Table 1. H2O Ice Shock Data
Symbol	Source	P,a GPa	Noteb
Elastic Shock Waves
?	this work	0.35–0.62	P
?	Larson [1984]c	0.15–0.30	P
?	Larson [1984]c	0.16–0.19	S
inline equation	Gaffney and Smith [1994]	0.05–0.11	P
inline equation	Davies and Smith [1994]	0.05–0.23	P
 
Deformation Shock Waves
?	this work	0.37–5.32	P
?	Anderson [1968]	3.55–30.10	P
inline equation	Anderson [1968]	18.00–27.40	S
inline equation	Gaffney [1973]	0.46–0.85	P
?	Bakanova et al. [1976]	3.43–50.30	P
inline equation	Gaffney and Ahrens [1980]	1.91	P
inline equation	Larson [1984]c	0.42–3.56	P
?	Larson [1984]c	0.26–0.31	S
inline equation	Gaffney and Smith [1994]	0.68–2.92	P
inline equation	Davies and Smith [1994]	0.36–4.45	P
aElastic shock amplitudes are principal stress; deformation shock amplitudes are pressure.
bP, polycrystalline ice sample; S, single crystal ice sample.
cIncludes revised analysis of data from Larson et al. [1973].