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You are here: Home / Footpaths / Surfacing

Surfacing

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Most paths have developed on surfaces that are resistant to a certain amount of trampling. Examples are paths on grassland, beaten earth paths through woodland and mountain paths on rock. Where unavoidable, paths cross peat bogs, marshes or sand dunes which are unstable and easily damaged by trampling. The addition or replacement of surfacing material becomes necessary either when the natural surface is damaged or destroyed by more use than its natural structure can bear, or where an unstable material needs protecting and strengthening.

Sections in this chapter

  • Types of surface
  • The path profile
  • Path edgings
  • Stone aggregate paths
  • Geotextiles
  • Subsoil paths or soil reorganisation
  • Stone pitching
  • Stone slab or ‘causey’ paths
  • Concrete paths
  • Corduroy and woodchip paths
  • Causeways
  • Planning and organising
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Footpaths

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  • Surfacing
    • Types of surface
    • The path profile
    • Path edgings
    • Stone aggregate paths
    • Geotextiles
    • Subsoil paths or soil reorganisation
    • Stone pitching
    • Stone slab or ‘causey’ paths
    • Concrete paths
    • Corduroy and woodchip paths
    • Causeways
    • Planning and organising
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