In the low-pressure, high-temperature metamorphic rocks of western Maine, USA, staurolite porphyroblasts grew at c. 400 Ma, very late during the regional orogenesis. These porphyroblasts, which preserve straight inclusion trails with small thin-section-scale variation in pitch, were subsequently involved in the strain and metamorphic aureole of the c. 370 Ma Mooselookmeguntic pluton. The aureole shows a progressive fabric intensity gradient from effectively zero emplacement-related deformation at the outer edge of the aureole $2900 m (map distance) from the pluton margin to the development of a pervasive emplacement-related foliation adjacent to the pluton. The development of this pervasive foliation spanned all stages of crenulation cleavage development, which are preserved at different distances from the pluton. The spread of inclusion-trail pitches in the staurolite porphyroblasts, as measured in two-dimensional (2-D) thin sections, increases nonlinearly from $16°to 75°with increasing strain in the aureole. These data provide clear evidence for rotation of the staurolite porphyroblasts relative to one another and to the developing crenulation cleavage. The data spread is qualitatively modelled for both pure and simple shear, and both solutions match the data reasonably well. The spread of inclusion-trail orientations (40-75°) in the moderately to highly strained rocks is similar to the spread reported in several previous studies. We consider it likely that the sample-scale spread in these previous studies is also the result of porphyroblast rotation relative to one another. However, the average inclusion-trail orientation for a single sample may, in at least some instances, reflect the original orientation of the overgrown foliation.