|
The cavern is located in the Fort Regent Granite which forms a prominent outcrop in the centre of St Helier. The scheme was required to reduce the risk
of flooding in St Helier and prevent the discharge of untreated sewage into the sea during periods of high flow. During high flows, waste water is stored in the 28,000 cubic metre cavern for later treatment and discharge.
Engineering Geology A comprehensive review of the geology, structure and geotechnical parameters using the site investigation data, published information and field
mapping was carried by out by SubTerra Engineering post tender.
The regional structure is dominated by an abundance of sub-vertical dykes between 1m and 10m thick, trending
ENE-WSW. Most dykes occupy minor faults or fissures and there is evidence of post dyke reactivation. No evidence of major faulting was found at the site, however minor faulting was indicated by zones
of no recovery in the three cavern boreholes, one of which was orientated enabling structural data to be correlated with the surface outcrops. |