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In complicated terrains, groundwater modelers benefit from continuous high\u2010resolution geologic maps and their related hydrogeologic\u2010parameter estimates. The USGS and its partners have collaborated to use airborne geophysical surveys for near\u2010continuous coverage of areas of the North Platte River valley in western Nebraska. The survey objectives were to map the aquifers and bedrock topography of the area to help improve the understanding of groundwater\u2010surface\u2010water relationships, leading to improved water management decisions. Frequency\u2010domain heliborne electromagnetic surveys were completed, using a unique survey design to collect resistivity data that can be related to lithologic information to refine groundwater model inputs. To render the geophysical data useful to multidimensional groundwater models, numerical inversion is necessary to convert the measured data into a depth\u2010dependent subsurface resistivity model. This inverted model, in conjunction with sensitivity analysis, geological ground truth (boreholes and surface geology maps), and geological interpretation, is used to characterize hydrogeologic features. Interpreted two\u2010 and three\u2010dimensional data coverage provides the groundwater modeler with a high\u2010resolution hydrogeologic framework and a quantitative estimate of framework uncertainty. This method of creating hydrogeologic frameworks improved the understanding of flow path orientation by redefining the location of the paleochannels and associated bedrock highs. 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