climatic morphogenesis

Climatic morphogenesis is a concept in geomorphology that relates climate, the processes that shape the Earth's surface, and the resulting landforms. The idea, first proposed by Julius Büdel in 1945, suggests that specific climatic conditions lead to dominant geomorphic processes that create characteristic landforms. Proponents argue that climate is more influential than rock type in shaping landforms because a rock's resistance to erosion depends on the climate it's exposed to. However, modern understanding indicates that landforms result from the interaction of climate, rock type, and physical processes.1

The concept of morphogenetic areas, developed by Büdel and others, defines a region where a particular set of landforms is produced under a specific climate. This understanding has been influenced by evidence of significant shifts between arid and humid climates across continents, highlighting the dynamic nature of these geomorphic systems.2