Due to political pressures, prior to the 1990s little was known about the nature of human foraging adaptations in the deserts, grasslands, and mountains of north western China during the last glacial period. Even less was known about the transition to agriculture that followed. Now open to foreign visitation, there is now an increasing understanding of the foraging strategies which led both to the development of millet agriculture and to the utilization of the extreme environments of the Tibetan Plateau. This text explores the transition from the foraging societies of the Late Paleolithic to...
Due to political pressures, prior to the 1990s little was known about the nature of human foraging adaptations in the deserts, grasslands, and mountai...
Camels Back Cave is in an isolated limestone ridge on the southern edge of the Great Salt Lake Desert. Recent archaeological investigations there have exposed a series of stratified deposits spanning the entire Holocene era (10,000 BP-present), deposits that show intermittent human occupations dating back through the past 7,600 years. Most human visits to the cave were brief--many likely representing overnight stays--and visitors did not dig pits or move sediment. As a result, fieldworkers were able...
University of Utah Anthropological Papers No. 125
Anthropology and Archaeology
Camels Back Cave is in an isolated limestone ridge on th...
Where did the first Americans come from and when did they get here? That basic question of American archaeology, long thought to have been solved, is re-emerging as a critical issue as the number of well-excavated sites dating to pre-Clovis times increases. It now seems possible that small populations of human foragers entered the Americas prior to the creation of the continental glacial barrier. While the archaeological and paleoecological aspects of a post-glacial entry have been well studied, there is little work available on the possibility of a pre-glacial entry. "Entering...
Where did the first Americans come from and when did they get here? That basic question of American archaeology, long thought to have been solved, ...
About 12,000 years ago, a major river ran from the Sevier Basin to the Great Salt Lake, feeding a wetland delta system and creating riparian habitat along its length. But after three thousand years the river dried up and the surrounding lands became more like what we see today. Because the Old River Bed Delta experienced less environmental and human disturbance than other areas, many of the Paleoarchaic sites found there have remained relatively intact a rarefind in the Great Basin. This book presents a comprehensive synthesis of a decade of investigations conducted by research teams...
About 12,000 years ago, a major river ran from the Sevier Basin to the Great Salt Lake, feeding a wetland delta system and creating riparian habita...