Proc. 7317 Title 3--The President cally aggregated into larger communities and dispersed into smaller com- munity units. Specifically, during Pueblo I (about 700-900 A.D.) the occu- pation and site density in the monument area increased. Dwellings tended to be small, with three or four rooms. Then, during Pueblo II (about 900- 1150 A.D.), settlements were diminished and highly dispersed. Late in Pueblo II and in early Pueblo III, around 1150 A.D., the size and number of settlements again increased and residential clustering began. Later pueb- los were larger multi-storied masonry dwellings with forty to fifty rooms. For the remainder of Pueblo III (1150-1300 A.D.), major aggregation oc- curred in the monument, typically at large sites at the heads of canyons. One of these sites includes remains of about 420 rooms, 90 kivas, a great kiva, and a plaza, covering more than ten acres in all. These villages were wrapped around the upper reaches of canyons and spread down onto talus slopes, enclosed year-round springs and reservoirs, and included low, de- fensive walls. The changes in architecture and site planning reflected a shift from independent households to a more communal lifestyle. Farming during the Puebloan period was affected by population growth and changing climate and precipitation patterns. As the population grew, the Ancestral Puebloans expanded into increasingly marginal areas. Natural resources were compromised and poor soil and growing conditions made survival increasingly difficult. When dry conditions persisted, Pueblo com- munities moved to the south, southwest, and southeast, where descendants of these Ancestral Puebloan peoples live today. Soon after the Ancestral Puebloans left the monument area, the nomadic Ute and Navajo took advantage of the natural diversity found in the vari- able topography by moving to lower areas, including the monument's mesas and canyons, during the cooler seasons. A small number of forked stick hogans, brush shelters, and wickiups are the most obvious remnants of this period of occupation. The natural resources and spectacular land forms of the monument help explain why past and present cultures have chosen to live in the area. The geology of the monument evokes the very essence of the American South- west. Structurally part of the Paradox Basin, from a distance the landscape looks deceptively benign. From the McElmo Dome in the southern part of the monument, the land slopes gently to the north, giving no indication of its true character. Once inside the area, however, the geology becomes more rugged and dissected. Rising sharply to the north of McElmo Creek, the McElmo Dome itself is buttressed by sheer sandstone cliffs, with mesa tops rimmed by caprock, and deeply incised canyons. The monument is home to a wide variety of wildlife species, including unique herpetological resources. Crucial habitat for the Mesa Verde nightsnake, long-nosed leopard lizard, and twin-spotted spiny lizard can be found within the monument in the area north of Yellow Jacket Canyon. Peregrine falcons have been observed in the area, as have golden eagles, American kestrels, red-tailed hawks, and northern harriers. Game birds like Gambel's quail and mourning dove are found throughout the monument both in dry, upland habitats, and in lush riparian habitat along the canyon bottoms. Section 2 of the Act of June 8, 1906 (34 Stat. 225, 16 U.S.C. 431), author- izes the President, in his discretion, to declare by public proclamation his- toric landmarks, historic and prehistoric structures, and other obiects of 94
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