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Salt Pan Creek

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A stream is a continuous body of surface water flowing within the bed and banks of a channel . Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long, large streams are usually called rivers , while smaller, less voluminous and more intermittent streams are known as streamlets , brooks or creeks .

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67-669: Salt Pan Creek is an urban watercourse of the Georges River catchment, located in the Canterbury-Bankstown region of Sydney , in New South Wales , Australia. Salt Pan Creek rises west southwest of the suburb of Mount Lewis , within the City of Canterbury-Bankstown local government area , and flows generally south by east through Georges River local government area, before reaching its confluence with

134-403: A bed armor layer, and other depositional features, plus well defined banks due to bank erosion, are good identifiers when assessing for perennial streams. Particle size will help identify a perennial stream. Perennial streams cut through the soil profile, which removes fine and small particles. By assessing areas for relatively coarse material left behind in the stream bed and finer sediments along

201-658: A continuous aquatic habitat until they reach maturity. Crayfish and other crustaceans , snails , bivalves (clams), and aquatic worms also indicate the stream is perennial. These require a persistent aquatic environment for survival. Fish and amphibians are secondary indicators in assessment of a perennial stream because some fish and amphibians can inhabit areas without persistent water regime. When assessing for fish, all available habitat should be assessed: pools, riffles, root clumps and other obstructions. Fish will seek cover if alerted to human presence, but should be easily observed in perennial streams. Amphibians also indicate

268-470: A continuous or intermittent stream. The same non-perennial channel might change characteristics from intermittent to ephemeral over its course. Washes can fill up quickly during rains, and there may be a sudden torrent of water after a thunderstorm begins upstream, such as during monsoonal conditions. In the United States, an intermittent or seasonal stream is one that only flows for part of

335-615: A creek, especially one that is fed by a spring or seep . It is usually small and easily forded . A brook is characterised by its shallowness. A creek ( / k r iː k / ) or crick ( / k r ɪ k / ): In hydrography, gut is a small creek; this is seen in proper names in eastern North America from the Mid-Atlantic states (for instance, The Gut in Pennsylvania, Ash Gut in Delaware, and other streams) down into

402-422: A drainage network. Although each tributary has its own source, international practice is to take the source farthest from the river mouth as the source of the entire river system, from which the most extended length of the river measured as the starting point is taken as the length of the whole river system, and that furthest starting point is conventionally taken as the source of the whole river system. For example,

469-401: A half-caste". Governor Broome insisted that the act contain within it a clause permitting traditional owners to continue hunting on their tribal lands. The effect of the act was to give increasing power to the board over Aboriginal people, rather than setting up a system to punish whites for wrongdoing in relation to Aboriginal people. An Aboriginal Department was set up, under the office of

536-540: A larger stream. Common terms for individual river distributaries in English-speaking countries are arm and channel . There are a number of regional names for a stream. A stream's source depends on the surrounding landscape and its function within larger river networks. While perennial and intermittent streams are typically supplied by smaller upstream waters and groundwater, headwater and ephemeral streams often derive most of their water from precipitation in

603-404: A path into mines or other underground chambers. According to official U.S. definitions, the channels of intermittent streams are well-defined, as opposed to ephemeral streams, which may or may not have a defined channel, and rely mainly on storm runoff, as their aquatic bed is above the water table . An ephemeral stream does not have the biological, hydrological, and physical characteristics of

670-412: A perennial stream and include tadpoles , frogs , salamanders , and newts . These amphibians can be found in stream channels, along stream banks, and even under rocks. Frogs and tadpoles usually inhabit shallow and slow moving waters near the sides of stream banks. Frogs will typically jump into water when alerted to human presence. Well defined river beds composed of riffles, pools, runs, gravel bars,

737-483: A perennial stream, fine sediment may cling to riparian plant stems and tree trunks. Organic debris drift lines or piles may be found within the active overbank area after recent high flow. Streams, headwaters, and streams flowing only part of the year provide many benefits upstream and downstream. They defend against floods, remove contaminants, recycle nutrients that are potentially dangerous as well as provide food and habitat for many forms of fish. Such streams also play

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804-539: A skirmish that saw Frederick Meredith, a European settler, injured with a spear and forced to abandon his farm. Meredith and another settler were seeking to clear and cultivate land surrounding the creek that may have been an important food source for Aboriginal people. In the 1920s, the Aboriginal Anderson and Rowley families bought land along the creek that was not farmed as it was low-lying, and had large amounts of sandstone and forest. The surrounding land

871-406: A slow-moving wetted channel or stagnant area. This is evidence that iron-oxidizing bacteria are present, indicating persistent expression of oxygen-depleted ground water. In a forested area, leaf and needle litter in the stream channel is an additional indicator. Accumulation of leaf litter does not occur in perennial streams since such material is continuously flushed. In the adjacent overbank of

938-486: A stream as intermittent, "showing interruptions in time or space". Generally, streams that flow only during and immediately after precipitation are termed ephemeral . There is no clear demarcation between surface runoff and an ephemeral stream, and some ephemeral streams can be classed as intermittent—flow all but disappearing in the normal course of seasons but ample flow (backups) restoring stream presence — such circumstances are documented when stream beds have opened up

1005-424: A stream is a critical factor in determining its character and is entirely determined by its base level of erosion. The base level of erosion is the point at which the stream either enters the ocean, a lake or pond, or enters a stretch in which it has a much lower gradient, and may be specifically applied to any particular stretch of a stream. In geological terms, the stream will erode down through its bed to achieve

1072-531: A suitable age, until they turned 21. An Aboriginal Protection Board was also established to prevent the abuses reported earlier, but rather than protect Aborigines, it mainly succeeded in putting them under tighter government control. It was intended to enforce contracts, employment of prisoners and apprenticeships, but there was not sufficient power to enforce clauses in the north, and they were openly flouted. The Act defined as "Aboriginal" as "every Aboriginal native of Australia, every Aboriginal half-caste, or child of

1139-524: A thin layer called sheet wash, combined with a network of tiny rills, which together form the sheet runoff; when this water is focused in a channel, a stream is born. Some rivers and streams may begin from lakes or ponds. Freshwater's primary sources are precipitation and mountain snowmelt. However, rivers typically originate in the highlands, and are slowly created by the erosion of mountain snowmelt into lakes or rivers. Rivers usually flow from their source topographically, and erode as they pass until they reach

1206-627: A vital role in preserving our drinking water quality and supply, ensuring a steady flow of water to surface waters and helping to restore deep aquifers. The extent of land basin drained by a stream is termed its drainage basin (also known in North America as the watershed and, in British English, as a catchment). A basin may also be composed of smaller basins. For instance, the Continental Divide in North America divides

1273-435: Is a stream that branches off and flows away from a main stream channel, and the phenomenon is known as river bifurcation . Distributaries are common features of river deltas , and are often found where a valleyed stream enters wide flatlands or approaches the coastal plains around a lake or an ocean . They can also occur inland, on alluvial fans , or where a tributary stream bifurcates as it nears its confluence with

1340-425: Is sometimes termed a "young" or "immature" stream, and the later state a "mature" or "old" stream. Meanders are looping changes of direction of a stream caused by the erosion and deposition of bank materials. These are typically serpentine in form. Typically, over time the meanders gradually migrate downstream. If some resistant material slows or stops the downstream movement of a meander, a stream may erode through

1407-517: Is the traditional country of the Bediagal clan of the Dharug people. Salt Pan Creek was named by early colonial settlers, who took salt from the swampland by evaporating the salt water. From as early as 1809, the land surrounding Salt Pan Creek was the site of uprising by Indigenous Australians against colonial settlement . Tedbury , the son of Pemulwuy , an Aboriginal elder , was involved in

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1474-456: Is usually called a creek and marked on topographic maps with a solid blue line. There are five generic classifications: "Macroinvertebrate" refers to easily seen invertebrates , larger than 0.5 mm, found in stream and river bottoms. Macroinvertebrates are larval stages of most aquatic insects and their presence is a good indicator that the stream is perennial. Larvae of caddisflies , mayflies , stoneflies , and damselflies require

1541-744: The Half-Caste Act , described as An Act to provide for the better protection and management of the Aboriginal Natives of Western Australia, and to amend the Law relating to certain Contracts with such Aboriginal Natives (statute 25/1886), and The Aborigines Act, 1889 (statute 24/1889). The 1886 act was enacted following the furore over the Fairburn Report (which revealed slavery conditions among Aboriginal farm workers) and

1608-582: The Aboriginal Protection Board . The land was important because it was freehold , and therefore not under any government or missionary control, and politics was a major source of conversation at the camp. The refugees included Bill Onus , Jack Patten , Jack(o) Campbell (from Kempsey ), Pearl Gibbs , Ted Thomas from Wallaga Lake Aboriginal Station , Bert Groves , and siblings Tom Williams Jnr and Ellen James, grandchildren of Ellen Anderson. In 1933, Joe Anderson (aka "King Burraga")

1675-740: The Chief Protector of Aborigines . Nearly half of the Legislative Council voted to amend the act for contract labour as low as age 10 but it was defeated. McKenzie Grant , the member for The North , claimed that child labour of age six or seven was a necessary commonplace, as "in this way they gradually become domesticated". The attorney general Septimus Burt , in debate on the 2nd reading speech, claimed that contracts were being issued, not for current work, but to hold Aboriginal people as slaves on stations for potential future work, and so prevent them from being free to leave. In 1898,

1742-606: The Cootamundra Domestic Training Home for Aboriginal Girls . Aboriginal children were removed from their families for various welfare reasons and transported to Kinchela and Cootamundra, where they were often abused and neglected while being taught farm labouring and domestic work, many of them ending up as servants in the homes of wealthy Sydney residents. In 1915, the Aborigines Protection Amending Act 1915 gave

1809-691: The Tombigbee River basin. Continuing in this vein, a component of the Mississippi River basin is the Ohio River basin, which in turn includes the Kentucky River basin, and so forth. Stream crossings are where streams are crossed by roads , pipelines , railways , or any other thing which might restrict the flow of the stream in ordinary or flood conditions. Any structure over or in a stream which results in limitations on

1876-480: The velocity of the stream. A perennial stream is one which flows continuously all year. Some perennial streams may only have continuous flow in segments of its stream bed year round during years of normal rainfall. Blue-line streams are perennial streams and are marked on topographic maps with a solid blue line. The word "perennial" from the 1640s, meaning "evergreen," is established in Latin perennis, keeping

1943-403: The 1886 Act started to remove Aboriginal people of mixed descent, known as " half-castes ", from Aboriginal stations or reserves to force them to assimilate into European society. These expulsions separated families and communities, causing distress and leading to protest. Nevertheless, the board refused to assist the expelled people. It was assumed that the expulsions would lead to the decline in

2010-520: The 1920s, Aboriginal rights activist Fred Maynard and missionary Elizabeth McKenzie Hatton. In 1924, AAPA set up a safe house in Homebush , not far away, for Aboriginal girls who had left their apprenticeships. Between 1926 and 1935, lands surrounding the creek became a focal point for Indigenous rights, as they set up squatter camps that consisted of refugee families whose traditional lands had been taken by settlers, and also those seeking to escape

2077-941: The Board authority to remove Aboriginal children "without having to establish in court that they were neglected." The Board was renamed the Aborigines Welfare Board (which was frequently referred to as the Aborigin al Welfare Board in later sources ) in 1940 by the Aborigines Protection (Amendment) Act 1940 , which stipulated that Aboriginal people should be assimilated into mainstream white society. It intended that Aboriginal culture would evaporate, and Aboriginal people would eventually become indistinguishable from Europeans. The Board consisted of 11 members, including two Aboriginal people, one "full-blood" and one having "a mixture of Aboriginal blood". It

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2144-704: The Caribbean (for instance, Guinea Gut , Fish Bay Gut , Cob Gut , Battery Gut and other rivers and streams in the United States Virgin Islands , in Jamaica (Sandy Gut, Bens Gut River, White Gut River), and in many streams and creeks of the Dutch Caribbean ). A river is a large natural stream that is much wider and deeper than a creek and not easily fordable, and may be a navigable waterway . The linear channel between

2211-653: The Friday night markets. They were all able to gather oysters , prawns and river fish, and there were swamp wallabies and other game which could be hunted for food. The land remained as open camping grounds for Aboriginal people until the 1930s. Ellen and Hugh Anderson maintained contact with the Aborigines Inland Mission , and met the founders of the Australian Aboriginal Progressive Association (AAPA) in

2278-516: The Georges River, at Riverwood . The catchment area of the creek is approximately 26 square kilometres (10 sq mi), and is subject to flooding due to vegetation modification and urban development . Vegetation in the catchment area consists of three endangered ecological species, including coastal saltmarsh , Cooks River Castlereagh Ironbark Forest, and Shale / Sandstone Transition Forest. Vegetation varies substantially throughout

2345-533: The atmosphere either by evaporation from soil and water bodies, or by plant evapotranspiration. By infiltration some of the water sinks into the earth and becomes groundwater, much of which eventually enters streams. Most precipitated water is partially bottled up by evaporation or freezing in snow fields and glaciers. The majority of the water flows as a runoff from the ground; the proportion of this varies depending on several factors, such as climate, temperature, vegetation, types of rock, and relief. This runoff begins as

2412-525: The base level of erosion throughout its course. If this base level is low, then the stream will rapidly cut through underlying strata and have a steep gradient, and if the base level is relatively high, then the stream will form a flood plain and meander. Typically, streams are said to have a particular elevation profile , beginning with steep gradients, no flood plain, and little shifting of channels, eventually evolving into streams with low gradients, wide flood plains, and extensive meanders. The initial stage

2479-597: The base stage of erosion. The scientists have offered a way based on data to define the origin of the lake. A classified sample was the one measured by the Chinese researchers from the University of Chinese Academy of Sciences. As an essential symbol of the river formation environment, the river source needs an objective and straightforward and effective method of judging . A calculation model of river source catchment area based on critical support flow (CSD) proposed, and

2546-820: The board was replaced by the Aborigines Department . The Queensland Aboriginal Protection Board was established by the Aboriginals Protection and Restriction of the Sale of Opium Act 1897 . The Aborigines Act Amendment Act 1939 created the Aborigines Protection Board in South Australia , which was "charged with the duty of controlling and promoting the welfare" of Aboriginal people (which included anyone descended from an Aboriginal person). Charles Duguid

2613-609: The boards had limited funds, protectors received very limited remuneration. A range of people were appointed as local protectors, including resident magistrates, jail wardens, justices of the peace and, in some cases ministers of religion, though most were local police inspectors. The minutes of the boards show they mostly dealt with matters of requests from religious bodies for financial relief and reports from resident or police magistrates pertaining to trials and convictions of Aboriginal people under their jurisdiction. Aboriginal protection boards also issued permits to allow Aboriginal people

2680-497: The catchment area and includes freshwater environments, estuarine environments, mangroves and saltmarshes, riparian and terrestrial environments, which provide important habitat for native fauna. Aboriginal Australians lived on both sides of the Georges Creek for many years before the colonisation of Australia . The Salt Pan Creek area, on the northern shore of the Georges River between present-day Padstow and Riverwood

2747-626: The communities. The New South Wales Board for the Protection of Aborigines was established in 1883 and was reconstituted under the Aborigines Protection Act 1909 with wide-ranging control over the lives of Aboriginal people. That included the power to remove children from families because, as stated in many of the files, their parents were Aboriginals, and the power to dictate where Aboriginal people lived, to ensure protection from violent colonialists and provide education in

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2814-633: The face of European opposition (McCallum, 2008). The Board also controlled their freedom of movement and personal finances. In particular, Aboriginal children could be removed from their homes and families and taken into care to be raised like white children, becoming the Stolen Generations . The 1911 amendment to the Aboriginal Protection Act established the Kinchela Aboriginal Boys' Training Home and

2881-707: The flow is reduced to a trickle or less. Typically torrents have Apennine rather than Alpine sources, and in the summer they are fed by little precipitation and no melting snow. In this case the maximum discharge will be during the spring and autumn. An intermittent stream can also be called a winterbourne in Britain, a wadi in the Arabic -speaking world or torrente or rambla (this last one from arabic origin) in Spain and Latin America. In Australia, an intermittent stream

2948-447: The form of rain and snow. Most of this precipitated water re-enters the atmosphere by evaporation from soil and water bodies, or by the evapotranspiration of plants. Some of the water proceeds to sink into the earth by infiltration and becomes groundwater, much of which eventually enters streams. Some precipitated water is temporarily locked up in snow fields and glaciers , to be released later by evaporation or melting. The rest of

3015-671: The function of regulating the lives of Aboriginal Australians . They were also responsible for administering the various half-caste acts where these existed and had a key role in the Stolen Generations . The boards had nearly ultimate control over Aboriginal people's lives. Protectors of Aborigines were appointed by the Board under the conditions laid down in the various Acts. In theory, protectors of Aborigines were often empowered to undertake legal proceedings on behalf of Aboriginal people, dictate where Aboriginal people could live or work, and keep all wages earned by employed Aboriginals. The exact powers varied over time and by jurisdiction. As

3082-407: The immediate vicinity of a stream is called a riparian zone . Given the status of the ongoing Holocene extinction , streams play an important corridor role in connecting fragmented habitats and thus in conserving biodiversity . The study of streams and waterways in general is known as surface hydrology and is a core element of environmental geography . A brook is a stream smaller than

3149-532: The lake has significant feeder rivers. The Kagera River, which flows into Lake Victoria near Bukoba's Tanzanian town , is the longest feeder, though sources do not agree on which is the Kagera's longest tributary and therefore the Nile's most remote source itself. To qualify as a stream, a body of water must be either recurring or perennial. Recurring (intermittent) streams have water in the channel for at least part of

3216-416: The lives of Aboriginal Victorians . The board exerted an extraordinary level of control over people's lives including regulation of residence, slavery as employment, marriage, social life and other aspects of daily life. The Victorian Half-Caste Act of 1886 gave the Board extensive new powers over the lives of Aboriginal people , including regulation of residence, employment and marriage. In particular,

3283-683: The mainly easterly-draining Atlantic Ocean and Arctic Ocean basins from the largely westerly-flowing Pacific Ocean basin. The Atlantic Ocean basin, however, may be further subdivided into the Atlantic Ocean and Gulf of Mexico drainages. (This delineation is termed the Eastern Continental Divide .) Similarly, the Gulf of Mexico basin may be divided into the Mississippi River basin and several smaller basins, such as

3350-412: The meaning as "everlasting all year round," per "over" plus annus "year." This has been proved since the 1670s by the "living years" in the sense of botany. The metaphorical sense of "enduring, eternal" originates from 1750. They are related to "perennial." See biennial for shifts in vowels. Perennial streams have one or more of these characteristics: Absence of such characteristics supports classifying

3417-413: The movement of fish or other ecological elements may be an issue. Aboriginal Protection Board Aboriginal Protection Board , also known as Aborigines Protection Board , Board for the Protection of Aborigines , Aborigines Welfare Board (and in later sources, incorrectly as Aboriginal Welfare Board ), and similar names, refers to a number of historical Australian state -run institutions with

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3484-453: The neck between two legs of a meander to become temporarily straighter, leaving behind an arc-shaped body of water termed an oxbow lake or bayou . A flood may also cause a meander to be cut through in this way. The stream load is defined as the solid matter carried by a stream. Streams can carry sediment, or alluvium. The amount of load it can carry (capacity) as well as the largest object it can carry (competence) are both dependent on

3551-596: The origin of the Nile River is the confluence of the White Nile and the Blue Nile, but the source of the whole river system is in its upper reaches. If there is no specific designation, "length of the Nile" refers to the "river length of the Nile system", rather than to the length of the Nile river from the point where it is formed by a confluence of tributaries. The Nile's source is often cited as Lake Victoria, but

3618-430: The other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes that respond to geological, geomorphological, hydrological and biotic controls. Streams are important as conduits in the water cycle , instruments in groundwater recharge , and corridors for fish and wildlife migration. The biological habitat in

3685-415: The parallel ridges or bars on a shoreline beach or river floodplain, or between a bar and the shore. Also called a swale . A tributary is a contributory stream to a larger stream, or a stream which does not reach a static body of water such as a lake , bay or ocean but joins another river (a parent river). Sometimes also called a branch or fork. A distributary , or a distributary channel ,

3752-597: The population of the reserves and their eventual closure. The Aborigines Act 1910 increased the rights of Aboriginal people in Victoria. The board was abolished in 1957 by the Aborigines Act 1957 . The Aboriginal Lands Act 1970 gave recognition of Aboriginal people's right to land. Under this Act the deeds of land at the Lake Tyers Mission and Framlingham reserves were transferred to

3819-469: The relationship between CSA and CSD with a minimum catchment area established. Using the model for comparison in two basins in Tibet (Helongqu and Niyang River White Water), the results show that the critical support flow (Qc) of the housing dragon song is 0.0028 m /s. At the same time, the white water curvature is 0.0085 m /s. Besides, the critical support flow can vary with hydrologic climate conditions, and

3886-704: The right to leave their respective missions and reserves and enter the mainstream society for a set period of time. The Central Board Appointed to Watch Over the Interests of the Aborigines was established in 1860. This was replaced by the Victorian Central Board for the Protection of Aborigines in 1869 (via the Aboriginal Protection Act 1869 ), making Victoria the first colony to enact comprehensive regulations on

3953-425: The side of the stream or within the floodplain will be a good indicator of persistent water regime. A perennial stream can be identified 48 hours after a storm. Direct storm runoff usually has ceased at this point. If a stream is still flowing and contributing inflow is not observed above the channel, the observed water is likely baseflow. Another perennial stream indication is an abundance of red rust material in

4020-655: The vital support flow Qc in wet areas (white water) is larger than in semi-arid regions (heap slot). The proposed critical support flow (CSD) concept and model method can be used to determine the hydrographic indicators of river sources in complex geographical areas, and it can also reflect the impact of hydrologic climate change on river recharge in different regions. The source of a river or stream (its point of origin) can consist of lakes, swamps, springs, or glaciers. A typical river has several tributaries; each of these may be made up of several other smaller tributaries, so that together this stream and all its tributaries are called

4087-512: The water flows off the land as runoff, the proportion of which varies according to many factors, such as wind, humidity, vegetation, rock types, and relief. This runoff starts as a thin film called sheet wash, combined with a network of tiny rills, together constituting sheet runoff; when this water is concentrated in a channel, a stream has its birth. Some creeks may start from ponds or lakes. The streams typically derive most of their water from rain and snow precipitation. Most of this water re-enters

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4154-480: The work of the Rev. John Gribble . The Act introduced employment contracts between employers and Aboriginal workers over the age of 14. There was no provision in the 1886 Act for contracts to include wages, but employees were to be provided with "substantial, good and sufficient rations", clothing and blankets. The 1886 act provided a resident magistrate with the power to indenture 'half-caste' and Aboriginal children, from

4221-521: The year and is marked on topographic maps with a line of blue dashes and dots. A wash , desert wash, or arroyo is normally a dry streambed in the deserts of the American Southwest , which flows after sufficient rainfall. In Italy, an intermittent stream is termed a torrent ( Italian : torrente ). In full flood the stream may or may not be "torrential" in the dramatic sense of the word, but there will be one or more seasons in which

4288-402: The year. A stream of the first order is a stream which does not have any other recurring or perennial stream feeding into it. When two first-order streams come together, they form a second-order stream. When two second-order streams come together, they form a third-order stream. Streams of lower order joining a higher order stream do not change the order of the higher stream. The gradient of

4355-625: Was abolished under the Aborigines Act 1969 (NSW). After its abolition, the NSW Aboriginal Advisory Council was formed, which advised the NSW Minister for Aboriginal Affairs directly. The Western Australian Aborigines Protection Board operated between 1 January 1886 and 1 April 1898 as a statutory authority . It was created by the Aborigines Protection Act, 1886 (WA), also known as

4422-515: Was filmed at Salt Pan Creek by Cinesound news delivering a message about Indigenous rights. 33°57′S 151°03′E  /  33.950°S 151.050°E  / -33.950; 151.050 Perennial stream The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater ), daylighted subterranean water , and surfaced groundwater ( spring water ). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on

4489-485: Was similar to these two blocks, and became camps for Aboriginal people not wanting to live on Aboriginal reserves , which were controlled by the Aborigines Welfare Board . They lived by working for a variety of jobs for cash, and by using their knowledge of the flora and fauna of the area. Some sold wildflowers door-to-door; others collected the bright red gum tips and Christmas bush and sold them at

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