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
: 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.
Identifying an ancient surface requires distinguishing it from modern landforms and recognizing it as a "horizon of demonstrable antiquity". Recognition often relies on several key indicators:
Palaeosurfaces: Recognition, — Reconstruction And...
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
: 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. Palaeosurfaces: Recognition, Reconstruction and...
Identifying an ancient surface requires distinguishing it from modern landforms and recognizing it as a "horizon of demonstrable antiquity". Recognition often relies on several key indicators: The study of —ancient landscapes preserved within the