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Geological map of Central Scotland
The geology of Scotlandmarker is unusually varied for a country of its size, with a large number of differing geological features. There are three main geographical sub-divisions: the Highlands and Islands is a diverse area which lies to the north and west of the Highland Boundary Fault; the Central Lowlandsmarker is a rift valley mainly comprising Paleozoic formations; and the Southern Uplands, which lie south of a second fault line, are largely composed of Silurian deposits.

The existing bedrock includes very ancient Archean gneiss, metamorphic beds interspersed with granite intrusions created during the Caledonian mountain building period (the Caledonian orogeny), commercially important coal, oil and iron bearing carboniferous deposits and the remains of substantial tertiary volcanoes. During their formation, tectonic movements created climatic conditions ranging from polar to desert to tropical and a resultant diversity of fossil remains.

Scotland has also had a role to play in many significant discoveries such as plate tectonics and the development of theories about the formation of rocks and was the home of important figures in the development of the science including James Hutton, (the "father of modern geology") Hugh Miller and Archibald Geikie. Various locations such as 'Hutton's Unconformity' at Siccar Pointmarker in Berwickshire and the Moine Thrustmarker in the north west were also important in the development of geological science.


Overview

The main geographical divisions of Scotland
From a geological and geomorphological perspective the country has three main sub-divisions all of which were affected by Pleistocene glaciations.

Highlands and Islands

The Highlands and Islands lie to the north and west of the Highland Boundary Fault, which runs from Arranmarker to Stonehavenmarker. This part of Scotland largely comprises ancient rocks, from the Cambrian and Precambrian eras, that were uplifted to form a mountain chain during the later Caledonian orogeny. These foundations are interspersed with many igneous intrusions of a more recent age, the remnants of which have formed mountain massifs such as the Cairngormsmarker and Skyemarker Cuillinsmarker. A significant exception to the above are the fossil-bearing beds of Old Red Sandstones found principally along the Moray Firth coast and in the Orkney islands. These rocks are around 400 million years old, and were laid down in the Devonian period. The Highlands are generally mountainous and are bisected by the Great Glen Fault. The highest elevations in the British Islesmarker are found here, including Ben Nevismarker, the highest peak at 1,344 metres (4,409 ft). Scotland has over 790 islands, divided into four main groups: Shetlandmarker, Orkneymarker, and the Hebridesmarker, further sub-divided into the Inner Hebridesmarker and Outer Hebridesmarker.

The Hebridean archipelago outlier of St Kildamarker is composed of Tertiary igneous formations of granites and gabbro, heavily weathered by the elements. These islands represent the remnants of a long extinct ring volcano rising from a seabed plateau approximately 40 m (130 ft) below sea level.

The geology of Shetland is complex with numerous faults and fold axes. These islands are the northern outpost of the Caledonian orogeny and there are outcrops of Lewisian, Dalriadan and Moine metamorphic rocks with similar histories to their equivalents on the Scottish mainland. Similarly, there are also Old Red Sandstone deposits and granite intrusions. The most distinctive feature is the ultrabasic ophiolite peridotite and gabbro on Unstmarker and Fetlarmarker, which are remnants of the Iapetus Ocean floor. Much of Shetland's economy depends on the oil-bearing sediments in the surrounding seas.

Midland Valley

Often referred to as the Central Lowlandsmarker, this is a rift valley mainly comprising Paleozoic formations. Many of these sediments have economic significance for it is here that the coal and iron bearing rocks that fuelled Scotland's industrial revolution are to be found. This area has also experienced intense vulcanism, Arthur’s Seatmarker in Edinburghmarker being the remnant of a once much larger volcano active in the Carboniferous period some 300 million years ago. This area is relatively low-lying, although even here hills such as the Ochilsmarker and Campsie Fellsmarker are rarely far from view.

Southern Uplands

The Southern Uplands
The Southern Uplands are a range of hills almost 200 km (125 miles) long, interspersed with broad valleys. They lie south of a second fault line running from Ballantraemarker towards Dunbarmarker. The geological foundations largely comprise Silurian deposits laid down some 4-500 million years ago.

Post-glacial events

The whole of Scotland was covered by ice sheets during the Pleistocene ice ages and the landscape is much affected by glaciation, and to a lesser extent by subsequent sea level changes. In the post-glacial epoch, circa 6100 BC, Scotland and the Faeroe Islandsmarker experienced a tsunami up to 20 metres high caused by the Storegga Slidesmarker, an immense underwater landslip off the coast of Norway. Earth tremors are infrequent and usually slight. The Great Glen is the most seismically active area of Britain, but the last event of any size was in 1901.

Chronology

Archean and Proterozoic eras

The oldest rocks of Scotland are the Lewisianmarker gneisses, which were laid down in the Precambrian period, up to 3,000 Ma (million years ago). They are the oldest in Europe and amongst the oldest rocks in the world. They form basement deposits to the west of the Moine Thrustmarker on the mainland, in the Outer Hebridesmarker and on the islands of Collmarker and Tireemarker. These rocks are largely igneous in origin, mixed with metamorphosed marble, quartzite and mica schist and intruded by later basaltic dykes and granite magma. One of these intrusions forms the summit plateau of the mountain Roineabhalmarker in Harrismarker. The granite here is anorthosite, and is similar in composition to rocks found in the mountains of the Moon.
Torridonian sandstones were also laid down in this period over the gneisses, and these contain the oldest signs of life in Scotland. In later Precambrian times, thick sediments of sandstones, limestones muds and lavas were deposited in what is now the Highlands of Scotland.

Paleozoic era

Cambrian period

Further sedimentary deposits were formed through the Cambrian period, (542–488 Ma) some of which, along with the earlier Precambrian sediments, metamorphosed into the Dalradian series. This is composed of a wide variety of materials, including mica schist, biotite gneiss schist, schistose grit, greywacke and quartzite. The area that would become Scotland was at this time close to the south pole and part of Laurentia. Fossils from the north-west Highlands indicate the presence of trilobites and other primitive forms of life.

Ordovician period

The proto-Scotland landmass moved northwards and from 460–430 Ma sandstone, mudstone and limestone was deposited in the area that is now the Midland Valleymarker. This occurred in shallow tropical seas at the margins of the Iapetus Ocean. The Ballantrae Complex near Girvanmarker was formed from this ocean floor and is similar in composition to rocks found at The Lizardmarker in Cornwallmarker. Nonetheless, northern and southern Britain were far apart at the beginning of this period, although the gap began to close as the continent of Avalonia broke away from Gondwana, collided with Baltica and drifted towards Laurentia. The Caledonian orogeny began forming a mountain chain from Norway to the Appalachiansmarker. There was an ice age in the southern hemisphere, and the first mass extinction of life on Earth took place at the end of this period.

Silurian period

The collision of Avalonia, Baltica and Laurentia.
(The names are in French).
During the Silurian period (443–416 Ma) the continent of Laurentia gradually collided with Baltica, joining Scotland to the area that would become England and Europe. Sea levels rose as the Ordovician ice sheets melted, and tectonic movements created major faults which assembled the outline of Scotland from previously scattered fragments. These faults are the Highland Boundary Fault, separating the Lowlands from the Highlands, the Great Glen Fault that divides the North-west Highlands from the Grampians, the Southern Uplands Fault and the Iapetus Suture, which runs from the Solway Firthmarker to Lindisfarnemarker and which marks the close of the Iapetus Ocean and the joining of northern and southern Britain.

Silurian rocks form the Southern Uplands of Scotland, which were pushed up from the sea bed during the collision with Baltica/Avalonia. The majority of the rocks are weakly metamorphosed coarse greywacke. The Highlands were also affected by these collisions, creating a series of thrust faults in the northwest Highlands including the Moine Thrustmarker, the understanding of which played an important role in nineteenth century geological thinking. Volcanic activity occurred across Scotland as a result of the collision of the tectonic plates, with volcanoes in southern Scotland, and magma chambers in the north, which today form the granite mountains such as the Cairngormsmarker.

Devonian period

The Old Red Sandstone Continent in the Devonian
The Scottish landmass now formed part of the Old Red Sandstone Continent and lay some 25 degrees south of the equator, moving slowly north during this period to 10 degrees south. The accumulations of Old Red Sandstone laid down from 408 to 370 million years ago were created as earlier Silurian rocks, uplifted by the formation of Pangaea, eroded and were deposited into a body of fresh water (probably a series of large river deltas). A huge freshwater lake - the Orcadian Lake - existed on the edges of the eroding mountains stretching from Shetland to the southern Moray Firth. The formations are extremely thick, up to 11,000 meters in places, and can be subdivided into three categories "Lower", "Middle", and "Upper" from oldest to youngest. As a result, the Old Red Sandstone is an important source of fish fossils and it was the object of intense geological studies in the 1800s. In Scotland these rocks are found predominantly in the Moray Firth basin and Orkney Archipelago, and along the southern margins of the Highland Boundary Fault.

Elsewhere volcanic activity, possibly as a result of the closing of the Iapetus Suture, created the Cheviot Hillsmarker, Ochil Hillsmarker, Sidlaw Hillsmarker, parts of the Pentland Hillsmarker and Scurdie Ness on the Angusmarker coast.

Carboniferous period

During the Carboniferous period (359–299 Ma), Scotland lay close to the equator. Several changes in sea level occurred and the coal deposits of Lanarkshiremarker and West Lothianmarker and limestones of Fifemarker and Dunbarmarker date from this time. There are oil shale near Bathgatemarker around which the nineteenth century oil-processing industry developed, and elsewhere in the Midland Valley there are ironstones and fire clay deposits that had significance in the early Industrial Revolution. Fossil Grovemarker in Victoria Park, Glasgow contains the preserved remains of a Carboniferous forest. More volcanic activity formed Arthur's Seatmarker and the Salisbury Crags in Edinburghmarker and the nearby Bathgate Hillsmarker.

Permian period

Map of Pangaea


The Old Red Sandstone Continent became a part of the supercontinent Pangaea in the Permian (299–251 Ma), during which proto-Britain continued to drift northwards. Scotland's climate was arid at this time and some fossils of reptiles have been recovered. However, Permian sandstones are found in only a few places - principally in the south west, on the island of Arran, and on the Moray coast. Stone quarried from Hopemanmarker in Moray has been used in the National Museum and Scottish Parliament buildingsmarker in Edinburgh.

At the close of this period came the Permian–Triassic extinction event in which 96% of all marine species vanished and from which bio-diversity took 30 million years to recover.

Mesozoic era

Triassic period

During the Triassic, (251–200 Ma) much of Scotland remained in desert conditions, with higher ground in the Highlands and Southern Uplands providing sediment to the surrounding basins via flash floods. This is the origin of sandstone outcrops near Dumfriesmarker, Elginmarker and the Isle of Arranmarker. Towards the close of this period sea levels began to rise and climatic conditions became less arid.

Jurassic period



As the Jurassic (200–145 Ma) started, Pangaea began to break up into two continents, Gondwana and Laurasia, marking the beginning of the separation of Scotland and North America. Sea levels rose, as Britain and Ireland drifted on the Eurasian Plate to between 30° and 40° north. Most of northern and eastern Scotland including Orkney, Shetland and the Outer Hebrides remained above the advancing seas, but the south and south-west were inundated. There are only isolated sedimentary rocks remaining on land from this period, on the Sutherlandmarker coast near Golspie and on Skye, Mull, Raasaymarker and Eiggmarker. This period does however have considerable significance.The burial of algae and bacteria below the mud of the sea floor during this time resulted in the formation of North Sea oil and natural gas, much of it trapped in overlying sandstone by deposits formed as the seas fell to form the swamps and salty lakes and lagoons that were home to dinosaurs.

Cretaceous period

In the Cretaceous, (146–65 Ma) Laurasia split into the continents of North America and Eurasia. Sea levels rose globally during this period and much of low-lying Scotland was covered in a layer of chalk. Although large deposits of Cretaceous rocks were laid down over Scotland, these have not survived erosion except in a few places on the west coast such as Loch Alinemarker in Morvernmarker. At the end of this period the Cretaceous–Tertiary extinction event brought the age of dinosaurs to a close.

Cenozoic era

Paleogene period

In the early Paleogene period between 63 and 52 Ma, the last volcanic rocks in the British Isles were formed. As North America and Greenlandmarker, separated from Europe the Atlantic Ocean slowly formed. This led to a chain of volcanic sites west of mainland Scotland including on Skyemarker, the Small Islesmarker and St. Kildamarker, in the Firth of Clydemarker on Arranmarker and Ailsa Craigmarker and at Ardnamurchanmarker. Sea levels began to fall, and for the first time the general outline of the modern British Isles was revealed. At the beginning of this period the climate was sub-tropical and erosion was caused by chemical weathering, creating characteristic features of the Scottish landscape such as the topographical basin of the Howe of Alfordmarker near Aberdeen. By 35 Ma the landscape included beech, oak, chestnut and sycamore trees, along with grassland.

Neogene period

Miocene and Pliocene epochs
In the Miocene and Pliocene epochs further uplift and erosion occurred in the Highlands. Plant and animal types developed into their modern forms, and by about 2 million years ago the landscape would have been broadly recognisable today, with Scotland lying in its present position on the globe. As the Miocene progressed, temperatures dropped and remained similar to today's.

Pleistocene epoch
Several ice ages shaped the land through glacial erosion, creating u-shaped valleys and depositing boulder clays, especially on the western seaboard. The last major incursion of ice peaked about 18,000 years ago, leaving other remnant features such at the granite tors on the Cairngorm Mountainmarker plateaux.

Holocene epoch
Over the last twelve thousand years the most significant new geological features have been the deposits of peat and the development of coastal alluvium. Post-glacial rises in sea level have been combined with isostatic rises of the land resulting in a relative fall in sea level in most areas. In some places, such as Culbin in Moray, these changes in relative sea level have created a complex series of shorelines. About half of the coastline of Scotland consists of machair habitat, a low lying dune pasture land formed as the sea level dropped leaving a raised beach. In the present day, Scotland continues to move slowly north.

Geologists in Scotland

James Hutton, painted by Abner Lowe
Scottish geologists and non-Scots working in Scotland have played an important part in the development of the science, especially during its pioneering period in the late eighteenth and nineteenth centuries.
  • James Hutton (1726-1797) the "father of modern geology" was born in Edinburgh. His Theory of the Earth, published in 1788 proposed the idea of a rock cycle in which weathered rocks form new sediments and that granites were of volcanic origin. At Glen Tiltmarker in the Cairngormmarker mountains he found granite penetrating metamorphic schists. This showed to him that granite formed from the cooling of molten rock, not precipitation out of water as the Neptunists of the time believed. This sight is said to have "filled him with delight". Regarding geological time scales he famously remarked "that we find no vestige of a beginning, no prospect of an end."
  • John Playfair (1748-1819) from Angusmarker was a mathematician who developed an interest in geology through his friendship with Hutton. His 1802 Illustrations of the Huttonian Theory of the Earth were influential in the latter's success.
  • John MacCulloch (1773-1835) was born in Guernseymarker and like Hutton before him, studied medicine at Edinburgh University. A president of the Geological Society from 1815-17, he is best remembered for producing the first geological map of Scotland, published in 1836. 'Macculloch's Tree', a high fossil conifer in the Mull lava flows, is named after him.


Charles Lyell


  • Sir Roderick Murchison (1792–1871) was born in Ross and Cromarty and served under Wellesley in the Peninsular War. Knighted in 1846, his main achievements were the investigation of Silurian rocks published as The Silurian System in 1839 and of Permian deposits in Russia. The Murchison cratermarker on the Moon and at least fifteen geographical locations on Earth are named after him.
  • Hugh Miller (1802-56) from Cromartymarker was a stonemason and self-taught geologist. His 1841 publication The Old Red Sandstone became a bestseller. The fossils founds in these rocks were one of his fascinations, although his deep religious convictions led him to oppose the idea of biological evolution.
  • James Croll (1821-90) developed a theory of climate change based on changes in the earth's orbit. Born near Perthmarker, he was self-educated and his interest in science led to his becoming appointed as a janitor in the museum at the Andersonian College and Museum, Glasgow in 1859. His 1864 paper On the Physical Cause of the Changes of Climate during Glacial Epochs led to a position in the Edinburghmarker office of the Geological Survey of Scotland, as keeper of maps and correspondence, where Sir Archibald Geikie, encouraged his research. He was eventually to become a Fellow of the Royal Society.
  • Sir Archibald Geikie (1835-1924) was the first to recognise that there had been multiple glaciations, and his 1863 paper On the glacial drift of Scotland was a landmark in the emergent theories of glaciation. He became Director-General of the Geological Survey of the United Kingdom in 1888 and was also well-known for his work on vulcanism.
  • Arthur Holmes (1890-1965) was born in England and became Regius Professor of Geology at the University of Edinburgh in 1943. His magnum opus was Principles of Physical Geology, first published in 1944, in which he proposed the idea that slow moving convention currents in the Earth's mantle created 'continental drift' as it was then called. He also pioneered the discipline of geochronology. He lived long enough to see the theory of plate tectonics become widely accepted, and he is regarded as one of the most influential geologists of the 20th century.


Important sites

  • Siccar Pointmarker, Berwickshiremarker is world famous as one of the sites that proved Hutton's views about the immense age of the Earth. Here Silurian rocks have been tilted almost to the vertical. Younger Devonian rocks lie unconformably over the top of them, dipping gently, indicating that an enormous span of time must have passed between the creation of the two beds. When Hutton and James Hall visited the site in 1788 their companion Playfair wrote:


  • The Moine Thrustmarker in Assyntmarker is one of the most studied geological features in the world. Its discovery in the 1880s was a milestone in the history of geology as it was one of the first thrust belts in the world to be identified. Investigations by John Horne and Benjamin Peach resolved a dispute between Murchison and Geikie on the one hand and James Nicol and Charles Lapworth on the other. The latter believed that older Moine rocks lay on top of younger Cambrian rocks at Knockan Crag, and Horne and Peach's work confirmed this in their classic paper The Geological Structure of the Northwest Highlands of Scotland, which was published in 1907. A statue to these two pioneers of fieldwork was erected at Inchnadamphmarker near the hotel there which played a prominent part in the annals of early geology. This area is at the heart of the 'North West Highlands Geopark'.
  • Lapworth also had a prominent role to play in the fame of Dob's Linnmarker, a small gorge in the Scottish Borders, which contains the 'golden spike' (i.e. the official international boundary or stratotype) between the Ordovician and Silurian periods. Lapworth's work in this area, especially his examination of the complex stratigraphy of the Silurian rocks by comparing fossil graptolites, was crucial in to the early understanding of these epochs.


  • The Skye Cuillinmarker mountains provide classic examples of glacial topography and were the subject of an early published account by James Forbes in 1846 (who had become a fellow of the Royal Society of Edinburgh aged only nineteen). He partnered Louis Agassiz on his trip to Scotland in 1840 and although they subsequently argued, Forbes went on to publish other important papers on Alpine glaciers.
  • In 1904 Alfred Harker published The Tertiary Igneous Rocks of Skye, the first detailed scientific study of an extinct volcano.
  • In the hills to the north of the village of Strontianmarker the mineral strontianite was discovered, from which the element strontium was first isolated by Sir Humphry Davy in 1808.
  • The island of Staffamarker, contains Fingal's Cavemarker made up of massive rectangular columns of Tertiary basalt and Mackinnon's Cave, one of the longest sea caves in the world.
  • The Munro Schiehallionmarker's isolated position and regular shape led Nevil Maskelyne to use the deflection caused by the mass of the mountain to estimate the mass of the Earth in a ground-breaking experiment carried out in 1774. Following Maskelyne's survey, Schiehallion became the first mountain to be mapped using contour lines.
  • The village of Rhyniemarker in Aberdeenshiremarker is the site of an important sedimentary deposit - Rhynie chertmarker. The bulk of this fossil bed consists of primitive plants that had water-conducting cells and sporangia but no leaves, along with arthropods: Collembola, Opiliones (harvestmen), pseudoscorpions and the extinct, spider-like Trigonotarbids. This fossil bed is remarkable for two reasons. Firstly, the age of the find (early Devonian circa 410 Ma) makes this one of the earliest sites anywhere containing terrestrial fossils, coinciding with the first stages of the colonisation of land by plants and animals. Secondly, these cherts are famous for their exceptional state of ultrastructural preservation, with individual cell walls easily visible in polished specimens. For example, stomata have been counted and lignin remnants detected in the plant material.
  • A disused quarry at East Kirkton in the Bathgate Hillsmarker is the location where the Carboniferous fossil of Westlothiana lizziae (aka 'Lizzie') was found in 1984. This lizard is one of the earliest known ancestors of the reptiles. The specimen was purchased in part by public subscription and is now on display in the National Museum of Scotland. The site was originally discovered in the early nineteenth century and has also provided fossil eurypterids, sharks and a variety of primitive acanthodian fish.
  • In 2008 the ejected material from a meteorite impact crater was discovered near Ullapool in Wester Ross. Preserved within sedimentary layers of sandstone, this is the largest known bolide impact from what are now the British Islesmarker.


See also

* Geology of Irelandmarker
* Geology of England
* Geology of Wales


References

General references:

  • Gillen, Con (2003) Geology and landscapes of Scotland. Harpenden. Terra Publishing.
  • Jones, Rosalind (1997) Mull in the Making. Aros. R Jones. ISBN 0953189007
  • Keay, J. & Keay, J. (1994) Collins Encyclopaedia of Scotland. London. HarperCollins.
  • McKirdy, Alan Gordon, John & Crofts, Roger (2007) Land of Mountain and Flood: The Geology and Landforms of Scotland. Edinburgh. Birlinn. ISBN 9781841583570
  • "Scottish Geology" Scottishgeology.com. Retrieved 30 September 2007.


Footnotes

  1. Keay & Keay (1994) page 415.
  2. University of Edinburgh - James Hutton Retrieved 16 August 2007.
  3. Keay & Keay (1994) pages 415-422.
  4. McKirdy et al. (2007) pages 124-31.
  5. SNH Trends- seas (PDF) Retrieved 2 January 2007.
  6. Gillen, Con (2003) pages 90-1.
  7. Keay & Keay (1994) page 867.
  8. Gillen, Con (2003) page 110.
  9. Gillen (2003) page 95.
  10. "Southern Uplands Fault" Gazetteer for Scotland. Retrieved 11 January 2008.
  11. "Regional Geology, Southern Uplands - Map" Scottishgeology.com. Retrieved 21 March 2008.
  12. Murray, W.H. (1973) The Islands of Western Scotland. London. Eyre Methuen.
  13. Murray, W.H. (1977) The Companion Guide to the West Highlands of Scotland. London. Collins.
  14. "Study Sees North Sea Tsunami Risk" Speigel Online. Retrieved 28 July 2007.
  15. Bondevik, Stein; Dawson, Sue; Dawson, Alastair; Lohne, Øystein. (5 August 2003) "Record-breaking Height for 8000-Year-Old Tsunami in the North Atlantic"(pdf) EOS, Transactions of the American Geophysical Union. Vol.84 Issue 31, pages 289-293. Retrieved 15 January 2007.
  16. "Earthquakes in the Inverness Area" Inverness Royal Academy. Retrieved 8 November 2007.
  17. Gillen (2003) page 44.
  18. McKirdy et al. (2007) page 95.
  19. McKirdy et al. (2007) page 94.
  20. McKirdy et al. (2007) page 68.
  21. "Precambrian History of the UK" geologyrocks.co.uk. Retrieved 1 August 2007.
  22. Sellar, W.D.H. (ed) (1993) Moray: Province and People. The Scottish Society for Northern Studies.
  23. McKirdy et al. (2007) page 68.
  24. "Palaeozoic History of the UK: Cambrian to Silurian" geologyrocks.co.uk. Retrieved 1 August 2007.
  25. Gillen (2003) pages 98 and 111.
  26. McKirdy et al. (2007) page 68.
  27. Gillen (2003) pages 69, 73, 75, 88 and 95.
  28. McKirdy et al. (2007) page 68.
  29. "Palaeozoic History of the UK: Cambrian to Silurian" Retrieved 1 August 2007.
  30. Gillen (2003) page 95.
  31. Butler, Rob (2000) The Moine Thrust Belt. Leeds University. Retrieved 27 January 2006.
  32. "The Devonian Period (416 ~ 359 million years ago)" Scottishgeology.com. Retrieved 15 August 2007.
  33. Gillen (2003) pages 110-119.
  34. McKirdy et al. (2007) pages 124-130.
  35. McKirdy et al. (2007) pages 132-135.
  36. Gillen, Con (2003) pages 120-5.
  37. McKirdy et al. (2007) pages 141-144.
  38. "The Permian & Triassic Periods (299 ~251 and 251 ~ 200 million years ago respectively)" Scottishgeology.com. Retrieved 31 July 2007.
  39. McKirdy et al. (2007) page 146.
  40. Gillen, Con (2003) pages 133-7.
  41. Gillen (2003) pages 138-9.
  42. "The Cretaceous Period (146 ~ 65 million years ago)" Scottish geology.com. Retrieved 16 August 2007.
  43. Gillen (2003) page 142.
  44. McKirdy et al. (2007) page 150.
  45. McKirdy et al. (2007) page 158.
  46. McKirdy et al. (2007) page 158.
  47. "Tertiary" Fettes.com Retrieved 16 August 2007.
  48. McKirdy et al. (2007) pages 159 and 163-171.
  49. "The Quaternary" Scottishgeology.com. Retrieved 16 August 2007.
  50. "Update to UKCIP02 sea level change estimates" (December 2005) UK Climate Impacts Programme. Retrieved 10 June 2008.
  51. Smith, David E., and Fretwell, Peter T. "Scottish Sea Levels" scottishsealevels.net. Retrieved 15 November 2007.
  52. Ross, Sinclair (1992) The Culbin Sands – Fact and Fiction. Aberdeen University Press.
  53. Keay & Keay (1994) page 415.
  54. Keay & Keay (1994) page 531.
  55. McKirdy et al. (2007) pages 61 and 115.
  56. Biographical Dictionary of Eminent Scotsmen (1856), reproduced in "Significant Scots" electricscotland.com. Retrieved 3 October 2007.
  57. McKirdy et al. (2007) page 156.
  58. Jones (1997) page 38.
  59. Keay & Keay (1994) page 641.
  60. "Westminster Abbey.—A Survey of the Building." British History Online. Retrieved 12 August 2007
  61. "Lyell, Sir Charles [1797 - 1875" About Darwin.com. Retrieved 12 August 2007.
  62. Morton, John L. (2004) King of Siluria — How Roderick Murchison Changed the Face of Geology. Horsham. Brocken Spectre. ISBN 0954682904.
  63. Keay & Keay (1994) page 717.
  64. "Who Was He, Then?" Discover Hugh Miller. Retrieved 8 July 2007.
  65. McKirdy et al. (2007) page 77.
  66. McKirdy et al. (2007) page 86.
  67. McKirdy et al. (2007) page 54.
  68. McKirdy et al. (2007) page 253.
  69. Gillen (2003) page 95.
  70. Peach, B.N., Horne, J., Gunn, W., Clough, C.T., Hinxman, L.W., and Cadell, H.M. (1888) Report on the recent work of the Geological Survey in the north-west Highlands of Scotland, based on field notes and maps by Messrs. B.N. Peach, J. Horne, W. Gunn, C.T. Clough, L.W. Hinxman, L.W. and H.M. Cadell. Quarterly Journal of the Geological Society of London, 44, 378-441.
  71. Peach, B.N., Horne, J., Gunn, W., Clough, C.T., and Hinxman, L.W., (1907) The Geological Structure of the Northwest Highlands of Scotland. Memoirs of the Geological Survey of Great Britain.
  72. McKirdy et al. (2007) pages 110 and 121-122.
  73. "Welcome to North West Highland Geopark northwest-highlands-geopark.org.uk. Retrieved 18 August 2007.
  74. McKirdy et al. (2007) page 88.
  75. Forbes, James D. (1846) Notes on the topography and geology of Cuchullin Hills in Skye, and on traces of ancient glaciers which they present. Edinburgh New Philosophical Journal No. 40. Pages 76-99.
  76. Forbes, James D. (1846) On the Viscous Theory of Glacier Motion Abstracts of the Papers Communicated to the Royal Society of London, Vol. 5, 1843 - 1850. Pages 595-596.
  77. McKirdy et al. (2007) pages 164-5 and 280.
  78. Harker, Alfred, (1904) The Tertiary Igneous Rocks of Skye. Geological Survey of Scotland Memoir.
  79. "Strontian" Undiscovered Scotland. Retrieved 8 July 2007.
  80. "History and Minerals of Strontian mines" rock-site.co.uk. Retrieved 8 July 2007.
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