Two new geodetic measurements of strain accumulation in the state of Washington for the interval 1972--1979 are reported. Near Seattle the average principal strain rates are 0.07¿0.03 μstrain/yr N19 ¿W and -0.13 ¿ 0.02 μstrain/yr N71 ¿E, and near Richland (south central Washington) the average principal strain rates are -0.02 ¿ 0.01 μstrain/yr N36 ¿W and -0.04 ¿ 0.01 μstrain/yr N54 ¿E. Extension is taken as positive, and the uncertainties quoted are standard deviations. A measurement of shear strain accumulation (dilatation not determined) in the epoch 1914--1966 along the north coast of Vancouver Island by the Geodetic Survey of Canada indicates a marginally significant accumulation of right-lateral shear (0.06 ¿ 0.03 μrad/yr) across the plate boundary (N40 ¿W strike). Although there are significant differences in detail, these strain measurements are roughly consistent with a crude dislocation model that represents subduction of the Juan de Fuca plate. The observed accumulation of strain implies that large, shallow, thrust earthquakes should be expected off the coast of Washington and British Columbia. However, this conclusion is not easily reconciled with either observation of elevation change along the Washington coast or the focal mechanism solutions for shallow earthquakes in Washington.