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Fluvial process and related landforms
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INTRODUCTION
This essay looks at the fluvial processes.
Fluvial comes from the Latin word fluvius which means river (Soanes) (CCSU). Hence the term is used to describe those processes involving rivers (fluvial processes) and their physical interaction interactions.
Basically there are three (3) fluvial processes:
1. Erosion
2. (Sediment) Transportation/Motion of Sediment
3. Deposition (University of California, 2008). Erosion
Erosion is the process by which the products of weathering are transported, in this case by water or rather streams or rivers (Sager, Ramsey, Phillips, & Watenpaugh, 1998).
In general, most of the landscape erosion that occurs in the world is due to water and the flow thereof (The Authors of Encyclopaedia Britannica).
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Hydraulic action
IV. Solution or corrosion (Waugh, 1995).
Erosion occurs in three (3) basic directions:
I. Head-ward erosion
II. Vertical erosion/downcutting
III. Lateral erosion
Head-ward Erosion
This occurs at the source of the stream (this would be first order streams according to Strahler’s method of stream ordering) where weathered materials like rocks are brought by overland flow and down the slope (slopes are steep in first order streams). This causes the source stream to erode backward or further inward thereby lengthening the river.
Vertical Erosion/Downcutting
This refers to the riverbed (the bottom of the river) being eroded and occurs on the river bed of the upper course of the stream. It results in the river becoming deeper.
Lateral Erosion
As the name suggests (i.e. lateral) this type of erosion occurs at the sides or banks of the river thereby widening the river. This mostly occurs at the banks of the middle and lower courses.
As the water passes through the channel, the water obviously wields pressure on the river bank resulting in undercuts which widens cracks, if they are present.
Some factors which affect erosion are the nature of the load (greater load weight results in increased erosion), amount of load, discharge and velocity (larger the load, high velocity and discharge all result in an increased
An increase in pebble roundness in the direction of long shore drift. The process of attrition will erode the pebbles. c) A decrease of pebble size in the direction of long shore drift, again attrition is involved. d) Undercutting (active erosion of the cliffs at one end of the bay).
Investigating the Geographical Processes that are Affecting the Physical and Built Coastal Environment There are three geographical processes that are affecting the physical and built coastal environment, they are; erosion, deposition, and transportation. Erosion is the group of natural processes, including weathering, dissolution, abrasion, corrosion, and transportation, by which material is worn away from the earth’s surface, this is mainly caused by wind, running water, and waves breaking on the coast. Deposition is the depositing something or the laying down of matter by a natural process. Transportation is when sand is moved along the coast by long shore drift. At North Cronulla beach erosion is evident.
3. 120 MY : Continued erosion of the land as it is slowly uplifted and
Sedimentary rock from the older Silurian Period is further from the river banks (Geological map of Victoria, 1973). Mudstone, inter-bedded shale and greywacke depositions indicate the Maribyrnong River may have previously taken a different shape, and younger sediments have replaced the older sediments in more recent geological periods.
As can be seen from the photo( Image 1), looking downstream, there were steep sections of bank where it appeared the erosive forces of the river when high have cause part of the bank to fall away leaving steep about 1m high drops on the bank with exposed rocky soil visible. The phenomenon also illustrate that it is an alluvial landforms, which will find erosional feature from fluvial
There are three clear landslides; the southwest landslide is stream-laid sand and gravel from the quaternary that was located on a steep slope resulting in gravity pulling sediments down the steep slope. The northeast landslide appears to be tuff sediments that have fallen upon biotite-quartz diorite rocks. The northwestern landslide is the largest of the landslides. The landslide occurred just south of the creek; erosion must have lowered the creeks elevation creating a steep decline resulting in Bena gravel to fall.
Periods that the folding occurred in which formed the outlines of the basin as it
The negative consequences of erosion were virtually non-existent because there was no infrastructure on the shore of the beach. As shown in the image, the sand was expansive and naturally progressed into
affects the ecosystem. The land's incline prevents some areas to receive and maintain a water
How does the smooth mountain rock surface type affect the amount of runoff? Speculate why this happens.
...ansportation in the natural direction of the littoral drift. This particular jetty is responsible for the accretion of sediment immediately adjacent to the South Jetty (Kraus).
Erosion is when the elements such as wind, water, and ice remove pieces of land. (“What is Coastal Erosion?”) Coastal Erosion takes place when destructive waves wear parts of the coast away. Four ways in which this takes place are corrasion/abrasion, hydraulic action, attrition, and corrosion/solution. (“Internet Geography”) Corrasion/abrasion is when materials are hurled at the base of cliffs through waves. Hydraulic action is when waves hit the base of a cliff and air is compacted, when the wave leaves air is rushed out and often this causes the material to break. Attrition is when the waves cause rocks and pebbles to smash into each other and eventually break into pieces. Finally, Corrosion/solution is when certain types of cliff erode from the result of acids in the sea. (“Internet Geography”) Coastal Erosion is the natural process of taking land away permanently from one place to put it somewhere else. (“What is Coastal Erosion?”) Eroding coastlines are an abundant and important topic because it can change people’s surroundings in a negative way. I would like to address the questions surrounding Coastal Erosion.
is being eroded by the sea so that cliffs, up to 20 metres high rise
If the gradient is steep (like the example on the right) then this can indicate that the amount of rainfall becoming overland flow is very high, the result of this is that all the water reaches the river very quickly and all in a short period of time, this gives the immediate steep ascending limb on the hydrograph. Reasons for large amounts of rainfall becoming overland flow can be little vegetation and maybe impermeable rock below the surface. Being impermeable rock, the water cannot infiltrate through this and become ground water, instead it flows over the ground to the river. Urban development and agricultural practices contribute to overland flow.
the the change in sea level is due to a change in the level of land