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Snowdonia / Eryri

North Wales

The cirques and ridges of Eryri make contour patterns easier to understand. Compare a mapped slope with the landform that gives the lines their shape.

Snow on Gallt y Wenallt above mist in Nant Gwynant, Eryri / Snowdonia.
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Nant Gwynant, Eryri / Snowdonia. A glacial valley lies beneath the steep Snowdon horseshoe.
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Location: 53.07°, -4.08°

Glacial erosion helped shape the cirques, sharp ridges and deep valleys around Yr Wyddfa. Contours turn these three-dimensional forms into lines of equal elevation. Closely spaced lines indicate steep slopes; their pattern helps distinguish a hollow from a projecting ridge.

Use the contours model to rotate a hill before viewing it from above. Ask students to predict the lines around a cirque and a spur, then compare their sketches with a map of Eryri. Check the map’s stated interval before calculating heights.

On an OS-style extract of Yr Wyddfa, how would you distinguish a cirque from a spur using contours alone?

Teacher hint: Look for a hollow enclosed by steep backwalls at a cirque, and contour bends pointing downhill along a spur.

  • Ordnance Survey
  • BGS Wales