The two largest of the Red-rock cliff houses to which I shall refer were named Honanki or Bear-house and Palatki or Red-house. The former of these, as I learned from the names scribbled on its walls, had previously been visited by white men, but so far as I know it has never been mentioned in archeological literature. My attention was called to it by Mr Schürmann, at whose hospitable ranch I outfitted for my reconnoissance into the Red-rock country. The smaller ruin, Palatki, we discovered by chance during our visit, and while it is possible that some vaquero in search of a wild steer may have visited the neighborhood before us, there is every reason to believe that the ruin had escaped even the notice of these persons, and, like Honanki, was unknown to the archeologist. The two ruins, Honanki and Palatki, are not the only ones in the lone canyon where we encamped. Following the canyon a short distance from its entrance, there was found to open into it from the left a tributary, or so-called box canyon, the walls of which are very precipitous. Perched on ledges of the cliffs there are several rows of fortifications or walls of masonry extending for many yards. It was impossible for us to enter these works, even after we had clambered up the side of the precipice to their level, so inaccessible were they to our approach. These "forts" were probably for refuge, but they are ill adapted as points of observation on account of the configuration of the canyon. Their masonry, as examined at a distance with a field glass, resembles that of Palatki and Honanki. I was impressed by the close resemblance between the large cliff houses of the Red-rocks, with their overhanging roof of rock, and those of the San Juan and its tributaries in northern New Mexico. While it is recognized that cliff houses have been reported from Verde valley, I find them nowhere described, and our lack of information about them, so far as they are concerned, may have justified Nordenskiöld's belief that "the basin of the Colorado actually contains almost all the cliff dwellings of the United States." As the Gila flows into the Colorado near its mouth, the Red-rock ruins may in a sense be included in the Colorado basin, but there are many and beautiful cliff houses higher up near the sources of the Gila and its tributary, the Salt. In calling attention to the characteristic cliff dwellings of the Red-rocks I am making known a new region of ruins closely related to those of Canyon de Tségi, or Chelly, the San Juan and its tributaries. Although the cliff houses of Verde valley had been known for many years, and the ruins here described are of the same general character, anyone who examines Casa Montezuma, on Beaver creek, and compares it with Honanki, will note differences of an adaptive nature. The one feature common to Honanki and the "Cliff Palace" of Mancos canyon is the great overhanging roof of the cavern, which, in that form, we miss in Casa Montezuma (figure 246).[26]