Geology
The geological strata present below the Gateshead area consists of the Upper Carboniferous Middle Coal Measures. The Coal measures consist of interbedded layers of sandstone, siltstone, mudstone and shale deposited approximately 300 million years ago. Thin layers, or seams of coal are present within the strata, many of which are sufficient thickness to have been mined in the past.
Above the Coal Measures at surface level more recent superficial or ‘drift’ deposits are present. These deposits consist of clays, sands and gravels deposited during / after the latest Ice Age.
In total seven seams of coal sub crop below the drift deposits in the northern part of the study area. These seams are named as the High Main, Metal, Top and Bottom Five Quarter, Top and Bottom Main and the Maudlin / Bensham.
The Coal Measures strata below the site dip in a south-easterly direction which results in the coal seams becoming progressively deeper below ground level from northwest to southeast across the study area.
The coal seams have been extensively worked below the study area in the past. A mining report obtained from the Coal Authority indicates the presence of recorded workings in nine seams of coal at depths ranging from 50 to 220m below ground level. It is also likely that additional unrecorded workings will be present below some / all of the study area.
The coal seams were worked from a series of shafts located throughout the study area. In total 41 shafts are recorded by the Coal Authority within the boundaries of the study area, and it is likely that additional unrecorded shafts could also be present in the area.