrated silicate of alumina and potash. This variety of mica is not attacked by hydrochloric acid. It is generally pale-coloured to silvery white, with pearly lustre on the cleavage surfaces. It occurs... in flakes, scales, and laminae, in many granites, gneisses, and phyllites. Fragments are often present in sand- stones and shales (derived, no doubt, originally from granitic rocks) ; and by their parallel arrangement impart to these rocks a fissile character.
100 DESCRIPTIVE MINERALOGY Less common than muscovite are the following light- coloured micas : Paragonite, or soda-mica. Lepidolite, or lithia-mica.
Biotite. The most important dark mica ; essentially a hydrated ferro-magnesian and aluminous silicate.
What to read after Mineralogy?
You can find similar books in the "Read Also" column, or choose other free books by F H Frederick Henry Hatch to read onlineMoreLess
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