Step 1. Allow the pampas grass to discolor over the winter months. The natural death of the leaves provides some texture in fall and winter landscape. To limit tipping of the heavy blades, tie twine around the entire plant at 6-inch intervals to keep the grass clump upright.
Rising damp is the common term for the slow upward movement of water in the lower sections of walls and other ground-supported structures by capillary action. Although rising damp of up to 5 metres in height has been observed the height of rise is typically much lower and is rarely above 1.5m.Rising damp has been a widely observed phenomenon for at least two hundred years.lthough rising damp of up to 5 metres in height has been observed the height of rise is typically much lower and is rarely above 1.5m. Rising damp has been a widely observed phenomenon for at least two hundred years.
A: A creep is the slow, downward movement of soil or debris. One factor thought to contribute to a creep is heaving. Heaving is the expansion and contraction of rock fragments during wet and dry cycles. A creep is hard to identify at first because the process moves so slowly. There are signs that indicate it is occurring, including bent trees, cracked walls and tilted fences. The rate of the creep depends on a variety of factors, including the steepness of the slope, the amount of water in the soil, the sedimentation and the vegetation. Creeps are what give hillsides their rounded slopes. Learn more about Earth Science