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ABSTRACTS / RESUMES - Comitato Glaciologico Italiano

ABSTRACTS / RESUMES - Comitato Glaciologico Italiano

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KANGNING XIONG, CAIHUA HE & XING CHENG<br />

Analysis of structural features of rimstone in karst caves<br />

Department of Geography, Guizhou Normal University,<br />

Waihuandong Rd, 550001Guiyang, China<br />

This paper, based on fieldwork and experiments, looks at<br />

structural types and features of rimstone in karst caves.<br />

The rimstones developed in caves are quite different from<br />

those formed on river beds, the former appear porous, like<br />

tufa, which are resulted from higher temperature and biological<br />

process. The rimstones in caves, apart from their<br />

features similar to river rimstone, obviously appear compacted<br />

and graded. Three types of rimstone are identified<br />

according to different conditions of water movement and<br />

different shapes of water recharge distribution, water-way<br />

model, fan model and circle model. Each reflects different<br />

408<br />

condition of water movement. Water of the water-way model<br />

is from stream or intermittent stream for recharge. Plan<br />

distribution of the fan model rimstone appears fan-shaped<br />

and the relevant recharge type is mainly fissure water or<br />

dripping flow. The circle model rimstone looks semi-circle-shaped<br />

on plan, which is a rare type developed in a<br />

special mini-topographic environment, formin from dripping<br />

recharge. Hydraulic conditions of these types above<br />

are respectively changing from strong to weak. The cave<br />

rimstons are also classified, from profile shape, dip angle<br />

and inner structure of lamination, as vertical dam, steep<br />

dam (60°-90°) and slope dam «60 0).These dip changes also<br />

reflect the conditions of water movement from strong to<br />

weak respectively. In addition, the paper notes some special<br />

rimstone types such as double dam, dam-in-dam, ect.<br />

and the relevant hydrogeological significance, presents relationship<br />

between cave rimstone structure, inner lamination<br />

and flow conditon of recharge water, reveals factors of<br />

water movement in rimstone formation, and disscuses initial<br />

morphological problems of rimstones.

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