The development of grass fires originating from both point and line ig
nitions and burning in both open grasslands and woodlands with a grass
y understorey was studied using 487 periods of fire spread and associa
ted fuel, weather and fire-shape observations. The largest fires trave
lled more than 1000 m from the origin and the fastest 2-minute spread
rate was over 2 m s(-1). Given continuous fuel of uniform moisture con
tent, the rate of forward spread was related to both the wind speed an
d the width of the head fire measured normal to the direction of fire
travel. The head fire width required to achieve the potential quasi-st
eady rate of forward spread for the prevailing conditions increased wi
th increasing wind speeds. These findings have important implications
for relating small-scale field or laboratory measurements of fire spre
ad to predictions of wildfire spread. The time taken to reach the pote
ntial quasi-steady rate of spread at any wind speed was highly variabl
e. This time was strongly influenced by the frequency of changes in wi
nd direction and the rate of development of a wide head fire.