place

Glen Rovers GAA

1916 establishments in IrelandEngvarB from July 2018Gaelic Athletic Association clubs established in 1916Gaelic Athletic Association clubs in County CorkGlen Rovers GAA
Hurling clubs in County Cork

Glen Rovers is a Cork-based Gaelic Athletic Association club based in Blackpool, Cork, Ireland. The club was founded in 1916 and is primarily concerned with the game of hurling. They were Cork senior hurling champions in 2015 and 2016, having won their first title in 26 years in 2015. They retained the championship in 2016, when they beat Erin's Own in the final. Only Blackrock have won more Cork senior hurling championships.

Excerpt from the Wikipedia article Glen Rovers GAA (License: CC BY-SA 3.0, Authors).

Glen Rovers GAA
Old Youghal Road, Cork

Geographical coordinates (GPS) Address Nearby Places
placeShow on map

Wikipedia: Glen Rovers GAAContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 51.906402777778 ° E -8.4674444444444 °
placeShow on map

Address

Collins Barracks

Old Youghal Road
T23 YE35 Cork (Blackpool ED B)
Ireland
mapOpen on Google Maps

Share experience

Nearby Places

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.