A HISTORY OF LANCASHIRE 



Gannistcr and Upper Foot seams, which takes place along an irregular north-west and south-east 

 line a little to the north of the Rossendale anticlinal. Although up to the point of union the 

 individual thicknesses of the two mines are but two feet six inches and eight inches respectively, 

 yet at their junction the united seams swell out to a thickness of nearly eight feet, and the average 

 over a great area is four feet. 



The special features of the union of these two seams were dealt with by J. Aitken,^ and his 

 explanation is probably the correct one, viz., that a part of the Gannister area was one of subsidence, 

 the submersion going on until a sufficient depth beneath water was obtained to allow of the 

 deposition of sufficient detritus to form the rock mass overlying that mine and separating it from 

 the thin coal above. He goes on to say in his paper : ' It would further appear that the surface 

 over which the four-foot coal was then in process of formation remained stationary and undisturbed, 

 and that the operations of nature were not in any way interrupted.' 



This view is supported by the fact that the coal of the Four-Feet Mine is considerably thicker 

 than the aggregate of the two mines while separate, the growth of vegetation over the area being 

 evidently continuous during the period in which the submerged portion was being silted up. 

 When the latter had taken place, the coal forest grew out over the shallows, giving rise to the thin 

 ' Upper Foot ' coal, after which the whole area occupied by the Four-Feet Mine and the Upper 

 Foot coals was submerged, and a uniform deposit of mud took place. 



The Upper Foot Mine is worthy of note, not on account of its thickness, which is almost 

 invariably 1 2 inches, but because of the occurrence of great quantities of ' bullions ' or coal balls 

 within it, each bullion ball containing portions of coal plants in which the structure has been so 

 well preserved as to allow of the closest microscopical investigation. From these bullions were 

 obtained the stems, etc., of coal plants described by Binney, Carruthers, Williamson, Hick, Scott, 

 and others. 



Upon the coal are found numerous flattened limestone nodules called ' bawn-pots,' each with 

 a thin crust of iron pyrites and containing well-preserved examples of GoniatiteSy Orthoceras, Pterino- 

 pecten [Aviculopecten\ and Posidoniella. 



The coals are all bituminous and caking. Iron pyrites occurs as nodules in some of the coals, 

 and also as a thin film upon joint planes, in some cases (the upper seams) so abundantly as to 

 seriously injure the usefulness of the coal. The demand for these coals is entirely local, and their 

 use as fuel is restricted to engine boilers and the open fireplaces of the people. 



The fireclays under the Gannister seams have been worked at times in conjunction with the 

 coal, as they make excellent firebricks, drain pipes, etc. Works of this description can be seen at 

 Colne, Townley near Burnley, Sharneyford, north-east of Bacup, Littleborough, and other places. 



MIDDLE COAL MEASURES 



We have already alluded to the broken-up character of these measures, whereby small isolated 

 portions have been dignified with the name of coalfields. The most southerly patch is the 

 Manchester coalfield, which is about four miles long from north-north-west to south-south-east 

 and a mile and a half broad across its greatest diameter. This coalfield, whilst relatively insignificant 

 and now little used, is of considerable geological importance in that the upper coal measures are 

 well developed. The Middle Coal Measures are deep seated and scarcely touched, owing to the 

 great thickening of the barren measures below the Four-Feet coal of Bradford and Clayton. 



This latter seam was formerly supposed to be the equivalent of the Worsley four-feet seam 

 which marks the upper limit of the Middle Coal Measures in other parts of Lancashire, but more 

 recent researches seem to render this correlation doubtful. Attempts to reach the thick coals of the 

 Middle Coal Measures have hitherto failed, the unproductive beds lying below the Bradford Four-Feet 

 having been penetrated by Mr. Livsey to a depth greater than should have been necessary had the 

 Crumbourke and Rams Mines occupied the same position relatively to the Bradford Four-Feet as thev 

 do to the Worsley Four-Feet. ^ 



Professor Hull is of opinion that at least 6i6 yards of barren measures will have to be 

 penetrated below the Bradford and Clayton Four-Feet seam before a workable coal is reached 



In this present state of our knowledge it is best to regard the presence of the Middle Measures 

 as certain, and the upper limit as undetermined. ^toauics 



elsewhere ^^^" ^"^^ Measures which have been worked in this coalfield will be dealt with 



SOUTH LANCASHIRE COALFIELD 



This coalfield which is extremely irregular and much cut up by faults, can be best dealt with 

 by a division into districts. uc<iit wiui 



' Trans. Manchesier Geol. Soc, v. 185. 

 14 



