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Everyman Palace Theatre

European theatre stubsIrish building and structure stubsTheatres in Cork (city)
Everyman Palace Theatre MacCurtain Street (5745077424)
Everyman Palace Theatre MacCurtain Street (5745077424)

The Everyman Theatre is a 650-seat Victorian theatre on MacCurtain Street in Cork, Ireland. It opened in 1897, and is the oldest purpose-built theatre building in Cork. The Everyman has undergone a number of changes in name and use, through its days as "Dan Lowrey’s Palace of Varieties" (hosting Laurel and Hardy and Charlie Chaplin), life as a cinema, periods of disrepair, and redevelopment as a modern theatre in the 1990s.The theatre is housed in a listed (protected) Victorian building with a large stage and auditorium, a proscenium arch, four elaborately decorated boxes, a studio space and a bar. The Everyman's programme is a mix of plays, operas, musicals and concerts, but it specialises in drama and usually stages three in-house productions per year. In the summer months, it hosts productions by Irish playwrights. Other recurring events include the Guinness Jazz Festival in October (for which the theatre is a primary venue), and the Christmas pantomime. A unique feature of the Everyman Palace is that its front of house ushering staff is composed entirely of volunteers.

Excerpt from the Wikipedia article Everyman Palace Theatre (License: CC BY-SA 3.0, Authors, Images).

Everyman Palace Theatre
MacCurtain Street, Cork

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N 51.9014 ° E -8.4682 °
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Vanity Hair

MacCurtain Street
T23 VN24 Cork (St. Patrick's A)
Ireland
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Everyman Palace Theatre MacCurtain Street (5745077424)
Everyman Palace Theatre MacCurtain Street (5745077424)
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Metropolitan Cork

Metropolitan Cork is a semi-official term which refers to the city of Cork, Ireland, its suburbs, the rural hinterland that surrounds it, and a number of the towns and villages in that hinterland. Some of the latter towns and villages are within the administrative area of County Cork. The term Metropolitan Cork was used in the Cork Area Strategic Plan to refer to the area whose labour and property market is shared with the city. The plan declared that it was envisaged as an area with "an integrated transport system, and the social, cultural and educational facilities of a modern European city". Metropolitan Cork is the core employment hub of the "Greater Cork" area. The term is loosely defined but has been taken by authorities to include the city of Cork, its suburbs and the towns of Ballincollig, Blarney, Carrigaline, Carrigtwohill, Cobh, Douglas, Glanmire, Glounthaune, Midleton, Passage West and Ringaskiddy.According to the Cork Area Transit System (CATS) Study Final Report of February 2010, at that time, the metropolitan area covered 820km2 and approximately 270,000 people.By mid-2018, legislation was drafted to expand the boundary of Cork city, to include a number of the metropolitan area towns (such as Blarney and Carrigtwohill). This change proposed to bring much of "Metropolitan Cork" within the bounds of the Cork City Council area. On 31 May 2019, the boundary change came into force, with the city bounds being extended to include Ballincollig, Blarney, Glanmire, Rochestown, Grange and Cork Airport, and thereby increasing the city population from 125,000 to approximately 210,000.

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.