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Travertin Noce

The close-up view of each stone type shows a relatively true image of the crystalline structure and the colouring. This is suitable for grained slabs to a limited extend only. In regard to the colour matching, please take an original sample of the stone from your furniture store as a basis.

Travertineis one of thevery fewstone types, which are lacquered with a specialstoneprotection because of their extremeabsorbency. The surfacereceives a finesilky luster. Theperformance characteristicsare similar to thoseof alacquered wood surface.

Petrography

Travertine is porous limestone in layers, which has been deposited in inland water (wells, rivers, fresh water lakes). The most famous and largest travertine deposit is located between Bagni di Tivoli and Guidonia, to the west of Rome. The type Travertin Noce is a light to medium brown, bright travertine with an indication of bands. Round to oval holes can be found lined up in layers, generated by crusts around water plants.

Petrogenesis

Travertine is fresh water lime, which has been generated by deposits of lime from the mineral-containing water on parts of plants and on the floor of a stretch of water. They are earth-historically young formations with thicknesses of up to 30 m. The lower layers have been compacted to such an extent by the superimposed younger layers that hardly any pores are left and they finally have converted into tight limestone; the original rock for crystalline meta-morphous marble. 

Hardness Soft Stone
Structure Type Homogeneous Structure
Synonyms Roma Classico, Roma Tiburtinus, Travertino Classico
Group Sediment rock
Petrographic Assignment Limestone
Age 1 million years (Holocene)
Colouring Minerals Lime
Average Hardness 3 (according to Mohs’s hardness scale 1-10)
Deposit Italy / near Bagni di Tivoli & Guidonia (Rome)