The most familiar anomaly is its increasing density with temperature, at ambient pressure, up to 4 o C. Above this temperature water behaves as a normal liquid and density decreases as temperature rises. Experiments for water allow to locate the line of temperatures of maximum density (TMD) in the pressure-temperature plane. Below TMD density decreases with decreasing temperature, differently from the behavior of the majority of fluids, for which density increases on lowering temperature 1 .Besides a number of thermodynamic and dynamic anomalies water exhibits many solid phases due to strucural and symmetry changes. Several coexistence lines separate the multiple solid phases. Thus, the energy landscape associated to the crystalline phases presents a number of sharp valleys with very low energies. The temperature and pressure ranges at which each one of these sharp valleys displays lowest energy values define the stable phase in that region of the phase diagram. Those valleys of the energy landscape that never achieve the lowest energy correspond to the amorphous configurations. Therefore it is reasonable to think that multiple amorphous phases are present. Even though the existence of water amorphous phases has been known since 1935 2 , the identification of two amorphous phases, one of lower density (LDA), the other of higher density (HDA) 3,4 , as well as the suggestion