Microscopy Primer
Light and Color
Microscope Basics
Special Techniques
Digital Imaging
Confocal Microscopy
Live-Cell Imaging
Photomicrography
Microscopy Museum
Virtual Microscopy
Fluorescence
Web Resources
License Info
Image Use
Custom Photos
Partners
Site Info
Contact Us
Publications
Home

The Galleries:

Photo Gallery
Silicon Zoo
Pharmaceuticals
Chip Shots
Phytochemicals
DNA Gallery
Microscapes
Vitamins
Amino Acids
Birthstones
Religion Collection
Pesticides
BeerShots
Cocktail Collection
Screen Savers
Win Wallpaper
Mac Wallpaper
Movie Gallery

Polarized Light Microscopy Digital Image Gallery

Mica Schist

Schists are crystalline rocks with a foliated structure that enables them to be easily divided into layers. The majority of schists are primarily comprised of platy minerals, such as micas.

Micas are a group of minerals that are characterized by their ability to easily separate into thin, relatively flexible sheets or plates. Present in various forms around the world, the hue of mica ranges from colorless to brown, black, and green, and largely depends upon the mineral’s iron content. The most economically important micas are phlogopite, which is rich in magnesium, and muscovite, which is potassium based. Utilized in sheets, as scraps, or ground, both have found use in a variety of products, such as paints, tiles, and wallpaper. The micas are also often utilized as an insulating material.

The most common schist that occurs on Earth is mica schist, which essentially consists of quartz and mica, but may also contain some feldspar. Similar to other schists, mica schist is metamorphic and flakes of its component minerals (usually muscovite or biotite) are visible to the unaided eye. Abundant amid Precambrian rocks, a variety of valuable materials may be interbedded with mica schists. For example, ancient Egyptians mined massive quantities of mica schist to find emeralds, which have also since been found in mica schists in Austria and the Russian Urals. Similarly, other types of beryl, aventurine, and even marble, are frequently found amid deposits of mica schist.


BACK TO THE ROCKS AND MINERALS GALLERY

BACK TO THE POLARIZED LIGHT GALLERY

Questions or comments? Send us an email.
© 1998-2022 by Michael W. Davidson and The Florida State University. All Rights Reserved. No images, graphics, scripts, or applets may be reproduced or used in any manner without permission from the copyright holders. Use of this website means you agree to all of the Legal Terms and Conditions set forth by the owners.
This website is maintained by our
Graphics & Web Programming Team
in collaboration with Optical Microscopy at the
National High Magnetic Field Laboratory.
Last modification: Friday, Nov 13, 2015 at 02:19 PM
Access Count Since November 20, 2003: 18004
For more information on microscope manufacturers,
use the buttons below to navigate to their websites: