Coumshingaun Corrie Lake in county Waterford is truly the land that time forgot !
In Ireland compared to some locations in North America and Canada it is impossible to be more than a few miles away from a town or a village, some locations in the north and far southwest of the country are more remote that here in the southeast county’s. Yet even here there is still the possibility of finding a remote feeling hidden away in a small location or two.
Coumshingaun Corrie Lake, county Waterford is for just one of these locations, the walk up to it from the valley floor and road below is no more than two kilometers, its a uphill walk from the car park located below the tree line, most people however given time would be able to do this walk !!. However in anyone’s book this is not going an an expedition 🙂
When you get there, the view of the lake at its surrounding cliffs is breath taking, the lake is a left over from the last ice age, some 15000 year ago, this is from a time well before Ireland had even a single human-being living here.
Most weekends you will find other Humans/people visiting here so if you want a true feeling of space and allown-ness then early morning, and weekdays evening is the best time to visit.
I love it here , its about an hours drive from home, yet it could be like a visit to Canada or Yellowstone park with a little imagination allowed to run out of control 🙂
Coumshingaun Corrie Lake, county Waterford : The land time forgot
Taken on the same day as the image of Milk hill, this image shows a view of Coumfea a corrie lake in the Nier valley, I have many other images of the lake that I will post in full.
A Corrie lake is formed as follows :
How Is a Corrie Formed?
A corrie is formed in different steps. First, the snow accumulates in a hillside hollow and turns to ice. Then, the hollow is deepened by abrasion and plucking and the ice in the corrie moves under the influence of gravity, deepening the hollow still further. Since the ice is at the foot of the hollow and moves more slowly, a rock lip forms. When the ice melts, a lake or tarn may be formed in the corrie. The steep back wall may be severely weathered by freeze€“thaw weathering, providing material for further abrasion.