The Selby Coalfield seismic surveys.
When the Selby Coalfield was conceived as a mining project in the 1970s one of the first things on the minds of the mining engineers was to prove the actual coal reserves available. They had to somehow ensure that the Selby Coalfield was worth the huge taxpayers investment needed to bring the project to fruition and have the coal actually coming out of the ground at Gascoigne Wood Drift Mine.
The No1 borehole at Cawood was drilled in late 1972. The Cementation Exploration Limited team, under the instruction of Ron Goosens who was a National Coal Board North Yorkshire Area geologist, found the Barnsley Seam to be over 3m thick and of an extremely good grade of coal when the test borings were completed. With the initial findings a strategic team was set up to manage the Selby project under the charge of Bill Forrest who was the deputy director of North Yorkshire Area N.C.B. One of the first job was to carry out a program of 84 exploratory boreholes to prove the size and quality of the seams and in particular the Barnsley Seam in the Selby area.
Drilling proved the geology in a small and specific section, but due to the scale of the undertaking of the enormous new coalfield a very thorough and technically challenging system of underground seismic surveys were required and the data analysed before the mines were planned and developed. The geologist and mining engineers had to survey the 100 square miles of the new coalfield for any geological issues and problems likely to interfere with the planning, designing, any equipment to be used and possible production losses caused by geological faults and intrusions.
The seismic surveying program undertaken in the Selby Coalfield was the biggest ever undertaken in the UK mining industry.
Seismic surveying is carried out by detonating a small charge of approximately 500g of dynamite just below the surface of the area to be surveyed. A system of cables and sensors called geophones are laid out in the surveying area in incremental distances or in grids set at pre-determined angles. When the detonation takes place directional seismic (acoustic) shock waves are generated which emanate through the strata being tested. These waves are measured against time to assess the depth, types and density of the strata encountered when the sound reflects back to the initial source. From this data the types of rock, coal and geological intrusions can be assessed by the geologists. This process is known as geophysical data acquisition.

From the above image you can see the number of two dimensional surveys carried out in the Selby Coalfield. Each red line is a seismic survey and could be kilometres in length. The surveys were carried out from 1973 onwards throughout the 70s and 80s.

The Selby Coalfield workings
Underground, in seam, seismic surveying also took place in the 1990s to prove future areas of the mines to be worked. Stillingfleet Mine carried out successful 3D surveys for the same reason in the late 1990s. On the link, at the top of this page, the entire seismic survey data is available to view.


































