The document discusses how landforms are dynamic and change over time due to natural and human-caused processes. It analyzes data from micro-erosion meters that measured the lowering of rock surfaces over periods ranging from 2 to 32 years in various locations in Australia. The results showed that rates of lowering varied significantly between different landforms and were influenced by climate, with tropical karst lowering faster than sub-alpine karst. Individual landforms like karst streams could lower by over 2 meters in 1000 years. These findings provide context for geomorphological processes and identifying areas with high rates of change, with implications for understanding geoheritage and informing land management.