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196 PROCESS AND FORM


              Papua New Guinea and Mount Api in Sarawak, consists  semi-arid areas. Smaller-scale versions are known from
              of bare, net-like, saw-topped ridges with almost verti-  the Nahanni limestone karst region of the Mackenzie
              cal sides that stand up to 120 m high. The spectacular  Mountains, Canada (Brook and Ford 1978). Here, the
              ridges rise above forest-covered corridors and depres-  labyrinth karst is stunning, with individual streets longer
              sions. They seem to have formed by limestone solution  than 1 km and deeper than 50 m (Plate 8.6).
              without having previously been buried.
                                                        Coastal karren
              Ruiniform karst                           Around coasts and lakes, limestone or dolomite outcrops

              This is an assemblage of exceptionally wide grikes and  often display a distinctive solutional topography, with
              degrading clints that have been exposed by soil erosion  features including intertidal and subtidal notches (also
              (Plate 8.5).The clints stick out like ‘miniature city blocks  called nips; Plate 8.7) and a dense formation of pits,
              in a ruined townscape’ (Ford and Williams 1989, 391).  pans, micropits, and spikes (Plate 8.8). Boring and graz-
              Ruiniform karst is found in the French Causses, where  ing organisms may help to form coastal karren, as may
              deforestation and soil erosion have occurred. On high
              crests, ruiniform karst is transitional to limestone tors.

              Corridor karst

              In places, grikes grow large to form a topography of
              aligned or criss-crossing corridors. The large grikes are
              called bogaz, corridors, zanjones, and streets. Grike-wall
              recession produces square-shaped or box valleys and large
              closed depressions called platea. Corridor karst land-
              scapesarecalledlabyrinth karst,corridor karst,orgiant
              grikeland.Itislarge-scaleclint-and-griketerrainbutmay
              have a complex history of development. Grikelands form
              under tropical and temperate rainforest and in arid and


















                                                        Plate 8.6 View of Nahanni labyrinth karst, showing
              Plate 8.5 A ruiniform assemblage (residual clint blocks) in  intersecting networks of karst streets interspersed with
              flat-lying limestones near Padua, Italy.   karst platea.
              (Photograph by Derek C. Ford )            (Photograph by George A. Brook)
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