From the Blue Ridge to the Coastal Plain: Field Excursions in the Southeastern United States 2012
DOI: 10.1130/2012.0029(02)
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Bluff to bluff: A field guide to floodplain geology and geomorphology of the Lower Congaree River Valley, South Carolina

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Cited by 5 publications
(7 citation statements)
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“…In late May in Congaree National Park, P. frontalis displays ardently across a forest of loblolly pines spreading along the convergence line between a bluff and the Congaree River floodplain (16). While the swarm stretches across hundreds of meters, most fireflies tend to coalesce into localized leks hovering above smaller parcels.…”
Section: Resultsmentioning
confidence: 99%
“…In late May in Congaree National Park, P. frontalis displays ardently across a forest of loblolly pines spreading along the convergence line between a bluff and the Congaree River floodplain (16). While the swarm stretches across hundreds of meters, most fireflies tend to coalesce into localized leks hovering above smaller parcels.…”
Section: Resultsmentioning
confidence: 99%
“…In late May in Congaree National Park, Photuris frontalis displays ardently across a forest of loblolly pines spreading along the convergence line between a bluff and the Congaree River floodplain [16]. While the swarm stretches across hundreds of meters, most fireflies tend to coalesce into localized leks hovering above smaller parcels.…”
Section: Resultsmentioning
confidence: 99%
“…Within the park, the USGS records water level at Cedar Creek (USGS Cedar Creek station, #02169672, Figure 1b). Water levels at this location are affected by both river inundation and runoff from upland source areas (Shelley et al., 2012; Xu et al., 2020). Two additional gauging stations outside of the study area provide water levels for the Santee River (USGS Santee River in Fort Motte, #02169810, rkm 48.4) and for the Wateree River (USGS Wateree River in Camden, #02148000, north of the study region, not shown Figure 1).…”
Section: Study Region and Hydrologic Conditionsmentioning
confidence: 99%
“…For reference, the along channel distance is reported with the prefix “rkm” for “river kilometer,” with rkm 0 at the upstream park boundary, increasing downstream. Railroad (rkm 38.3) and highway (rkm 42.6) berms are the major anthropogenic structures in the floodplain, consisting of embankment‐bridge systems, that likely affect floodplain circulation during high flows (Patterson et al., 1985; Sharitz & Allen, 2009; Shelley, 2007). The railroad embankment extends 3.7 km into the floodplain, after which the bridge is supported by 4.5 by 6.8 m piers, spaced ∼50 m apart that continues for 1.8 km (Figure 1b).…”
Section: Study Region and Hydrologic Conditionsmentioning
confidence: 99%