In order to clarify common assumptions on the form of energy and momentum i
n elasticity, a generalized conservation format is proposed for finite elas
ticity, in which total energy and momentum are not specified a priori. Velo
city, stress, and total energy are assumed to depend constitutively on defo
rmation gradient and momentum in a manner restricted by a dissipation princ
iple and certain mild invariance requirements. Under these assumptions, rep
resentations are obtained for energy and momentum, demonstrating that (i) t
he total energy splits into separate internal and kinetic contributions, an
d (ii) the momentum is linear in the velocity. It is further shown that, if
the stress response is strongly elliptic, the classical specifications for
kinetic energy and momentum are sufficient to give elasticity the standard
format of a quasilinear hyperbolic system.