Temporal and Spatial Variations in Rock Uplift From River‐Profile Inversions at the Central Anatolian Plateau Southern Margin

In geodynamically active areas, spatio-temporal variations in rock uplift can provide key insights into the processes responsible for evolution of topography. The Central Anatolian Plateau (CAP) southern margin experienced a rapid rock-uplift pulse with maximum rates 3.5 m/kyr during Quaternary, based on marine sediments dated to middle Pleistocene that are now located at 1,500 m.a.s.l. Fluvial landscapes record elements reflect temporal and spatial rates, such as normalized river steepness index, which is affected by rate, erodibility underlying rock, climate. Following calibration profiles an erosion coefficient value, be done using independent data (in our case, uplifted terraces sediments), inverted histories created them. Here, we demonstrate how it possible define history CAP quantitative analysis profiles.