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
Coast Plutonic Complex: A mid-Cretaceous contractional orogen
Early Late Cretaceous east-vergent thrusts deform much of the eastern margin of the Coast Plutonic Complex in western British Columbia. Similarities in timing and style suggest that the faults represent a system of backthrusts to a west- vergent thrust belt on the west side of the complex. This geometry and the rarity of mid-Cretaceous strike-slip faults indicate that the Coast Plutonic Complex was a strongly contractional orogen in mid-Cretaceous time.
The administration of the courts
Section 28 of Article VI of the State Constitution provides that the Chief Judge of the Court of Appeals is the Chief Judge of the State and its chief judicial officer. The Chief Judge appoints a Chief Administrator of the Courts (or Chief Administrative Judge of the Courts if the appointee is a judge) with the advice and consent of the Administrative Board of the Courts. The Administrative Board consists of the Chief Judge as chair and the Presiding Justices of the four Appellate Divisions of the Supreme Court. The Chief Judge establishes statewide administrative standards and policies after consultation with the Administrative Board and approval by the Court of Appeals.