Description
GOGOTTE greasy concretion of siliceous sand resulting from the displacement of phreatic liquid (saturated water dissolving silica) leading to the phenomenon of grésification giving the unusual appearance characteristic of gogottes. Dating on the geological time scale (fossiliferous) probably Lower Oligocene (33-28 mA). Nicely sinuosic specimen on base This mineral specimen is not subject to regulation under the Washington Convention (CITES), European Community Regulation 338/97 of 09/12/1996, or the French Environment Code. Gogotte, Fontainebleau, probably from the Lower Oligocene (33-28 million years) Weight :80000 g. - 2 821.92 OZ HEIGHT 78 - WIDTH 45 CM - H. 30,7 - W. 17,7 IN.
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GOGOTTE greasy concretion of siliceous sand resulting from the displacement of phreatic liquid (saturated water dissolving silica) leading to the phenomenon of grésification giving the unusual appearance characteristic of gogottes. Dating on the geological time scale (fossiliferous) probably Lower Oligocene (33-28 mA). Nicely sinuosic specimen on base This mineral specimen is not subject to regulation under the Washington Convention (CITES), European Community Regulation 338/97 of 09/12/1996, or the French Environment Code. Gogotte, Fontainebleau, probably from the Lower Oligocene (33-28 million years) Weight :80000 g. - 2 821.92 OZ HEIGHT 78 - WIDTH 45 CM - H. 30,7 - W. 17,7 IN.
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