Dundrum Bay

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Coordinates54°13′43″N 5°46′9″W / 54.22861°N 5.76917°W / 54.22861; -5.76917
EtymologyPossibly from Old Irish Loch Rudraige
Dundrum Bay
Loch Rudraige (Old Irish)
View of Dundrum Inner Bay from Marlough Quay
Inner Dundrum Bay
LocationDundrum, County Down, Northern Ireland
Coordinates54°13′43″N 5°46′9″W / 54.22861°N 5.76917°W / 54.22861; -5.76917
TypeBay
EtymologyPossibly from Old Irish Loch Rudraige
Part ofIrish Sea
Primary inflowsCarrigs River, Moneycarragh River, Blackstaff River, Ardilea River
Primary outflowsIrish Sea
Basin countriesUnited Kingdom
DesignationArea of Special Scientific Interest (ASSI), part of Murlough Nature Reserve
Max. length8 km (5.0 mi)
Max. width5 km (3.1 mi)
Average depth2 m (6.6 ft) (minimum at anchoring pool)
Surface elevation0 m (0 ft)
FrozenNo
IslandsNone
Sections/sub-basinsInner Bay, Outer Bay
SettlementsDundrum
References[1]
Location

Dundrum Bay (Old Irish Loch Rudraige) is a bay located next to Dundrum, County Down, Northern Ireland. It is divided into the Outer Bay, and the almost entirely landlocked Inner Bay. They are separated by the dune systems of Ballykinler to the north and Murlough to the south.

Dundrum Harbour is a small, sheltered harbour located at the head of Dundrum Bay on the northeastern coast of Ireland, roughly midway between Carlingford and Strangford Loughs. Positioned within a tidal estuary, it provides a secure anchorage near the old town quay. However, access requires careful navigation due to a shifting sandbar at the entrance and a narrow estuary channel. The harbour is best suited for shallow-draft vessels and should only be approached on a rising tide, in calm sea conditions, and with clear visibility. Approaching the bay during onshore winds is hazardous, as strong in-draughts and heavy seas can trap vessels. Southerly winds, in particular, make the estuary impassable.[2]

History

Walter Harris wrote in 1744 that the 'North and South Tides meeting off this Bay and breaking upon St John's Point occasion a greater eddy or suction inwards than in other places; for many ships have found themselves embayed.'[3] Local historian John W Hanna described in the 1860's how 'not a foot of the shore from St John's Point to Annalong but has from time to time been strewn with the broken masts and timbers of Royal and merchant ships.'[3] The worst loss of life was 74 crew and 11 fishing boats on 13 January 1843.[3]

SS Great Britain

The bay was home to the SS Great Britain for a year having run aground on a sandbar in 1846.[4] In 1846, the SS Great Britain, an innovative iron-hulled steamship designed by Isambard Kingdom Brunel, ran aground in Dundrum Bay, Northern Ireland, due to a navigational error. Though no lives were lost, the ship remained stranded for nearly a year before being successfully salvaged in 1847 using pioneering techniques. In 2024, archaeologists from the University of Bristol used magnetic survey equipment to locate the exact grounding site at Tyrella Beach, identifying a buried ring of iron debris matching the ship’s shape.[5]

Dundrum Harbour

The harbour, located at the head of Dundrum Bay, was historically a small tidal port used primarily for importing coal and occasionally exporting pit props. Due to increasing ship sizes and the navigational challenges posed by a shifting sandbar, commercial operations ceased in 1984.[6] The harbour, once operated by the East Downshire Steamship Company, fell into disrepair by the late 1990s, with several buildings, including a former coal store, left decaying. Since then, the area has been redeveloped for residential use, with apartment complexes now overlooking the estuary. The harbour lies within a hammerhead-shaped tidal inlet, accessed via a narrow channel through sand hills, and is overlooked by the ruins of a Norman castle. The nearby village of Dundrum sits behind the quay.[7]

Dune systems

The Dundrum Bay complex is located on the southeast coast of County Down, Northern Ireland. It includes four main natural features: the Murlough and Ballykinler dune systems, and Dundrum Outer and Inner Bays. The area stretches from St. John’s Point in the east to the Mourne Mountains in the southwest, focusing specifically on the section between Craigalea Rocks and the mouth of the Glen River in Newcastle.[8]

The geological history of the area was first noted in an 1871 Geological Survey map, which showed raised beaches and ancient sea levels behind the dune systems.[9] Interest in the area grew in the 1950s and 60s when researcher Stephens studied the Murlough dunes, particularly the raised gravel ridges.[10] He linked these features to sea level changes during the mid-Holocene period (around 6000–5000 years ago). Although Stephens published limited detailed findings, his work influenced later interpretations of sea level changes along Ireland’s east coast.[10]

Coastal path

References

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