Under the pressure of 1-1.6 GPa, hexagonal ice at 77 K collapses to a high density amorphous ice (HDA). The HDA recovered from the pressure vessel is highly strained. It is called unrelaxed HDA, or uHDA. Here, first we examine the merits of the ambient pressure differential scanning calorimetry (DSC) study of uHDA by P. H. Handle, M. Seidl and T. Loerting, Phys. Rev. Lett. 108 (2012) 225901, which was used to determine its alpha-relaxation time and T-g at high pressures. We find that their procedure does not yield the alpha-relaxation time of 10(3) s to 10(6) s at T < T-g, nor does it yield the activation energy and T-g of uHDA. uHDA does not have T-g because there is no unrelaxed water. Second, we discuss the nature of the transformations of uHDA to eHDA (the expanded or relaxed form of HDA), and of eHDA to LDA (the 20% bulkier amorphous ice formed on heating HDA). By using the available results for the uHDA -> eHDA and eHDA -> LDA transformations, which had been obtained by heating at 10 K/min and 10 K/h rates, we argue that the strain (internal stress) brings the two transformations mutually closer, and loss of strain on annealing separates them. The highest enthalpy loss on stress-release is as much as twice the enthalpy loss on structure-change. The analysis confirms that on annealing or heating, transformation of the as-made HDA to LDA occurs through a series of metastable states of increasing volume. (C) 2014 Elsevier B.V. All rights reserved.