The Macon Trading Post, an Historical Foundling

1939 ◽  
Vol 4 (4) ◽  
pp. 328-333 ◽  
Author(s):  
A. R. Kelly

Explorations on the Ocmulgee River, near Macon, Georgia, carried out over a period of four years under the sponsorship of the Smithsonian Institution and the National Park Service, and under the auspices of the successive relief agencies of CWA, FERA, WPA, and CCC, have uncovered many remarkable finds and discoveries, many of which will be permanently restored or exhibited in the development of Ocmulgee National Monument, established by Act of Congress in 1934.

Author(s):  
Kari A. Prassack ◽  
Laura C. Walkup

AbstractA canid dentary is described from the Pliocene Glenns Ferry Formation at Hagerman Fossil Beds National Monument, south-central Idaho, USA. The specimen possesses traits in alliance with and measurements falling within or exceeding those of Canis lepophagus. The dentary, along with a tarsal IV (cuboid) and an exploded canine come from the base of the fossiliferous Sahara complex within the monument. Improved geochronologic control provided by new tephrochronologic mapping by the U.S. Geological Survey-National Park Service Hagerman Paleontology, Environments, and Tephrochronology Project supports an interpolated age of approximately 3.9 Ma, placing it in the early Blancan North American Land Mammal Age. It is conservatively referred to herein as Canis aff. C. lepophagus with the caveat that it is an early and robust example of that species. A smaller canid, initially assigned to Canis lepophagus and then to Canis ferox, is also known from Hagerman. Most specimens of Canis ferox, including the holotype, were recently reassigned to Eucyon ferox, but specimens from the Hagerman and Rexroad faunas were left as Canis sp. and possibly attributed to C. lepophagus. We agree that these smaller canids belong in Canis and not Eucyon but reject placing them within C. lepophagus; we refer to them here as Hagerman-Rexroad Canis. This study confirms the presence of two approximately coyote-sized canids at Hagerman and adds to the growing list of carnivorans now known from these fossil beds.


2018 ◽  
Vol 40 (3) ◽  
pp. 211-231
Author(s):  
Priscilla Hancock Cooper

The Birmingham Civil Rights Institute marks its twenty-fifth year as the focal point for the city’s civil rights district. Inspired by the vision of Mayor David Vann, it became a reality under the leadership of the Dr. Richard Arrington, the city’s first African American mayor. A team of committed community volunteers led the institute through thirteen years of development in spite of corporate skepticism and citizen resistance. BCRI evolved as a model for staff development, community engagement and leadership and is now a key partner in the Birmingham Civil Rights National Monument, a unit of the National Park Service established in 2017.


Author(s):  
University of Wyoming National Park Service Research Center

This section contains a summary of research activities within the National Park Service areas cooperating with the U.W.-N.P.S. Research Center in 1986, including Bighorn Canyon National Recreation Area, Canyonlands National Park, Capitol Reef National Park, Custer Battlefield National Monument, Dinosaur National Monument, Fort Laramie National Historic Site, Glacier National Park, Glen Canyon National Recreation Area, Grand Teton National Park, Jewel Cave National Monument, Knife River Indian Villages National Historic Site, Theodore Roosevelt National Park, Wind Cave National Park, Yellowstone National Park and Zion National Park.


Author(s):  
University of Wyoming National Park Service Research Center

This section contains a summary of Research Activities within the National Park Service Areas cooperating with the U.W.-N.P.S. Research Center in 1984, inclucing Badlands National Monument, Devils Tower National Monument, Fort Laramie National Historic Site, Fossil Butte National Monument, Glacier National Park, Grand Teton National Park, Wind Cave National Park and Yellowstone National Park.


2008 ◽  
Vol 82 (3) ◽  
pp. 638-642 ◽  
Author(s):  
Dennis R. Ruez ◽  
Philip A. Gensler

The cooling during the Pliocene that preceded major continental glaciation in North America is recorded by thick fluvial and lacustrine sequences at Hagerman Fossil Beds National Monument (HAFO) in southcentral Idaho (McDonald et al., 1996). Fossiliferous beds at HAFO occur within the nearly 200 m of exposed Glenns Ferry Formation west of the Snake River. This formation extends from southwestern Idaho into easternmost Oregon (Malde and Powers, 1962). The Glenns Ferry Formation within HAFO contains hundreds of localities that are within the Blancan North American Land Mammal Age. Collection of specimens from these localities since the late 1920s has resulted in large repositories of fossils currently housed, in part, at the United States National Museum, the University of Michigan Museum of Paleontology (UMMP), and the Idaho Museum of Natural History (IMNH); additionally, smaller collections were accumulated by other museums (McDonald et al., 1996). Today the paleontological resources of HAFO are stewarded by the National Park Service. In spite of the extensive previous collections, significant new discoveries are still being made at HAFO.


2019 ◽  
Vol 100 (2) ◽  
pp. 217-222
Author(s):  
Alan W. Black ◽  
John A. Knox ◽  
Jared A. Rackley ◽  
Nicholas S. Grondin

AbstractWe examine the trajectories of four historical markers displaced during an enhanced Fujita scale 2 (EF2) tornado at the Fort Pulaski National Monument located on Cockspur Island, east of Savannah in southeast Georgia. The careful work of National Park Service employees in cataloguing the origin and landing points of the debris allows for an unusually accurate analysis of tornado debris trajectories for heavy objects. These markers, weighing around 68 kg (150 lb) each, traveled intact for distances of up to 220 m (750 ft). One of the historical markers was fractured into at least three pieces, the larger of which traveled 300 m (1,000 ft). Understanding the travel for these relatively heavy items is important, as they are similar in weight to household appliances that could commonly be part of a tornado debris field.


1949 ◽  
Vol 15 (1) ◽  
pp. 53-55 ◽  
Author(s):  
Robert L. Stephenson

During August and September, 1948, the writer made an archaeological survey of the Lavon Reservoir area in Collin County, Texas. This was a project of the River Basin Surveys program of archaeological salvage, undertaken by the Smithsonian Institution, with the cooperation of the Corps of Engineers and the National Park Service. This reservoir is being built on the East Fork of the Trinity River near Wylie, Texas and approximately 25 miles northeast of Dallas.Twenty-five sites were located in or near the proposed reservoir area during the course of this survey. Nineteen of these appear to be small, temporary campsites, some producing a few potsherds; others are apparently non-pottery sites. However, six of the sites appear to be permanent village locations occupied by relatively large groups of pottery-using people over a long period of time. The material from these sites is in the process of laboratory analysis at the present time and a statement of the cultural affiliations involved cannot yet be made.


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