Van Kranendonk et al. (1994) and Van Kranendonk and Wardle (1994) mapped ultramafic lithologies that they associate with the Tasiuyak Gneiss and Noodleook Complex in the Lorière Lake (NTS sheet 24P10) and Ryans Bay (sheet 24P09) area. Mathieu et al. (2018) corroborate these observations in the Point Le Droit area (sheet 24P) and Grenfeld Sound area (sheet 25A). They also map websterites in rocks of the Killinek Suite and introduce the Lepers Suite to group ultramafic intrusions of the Burwell Lithotectonic Domain spatially associated with both metasedimentary rocks and gneiss and intrusions.

The Lepers Suite consists solely of a metamorphosed ultramafic intrusive rock unit. Samples show high magnetic susceptibility but the small size of intrusions, combined with a very wide mesh aeromagnetic survey, makes it impossible to separate this unit based on the geophysical survey (Geological Survey of Canada, 1985). However, rocks are easily visible in the field due to the whaleback appearance of outcrops, their dark brown patina and elephant skin texture. Some magmatic textures, such as cumulate horizons, are generally preserved despite deformation and metamorphism. Outcrops are homogeneous and only composed of olivine websterite and show magmatic bedding. Serpentine veins and magnetite ridges are frequently observed. Bands of olivine-relic cumulate are reported. The patina is dark brown and the rock is very dark green in fresh exposure.

Preserved primary phases are surrounded by a finer, even-grained matrix composed mostly of actinolite, clinopyroxene and orthopyroxene. Rocks are composed of actinolite (25-30%), orthopyroxene partially replaced by iddingsite and carbonates (20-50%), partially serpentinized olivine (5-30%), clinopyroxene (5-20%), magnetite (5-10%) and green (herspinitis) and locally brown (picotite) spinel. Orthopyroxene and clinopyroxene are medium to coarse grained with a finer granoblastic rim. They incorporate oxides in slats into the cleavage of the preserved core. Orthopyroxene and olivine are altered to iddingsite and serpentine, respectively, matted or in veins. Olivine is cracked and also forms coarse-grained zones. Opaque minerals are disseminated homogeneously. Foliation is marked by a slight preferential orientation of stocky actinolite.