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6 - CATALOGUE OF MINERALS SHOWN AT EDINBURGH (1884)

Published online by Cambridge University Press:  05 March 2012

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Summary

GROUP I.—1–20

Introductory Examples, ascending from COMMON FLINT to PERFECT ENDOGEN AGATE

  1. Amber chalcedony with flint.

  2. Quartzite chalcedony with cycloidal superstructure.

  3. Cycloidal chalcedony in films on flint.

  4. Flint with chalcedonic fissure.

  5. Nodule of red flint-chalcedony.

  6. Chalcedony in stalactitic coats, varying in their lines of current.

  7. Finest state of pure chalcedony, in irregularly combined rods and films.

  8. Chalcedony on hæmatite.

  9. Spheroidal haematite in quartz.

  10. Grey spheroidal agate, partly stalactitic.

  11. Perfectly formed agatescent stalactite, of white chalcedony, with external quartz.

  12. Agatescent stalactites of pure chalcedony, with green, more or less tubular, centres.

  13. Filiform chalcedony with green tubular centres, its threads collecting gradually into a solid mass.

  14. Filiform chalcedony, with green centres, not tubular.

  15. Pisolitic heliotrope (showing the spherical structure at the edge).

  16. Pisolitic heliotrope in parallel bands. Look at it by transmitted light.

  17. Tubular agate, the common form, but a singularly fine example.

  18. Pure spheroidal agate, developing itself round an earthy stalactitic centre, with external quartz (magnificent).

  19. Half of a perfect geode of spheroidal agate, with external quartz.

  20. Portion of a nodule of irregularly muscose and spheroidal agate, with external quartz.

Note especially in this example, on its polished side, the portion of the external salmon-coloured band of the agate, which has been separated from the rest and carried up into the body of the crystallizing quartz.

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Publisher: Cambridge University Press
Print publication year: 2010
First published in: 1906

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