Brimbank Park is located at north-west of Melbourne, which is about 30 minute drive from Melbourne CBD. As can be seen from the map (Figure 1), it is adjacent to the suburb of Keilor to the north, Kealba to the west. The landform pattern of Brimbank Park is alluvial landforms. Based on the map (Figure 1), Maribyrnong River is across the park. Therefore, the flowing water erodes, transports and deposits sediments, and erosional and depositional feature can be found from fluvial action.
As can be seen from the map (Figure 2), the sites have been selected for this analysis. Site 1 is Top carpark (55H 31044.20m E 5821325.06m S), which is located on the top of the Brimbank Park. Site 2 is Ford on Maribyrnong River (55H 309261.56m
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As can be seen from the map (Figure 5), the Maribyrnong Rivers begins when the two major tributaries- Deep Creek and Jackson’s creek merge together, and then the river go through the Brimbank Park, downstream flows through suburban Melbourne before joining the Yarra River estuary on its way out to Port Phillip Bay. Therefore, because of the hydrology, there is erosion can be found in the Site 2 area.
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
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On the Sandy beach side, as can be seen from the image 2 and image 3, tussock and native grasses leading up to bank, thicker denser vegetation closer to water, the plants are all lower stratum. Opposite the beach, where on the other side of Maribyrnong River, there is a numbers of Mid-stratum trees. As a result of this, the plant from two sides are slightly different probably because the different direction of slope. Therefore, there is different sunshine area being exposed. More complicated, it is also an influence by climate. Melbourne is monsoon climate, accoding to Figure 6, Brimbank Park is located in Australia Climate zone 6. According to the total rainfall map in Victoria in 2015 (Figure 6) (Australian Government, 2015), the total rainfall of Brimbank is between 200mm and 300mm, which is a moderate figure in Victoria. Moderate rainfall create a comfortable basic environment for plant to grow, and different area of plant would have soil different structure, weathering and erosion. As a result of this, the plant at south facing slope would be more sheltered and moister, more productive forests. As for north facing slope, the plant would be usually drier, and less productive
Dawlish warren is a major sand spit at the mouth of the River Exe, and
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.
1. 225 MY : Weathering and erosion of very old folded rocks on an area
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.
middle of paper ... ... Site 1 Grid Reference: 211690 Types of Management: - Recurved Sea Wall - Wooden groynes Site 2 Grid Reference: 205687 Types of Management: - Straight Sea Wall - Wooden groynes Site 3 Grid Reference: 201686 Types of Management: - Rip rap boulders Site 4 Grid Reference: 222693 Types of Management: - No management, all natural. Managed retreat. Site 5 Grid Reference: 228695 Types of Management: - Rip rap boulders - Rip rap rock groynes - Wooden groynes - Revetment Site 1 is near Herne Bay and the sites are along the coastline towards Reculver in a North East direction. Site 5 is situated on the beach below the Twin Towers at Reculver.
In conclusion these various factors explain the theory that Kaibab Plateau is actually much older than the Colorado River and that the lake overflow theory best explains the multiple processes that contributed to this natural features current landscape. Lake Bidahochi would have flooded from time to time and combined with the lowest elevation on the Kaibab Plateau, the incision would have started. Considering major rivers have the capability to erode materials such as basaltic bedrock, going through the Kaibab Plateau would have proven possible. With circular scarps retreating from the plateau, the meandering of both rivers are explained and the presence of Colorado River limestone in a sequence of ancient basins today prove the river was younger than the uplift that took place in this region.
The average elevation in the Hudson Plains is 120m above sea level. It is a flat lowland area. The land is made up of mineral soils, with few outcrops of underlying sandstone and shale. This land was created when the weight of glaciers depressed the Hudson Bay region and the ocean waters flooded areas up to 300 km inland from the current coastline. Then, during the retreat of the huge continental ice sheets, drainage into the Hudson Bay was blocked and lakes (Agassiz and Ojibway for example) were formed along th...
Newman, B., 2012. Australian Regolith and Clays Conference. River Murray Salinity Management and Irrigation, pp. 163 - 166.
P5: ‘It would be more convenient for Australians to visit nearby natural locations compared to the parks in the gold coast, (para 2).
Stephen .G,Malcolm.W, Guy H,(2014), GEOL20001 The Geology of Southeast Australia, School of Earth Sciences, University of Melbourne, pg. 23-25
In the park written by Gwen Harwood, was originally written under a male pseudonym. The poem represents the idea of changing identity because of certain circumstances as well as challenging common ideas, paradigms and values & beliefs which is commonly held amongst mothers in today’s society.
Marshes - An area of soft, wet, low-lying land, characterized by grassy vegetation and o...
A river or “stream, ribbons of water confined to channels, or troughs, cut into the land,” (Marshak, 2009) is formed from a drainage network or “the array of interconnecting streams” that form tributaries. (Marshak, 2009). The amount of water that flows down a stream is its discharge. The discharge measurement takes the width and depths or cross sectional area of a river as well as the downstream velocity to get a numeric value for amount of water moving down stream. (Marshak, 2009)
How does the vegetation surface type affect the amount of runoff? Speculate why this happens.
Yarra Rangers Shire Conci, . (2012, 04 05). Retrieved from Yarra Ranges Shire Concil: vic.gov.au/Business/What_is_Economic_Development