Neutron and x-ray diffraction data for low, high, and very high density amorphous ice and liquid water, silicon, and germanium have been compared in terms of the first sharp diffraction peak in the structure factor and at the radial distribution function level. The low and high density forms of H 2 O, Si, and Ge are shown to have very similar structures if the contributions from the hydrogen correlations in water are neglected. The very high density amorphous ice form is shown to be structurally analogous to recently reported high pressure liquid forms of Si and Ge, although there are slight differences in the way interstitial atoms or molecules are pushed into the first coordination shell.The structure of tetrahedral low density, 1-4 high density, 5-7 or very high density, 8-13 glassy and liquid forms has been investigated in several materials over the past two decades, with much attention focused on amorphous ice. 1,5,9,10,12,14,15 Although the structural changes in densified amorphous or liquid water are usually associated with that of glassy SiO 2 under pressure, 16,17 in this paper we show that the structures of low, high, and very high density amorphous ice ͑denoted LDA, HDA, and VHDA, respectively͒ exhibit remarkable similarities with amorphous and liquid silicon and germanium. All form low density amorphous tetrahedral networks with intermediate range ordering 1 having well defined second and higher coordination shells. Water, Si, and Ge also have a high density liquid structure in which the second nearest neighbor shell has largely collapsed into the interstitial region between the first and second shells. Recently, higher density forms have been measured using high pressure diffraction techniques for both Si ͑Ref. 8͒ and Ge, 11 which show strong structural similarities to that of very high density amorphous ice 10,12 and with liquid water at a high pressure. 13 The very high density forms all show increased intermediate range ordering compared to the high density form, but differences occur in the way additional atoms or molecules are pushed into the nearest neighbor shell in water.Several theories have been suggested to explain transitions between high and low density liquid or amorphous forms, including a first order phase transition between two different states, i.e., polyamorphism, and a singularity free scenario. 15 In liquid Si, polyamorphism has been used to explain the transition between the high and very high density forms of liquid Si, 8 and the transformation from very high density to low density amorphous ice. 9,18,19 However liquid water and low density amorphous ice at normal pressure are physically separated by a region referred to as "no man's land," 15 since it is not possible to supercool bulk liquid water below the homogenous nucleation temperature of 228 K without the onset of crystallization ͑except by very rapid cooling of small droplets or hyperquenching 20 ͒ and the low density amorphous ice form crystallizes on heating above ϳ130 K. Similar discontinuities exist between the supe...