...D. H. Hall Abstract A significant correlation exists between direction patterns in magnetic and tectonic trends on the northern two thirds of Texada Island, British Columbia. Patterns are analyzed by dividing the area into regions based on amplitudes of magnetic anomalies and on patterns...

...Fig. 2. Observed gravity (free-air offshore, Bouguer onshore) data in southwestern British Columbia. The study area is outlined by the large black rectangle. Very small dots denote the locations of the gravity stations. BI, Bowen Island; LI, Lasqueti Island; TI, Texada Island; SJI, San Juan...

... ‐ and S ‐arrival times were picked manually for up to 65 stations. Catalog hypocenters for earthquakes between 35 and 70 km depth in Cascadia are mapped in Figure  1a with a focus on southern Vancouver Island in Figure  1b . Texada seismicity is notably clustered, isolated, and represents the only...

..., island-arc-related Fe skarns, including the Merry Widow and Texada Island deposits (Fig. 1 ; Bacon, 1957 ; Sutherland Brown, 1962 ; Stevenson and Jeffrey, 1964 ; Eastwood, 1965 ; Sangster, 1969 ; Meinert, 1984 ; Webster and Ray, 1990 ). A number of less well known Fe oxide-rich Cu skarns also...

...Figure 1 —Index map showing geographic areas mentioned in the text. 1 = Texada Island; 2 = Vancouver Island; 3 = Sucia Island; 4 = Pentz; 5 = Anticline Ridge, north of Coalinga; 6 = Simi Hills; 7 = Santa Ana Mountains; 8 = Carlsbad; 9 = San Antonio del Mar; 10 = Arroyo Santa Catarina ...

...., 1969) and gravity data modeling (Hamilton and Seemann, 1992), it is normally fault- ed, down to the southwest, by the northwest-striking Texada fault (Hamilton and Seemann, 1992). To the east, there are sev- eral erosional remnants preserved on western Texada Island, Lasqueti Island, and Lang Bay...

.... On the northeast side of the Straits, small remnants of the lower parts of the series reappear on Texada, Lasqueti, and smaller islands. The most interesting part of these remnants consists of the probable equivalents of the Comox Formation on the south shore of Lasqueti, which there take the form of coarse...

... ~ - ~ N IC! F~G. 2. Generalized map of geologyof Vancouver Island and adjacent areas. Cretaceous, and small outcrops are found on Lasqueti and Texada Islands (see Figure 2). Clapp (1912) has described the geology of the south-east part of Van- couver Island. Buckham (unpublished manuscript) has discussed...

... reefs and coral-algal sands ( Figure 3 ). The inner shelf is capped by supratidal islands that protect coastal lagoons and enable the development of wide tidal flats. The carbonate barrier islands, tidal channels, tidal deltas, and shallow lagoons are the site of accumulation of oolitic sands and finer...

..., recovered normal polarity at one of their sites, the thick section at Punta San Jose, as well as reversed directions from Punta Banda in Baja California. Ward et al. (1997) subsequently identified reversed magnetochrons in Campanian rocks of the Nanaimo Group on Hornby Island and Texada Island, British...

... are observing the southward motion of North America while the Nanaimo Basin is maintaining a constant paleolatitude. It is interesting to note that the Texada Island samples of Ward et al. ( 1997 ) give a slightly (though insignificantly) steeper inclination than the younger, stratigraphically higher samples...

... attenuation with aqueous Pb, Cu, and Zn under active flow conditions ( Fig. 1 ). An acrylic column with 11 sampling ports uniformly spaced 5 cm apart was filled with marble originating from Texada Island, B.C., Canada (Lafarge Ltd., Coquitlam, B.C., Canada). The material was crushed and sieved to between 280...

.... Churches were built in all of these cities and towns. In the year 1544, over 40 churches and five hospitals existed on the island (Bayamo (1518), SC (1520), LH (1521), Port-au-Prince (1523), and Sancti Spíritus (1523)). All the hospitals had their barbers, nurses or itinerant quack doctors, but rarely real...

..., and in the location of the plate interface, it is frequently problematic to distinguish between intraslab or interface origins. Although focused on depths where slow slip appears more common beneath Vancouver Island (VI), the detailed study of the structure and both regular and low‐frequency earthquakes by Calvert...