Pearl jewelry for bridal and wedding tradition, bridal pearl necklace set for wedding ceremony, pearl jewelry for graduation and wedding celebration
This objection, which at first glance appears to be a verythorough, we will reply, firstly, that the evidence speaking in favorsuch relationships are always more or less dubious. Wehave already had occasion to hint at some "idols" (to use a metaphorBacon), which the geologists, without knowing it, make a sacrifice, interpretingthe device is still little known areas. Guided by the classificationstrata existing in Europe, and assuming that groups of strata in other partslight must necessarily coincide with some of the groups of layers,known to us, geologists, naturally, too slow to recognizethe existence of a parallelism on insufficient evidence. Theyrarely ask ourselves the prior question: are there still considering themformation of the corresponding formations in Europe? For them, the question lies is: which of the European groups to classify them these formations? theyrepresent the most similarities? from which they differ least? Inevitablethe result of this method of research is a great negligence inconclusions. What comes to this negligence, we will not be difficult to showexamples. Where the layers are interrupted, as, for example, between Europe andAmerica, you can't have any evidence, based on the order inwhich the layers lie on one another, regardless of the mineralogicalsigns and organic residues. Everywhere where it is impossible to trace the beds incontinuous communication, mineralogical characteristics and organic residues servethe only way to determine the membership of the layers to one oranother system. With regard to the reliability of the mineralogical characteristics, wehave seen that they almost have no meaning, and none ofmodern geologists would not dare to assert that they can rely on.If the group of the old red Sandstone in the Midlands completely differentin lithology from the corresponding group in South Devon, itit is clear that the similarity in structure and composition may not be sufficientthe basis for equating the layers from another part of the world to which any ofEuropean systems.
Post a Comment