Fig. 1. 3D in A large marine eosauropterygian reptile with affinities to nothosauroid diapsids from the Early Triassic of British Columbia, Canada

Fig. 1. 3D landscape images of Ganoid Ridge, Wapiti Lake area, British Columbia [downloaded from Google Earth Pro on October 3rd 2018; imagery Landsat/Copernicus (09/14/2011), ©2018 DigitalGlobe, ©2018 Province of British Columbia]. A. Overview of the complete Ganoid Ridge reversed). White letters indicate different cirques at Ganoid Ridge. The stippled white line indicates the trend of the major anticline in the area (adopted from Mutter 2004: fig. 1a and references therein). B. Close-up of the southeastern cirques of Ganoid Ridge seen from the North. The anticline is well visible in the grey sediments of the Permian Mowitch Formation in the E and D cirques, surrounded by the darker brownish colored sediments of the Sulphur Mountain Formation. C. Close-up of the fossil site 54°30'32" N; 120°41'24" W) indicated by the white star in the talus slop of the L cirque, seen from the Northeast. Note that well exposed layers in the E cirque can be traced into the L cirque, indicating a similar stratigraphic succession in both cirques. Abbreviations: MM, Meosin Mountain Member; MO, Mowitch Formation; P, Phroso Member, V, Vega Member.