Ridley College papers, 1983, 1985-1986, 1989-1990

Ridley College was conceived in 1888 by a group of Anglican clergy and laymen eager to establish a school for boys in Ontario that emphasized strong academic and religious values. The school was originally known as Bishop Ridley College, in tribute to Nicholas Ridley, a 16th century English churchman who was martyred during the Protestant Reformation for refusing to renounce his Anglican faith. The first facility was the stately and spacious Springbank Sanatorium; shortly thereafter, construction was begun across the old Welland Canal on a lower school for boys age 5 to 13 on the present-day campus site. The name “Springbank” stems from the name of the hotel constructed in 1864 by Dr. Theophilus Mack on Yates Street. Fortuitously, the directors of what would become Ridley College were looking to found a new boys’ school. The sale of the building was completed in 1888 and Ridley began operations in September 1889. In October 1903, the Springbank building complex was consumed by fire forcing the school to move across the canal to its modern western campus. The Ridley campus grew dramatically during the 1920's, and new buildings and facilities were added in each of the following decades. The school became co-educational in 1973; just over a dozen girls enrolled in the inaugural year, while today almost half of Ridley's students are girls. Adapted from: http://www.ridleycollege.com/podium/default.aspx?t=125335 (March 22, 2011)

Ridley College Cadet Dance Card - May 7th, 1920

A dance card from a Ridley College Cadet dance, dated 7 May, 1920. The programme is twenty dances long with each dance filled with a name. The back page also has some writing, it is unclear if they are names.

Photograph - Ridley College

A photograph of Ridley College. There is a note on the back that reads, "This is the old building of Ridley College 'R!R!'".

Ridley College Pin

A Ridley College, St. Catharines pin which belonged to Chester Woolworth of the Woolworth Family.

Sistema reprodutivo do Ipê-Branco: Tabebuia roseo-alba (Ridley) Sandwith (Bignoniaceae)

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Medhi Charef, Emir Kusturika, Spike Lee, Katia Lund, Jordan y Ridley Scott, Stefano Veneruso, y John Woo. Todos los niños invisibles (All the invisible children)

Fil: Vicente, María Eugenia. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Medhi Charef, Emir Kusturika, Spike Lee, Katia Lund, Jordan y Ridley Scott, Stefano Veneruso, y John Woo. Todos los niños invisibles (All the invisible children)

Fil: Vicente, María Eugenia. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Medhi Charef, Emir Kusturika, Spike Lee, Katia Lund, Jordan y Ridley Scott, Stefano Veneruso, y John Woo. Todos los niños invisibles (All the invisible children)

Fil: D'Assaro, Adriana. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Henrici Ridley ... Anatomia cerebri complectens : ejus mechanismum [et] physiologiam, simulque nova quædam inventa, cum correctionibus aliquod veterum ac recentiorum, qui in eandem materiam scripserunt. Cui annexum est examen accuratum functionum animalium et motus muscularis. Omnia elegantibus ad vivum expressis sculpturis illustrata, ex Anglico in Latinum fidelitur translata.

Mode of access: Internet.

The works of Nicholas Ridley, D.D., sometime Lord Bishop of London, martyr, 1555 /

Includes reprints of original title-pages.

Ridley & Co.'s Monthly Wine and Spirit Trade Circular

Mode of access: Internet.

Evaluation of Potential Post-Glacial Faults Using Bare-Earth LiDAR Topographic Data Near Ridley Island, British Columbia

I present results of my evaluation to identify topographic lineaments that are potentially related to post-glacial faulting using bare-earth LiDAR topographic data near Ridley Island, British Columbia. The purpose of this evaluation has been to review bare-earth LiDAR data for evidence of post-glacial faulting in the area surrounding Ridley Island and provide a map of the potential faults to review and possibly field check. My work consisted of an extensive literature review to understand the tectonic, geologic, glacial and sea level history of the area and analysis of bare-earth LiDAR data for Ridley Island and the surrounding region. Ridley Island and the surrounding north coast of British Columbia have a long and complex tectonic and geologic history. The north coast of British Columbia consists of a series of accreted terranes and some post-accretionary deposits. The accreted terranes were attached to the North American continent during subduction of the Pacific Plate between approximately 200 Ma and 10 Ma. The terrane and post-accretionary deposits are metamorphosed sedimentary, volcanic and intrusive rocks. The rocks have experienced significant deformation and been intruded by plutonic bodies. Approximately 10 Ma subduction of the Pacific Plate beneath the North America Plate ceased along the central and north coast of British Columbia and the Queen Charlotte Fault Zone was formed. The Queen Charlotte Fault Zone is a transform-type fault that separates the Pacific Plate from the North America Plate. Within the past 1 million years, the area has experienced multiple glacial/interglacial cycles. The most recent glacial cycle occurred approximately 23,000 to 13,500 years ago. Few Quaternary deposits have been mapped in the area. The vast majority of seismicity around the northwest coast of British Columbia occurs along the Queen Charlotte Fault Zone. Numerous faults have been mapped in the area, but there is currently no evidence to suggest these faults are active (i.e. have evidence for post-glacial surface displacement or deformation). No earthquakes have been recorded within 50 km of Ridley Island. Several small earthquakes (less than magnitude 6) have been recorded within 100 km of the island. These earthquakes have not been correlated to active faults. GPS data suggests there is ongoing strain in the vicinity of Ridley Island. The strain has the potential to be released along faults, but the calculated strain may be a result of erroneous data or accommodated aseismically. Currently, the greatest known seismic hazard to Ridley Island is the Queen Charlotte Fault Zone. LiDAR data for Ridley Island, Digby Island, Lelu Island and portions of Kaien Island, Smith Island and the British Columbia mainland were reviewed and analyzed for evidence of postglacial faulting. The data showed a strong fabric across the landscape with a northwest-southeast trend that appears to mirror the observed foliation in the area. A total of 80 potential post-glacial faults were identified. Three lineaments are categorized as high, forty-one lineaments are categorized as medium and thirty-six lineaments are categorized as low. The identified features should be examined in the field to further assess potential activity. My analysis did not include areas outside of the LiDAR coverage; however faulting may be present there. LiDAR data analysis is only useful for detecting faults with surficial expressions. Faulting without obvious surficial expressions may be present in the study area.

Age and growth in olive ridley seaturtles (Lepidochelys olivacea) from the north-central Pacific: a skeletochronological analysis

The olive ridley is the most abundant seaturtle species in the world but little is known of the demography of this species. We used skeletochronological data on humerus diameter growth changes to estimate the age of North Pacific olive ridley seaturtles caught incidentally by pelagic longline fisheries operating near Hawaii and from dead turtles washed ashore on the main Hawaiian Islands. Two age estimation methods [ranking, correction factor (CF)] were used and yielded age estimates ranging from 5 to 38 and 7 to 24 years, respectively. Rank age-estimates are highly correlated (r = 0.93) with straight carapace length (SCL), CF age estimates are not (r = 0.62). We consider the CF age-estimates as biologically more plausible because of the disassociation of age and size. Using the CF age-estimates, we then estimate the median age at sexual maturity to be around 13 years old (mean carapace size c. 60 cm SCL) and found that somatic growth was negligible by 15 years of age. The expected age-specific growth rate function derived using numerical differentiation suggests at least one juvenile growth spurt at about 10–12 years of age when maximum age-specific growth rates, c. 5 cm SCL year−1, are apparent.