By Sarah M. Nelson
A bright account of the prehistory and background of Denver as published in its archaeological list, this booklet invitations us to visualize Denver because it as soon as used to be. round 12,000 BC, teams of leather-clad Paleoindians undergone the juncture of the South Platte River and Cherry Creek, following the herds of vast or buffalo they hunted. within the Archaic interval, humans rested less than the color of timber alongside the riverbanks, with baskets jam-packed with plums as they waited for rabbits to be stuck of their within reach snares.In the early Ceramic interval, a bunch of mourners embellished with yellow pigment on their faces and beads of eagle bone Cherry Creek to the South Platte to wait a funeral at a neighbouring village. And in 1858, the realm was once populated by way of the crude cottonwood log shacks with dust flooring and glassless home windows, the houses of Denver's first population. for no less than 10,000 years, better Denver has been a suite of numerous lifeways and survival concepts, a crossroads of interplay, and a locus of cultural coexistence. atmosphere the scene with precise descriptions of the traditional surroundings, summaries of prehistoric websites, and archaeologists' wisdom of Denver's early population, Nelson and her colleagues convey the region's background to lifestyles. From prehistory to the current, this can be a compelling narrative of Denver's cultural background that may fascinate lay readers, beginner archaeologists, expert archaeologists, and educational historians alike.
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Extra info for Denver: An Archaeological History
It is named for a northwest/southeast trending ridge of the Dakota Sandstone that is itself a distinctive feature, being part of the Colorado Front Range uplift that has remained resistant to weathering (Fig. 4). The tilted sandstone outcrops of the hogback form the eastern boundary of the valley, which has an elevation at the bottom of 5,600 to 5,900 feet. Similar formations occur north and south of the Dakota Hogback. Green Mountain and North and South Table Mountains form large mesa-like features within the Hogback subregion.
Both obsidian sourcing and obsidian hydration studies rely on the collection of samples from a variety of contexts. The ability to assign such information to lithic materials provides data concerning the cultural affiliation of its users, the antiquity of the artifact’s use, and functional use patterns, and allows inferences regarding social and economic interactions between prehistoric populations on regional and interregional scales. Other attempts to directly date lithic materials include techniques such as cation ratio dating, which measures the accretion of desert varnish on the surface of materials that have been left lying on the surface of archaeological sites since the time they were deposited.
When struck, obsidian makes a conchoidal fracture, named for its resemblance to a conch shell. The fracture is smooth and can occur in any direction. Obsidian thus breaks in a way that is easier to control and predict than most other rocks, which may break irregularly in undesired directions. Furthermore, the edges of obsidian flakes are extremely sharp. Identifying the precise sources of obsidian has given archaeologists an additional tool for dating sites and artifact assemblages, and also for characterizing cultural interaction and relationships by tracing prehistoric obsidian trade.