|Glen Roy National Nature Reserve|
The Parallel Roads of Glen Roy, highlighted by recent snowfall
|Location||Roybridge, Lochaber, Scotland|
|Governing body||Scottish Natural Heritage (SNH)|
|Glen Roy National Nature Reserve|
Glen Roy (Scottish Gaelic: Gleann Ruaidh meaning "red glen") in the Lochaber area of the Highlands of Scotland is a National Nature Reserve and is noted for the geological puzzle of the three roads ("Parallel Roads"). The "Parallel Roads" of Glen Roy are lochterraces that formed along the shorelines of an ancient ice-dammed loch. The loch existed during a brief period (some 900-1,100 years in duration) of climatic deterioration, during a much longer period of deglaciation, subsequent to the last main ice age (The Devensian). From a distance they resemble man-made roads running along the side of the Glen, hence the name.
Location and access
The glen runs north from Glen Spean which takes the main A86 trunk road and the railway of the West Highland Line, both running about a further 14 miles southwest via Spean Bridge to Fort William. The village of Roybridge and Roy Bridge railway station are sited where the River Roy joins the River Spean, and from there a narrow single track road runs north up the glen for almost 10 miles to Brae Roy Lodge.
Glen Roy National Nature Reserve
Glen Roy National Nature Reserve is managed by Scottish Natural Heritage (SNH). Glen Roy was acquired by the then Nature Conservancy in 1970 and declared a National Nature Reserve in order to protect the site against proposed afforestation. While Glen Roy was protected as a Site of Special Scientific Interest (SSSI) at this time, this accolade offered much weaker protection than it does today, however now the protection comes from both its SSSI and NNR status.
The Parallel Roads of Glen Roy
The Parallel Roads of Glen Roy, Scottish Highlands, represent a series of ice-dammed proglacial lake shorelines produced during the cold climate of the Younger Dryas (GS1). It has been demonstrated by Dawson, Hampton, Harrison, Greengrass and Fretwell (2002) that each lake shoreline exhibits evidence of glacio-isostatic tilting associated with the decay of the last (Late Devensian) ice sheet. The directions of tilting of the three shorelines (in the quadrant between north and east), are at variance with published glacio-isostatic uplift isobases based on marine shoreline data that suggest a pattern of decreased uplift towards the northwest. The gradient of shoreline tilting (between 0.11 and 0.14 m/km) is similar to measured regional tilts of a well-developed marine shoreline (the Main Rock Platform) considered to have been produced in Scotland during the same period of extreme cold climate. Consideration of the ice-dammed lake shoreline data also points to the former occurrence of two separate episodes of tectonic activity during the Younger Dryas (Greenland Stadial 1 - GS1).
Historic geological investigations
In the 19th century, the Parallel Roads attracted the attention of many early geologists, including the Reverend William Buckland, Charles Lyell, James Nicol, Charles Babbage, James Geikie, and Joseph Prestwich. This interest ensured that the Parallel Roads featured prominently in the development of geological science.
Charles Darwin visited the glen in June 1838 and, drawing on his recent findings in South America during the Beagle expedition concluded that the shorelines were raised beaches of marine origin. His paper on the subject was published in 1839 in the Philosophical Transactions of the Royal Society. This was contradicted in 1840 by Louis Agassiz's Glacial theory which postulated that the Glen Roy shorelines had been cut by freeze-thaw processes of loch ice during the maximum extent of glacial ice in the climatic reversal known as the Younger Dryas / Greenland Stadial, or locally the Loch Lomond Readvance. Darwin defended his paper over many years.
In 1861 Thomas Jamieson was advised by Lyell and Darwin about visiting the Glen, and given memoranda and maps by Darwin. After visiting the glen a second time in the summer of 1862, Jamieson wrote to Lyell on 15 August reporting his findings. On 6th September Darwin told Lyell and Jamieson that he was convinced: "My paper is one long gigantic blunder". Jamieson's paper on his investigations was published in 1863. Four decades after Darwin's 1839 paper and shortly before his death, in a letter to Joseph Prestwich, he said that he gave up his Glen Roy theory when he read T. F. Jamieson's (1863) paper but he agreed with Prestwich's criticism of Jamieson's interpretation of the Glen Turret delta.
Interest in the Parallel Roads continues to this day, both among earth scientists intrigued by the dramatic processes that shaped that landscape, and among tourists attracted by the natural wonder of the landforms.
- Ainmean-Àite na h-Alba
- Nicol, James (Jan 1, 1869). "On the Origin of the Parallel Roads of Glen Roy". Quarterly Journal of the Geological Society of London. 25: 282–291. doi:10.1144/gsl.jgs.1869.025.01-02.50.
- Babbage, Charles (Feb 26, 1868). "Observations on the parallel roads of Glen Roy". Quarterly Journal of the Geological Society of London. 24: 273–277. doi:10.1144/gsl.jgs.1868.024.01-02.30.
- Darwin Correspondence Project, “Letter no. 3246”, Charles Darwin to Charles Lyell, 6 September , accessed on 14 January 2018,
Darwin Correspondence Project, “Letter no. 3247,” accessed on 14 January 2018, http://www.darwinproject.ac.uk/DCP-LETT-3247
Darwin Correspondence Project, “Letter no. 3761,” accessed on 14 January 2018, http://www.darwinproject.ac.uk/DCP-LETT-3761
- "On the parallel roads of Glen Roy", Quart. Journ. Geol. Soc. Lond. 19 (1863): 235–258.
- SNH Publications - Landscape Fashioned by Geology - Glen Roy
- Observations on the Parallel Roads of Glen Roy, and of other parts of Lochaber in Scotland, with an attempt to prove that they are of marine origin. By CHARLES DARWIN, Esq., M.A. F.R.S. Sec. G.S (1839)
- Environmental History Resources - The Parallel Roads of Glen Roy and Forestry
- The Parallel Roads of Glen Roy - Short Video
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