River Tolka

The Tolka has many tributaries, the first major one being the Castle Stream at Dunboyne. There are at least fourteen infalls within Dublin City boundaries (the count is complicated by connections with the Wad River system).

Dublin City Council area tributaries include the East and West Pinkeen Streams, and another waterway in semi-rural Dublin, then the Scribblestown Stream (visible from Abbotstown to past Dunsink), the Finglaswood (or Mount Olivat) Stream from around Cappagh, the Finglas River (joined by a stream from St. Margaret's Road), the Claremont Stream which joins the Tolka near Bon Secours Hospital, the Cemetery Drain (so-called as it runs near Glasnevin Cemetery) before joining the Tolka just past the Botanic Gardens, the Hamstead Stream (from the area now occupied by Hamstead Park and DCU), inflowing somewhat downstream of Mobhi Bridge, and a small stream from around St. Patrick's Teacher Training College, Drumcondra.[4]

The last few tributaries connect to the tidal part of the Tolka, or its estuary, but have been confused by the merging of natural watercourses and city drainage lines. There are at least four such watercourses, including the multi-branched water sometimes called the "Grace Park Stream", another sometimes "Middle Arch Stream" and the Marino Stream.[4][5]

The Wad River system, coming from north Ballymun, interconnects with the Tolka, most notably via a link with the Claremont Stream, and with the Wad River Diversion, which flows along Ballymun Road and Glasnevin Avenue (the Wad's main outfall to the sea is at Clontarf, not far east from the Tolka's mouth).[6]

The path of the river through Dublin takes it through a number of parks. It passes initially through the Tolka Valley Linear Park near Blanchardstown, then between trees north of River Road, then along the southern edge of the Tolka Valley Park in the western City Council area, where it receives a tributary which provides the source of water for a pond featuring considerable birdlife, including swans, ducks and herons. A large landscaped pitch and putt facility operated by Dublin City Council is situated on the southern side of the park, just south of the meandering river.

The river then flows past the tree-lined recreational areas adjacent to Glasnevin Woods and Violet Hill and forms the northern boundary of Glasnevin (Prospect) Cemetery before meeting the National Botanic Gardens. The river forms the northern border of the Botanic Gardens except for the beautiful Rose Gardens situated on the northern side and accessed via a bridge. Thereafter it passes Glasnevin village and flows into Griffith Park where it forms a major feature of the park.[4] Having passed by Drumcondra village, the river runs behind housing, and the green spaces at the Archbishop's Palace and Clonliffe College, before coming to Ballybough. Below Annesley Bridge at Fairview, around which was originally the river mouth, before reclamation, it runs beyond one last green space, Fairview Park, and turns to reach the sea between East Wall and western Clontarf.[5]

The river floods infrequently but with occasional severity. It is not "flashy" like the Dodder but builds up over a period. Notable floods occurred in October 1880, December 1954, November 1965, August 1986 (Hurricane Charley), November 2000, November 2002, January and April 2005, August 2008 and October 2011; those of 1954 and 2002 were the most severe.

In November 2002, flooding caused extensive damage to residential areas along the Tolka banks. After this, much work was done to strengthen the river's flood defences, and following heavy flooding in 2005, major works to deepen and widen the river were carried out on a number of stretches most notably at Glasnevin Woods and at Drumcondra Bridge. Controversially, the small natural waterfall at Glasnevin Woods was replaced by an artificial stepped fall.

Analysis of the hydrological conditions giving rise to the 2002 flood showed that the classic conditions for a severe flood in the Tolka occurred, these being winter conditions with heavy rain in the previous days and weeks leading to saturated conditions followed by sustained severe rain over around 48 hours.