Geomorphology IAG Paris

Geomorphology is nothing but the study of landforms, their processes, form and the sediments at the surface of the planets. Initially, the landforms are produced by the deposition or the erosion. The real fact is that both rock and the sediments are worn by a unique process known to be the earth surface process and then it is transported to the different locations. There is a list of different climatic environments which are produced by the different suites of the landforms. The sand dunes and the ergs ate the different landforms of the deserts which is totally a different one from the periglacial features and they are found in the polar and sub-polar regions. In order to get a deeper knowledge and for a better understanding the Geomorphologists maps are the best ones.

In the present era, the earth surface processes are processing and forming the landforms, changing the landscape etc. Most of the geomorphic processes operate at the slower rate. The dangerous landslide or the flood causes the rapid change to the environment and sometimes it threatens the human beings also. Many geological hazards such as the volcanic eruptions, earthquakes, tsunamis including the landslides fall within the factor of the Geomorphologists. The advancements in the remote sensing techniques have benefitted the Geomorphologists in many ways from the ancient days and thus to get deeper knowledge about the global distributions using the uber for x.

Geomorphology is an important study in order to understand the geomorphologic process of the various environments, to detect the natural hazards such as the earthquake, flooding, tsunami, and volcanism etc. Finally in order to identify the various landform features including the landscapes this geomorphology is more important one. There are several agents for the geomorphologic process such as the river activities, wind activities, glacier activities and the wave activities. Here three types of activities are done such as the erosion activities, transportation, and the depositional activities.

The geomorphic process is divided into two types such as the terrestrial process and the extraterrestrial process. The terrestrial process is again differentiated into two types such as the exogenous process and the endogenous Uber app script process. The Endogenic process is originated in the interior of the earth. Here there are sudden rapid movements such as the earthquake, faulting, and diastrophism. The exogenic process is originated on the surface of the earth and also it causes the slow movements such as the erosion and the depositional process. Weathering, Erosion, Transportation, Aggradations and the mass movement are the different types of the exogenous process. Denudation is nothing but the things to be exposed; here the rocks presented on the earth’s surface are broken into the pieces through the external physical forces. This entire work is performed through three processes such as the weathering, erosion, and transportation.

The geomorphologic resources include both the raw materials and the landforms. Both these forms are used to the human beings which are totally depending on the economic, social and the technological factors. This gigantic process is involved in the deeper investigation in the evolution of the landforms and finally targeting on the mountain hill slopes, rivers, glaciers including the coasts. The Volcanic process is the complex one and it results in the larger variations in the landforms, deposits, and series of effects on the surrounding environment. It plays an important role in the present era and at the same time, it can entirely alter the social evolution. It is an important factor in the climate change in both the ways of locally and globally. There is a list of the classical studies in the geomorphology such as the morphometry, morphological evolution including the volcanic edifices.


There are several quantitative techniques such as the DEM analysis, remote sensing, experimental approach, statistical analysis including the dating methods in order to measure the timescales of the volcano growth including the degradation. Both the erosion and the aggradations processes are distributed by the volcanic eruptions. The modern techniques are used for the associated hazards which include the various volcanic processes for the eruption activity in the future. Apart from the geomorphology the other stratigraphy, sedimentology, geochronology and the physical volcanology are used as the tools for the reconstruction of the geomorphologic evolution of the volcanic areas.

Bio Geomorphology is one rapid development of the geomorphology which is focused on the living world such as the plants, animals, microbes including the geomorphic processes and the landforms. The technological developments have made everything easier in order to study the complicated interactions between the life and the geomorphology. Next, the fluvial geomorphology has changed and shown a lot of improvement long back. There is a list of topics covered here such as the sediment dynamics, network dynamics, catchment process, fluvial information system etc. This gigantic topic has a great influence in several areas such as the management of the natural resources, mitigation of the risks and the conservation of the natural systems etc. In the present era, there is much development concerned with the geomorphology of the dry lands. Especially the dating of dunes has changed the entire world. There is a list of the contribution that targets on the practical implications of the geomorphologic science and there is integration between the quantitative geomorphic systems. Both the applications of the Remote Sensing and the Geographical Information Systems are relatively new one in the long history of the Geomorphology. The real fact is that there is a great human adaptation to the geomorphic processes in the mountain areas.