Moray coast and Inverness

The Moray coast regional model

The Kessock Bridge over the Moray Firth at Inverness (© Patricia & Angus Macdonald / Aerographica / SNH)

The low-lying southern coastal hinterland of the Moray Firth is one of the most populous parts of the Highlands. It is blessed with fertile soils, principally derived from sandy glacial sediments laid down by glaciers that flowed from the Great Glen and surrounding uplands.

Interaction between these glaciers has left behind a complex and often thick sequence of highly permeable sediments which obscure much of the underlying Devonian sandstone bedrock between Elgin and Inverness.

3D modelling

Since 2007 the BGS has been developing 3D models to capture and visualise the complexity of both the superficial and bedrock geology. These models will enable planning authorities and regulators to address land-use issues associated with rapidly increasing urban development, particularly around Inverness.

Potential for river flooding

One of the most significant issues is the potential for river flooding. This prompted the construction of the first bespoke linked field survey and 3D geological framework model in Scotland, for the ground around the town of Forres.

Targeted field investigations by a team of geologists, hydrogeologists and engineering geologists enabled a complex 3D geological model to be produced.

This work has been used to investigate the shallow groundwater component of flooding within the Lower Findhorn catchment. The collaborative research, which allowed grouping of the superficial deposits in terms of their volume and permeability, enabled construction of a detailed shallow groundwater model. This built upon the results of commissioned site investigations, as well as an evaluation of new and pre-existing surface and subsurface data.

The results of these studies have influenced the planning and design of flood alleviation measures within the flood-prone ground.

From Forres to Inverness

Since 2011, many of the modelling concepts developed for the Forres modelling studies have started to be applied to Inverness. Here, the complex geology is rapidly being concealed by man-made deposits and modified by excavations associated with the expanding city.

The results of co-funded geophysical surveys, undertaken by BGS marine geologists in the adjacent shallow waters of the Firth, are now being included in the developing model for Inverness and its suburbs. This will provide a holistic 3D baseline for the future development of the whole onshore-offshore area.

Contact

Contact Katie Whitbread or Sarah Arkley for further information