Proposed sketch of Academical Department. State University of Michigan

Photographer''s stamp: Henry Rocher, 88 North Clark Street , Chicago. On verso: E.S. Jenison, Archit [architect] - Rooms 13, 14 & 15. 128 La Salle St. Chicago

University of Michigan Men's Basketball Team, 1963

Back Row:asst. coach Tom Jorgenson, Richard Hildreth, John Oosterbaan, George Pomey, George Thomas Cole, Bill Buntin, Douglas Greenwald, John Harris, Lawrence Tregoning, Paul Schuldt, asst. coach James Skala

Front Row: Edward Petrick, Robert Cantrell, Horace Thomas Ludwig, coach Dave Strack, Charles Adams, Hiram Jackson, Douglas Herner

Instrumentation at CERC's Field Research Facility, Duck, North Carolina /

"October 1980."

Long-term changes in beach fauna at Duck, North Carolina /

Long-term changes in the beach fauna at Duck, North Carolina, were investigated. Twenty-one stations located on three transects on the oceanside and twenty-four stations located on three transects on the sound side were sampled seasonally from November 1980 to July 1981. The data collected in this study were compared to a previous study conducted in 1976 (Matta, 1977) to investigate the potential effects of the construction of the CERC Field Research Facility pier on the adjacent beaches. No effects on the benthic fauna were found. Changes observed in the benthic macrofauna on the ocean beaches were well within the range attributable to the natural variation of an open coast system. The ocean beach macrofauna was observed to form a single community migrating on an off the beach with the seasons. On the sound beaches, changes were detected in the benthic macrofauna; however, these were attributed to a salinity increase during the 1981 sampling year. (Author).

Beach changes at Holden Beach, North Carolina, 1970-74 /

Beach profile lines at 21 near-evenly spaced intervals along Holden Beach, North Carolina, between Lockwoods Folly and Shallotte Inlets, were measured from November 1970 to December 1974. These have been analyzed to determine the spatial and temporal variabilities on long-term, seasonal, and short-term scales. Profile lines near the inlets showed the greatest variability in mean sea level (MSL) position, above MSL volume, foreshore slope, and profile envelope. This variability near Lockwoods Folly Inlet was partly enhanced by artificial nourishment at profile line 2. Temporary, low-cost shore protection devices (e.g., sandbag groins) were constructed near that inlet during part of the study. No other modifications or activities that affected beach processes were known to occur during the study period. The central part of Holden Beach was studied separately because of the high variability of the inlet sections at either end of the island. Foreshore slopes along this reach increased from an average of 1:30 at the east end to 1:17 at the west. A seasonal change in above MSL volume indicates loss of sand during autumn and winter, and gain during spring and summer. Changes in MSL shoreline intercept and above MSL volume were highly variable during the study.

NAEP 1996 mathematics state report for North Carolina /

"NCES 97-974 NC"--P. [4] of cover.

Graptolites of North America /

Mode of access: Internet.