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Garage sale in northern California Diverse items bought at a moving sale held in Boise, Idaho. A garage sale (also known as a yard sale, tag sale, moving sale and by many other names [1]) is an informal event for the sale of used goods by private individuals, in which sellers are not required to obtain business licenses or collect sales tax (though, in some jurisdictions, a permit may be ...
This archetypal form of swale is a dug-out, sloped, often grassed or reeded "ditch" or "lull" in the landform. One option involves piling the soil onto a new bank on the still lower slope, in which case a bund or berm is formed, mitigating the natural (and often hardscape-increased ) risks to slopes below and to any linked watercourse from ...
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[2]: 19 Bioswale design is intended to safely maximize the time water spends in the swale, which aids the collection and removal of pollutants, silt and debris. Depending on the site topography, the bioswale channel may be straight or meander.
The parish contains the village of Brompton-on-Swale and the surrounding countryside. Most of the listed buildings are houses, cottages and associated structures, farmhouses and farm buildings, the majority of them along Richmond Road in the village. The other listed buildings include a bridge, a church, a milepost and a war memorial.
The Swale returns eastward near Hudswell before it flows past the main town of the valley, Richmond. It starts a series of long south-east meanders past Brompton-on-Swale and passes under the A1 at Catterick Bridge before turning south past Catterick. The river continues long south and south-east meanders past Thrintoft and Morton-on-Swale.
South Swale is a 410.5-hectare (1,014-acre) Local Nature Reserve (as South Bank of the Swale) north of Faversham in Kent. It is owned by Kent County Council and managed by Kent Wildlife Trust . [ 1 ] [ 2 ] [ 3 ] It is part of The Swale Ramsar site , [ 4 ] Special Protection Area [ 5 ] and Site of Special Scientific Interest [ 6 ]
At these times the Swale was a gully from what had been a sea channel in very warm periods. Namely before the Strait of Dover had swept away so much swampy land, accentuated by sea levels being lower, even to beyond the end of the ice age, i.e. in the mid seventh millennium BC, the coasts of Essex and Kent stretched much further into the North Sea.