i had trouble with that diagram but making more sense now after some serious study. It looks to me as if and when mankind ever gets the tech to land on an ice ball water world that a hydrologist will be part of the crew.
Once the pressure gets up around 100Gpa then Ice VII, VIII, X & XI appear and the temps range from above to below 0°. How can ice be both super cold and hot? Does it depend on whether the pressure was originally applied to water while in ice, liquid or vapor state?
Substances can vary a lot in form according to the prevailing temperature and pressure. Water is no exception.
The phase diagram shows you what phases prevail under different conditions at equilibrium. This does not depend on where you start from. You could in principle prepare a sample of ice VII at 50C and 10Gpa either starting with liquid water at 1 atm and 50C or vapour at 10 atm and 150C. Similarly a sample of ice VII at 50C would be expected to revert to liquid once the pressure is reduced to 1atm, or to vapour at 0.1atm.
However the phase diagram does not tell you anything about
rates of change when conditions are altered. In other words it tells you the thermodynamically stable phases but does not tell you about the kinetics of changing from one phase to another. I looked this up and find that ice VII is said to be metastable, which implies it takes time to change when the pressure is reduced. I could not find out how long it takes to change though. (It would be fun if it takes more than a few minutes, in which case you could in principle get a sample and drop it in your gin and tonic, whereupon it would sink to the bottom as it is denser than water, unlike normal ice.)
I also found ice VII seems to be thought important in the physics of the outer planets. (Perhaps this is why you are asking about it?) I also found that it is even said to be a terrestrial "mineral", due to the discovery of inclusions of ice VII within certain specimens of diamond! Presumably the diamond, which was formed under great pressure within the Earth, is able to maintain that pressure internally and keep the ice in its VII phase.
(As a matter of fact diamond is itself a phase of carbon which is technically only metastable at ambient temperature and pressure, though the rate of change to graphite is infinitesimally slow.)