Troodontid material from the Maastrichtian of North America is extremely rare, beyond isolated teeth from microvertebrate sites. Here we describe troodontid frontals from the early Maastrichtian Horseshoe Canyon Formation (Horsethief Member). The most complete specimen, TMP 1993.105.01, is notably foreshortened and robust when compared to numerous specimens referred to Troodon from the Dinosaur Park Formation, and exhibits several characteristics that distinguish it from other Late Cretaceous troodontids. Morphometric analyses reinforce shape differences between TMP 1993.105.01 and other North America troodontids, and show that proportional differences are independent of size. We therefore erect a new taxon, Albertavenator curriei gen. et. sp. nov., that is diagnosed by the following autapomorphies: 1) primary supraciliary foramen is truncated anteriorly by the lacrimal contact, 2) superficial (ectocranial) surface of the frontal proportionally shorter than all known troodontids, with a length to width ratio under 1.25, and 3) frontoparietal contact in which an enlarged lappet of the frontal extends medially to extensively overlap the lateral region of the anteromedial process of the parietal.