Sep 20, 2017 · A peat hag is a type of erosion that can occur at the sides of gullies or seemingly in isolation. Peat hags arise as a result of water flow eroding downwards into the peat or where a fire or overgrazing has exposed the peat surface to dry out and blow or wash away.

Peat "hags" are a form of erosion that occur at the sides of gullies that cut into the peat; they sometimes also occur in isolation. [80] Hags may result when flowing water cuts downwards into the peat and when fire or overgrazing exposes the peat surface.

• Steep peat faces found in hags and gully sides cannot be readily revegetated. The gradient must first be reduced by reprofiling (see Section on hag/gully/peat bank reprofiling). • In narrow steep gullies, re-vegetation should begin to propagate upstream from local blockages.

May 14, 2021 · A hagg is a bare face of peat, fairly steep and almost like a mini cliff. These are often eroded further by stock which shelter against the wind here, and rub more of the oxidised peat away. It’s hugely important to treat bare peat due …

The meaning of PEAT HAG is ground from which peat has been cut.

Jul 15, 2016 · Peat hags, for those who haven’t yet encountered them, comprise of ridiculously large patches of peat (you know the stuff, we wouldn’t dream of trying to walk in it on Dartmoor) punctuated by man-sized tufts of more solid greenery.

Jun 17, 2016 · However, up close, there is a great deal of variation in the surface of a peat bog including raised mushroom-shaped mounds called peat hags, continuous ribbons of sedge grass, holes in the ground that lead to underground streams, drier areas of peat, and wetter sections that will suck off your shoes and may be difficult to escape from.

Sep 17, 2024 · Peatland ACTION is a national programme to restore peatlands across Scotland. It is led and funded by Scottish Government and delivered in partnership with NatureScot, Loch Lomond & the Trossachs National Park Authority, Cairngorms National Park Authority, Scottish Water, and Forestry and Land Scotland.

Peat hags are steep faces of eroding peat, largely formed as a result of historic peat cutting for fuel. In order to enable these to become revegetated, an excavator with low ground pressure tracks is used to reduce the angle of the peat face.

It provides an overview of the procedural and technical requirements for peatland restoration in Scotland, alongside an introduction to the types of restoration interventions that have been applied to date by Peatland ACTION.