The Dil-Dil Plateau is a small lava plateauBulletin 100: Geology and Mineral Occurrences of the Taseko - Bridge River Area, p.11, p.54, by P. Schiarizza, R.G. Gaba, J.K. Glover, J.I. Garver and P.J. Umhoefer, publ. BC Ministry of Energy, Mines and Petroleum Resources on the west side of the upper valley of Big Creek in the southern Chilcotin District of the Central Interior of British Columbia. The plateau is a shelf-like extension of the subrange of the Chilcotin Ranges containing Taseko Mountain and Mount Vic to the west, and is roughly rectangular in shape, and of c.25–30 km2 in area and forming a transition between the range and the Chilcotin Plateau at 2000m-2300m.Bulletin 100: Geology and Mineral Occurrences of the Taseko - Bridge River Area, p.13, by P. Schiarizza, R.G. Gaba, J.K. Glover, J.I. Garver and P.J. Umhoefer, publ. BC Ministry of Energy, Mines and Petroleum Resources
The Dil-Dil Plateau consists mostly of flat-lying basaltic lava flows ranging from Miocene to Pliocene age.Geological, geochemical and geophysical report on the Big Creek 1, 2 and 3 claims These basalts are part of a larger volcanic formation known as the Chilcotin Group.
References
External links Trail Ventures BC photogallery (see 3/4 of the way down the page, on the right)