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Updated: May 28, 2025


J. W. Powell, geologist in charge, have furnished a large amount of additional information concerning the ruins on the San Juan and its tributaries, the Cliff Houses on the Mancos River and elsewhere, and the Moki Pueblos. Valuable as this information is to us, it falls short of a full exposition of these several subjects.

Indeed, so great has been the erosion that many of the caves have been almost obliterated, and are now not deep enough to give shelter to a bird or bat. U.S. Geol. Walled fronts, the author states, were observed frequently on the Rio Mancos, where there are many well-preserved specimens.

In the eighties Mancos was forty miles from the nearest railway, but news of the reckless extravagances of its visiting miners and cowboys tempted Fells Brothers' "Greatest Aggregation on Earth of Ring Artists and Monsters" to visit it.

Thus it was barely high noon of the third day when the thirty Cross Cañonites reached their destination. Deep down in a mighty gorge, nestled beside the stream that gave its name alike to cañon and to town, Mancos stewed contentedly in a temperature that would try the strength and temper of any unaccustomed to the climate of southwestern Colorado.

Am. Geog. In recent years several publications have appeared which, while not bearing directly on the De Chelly ruins, are of great interest, as they treat of analogous remains the cliff ruins of the Mancos canyon and the Mesa Verde. These ruins were discovered in 1874 by W.

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