South Shields in the context of "Jarrow"

Tyne and Wear (/ˌtaɪn  ...  ˈwɪər/) is a ceremonial county in North East England. It borders Northumberland to the north and County Durham to the south, and the largest settlement is the city of Newcastle upon Tyne.

The county is largely urbanised, with an area of 540 square kilometres (210 sq mi) and a population of 1,178,389 in 2024. Newcastle is located on the north bank of the River Tyne in the centre of the county, and Gateshead opposite on the south bank. South Shields lies in the east at the river's mouth, and the city of Sunderland in the south-east at the mouth of the River Wear. Nearly all of the county's settlements belong to the Tyneside or Wearside conurbations, the latter of which extends into County Durham. For local government purposes Tyne and Wear comprises five metropolitan boroughs: Gateshead, Newcastle upon Tyne, Sunderland, North Tyneside and South Tyneside. The borough councils collaborate through the North East Combined Authority, which also includes Durham County Council and Northumberland County Council. The county was created in 1974 from south-east Northumberland and north-east County Durham.

A brig is a type of sailing vessel defined by its rig: two masts which are both square-rigged. Brigs originated in the second half of the 18th century and were a common type of smaller merchant vessel or warship from then until the latter part of the 19th century. In commercial use, they were gradually replaced by fore-and-aft rigged vessels such as schooners, as owners sought to reduce crew costs by having rigs that could be handled by fewer men. In Royal Navy use, brigs were retained for training use when the battle fleets consisted almost entirely of iron-hulled steamships.

Brigs were prominent in the coastal coal trade of British waters. 4,395 voyages to London with coal were recorded in 1795. With an average of eight or nine trips per year for one vessel, that is a fleet of over 500 colliers trading to London alone. Other ports and coastal communities were also served by colliers trading to Britain's coal ports. In the first half of the 19th century, the vast majority were rigged as brigs, and that rig was retained for longer in the northeast of England.

In horticulture, the term bedding refers to flowering plants which can be planted in flower gardens and flower beds. These fast-growing plants in seasonal flower beds create colourful displays, during spring, summer, fall or winter, depending on the climate. Plants used for bedding are generally annuals, but biennials, tender perennials, and succulents are also used.

Flowering bedding plants are also grown in containers and pots positioned on patios, terraces, decks and other areas around houses. Large containers of bedding plants are used in public displays along city streets, plazas and hanging from city light posts.

The Magnesian Limestone is a suite of carbonate rocks in north-east England dating from the Permian period. The outcrop stretches from Nottingham northwards through Yorkshire and into County Durham where it is exposed along the coast between Hartlepool and South Shields. The term has now been discontinued in formal use though it appears widely in popular and scientific literature on the geology of northern England.

The Magnesian Limestone is now incorporated within the Zechstein Group. In the southern part of its outcrop, the former 'Lower Magnesian Limestone' is now referred to as the 'Cadeby Formation'. Overlying this it is the 'Edlington Formation' (formerly the 'Middle Permian Marl') and above this the Brotherton Formation (formerly the 'Upper Magnesian Limestone'). In the north, the Lower Magnesian Limestone is now referred to as the Raisby Formation and the middle Magnesian Limestone as the Ford Formation. The Upper Magnesian Limestone is replaced by the Roker Formation (in its lower part) and the Seaham Formation (in its upper part) with the Edlington formation between them, though in the Durham area this last is replaced by the Fordham Evaporite Formation and the Seaham Residue.