A model of the cascading acceleration of quasi-thermal electrons by MHD tur
bulence in solar flares is considered. Analysis shows that fast magnetoacou
stic wave modes with large wavenumhers (> 3 x 10(-8) cm(-1)) strongly damp
due to ion viscosity for both preflare and flare conditions. The viscous da
mping of fast magnetoacoustic wave modes is 10 - 100 times more efficient t
han Fermi or transit-time electron acceleration.