The Himalayas and Other Peninsular Mountains
Unlike the stable and rigid Peninsular Block, the Himalayas and other Peninsular mountains possess a young, weak, and flexible geological structure. Consequently, they continue to undergo the interplay of exogenic and endogenic forces, leading to the formation of faults, folds, and thrust plains. Tectonic in origin, these mountains are characterized by fast-flowing rivers in their youthful stage, which dissect the terrain and carve out various landforms such as gorges, V-shaped valleys, rapids, and waterfalls. These features are indicative of the dynamic geological processes shaping the Himalayas and other mountainous regions.
Structure and Physiography| Chapter 2 Class 11 Geography Notes
Class 11 Geography Ch 2 Structure and Physiography Notes: In Class 11 Geography Chapter 2, we learn about the different shapes and features of the Earth’s surface. This includes things like mountains, plateaus, plains, and valleys. We examine how these features are formed over a long time by various natural processes like movement of the Earth’s crust, erosion, and deposition. By studying this chapter, we get to understand more about how the Earth’s surface changes and how it’s connected to geological processes.
The Structure and Physiography notes cover all the necessary topics that are extremely important for the examination 2024. It can save you time and will positively affect your results.