Download PDF - Speleogenesis
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PLATES 12 AND 13 PARTITIONS<br />
Plate 12. Bedrock partitions between closely-spaced passages in maze caves. A = Parallel slot-like passages opened to the walls of Marble<br />
Canyon, Arizona, USA. Top to bottom height is about 65 m (from Huntoon, 2000); B = Slot-like passages with a thin partition in Wind Cave,<br />
SD, US (photo by A. Palmer); C and D = Thin partitions between passages in Slavka Cave, western Ukraine (photo by A. Klimchouk); E and<br />
G = Thin partitions between passages in Zoloushka Cave, western Ukraine (photos by B. Ridush and V. Kisselev). The pillars were thinned<br />
by dissolution at the water table during a late stage of cave development; F = Thin partition between parallel passages in the Lower Cave<br />
section of Carlsbad Cavern (photo by A. Klimchouk).<br />
Plate 13. Partitions of carbonate fracture fill,<br />
only 1-10 cm thick, completely (left photo) or<br />
partially (right photo) partitioning large<br />
passages in Zoloushka Cave, western<br />
Ukraine. Photos by B. Ridush.<br />
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