About Travertine
Travertine is a
natural chemical precipitate of carbonate minerals; typically aragonite, but
often recrystallized to or primarily calcite; which is deposited from the water
of mineral springs or streams saturated with calcium carbonate. When pure,
travertine is white, but often is brown to yellow due to impurities. When
carbon dioxide-rich water percolates through rocks in limestone areas, the
water dissolves the limestone and becomes saturated with it. When the water
resurfaces later, the sudden drop in pressure and the change in temperature
cause the water to release carbon dioxide gas, much like fizzy drinks. The
calcium carbonate then recrystallizes, often over minute underwater plants. The
resulting rock is typically quite porous with numerous cavities. When
exceptionally porous it is known as calcarious tufa.
Extensive deposits of Travertine exist at
Travertine has formed 16 huge, natural dams in a valley in
Other beautiful cascades of natural lakes formed behind travertine dams can
be seen in Band-i-Amir (
Travertine is one of several natural stones that are used for paving patios
and garden paths. It is sometimes known as travertine limestone, sometimes as
travertine marble; these are the same stone, even though it is neither
limestone nor marble. The stone is characterised by pitted holes and troughs in
its surface. Although these troughs occur naturally, they suggest to some eyes
that considerable wear and tear has occurred over many years. Some installers
use a grout to fill these holes, whereas others leave them open — travertine
can even be purchased "filled" or "unfilled." It can be
effectively polished to a smooth, shiny finish and comes in a variety of colors
from grey to coral-red. Travertine is most commonly available in tile sizes for
floor installations. Travertine is one of the most frequently used stones in
modern architecture, and is commonly seen as facade material, wall cladding,
and flooring.