A distinctive physical property of bulk water is its rich solid-state phase behavior, which includes 15 crystalline (ice I-ice XIV) and at least 3 glassy forms of water, namely, low-density amorphous, highdensity amorphous, and very-high-density amorphous (VHDA). Nanoscale confinement adds a new physical variable that can result in a wealth of new quasi-2D phases of ice and amorphous ice. Previous computer simulations have revealed that when water is confined between two flat hydrophobic plates about 7-9 Å apart, numerous bilayer (BL) ices (or polymorphs) can arise [e.g., BL-hexagonal ice (BL-ice I)]. Indeed, growth of the BL-ice I through vapor deposition on graphene/Pt(111) substrate has been achieved experimentally. Herein, we report computer simulation evidence of pressure-induced amorphization from BL-ice I to BL-amorphous and then to BL-VHDA 2 at 250 K and 3 GPa. In particular, BL-VHDA 2 can transform into BL-VHDA 1 via decompression from 3 to 1.5 GPa at 250 K. This phenomenon of 2D polyamorphic transition is akin to the pressure-induced amorphization in 3D ice (e.g., from hexagonal ice to HDA and then to VHDA via isobaric annealing). Moreover, when the BL-ice I is compressed instantly to 6 GPa, a new very-high-density BL ice is formed. This new phase of BL ice can be viewed as an array of square ice nanotubes. Insights obtained from pressure-induced amorphization and crystallization of confined water offer a guide with which to seek a thermodynamic path to grow a new form of methane clathrate whose BL ice framework exhibits the Archimedean 4·8 2 (square-octagon) pattern.bilayer water and ice | molecular dynamics simulation | bilayer methane hydrate | amorphous-to-amorphous transition T he special character of confined water stems not only from unique properties of a hydrogen-bonding network, such as its ability to expand when cooled below the freezing point or to form rich structures of polymorphs under strong compressions, but from its spatial inhomogeneity, particularly in the nanoscale spaces. Forced to pack into the nanoscale spaces severely constricted by confining surfaces, water molecules in the vicinity of a flat surface tend to arrange themselves in layers parallel to the surface. The resulting oscillations in local density are reflected in properties of the confined water that can differ drastically from those of the bulk water. Not only are intriguing properties of confined water of fundamental interest, but they have implications for diverse practical phenomena at the intersection between chemistry, biological sciences, engineering, and physics: boundary lubrication in nanofluidic and laboratory-on-a-chip devices; frost heaving in soil; synthesis of antifreeze proteins for ice-growth inhibition; rapid cooling of biological suspensions or quenching emulsified water under high pressure; storage of gas hydrates; and hydrogen fuel cells that generate electricity by passing hydrogen ions across a membrane, where water is confined in nanoscale channels. Hence, an improved understanding of the behavi...