scholarly journals Identification of American Shad Spawning Sites and Habitat Use in the Pee Dee River, North Carolina and South Carolina

2011 ◽  
Vol 31 (6) ◽  
pp. 1019-1033 ◽  
Author(s):  
Julianne E. Harris ◽  
Joseph E. Hightower
Author(s):  
Smoot Z.T. ◽  
A.D. Jayakaran ◽  
D.M. Park ◽  
D.R. Hitchcock

Hydraulic bankfull geometry or regional curves are a useful metric for evaluating stream stability and planning stream restoration projects. Streams and tributaries within the Middle Pee Dee River Basin (MPDRB) in South Carolina drain an agrarian and forested landscape characterized by water conveyance structures, such as active and historical ditches which support forestry and agriculture. While streams in the region are generally stable, pockets of this landscape are beginning to face increasing pressure from development with signs of stream instability apparent in several locations as evidenced by streams in and around the urbanizing areas around Darlington and Florence, SC. In order to provide a foundation for potential stream restoration projects in the area, 15 sites in the MPDRB were selected on the basis of catchment area, in categories of small (km2), small-medium (50-500 km2), medium (500-1000 km2), and large (>1000 km2). Bankfull geometries, channel substrate, flow and water temperature were measured at all the sites and a set of regional hydraulic geometry curves developed. The frequency of bankfull flows that occurred over the period of sampling were also estimated to document floodplain connectivity. Results suggest that bankfull dimensions in the MPDRB were well correlated with bankfull discharge and drainage area. The results showed that hydraulic geometry in the region were similar to those measured in a similar physiographic region in North Carolina. The study also shows that streams in the MPDRB experience bankfull exceeding flows much more frequently than streams in other parts of the country, but at a frequency that is comparable to streams in the coastal plains of North Carolina.


1959 ◽  
Vol 25 (1) ◽  
pp. 79-85 ◽  
Author(s):  
John Witthoft

AbstractThe long stratigraphic sequence of separate archaeological horizons at the mouth of the gorge of the Pee Dee River in North Carolina necessitates changing earlier reconstructions of Piedmont archaeology. The stratigraphically documented series of projectile points from this site makes it possible to separate in time the varied forms of points originally assigned to the Baden and Guilford foci. Moreover, this evidence contradicts the typological arrangements of points in terms of logical evolutionary development and suggests that Archaic sequences in other parts of the Appalachian region may have to be radically changed when stratigraphic data become available. Stratigraphy at the Duncan's Island site in Pennsylvania, though less precise than that at the Pee Dee site, indicates that the local typological reconstructions for parts of Pennsylvania are in need of revision. Basal levels at Duncan's Island produce quartzite tools of types scattered throughout central Pennsylvania and often considered to represent an extremely early Archaic industry. The concentration of quartzite tools at the DeTurk site, though not dated stratigraphically, provides typological justification for the idea that the quartzite industry may be a survival of an earlier forest-based proto-Archaic tradition.


Author(s):  
Melissa Griffin ◽  
Mark Malsick ◽  
Hope Mizzell ◽  
Leah Moore

For the third time in four years, record-breaking flooding occurred in South Carolina. Hurricane Florence, which made landfall near Wrightsville Beach, North Carolina, on September 14, 2018, moved slowly across South Carolina from September 14–17, 2018. Over those four days, heavy rain fell over portions of the Pee Dee Watershed and eastern North Carolina, with over 30 inches of rain measured by an observer in Swansboro, North Carolina. Most of the excessive rainfall was confined to the Pee Dee region, with reported totals of over 24 inches in Horry County, while closer to the Savannah River Valley observers measured less than an inch of rain. Unlike the more recent flooding events across the state, not as many rainfall records were set during this event. The amount of rainfall at various locations, and at different time intervals (1-day, 2-day, 3-day, and 4-day), had a statistical probability of occurrence of 0.1%, or 1 in 1,000 chance of happening in any given year, according to the National Oceanic and Atmospheric Administration (NOAA) Atlas 14 (Bonnin et al., 2004). The rainfall associated with Hurricane Florence produced a long duration and significant flood that impacted many of the same communities still recovering from the October 2015 floods and Hurricane Matthew in 2016. Many of the rivers and streams within the Pee Dee Watershed experienced major or extreme flooding, with six stream gauges reaching record peaks, some surpassing the records set in 2016. This report provides an overview of the antecedent conditions, a synoptic summary of the event, and documentation on the meteorological and hydrological impacts observed across the Palmetto State.


2006 ◽  
Vol 118 (5-6) ◽  
pp. 533-549 ◽  
Author(s):  
W. E. Baldwin ◽  
R. A. Morton ◽  
T. R. Putney ◽  
M. P. Katuna ◽  
M. S. Harris ◽  
...  

2013 ◽  
Vol 129 (3) ◽  
pp. 82-106 ◽  
Author(s):  
Bryn H. Tracy ◽  
Robert E. Jenkins ◽  
Wayne C. Starnes

Abstract North Carolina's river drainages continue to lose their faunal distinctiveness as nonnative fish species establish themselves and expand their distributions, resulting in biotic homogenization. One such example is the Pee Dee drainage on the Atlantic Slope. It is the most speciose drainage in North Carolina, inhabited by 113 species of which 34 are nonindigenous, many introduced from adjacent drainages. The history of fish investigations in the Pee Dee in North Carolina and Virginia is detailed herein. The fauna was first sampled by Cope in 1869 at two conjoined sites—Yadkin River and Gobble Creek, a small tributary at the Yadkin River site (Cope 1870). Cope described numerous new taxa from the drainage, and many subsequent researchers provided data that show additions of nonnative faunal elements. As a case study, indications are that Hypentelium roanokense, Roanoke Hog Sucker, Hypentelium nigricans, Northern Hog Sucker, and Moxostoma rupiscartes, Striped Jumprock, were cryptically introduced after the late 1950s. The Roanoke Hog Sucker, introduced as recently as the 2000s, is found only in three tributaries of the Ararat subsystem in North Carolina and Virginia. The Northern Hog Sucker has expanded its range very little, confined primarily to the North Fork Reddies and Ararat subsystems and a short segment of the mainstem Yadkin River in North Carolina. The Striped Jumprock is now in much of the upper Yadkin system, but not in Virginia, and at several sites in the South Yadkin subsystem. Natural dispersal of all three species is limited by dams and impoundments, but the dispersal by Striped Jumprock has probably been aided by multiple bait bucket introductions. Consequences of nonindigenous species introductions in the drainage are well known for some species but unknown for the Roanoke Hog Sucker, Northern Hog Sucker, and Striped Jumprock.


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