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Résumé : Quantifying the balance between uplift and erosion is essential for understanding mountain landscape evolution, and river longitudinal profiles provide an effective archive of this process. Clarifying the uplift history of the Malá Fatra Mountains is key to constraining the Cenozoic tectonic evolution of the Western Carpathians in Central Europe. Here, we integrate the stream power incision model with linear river-profile inversion, catchment-wide denudation rates from in-situ cosmogenic ¹⁰Be, and χ-plot analyses to reconstruct the uplift history of the Malá Fatra Mountains, comprising the SW Lúčanská Fatra and NE Krivánska Fatra. Corrected ¹⁰Be-based denudation rates range from 49.6 ± 9.0 to 163.0 ± 13.1 m Myr⁻¹, with a mean of 94.8 ± 7.2 m Myr⁻¹, indicating low to moderate long-term erosion. Using a mean erosion coefficient of K = (1.27 ± 0.13) × 10⁻⁶ m⁰·¹ yr⁻¹, modeling results show that the Lúčanská Fatra experienced a rapid uplift (~0.13 mm yr⁻¹) between ~6.3–3.5 Ma, whereas the Krivánska Fatra underwent a similar uplift (~0.14 mm yr⁻¹) between ~2.85–0.65 Ma. Knickpoint residuals yield ages consistent with these simulated phases, confirming the robustness of the approach. Our results reveal asynchronous uplift of the Malá Fatra Mountains since the Late Miocene, with an earlier phase linked to post-orogenic collapse near volcanic and attenuated lithosphere, and a later phase attributed to far-field compression from Pannonian Basin inversion. This integrated cosmogenic–geomorphic framework provides a transferable methodology for quantifying uplift histories and erosion in orogenic landscapes.