Fig. 6From: Distribution, geometry, age and origin of overdeepened valleys and basins in the Alps and their forelandLongitudinal cross-section of the Inn Valley west of Innsbruck revealing the discrepancy between expected Quaternary infill deduced from seismic surveys and evidence of the counter-flush drilling of Wattens (brown layer, Weber et al. 1990) compared to the results of the spot-cored drilling of Kramsach (Gasser, pers. comm.)Back to article page