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Hack argued that landscape forms reflect a continuous balance between local tectonic uplift rates and the resistance of underlying bedrock to climate-driven erosion.

: Research published in the Geological Society of America Bulletin suggests that these surfaces are remnants of late Cenozoic geomorphology. They were formed through a combination of "aggradational" (building up of sediment) and "degradational" (eroding away) processes over at least 19 million years. matureland

By analyzing the steepness of river channels in a mature terrain using digital elevation models (DEMs), geologists can calculate how fast a mountain range is growing and identify hidden fault lines. Conclusion Hack argued that landscape forms reflect a continuous

[ Youthful Stage ] ----> [ MATURELAND ] ----> [ Old Age / Peneplain ] - Steep V-Valleys - U-Shaped/Broad Valleys - Near Sea-Level Plains - Rapid Downcutting - Lateral Erosion Peak - Minimal Relief - Unintegrated Streams - Maximum Drainage Network - Monadnocks / Residuals 1. The Youthful Stage By analyzing the steepness of river channels in

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