Upper Lake, Killarney - 4 Things to Know Before Visiting

Located at the ‘end’ of the gap, if you walk from the Kate Kearny side, Lord Brandon’s Cottage is a welcome site for those that have conquered the first leg of the walk. Once a grand hunting lodge, the cottage has a tale of love and betrayal tide to it, which you’ll discover shortly.

Purple Mountain, is the 21st–highest peak in Ireland on the Arderin scale, and the 28th–highest according to the Vandeleur-Lynam scale. It is located in County Kerry, and is the highest point of the Purple Mountain Group. It is composed of sandstone particles of various sizes which are collectively known as Old Red Sandstone. Old Red Sandstone has a purple-reddish colour, and has virtually no fossils.

Cruach Mhór, is the tenth-highest peak in Ireland on the Arderin list, and the eleventh-highest peak in Ireland according to the Vandeleur-Lynam list. A distinctive square grotto marks the summit. It is part of the MacGillycuddy's Reeks in County Kerry. A good trekking destination and also it offers beautiful views too.

The Gap of Dunloe is one of the most stunningly beautiful parts of County Kerry and indeed Ireland. Stretching through the MacGuillicuddy Reeks mountain range, this beautiful glacial valley simply must be experienced to be appreciated. It is a narrow mountain pass running north-south in County Kerry, Ireland. It is one of Kerry's most popular tourist destinations due to its scenery.

Dinis Cottage on Dinis Island in Killarney National Park looks out over the Middle Lake and was built by the Herberts who at one time owned the lands that are now part of Killarney National Park . The cottage has been described as a hunting lodge and a woodcutter’s hut and dates back to the 1700s. It provides a tempting stop-off for the many visitors, walking the popular Muckross and Dinis 10km circular trail through the National Park and taking in Torc Waterfall.

Moll's Gap is a gap in County Kerry and has an elevation of 237 metres. Moll's Gap is situated south of Derrylea. It offers views of the MacGillycuddy's Reeks mountains, and is a popular tourist location. The rocks at Moll's gap are formed of Old Red Sandstone, which are small quartz grains laid down over 350 million years ago; unlike most of the Old Red Sandstone around Killarney which is stained red by iron oxide, the rock at Moll's gap is stained green by chlorite.