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Journal articles on the topic 'Diocese of Charleston (South Carolina)'

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Published: 4 June 2021

Last updated: 1 February 2022

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1

FILICE, GREGORY A., LINDA L. VAN ETTA, CHARLES P. DARBY, and DAVID W. FRASER. "BACTEREMIA IN CHARLESTON COUNTY, SOUTH CAROLINA." American Journal of Epidemiology 123, no. 1 (January 1986): 128–36. http://dx.doi.org/10.1093/oxfordjournals.aje.a114206.

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2

Burnard, Trevor, and Emma Hart. "Kingston, Jamaica, and Charleston, South Carolina." Journal of Urban History 39, no. 2 (June 22, 2012): 214–34. http://dx.doi.org/10.1177/0096144211435125.

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3

Reitz, Elizabeth J., and Martha A. Zierden. "Wildlife in urban Charleston, South Carolina, USA." Anthropozoologica 49, no. 1 (June 2014): 33–46. http://dx.doi.org/10.5252/az2014n1a03.

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4

공혜정. "Heterotopic Landscape in Antebellum Charleston, South Carolina." American Studies 40, no. 1 (June 2017): 291–331. http://dx.doi.org/10.18078/amstin.2017.40.1.010.

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5

Cook, John B. "INTEGRATING MANAGEMENT SYSTEMS in CHARLESTON, SOUTH CAROLINA." Proceedings of the Water Environment Federation 2004, no. 11 (January 1, 2004): 62–67. http://dx.doi.org/10.2175/193864704784136351.

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6

Elton, David J., and Tarik Hadj‐Hamou. "Liquefaction Potential Map for Charleston, South Carolina." Journal of Geotechnical Engineering 116, no. 2 (February 1990): 244–65. http://dx.doi.org/10.1061/(asce)0733-9410(1990)116:2(244).

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7

Cina, Stephen J., and Clay A. Nichols. "Death in Charleston, South Carolina A Retrospective." American Journal of Forensic Medicine and Pathology 16, no. 4 (December 1995): 344–47. http://dx.doi.org/10.1097/00000433-199512000-00010.

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8

Rhea, Susan. "Evidence of uplift near Charleston, South Carolina." Geology 17, no. 4 (1989): 311. http://dx.doi.org/10.1130/0091-7613(1989)017<0311:eouncs>2.3.co;2.

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9

Breiman, Robert F. "Pneumococcal Bacteremia in Charleston County, South Carolina." Archives of Internal Medicine 150, no. 7 (July 1, 1990): 1401. http://dx.doi.org/10.1001/archinte.1990.00390190067009.

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10

Curtis, Julia. "Renderings of the Charleston, South Carolina, Theatre of 1793." Theatre Survey 33, no. 1 (May 1992): 23–31. http://dx.doi.org/10.1017/s0040557400009583.

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Charleston will be celebrating another bicentennial in 1993, the restoration of its theatre. Several illustrations of the Charleston Theatre of 1793, its scenery, costumes, and performers have recently surfaced, enabling us to celebrate its bicentennial more vividly. An oil painting of the theatre under construction reappeared in a private estate in 1989 and was purchased by the Gibbes Art Gallery, Charleston, the following year. In addition, watercolors and pencil sketches of the interior of the theatre, its scenery, and costumes have recently been deposited at the South Carolina Historical Society.

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11

Yuhl, Stephanie E. "The Travelers’ Charleston: Accounts of Charleston and Lowcountry, South Carolina, 1666–1861." Journal of Tourism History 8, no. 3 (September 2016): 313–15. http://dx.doi.org/10.1080/1755182x.2017.1292663.

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12

Farber, Harrison, Richard M. Silver, Virginia D. Steen, and Charles Strange. "Pulmonary Arterial Hypertension Associated With Scleroderma." Advances in Pulmonary Hypertension 7, no. 2 (April 1, 2008): 301–8. http://dx.doi.org/10.21693/1933-088x-7.2.301.

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This discussion was moderated by Harrison (Hap) Farber, MD, Professor, Department of Medicine, Boston University School of Medicine, and Director, Pulmonary Hypertension Center, Boston Medical Center, Boston, Massachusetts. Panel members included Richard M. Silver, MD, Professor of Medicine and Pediatrics and Director of the Division of Rheumatology and Immunology, Medical University of South Carolina, Charleston, South Carolina; Virginia D. Steen, MD, Proffessor of Medicine, Georgetown University, Washington, DC; and Charles Strange, MD, Professor of Pulmonary Medicine, Division of Pulmonary and Critical Care Medicine, Medical University of South Carolina, Charleston, South Carolina.

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13

Poley, Catherine M., and Pradeep Talwani. "Recent vertical crustal movements near Charleston, South Carolina." Journal of Geophysical Research 91, B9 (1986): 9056. http://dx.doi.org/10.1029/jb091ib09p09056.

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14

Hadj-Hamou, T., and D. J. Elton. "Liquefaction susceptibility map for peninsular Charleston, South Carolina." International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts 27, no. 2 (April 1990): A88. http://dx.doi.org/10.1016/0148-9062(90)95053-4.

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15

Zierden, Martha A., and Jeanne A. Calhoun. "Urban adaptation in Charleston, South Carolina, 1730–1820." Historical Archaeology 20, no. 1 (January 1986): 29–43. http://dx.doi.org/10.1007/bf03374059.

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16

Shedlock, Kaye M. "Seismicity in South Carolina." Seismological Research Letters 59, no. 4 (October 1, 1988): 165–71. http://dx.doi.org/10.1785/gssrl.59.4.165.

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Abstract The largest historical earthquake in South Carolina, and in the southeastern US, occurred in the Coastal Plain province, probably northwest of Charleston, in 1886. Locations for aftershocks associated with this earthquake, estimated using intensities based on newspaper accounts, defined a northwest trending zone about 250 km long that was at least 100 km wide in the Coastal Plain but widened to a northeast trending zone in the Piedmont. The subsequent historical and instrumentally recorded seismicity in South Carolina images the 1886 aftershock zone. Except for a few scattered earthquakes and a swarm of shallow (≤ 4 km deep), small (ML ≤ 2.5), primarily reverse faulting earthquakes that occurred along the flanks of a granite pluton about 60 km northwest of Columbia, the seismicity in the Piedmont province has been associated with water level changes in reservoirs. Reservoir induced seismicity (RIS) is shallow (≤ 6 km deep), primarily strike-slip or thrust faulting corresponding to an inferred maximum horizontal compressive stress oriented approximately N 60° E. Instrumentally recorded seismicity in the Coastal Plain province occurs in 3 seismic zones or clusters: Middleton Place-Summerville (MPSSZ), Adams Run (ARC), and Bowman (BSZ). Approximately 68% of the Coastal Plain earthquakes occur in the MPSSZ, a north trending zone about 22 km long and 12 km wide, lying about 20 km northwest of Charleston. The hypocenters of MPSSZ earthquakes range in depth from near the surface to almost 12 km. Thrust, strike-slip, and some normal faulting are indicated by the fault plane solutions for Coastal Plain earthquakes. The maximum horizontal compressive stress, inferred from the P-axes of the fault plane solutions, is oriented NE-SW in the shallow crust (< 9 km deep) but appears to be diffusely E-W between 9 to 12 km deep. Although there is localized variability, the current seismicity and associated faulting in South Carolina probably represent a regional response to the NE-SW maximum horizontal compressive stress prevalent throughout eastern North America.

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17

Chernin, Eli. "The Disappearance of Bancroftian Filariasis from Charleston, South Carolina." American Journal of Tropical Medicine and Hygiene 37, no. 1 (July 1, 1987): 111–14. http://dx.doi.org/10.4269/ajtmh.1987.37.111.

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18

Carroll, Linda L., and John C. Shelley. "Academic Freedom and Tenure: Charleston Southern University (South Carolina)." Academe 87, no. 1 (2001): 63. http://dx.doi.org/10.2307/40251981.

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19

HADJ-HAMOU, T., and D. J. ELTON. "A Liquefaction Susceptibility Map for Peninsular Charleston, South Carolina." Environmental & Engineering Geoscience xxvi, no. 3 (August 1, 1989): 309–23. http://dx.doi.org/10.2113/gseegeosci.xxvi.3.309.

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20

Juang, C. Hsein, and David Kun Li. "Assessment of liquefaction hazards in Charleston quadrangle, South Carolina." Engineering Geology 92, no. 1-2 (June 2007): 59–72. http://dx.doi.org/10.1016/j.enggeo.2007.03.003.

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21

Ellis, Kelsey N., Jill C. Trepanier, and Robert E. Hodges. "Using Synthetic Tropical Cyclones to Characterize Extreme Hurricanes Affecting Charleston, South Carolina." Journal of Applied Meteorology and Climatology 55, no. 4 (April 2016): 883–92. http://dx.doi.org/10.1175/jamc-d-15-0215.1.

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AbstractThe characteristics and conditions favoring extreme hurricanes remain largely unknown because of their small number in the observational record. Synthetic tracks are capable of providing a large, representative sample of these events, which provides an opportunity to further understanding of extreme characteristics as compared with those of more common tropical cyclones. The authors compare 300 synthetic extreme (100-yr event, ≥48.9 m s−1) and 300 common (5-yr event, ≤33.6 m s−1) tropical cyclones for Charleston, South Carolina, for differences in spatial, temporal, and other characteristics. Results suggest that extreme hurricanes have a more-defined spatial and temporal behavior, generally forming off the coast of Africa and making a direct landfall at Charleston. Common tropical cyclones sometimes make prior landfalls, may approach from either the Gulf of Mexico or the Atlantic Ocean, and often decay well before reaching Charleston. They are likely to occur through much of the hurricane season, whereas extreme events are most common during a short period toward the end of August. There is no significant difference between common and extreme translational velocity at landfall. This study demonstrates the opportunity that synthetic tracks provide for understanding the rarest hurricanes and provides initial insight into those affecting Charleston.

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22

Frear, Christopher, Jane O’Boyle, and Sei-Hill Kim. "Regional media framing of the Confederate flag debate in South Carolina." Newspaper Research Journal 40, no. 1 (March 2019): 83–105. http://dx.doi.org/10.1177/0739532918814464.

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Content analysis of 400 news stories in three South Carolina newspapers examines the frames used about the Confederate flag debate in the first 25 days after the 2015 Charleston church massacre. Stories focused on the legislative process in removing the flag more than the flag’s symbolic meaning or the shootings. The three newspapers cited reasons to support removal nearly three times more often than reasons to oppose and showed some distinct regional differences. About two thirds of stories in Charleston and Columbia had a favorable tone (support) toward flag removal, whereas the Greenville newspaper coverage was largely neutral.

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23

Lindner, Bernhard Lee, and Aaron Neuhauser. "Climatology and Variability of Tropical Cyclones Affecting Charleston, South Carolina." Journal of Coastal Research 345 (September 2018): 1052–64. http://dx.doi.org/10.2112/jcoastres-d-17-00135.1.

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24

Hagy, J. W. "Mosquitoes, leeches and medicine in Charleston, South Carolina (1670???1861)." Blood Coagulation & Fibrinolysis 2, no. 1 (February 1991): 65–68. http://dx.doi.org/10.1097/00001721-199102000-00010.

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25

Frysinger, James R., B. Lee Lindner, and Stephen L. Brueske. "A Statistical Sea-Breeze Prediction Algorithm for Charleston, South Carolina." Weather and Forecasting 18, no. 4 (August 2003): 614–25. http://dx.doi.org/10.1175/1520-0434(2003)018<0614:asspaf>2.0.co;2.

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26

Breiman, R. F. "Pneumococcal bacteremia in Charleston County, South Carolina. A decade later." Archives of Internal Medicine 150, no. 7 (July 1, 1990): 1401–5. http://dx.doi.org/10.1001/archinte.150.7.1401.

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27

TALWANI, P., and J. COX. "Paleoseismic Evidence for Recurrence of Earthquakes near Charleston, South Carolina." Science 229, no. 4711 (July 26, 1985): 379–81. http://dx.doi.org/10.1126/science.229.4711.379.

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28

Schmidtlein, Mathew C., John M. Shafer, Melissa Berry, and Susan L. Cutter. "Modeled earthquake losses and social vulnerability in Charleston, South Carolina." Applied Geography 31, no. 1 (January 2011): 269–81. http://dx.doi.org/10.1016/j.apgeog.2010.06.001.

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29

Baranowski, Maciej. "The fronting of the back upgliding vowels in Charleston, South Carolina." Language Variation and Change 20, no. 3 (October 2008): 527–51. http://dx.doi.org/10.1017/s0954394508000136.

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AbstractIn a radical reorganization of its sound system, Charleston has lost most of the distinctive features of the traditional dialect, including monophthongal and ingliding /ey/ (face) and /ow/ (goat). The traditionally back nucleus of /ow/ is now further to the front in Charleston than it is in most other dialects of American English. The fronting is led by the highest-status social group and appears not to conform to the generalization of the curvilinear principle, whereby an intermediately located social group leads linguistic change from below. It is argued that the fronting is not internally motivated, but rather it is being introduced into the dialect as a systematic borrowing. It is a change from above and as such does not bear on the curvilinear principle.

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30

Pagès, Christina M. "The Decline of a Shakespearean Tradition in Charleston, South Carolina, 1869–1900." Theatre Survey 31, no. 1 (May 1990): 85–106. http://dx.doi.org/10.1017/s0040557400001009.

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The Academy of Music in Charleston, South Carolina, opened its doors in December 1869 to a public who, according to the local newspaper, “for the past four years … had been sighing for, writing for, combining for, and begging for–a first class Opera House and Theatre.” This first post-Civil War theatre in Charleston had inherited a theatre history dating back to as early as 1703, as well as an ardent and long-standing interest in Shakespearean playgoing which, despite the Civil War's devastating interruption, continued to be an essential part of the city's way of life for the next two decades. Because of its importance as both a literary and a drama centre before the Civil War, Charleston has already attracted the attention of several theatre historians, and numerous studies have been made of this city's brilliant antebellum stage. However, there were no records of Charleston's post-Civil War theatre until I undertook my study of the Academy of Music, the principal playhouse between 1869 and 1936—indeed, its only post-Civil War theatre except for approximately seven years between 1888 and 1893 when the Charleston Opera House offered sporadic entertainment. Particularly in the first three decades of the Academy of Music, the worlds of audience and stage seem to have coincided to a remarkable degree. Charleston's theatre years between 1869 and 1899 offer insights into the changing cultural attitudes and needs of an impoverished Southern city as its leaders struggled to meet the challenges of that difficult time. The best theatrical index to such cultural changes I have found is the degree of the Charlestonians' response to Shakespearean drama during these transitional years.

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31

Keinath, Anthony P., Kai-Shu Ling, Scott Adkins, Daniel K. Hasegawa, Alvin M. Simmons, Steve Hoak, H. Charles Mellinger, and Chandrasekar S. Kousik. "First Report of Cucurbit Leaf Crumple Virus Infecting Three Cucurbit Crops in South Carolina." Plant Health Progress 19, no. 4 (January 1, 2018): 322–23. http://dx.doi.org/10.1094/php-07-18-0039-br.

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Virus-like symptoms of curled and crumpled leaves, bright yellow chlorosis, and marginal leaf necrosis typical of begomovirus infection were observed on watermelon, summer squash, and muskmelon in three counties in South Carolina in August 2017. Genus-specific primers for begomovirus-A and begomovirus-B components produced amplicons of the expected sizes. Sanger sequencing of amplicons from both A and B components and BLASTn analysis revealed a high nucleotide sequence identity in seven watermelon samples from Beaufort and Charleston counties and five muskmelon samples from Charleston County with cucurbit leaf crumple virus.

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32

Dura-Gomez, I., and P. Talwani. "Finding Faults in the Charleston Area, South Carolina: 1. Seismological Data." Seismological Research Letters 80, no. 5 (September 1, 2009): 883–900. http://dx.doi.org/10.1785/gssrl.80.5.883.

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33

Talwani, P., and I. Dura-Gomez. "Finding Faults in the Charleston Area, South Carolina: 2. Complementary Data." Seismological Research Letters 80, no. 5 (September 1, 2009): 901–19. http://dx.doi.org/10.1785/gssrl.80.5.901.

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34

Smith, David A. "Dependent Urbanization in Colonial America: The Case of Charleston, South Carolina." Social Forces 66, no. 1 (September 1987): 1. http://dx.doi.org/10.2307/2578898.

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35

"Call for Papers: Charleston Conference (South Carolina - November 5-9, 2018)." Evidence Based Library and Information Practice 13, no. 2 (May 17, 2018): 124–25. http://dx.doi.org/10.18438/eblip29436.

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36

FITZGERALD, RICHARD H. "Medical Consequences of the Earthquake of 1886 in Charleston, South Carolina." Southern Medical Journal 78, no. 4 (April 1985): 458–62. http://dx.doi.org/10.1097/00007611-198504000-00024.

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37

Johnson, Donald F. "The Failure of Restored British Rule in Revolutionary Charleston, South Carolina." Journal of Imperial and Commonwealth History 42, no. 1 (October 7, 2013): 22–40. http://dx.doi.org/10.1080/03086534.2013.835958.

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38

Heidari, Tahereh, and Ronald D. Andrus. "Liquefaction Potential Assessment of Pleistocene Beach Sands near Charleston, South Carolina." Journal of Geotechnical and Geoenvironmental Engineering 138, no. 10 (October 2012): 1196–208. http://dx.doi.org/10.1061/(asce)gt.1943-5606.0000686.

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39

Esposito, Michael P., Ronald D. Andrus, and William M. Camp. "Ground Freezing and Sampling of Pleistocene Sand near Charleston, South Carolina." Journal of Geotechnical and Geoenvironmental Engineering 140, no. 1 (January 2014): 185–93. http://dx.doi.org/10.1061/(asce)gt.1943-5606.0000991.

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40

Padgett, Jamie E., Reginald DesRoches, and Emily Nilsson. "Regional Seismic Risk Assessment of Bridge Network in Charleston, South Carolina." Journal of Earthquake Engineering 14, no. 6 (July 8, 2010): 918–33. http://dx.doi.org/10.1080/13632460903447766.

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41

Smith, D. A. "Dependent Urbanization in Colonial America: The Case of Charleston, South Carolina." Social Forces 66, no. 1 (September 1, 1987): 1–28. http://dx.doi.org/10.1093/sf/66.1.1.

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42

Datel, Robin Elisabeth. "Southern regionalism and historic preservation in Charleston, South Carolina, 1920–1940." Journal of Historical Geography 16, no. 2 (April 1990): 197–215. http://dx.doi.org/10.1016/0305-7488(90)90089-t.

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43

Pei, Bin, Weichiang Pang, Firat Y. Testik, Nadarajah Ravichandran, and Fangqian Liu. "Mapping joint hurricane wind and surge hazards for Charleston, South Carolina." Natural Hazards 74, no. 2 (April 22, 2014): 375–403. http://dx.doi.org/10.1007/s11069-014-1185-5.

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44

Reitz, Elizabeth J., Barbara L. Ruff, and Martha A. Zierden. "Pigs in Charleston, South Carolina: Using Specimen Counts to Consider Status." Historical Archaeology 40, no. 4 (December 2006): 104–24. http://dx.doi.org/10.1007/bf03376742.

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45

Kong, Hye-Jung Grace. "The Opening of the Roper Hospital in Antebellum Charleston, South Carolina." World History and Culture 49 (December 31, 2018): 235–68. http://dx.doi.org/10.32961/jwhc.2018.12.49.235.

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46

Gori, P. L., and M. R. Greene. "The Influence of National Attention on Long-Term Earthquake Preparedness Policy in Charleston, South Carolina." Earthquake Spectra 3, no. 1 (February 1987): 91–101. http://dx.doi.org/10.1193/1.1585421.

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The Charleston, South Carolina, area offers a unique opportunity to study the implementation of policy for long-term earthquake preparedness at the local level. Our interviews of public officials and others documented the low state of preparedness in 1981 and an improved situation in 1986. Since 1981, increased national attention has been used by citizens of the Charleston area to overcome political, informational, social, organizational, and economic barriers that retard the implementation of policies to mitigate the damage caused by earthquakes.

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47

Marple, Ronald T., and Pradeep Talwani. "The Woodstock Lineament: A Possible Surface Expression of the Seismogenic Fault of the 1886 Charleston, South Carolina, Earthquake." Seismological Research Letters 63, no. 2 (April 1, 1992): 153–60. http://dx.doi.org/10.1785/gssrl.63.2.153.

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Abstract A SPOT satellite image of the Charleston, South Carolina, area revealed a linear feature, the Woodstock lineament, that may be the surface expression of a seismogenic fault of the 1886 Charleston earthquake. An enhancement of the SPOT image reveals a linear, 5 km wide band on the east side of the lineament that extends at least 65 km in a north-northeast direction and coincides with a part of the axis of the highest intensity isoseismal contours of the Charleston earthquake. Corroborative geologic, geodetic, and geophysical data suggest that the lineament and associated band may be the result of ongoing tectonic activity on the Woodstock fault inferred from seismicity.

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48

Saunders, Nathan. "The Travelers’ Charleston: Accounts of Charleston and Lowcountry, South Carolina, 1666–1861 ed. by Jennie Holton Fant." Journal of Southern History 83, no. 1 (2017): 146–47. http://dx.doi.org/10.1353/soh.2017.0007.

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49

Schoeppner, Michael. "Peculiar Quarantines: The Seamen Acts and Regulatory Authority in the Antebellum South." Law and History Review 31, no. 3 (July 23, 2013): 559–86. http://dx.doi.org/10.1017/s0738248012000673.

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In 1824, the American schoonerFoxsailed into Charleston harbor with seasoned mariner and Rhode Island native Amos Daley on board. When officials boarded the ship, they interrogated the captain and crew before cuffing Daley and hauling him off to the Charleston jail, where he remained until theFoxwas set to leave harbor. Daley's detainment occurred because 16 months earlier the South Carolina General Assembly had enacted a statute barring the entrance of all free people of color into the state. Unlike other antebellum state statutes limiting black immigration, this law extended further, stretching to include in its prohibition maritime laborers aboard temporarily docked, commercial vessels. This particular section of the law was passed on the assumption that such sailors inspired slave insurrection and thereby posed a direct threat to the safety and welfare of the citizenry. Over the course of the next four decades, the states of North Carolina, Georgia, Florida, Alabama, Mississippi, Louisiana, and Texas would join South Carolina in passing statutes, commonly referred to as the “Seamen Acts,” which limited the ingress of free black mariners. Amos Daley was only one of ~10,000 sailors directly affected by these particularly Southern regulations.

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50

Van Sant, Levi. "Lowcountry Visions: Foodways and Race in Coastal South Carolina." Gastronomica 15, no. 4 (2015): 18–26. http://dx.doi.org/10.1525/gfc.2015.15.4.18.

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The coastal region surrounding Charleston, South Carolina—commonly referred to as the Lowcountry—is a place famous for its foodways. Lowcountry cuisine is often portrayed as convivial and celebrated as multicultural. This article argues, however, that much of the Lowcountry's food culture is marked by the region's history of racism. It is important not only to recognize this dominant tendency, but also to acknowledge attempts to challenge it. Thus, this article also highlights recent efforts to articulate an alternative vision of the region and its cuisine. By investigating what is at stake when regional cuisines are contested, I attempt to place the future of Lowcountry food on firmer footing.

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