Reference

Morphostructural knots are significant in the study of natural events due to their relationship with seismic activity and the stability of geological structures. They consist of smaller, more mobile blocks compared to larger, more stable ones, which can lead to increased seismic activity and natural hazards such as earthquakes. This is supported by research indicating that earthquakes in the vicinity of such knots can be explained by the movement of these macroblocks. Furthermore, morphostructural analysis can help predict the location of natural resources, such as oil and gas, by understanding the zoning and movement of these knots. The study of these knots is therefore crucial for understanding and predicting natural events and their impacts on human society and the environment. For more detailed information, refer to the studies on morphotectonics of various regions like the Iberian Peninsula and Hispaniola, which further elaborate on the significance of these knots in understanding natural events [1][2][3].