The dynamic brittle fracture of amorphous soda-lime glass and single-crysta
lline silicon was studied in a comparative experimental investigation. A po
tential drop technique was used to accurately determine the crack velocity.
A terminal crack velocity ve of about 50 % of the Rayleigh wave velocity v
(R) was determined for glass. The terminal crack velocity in single-crystal
line silicon is significantly higher, reaching about 0.85 v(R) = 3800 m/s.
Inspection of the fracture surface revealed significant differences between
the amorphous and the single-crystalline materials. A continuous increase
in the size of the characteristic features is typical for the transition fr
om mirror to mist and hackle regions of the fracture surface in glass. In c
ontrast, the onset of a rough, hackle-like region is clearly discontinuous
in silicon single crystals. Mirror-like flat and hackle regions may coexist
at the same location on the fracture surface.