place

Church of St Oswald, Lythe

12th-century church buildings in EnglandChurch of England church buildings in North YorkshireGrade I listed churches in North YorkshireUse British English from April 2019
St. Oswald's church, Lythe, through lych gate 2016 05 28
St. Oswald's church, Lythe, through lych gate 2016 05 28

The Church of St Oswald, Lythe, is the parish church for the village of Lythe, 4 miles (6.4 km) west, north west of Whitby in North Yorkshire, England. The church is at the top of Lythe Bank (the western end) and is just east of the village on the A174 road. A church has been on the site since the 13th century, though the present building was adapted from the old church in 1910 by Sir Walter Tapper. It was grade I listed in 1969.

Excerpt from the Wikipedia article Church of St Oswald, Lythe (License: CC BY-SA 3.0, Authors, Images).

Church of St Oswald, Lythe
Lythe Bank,

Geographical coordinates (GPS) Address Nearby Places
placeShow on map

Wikipedia: Church of St Oswald, LytheContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 54.5066 ° E -0.6884 °
placeShow on map

Address

Lythe Bank
YO21 3RG
England, United Kingdom
mapOpen on Google Maps

St. Oswald's church, Lythe, through lych gate 2016 05 28
St. Oswald's church, Lythe, through lych gate 2016 05 28
Share experience

Nearby Places

Sandsend Ness
Sandsend Ness

Sandsend Ness is an old alum quarrying site close to Whitby in North Yorkshire, England. Beneath extensive deposits of grey pyritic shale a thin band of sideritic mudstone is present at this site and there is a further 6 metres (20 ft) of almost non-bituminous shale beneath it. This geological configuration, along with its proximity to the port of Whitby, offered Sandsend near-ideal conditions for the rapidly expanding alum industry from the early 17th century onwards. So wide-scale and prolonged were these activities, that significant areas of the Yorkshire coast were permanently altered. The double sulphate of aluminium and either potassium or ammonia is commonly known as alum. This material was of great importance through to the late 19th century in leather tanning and in the wool dying industry. Even today it is still used in some places as a mordant (dye fixative). Fossils are present in large numbers in the deposits, including ammonites such as Hildoceras bifrons and Dactylioceras bifrons and also Ichthyosaur and Plesiosaur remains, though the latter are nowadays much less commonly found. In fact, the ammonite Hildoceras is named after an early Christian saint, the Abbess of Whitby St. Hild or Hilda (614–680). It was believed that such ammonite fossils were the snakes which had been miraculously turned into stone by St. Hilda. It was not unknown for local "artisans" to carve snakes' heads onto ammonites, and sell these "relics" as proof of the miracle. The coat of arms of nearby Whitby actually include three such 'snakestones'.