This is the power to discriminate
accurately between the several classes of color,--the local, the
reflected, and the prismatic. It will be found on reference to most
landscapes, especially those of the English schools, that it is the
understanding, already informed on the subject, which accepts as
reflected the continual attempts to render this kind of color: they are
regarded as indicative. But the eye, which should have been satisfied
first, recognizes nothing more than local coloring. Near objects, under
broad, open daylight, yield us their local coloring,--as the surfaces
of stones, the trunks of trees, and the many tints of soil and
vegetation,--yet even here all is modified by reflections. We remember
a cliff at L'Ariccia, which, gray in morning light, became, as evening
approached, a marvellous beryl green, upon which some large poppies cast
wafts of purest scarlet. Farther away, both local and reflected color
lose their power. The rays no longer convey information of surfaces as
separate existences. Nature gathers up into masses, and these masses
tide back to the foreground colors far removed in character from the
near. Vast combinations of rays and atmospheric influences have wrought
this change. As we have said, noon gives us the earth clean and itself;
but, as the sun declines, flushes of color pass along the ground. Their
character we have already described. The particles which fill the
atmosphere just above the surface of the earth become illuminated and
visible in radiant masses.
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