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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).
Yes this feature is the result of erosion and depositional processes however, it is not associated with the current water course. This feature may be the result of a Gilbert type delta that once occupied this area. Gilbert type deltas have three main components; topsets, foresets and bottomsets. Topsets are fluvial sediments (primarily sandur deposits) that were deposited on the subaerial delta surface. Erosive events occurring on the upper forslope can result in downslope channels and chutes. These features are then eroded by either strong currents or by debris flow resulting in these channels and chutes to become filled. Foresets are a combination of sand and gravel facies. The are deposited by gravitational processes on the delta foreslope and the grains tend to become finer and more angular downslope. Bottomsets consist of fine grained silts and clay and are deposited at the foot of the delta front.
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.
A major flood on any river is both a long-term and a short-term event, particularly any river basin where human influence has exerted "control" over the ri...
is being eroded by the sea so that cliffs, up to 20 metres high rise
Periods that the folding occurred in which formed the outlines of the basin as it
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.
affects the ecosystem. The land's incline prevents some areas to receive and maintain a water
When it floods sediments can affect the land by losing nutrients in the soil and it can also affect the clarity of
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
the the change in sea level is due to a change in the level of land
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.
Mudslides usually occur in hilly areas, for an example, when there was a mudslide in Bangladesh few months back, it occurred at Chittagong. Mudslides occur when a portion of a hill side becomes too weak to hold up its own weight. This is generally caused by an intense amount of rain fall. With all of the new water introduced into the slope the content of liquid makes it so heavy that gravity pulls it downward. Although water plays a major factor in creating the mud that flows in a mudslide the real reason that the land begins to slide is gravity. What happens is mudslides redistribute soil and sediments in a process that can be in abrupt collapses or in slow gradual slides.