The Lowland Hundred (band)

, also known as or ( en, The Lowland Hundred), is a legendary ancient sunken kingdom said to have occupied a tract of fertile land lying between Ramsey Island and Bardsey Island in what is now Cardigan Bay to the west of Wales. It has been described as a "Welsh Atlantis" and has featured in folklore, literature, and song.

The legend

Cantre'r Gwaelod was an area of land which, according to legend, was located in an area west of present-day Wales which is now under the waters of Cardigan Bay. Accounts variously suggest the tract of land extended from Bardsey Island to Cardigan or as far south as Ramsey Island. Legends of the land suggest that it may have extended 20 miles west of the present coast.

Rachel Bromwich questions this identification, saying that "There is no certainty, however, that in twelfth century tradition Maes Gwyddneu did represent the submerged land in Cardigan Bay." She also links Gwyddno Garanhir with the Hen Ogledd, not Wales.

There are several versions of the myth. The earliest known form of the legend is usually said to appear in the '' Black Book of Carmarthen'', in which the land is referred to as ( en, the Plain of Gwyddno). In this version, the land was lost to floods when a well-maiden named Mererid neglected her duties and allowed the well to overflow.

The popular version known today is thought to have been formed from the 17th century onwards. Cantre'r Gwaelod is described as a low-lying land fortified against the sea by a dyke, Sarn Badrig (" Saint Patrick's causeway"), with a series of sluice gates that were opened at low tide to drain the land.

Cantre'r Gwaelod's capital was , seat of the ruler Gwyddno Garanhir. Two princes of the realm held charge over the dyke. One of these princes, called Seithenyn, is described in one version as a notorious drunkard and carouser, and it was through his negligence that the sea swept through the open floodgates, ruining the land.

The church bells of Cantre'r Gwaelod are said to ring out in times of danger.

Relationship to myth of Llys Helig

Rachel Bromwich discusses a similar tale, that of the submergence of the kingdom of Helig ap Glanawg in the Conwy estuary. As with Cantre'r Gwaelod, there are tales of remains being seen of the sunken kingdom ( Llys Helig). Bromwich believes that the two stories influenced each other, and that "The widespread parallels to this inundation theme would suggest that the two stories are in fact one in origin, and were localized separately in Cardiganshire and in the Conway estuary, around two traditional figures of the sixth century. She also notes that J.O Halliwell in his 1859 text ''An Ancient Survey of Pen Maen Mawr'' gives Helig the title "Lord of Cantre'r Gwaelod". In the book ''New Directions In Celtic Studies'' Antone Minard wrote that "The Welsh legends of Cantre'r Gwaelod and Llys Helig (Helig's Court) contain the same details of audible bells beneath the waves and ruins which are visible at the equinoctial tides, which are the anchors of credulity in the story".

Physical evidence

There is no reliable physical evidence of the substantial community that according to legend lies under the sea, although there are several reports of remains being sighted.

In 1770, Welsh antiquarian scholar William Owen Pughe reported seeing sunken human habitations about four miles (6 km) off the Ceredigion coast, between the rivers Ystwyth and Teifi.

In the 1846 edition of ''The Topographical Dictionary of Wales'', Samuel Lewis described a feature of stone walls and causeways beneath the shallow waters of Cardigan Bay:

Lewis takes the view that maps by the cartographer Ptolemy marked the coastline of Cardigan Bay in the same location as it appears in modern times, suggesting that the flood occurred before the second century AD.

The "causeways" described by Lewis can be seen today at beaches around Cardigan Bay. Known as , these ridges stretch several miles into the sea at right angles to the coast, and are located between each of the four river mouths in the north of Cardigan Bay. Modern geologists surmise that these formations of clay, gravel and rocks are moraines formed by the action of melting glaciers at the end of the last ice age. In a 2006 episode of the BBC
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