August 23, 1918. THE COLLIERY GUARDIAN 387 were published in the years 1878-1910 by the North of England Institute of Engineers, and that accounts of a number of borings in Yorkshire have been recently published by a committee of the Midland Institute of Mining, Civil and Mechanical Engineers. These publications relate to Northumberland, Durham, and (with one or two exceptions) to that part of the Great North Midland Coalfield which lies within the southern half of the county of York. They are of high value as far as they go, but they cover a limited part of the country, and are non-critical compilations of borers’ or sinkers’ records. The identification of coal- seams and the classification of strata under forma- tions are rarely attempted. Fossils, which are proving of great value in determining horizons in coal measures as well as in secondary strata, are ignored. While, therefore, the fact of those records having been published indicates a demand for the preservation of such information, it does not show that the demand has been inadequately met. (3) Underground explorations, which often take the form of trial-tunnels driven for long distances under unproved ground, are indicated as drifts or levels on the colliery plans, but there is no machinery for the preservation of the results obtained further than that they may be given by courtesy to the Geological Survey, if any of the officers happen to be engaged in the part of the country where the exploration is made. Unless developments of the new area follow, the results of these costly explorations are apt to be- come mere traditions, and though much information has been collected by the Geological Survey, it is not exhaustive, and, for the reason stated, does not cover all parts of the country. Visible Coalfields. (I) Proved New Coalfields and Extensions. (2> Probable New Coalfields and Extensions. Concealed Areas devoid of Coal Measures Areas occupied by older formations. Areas concealed by newer formation^ under which (3) Possible New Coalfields and Extensions may exist. ; •' •°b