: For more recent Holocene surfaces, researchers use coring and electrical resistivity tomography to identify flood-safe locations, such as Pleistocene sand mounds (Geziras), that influenced human settlement patterns.
: Features such as lateritization, bauxitization, and palaeokarstification provide chemical evidence of past weathering processes acting on a surface. Palaeosurfaces: Recognition, Reconstruction and...
: Trace fossils, such as dinosaur tracks on a bedding plane , can confirm the preservation of primary palaeotopography and indicate the biological activity present at the time. Reconstruction Methods : For more recent Holocene surfaces, researchers use
: High-resolution Digital Elevation Models (DEMs) can be constructed by integrating LiDAR data with geological and historical information to map past valley floors and floodplains. : For more recent Holocene surfaces
The study of —ancient landscapes preserved within the rock record—serves as a critical bridge between geology and geomorphology. These surfaces provide a spatial and temporal framework for understanding how tectonic processes and environmental changes have shaped the Earth's face over millions of years. Recognition of Palaeosurfaces
Reconstructing these ancient landscapes involves piecing together fragmented geological data to build a coherent model of the past topography:
: In volcanic terrains, monogenetic volcanic landforms can act as reference points for reconstructing syn-volcanic surfaces , allowing researchers to calculate rock uplift rates and vertical motion history.