BLOOMFIELD AREA NEAR THE CONNSWATER SHOPPING CENTRE AND CS LEWIS SQUARE
I am not fully sure how to described the area featured in this series of photographs but, basically, I got a Glider Bus to Connswater and visited the CS Lewis Square. Then I walked along the river as far as the Connswater Shopping Centre and then returned to the Newtownards Road and the on to the Holywood Arches bus stop in order to return to the city centre. To be honest I found the area to be less that attractive but I must admit that I have little interest in shopping centres. CS Lewis Square is well worth a visit.
Bloomfield is contained within the area bounded by the North Road, the Knock River, Connswater River, the top of the Newtownards Road and the Upper Newtownards Road. Modern-day Bloomfield is a ward within Pottinger, one of Belfast City Council’s nine district electoral areas.
The Holywood Arches referred to railway bridges that carried the Belfast & County Down Railway (BCDR) line across the Holywood Road and Upper Newtownards Road to Newtownards via Comber from May 1850. I have been advised that the bridges were not actually located in Holywood and were not arches. The railway line was closed in 1950 after nearly one hundred years in serving the community and the railway bridges were later demolished. However, the stone pillars remained for several years before being demolished in the 1960s.
Connswater Shopping Centre features many discount retailers. The complex was built in east Belfast with work starting in 1983 and being finished by 1994, making it one of Northern Ireland’s oldest shopping centres. It pre-dates CastleCourt in the city centre and the Buttercrane Centre in Newry.
CS Lewis Square is located at the intersection of the Connswater and Comber Greenways, beside the EastSide Visitor Centre, where visitors can access information on the city’s attractions from interactive screens, interpretative panels and a wall map, connecting people to EastSide’s famous faces, places and industries.
CS Lewis Square is open 24 hours a day, seven days a week and are fully illuminated. It features seven bronze sculptures from ‘The Lion, The Witch and The Wardrobe’, including Aslan, The White Witch, Mr Tumnus, The Beavers, The Robin and The Stone Table, it is a stunning display of public art.
The River Poddle is a river in Dublin, Ireland, a pool on which (dubh linn, “black pool” or “dark pool” in Irish) gave the city its English language name. Boosted by a channel made by the Abbey of St. Thomas à Becket, taking water from the far larger River Dodder, the Poddle was the main source of drinking water for the city for more than 500 years, from the 1240s. The Poddle, which flows wholly within the traditional County Dublin, is one of around a hundred members of the River Liffey system (excluding the Dodder tributaries), and one of over 135 watercourses in the county; it had just one significant natural tributary, the Commons Water from Crumlin.
The Poddle rises in the southwest of the Dublin Region, in the Cookstown area, northwest of Tallaght, in the functional area of South Dublin County Council, and flows into the River Liffey at Wellington Quay in central Dublin, overseen by Dublin City Council. Flowing in the open almost to the Grand Canal at Harold’s Cross, its lower reaches, including multiple connected artificial channels, are almost entirely culverted. Aside from supplying potable water for the city from the 13th century to the 18th, to homes, and to businesses including breweries and distilleries, the river also provided wash water for skinners, tanners and dyers. Its volume boosted by a drawing off from the much larger River Dodder, it powered multiple mills, including flour, paper and iron production facilities, from at least the 12th century until the 20th. It also provided water for the moat at Dublin Castle, through the grounds of which it still runs underground.
The Poddle has frequently caused flooding, notably around St. Patrick’s Cathedral, and for some centuries there was a commission of senior state and municipal officials to try to manage this, with the power to levy and collect a Poddle Tax. The flooding led both to the lack of a crypt at the cathedral and to the moving of the graves of satirist Dean Swift, author of Gulliver’s Travels, and his friend Stella. The river and its associated watercourses were famously polluted in certain periods, at one point allegedly sufficiently so as to kill animals drinking the water. The river is mentioned briefly in James Joyce’s novel Ulysses, and multiple times in Finnegans Wake, which mentions its role in Dublin’s growth.
The River Poddle Flood Alleviation Scheme which has been developed in collaboration with the Office of Public Works (OPW), proposes flood protection, flood storage and flood prevention measures at locations along a 6km stretch of the Poddle River from Tymon North, Tallaght to St. Teresa’s Gardens and Donore Avenue, and at the National Stadium, South Circular Road, Merchant’s Quay, Dublin. It combines main flood storage at Tymon Park and additional flood storage at Ravensdale Park, with linear defences along the River where they are required to provide flood protection, new flap valves and culvert screens, and sealing manholes to prevent surcharging during a flood event.
The intervention area of the proposed Flood Alleviation Scheme extends along the Poddle River from Tymon Park (west of the M50) in Tallaght to Mount Argus Close in Harold’s Cross; with further works to seal manholes in the vicinity of Poddle Park and Ravensdale Park, Kimmage, and in St. Teresa’s Gardens and Donore Avenue, and at the National Stadium in Merchant’s Quay, Dublin.
There are three areas where more substantial works are proposed in green spaces and parks, including: • In Tymon Park (east of the M50) where the main flood storage embankment is to be constructed and an Integrated Constructed Wetland (ICW) is also planned; • at Whitehall Park, east of Templeville Road in Templeogue where a channel re-alignment is proposed; and • at Ravensdale Park in Kimmage where flood walls are to be constructed to provide flood protection and storage.
Today I used a Voigtlander 40mm Manual Focus lens.
The river floods surrounding areas from time to time, as it is too short and shallow to hold the volume of water which pours into it from its tributaries during heavy rain. The River Dodder “has a history of flooding and is known as a “flashy” river with a quick response to rainstorms.”
A flood on the Dodder in March 1628 claimed the life of Arthur Ussher, Deputy Clerk to the Privy Council of Ireland, who was “carried away by the current, nobody being able to succour him, although many persons…. his nearest friends, were by on both sides.”
The two greatest Dodder floods before 1986 occurred on 25 August 1905, and on 3 and 4 August 1931. Hurricane Charley (often spelt “Charlie” in Ireland) passed south of the country on 25 August 1986. In 24 hours, 200mm (almost 8 inches) of rain poured down on Kippure Mountain while 100mm fell on Dublin causing heavy river flooding, including the Dodder in many places, and hardship and loss were experienced.
It has long been recognised that the problem of flooding is very difficult to solve, due to the sheer volume of water which pours into the river during periods of heavy rainfall.
THE RIVER SLANG – THE DUNDRUM SLANG OR THE DUNDRUM RIVER
Please correct me if I am wrong whey I say that the stream flowing through the green space in my photographs is the River Slang
The River Slang , also known as the Dundrum Slang or the Dundrum River, a tributary of the River Dodder, is a stream which rises on Three Rock Mountain, County Dublin. It is in the jurisdiction of Dun Laoghaire-Rathdown County Council.
This is new to me. I got off the tram at Windy Arbour and walked along St Columbanus Road which I never visited before and then I came across what could be described as a linear park on the banks of a small stream and I could not decide if I was in Dundrum. Clonskeagh, Milltown or Dundrum. Why Clonskeagh? Because Our Lady’s National School had a sign showing its address as Clonskeagh.
I asked two people who I met on my journey and one said Dundrum and the other said Milltown [the property foe sale advertisements appear to agree]. Later a friend told me that legally it is in Rathmines Great which came as a surprise but according to my friend Rathmines Great is in the Electoral Division of Dundrum, in Civil Parish of Taney, in the Barony of Rathdown, in the County of Dublin.
From Three Rock Woods on the northern slopes of Three Rock Mountain, the Slang flows down through Ticknock, passing Ballinteer north to Dundrum, where it (sometimes known this far as “Ticknock Stream”) receives the Wyckham Stream, and then loops east, north, and west, coming to a mill pond north of the Dundrum Town Centre retail complex. The Slang then runs north via Windy Arbour and subsequently joins the River Dodder at Milltown, near the Nine Arches viaduct, now used by the Luas.
The small Wyckham Stream, joining from the west, is a natural tributary, visible on early maps, but was later connected to the Little Dargle River, further west, to take some of the flow of that river into the Slang, to increase the supply for powering of mills.
Today there is a walk made by the County Council from south Dundrum to Marlay Park, along part of the Slang, the Wyckham Stream, and part of the Little Dargle.
FOLLOWING THE DODDER RIVER FROM MILLTOWN TO CLONSKEAGH
The Dodder lay well beyond the original city of Dublin but began to have an important impact in the 13th century, when water from its course was diverted to boost the small Poddle River, which in turn did supply fresh water to parts of Dublin.
Over centuries, the Dodder and its tributaries drove many mills, crucial to Dublin’s industrial base, but all are now disused. In many cases, all traces have been erased but there are some indications, such as of millraces.
The de Meones family, who gave their name to the nearby suburb of Rathmines, owned a mill in that area as early as the mid-fourteenth century.In the sixteenth century much of the surrounding lands belonged to the Talbot family, ancestors of the Talbots of Mount Talbot. In the seventeenth and eighteenth centuries the Domvile family, who owned much of Templeogue, effectively controlled access to much of the river, which passed through their estates. At that time the Dodder was the main source of Dublin’s drinking water, and whether fairly or unfairly, the Domviles were accused of using their control of the Dublin water supply to further their own selfish ends, by threatening to divert its course if their wishes were not met. In fact the legal right to control the course of the river was vested in the Mayor and Corporation of Dublin; this was confirmed by a legal ruling as early as 1527.
The Dodder rises on the northern slopes of Kippure in the Wicklow Mountains and is formed from several streams. The headwaters flow from Kippure Ridge, and include, and are often mapped solely as, Tromanallison (Allison’s Brook), which is then joined by Mareen’s Brook, including the Cataract of the Brown Rowan, and then the combined flow meeting the Cot and Slade Brooks.
In the river’s valley at Glenasmole are the two Bohernabreena Reservoirs, a major part of the Dublin water supply system.
The Dodder is 26 kilometres (16 mi) long. It passes the Dublin suburbs of Tallaght and then Firhouse, travels by Templeogue, passes Rathfarnham, Rathgar, Milltown, Clonskeagh, and Donnybrook, and goes through Ballsbridge and past Sandymount, before entering the Liffey near Ringsend, along with the Grand Canal, at Grand Canal Dock.
There is a weir just above the bridge at Ballsbridge and the river becomes tidal roughly where the bridge at Lansdowne Road crosses it. The Dodder and the River Tolka are Dublin’s second-largest rivers, after the Liffey.
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