The River Styles Framework is a scientific tool used to describe and explain the diversity and distribution of river types in a catchment according to river character and behaviour. [1] The River Styles Framework is based on the science of fluvial geomorphology. Each river type is called a "River Style" and its name is constructed following a consistent naming convention. [2] The River Styles Framework provides an open-ended process for interpreting rivers rather than fitting them into pre-existing categories. [1] [3] The River Styles Framework is designed to provide a scientific basis for river management. It was developed by researchers at Macquarie University. [4]
The River Styles Framework was developed by Gary Brierley and Kirstie Fryirs at Macquarie University. The first peer reviewed paper on River Styles was published in 2000. [5] Initial research that helped to develop the River Styles Framework was funded by Land & Water Australia and New South Wales Department of Land and Water Conservation. [1]
The River Styles Framework has four stages of analysis, which provide a framework to describe river character, explain how the river behaves and predict how a river may adjust its form in the future. The following overview of the stages is sourced from the book,"Geomorphology and River Management: Application of the River Styles Framework". [1]
Stage 1 provides a baseline survey of a river's character and behaviour. Steps in Stage 1 include:
Stage 2 assesses and explains geomorphic river condition throughout a catchment. River condition is a determination of environmental quality pertaining to a river's geomorphology. [6] Steps in Stage 2 include:
Stage 3 determines the potential for a river to 'recover', or improve in condition. Steps in Stage 3 include:
Stage 4 uses information from Stages 1 to 3 to identify 'target conditions' for a River Style as a goal toward which river rehabilitation (or restoration) can work. Steps in Stage 4 include:
The River Styles Framework has been used to support river management in Australia, [7] New Zealand, [8] United States [9] and Brazil. [10] In Australia, the Department of Industry (New South Wales) used the River Styles Framework as a key component in developing the River Condition Index (RCI) as a tool to assess river value, risk to river value and to monitor changes in river condition over time. [11] The River Styles Framework also contributes to the method for determining 'High Ecological Value Aquatic Ecosystems' (HEVAE) as part of the Australian National Water Initiative.
In the United States, The River Styles Framework formed part of the protocol for the Columbia Habitat Monitoring Program (CHaMP) developed for the Columbia River Basin. The CHaMP protocol used River Styles to help with comparing river types, predicting fish habitat suitability and prioritising river conservation and rehabilitation activities. [12]
A cost-benefit analysis completed by Land & Water Australia found that the River Styles Framework had a benefit-to-cost ratio of 28:1 and had contributed a net value of $40 million (AUD) in 2010. [13]
An accreditation framework has been developed for use of the River Styles Framework to ensure quality control. There are two levels of accreditation: 'Provisional' and 'Accredited'. 'Provisional' practitioners have undertaken a River Styles Short Course and have passed the associated assessment tasks. 'Provisional' practitioners may undertake assessments of River Styles under the supervision of a fully accredited practitioner. Full accreditation is gained following successful completion of a River Styles Short Course and completion of a satisfactory River Styles Report. 'Accredited' practitioners may undertake River Styles assessments unsupervised and may also supervise 'Provisional' practitioners. [14]
Geomorphology is the scientific study of the origin and evolution of topographic and bathymetric features created by physical, chemical or biological processes operating at or near the Earth's surface. Geomorphologists seek to understand why landscapes look the way they do, to understand landform history and dynamics and to predict changes through a combination of field observations, physical experiments and numerical modeling. Geomorphologists work within disciplines such as physical geography, geology, geodesy, engineering geology, archaeology, climatology and geotechnical engineering. This broad base of interests contributes to many research styles and interests within the field.
Murrumbidgee River, a major tributary of the Murray River within the Murray–Darling basin and the second longest river in Australia. It flows through the Australian state of New South Wales and the Australian Capital Territory. It descends 1,500 metres (4,900 ft) as it flows 1,485 kilometres (923 mi) in a west-northwesterly direction from the foot of Peppercorn Hill in the Fiery Range of the Snowy Mountains towards its confluence with the Murray River near Boundary Bend.
The Molonglo River, a perennial river that is part of the Murrumbidgee catchment within the Murray–Darling basin, is located in the Monaro and Capital Country regions of New South Wales and the Australian Capital Territory, in Australia.
Macquarie River a watercourse that is part of the Macquarie–Barwon catchment within the Murray–Darling basin, is one of the main inland rivers in New South Wales, Australia.
The Snowy River is a major river in south-eastern Australia. It originates on the slopes of Mount Kosciuszko, Australia's highest mainland peak, draining the eastern slopes of the Snowy Mountains in New South Wales, before flowing through the Alpine National Park and the Snowy River National Park in Victoria and emptying into Bass Strait.
The Lachlan River is an intermittent river that is part of the Murrumbidgee catchment within the Murray–Darling basin, located in the Southern Tablelands, Central West, and Riverina regions of New South Wales, Australia.
Nepean River, is a major perennial river, located in the south-west and west of Sydney, New South Wales, Australia. The Nepean River and its associated mouth, the Hawkesbury River, almost encircles the metropolitan region of Sydney.
Manning River, an open and trained mature wave dominated barrier estuary, is located in the Northern Tablelands and Mid North Coast districts of New South Wales, Australia.
Hastings River, an open and trained intermediate wave dominated barrier estuary, is located in the Northern Tablelands and Mid North Coast districts of New South Wales, Australia.
Lake Macquarie or Awaba is Australia's largest coastal salt water lake. Located in the Hunter Region of New South Wales, it covers an area of 110 square kilometres (42.5 sq mi) and is connected to the Tasman Sea by a short channel. Most of the residents of the City of Lake Macquarie live near the shores of the lake.
The Parliament House in Sydney is a heritage-listed complex of buildings housing the Parliament of the state of New South Wales, Australia. The building is located on the east side of Macquarie Street in Sydney, the state capital. The façade consists of a two-storey Georgian building, the oldest public building in the City of Sydney, flanked by two Neo-gothic additions containing the parliamentary chambers. These buildings are linked to a 1970s 12-storey block at the rear, facing onto the Domain. It is also known as Parliament of New South Wales, Parliamentary Precincts and the Rum Hospital.
The Prospect Reservoir is a heritage-listed 50,200-megalitre potable water supply and storage reservoir created by the Prospect Dam, across the Prospect Creek located in the Western Sydney suburb of Prospect, in New South Wales, Australia. The eastern bounds of the reservoir are a recreational area and the western periphery are within the bounds of Western Sydney Parklands. It was added to the New South Wales State Heritage Register on 18 November 1999.
The Tumut River, a perennial stream that is part of the Murrumbidgee catchment within the Murray–Darling basin, is located in the Snowy Mountains and South West Slopes districts of New South Wales, Australia.
Wilsons River, a perennial river and part of the Richmond River catchment, is situated in the Northern Rivers district of New South Wales, Australia.
The Kowmung River, a perennial river that is part of the Hawkesbury-Nepean catchment, is located in the Central Tablelands region of New South Wales, Australia.
Murrah River is an open mature wave dominated barrier estuary or perennial river located in the South Coast region of New South Wales, Australia.
Coolaburragundy River, a perennial stream that is part of the Talbragar catchment within the Murray–Darling basin, is located in the Orana district of New South Wales, Australia.
Estuaries of Australia are features of the Australian coastline. They are linked to tides, river mouths and coastal features and conditions. In many cases the features of estuaries are also named inlets.
Legacy sediment (LS) is depositional bodies of sediment inherited from the increase of human activities since the Neolithic. These include a broad range of land use and land cover changes, such as agricultural clearance, lumbering and clearance of native vegetation, mining, road building, urbanization, as well as alterations brought to river systems in the form of dams and other engineering structures meant to control and regulate natural fluvial processes. The concept of LS is used in geomorphology, ecology, as well as in water quality and toxicological studies.
The Macquarie River railway bridge is a heritage-listed disused railway bridge across the Macquarie River that was previously located on the Main Western line in Bathurst in the Bathurst Region local government area of New South Wales, Australia. It was built in 1876. It is also known as Bathurst Rail Bridge over Macquarie River and Bathurst - Kelso Railway Bridge. The property is owned by RailCorp, an agency of the Government of New South Wales. The bridge was added to the New South Wales State Heritage Register on 2 April 1999 and was added to the Register of the National Estate on 18 April 1989.