3i6 



Pot hole in Wark gabbro-diorite gneiss, formed by 

 glacial stream descending through a crevasse, or by inter- 

 glacial stream. Wark gneiss cut by apophyses of Colquitz 

 quartz diorite. 



Locality 10 — From 9 over pre-Glacial lowland, largely 

 covered by Maywood clays with thin mantle of Vashon 

 drift in places and a few outcrops of Wark gneiss. 



Maywood clays. Clays used for the manufacture of 

 common brick and tile. Marine fossils. 



Excursion G 2, (Sections I and II). 



Leaving the Empress hotel the entire excursion proceeds 

 along the shore south of Victoria to Oak bay, stopping at 

 various points of interest, and then returns to Victoria, via 

 Mt. Tolmie. 



Locality 11 — Contact shatter breccia of Wark gabbro- 

 diorite gneiss and Saanich granodiorite, cut by complex of 

 diorite porphyrite dykes. Minor faulting. Glacial 

 scouring, producing roches moutonnees, deep grooves, and 

 striations. General view of contraposed shoreline. 



Locality 12 — Good view to the east of an irregular 

 rocky, contraposed shore line. Hard rocks overlain by 

 retrograded Vashon drift and Maywood clays. 



Locality 13 — Contact complex and shatter breccia of 

 Vancouver meta-andesite, Wark gabbro-diorite gneiss, and 

 Saanich granodiorite. Aplitic apophyses with quartz 

 segregations and quartz veinlets. Hybridiom. 



Breccia foliated and slightly faulted Glacial grooving 

 and striation. East to Clover point, submaturely retro- 

 graded portion of shore line. Clover point, a hard rock 

 headland, showing beginning of contraposition. 



Locality 14 — Between 13 and 14 pre-Glacial lowland 

 covered by Maywood clays with a thin mantle of Vashon 

 drift and frequent outcrops of Vancouver meta-volcanics. 

 To the south Gonzales hill, altitude 215 feet (65 m.), a 

 monanock surmounting the lowland. 



Vancouver meta-volcanics, foliated flow-breccia. Roches 

 moutonnees, grooving, and crossed striations. 



Locality 15 — Between 14 and 15 pre-Glacial lowland 

 of Maywood clays with thin mantle of Vashon drift and 

 numerous outcrops of Vancouver meta-andesites. Foliated, 

 contact metamorphosed Vancouver volcanics, cut by a 



