1 62 HISTORICAL PALEONTOLOGY. 



tation ; but, before reviewing these, a few words must be said 

 as to the origin and mode of formation of coal. 



The coal - beds, as before mentioned, occur interstratified 

 with shales, sandstones, and sometimes limestones ; and there 

 may, within the limits of a single coal-field, be as many as 80 

 or 100 of such beds, placed one above the other at different 

 levels, and varying in thickness from a few inches up to 20 or 

 30 feet. As a general rule, each bed of coal rests upon a bed 

 of shale or clay, which is termed the "under-clay," and in 

 which are found numerous roots of plants ; whilst the strata 

 immediately on the top of the coal may be shaly or sandy, 

 but in either case are generally charged with the leaves and 

 stems of plants, and often have upright trunks passing vertically 

 through them. When we add to this that the coal itself is, 

 chemically, nearly wholly composed of carbon, and that its 

 microscopic structure shows it to be composed almost entirely 

 of fragments of stems, leaves, bark, seeds, and vegetable debris 

 derived from land-plants, we are readily enabled to understand 

 how the coal was formed.. The ^^ under -clay ^^ immediately 

 beneath the coal-bed represents an old land -surface — some- 

 times, perhaps, the bottom of a swamp or marsh, covered 

 with a luxuriant vegetation ; • the coal bed itself represents the 

 slow accumulation, through long periods, of the leaves, seeds, 

 fruits, stems, and fallen trunks of this vegetation, now hardened 

 and compressed into a fraction of its original bulk by the pres- 

 sure of the superincumbent rocks ; and the strata of sand or 

 shale above the coal-bed — the so-called "roof" of the coal — 

 represent sediments quietly deposited as the land, after a long 

 period of repose, commenced to sink beneath the sea. On 

 this view, the rank and long-continued vegetation which gave 

 rise to each coal-bed was ultimately terminated by a slow 

 depression of the surface on which the plants grew. The 

 land-surface then became covered by the water, and aqueous 

 sediments were accumulated to a greater or less thickness upon 

 the dense mass of decaying vegetation below, enveloping any 

 trunks of trees which might still be in an erect position, and 

 preserving between their layers the leaves and branches of 

 plants brought down from the neighbouring land by streams, 

 or blown into the water by the wind. Finally, there set in a 

 slow movement of elevation, — the old land again reappeared 

 above the water; a new and equally luxuriant vegetation 

 flourished upon the new land-surface ; and another coal-bed 

 was accumulated, to be preser^-ed ultimately in a similar 

 fashion. Some few beds of coal may have been formed by 

 drifted vegetable matter brought down into the ocean by rivers, 



