perennial spring (Other Keyword)
1-4 (4 Records)
Recent research on the Garrett Allen site has discussed the excavation history, projectile points and chronology of the site (Eckles 2013), chipped stone raw materials and obsidian sourcing (Eckles and Guinard 2015), chipped stone projectile points (Eckles and Miller 2019), and research potential of the collection (Clauter 2013). Data on these topics have indicated support for the idea the site represents a series of special place gatherings over about 3,100 years of prehistoric occupation....
Chipped Stone Raw Materials from the Garrett Allen (Elk Mountain) Site, 48CR301 (2015)
In this article, chipped stone raw materials from the Garrett Allen site are discussed, with emphasis on the stone tools. As indicated by Eckles (2103), who discussed the history of investigations and chronology, this is one of several articles to be presented on various aspects of the site’s artifacts. One of the remarkable aspects of the site is the variety of chipped stone raw materials. There are varieties of flint, chert, agate, jasper, chalcedony, petrified wood, orthoquartzite,...
Faunal Remains from the Garrett Allen (Elk Mountain) Site (48CR301) (2020)
Excavations at the Garrett Allen (Elk Mountain) archaeological site recovered a large and diverse faunal assemblage. The purpose of this article is to summarize data on the faunal remains with emphasis on the unusual aspects of the assemblage. A brief introduction to the site excavations and chronology is presented first. More detailed information about previous investigations at the site is discussed in Eckles (2013).
Projectile Points from the Garrett Allen (Elk Mountain) Site, 48CR301 (2019)
The Garrett Allen (Elk Mountain) archaeological site is located in southeastern Carbon County, Wyoming at the northern end of the Medicine Bow Mountains and southern edge of the Hanna-Carbon Basin. It is within a homoclinal valley adjacent to the perennial Quealy Spring which forms an ephemeral drainage flowing north-northwest. The site is surrounded by Upper Cretaceous sedimentary rocks, primarily of the Pine Ridge Sandstone (Hayter 1983:5). Previously published articles on the site have...