958 resultados para Rflp Map


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Commençant par : «... nois negée et si li out aparellée à sa chevalerie robe blanche de samit, cote et mantel... » et finissant par : «... conquier, damoisele, nos en aurons... helmes et cil chevaliers a... » . Incomplet an commencement et à la fin ; le dernier feuillet est en partie effacé.

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Contient : «... l'assemblée qui lors i fu la veille de Pantecouste. Explicit. Ci fenist mestre Gautier Map son livre et commance le Galaad. (Fol. 152.) A la veille de Pantecouste quant li compaignon de la Table ronde... » (Incomplet. de la fin.) — Miniatures

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Master Plan Phase 2. Map of the original 1964 master plan showing the planned campus layout and distances from the centre of campus (ie. the Tower).

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Master Plan Phase 2. This overhead map of the original 1964 Master Plan shows the planned campus layout along the escarpment.

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This map shows the entire campus master plan and details what each area of land would be used for.

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Note the land allocated for Brock University shaded in gray between Thorold and Grantham townships.

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Phase 1 Map of the Master Plan showing the Tower and Thistle Complex, along with some additional buildings and the main parking lot. Note the location of the Central Utilities Building to the east differs from it's actual location along the escarpment.

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Sediment relationships observed during geological mapping in southeastern Ontario indicate a relatively simple deglaciation history for the area during late Wisconsin time. The ice from the north (part of the Lake Simcoe lobe) and the Lake Ontario ice lobe, which were coalesced during most of late Wisconsin time, initially separated along the crest of the Oak Ridges Moraine. Available data indicate that the Oak Ridges Moraine is composed primarily of sediments pre-late Wisconsin in age capped by late Wisconsin till and interlobate deposits. Retreat of the northern ice was relatively steady and resulted in the deposition of the Dummer Moraines, a facies of the drumlinized till to the south. Retreat of the Lake Ontario ice lobe into the Lake Ontario basin was interrupted by a re-advance which covered the southeastern half of the map area. The northern ice had already retreated from the area by this time. The Lake Ontario lobe was fed through the St. Lawrence Valley, indicating that the Ottawa Valley was ice filled at this time. High level glacial lakes fronted the ice during deglaciation. These waters quickly fell to low levels as the ice retreated from the St. Lawrence Valley, opening lower outlets.