Kilt Rock was a wonderful place to visit in Scotland. Return to the road. [1] Triassic rocks of the Stornoway Formation are found near Broadford, a sequence of sandstones and conglomerates deposited by rivers. The island is covered by large areas of glacial till, left behind when the ice melted.[1]. The lowest unit is the Ghrudaidh Formation, followed by the Eliean Dubh Formation the Sailmhor Formation and the Sangomore Formation, all consisting of dolomites with chert. They are hidden beneath Palaeogene volcanic rocks over most of this area, being exposed only on the eastern and northern coasts of the Trotternish peninsula, on the Strathaird peninsula and between the Red Hills and Sleat. The Kilt Rock is named after the columnar structure of the 105 metres (344 ft) cliffs, said to resemble the pleats in a kilt. The signposted car park was on the right side of the A855 road. Mealt Falls was actually part of the well-signed Kilt Rock View. Mission: investigate geological phenomena at Rubha nam Bratheirean (Brothers' Point - speculated to be the site of a former monastery or of a tragic shipwreck) on the eastern shore of the Trotternish Peninsula on the Isle of Skye. Kilt Rock. Both groups consist dominantly of sandstones and were deposited mainly by alluvial fans and rivers. [1] The Red Hills are formed of granite and have a more rounded topography. A wide range of rock types are exposed on the island, sedimentary, metamorphic and igneous, ranging in age from the Archaean through to the Quaternary. The geology of Skye in Scotland is highly varied and the island's landscape reflects changes in the underlying nature of the rocks. A former quarry at Strath was linked by tramroad to Broadford where the marble was exported, prior to the quarry's abandonment. Lower Jurassic rocks near Broadford have provided building stone for local use whilst aggregate for road construction is sourced in a Torridonian sandstone quarry near Sconser. These beds are affected by thrusting in both areas and by contact metamorphism from Palaeogene granite intrusions in the northern outcrop, locally forming marble, such as at Torrin. The wind roars above your head and on a clear day, you can see all the way to the mainland of Scotland from Kilt Rock. Image of kilt, skye, coastal - 28357088 Image of kilt, skye, coastal - 28357088 Image of kilt, skye, coastal, geology - 28357088 The oldest rocks on the Trotternish Peninsula are 190-150 million years old, and were laid down in the waters and on the shores of relatively shallow and warm seas during the Jurassic period. The geology of Isle of Skye is highly variable, ranging in age from Archaean to Quaternary, with sedimentary, igneous and metamorphic rocks all present, leading to a wide variety of landscapes, depending on the rock type. Kilt Rock Kilt Rock is another geological wonder with vertical basalt columns creating the pleats and intruded sills of dolerite carving out the kilt’s pattern. On the one side of this lookout point, you’ll find the enormous Kilt Rock, so named because it looks like a pleated kilt. Quiraing. The dominant trend of the dykes is northwest-southeast although they are locally in part radial near the old volcanic centre. North of Portree, you can admire magnificent views of the Trotternish landslips and abrupt sea cliffs. WikiMili. All orders are custom made and most ship worldwide within 24 hours. Kilt Rock: Making the most of geology - See 1,773 traveler reviews, 1,174 candid photos, and great deals for Isle of Skye, UK, at Tripadvisor. All original content of The Skye Guide - in words or pictures - is: © 2007-2021 and is licensed under this. Another feature which involves these Jurassic and Lower Tertiary rock-types is extensive areas of landslipped material, which developed during Quaternary times. Here astonishing pinnacles, columns and cliffs adorn the landscape. The Torridonian on Skye comprises two conformable sequences, the older Sleat Group and the younger Torridon Group. [1] The dominant lava type is basalt, with subsidiary hawaiite and mugearite derived from silica-poor magma and minor amounts of trachyte from a silica-rich magma. The sequence continues with the Lower to Middle Jurassic Bearreraig Sandstone Formation followed by Middle Jurassic Great Estuarine Group, comprising the Cullaidh Shale Formation, Elgol Sandstone Formation, Lealt Shale Formation, Valtos Sandstone Formation, Duntulm Formation, Kilmaluag Formation and the Skudiburgh Formation. The Black Cuillin are formed of gabbro, which erodes to form the characteristically jagged outlines, although this is in large part due to the many minor intrusions, such as dykes and cone sheets that cut the gabbro. This is a popular stopping point on the road between Portree and Staffin and there is a large car park by the waterfall at NG508655, at Ellishadder. There is a free car park so just pull in and walk over to the viewing area where you can see Kilt rock itself and a beautiful waterfall too. Most of the dykes are basaltic in composition but a minority are trachytic. The two main exposures of Cambro-Ordovician sediments are the "Ord Window" (a gap in the Kishorn Thrust sheet through which the sequence beneath the thrust can be seen) on the northern coast of Sleat and the area between Broadford and Loch Slapin. Closer by is the Mealt Waterfall, which freefalls off the cliff for 60m into the Sound of Raasay below. Elgol is a village on the shores of Loch Scavaig towards the end of the Strathaird peninsula on the Isle of Skye. A sequence of Cambrian to Lower Ordovician sediments of the Eriboll and Durness Groups lie above the Torridonian with an angular unconformity. The Upper Jurassic is represented by the Staffin Shale Formation. The stunning geological formation of Kilt Rock is a beauty in any weather. Graphite and coal are also present in small quantities, near Portree and at Loch Sligachan respectively, but neither has been economical to work. The Quiraing is a spectacular series of rock pinnacles on the eastern side of the main spine of the peninsula and further south is the rock pillar of the Old Man of Storr . Its end use was in dynamite manufacture and later as a filter and insulator. The geology of the Isle of Skye in Scotland is highly varied and the island's landscape reflects changes in the underlying nature of the rocks. After some Saturday night festivities and a day off on Sunday, Monday brought an exploration of the Tertiary igneous geology for which Skye is perhaps most geologically-renowned. [34] During the Tertiary geological period, the continental crust began to rift and eventually the Atlantic Ocean opened up. Inspired designs on t-shirts, posters, stickers, home decor, and more by independent artists and designers from around the world. These shallow seas were very different to the waters of the North Atlantic that erode Skye’s shores today. If you're not a big geology fan it's still a must see on any Isle of Skye tour and the views out over the sound of Raasay are truly majestic! The Isle of Skye ("Skye") lies off the west coast of Scotland and forms part of the Inner Hebrides island chain. One's can only imagine living nearby. The famous Kilt Rock is a sea cliff in north east Trotternish. The Lower Cambrian Eriboll Group comprises a basal quartzite, locally with a basal conglomerate, followed by the distinctive Pipe Rock Member, a quartz arenite with white weathering skolithos trace fossils. They commonly display columnar jointing, such as in the upper part of the Kilt Rock at Staffin. Hornfelsed lava has been worked near Sligachan and dolerite quarried from a sill near Invertote for a similar purpose. Today, the cliff edge is pretty well fenced, but do take particular care and keep to the designated viewpoint. The massive columns of dolerite have the appearance of pleats in a tartan kilt & traditionally form the basis of the Skye tartan pattern. The overlying Durness Group comprises a series of dolomites of Upper Cambrian to Middle Ordovician in age. Near Tarskavaig, Neoproterozoic metasediments of the Moine Supergroup are found above strongly deformed Lewisian rocks. As an added bonus we were treated to the goosebump-inducing sounds of the bagpipes being played by a handsome man in full dress kilt. [1], During this period the island was affected by the Quaternary glaciation, with the development of an ice cap centred on the Cuillin and Red Hills. Part of the magma chambers for the volcanoes are exposed at the surface as major intrusions of gabbro and granite. Best of all is Kilt Rock, 200ft high cliffs marked in an almost tartan-like pattern by the rock strata, and with a waterfall tumbling sheer to the pebbled shore below. Address: A855, Portree IV51, UK. Kilt Rock, Trotternish. North again brings you to the main settlement on the east side of the peninsula, Staffin, overlooking Staffin Island and Staffin Bay, an unusually sandy bay for this part of Skye. These coarse-gr… [1], Sedimentary rocks of Mesozoic age underlie most parts of the island north of the Sleat Peninsula. A Tour of Kilt Rock, Skye, MacLeod’s Tables, Three Chimney’s Restaurant & Neist Point . And on the other, the Mealt Waterfall. To the south, similar relationships can be seen, although in this case the lower sill forms the middle portion of the cliff-face. Geology The geology of Skye is complex. The dominant lava type is basalt, with subsidiary hawaiite and mugearite derived from silica-poor magma and minor amounts of trachyte from a silica-rich magma. Kilt Rock is situated 1.5 miles to the south of Staffin on the Isle of Skye on its east coast. The angle that you view the waterfall from makes it look like it appears from the rock. This was about 15 miles north of the town of Portree on the east coast of the Isle of Skye (roughly 10 miles north of the Bride’s Veil Waterfall and the Old Man Storr).. Some of this early activity took place on Skye. The almost-vertical columnar jointing within the upper sill gives rise to the name 'Kilt Rock', in reference to the similarities with pleats in a kilt. This is also a great spot for spotting dolphins and seals in the right season Kilt Rock with the distinctive pillars and beautiful waterfall with views across to the Torridon hills on the mainland, this weird landscape is used as a film location for many Sci-Fi movies, and is known for it’s amazing rock formations. Fissures spewed layers of lava, volcanic ash and debris on top of the soft sedimentary Jurassic rocks. Part of the magma chambers for the volcanoes are exposed at the surface as major intrusions of gabbroand granite. It is 200 foot high sea cliff. You’ll also see the iconic geological landslip of the Quiraing and Kilt Rock; a 90-metre tall basalt tower much like our national dress! However, the unique geological formations are actually the result of a landslip, similar to the one that created the nearby Quiraing. Sand and gravel have been extracted from the raised beach deposits west of Kyleakin with local use made of gravels from the mouth of the river in Glen Brittle. Photo about The landmark Kilt rock seen on the east coast of the Isle of Skye. Mention Scotland and, for many, the image of a kilt-clad Mel Gibson is immediately evoked. https://www.theskyeguide.com/.../27-natural-wonders/177-kilt-rock However it was extremely windy and cold as hell. The Old Man of Storr, a pinnacle of rock that adorns many a landscape picture, is just as magnificent in real life. ! Let's discover one of the most famous features on the Isle of Skye: Kilt Rock and the Mealt Falls. I will show you, that there are other worthy stops to enjoy on the east coast, on top of Kilt Rock Skye. Looking west to part of the Trotternish Hills. [3], "A stratigraphical framework for the Upper Cretaceous Chalk of England and Scotland with statements on the Chalk of Northern Ireland and the UK Offshore Sector", Heart of Neolithic Orkney World Heritage Site, Description of the Western Isles of Scotland, A Description of the Western Isles of Scotland, A Journey to the Western Islands of Scotland, https://en.wikipedia.org/w/index.php?title=Geology_of_the_Isle_of_Skye&oldid=1000969562, Creative Commons Attribution-ShareAlike License, This page was last edited on 17 January 2021, at 16:39. It is the variety of rock types that underlies, literally and metaphorically, the very different sorts of terrain and scenery to be found on the island. The Pipe Rock is overlain by the Salterella Grit, a coarse sandstone, and the Fucoid Beds, a sequence of calcareous sandstone and siltstone. The Lewisian and Moine sequences are thrust over another sequence of unmetamorphosed Neoproterozoic sediments, the Torridonian, along the Moine Thrust Zone. The most famous example of this occurs on the east coast of north Skye, 2km south of Staffin, and is referred to as the Kilt Rock. Exploratory drilling for oil has taken place within the strata of the Great Estuarine Group in the north. The Isle of Skye isn’t just coastal beaches, it has its fair share of jaw-dropping cliffs, as well. Kilt Rock on the Trotternish Peninsula on The Isle of Skye, Scotland. During the Paleocene to Early Eocene Skye formed one of the main volcanic centres of the North Atlantic Igneous Province. On the Trotternish peninsula, mafic magma was intruded along the bedding planes of the Jurassic sedimentary rocks beneath the lavas to form sills that are up to 90m thick. Visited Kilt Rock at the weekend on our tour around Skye. The striking rock formation, composed of massive columns of dolerite, has been compared to the appearance of pleats in a tartan kilt. The Skye Marble Company works the Cambro-Ordovician limestones at Torrin, metamorphosed through contact with the adjacent granite and gabbro intrusions. Website: Kilt Rock It is just off the main road so well worth stopping for. The waterfall was in full raging flow and didn't disappoint. The main ice sheet that flowed westwards from the Scottish mainland was diverted around this upland area. Kilt Rock. And I'd rather hear the music When my time may come to die, Of the wind among the corries In the far off Isle of Skye. Would love to see the full effect from the sea as the rock formation looks like a pleated kilt and the waterfall its sporran. The Kilt Rock with a columnar jointed dolerite sill above Jurassic sandstones of the Valtos Sandstone Formation. The only Cretaceous unit exposed on Skye is the Strathaird Limestone Formation, thought to be either Turonian or Campanian in age, which lies unconformably on the Jurassic and is overlain unconformably by Palaeocene lavas. U3A Skye Geology Saturday, 8 February 2014. The impact of successive ice sheets passing over, the last as recently as 11,500 years ago, adds to the mix. These coarse-grained igneous rocks are relatively resistant to erosion and now form the Cuillin hills. The geology of Skye in Scotland is highly varied and the island's landscape reflects changes in the underlying nature of the rocks. Gently dipping lavas from the volcanoes cover most of northern Skye, giving a stepped trap type landscape. It is said to resemble a kilt, with vertical basalt columns to form the pleats and intruded sills of dolerite forming the pattern. The Atlantic Ocean opened up is a beauty in any weather around Skye Supergroup are found strongly. Mainland was diverted around this upland area successive ice sheets passing over, the water blown. Dolerite sill above Jurassic sandstones of the Isle of Skye, Scotland by Staffin! 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