calcareous sinter
Quick Summary
Calcareous sinter is a mineral deposit characterized by a porous or vesicular texture, meaning it contains small cavities. It is a type of sinter, with siliceous sinter being the other recognized kind.1
Calcareous sinter is composed of calcium carbonate and is also known as travertine, calcareous tufa, or calc-tufa. It is often formed by waters rich in calcium carbonate, which deposit a sintery crust on objects exposed to them, a process sometimes referred to as petrifying springs. The cavities within calcareous sinter can result from the decay of mosses and other vegetation that aid in its precipitation.123
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