his work presents a comprehensive study on pressure-induced amorphization (PIA) in
-eucryptite(
LiAlSiO
4) and on the equilibrium states of so-formed amorphous phase at elevated temperatures. Ourresults revealed that at 300 K
-LiAlSiO
4 underwent progressive amorphization at pressures above 4.5GPa and became completely amorphous above 17.0 GPa. After release of pressure,
-LiAlSiO
4 that waspartially amorphized at 7.5, 14.0, and 16.0 GPa reverted back to its original crystalline state. Whensubjected to a complete loss of long-range structural order, the system was recovered as an amorphousstate and did not retain the so-called structural memory. Upon heating at high pressures, the partially orcompletely amorphous
-LiAlSiO
4 transformed into various crystalline phases at temperatures above973 K: between 6.9 and 10.7 GPa it was decomposed into a mixture of LiAlSi
2O
6 and LiAlO
2; at 15.3GPa the two phases recombined to form a new phase with a spinel structure; and at 22 GPa the spinelphase of LiAlSiO
4 was decomposed into its constituent oxides. The observed transformations are all ofa reconstructive type and also involve profound changes in atomic coordination environments. A largeactivation energy barrier associated with coordination changes and a hindrance of atomic mobility atkinetically low temperatures are the primary factors that trigger the PIA.