The Wolds


The Wolds is a term used in England to describe a range of hills which consists of open country overlying a base of limestone or chalk.

Geography

The Wolds comprise a series of low hills and steep valleys underlain by calcareous and sandstone rock, laid down in the Cretaceous period. The characteristic open valleys of the Wolds were created during the last glacial period through the action of glaciation and meltwater. The chalk that underlies the Chalk Wolds Landscape Character Type extends from the Yorkshire Wolds to the south coast of England, in East Sussex and in Dorset. Geologically, the Lincolnshire Wolds is a continuation of the Yorkshire Wolds which runs through the East Riding of Yorkshire; the point at which the ranges of hill crosses the Humber is known as the Humber Gap.

Etymology

The name Wold is derived from the Old English meaning "forest",. Wold is an Anglian form of the word, as in other parts of England, different variations can be found.
Over the years the meaning has changed from "forest" to "open high ground". Wold originally would have applied to high forest land. However when the forest was cleared, it is probable that the original name survived. This was particularly true in the Cotswolds, the Lincolnshire Wolds and also the Yorkshire Wolds.

Example of Wolds in literature

Westward before her rose fold upon fold of the encircling hills, piled rich and golden.
Description of the Yorkshire Wolds by Winifred Holtby.

Citations