Trow Gill, North Yorkshire - Places of Geologic Significance on Waymarking.com

Trow Gill could have been formed as melt waters flowed as glaciers melted. Typical of other rocks but Trow Gill is limestone. So more likely surface water found weaknesses between the layers to create an underground chamber. Eventually the roof collapsed. The water is elsewhere now.

The exposed walls have not gone unnoticed. There are many climbing routes throughout between 6 - 20 meter high. The path to Ingleborouqh ascends the notch at the back.

After parking for free on street in Clapham, there is a 60 pence (adult in 2008) charge to walk through landscaped woodland along the shortest route Clapdale Drive vehicle track. There are alternate free routes, only marginally further, one along Long Lane and across Clapdale Beck (visit link) and another via Clapdale farm.

Links
Climb info (visit link)
Rockfax Climb info (visit link)
go4awalk (visit link)
Been There .... picture (visit link)
Peak and Fell Walking (visit link)

Waymark is confirmed to be publicly accessible: yes Parking Coordinates: N 54° 07.183 W 002° 23.431 Access fee (In local currency): .00 Requires a high clearance vehicle to visit.: no Requires 4x4 vehicle to visit.: no Public Transport available: no Website reference: [Web Link]

Visit Instructions:
No specific requirements, just have fun visiting the waymark.

Recent Visits/Logs:

Date Logged Log User Rating   09/03/2014 xtqx1 visited it 09/03/2014 Lettertrolline visited it 08/12/2012 flosse07 visited it 04/08/2012 Jurassic Parkinsons visited it 11/29/2009 hillhiker1 visited it 03/16/2009 pete37038 visited it

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