DISTRIBUTION OF SOILS. 211 



'that this variation is confined between the limits of a southeast and a soutlnvest course, 

 with a few interesting exceptions which will be given in the sequel. The numl)er of re- 

 corded observations which go to establish the general fact of a sontherly distribution of llie 

 soil and boulders, is extremely great, and is gathered from the whole extent of country 

 between the Atlantic ocean and the base of the Rocky mountains ; and no instance has 

 happened in wlucli a boulder lias travelled northwardly, or lieen foimd in a situation with 

 its parent rock towards the south. The two great facts, then, wliich geologists have been 

 able to establish on this question as general, are, first, the transportation of rocks and soils ; 

 and, secondly, the southerly direction in which they have been uniformly carried. Ac- 

 cording to this general announcement, a soil occupying any given situation, if out of place, 

 lies south of the rock -which gave it origin ; and the pebbles which are large enough to be 

 readily distinguished, indicate the origin of the soil, or the rock to which it belongs. If 

 we llnd many limestone pebbles, or if lumps of earth are found to effervesce with vinegar 

 or other acids, it shows that the soil is formed of tlie debris of a calcareous rock. 



A soil which contains many pebbles, or rolled stones like paving stones, is frequently 

 called drift., a term which is convenient, as well as short. All soils which have been 

 transported, may be termed drift ; hut where cobblestones make up a large proportion of 

 a formation, the evidence of its having been drifted is obvious, and hence the term is 

 usually confined to beds exhiljiting these sure marks of transportation. The term drift, 

 however, would not be properly applied to a pebbly beach. 



Scored surfaces. The second phenomenon above mentioned, which is believed to be 

 somehow connected with the transportation of soils, is an effect observed upon hard sur- 

 faces over which the drifting soil has passed. The upper surface of most hard rocks, of 

 whatever age they may be, is scratched, grooved, or sometimes polished. These effects 

 differ at different places, according to the nature of the materials which have passed over 

 the surface. If these materials were coarse and heavy, deep scorings seem to have been 

 the only result ; if of a finer texture, the surface is slightly scratched, or it may be polished, 

 an effect which can not be produced by coarse substances. The markings vary in degree, 

 from the slightest scratch, to a groove four or five inches in depth. The direction of these 

 scratches or grooves is southerly ; and it is a cm-ious fact that they are not made in vary- 

 ing directions, and without order, but always correspond to the direction which, from other 

 considerations, we find the soil to have taken in its transportation : in other words, the 

 grooves run in a southerly direction, and are parallel in sets ; and, as a general rule, their 

 directions are confined within the limits of the southeast and southwest points of the com- 

 pass. From this correspondence between the direction of tlie grooves, and that of the 

 transportation of the boulders and soil, we are legitimately authorised to associate the two 

 phenomena as cotemporaneous effects of one common cause, whatever that cause may 

 have been. This interpretation seems to be borne out by the fact, that in uncovering a 

 rock of its soil, which we usually denominate drift, the bottom boulders are frequently 

 found each occupying the groove it had made, like a plough left in its furrow ; and like 



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