GEOLOGY AND MINERAL OCCURRENCES OF THE TATLAYOKO LAKE MAP AREA ( 92 N / 8 , 9 and 10 )
Agreement,  was initiated in 1992  with  geological mapping of the Mount Tatlow map area (Riddell et al., 1993a,b). No fiddwork was done in 1993, but the project was continued 'In 1994 with geological mapping of the Tatlayoko Lake map area, reported on here. The project's objectives are to update the geological database for the eastem Coast Belt in portions of the Mount Waddington and  Taseko  Lakes  map areas, and to integrate the structural and stratigraphic relationships established within this area with rapidly evolving concepts regarding the tectonic anti stratigraphic framework of the region. This will provide an improved geological framework for understanding the settings and controls of known mineral
The Wineglass assemblage, lower Chilcotin River, south-central British Columbia: Late Permian volcanic and plutonic rocks that correlate with the Kutcho assemblage of northern British Columbia
Late Permian volcanic and plutonic rocks that were identified along the lower Chilcotin River by Read (1993) were examined to evaluate a possible correlation with the Kutcho assemblage of northern British Columbia, host to the Kutcho Creek volcanogenic massive sulphide deposit. These rocks, herein named the Wineglass assemblage, include a lower volcanic unit of mainly basalt, an upper volcanic unit that includes rhyolite, basalt, and felsic volcaniclastic rocks, and an intrusive body of tonalite, quartz diorite, and granodiorite, referred to as the Wineglass pluton. The Wineglass assemblage is correlated with the Kutcho assemblage on the basis of its striking lithologic similarity, overlapping U-Pb zircon ages, similar unconformable relationship with an overlying Triassic-Jurassic sedimentary sequence, and similar relationship to structurally overlying Cache Creek Complex. Clastic sedimentary rocks that unconformably overlie the Wineglass assemblage are part of the predominantly Late Triassic-Middle Jurassic Cadwallader arc terrane. Expanding the definition of Cadwallader terrane to include the Wineglass assemblage and correlatives makes for a compelling correlation with Wallowa terrane, in the Blue Mountains region of northeastern Oregon and west-central Idaho.
Thermal properties of the Florida Current as related to Ocean Thermal Energy Conversion (OTEC)
The thermal properties of the Florida Current are presented and analyzed for the available ocean thermal energy. For a cold water intake depth equal to or greater than 600 m, potential sites for Ocean Thermal Energy Conversion (OTEC) power plants appear to exist in the Straits of Florida and, to a lesser extent, off the coasts of Georgia and South Carolina. The maximum thermal differences occur on the continental shelf because of the geostrophic motion of the Gulf Stream. An estimate of the total available ocean thermal energy from the Florida Current, delivered in the form of electricity, is 3.5 × 1012 kWh yr−1. For a cold water suction depth of 600 m or more, seasonal variability in the ocean thermal resource is approx. ±35 per cent of average annual output.