The Marros Group is the name given to a suite of rocks of Namurian age laid down during the Carboniferous Period in South Wales . These rocks were formerly known as the Millstone Grit Series but are now distinguished from the similar but geographically separate rock sequences of the Pennines and Peak District of northern England and northeast Wales by this new name.
6-689: The Group comprises a thick unit of coarse sandstone known as the Twrch Sandstone (formerly the ‘Basal Grit’) which is overlain by the Bishopston Mudstone and the Telpyn Point Sandstone . The mudstones of these latter two formations was formerly known as the ‘Middle Shales’, a name reflecting the position of this sequence sandwiched between the Basal Grit below and the Farewell Rock ,
12-601: Is conformable. The Marros Group is named from the locality ( Marros ) in southwest Carmarthenshire where these rocks are well exposed in spectacular coastal cliffs. The Twrch Sandstone derives its name from the vicinity of the Afon Twrch where these beds reach their maximum thickness. The mudstones derive their name from Bishopston on the Gower Peninsula , southwest of Swansea and the Telpyn Point Sandstone from
18-588: The east. Faulted blocks of the Twrch Sandstone and Bishopston Mudstone formations are responsible for much of the dramatic scenery within the national park's Waterfall Country . The Marros Group is underlain by the Carboniferous Limestone , the boundary being unconformable . In contrast, the contact with the overlying Farewell Rock which lies at the base of the South Wales Coal Measures
24-537: The lowermost sandstone of the South Wales Coal Measures , above. The mudstone itself contains a few bands of sandstone such as the ‘Twelve Foot Sandstone’ and locally the ‘Cumbriense Sandstone’. Likewise the Twrch Sandstone contains bands of mudstone, often correlating with marine bands . The sequence as developed along the north crop of the South Wales Coalfield varies along its length but within
30-577: The mudstone which forms the greater thickness of the Bishopston Mudstone Formation, the following are observed: Note that the names of many of the sandstone units are derived from the marine bands (themselves named for diagnostic fossils within them) beneath which they typically occur. Not all of the sandstones occur within any one place, the Subcrenatum thins out to the east whilst the typically double-layered Cumbriense Sandstone thins out to
36-688: The west. Further west in Pembrokeshire the sequence above and including the Sub-Carbonicola is absent and is replaced by the Telpyn Point Sandstone Formation. The Twrch Sandstone Formation gives rise to numerous positive landscape features such as Carreg Dwfn , Tair Carn Uchaf , Gwaun Cefnygarreg in the west of the Brecon Beacons National Park and the plateau surfaces of Mynydd Llangatwg and Mynydd Llangynidr in
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