Matches in DBpedia 2016-04 for { ?s ?p "The mountain Quinag (808 m) (Scottish Gaelic: A’ Chuineag, pronounced [ə xɯɲaɡ̊]) in Sutherland, in the Scottish Highlands, is in fact a mountain range with an undulating series of peaks along its Y-shaped crest. The name Quinag is an anglicisation of the Gaelic name Cuinneag, a milking pail, reflecting its distinctive shape.Geologically, Quinag is made of Torridonian sandstone, resting on a substrate of Lewisian gneiss. The highest peaks are capped by a thin skin of Cambrian quartzites with the gentle eastern slope of Spidean Coinich being a dip slope formed along the quartzite beds. The massif is an excellent place to appreciate the relationship between these three major rock units of the NW Highland."@en }
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- Quinag abstract "The mountain Quinag (808 m) (Scottish Gaelic: A’ Chuineag, pronounced [ə xɯɲaɡ̊]) in Sutherland, in the Scottish Highlands, is in fact a mountain range with an undulating series of peaks along its Y-shaped crest. The name Quinag is an anglicisation of the Gaelic name Cuinneag, a milking pail, reflecting its distinctive shape.Geologically, Quinag is made of Torridonian sandstone, resting on a substrate of Lewisian gneiss. The highest peaks are capped by a thin skin of Cambrian quartzites with the gentle eastern slope of Spidean Coinich being a dip slope formed along the quartzite beds. The massif is an excellent place to appreciate the relationship between these three major rock units of the NW Highland.".
- Q2219266 abstract "The mountain Quinag (808 m) (Scottish Gaelic: A’ Chuineag, pronounced [ə xɯɲaɡ̊]) in Sutherland, in the Scottish Highlands, is in fact a mountain range with an undulating series of peaks along its Y-shaped crest. The name Quinag is an anglicisation of the Gaelic name Cuinneag, a milking pail, reflecting its distinctive shape.Geologically, Quinag is made of Torridonian sandstone, resting on a substrate of Lewisian gneiss. The highest peaks are capped by a thin skin of Cambrian quartzites with the gentle eastern slope of Spidean Coinich being a dip slope formed along the quartzite beds. The massif is an excellent place to appreciate the relationship between these three major rock units of the NW Highland.".