Old Shire Hall, Cardigan

Castle Green House is a Grade II* listed house located in the grounds of Cardigan Castle, Cardigan, Ceredigion, Wales. It was restored in the 2000s and now acts as a museum, events centre and residential accommodation.

Cardigan Castle (Welsh: Castell Aberteifi) is a castle overlooking the River Teifi in Cardigan, Ceredigion, Wales. It is a Grade I listed building. The castle dates from the late 11th-century, though was rebuilt in 1244. Castle Green House was built inside the castle walls in the early 1800s. After falling into disrepair the castle was restored in the early 2000s and opened to the public in 2015. It is owned by Ceredigion County Council and now includes a heritage centre and open-air concert facilities. The castle's gardens are listed on the Cadw/ICOMOS Register of Parks and Gardens of Special Historic Interest in Wales.

Cardigan Guildhall (Welsh: Neuadd y Dref Aberteifi), is a municipal building in Pendre, Cardigan, Ceredigion, Wales. The structure, which is now used as an art gallery and community events venue, is a Grade II* listed building.

Cardigan County School is the name given to the endowed grammar school in Cardigan which was founded there in the mid seventeenth century (1653). The Intermediate School was opened in the Cardigan Free Grammar School on 4 November 1895, and a new building was opened on 21 September 1898. It seems the school lost its county status in 1949 and was succeeded by the Cardigan Secondary School. Records of the school up to 1949 are held in the Ceredigion Archives in Aberystwyth.

Cardigan (Welsh: Aberteifi, pronounced [abɛrˈtei̯vi] ) is both a town and a community in the county of Ceredigion, Wales. Positioned on the tidal reach of the River Teifi at the point where Ceredigion meets Pembrokeshire, Cardigan was the county town of the historic county of Cardiganshire. Cardigan is the second-largest town in Ceredigion. The largest town, Aberystwyth, is one of the two administrative centres; the other is Aberaeron. The settlement at Cardigan was developed around the Norman castle built in the late 11th or early 12th century. The castle was the location of the 1176 Cardigan eisteddfod, precursor of the present-day National Eisteddfod. The town became an important port in the 18th century, but declined by the early 20th century owing to its shallow harbour. The castle underwent restoration in 2014. The population in 2001 was 4,203, reducing slightly to 4,184 at the 2011 census.

Cardigan railway station in the county town of Cardigan, Ceredigion was the terminus of the Whitland and Cardigan Railway, opened on 31 August 1886. The line, previously known as the Whitland and Taff Vale Railway, and later familiarly as the 'Cardi Bach', was built between 1869 and 1873. With the extension to Cardigan opening in 1886, operations were taken over by the Great Western Railway.Situated on the south side of the River Teifi, the arrival of the railway to Cardigan saw a gradual decline of trade from the port, with goods thereafter travelling on the railway. The railway station closed to passengers on 10 September 1962 (prior to the Beeching Axe) but remained open to goods traffic until 27 May 1963. After that date the station remained open as a coal depot until April 1965, staffed by British Railways staff until November 1964. Final closure came on 6 September 1965. The old goods shed marks the site of the former station. The section of old trackbed between Cardigan and Cilgerran is now a footway and cycle path through Teifi Marshes and Wildlife Park.

St Mary's Church is an Anglican church located in Cardigan, Ceredigion, Wales. In 1428, with the disappearance of Holy Trinity Church, St Mary's formally became the parish church of Cardigan, but it continued to serve as a priory church until the Reformation, being located close to Cardigan Priory. It is a Grade II* listed building.

Cardigan Priory (formally: The Priory Church of Our Lady of Cardigan; alternative: Cardigan Cell) was a Benedictine priory located in Cardigan, Ceredigion, mid-west Wales. Its church survives as a parish church, St. Mary's Church, Cardigan, whereas the priory itself was a separate building.

Cardigan and District Community Hospital (Welsh: Aberteifi a'r Cylch Ysbyty Cymunedol) was a community hospital in Cardigan, Ceredigion, Wales. It was managed by Hywel Dda University Health Board.

Ysgol Uwchradd Aberteifi, translated as Cardigan Secondary School is a bilingual secondary school in Cardigan, Ceredigion, Wales. It offers secondary education from ages 11 to 18, incorporating GCSEs and A-Levels in its sixth form. The motto is Egni a Lwydd (Energy Succeeds). The school is categorized as a 'Bilingual (Type C)' school by the Welsh Government, meaning that 50 - 79% of subjects, excluding Welsh and English, are taught through the medium of Welsh but are also taught through the medium of English. According to the latest Estyn report in 2022, 21.3% of pupils spoke Welsh at home.There have been several allegations of bullying against the headteacher, Mrs Nicola James with staff going on strike both in 2018 and 2019. Following an investigation, no evidence of bullying against staff was found.The school appeared on S4C's Hip neu Sgip?: Yn erbyn y cloc in 2011, as part of a garden makeover item which took place at the school in September 2010.The school is referenced in the 2020 fiction book 'A Deadly Education' by Naomi Novik, (p.114) as attended by the protagonist Galadriel Higgins.

Our Lady of Cardigan (Welsh: Mair o Aberteifi), also known as Our Lady of the Taper, the Catholic national shrine of Wales, is a statue of the Blessed Virgin Mary created by Sr Concordia Scott and located in a chapel in Cardigan, Ceredigion, Wales.

The Ceibwr Bay Fault is a WSW-ENE trending fault zone that cuts Ordovician rocks of the Ashgill Nantmel Mudstones Formation and the Caradoc Dinas Island Formation. The fault is exposed on the south side of Cardigan Bay in Wales and forms part of the Fishguard-Cardigan Fault Zone. It extends from the coast at Ceibwr Bay at its western end to the coast at Aberporth at its eastern end. The fault zone is thought to have been active as a normal fault throughout the deposition of the Ordovician sequence.