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Other Sites Within 500m

CG23  CG25  Pharnassus (Uamh)  East Gully Upper Through Cave  CG30  CG21  Lower Parnassus Cave  West Gulley Upper Through Cave  West Gulley Upper Through Cave [entrance]  West Gulley Upper Through Cave [lower entrance]  West Gulley Lower Through Cave [sink]  West Gulley Lower Through Cave [resurgence]  Slaodach (Uamh)  Shelf (Uamh an t-) hole to daylight  Shelf (Uamh an t-)  CG35  Tiny Pot  Briste (Uamh)  CG33  CG39  CG13  CG14  CG15  CG38  Sheep's Head Cave  West Resurgence  East Resurgence  Sheep's Head Resurgence  Cos Mointeachail (Uamh an)  Iarann, Uamh an t-  Angel's Cave  CG31  CG12  CG43  Crioch, Uamh  CG11 

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East Gulley Stream Sink

Skye, Coille Gaireallach, East Gulley, Invernessshire.

NGR:NG 60600 19405
WGS84:57.20268, -5.96527
Length:9.1 m
Vert. Range:4.6 m
Altitude:145 m
Geology:Limestone, Beinn An Dubhaich Granite (Skye Eastern Red Hills Centre: Phase 3) - Granite, Granophyric
Tags:Cave, Sink, SSSI
Registry:main

Sink in the East Gulley (a non-continuous string of holes, uphill of the rising near the West Gulley Upper Through Cave - C.G. 17/18). A stream sink at the head of the East Gulley. The entrance was dug out by Moldywarps Speleological Group, Oct. 1978. A grovel in the stream under a low arch into a chamber 4 m long, 1 m high. At end on the right, a stream drops into a narrow rift passage then turns right along a large slab. Step through 'window' to inclined rift becomes too tight. Good draught but little prospect of progress.

Alternative Names: CG24, C.G. 24, Cross Rift Cave

Notes: Coille Gaireallach is part of the Strath SSSI. Best example of an Oak and Birch/Hazel wood developed on Durness limestone. Situated on a gentle north-facing slope, a rich limestone ground flora alternates with acid heath and flushes, with open areas and sink holes.

From coordinates plotted on aerial photograph this would appear to be well up the the granite slope, uphill to the south of the Oak and Birch/Hazel woodland beyond a drystone dyke. Geological map shows a band of granite which suggests surface run off through a hole in the the granite into limestone below.

Hydrographic Feeds: Granite hillside northeast of Beinn an Dubhaich

Hydrographic Resurgences: Minor feeder to Allt Strath Suardal

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This entry was last updated: 2021-04-09 20:16:35

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