Why group these materials together? Marble, limestone and travertine are different stones, but they share many practical maintenance characteristics because they are predominantly carbonate-based materials. They are generally acid-sensitive, relatively soft compared with granite and quartzite, and can often be refinished using similar restoration methods.
Geologically, however, they are not the same. Limestone is a sedimentary rock, travertine is a type of limestone formed by mineral precipitation, and marble is a metamorphic rock produced when limestone or other carbonate stone is subjected to heat and pressure. These differences contribute to the wide range of textures, densities, porosities and appearances found within the group.
All three are commonly used for floors, bathrooms, wall installations and countertops. Marble's recrystallized structure often allows it to develop excellent clarity and depth when polished, while limestone and travertine can range from very dense materials to much more open-grained varieties.
Travertine deserves a special mention from a maintenance standpoint. Its natural voids, fills and visual variation can make minor etching, scratches and traffic wear less obvious than they would be on a very uniform polished marble. That does not make travertine maintenance-free, but it can make normal wear easier to live with.
Marble, limestone and travertine are generally sensitive to acids because carbonate minerals—particularly calcite—make up a large part of their composition. Everyday products such as vinegar, citrus, wine and acidic cleaners can react with the surface and leave dull etch marks.
The severity and speed of the reaction vary with the mineral composition and finish of the individual stone. Dolomitic stones, for example, may react more slowly than calcite-rich materials, but they should still be considered acid-sensitive.
Calcite, the principal mineral in many marbles and limestones, has a Mohs hardness of about 3. Dolomite is somewhat harder, and individual stones may also contain other minerals, so the hardness of the finished stone can vary.
Because these materials are relatively soft, grit tracked in from outdoors can gradually scratch and abrade floors. Quartz, a common component of sand and soil, has a Mohs hardness of 7 and is easily capable of scratching calcite-based stone. Entrance mats and regular dust-mopping are therefore particularly useful for marble and limestone floors.
Porosity varies considerably within this group. Some marbles are very dense and absorb relatively little moisture, while limestone and travertine can range from low-absorption materials to highly porous stones. Even two stones sold under the same general family name can behave very differently.
For that reason, sealing should be based on the actual absorption characteristics of the stone and how the surface is being used rather than on a fixed schedule. Countertops, showers and other areas exposed to water, oils or contaminants should be checked periodically and resealed when the stone begins absorbing liquids readily.
Penetrating sealers can reduce absorption and help protect against staining, but they do not waterproof the stone or prevent etching.
Marble, limestone and travertine are generally very workable materials from a restoration standpoint. Their relative softness allows damaged surfaces to be mechanically ground, honed and polished without the difficulty associated with much harder stones such as granite and quartzite.
Scratches, etches and many forms of surface wear can often be isolated and blended into the surrounding finish, although the ease of a localized repair depends on the particular stone, pattern and level of finish. These materials can also usually be converted between polished, Patina and honed finishes when the installation is suitable.
Natural fissures, filled areas, strong veining and variation in mineral composition can make some repairs more challenging, so repairability still varies from one stone to another.