I was up on the cliffs yesterday and noticed the amount of erosion that has occurred over the winter months. It appears that no action is being taken but I wonder how long it can continue its course without parts of it finally plummeting into the sea? This will impact the cliff walk to Bradda Glen, just as the closure of the lower route has done, but having the higher route at least has always meant an alternative route.
The coast path to the south is closed behind the marine biological station for slippage up until May 27th, reopening just in time for TT.
It has been quite a wild winter over here. Not that it has been cold, wet or snowy. Just windy. It is noticeable the number of trees in the glens that were demolished by the winds and what were quite leafy glades are now more exposed to the sky, though this will change as they come into leaf. It does enable to ground-loving plants to come into their own, so there is always an upside to this kind of destruction.
I stopped at my usual hotspot on the beach and watched the tide come in until it lapped against my feet, then I walked home via Athol Park Glen. This must be one of the smallest glens anywhere. It takes less than 5 mins to walk end to end, unless like me you amble slightly off the footpath to take in its hidden gems. Even so, at its widest it can only be 200 yards or so! The bluebells and white bells looked almost more effective there being only a few of them, and the light cast wonderful shadows of the trees.