• Filters
  • Sort by
    ...
  • -10%Limited
    Tourmaline Slide
    Tourmaline Slide £18.00 ex VAT

    Microscope slides of tourmaline from Brazil, these slides display the crystal structure of the mineral on a microscopic level which assists in the identification of this mineral in other slides. Each section is made to 30 microns thickness and the glass is 46 x 27 mm in size, supplied in a protective card sleeve with a label, ideal for microscopy & educational use.

    Add to cart

    3 in stock

  • -10%Limited
    Travertine Slide £18.00 ex VAT

    Travertine thin section slide. Travertine is a form of limestone deposited by mineral rich springs, especially hot springs. It is formed by the rapid precipitation of calcium carbonate, often at the margins of a hot spring or in a limestone caves.

    Add to cart

    6 in stock

  • -10%Limited
    Tufa Slide £18.00 ex VAT

    Tufa thin section slide. Tufa is a variety of limestone, formed by the precipitation of carbonate minerals from ambient temperature water bodies. This particular material is from the Flandrian epoch of the Quaternary Period and it was collected in Caerwys, North Wales.

    Add to cart

    5 in stock

  • -10%Limited
    Volcanic Scoria Slide £18.00 ex VAT

    Volcanic scoria thin section slide exhibiting the highly vesicular nature of this extrusive volcanic rock. Typically volcanic scoria is basaltic or andesitic in composition; these magmas are typically runnier which results in a denser rock with larger vesicles.

    Add to cart

    26 in stock

  • -10%LimitedSold Out
    Volcanic Tuff Slide £18.00 ex VAT

    Volcanic tuff thin section exhibiting welded angular clasts of varying size. A degree of orientation can be identified as a result of the fallout of volcanic ejecta. Each section is made to 30 microns thickness and the glass is 46 x 27 mm in size with a cover slip.

    Read more

    Out of stock

  • -10%Limited
    Welded Tuff Slide £18.00 ex VAT

    Welded tuff thin section slide exhibiting a jumbled mass of irregularly sized broken clasts held in situ by finer ash particles which have become welded together. This material was collected from Cumbria, the original rock is likely rhyolite, and indeed in hand specimen the tuff almost still looks like rhyolite and appears to show a form of banding.

    Add to cart

    6 in stock

Close
Price
Price: Reset
Close My Cart
Close Wishlist
Recently Viewed Close
Close

Close
Navigation
Categories