Introduction:
The study of landforms and processes is a multidisciplinary field that involves the examination of various landforms and the processes that shape them. It encompasses both global and regional examples, including Indian examples. In this response, we will explain in detail how the study of landforms and processes incorporates Indian examples along with global examples.

Global Examples:
The study of landforms and processes is based on global examples to understand the Earth's surface and its evolution over time. It includes the examination of landforms such as mountains, valleys, plains, plateaus, and coastal features found across different continents. The processes that shape these landforms, such as erosion, weathering, tectonic activity, and deposition, are also analyzed on a global scale. Global examples provide a broader perspective and help in understanding the fundamental principles and mechanisms involved in landform development.

Indian Examples:
The study of landforms and processes also includes Indian examples to understand the unique landforms and processes specific to the Indian subcontinent. India is a geographically diverse country with a wide range of landforms shaped by various geological and geomorphological processes. Some prominent Indian landforms include:

1. The Himalayan Mountain Range: The Himalayas, located in northern India, are the youngest and highest mountain range in the world. They are a result of the collision between the Indian and Eurasian tectonic plates. The study of the Himalayas provides insights into the processes of mountain building, glaciation, and erosion.

2. The Western Ghats and Eastern Ghats: These mountain ranges run parallel to the western and eastern coasts of India, respectively. They are older than the Himalayas and have been shaped by weathering, erosion, and tectonic forces. The Western Ghats are known for their rich biodiversity and are recognized as a UNESCO World Heritage Site.

3. The Deccan Plateau: The Deccan Plateau covers a significant portion of peninsular India. It is a volcanic plateau formed by extensive volcanic activity in the past. The study of the Deccan Plateau helps in understanding volcanic processes and their impact on landform development.

4. The Ganges-Brahmaputra Delta: This delta is formed by the deposition of sediment carried by the Ganges and Brahmaputra rivers. It is the largest delta in the world and provides insights into the processes of riverine sedimentation and coastal landform evolution.

5. The Thar Desert: Located in northwest India, the Thar Desert is an arid region characterized by sand dunes and low rainfall. The study of the Thar Desert focuses on aeolian processes, such as wind erosion and deposition, and their influence on landform development.

Conclusion:
The study of landforms and processes incorporates both global and Indian examples. While global examples provide a broader understanding of landform development, Indian examples offer insights into the unique landforms and processes specific to the Indian subcontinent. By examining landforms and processes at various scales, researchers can gain a comprehensive understanding of the Earth's surface and its dynamic evolution.