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Jim Holmes: Track/2837 in area near Brandon, Brandon Group (Ireland)
The Tom Crean Challenge
Ascent: 1770m,
Length: 29.6km,
Creator time taken: 10h11m
Descent: 1859m,
Time predicted from Naismith's rule: 8h 53m + breaks
Ballybrack Mid (B'Brack) Q42763 09257, Brandon, Brandon South Top, Gearhane, Ballysitteragh, Beennabrack, An Bhinn Dubh, An Cnapán Mór, Cnoc na Bánóige, Knockmulanane West Top, Knockmulanane, end at Anascaul Village (AnScaul) Q59278 01879, 18km E from Start
Track Rating ..
[RWD version 1 ]
This was the Tom Crean Challenge 2014 as hosted by the Annascaul Hillwalking Club - this beautiful "Ridge" walk took place on an absolutely glorious day in June. With the day affording the best of views there was never going to be any mad rush home!
Jim Holmes.
Read the Report of the day (copy and paste address into your browser).
http://mountainviews.ie/challengecalendar/node/41/
Jim Holmes.
Read the Report of the day (copy and paste address into your browser).
http://mountainviews.ie/challengecalendar/node/41/
Editing Details for track/2837
NOTE: ALL information such as Ascent, Length and Creator time taken etc should be regarded as approximate. The creator's comments are opinions and may not be accurate or still correct.
Your time to complete will depend on the speed of the slowest plus break time and your mode of transport.
NOTE: It is up to you to ensure that your route is appropriate for you and your party to follow bearing in mind all factors such as safety, weather conditions, experience and access permission.
Your time to complete will depend on the speed of the slowest plus break time and your mode of transport.
NOTE: It is up to you to ensure that your route is appropriate for you and your party to follow bearing in mind all factors such as safety, weather conditions, experience and access permission.
Uploaded on: Sun, 29 Mar 2015 (22:17:31), Linkback: https://mountainviews.ie/track/2837/
* Note: A GPS Height in the elevation profile is sourced from the device that recorded the track. An "SRTM" height is derived from a model of elevations for parts of the earth. More detail
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