Cr-bearing staurolite in a kyanite-zone amphibolite-facies rock of bulk composition gradational between a metapelite and a metaquartzite , with abundant kyanite and almandine garnet, in a matrix of predominately quartz and some Cr-bearing muscovite ("fuchsite") and "oligoclase" (sodic plagioclase: Ab88), accompanied by minor biotite, oxides, and apatite. In the absence of independently-determined Fe3+/∑Fe or H2O, all measured Fe is assumed to be Fe2+, then with sufficient calculated H added to achieve charge balance; that the stoichiometry is good and the analytical total is near 100 wt% suggests the FeO* and H2O assumptions are likely reasonable.