Walther Penck, a German geologist saw landforms as the result of continuous interactions between internal (endogenetic) and external (exogenetic) forces. Unlike William Morris Davis, who believed in a time-dependent “cycle of erosion” (where landforms evolve in distinct stages over time), Penck focused on processes rather than time. He argued that landscapes do not follow a…
William Morris Davis, the father of geomorphology, introduced a fascinating theory—the Geographical Cycle of Erosion, also called the Cycle of Erosion. According to Davis landforms undergo sequential changes through time (passing through three stages of youth, mature and old). Over time, the battle between these two forces leads to a systematic transformation of landforms through…
Grove Karl Gilbert, an American geologist looked at landscapes not as fixed entities but as living, breathing systems shaped by an ongoing battle between forces. His theory of dynamic equilibrium explains how landforms evolve—not through a rigid cycle, but through a constant balancing act between driving forces and resisting forces. The Battle of Two Forces:…
Imagine you are standing on a vast mountain peak, looking at the world below. The towering Himalayas stretch into the distance, deep valleys cut through the earth, and winding rivers snake their way across the plains. Have these landscapes always been like this? Were the Himalayas always this tall? Did the rivers always carve these…
Today, when we study geomorphology, we rely on precise tools, satellite data, and theories of plate tectonics. But remember, this field didn’t emerge overnight. It evolved over centuries—from the philosophical speculations of ancient thinkers to scientific theories of geologists in the 18th and 19th centuries. Let’s trace this journey step by step. 🏺Ancient Period: The…
Imagine you are a traveler exploring the vast landscapes of Earth. As you move through different terrains, you notice some mountains standing tall and rigid, split apart by deep valleys, while others rise dramatically from volcanic eruptions. Some appear old and worn down, as if time itself has chipped away at them. These mountains, shaped…
The traditional concept of Geosynclines, which was initially proposed by theorists like Kober, explained mountain building as a result of the contraction of the Earth due to cooling. However, with the advent of Plate Tectonic Theory, this explanation was largely replaced by a more dynamic and scientifically accurate model. Let’s explore how Geosynclines fit into…
Imagine you are in a vast, ancient land, where the Earth itself is a living, breathing entity—but over time, it starts to shrink, like an old fruit losing its moisture. As this grand planet cools, its surface begins to crumple, much like a drying apple, creating the towering mountain ranges, deep ocean basins, and the…
Kober defined: According to Kober the whole process of mountain building passes through three closely linked stages (LOG):1️⃣ Lithogenesis – The formation of geosynclines.2️⃣ Orogenesis – The birth of mountains.3️⃣ Gliptogenesis – The aging and erosion of mountains. Now, let’s discuss them one by one: Stage 1: Lithogenesis Millions of years ago, the Earth was…
Think of a book that different authors have written over centuries. Some ideas remain unchanged, while others evolve as new evidence emerges. The concept of geosynclines is similar—various geographers have contributed their theories to explain how these long, narrow water depressions transform into majestic mountains. So, let’s take a journey through the minds of some…
