29 March 2021• Blog Posts
19 March 2021• Tool kit
The coastlines of Wales and Ireland form an extensive stretch of landscape, and coastal zone assessments provide a rapid, though detailed, method of gathering information on the historic environment, on the geology and geomorphology of the coast and on erosion at a given point in time.
Since the 1990s Coastal Zone Assessments have been undertaken in Wales, Scotland and England which follow a broadly similar methodology of:
Information gathered through coastal zone assessments provide an incredibly valuable baseline dataset on the stability of the coast, the nature and extent of archaeology in the coastal zone, the threats and rates of erosion to that archaeology along with recommendations for the appropriate management of it. One outcome of these assessments has been initiatives such as Arfordir in Wales, SCHARP (Scotland’s Coastal heritage at Risk Project) in Scotland and CITiZAN (the Coastal and Intertidal Zone Archaeological Network) in England which work with individuals and communities to provide additional data and longer term monitoring of the archaeology in the coastal zone. SCHARP and CITiZAN use an App which allows volunteers to gather and submit information, and a similar App is being developed by CHERISH for Ireland and Wales.
In Wales, we’ve used CHERISH Lidar gathered on 6 islands –Skerries, Puffin, Bardsey, Tudwals and Grassholm as our principal baseline dataset, creating new archaeological maps that are then verified on the ground. During island visits we’re also walking the coastline to record geology and geomorphology, and assess erosion status.
4 March 2021• Irish Project Areas
The CHERISH site Ferriter’s Castle and Promontory Fort is located on the Ballyferriter Headland, Dingle peninsula in county Kerry. Doon Point (Dún an Fheirtéaraigh) is a long, narrow promontory extending slightly over five hundred metres from north east to south west. This prehistoric fort is one of 95 coastal promontory forts in County Kerry, 42 of which are located on the Dingle peninsula.
This headland sits directly to the north of the Mesolithic- Neolithic transition period site at Ferriter’s Cove. Along the length of the promontory, narrow inlets of the sea are present in two locations due to softer sediments being carved out from the harder lava beds in these areas. These inlets divide the promontory into two distinct areas. These necks have been anthropogenically utilised and adapted in the construction of the Promontory Fort with a series of banks and ditches, forming an outer and inner set of defences. There are a number of hut sites and archaeological features visible within the boundaries of the fort. In the western section of the fort, there are a number of hut sites being heavily impacted by erosion. In the 15th or 16th century, later reuse of the fort occurred when the Anglo-Norman Ferriter family constructed a castle on the inner bank of the outer defences. This tower house was originally a 4-5 story rectangular tower, occupied by the Ferriter Family until the 17th century.
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