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What is the definition of geomorphology?

Geomorphology is the study of the origin, evolution, form, and distribution of landforms. It encompasses the processes that shape the Earth's surface, both physical and chemical, as well as the interactions between these processes and the resulting landforms.

Key aspects of geomorphology include:

* Landform analysis: Identifying and describing the characteristics of landforms, such as mountains, valleys, rivers, and coastlines.

* Process understanding: Investigating the processes that create, modify, and destroy landforms, including:

* Weathering: The breakdown of rocks and minerals.

* Erosion: The transportation of weathered material by wind, water, or ice.

* Deposition: The accumulation of eroded material.

* Tectonics: The movement of Earth's plates, which can uplift or depress landmasses.

* Volcanism: The eruption of molten rock, which can create new landforms.

* Geomorphological mapping: Creating maps that depict the distribution and characteristics of landforms.

* Landform evolution: Studying the changes in landforms over time, including their origins, development, and eventual destruction.

* Applications: Geomorphology has important applications in:

* Environmental management: Understanding and mitigating the impacts of natural hazards such as landslides and floods.

* Resource management: Identifying and assessing natural resources, such as groundwater and mineral deposits.

* Urban planning: Planning for sustainable development by understanding the geomorphological constraints and opportunities of a site.

In essence, geomorphology is a multidisciplinary field that seeks to unravel the intricate relationship between Earth's surface processes and the landscape we see today.

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