Old Red Sandstone

Old Red Sandstone Stratigraphic range: late Silurian to earliest Carboniferous
Cross-section showing quartz and chert pebbles in a sample from central England (scale bar is 10 mm).
Type	Supergoup
Lithology
Primary	Sandstone
Other	Conglomerate, shale, mudstone, siltstone, limestone
Location
Region	North Atlantic
Extent	700 km[1]

Hutton's angular unconformity at Siccar Point where 370-million-year-old Devonian Old Red Sandstone overlies 435-million-year-old Silurian greywacke.^[2]

The Old Red Sandstone is an assemblage of rocks in the North Atlantic region largely of Devonian age. It extends in the east across Britain, Ireland and Norway and in the west along the northeastern seaboard of North America. It also extends northwards into Greenland and Svalbard.^[3] In Britain it is a lithostratigraphic unit (a sequence of rock strata) to which stratigraphers accord supergroup status^[4] and which is of considerable importance to early paleontology. For convenience the short version of the term, ORS is often used in literature on the subject. The term was coined to distinguish the sequence from the younger New Red Sandstone which also occurs widely throughout Britain.

Sedimentology

Bedding plane of Old Red Sandstone with quartz and chert pebbles, central England; scale bar is 10 mm

The Old Red Sandstone describes a suite of sedimentary rocks deposited in a variety of environments during the Devonian but extending back into the late Silurian and on into the earliest part of the Carboniferous. The body of rock, or facies, is dominated by alluvial sediments and conglomerates at its base, and progresses to a combination of dunes, lakes and river sediments.

The familiar red colour of these rocks arises from the presence of iron oxide but not all the Old Red Sandstone is red or sandstone — the sequence also includes conglomerates, mudstones, siltstones and thin limestones and colours can range from grey and green through red to purple. These deposits are closely associated with the erosion of the Caledonian Mountain chain which was thrown up by the collision of the former continents of Avalonia, Baltica and Laurentia to form the Old Red Sandstone Continent- an event known as the Caledonian Orogeny.

Many fossils are found within the rocks, including early fishes, arthropods and plants. The rocks may appear paleontologically barren to amateur geologists but careful study, particularly with an accomplished fossil hunter, can uncover pockets of fossils. Rocks of this age were also laid down in southwest England (hence the name 'Devonian') though these are of true marine origin and are not included within the Old Red Sandstone.^[1]

Stratigraphy

Since the Old Red Sandstone consists predominantly of rocks of terrestrial origin, it does not generally contain marine fossils which would otherwise prove useful in correlating one occurrence of the rock with another, both between and within individual sedimentary basins. Accordingly, local stage names were devised and these remain in use to some extent today though there is an increasing use of international stage names. Thus in the Anglo-Welsh Basin, there are frequent references to the Downtonian, Dittonian, Breconian and Farlovian stages in the literature. The existence of a number of distinct sedimentary basins throughout Britain has been established.^[1]

The Orcadian Basin

Lower Old Red Sandstone at Yesnaby, Orkney, cross-bedded aeolian sandstone

The Orcadian Basin extends over a wide area of North East Scotland and the neighbouring seas. It encompasses the Moray Firth and adjoining land areas, Caithness, Orkney and parts of Shetland. South of the Moray Firth, two distinct sub-basins are recognised at Turriff and at Rhynie. The sequence is more than 4 km thick in parts of Shetland. The main basin is considered to be an intramontane basin resulting from crustal rifting associated with post-Caledonian extension, possibly accompanied by strike-slip faulting along the Great Glen Fault system.^[5]

The Midland Valley of Scotland

The Midland Valley graben defined by the Highland Boundary Fault in the north and the Southern Uplands Fault in the south harbours not only a considerable amount of Old Red Sandstone sedimentary rocks but also igneous rocks of this age assciated with extensive volcanism. There is a continuous outcrop along the Highland Boundary Fault from Stonehaven on the North Sea coast to Helensburgh and beyond to Arran. A more disconnected series of outcrops occur along the line of the Southern Uplands Fault from Edinburgh to Girvan. Old Red Sandstone often occurs in conjunction with conglomerate formations, one such noteworthy cliffside exposure being the Fowlsheugh Nature Reserve, Kincardineshire.

The Scottish Borders

A series of outcrops occur from East Lothian southwards through Berwickshire. Hutton's famous unconformity at Siccar Point occurs within this basin - see History of study below.

The Anglo-Welsh Basin

This relatively large basin extends across much of South Wales from southern Pembrokeshire in the west through Carmarthenshire into Powys and Monmouthshire and through the southern Welsh Marches, notably into Herefordshire, Worcestershire and Gloucestershire. Outliers in Somerset and north Devon complete the extent of this basin.

With the exception of south Pembrokeshire, all parts of the basin are represented by a range of lithologies assigned to the Lower Devonian and to the Upper Devonian, the contact between the two being unconformable and representing the complete omission of any Middle Devonian sequence. The lowermost formations are of upper Silurian age, these being the Downton Castle Sandstone Formation and the overlying Raglan Mudstone Formation except in Pembrokeshire where a more complex series of formations is recognised. In the east of the basin, the top of the Raglan Mudstone is marked by a well-developed calcrete, the Bishop's Frome Limestone.^[6] The lowermost Devonian formation is the St Maughans Formation, itself overlain by the Brownstones Formation though with an intervening Senni Formation over much of the area. The Upper Devonian sequence is rather thinner and comprises a series of formations which are more laterally restricted. In the Brecon Beacons, the Plateau Beds Formation is unconformably overlain by the Grey Grits Formation though further east these divisions are replaced by the Quartz Conglomerate Group which is itself subdivided into a variety of different formations.

Pembrokeshire

The sequence in Pembrokeshire differs from that of the main part of the basin and falls into two parts.^[7] In North Pembrokeshire to the north of the Ritec Fault, both the middle and upper ORS are missing with only the lower ORS present; this is divided into an earlier Milford Haven Group comprising in ascending order, the Red Cliff, Sandy Haven and Gelliswick Bay formations and a later Cosheston Group with, again in ascending order, its constituent Llanstadwell, Burton Cliff, Mill Bay, Lawrenny Cliff and New Shipping formations. These respectively equate with the Temeside, Raglan Mudstone and St Maughans formations of the central and eastern part of the basin.

• - middle and upper ORS missing -
• Cosheston Group
  • New Shipping Formation
  • Lawrenny Cliff Formation
  • Mill Bay Formation
  • Burton Cliff Formation
  • Llanstadwell Formation
• Milford Haven Group
  • Gelliswick Bay Formation
  • Sandy Haven Formation (inc. Townsend Tuff Beds)
  • Albion Sands Formation / Lindsway Bay Formation
  • Red Cliff Formation

In South Pembrokeshire to the south of the Ritec Fault, the lower ORS is represented by, in ascending order, the Freshwater East, Moors Cliff and Freshwater West formations. These are unconformably overlain by the Ridgeway Conglomerate Formation. The middle ORS is missing whilst the Upper ORS is represented by the Gupton and West Angle formations.

• Skrinkle Sandstone Group
  • West Angle Formation
  • Gupton Formation
• - part of middle ORS missing -
• Ridgeway Conglomerate Formation
• - part of middle ORS missing -
• Milford Haven Group
  • Freshwater West Formation (inc. Rat Island Mudstone Member and Conigar Pit Sandstone Member)
  • Moor Cliffs Formation (inc Chapel point calcretes member and Townsend Tuff Bed)
  • Freshwater East Formation

The Freshwater East Formation, and corresponding Red Cliff Formation of north Pembrokeshire, are both late Silurian in age.^[8]

Anglesey

A small and separate basin exists here where both alluvial and lacustrine deposits are recorded. Both the middle and upper ORS are missing but the lower ORS is represented, in ascending order, by the Bodafon, Traeth Bach, Porth y Mor and Traeth Lligwy formations. Calcretes are also recorded representing carbonate-rich soils developed between periods of sediment deposition. The present day outcrop occupies a narrow zone from Dulas Bay on Anglesey's northeast coast, southwards to the town of Llangefni.^[1][9]

History of study

In 1787 James Hutton noted what is now known as Hutton's Unconformity at Inchbonny, Jedburgh, and in the spring of 1788 he set off with John Playfair to the Berwickshire coast and found more examples of this sequence in the valleys of the Tower and Pease Burns near Cockburnspath.^[10] They then took a boat trip from Dunglass Burn east along the coast with the geologist Sir James Hall of Dunglass and at Siccar Point found what Hutton called "a beautiful picture of this junction washed bare by the sea",^[11] where 345-million-year-old Old Red Sandstone overlies 425-million-year-old Silurian greywacke.^[2][12]

In the early 19th century, the paleontology of the formation was studied intensively by Hugh Miller, Henry Thomas De la Beche, Roderick Murchison, and Adam Sedgwick—Sedgwick's interpretation was the one that placed it in the Devonian: in fact it was he who coined the name of that period. The term 'Old Red Sandstone' was originally used in 1821 by Scottish naturalist and mineralogist Robert Jameson to refer to the red rocks which underlay the 'Mountain Limestone' i.e. the Carboniferous Limestone. They were thought at that time to be the British version of Germany's Rotliegendes, which is in fact of Permian age.^[1] Many of the science of stratigraphy's early debates were about the Old Red Sandstone.

Note that in older geological works predating theories of plate tectonics, the United States' Catskill Delta formation is sometimes referred to as part of the Old Red Sandstone. In the modern day, however, it is recognized that the two are not stratigraphically continuous but are very similar due to being formed at approximately the same time by the same processes.

Use as a Building Stone

St. Helen's Chapel at Siccar Point has walls faced in Old Red Sandstone, with greywacke used on the inner face and surrounding drystane dykes.

The Old Red Sandstone has been widely used as a building stone across those regions where it outcrops. Notable examples of its use can be found in the area surrounding Stirling , Stonehaven , Perth , and Tayside. The inhabitants of Caithness at the northeastern tip of Scotland also used the stone to a considerable extent. Old Red Sandstone has also frequently been used in buildings in Herefordshire, Monmouthshire and the former Brecknockshire (now south Powys) of south Wales.

Notable buildings

St Magnus Cathedral, Kirkwall, Orkney, constructed of locally quarried sandstone.

Canada

• New York Life Insurance Building, Montreal

England

• Goodrich Castle, Herefordshire^[13]
• Ross-on-Wye market hall, Herefordshire
• Shrewsbury Castle, Shropshire

Scotland

• Arbroath Abbey, Angus
• Muchalls Castle, Aberdeenshire
• St Magnus Cathedral, Orkney^[14]
• Stonehaven Tolbooth, Aberdeenshire

Wales

• Raglan Castle, Monmouthshire^[13]
• Tintern Abbey, Monmouthshire and ^[13]
• Brecon Cathedral, Powys

See also

• New Red Sandstone
• Geology of Great Britain

References

External links

Wikimedia Commons has media related to Old Red Sandstone.

• Gly.uga.edu: Cawdor Castle — built from Old Red Sandstone.