1. Davis – Geographical Cycle of Erosion (Time-Controlled Model) Proposed by: William Morris Davis Core Concept Davis proposed that landforms evolve through a sequential, time-dependent cycle following a single episode of rapid tectonic uplift . After uplift, erosion becomes the dominant geomorphic agent. Fundamental Assumptions Structure + Process + Time = Landscape form Uplift is rapid and followed by tectonic stability Denudation operates progressively through stages Landscape evolution is orderly and predictable Stages of the Cycle Youth Stage High relief and steep gradients Deep, narrow V-shaped valleys Active vertical erosion Presence of waterfalls and rapids Maturity Stage Maximum relief Valley widening through lateral erosion Well-developed drainage network Reduced interfluves Old Age Stage Low relief surface Extensive lateral erosion Broad floodplains Formation of a nearly level surface called a peneplain Key Terminologies Base level Graded river Peneplain Sequential develop...
Focused on advancing knowledge and expertise in Geography, GIS, Remote Sensing, Geographical Data Science, and Analysis, I am deeply committed to teaching and conducting research in these fields. With a keen interest in leveraging data-driven approaches for informed decision-making, I specialize in crafting maps that facilitate effective analysis and interpretation of spatial information. Assistant Professor Of Geography, PG and Research Department of Geography, Government College Chittur