We calculate spatially and temporally periodic standing waves using a
spectral boundary integral method combined with Newton iteration. When
surface tension is neglected, the non-monotonic behaviour of global w
ave properties agrees with previous computations by Mercer & Roberts (
1992). New accurate results near the limiting form of gravity waves ar
e obtained by using a non-uniform node distribution. It is shown that
the crest angle is smaller than 90 degrees at the largest calculated c
rest curvature. When a small amount of surface tension is included, th
e crest form is changed significantly. It is necessary to include surf
ace tension to numerically reproduce the steep standing waves in Taylo
r's (1953) experiments. Faraday-wave experiments in a large-aspect-rat
io rectangular container agree with our computations. This is the firs
t time such high-amplitude, periodic waves appear to have been observe
d in laboratory conditions. Ripple formation and temporal symmetry bre
aking in the experiments are discussed.