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

Travertine

Travertine is a crystalline form of calcite that occurs in massive form. The material is most often found around the rims of hot springs and streams because it develops through the separation of calcium carbonate from water via the process of evaporation.

Typically banded, travertine is generally quite beautiful in appearance, exhibiting a variety of colors depending upon the impurities it contains. The material, which is also easy to cut and highly polishable, therefore, is often utilized as an ornamental stone. It is sometimes better known as Egyptian alabaster, onyx marble, or Mexican onyx when sold commercially for interior walls, floors, balustrades, stairways, and similar items. Travertine is also often utilized in combination with other types of marble, further increasing the magnificence of many decorative objects it is commonly utilized to construct.

The term travertine derives from an old Roman name for Tivoli, an Italian town where large deposits of the calcium carbonate can be found. Travertine quarried in Tivoli under the late Roman republic as well as the early empire was an extremely popular building material. It was, for instance, utilized to create the exterior of the famous Coliseum in Rome. Significant deposits of travertine also occur at Mammoth Hot Springs in Yellowstone National Park, Wyoming and various other locations around the world where limestone is common and calcium carbonate is present in circulating ground water.


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: 12081
For more information on microscope manufacturers,
use the buttons below to navigate to their websites: