RECONNAISSANCE OF BEDROCK GEOLOGY BY SUB-BOTTOM PROFILER,BAY OF FUNDYSWIFT DJP; LYALL AK.1968; GEOL. SOC. AMER., BULL.; USA; 1968(5), VOL. 79, NUM. 0005, P. 639 A 646Miscellaneous

EROSIONAL SAND COLUMNS IN DUNE SANDS, CAPE SABLE ISLAND, NOVA SCOTIA, CANADA.GEES R; LYALL AK.1969; CANAD. J. EARTH SCI.; CAN; 1969(4), VOL. 6, NUM. 0002, P. 344 A 347Miscellaneous

ORIGIN OF THE BAY OF FUNDY,AN INTERPRETATION FROM SUB-BOTTOM PROFILESSWIFT DJP; LYALL AK.1968; MAR. GEOL.; NLD; 1968(8), VOL. 6, NUM. 0004, P. 331 A 343Miscellaneous

SEDIMENTS OF THE BAY OF FUNDY, A PRELIMINARY REPORT.SWIFT DJP; PELLETIER BR; LYALL AK et al.1969; MARIT. SEDIMENTS; CAN; 1969(12), VOL. 5, NUM. 0003, P. 95 A 100Miscellaneous

SUSPENDED SEDIMENT TRANSPORT AND RESUSPENSION AT THE SHELF-BREAK AND ON THE SLOPE, WILMINGTON CANYON AREA, EASTERN U.S.A.LYALL AK; STANLEY DJ; GILES HN et al.1970; GEOL. SOC. AMER., ABSTR. PROGRAMS; USA; 1970(10), VOL. 2, NUM. 0007, P. 612Miscellaneous

QUATERNARY SEDIMENTATION IN THE BAY OF FUNDY.SWIFT DJP; PELLETIER BR; LYALL AK et al.sdGEOL. SURV. CANADA, PAPER; CANADA; (EARTH SCI. SYMP. OFFSHORE EAST. CAN.; OTTAWA; 1971),1973, NUM. 0071-0023, P. 113 A 151Miscellaneous