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its beginning, the importance of these final paragraphs slowly diminished, and the information they gave was gradually transferred to the title-page. Complete title-pages bearing the date and name of the publishers are found in most books printed after 1520, and the final paragraph, if retained at all, was gradually reduced to a bare statement of the name of the printer. From the use of the word in the sense of a "finishing stroke," such a final paragraph as has been described is called by bibliographers a "colophon" (Gr. [Greek: kolophon]), but at what period this name for it was first used has not been ascertained. It is quite possibly not earlier than the 18th century. (For origin see COLOPHON [city].) (A. W. PO.) COLORADO, a state of the American union, situated between 41 deg. and 37 deg. N. lat. and 102 deg. and 109 deg. W. long., bounded N. by Wyoming and Nebraska, E. by Nebraska and Kansas, S. by Oklahoma and New Mexico, and W. by Utah. Its area is 103,948 sq. m. (of which 290 are water surface). It is the seventh largest state of the Union. _Physiography._--Colorado embraces in its area a great variety of plains, mountains and plateaus. It lies at the junction of the Great Plains--which in their upward slant to the westward attain an average elevation of about 4000 ft. along the east boundary of the state--with the Rocky Mountains, to the west of which is a portion of the Colorado Plateau. These are the three physiographic provinces of the state (see also UNITED STATES, section _Geology_, ad fin., for details of structure). The last-named includes a number of lofty plateaus--the Roan or Book, Uncompahgre, &c., which form the eastern continuation of the high plateaus of Utah--and covers the western quarter of the state. Its eastern third consists of rich, unbroken plains. On their west edge lies an abrupt, massive, and strangely uniform chain of mountains, known in the neighbourhood of Colorado Springs as the Rampart Range, and in the extreme north as the Front Range, and often denominated as a whole by the latter name. The upturning of the rocks of the Great Plains at the foot of the Front Range develops an interesting type of topography, the harder layers weathering into grotesquely curious forms, as seen in the famous Garden of the Gods at the foot of Pike's Peak. Behind this barrier the whole country is elevated 2000 ft. or so above the level of the plains region. In its lowest portions just behi
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