Carrauntoohil and MacGillycuddy's Reeks
By Jim Ryan
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About this ebook
Jim Ryan
Jim Ryan is a chartered civil engineer with a passion for the outdoors, who has had several successful guidebooks and two works of fiction published. Jim's approach to guidebook writing is not simply to take the reader to the destination, but to provide them with a total experience. Geology, flora and fauna, the natural environment, and the folklore and history of the locality are very important to him. Jim splits his time between summers in Cork, Ireland, and winters in Nerja, Spain. He has been climbing the mountains of Andalucía for over 20 years. This guidebook is his way of repaying Nerja and Andalucía for many years of pleasure; his share of the proceeds from its sales go to local charities in Nerja.
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Carrauntoohil and MacGillycuddy's Reeks - Jim Ryan
Contents
Using this Book
Maps, Grid References and GPSs
Walk Times, Escape Routes, Access to Lands
MacGillycuddy’s Reeks – A Profile
Ireland’s Highest Mountains
Geology
History
Evicted from the Gap of Dunloe
Flora
Fauna
Who Owns the Reeks?
People of the Reeks
Climate
Placenames and Townlands
Kerry Mountain Rescue
Action Plan for the Reeks
Getting There
Maps
Killarney to the Gap of Dunloe
The Gap of Dunloe and the Black Valley
Cronin’s Yard
Lisleibane
Glencar
Practicalities
Checking the Weather Forecast
Camping
Hostels
Killarney
Fossa
Beaufort
The Gap of Dunloe
The Black Valley
Glencar
The Walks
An Overview with Difficulty Ratings
The Gap Of Dunloe Area
Walk 1 The Gap of Dunloe and the Eastern Reeks
Walk 2 Purple Mountain
Walk 3 Tomies via The Chimneys
Walk 4 The Lough Googh Circuit
Safe Ascents & Descents on Carrauntoohil
Critical Appraisal of Routes
Popularity of Routes
Hag’s Glen Eastern Side
Walk 5 Cummeenapeasta Circuit
Walk 6 Carrauntoohil via The Devil’s Ladder
Walk 7 Up the Zig-zags (Bóthar na Gíge) and Down The Bone
Hag’s Glen Western Side
Walk 8 Carrauntoohil via O’Shea’s Gully returning by Heavenly Gates
Walk 9 Carrauntoohil via Curved Gully or Central Gully
Walk 10 Stumpa an tSaimh Ridge to Beenkeragh
Walk 11 Beenkeragh via Cummeenagearagh
Routes from Glencar
Walk 12 The Coomloughra Horseshoe
Walk 13 The Black Mare Ascent to Carrauntoohil
The Reeks Walks
Walk 14 The Gap of Dunloe to Glencar
Walk 15 The Hag’s Glen Circuit
The Black Valley and the Bridia Valley
Walk 16 Carrauntoohil from the Black Valley
Walk 17 Caher from the Lack Road
Walk 18 The Lough Duff Circuit
Low Level Walks
Walk 19 The Gap of Dunloe to Derrycunnihy Church
Walk 20 The Kerry Way through the Black Valley to Lough Acoose
References and Further Reading
About the Author
Maps
Map 1 West Munster
Map 2 The Killarney Area
Map 3 The Reeks
Map 4 The Gap of Dunloe and Eastern Reeks
Map 5 Purple Mountain
Map 6 The Lough Googh Circuit and Cummeenapeasta
Map 7 Ascents and Descents on Carrauntoohil
Map 8 The Devil’s Ladder, the Zigzags and the Bone
Map 9 O’Shea’s, Curved and Central Gullies, Heavenly Gates
Map 10 Stumpa an tSaimh and the Beenkeragh Ridge
Map 11 Cummeenagearagh Ascent, the Black Mare Ascent & the Coomloughra Horseshoe
Map 12 The Reeks Walk from Dunloe to Glencar
Map 13 The Kerry Way from the Black Valley to Lough Acoose
Map 14 The Gap of Dunloe to Derrycunnihy
USING THIS BOOK
Maps, Grid References and GPSs
The maps in this book are extracted from the Ordnance Survey Ireland (OSI) 1:25,000 map of the MacGillycuddy’s Reeks. They were produced by OSI and are subject to copyright.
GPSs should be configured to the Irish Grid, with units in metres.
Throughout this book key landmarks are given using Ordnance Grid References. For example: Carrauntoohil is at grid reference Height: 1039 Longitude: 80360 Latitude: 84415. The six-digit conventional reference would be 803844 i.e. the first three digits of the GPS co-ordinates.
The longitude refers to the horizontal distances between the vertical grid lines. Since the longitude and latitude grid lines are somewhat similar to each other in this area it is important not to mistake one for the other.
The GPS reading is only as good as the satellites it can track. In mountainous areas the surrounding high ground will often obscure satellites. In gullies, for instance, a GPS will have limited accuracy.
Jim Ryan (standing) with friends at dawn on the summit of Beenkeragh
Walk Times, Ascents
The common time calculation of one hour for every 400m ascent and one hour for every 4 km of flat walking should generally agree with the walk times given in this book. The ascents given are the cumulative ascents over the walk.
Escape Routes
Escape routes are suggested in case of an emergency, where it is imperative that one has to descend to lower ground. They are not intended as alternative routes.
Access to Lands
The walks shown in this book are generally over private property. Although much of the lands are classed as commonage, this merely relates to their ownership in common by a number of people. There are few rights of way, except on public roads, so that the walker enters the lands at the discretion of the owners.
The Country Code
Hillwalkers should be familiar with the country code of leaving no trace. Please do not block gateways or access points, close all gates, do not interfere with fences, ensure that sheep and other farm animals are not interfered with, make as little noise as possible, remove all rubbish, even if it is not your own.
MACGILLYCUDDY’S REEKS A PROFILE
Ireland’s Highest Mountains
The MacGillycuddy’s Reeks are Ireland’s highest mountains. They include the country’s three highest peaks, all over 1000 m: Carrauntoohil which soars to 1039 m, nearby Beenkeragh which has a height of 1010m and Caher at 1001 m.
The Reeks stretch from the picturesque Gap of Dunloe in the east to Glencar in the west. Within this relatively confined area of 100 square km there is great natural beauty and wild rugged mountain terrain. The placenames are evocative and give some sense of the history and charm of this part of Kerry: Hag’s Glen, The Big Gun, Eagle’s Nest, The Devil’s Ladder and the Hag’s Tooth. Attracting over 25,000 walkers each year, the area is a wonderful natural resource.
As the numbers increase, the degree of tragedy on the mountains multiplies. Between 1966 and 2000 there were seventeen fatalities on the Reeks, equating to one every second year. Since 2000 this rate has increased to two per annum. Many come ill-prepared, lacking proper gear, possibly without even a map. The routes up the Reeks are not clearly marked; the mountains are covered in mist for three-quarters of the time; it is therefore essential for visitors to have a basic knowledge before entering the area.
The Reeks from Maolán Buí
In books that describe the climbing routes on the Reeks the information provided is often scant. The main purpose of this book is to indicate with clear maps and photographs a variety of popular trails. The route descriptions give grid reference locations of important landmarks. This will enable the hillwalker to discover, either with a map and a compass or a GPS, where he/she is and what direction to take.
Climbing a mountain should never be simply about getting to the top. It is in these wild and secluded places that we see nature at its best. There is much to interest the hillwalker, from the wonder of how the mountains were formed in the first place to the creatures and plants that make them their home. A secondary purpose, therefore, is to make a visit to this part of Kerry as memorable and enjoyable as possible. Thus information is provided on the geology, history, flora and fauna of the Reeks.
GEOLOGY
The Bedrock of the Reeks
The bedrock of the Reeks is composed generally of sandstones of varying particle size, which are collectively known as the ‘Old Red Sandstone’. These rocks date from the Devonian Period (410 to about 350 million years ago) when Ireland was located in a hot, arid, equatorial setting. During these 60 million years, southern Ireland was the site of a major sedimentary basin known as the Munster Basin in which sediment accumulated to an enormous thickness. Most of Counties Kerry and Cork was a vast low-lying alluvial plain into which seasonal rivers drained southwards. The layers of sediment which were deposited on the alluvial plain formed the Old Red Sandstone and were derived from a mountainous area to the north. Chemical oxidation resulted in much of the sediment becoming stained with a distinctive red or purple colour. This is due to the mineral haematite, a form of iron oxide.
The composition of the Old Red Sandstone is variable. It contains mudstones, fine to coarse grained sandstones, quartz pebbly sandstones and the concrete-like quartz conglomerates of varying colours. Outcrops of quartz conglomerate are visible at the base of the Turf Path in the Gap of Dunloe, on the Beenkeragh Ridge, at Tomies Chimneys and the northern side of Purple Mountain at Cathair and Tomies. Boulders of quartz conglomerate are dispersed throughout the Reeks at many locations.
Quartz conglomerate rock
The sedimentary layers of the Iveragh Peninsula can be subdivided into three rock formations: the Lough Acoose Formation, the Chloritic Sandstone Formation and the Ballinskelligs Sandstone Formation in ascending order. The cumulative thickness of these layers is quite startling, being in excess of 7 km.
Old Red Sandstone is not particular to the south of Ireland. It is also common in many parts