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Great Gibraltar Sand Dune

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The Great Gibraltar Sand Dune is an ancient sand dune in the British Overseas Territory of Gibraltar . It forms part of the Upper Rock Nature Reserve and dominates the eastern cliffs of the Rock of Gibraltar . It was once used to capture rainwater which was contained in underground tanks within the Rock to satisfy the population's potable water needs.

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54-450: The prehistoric dune is made from yellow, windblown sands lacking the red component of the sands on the west side of the Rock. It is made of the same sand that once formed part of a vast savanna of the late Pleistocene where Neanderthals hunted. The levant winds of prehistory continuously blew sand from this savanna westwards, accumulating against the eastern cliffs of the Rock, reaching from

108-438: A continuous tree canopy which would prevent further grass growth. Prior to European settlement aboriginal land use practices, including fire, influenced vegetation and may have maintained and modified savanna flora. It has been suggested by many authors that aboriginal burning created a structurally more open savanna landscape. Aboriginal burning certainly created a habitat mosaic that probably increased biodiversity and changed

162-491: A dramatic reduction in basal area and canopy cover, often leaves a high percentage of woody plants alive either as seedlings too small to be affected or as plants capable of re-sprouting from lignotubers and broken stumps. A population of woody plants equal to half or more of the original number often remains following pulling of eucalypt communities, even if all the trees over 5 metres are uprooted completely. A number of exotic plants species have been introduced to savannas around

216-481: A fifth reservoir was excavated inside the Rock and the catchment area increased to 24 acres (97,000 m ). By 1961 the total catchment area had increased to its maximum of 34 acres (140,000 m ). In 2001, the Gibraltar Ornithological and Natural History Society began to manage the phased work of dismantling this catchment construction. By 2006 the slope was entirely restored to its natural state and

270-468: A fifth reservoir was excavated inside the Rock and the catchment area increased to 24 acres (97,000 m). By 1961 the total catchment area had increased to its maximum of 34 acres (140,000 m). It took roughly 5,928 rafters, 1,112 purlins, 1,161 piles, 5,928 sheets, 2,920 kg of screws and 850 kg of washers for every hectare of the Great Dune that was covered. The Great Dune served to maintain

324-402: A means of clearing land. In the 1950s arboricides suitable for stem injection were developed. War-surplus heavy machinery was made available, and these were used for either pushing timber, or for pulling using a chain and ball strung between two machines. These two new methods of timber control, along with the introduction and widespread adoption of several new pasture grasses and legumes promoted

378-444: A reduction in the need to burn to produce a flush of green growth because legumes retain high nutrient levels throughout the year, and because fires can have a negative impact on legume populations which causes a reluctance to burn. The closed forest types such as broadleaf forests and rainforests are usually not grazed owing to the closed structure precluding grass growth, and hence offering little opportunity for grazing. In contrast

432-425: A regular supply of sand on the eastern beaches of Gibraltar, especially Sandy Bay particularly when the sea removed material from the beach. This dynamic nature meant that little vegetation of any significant height could grow on the dune with any permanence as many pre-catchment photographs demonstrate. In 2001, the Gibraltar Ornithological and Natural History Society began to manage the phased work of dismantling

486-399: A result of global climate change, particularly at ecotones such as savannas so often represent. A savanna can simply be distinguished by the open savanna, where grass prevails and trees are rare; and the wooded savanna, where the trees are densest, bordering an open woodland or forest. Specific savanna ecoregions of several different types include: Sandy Bay, Gibraltar Sandy Bay

540-469: A resurgence in tree clearing. The 1980s also saw the release of soil-applied arboricides, notably tebuthiuron , that could be utilised without cutting and injecting each individual tree. In many ways "artificial" clearing, particularly pulling, mimics the effects of fire and, in savannas adapted to regeneration after fire as most Queensland savannas are, there is a similar response to that after fire. Tree clearing in many savanna communities, although causing

594-455: A simplified yet widespread climatic concept. The divergence has sometimes caused areas such as extensive savannas north and south of the Congo and Amazon Rivers to be excluded from mapped savanna categories. In different parts of North America, the word "savanna" has been used interchangeably with " barrens ", " prairie ", " glade ", "grassland" and " oak opening ". Different authors have defined

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648-472: Is a village, bay and beach located on a small bay on the eastern Mediterranean coast of Gibraltar , on the opposite side of The Rock from the main city. It is situated to the south of Catalan Bay and is accessible via Sir Herbert Miles Road. Directly above Sandy Bay and the Sir Herbert Miles coast road were Gibraltar's large water catchments, which are no longer in use. The slope on which they sat

702-477: Is not prominent but that rivers in savanna landscapes erode more by lateral migration . Flooding and associated sheet wash have been proposed as dominant erosion processes in savanna plains. The savannas of tropical America comprise broadleaved trees such as Curatella , Byrsonima , and Bowdichia , with grasses such as Leersia and Paspalum . Bean relative Prosopis is common in the Argentinian savannas. In

756-458: Is now completely covered in vegetation native to this unique habitat of Gibraltar. It is possible to continue south along Sir Herbert Miles road and through Dudley Ward Tunnel all the way to Europa Point at the southern tip of Gibraltar. Following a rockfall on 18 February 2002, which killed a man, the Government concluded that the risk of further such incidents was too great, and the tunnel

810-772: Is often believed that savannas feature widely spaced, scattered trees. However, in many savannas, tree densities are higher and trees are more regularly spaced than in forests. The South American savanna types cerrado sensu stricto and cerrado dense typically have densities of trees similar to or higher than that found in South American tropical forests, with savanna ranging from 800 to 3300 trees per hectare (trees/ha) and adjacent forests with 800–2000 trees/ha. Similarly Guinean savanna has 129 trees/ha, compared to 103 for riparian forest , while Eastern Australian sclerophyll forests have average tree densities of approximately 100 per hectare , comparable to savannas in

864-473: Is possible for there to be multiple stable biomes. The annual rainfall ranges from 500 mm (19.69 in) to 1,270 mm (50.00 in) per year, with the precipitation being more common in six or eight months of the year, followed by a period of drought. Savannas may at times be classified as forests. In climatic geomorphology it has been noted that many savannas occur in areas of pediplains and inselbergs . It has been posited that river incision

918-594: Is the Great Gibraltar Sand Dune , an ancient consolidated sand dune which dominates the east side of the Rock of Gibraltar . The dune's naturally smooth surface allowed for the construction of a water catchment area made up of a corrugated steel sheets and a layer of concrete . Rainwater flowed down the slope into an open channel which fed into the reservoir system inside The Rock. In 1898, work began on four 5 million gallon water reservoirs which were cut into

972-419: Is vague and therefore the two can be combined into a single biome as both woodlands and savannas feature open-canopied trees with crowns not usually interlinking (mostly forming 25-60% cover). Over many large tropical areas, the dominant biome (forest, savanna or grassland) can not be predicted only by the climate, as historical events plays also a key role, for example, fire activity. In some areas, indeed, it

1026-455: The Mediterranean region were likewise created and maintained by anthropogenic fire. Intentional controlled burns typically create fires confined to the herbaceous layer that do little long term damage to mature trees. This prevents more catastrophic wildfires that could do much more damage. However, these fires either kill or suppress tree seedlings, thus preventing the establishment of

1080-745: The Signal House , and the Middle-hill Guards . These parts were formerly accessible, which made it necessary to keep constant guards there, as well to prevent desertions from within as a surprise from without. Of late years, much labour has been bestowed in making all these parts more abrupt and difficult, yet it is still necessary to watch them, as there are always some hardy adventurers who will wantonly risk their lives down these perilous cliffs, either in attempting to desert or in search of flowers." Gibraltar has few natural sources of fresh water which has been historically problematic for its population over

1134-476: The greenhouse effect may result in an alteration of the structure and function of savannas. Some authors have suggested that savannas and grasslands may become even more susceptible to woody plant encroachment as a result of greenhouse induced climate change . However, a recent case described a savanna increasing its range at the expense of forest in response to climate variation, and potential exists for similar rapid, dramatic shifts in vegetation distribution as

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1188-717: The prairies in North America and steppes in Eurasia , which feature cold winters, savannas are mostly located in areas having warm to hot climates, such as in Africa, Australia, Thailand, South America and India. The word derives from the Spanish sabana , which is itself a loanword from Taíno , which means "treeless grassland" in the West Indies . The letter b in Spanish, when positioned in

1242-544: The Australian savanna, mammals in the family Macropodidae predominate, such as kangaroos and wallabies, though cattle, horses, camels, donkeys and the Asian water buffalo , among others, have been introduced by humans. It is estimated that less than three percent of savanna ecosystems can be classified as highly intact. Reasons for savanna degradation are manifold, as outlined below. Savannas are subject to regular wildfires and

1296-499: The East African savannas, Acacia , Combretum , baobabs , Borassus , and Euphorbia are a common vegetation genera. Drier savannas there feature spiny shrubs and grasses, such as Andropogon , Hyparrhenia , and Themeda . Wetter savannas include Brachystegia trees and Pennisetum purpureum , and elephant grass type. West African savanna trees include Anogeissus , Combretum , and Strychnos . Indian savannas are mostly cleared, but

1350-513: The Northern Territory, Australia savanna, and 480,000 ha of savanna were being cleared annually in Queensland in the 2000s, primarily to improve pasture production. Substantial savanna areas have been cleared of woody vegetation and much of the area that remains today is vegetation that has been disturbed by either clearing or thinning at some point in the past. Clearing is carried out by

1404-505: The Rock running east-west to channel the water to the existing reservoirs. The catchment which was the original idea of the then City Engineer of Gibraltar and was constructed in 1903 on the Great Sand Dune which has an average inclination of 1⅓ to 1. The largest of the boulders embedded in the dune were blasted away in order to trim the surface as even as possible. A footpath and channel for the collection of rainwater were constructed along

1458-526: The base of the cliff right down to sea level (at that time there was no road where Sir Herbert Miles Road is today). The occasional rockfall from the precipice above added boulders to the dune so the formation seen today is a consolidated composite of rocks and windblown sands. The upper limits of the dune were scarped by the British garrison for two reasons - to avoid soldiers deserting the place and to prevent surprise attacks by Spanish troops. The Great Sand Dune

1512-445: The catchment construction. By 2006 the slope was entirely restored to its natural state and is now completely covered in vegetation native to the habitat of Gibraltar. Savanna A savanna or savannah is a mixed woodland - grassland (i.e. grassy woodland) biome and ecosystem characterised by the trees being sufficiently widely spaced so that the canopy does not close. The open canopy allows sufficient light to reach

1566-631: The centuries. In 1898, the construction on the waterworks began with the construction of four 5,000,000 imperial gallons (23,000,000 L) reservoirs cut inside the western side of the Rock at an elevation of 103.6 metres (340 ft) above sea level, each being 60.96 metres (200.0 ft) long 15.24 metres (50.0 ft) high and with an average width of 6.1 metres (20 ft), with a total capacity of 22,727 square metres (244,630 sq ft). They were officially inaugurated by Governor of Gibraltar Sir George White in 1901. These reservoirs were initially fed by relatively small water catchment areas on

1620-415: The court of the cacique Carlos in present-day Panama . The accounts are inexact, but this is usually placed in present-day Madugandí or at points on the nearby Guna Yala coast opposite Ustupo or on Point Mosquitos . These areas are now either given over to modern cropland or jungle . Many grassy landscapes and mixed communities of trees, shrubs, and grasses were described as savanna before

1674-555: The ecosystem appears to be the result of human use of fire. For example, Native Americans created the Pre-Columbian woodlands of North America by periodically burning where fire-resistant plants were the dominant species. Aboriginal burning appears to have been responsible for the widespread occurrence of savanna in tropical Australia and New Guinea , and savannas in India are a result of human fire use. The maquis shrub savannas of

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1728-467: The establishment, growth and survival of plant species and in turn can lead to a change in woodland structure and composition. That being said, impact of grazing animals can be reduced. Looking at Elephant impact on Savannas, the overall impact is reduced in the presence of rainfall and fences. Large areas of Australian and South American savannas have been cleared of trees, and this clearing continues today. For example, land clearing and fracking threaten

1782-483: The grazing industry in an attempt to increase the quality and quantity of feed available for stock and to improve the management of livestock. The removal of trees from savanna land removes the competition for water from the grasses present, and can lead to a two to fourfold increase in pasture production, as well as improving the quality of the feed available. Since stock carrying capacity is strongly correlated with herbage yield, there can be major financial benefits from

1836-402: The ground to support an unbroken herbaceous layer consisting primarily of grasses. Four savanna forms exist; savanna woodland where trees and shrubs form a light canopy, tree savanna with scattered trees and shrubs, shrub savanna with distributed shrubs, and grass savanna where trees and shrubs are mostly nonexistent. Savannas maintain an open canopy despite a high tree density. It

1890-554: The lower limits of savanna tree coverage as 5–10% and upper limits range as 25–80% of an area. Two factors common to all savanna environments are rainfall variations from year to year, and dry season wildfires . In the Americas , e.g. in Belize , Central America , savanna vegetation is similar from Mexico to South America and to the Caribbean . The distinction between woodland and savanna

1944-469: The lower perimeter of the catchment area. Timber piles 1,500 millimetres (59 in) x 150 millimetres (5.9 in) x 40 millimetres (1.6 in) were driven their full length into the smoothed dune. To these a timber framing of 75 millimetres (3.0 in) x 75 millimetres (3.0 in) x 4,500 millimetres (180 in) purlins and 75 millimetres (3.0 in) x 75 millimetres (3.0 in) x 2,400 millimetres (94 in) rafters were nailed to them which

1998-461: The middle of a word, is pronounced almost like an English v; hence the change of grapheme when transcribed into English. The word originally entered English as the Zauana in a description of the ilands of the kinges of Spayne from 1555. This was equivalent in the orthography of the times to zavana (see history of V ). Peter Martyr reported it as the local name for the plain around Comagre,

2052-425: The middle of the 19th century, when the concept of a tropical savanna climate became established. The Köppen climate classification system was strongly influenced by effects of temperature and precipitation upon tree growth, and oversimplified assumptions resulted in a tropical savanna classification concept which considered it as a "climatic climax" formation. The common usage to describe vegetation now conflicts with

2106-468: The new Sandy Bay after a considerable public investment to recover the almost non-existent beach. The works enlarged the beach with approximately 50,000 tons of sand imported from Laayoune in the Western Sahara . Two curved groynes and a frontal breakwater were constructed to protect the beach from the full erosional impact of wave action and trap shifting sand, including a submerged breakwater connecting

2160-469: The open structure of savannas allows the growth of a herbaceous layer and is commonly used for grazing domestic livestock. As a result, much of the world's savannas have undergone change as a result of grazing by sheep, goats and cattle, ranging from changes in pasture composition to woody plant encroachment . The removal of grass by grazing affects the woody plant component of woodland systems in two major ways. Grasses compete with woody plants for water in

2214-438: The potential to significantly alter the structure and composition of savannas worldwide, and have already done so in many areas through a number of processes including altering the fire regime, increasing grazing pressure, competing with native vegetation and occupying previously vacant ecological niches. Other plant species include: white sage, spotted cactus, cotton seed, rosemary. Human induced climate change resulting from

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2268-431: The removal of trees, such as assisting with grazing management: regions of dense tree and shrub cover harbors predators, leading to increased stock losses, for example, while woody plant cover hinders mustering in both sheep and cattle areas. A number of techniques have been employed to clear or kill woody plants in savannas. Early pastoralists used felling and girdling , the removal of a ring of bark and sapwood , as

2322-580: The reserved ones feature Acacia, Mimosa , and Zizyphus over a grass cover comprising Sehima and Dichanthium . The Australian savanna is abundant with sclerophyllous evergreen vegetation, which include the eucalyptus , as well as Acacia, Bauhinia , Pandanus with grasses such as Heteropogon and kangaroo grass (Themeda). Animals in the African savanna generally include the giraffe, elephant, buffalo, zebra, gnu, hippopotamus, rhinoceros, and antelope, where they rely on grass and/or tree foliage to survive. In

2376-449: The same region. Savannas are also characterised by seasonal water availability, with the majority of rainfall confined to one season. They are associated with several types of biomes , and are frequently in a transitional zone between forest and desert or grassland , though mostly a transition between desert to forest. Savanna covers approximately 20% of the Earth's land area. Unlike

2430-515: The soil caused by the hooves of animals and through the erosion effects caused by the removal of protective plant cover. Such effects are most likely to occur on land subjected to repeated and heavy grazing. The effects of overstocking are often worst on soils of low fertility and in low rainfall areas below 500 mm, as most soil nutrients in these areas tend to be concentrated in the surface so any movement of soils can lead to severe degradation. Alteration in soil structure and nutrient levels affects

2484-606: The spread of weeds in savannas by the removal or reduction of the plants which would normally compete with potential weeds and hinder establishment. In addition to this, cattle and horses are implicated in the spread of the seeds of weed species such as prickly acacia ( Acacia nilotica ) and stylo ( Stylosanthes species). Alterations in savanna species composition brought about by grazing can alter ecosystem function, and are exacerbated by overgrazing and poor land management practices. Introduced grazing animals can also affect soil condition through physical compaction and break-up of

2538-519: The structure of woodlands and geographic range of numerous woodland species. It has been suggested by many authors that with the removal or alteration of traditional burning regimes many savannas are being replaced by forest and shrub thickets with little herbaceous layer. The consumption of herbage by introduced grazers in savanna woodlands has led to a reduction in the amount of fuel available for burning and resulted in fewer and cooler fires. The introduction of exotic pasture legumes has also led to

2592-463: The topsoil and removal by grazing reduces this competitive effect, potentially boosting tree growth. In addition to this effect, the removal of fuel reduces both the intensity and the frequency of fires which may control woody plant species. Grazing animals can have a more direct effect on woody plants by the browsing of palatable woody species. There is evidence that unpalatable woody plants have increased under grazing in savannas. Grazing also promotes

2646-445: The western side of The Rock. They were officially opened by Governor George Stuart White in 1901. These reservoirs were fed by relatively small water catchment areas on the western side of The Rock. The water catchments above Sandy Bay were built in stages between 1903 and 1961, and were designed to cater for Gibraltar's ever increasing demand. The original plan was to cover an area of 10 acres (40,000 m ). Between 1911 and 1914

2700-482: The western side of the Rock above the Moorish Castle . As Gibraltar's population and demand for a fresh water supply increased, further sources of supply were required and a scheme to expand the system was proposed and carried out. This consisted of the construction of a 40,000 square metres (4.0 ha) water catchment area on the east side of the Rock and the driving of an 800 metres (2,600 ft) tunnel through

2754-665: The world. Amongst the woody plant species are serious environmental weeds such as Prickly Acacia ( Acacia nilotica ), Rubbervine ( Cryptostegia grandiflora ), Mesquite ( Prosopis spp.), Lantana ( Lantana camara and L. montevidensis ) and Prickly Pear ( Opuntia spp.). A range of herbaceous species have also been introduced to these woodlands, either deliberately or accidentally including Rhodes grass and other Chloris species, Buffel grass ( Cenchrus ciliaris ), Giant rat's tail grass ( Sporobolus pyramidalis ) parthenium ( Parthenium hysterophorus ) and stylos ( Stylosanthes spp.) and other legumes . These introductions have

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2808-466: Was closed indefinitely. However, in 2007 its reopening was suggested by the Government to ease traffic flow in the area of the new Rosia residential developments . The tunnel re-opened in November 2010, on completion of extensive engineering works. Sandy Bay is home to one of the few residential areas on the east side of The Rock, known as Both Worlds. On 25 June 2014, officials of Gibraltar inaugurated

2862-425: Was constantly shifting right up to the late 19th century when corrugated iron sheets were laid over the dune for the collection of rainwater. John White described this and the efforts to make it inaccessible: "The Eastern side of the hill consists of an immense sloping bank of whitish sand interspersed with huge fragments of rock, and reaching from the sea nearly to the summit of the rock in some parts not far from

2916-448: Was followed by screwing corrugated galvanised iron sheets 2,400 millimetres (94 in) x 900 millimetres (35 in) round the edges. The timber had been previously pressure treated with creosote at a pressure of 170 pounds per square inch (1,200 kPa). Further expansions of the Great Sand Dune catchments were carried out in stages up until 1961. The original plan was to cover an area of 10 acres (40,000 m). Between 1911 and 1914

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