Fig. 1
From: Subaqueous evidence of the last glacial maximum and its termination in southern Patagonia
Topographic and satellite (inset) map of the study area showing the location of the seismic reflection data used for this study (all, solid gray lines; shown, solid black lines). Solid, colored lines: mapped and dated moraines with ages taken from original studies27,29. Dashed, colored lines: subaqueous moraines and glacial landforms mapped by this study. Lake bathymetry modeled from seismic data from this study, displayed with 100 m contours. White circles and black labels along the seismic profiles indicate distance in km. The hillshade basemap was generated using Shuttle Radar Topography Mission (SRTM) Digital Elevation Model (DEM) data67,68 (Void Filled, 3-arc second global) in ESRI ArcGIS Pro available from https://www.esri.com and used herein under license. The satellite map was generated using Maxar, Earthstar Geographics imagery in ESRI ArcGIS Pro available from https://www.esri.com and used herein under license.
