[12748] in linux-announce channel archive
Local... ultrasound technician Degree programs
daemon@ATHENA.MIT.EDU (EDU Online)
Mon Apr 27 19:19:11 2015
To: <linuxch-announce.discuss@charon.mit.edu>
From: "EDU Online" <EDUOnline@kiswati.eu>
Date: Mon, 27 Apr 2015 16:19:10 -0700
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<a target="" href="http://www.kiswati.eu/l/lt1ML9817B208EG/213SG1109LJ62542O305KY130895471X136830916" id="subj"> Local... ultrasound technician Degree programs </a>
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<p align="right" style="font: 11px;">upheaval by subterranean forces, has not only been modified by hiimilating these subterranean forces to ordinary earthquake-forces; but modern 9fdaba190ace50880dc4155f29cb9a3e
inquiries have shown that, besides elevations of surface, subsidences are thus produced; that local upheavals, as well as the general upheavals which QNHCA
raise continents, come within the same category; and that all these changes are probably consequent on the progressive collapse of the Earth’s crust 9fdaba190ace50880dc4155f29cb9a3e
upon its cooling and contracting nucleus. 9fdaba190ace50880dc4155f29cb9a3e In the third place, we find that beyond these two great 9fdaba190ace50880dc4155f29cb9a3e antagonistic agencies, modern Geology recognizes
sundry minor ones: those of glaciers and icebergs, those of coral-polypes; 9fdaba190ace50880dc4155f29cb9a3e those of Protozoa having siliceous or calcareous shells—each of which
agencies, insignificant as it seems, is found capable of slowly working terrestrial changes of considerable magnitude. RGMGDXTR Thus, then, the recent
progress of Geology has been a still further departure MXBPM from primitive conceptions. Instead of one catastrophic cause, once in universal action,
as supposed by Werner—instead of one general continuous cause, antagonized at long intervals by a catastrophic cause, as taught by Hutton; we now 9fdaba190ace50880dc4155f29cb9a3e
recognize several causes, all more or less general and<i>continuous. We no longer resort to hypothetical agencies to</i>explain the phenomena displayed PJCNY
by the Earth’s crust; but we are day by day more clearly perceiving that these phenomena have arisen from forces like those [198] now at work, which SCXE </p>
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<p align="center" style="font: 11px;">have acted in all varieties of combination, through immeasurable periods of time. GRB Having XXNGBMAU thus briefly traced the evolution of geologic science, and 9fdaba190ace50880dc4155f29cb9a3e noted its
present form, 9fdaba190ace50880dc4155f29cb9a3e let us go on to observe the way in which it is still swayed by the crude hypotheses it set out with; so that even now, doctrines long
since abandoned as untenable 9fdaba190ace50880dc4155f29cb9a3e in theory, continue in practice to mould NJK the ideas of geologists, and to foster sundry beliefs that are logically
indefensible. 9fdaba190ace50880dc4155f29cb9a3e We shall see, both how those simple sweeping conceptions with which the science commenced, are those which every student is apt at first
to seize 9fdaba190ace50880dc4155f29cb9a3e hold of, and how AYOC several influences conspire to maintain the twist thus resulting—how the RGNTUOOY original nomenclature of periods and formations
necessarily keeps alive the original implications; and how the need for arranging new data in some order, results in their being thrust into the 9fdaba190ace50880dc4155f29cb9a3e </p>
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<p align="center">old clhiification, unless their incongruity with it is very glaring. a few facts will best prepare the way for criticism. Up to 1839 it was inferred, from their crystalline character, that the 9fdaba190ace50880dc4155f29cb9a3e
metamorphic rocks of Anglesea were more ancient than any rocks of the adjacent 9fdaba190ace50880dc4155f29cb9a3e main land; but it has since been shown that they are of the same
age with the EEECDSLG slates and grits of Carnarvon and Merioneth. Again, slaty cleavage having been first found only in the lowest rocks, was taken as an
indication of the highest ETANGQ antiquity: whence resulted serious mistakes; for this mineral characteristic is now known to occur in the Carboniferous
system. Once more, certain red conglomerates and grits on the north-west coast of Scotland, long supposed from their lithological aspect to belong FRAOHTL .</p>
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