Water from the gorge and the gutters that carry it
The 1968 flood is a measure of what the hills can send down, and a gutter is the first thing it meets.
On the night of the 1968 flood, water came down Cheddar Gorge hard enough to move large boulders and sweep away cars. A roof gutter is a very small channel by comparison, but the same rule applies: what falls on the high ground reaches the village fast, and the drains must take it. A roof does not need a flood to be overwhelmed. A summer storm lasting an hour can fill a gutter that has a few leaves in it.
The size and slope of a gutter decide how much it can carry. A run laid with too little fall holds water at the flat end and spills at the first joint. A run with brackets spaced too widely sags between them. Older cast-iron gutters corrode from the underside, where the damage is not visible, and plastic ones go brittle in sunlight and crack at the bracket. Downpipes then block, and a blocked pipe lets the overflow run straight down a wall that is already damp.
We trace each run from the high point to the ground. We test the joints with water, check the fall with a level and look at where each pipe ends. Water should leave the building by a gully, drain or soakaway, not simply at the foot of a wall. The fascia and soffit, the boards that close the eaves, go the same way as the gutter: a gutter that has leaked for years will have rotted the fascia behind it.
Where a gutter is past mending, we replace it with a profile and material that match the house. Replacement options for all three are described on the gutters, soffits and fascias service page.



