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South Mall, Cork

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South Mall Cork City
South Mall Cork City

South Mall (Irish: An Meall Theas) is one of the main streets of Cork city, Ireland. It runs from Grand Parade in the west to Parnell Place in the east. Like Grand Parade and St. Patrick's Street, it is built over what was once a channel of the River Lee.

Excerpt from the Wikipedia article South Mall, Cork (License: CC BY-SA 3.0, Authors, Images).

South Mall, Cork
South Mall, Cork City Centre (Centre A ED)

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Wikipedia: South Mall, CorkContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 51.8971 ° E -8.4697 °
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South Mall 7
T12 A2YT Cork, City Centre (Centre A ED)
Ireland
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South Mall Cork City
South Mall Cork City
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Munster Basin

This the Irish Munster Basin should not be confused with the Münster Basin in northern GermanyThe Munster Basin is a late Middle to Upper Devonian age extensional (rift) sedimentary basin in the south-west of Ireland. The basin fill comprises fluvial Old Red Sandstone (ORS) magnafacies with minor silicic volcanic and mafic sub-volcanic centres. The depocentre of the basin is located between the MacGillycuddy's Reeks and the Kenmare River on the Iveragh peninsula where the succession is at least ca. 6 km thick. The non-marine ORS is conformably succeeded by latest Devonian coastal plain and shallow marine clastic deposits (the Toe Head Sandstone and Old Head Sandstone Formations, and equivalents), followed by shallow to deeper marine Carboniferous sandstones, mudstones and limestones of the South Munster Basin. During the Late Palaeozoic Variscan (or Hercynian) orogeny the deposits in the basin were subjected to compressional deformation that resulted in pressure solution cleavage formation, buckle folding and contractional faulting under very low-grade metamorphic conditions.The oldest deposits found in the Munster Basin belong to the Valentia Slate Formation from which a silicic air-fall tuff bed (the Keel-Enagh Tuff) was radiometrically dated as 384.9 ± 0.7 Ma, which can be linked to local miospore biostratigraphic records. In combination, this corresponds to a late Givetian chronostratigraphic age on recent Devonian time scales. The general Late Devonian age of the basin fill is also given by miospore and fish fossil records.

St. Finbarr's South Church
St. Finbarr's South Church

St. Finbarr's South, also known as the South Chapel, is an 18th century church in Cork in Ireland. Constructed in 1766 as the "first Catholic church built in Cork since before the Reformation", the Penal-era church was deliberately built to be relatively unimposing. It is the oldest Catholic church still in use in Cork city, and is the parish church of St Finbarr's South parish in the Roman Catholic Diocese of Cork and Ross. The church is included in the Record of Protected Structures maintained by Cork City Council.Built of local limestone and red sandstone, the church was commissioned by the then parish priest, Daniel Albert O'Brien, to replace an existing thatched building. O'Brien, who had been appointed as parish priest and vicar general in 1760 by the then Bishop of Cork, Richard Walsh, was a member of the Dominican Order. O'Brien was succeeded as parish priest, in 1774, by Francis Moylan (later Bishop of Cork).Originally built to an "L" shape, the church was extended and an additional transept was added in 1809. The main altar holds a statue, known as The Dead Christ, which was sculpted by John Hogan (1800–1858). A painting of the crucifixion, behind the altar, is attributed by some sources to the artist John O'Keeffe (c.1797–1838). The church was further extended in the 1860s, and additional work undertaken on the altar, in the 1870s, by ecclesiastical architect George Goldie (1828–1887).Notable parishioners include John Stanislaus Joyce, who was baptised in the church in 1849. Other former parishioners include educator Nano Nagle, hospital founder Mary Aikenhead, military general Daniel O'Leary, sculptor John Hogan and Arctic explorer Jerome Collins.