Geomorphology Course (Geo 301)

Through the study of this course, the students' experience in defining, understanding and studying the formation of various topographical phenomena is crystallized, focusing on the role of the rapid and slow internal and climatic geomorphological processes of the globe over geological time, and knowing the relationship to the extent to which these topographical phenomena are particularly affected with the rock, mineral and chemical structures of the various rock structures (the system of layers and their placement, such as that hard layers alternate with soft ones, and the layers may be horizontal, oblique, twisted or cracked, and other characteristics), and the various processes formed of terrain, including erosion, sedimentation, tectonic activity, and weathering. Erosion is the process of minimized the earth’s elevation of rocks and soil through the action of water, wind, or ice. And through the earths internal processes (Folding. Faults, Volcanoes, earthquakes, … etc.). The movement and creep of soil and rocks masses, land slides, the formation of river basins and alluvium deposits, formation sea coastal shore and ports, karst topography forms in desert environments, and the assessment of natural hazards by understanding the geomorphology of the region, geologists can predict the risks of natural hazards such as landslides, floods and earthquakes.

Therefore, by studying the formation and change of the topography of the Earth's surface, from the smallest grains of sand to the largest mountain ranges, we can learn about the history of the formation of the Earth and the potential impact of human activity on it, and therefore we can:

1. Understand the internal and external operations and processes in/on the earth:

One of the primary benefits of studying geomorphology is gaining a deeper understanding of the processes that make up the Earth's surface. For example, by studying the way rivers erode and sediment deposition, geologists can gain insight into how landscapes change over time. This information can be used to predict the impact of natural disasters, such as floods and landslides, as well as to understand the impact of human activity on the environment.

2. Identification of natural resources:

By studying the method of sediment deposition in the river delta, we as geologists can determine where oil and gas can be found. Similarly, by studying the way glaciers erode rocks, geologists can identify areas where valuable minerals may exist. Understanding the geomorphology of an area can be critical to identifying and exploiting natural resources.

3. Prediction and forecasting of the Natural disaster :

Another important application of geomorphology is the prediction of natural disasters. By studying the way rivers erode and sediment deposition.

Geologists can predict where flooding and where landslides are likely to occur. This information can be used to help prepare and reduce various geological hazards and deal with them in advance.

4. Environmental protection:

By understanding the way natural terrain changes over time, geologists can identify areas that are particularly vulnerable to erosion and other forms of environmental damage. This information can be used to develop strategies to protect these areas and minimize the impact of human activity on the environment.

In general, geomorphology is an important part of the earth sciences. It helps us understand the internal and external processes of the globe and the formation of its topography, identify natural resources, predict natural disasters, and protect the environment. As we can get.