-wich town

A "-wich town" is a settlement in Anglo-Saxon England characterised by extensive artisanal activity and trade – an "emporium" – and supplied from outside the protected community. The name is derived from the Anglo-Saxon suffix -wīc, signifying "a dwelling or fortified place". Such settlements were usually coastal and many have left material traces found during excavation.

Eilert Ekwall wrote: "OE wīc, an early loan-word from Lat vicus, means ‘dwelling, dwelling-place; village, hamlet, town; street in a town; farm, esp. a dairy-farm’. . . . It is impossible to distinguish neatly between the various senses. Probably the most common meaning is ‘dairy-farm’. . . . In names of salt-working towns . . . wīc originally denoted the buildings connected with a salt-pit or even the town that grew up around it. But a special meaning ‘salt-works’, found already in DB, developed."

As well as -wich, -wīc was the origin of the endings -wyck and -wick, as, for example, in Papplewick, Nottinghamshire.

History of salt

Salt, NaCl, is an ionic compound made of sodium and chloride ions which has been exceptionally important to humans for thousands of years, because it is one of the substances upon which all of life evolved to depend. Humans, like all life, need a supply of salt in order to simply survive. Salt's ability to preserve food was a foundation of civilization. It helped to eliminate the dependence on the seasonal availability of food and it allowed travel over long distances. However, salt was difficult to obtain, and so it was a highly valued trade item to the point of being considered a form of currency by certain peoples. Many salt roads, such as the via Salaria in Italy, had been established by the Bronze age.

Today, salt is almost universally accessible, relatively cheap and often iodized.

Sources

There have been two main sources for salt: sea water and the sodium chloride mineral halite (also known as rock salt). Rock salt occurs in vast beds of sedimentary evaporite minerals that result from the drying up of enclosed lakes, playas, and seas. Salt beds may be up to 350 m thick and underlie broad areas. In the United States and Canada extensive underground beds extend from the Appalachian basin of western New York through parts of Ontario and under much of the Michigan basin. Other deposits are in Texas, Ohio, Kansas, New Mexico, Nova Scotia, and Saskatchewan. In the United Kingdom underground beds are found in Cheshire and around Droitwich. Salzburg, Austria, was named "the city of salt" for its mines. High-quality rock salt was cut in medieval Transylvania, Maramureş and Southern Poland (Wieliczka). Tuzla in Bosnia and Herzegovina was named in Hungarian Só (salt) from the twelfth century on and later "place of salt" by Turks.

Droitwich (UK Parliament constituency)

Droitwich was the name of a constituency of the House of Commons of England in 1295, and again from 1554, then of the House of Commons of Great Britain from 1707 to 1800 and of the House of Commons of the Parliament of the United Kingdom from 1801 to 1918. It was a parliamentary borough in Worcestershire, represented by two Members of Parliament until 1832, and by one member from 1832 to 1885. The name was then transferred to a county constituency electing one MP from 1885 until 1918.

History

The borough consisted of three parishes and parts of two others in the town of Droitwich, a market town which for many centuries depended on the salt trade for its prosperity. When Droitwich's right to return MPs (which had been allowed to lapse) was restored in 1554, there was only one salt pit in the borough, and this became the basis of Droitwich's unique franchise: the right to vote was vested solely in those burgesses (members of the corporation) who owned shares in the pit giving them the right to draw brine. This was finally established by a resolution of the House of Commons in 1690; yet within a few years of this date that salt pit had dried up completely; by 1747 it was accepted that ownership of this property had no function except conferring the vote, and had to be proved by possession of the title deeds since there could be no evidence of an otherwise meaningless right which could not be exercised in practice.