Bunsen7: Track 3374 in area near Stradbally Mountain, Central Dingle (Ireland)
Central Dingle Quartet from Anascaul
Length: 15.8km, Creator time taken: 4h45m, Ascent: 949m, Descent: 912m
Places:Start at Q58254 05103, Stradbally Mountain, Beenoskee, Coombane, Beenatoor, end at Start Logged as completed by 1
Follow the track from Anascaul lake car park northwards up onto the mountain plateau. Upon reaching the mountain plateau leave track (which otherwise follows into Glenahoo) and set out in a north easterly direction across open ground.
The views upon reaching the summit of "shrawballa" are fantastic in good weather. My route then headed west over the summit of Beenoskee (pictured on left below, with coumbane and then beenator the lower tops in centre of picture).After Beenoskee, the highpoint of the route, continue west to Coumbane, crossing wire fence. Cross back then after the Coumbane detour and head west for Beenatoor. Beenator summit looks mundane on approach from the East but then it reveals a wondrous view into the Glenahoo valley that should be taken in before returning southwards to the startpoint at Anascaul lake.
Uploaded on: Mon, 16 Jan 2017 (09:55:30) Linkback: https://mountainviews.ie/track/3374/ To download GPS tracks you must be enrolled and logged in. See "Login or enrol", top right - quick and easy.
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 your speed plus break time and your mode of transport. For walkers: Naismith's rule, a rough and often inaccurate estimate, suggests a time of 4h 45m + time stopped for breaks
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.
* 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