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of Aminas River, east of the Mancos;<19> and he also speaks of the ruins at the commencement of McElmo Canyon as being large communal buildings. We should judge from Mr. Jackson's report just given that these ruins were rather small clusters of houses of the same design as the ruins at Apache Springs. Near the Utah boundary line we notice the Hovenweep Creek joining the McElmo from the north. The mesa, narrowing to a point where the two canyons meet, is covered with ruins much like what we have described already. The Hovenweep is appropriately named, meaning "deserted valley." Illustration of Ruins in the Hovenweep Canyon.-------- Further west still is the Montezuma Valley. Mr. Jackson's party found the ruins so numerous as to excite surprise at the numbers this narrow valley must have supported. He says, "We camped at the intersection of a large canyon coming in from the west.... At this point the bottoms widen out to from two to three hundred yards in width, and are literally covered with ruins, evidently those of an extensive settlement or community, although at the present time water was so scarce (there not being a drop within a radius of six miles) that we were compelled to make a dry camp. The ruins consist evidently of great solid mounds of rock _debris,_ piled up in rectangular masses, covered with earth and a brush growth, bearing every indication of extreme age--just how old is about as impossible to tell as to say how old the rocks of this canyon are. This group is a mile in length, in the middle of the valley space, and upon both sides of the wash. Each separate building would cover a space, generally, of one hundred feet square; they are seldom subdivided into more than two or four apartments. Relics were abundant, broken pottery and arrow-points being especially plenty. At one place, where the wash held partially undermined the foundation of ore of the large buildings, it exposed a wall of regularly laid masonry, extending down six feet beneath the superincumbent rubbish to the old floor-level, covered with ashes and the remains of half-charred sticks of juniper." Lower down, the valley was noted for little projecting tongues of rock extending out into the canyon, sometimes connected with the main walls of the canyon by narrow ledges of rock, and in cases even this had disappeared, leaving detached masses of rock standing quite alone. "Within a distance of fifteen miles there are some sixteen o
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