RESEARCH NEWS.The following bulletins seem timely given the exciting and new archaeological discoveries at Beamish and Crawford, as reported recently in the newspapers.
CORK and CAEN together?
Recent research by the editor has shown that the medieval canals in the city seem to be closely allied to canals of similar date in Caen in Normandy. This equivalence between the early infrastructure of Cork and Caen also applies in terms function and design. Thus, it appears that the earliest canals in Cork may be an example of Norman influence in Ireland prior to the later Anglo-Norman occupation of the town in the thirteenth century.
SUBSURFACE CORK. Further analysis of the subsurface geology of the City, using the evidence of archaeological excavations and historical engineering boreholes, has provided detailed information concerning the course of the South Channel prior to its diversion at the end of the eleventh century.
Anthony Beese is trading as a consulting geologist with Carraigex GeoServices, who provide services in geoarchaeology and engineering geology. He has also written diverse articles on geology, landscape archaeology, the historical environment and natural history.
Here is an introduction to the story of Cork’s landscapes. Glimpses of the past. Amazing changes have occurred in the Lee valley since the last glaciation ended 11,700 years ago. Ice, river and estuary. Cork before Cork.
And then Cork. Archaeologists have discovered that, about nine hundered years ago, Hiberno-Norse people established the beginnings of the city by undertaking a major programme of land-claim, which consisted of filling the estuary with locally sourced silt. They began this task by diverting the South Channel and forming a new settlement near South Gate Bridge, as it is now.
The video shows the South Channel as it roars over South Gate Weir; the powerful flow was observed on February 25th, 2014 and includes water released by the ESB at the Inniscarra Dam after the prolonged wet weather of last winter (Donal Lehane, personal communication). The estimated discharge flow of about 70 m3/s could be considered to be representative of a typical river flood, of which there were probably many that swept down the South Channel during the medieval period; scouring mudbanks and undermining any timber structures that were in its path.
The image shows the residual flow in the North Channel at St Patrick’s Bridge on November 21st, 2009, one day after the infamous flood that caused extensive damage to the city. During the flood, a peak discharge flow of more than 800 m3/s is estimated. If such an extreme event had occurred in the eleventh or twelfth centuries, it seems unlikely that the early settlement of timber houses would have survived. Perhaps, earlier attempts to develop the wetland at Cork had already been postponed?