Free Geomorphology Essays and Papers

the book “Process Geomorphology” which become a must text book in geomorphic science. Most of his work related to paleoenvironmental and paleocimate reconstruction. Albert Lincoln Washburn His contribution on the book of “Periglacier Processes and Environments”, a standard text book on periglacier geomorphology, become wide acceptance among students and researchers who are interested in the area of high altitude and latitude environment, ecology, and environmental geomorphology. Most his research

Geographical processes can result in the creating of magnificent landscapes that one would expect to see in a sci-fi movie or read of in a fairy tale. A wonderful example of such a natural creation is the complex yet intriguing region of Cappadocia, Turkey. It is riddled with bizarre sites such as mushroom rocks, pillars and the tunnels that were once the largest underground city. Nature has shaped and allowed humans to shape this area into a natural and historical landmark. This essay will examine

Colorado Springs, Colorado. U.S. geological Survey Open File Report 2012-1158, 8p. http://pubs.usgs.gov/of/2012/1158/ Woods, S., Birkas, A., & Ahl, R. (2007). Spatial variability of soil hydrophobicity after wildfires in Montana and Colorado. Geomorphology, 86, 465-479. doi: 10.1016/j.geomorph.2006.09.015

The Concept of Equilibrium in Geomorphology INTRODUCTION The concept of equilibrium in geomorphology as a theory to explain landform evolution was first tabled by American geologist Grove Karl Gilbert. He was born on May 6, 1843 in Rochester, New York, United States of America. (Pyne &Stephen,1980) He was also one of the founders of the modern study of geomorphology. Howard,1988 said “Gilbert’s concept of equilibrium is also known as the principle of least force or Gilbert’s theory” (Howard,1988)

INTRODUCTION: Tectonic geomorphology is defined as the study of landforms produced by tectonic processes, or the application of geomorphic principles to the solution of tectonic problems (Keller, E.A. and Pinter N. 1996). Geological structure plays a crucial role in determining a wide field of relief forms, even in areas where exogenetic factors are regarded as the dominant ones in the landscape (Ahnert 1998; Bloom 1998; Ritter et al. 2002). In recent years Digital Elevation Model (DEM) data and

integration of geomorphology and pedology. London: George Allen and Unwin Limited. Schaetzl, R. and Anderson, S. 2005. Soils: Genesis and Geomorphology. Cambridge: Cambridge University Press. Waugh, D. 2009. Geography: An integrated approach. London: Nelson Thornes. Young, A. 1976. Tropical soils and soil survey. Cambridge: Cambridge University Press. Unknown Author (n.d). Slopes. [Online]Available:http://sageography.myschoolstuff.co.za/geogwiki/grade-11-caps/grade-11-caps-geomorphology/slopes/ [Accessed

Fundamentals of Soil science, John Wiley and Sons • Knapp B.J.1979. Soil Processes, George Allen & Unwin • Peter W. Birkeland. (1999) Soils and Geomorphology, Oxford University Press • Schaetzl, R. and Anderson, S. 2005. Soils: Genesis and Geomorphology, Cambridge University Press. • Weyman D. And Weyman V.1977. Landscape Processes: An introduction to Geomorphology, George Allen & Unwin

1. INTRODUCTION 1.1 Introduction “Anyone who can solve the problems of water will be worthy of two Nobel Prizes - one for Peace and one for Science”, stated by John F. Kennedy. Since the beginning of civilization, mankind has faced tribulations allied with river and its flow. With increase in utilization of water resources; flow in river channels are gaining significant importance among the research scholars. More and more complicated problems are encountered due to multipurpose use of alluvial

Describe and explain the changes that occur in a river channel as it moves from source to mouth. All rivers have an upper, middle and lower course. The long profile of a river is basically the changes in gradient at these different stages in the river, every river is trying to achieve a smooth, concave, long profile. The river begging in the upper course, normally in the hills and mountains. Here the river is smaller, the flow is fast and load and water volume are slow. The river erodes

Drainage Density and Stream Order in a Drainage Basin Drainage Density represents an approach to the quantitative analysis of drainage basin. It is the average length of channel per unit area of the drainage basin. It is calculated as shown below. Drainage density is a qualitative analysis of the areal properties of a river basin . Drainage density is useful as a measure of frequency and spacing of streams within the drainage basin. It also helps to determine the texture of dissection

The Philippines, consisting of 7,100 islands, is considered as one of the megadiverse country all over the world. Not only that it has rich biological component, it also has exemplary landscapes like mountains, hills, valleys, falls and the likes. One of the most important landscapes that the Philippines possesses is the watershed. Watershed, as defined in the Revised Forestry Code (PD 705), is a land area drained by a stream or fixed body of water and tributaries having a common outlet for surface

Write-up on Water Forces Day 1.)     There seemed to be quite a difference in the flow patterns between land with a small amount of slope and land with a steep slope. It seemed that when we would run the water down a small amount of slope the water would barely run anywhere and would almost just puddle up and not do much. However, with a steeper slope the water would run a lot more quickly and would form a stream down the sand into the runoff container. It would form accurately and you could definitely

part of Kumaun Himalaya, Current Science, 58(9), 486-491. Vanacker, V., Molina, A., Govers, G., Poesen, J. & Deckers, J., 2007. Spatial variation of sediment concentrations in a tropical Andean river system: The Paute river, southern Ecuador. Geomorphology, 87, 53-67. S. Rai, S,P. (1993). Response of Hydrologic Cycle to Environmental

A Study of the Changes in River Processes This is a study of the changes in river processes along the long profile of a river. To study this we will use a sample river. The river the study will be based on Loughton Brook, which is a river situated in Epping Forest in Essex and is also a tributary of the river Thames. A journey will be made to the river and measurements will be made at three different sites. The measurements that were taken will be studied so conclusions can be made about

Coastal Landforms and Features Related to the Rock Type of the Area Coastal landforms and features are related to the rock type (geology) of the area. To collect information for hypothesis1 we visited a number of places. These are all recorded by number on the geological map of the Isle of Purbeck. This also served as a location map (see M1 for details). * Man O War Cove * Lulworth Cove * North Swanage Bay * South Swanage Bay * Redend point * North Studland Beach * South

The Physical Characteristics of a River Introduction: River Features are elements of the landscape produced by fluvial processes-that is, the action of running water as it flows through the channels forming the drainage network of a river basin, eroding, transporting, and depositing sediment. (Source from Microsoft Encarta Encyclopedia 2001) A useful way to study a river is to look at its long profile and its cross sectional profile. The long profile of a river is a section drawn along

The precise and depictive accumulation of a stream flow data is vital in illustrating the water resources of a region. Hydrometric gauging stations are locations containing tools and equipment used to calculate the flow of water in rivers, lakes, canals and streams. The aim of this assignment is to develop my understanding of stream power and specific stream power through my individual critical assessment of the class stream power exercise results. Stream power is a criterion that measures the amount

There are many definitions that refer to the term geography. You can take the technical term straight from a geography textbook that says, “Physical geography is the study of spatial distributions of phenomena across the landscape, processes that created and changed those distributions, and implications for those distributions on people.” While physical geography refers to the geography of the land, urban geography refers to the geography of the city. By definition urban geography is, “the sub-discipline

‘Ultimately, our ties to the landscape shape our identity’ STATEMENT OF INTENTION: I have chosen to response to the prompt ‘Ultimately, our ties to the landscape shape our identity’ in a creative mode in the form of a regular column in Sunday Style magazine called ‘Literary Expeditions’. The column combines historical, literary and travel-related information in describing the narrator’s experience in returning to the historical village of Walhalla to explore her family history. The persona of Helen

Rivers constitute a major natural phenomena found on the surface of the earth. They have unique patterns and systems that perfectly fit in the geographical grid. One can establish the facts behind the formation of rivers and the important part they play in the ecosystem by carefully studying their features. However, the topic needs more research to know the reasons behind the uniqueness portrayed by each river. As the river flows, it cuts rocks which it carries them down its course and grinds them