Transition Metals Corp. reported the results of a successful property-wide helicopter-supported, tree-top, biogeochemical survey completed over approximately 150 square kilometers of its 100% owned Wollaston Copper project in north central Saskatchewan. Transition has added an additional 23 square kilometres to cover significant areas of anomalous copper outlined by this survey. The project is located. Approximately 60 kilometres southwest along strike from the Janice Lake project, a sedimentary hosted copper project being aggressively explored by Rio Tinto Exploration Canada (RTEC) and Forum Energy Metals (Forum). The survey included the collection and analysis of tree-top twigs from 637 trees at approximately 500 metre spacing, with infill sampling around several known base metal showings. The 663 ashed twig samples, including duplicates, of jack pine and black spruce were analyzed by ICP-MS1 and yielded copper (Cu) values from 88 parts per million (ppm) to 650 ppm. The survey was successful at confirming the presence of copper enrichment in samples collected over and proximal to historical showings, as well as delineating new anomalous trends and target areas for future investigation. The results highlight large and continuous zones exhibiting enriched copper signatures in vegetation on both the Fannon and Porcupine blocks associated with favourable rock types and structures for sediment hosted copper. On the Fannon block vegetation samples defined trends around known showings, including an approximate 500 metres by 2 kilometres long trend of highly anomalous copper around the only drilled showing (the Flag Lake Showing) on the block, which was reported to have returned 10.82 metres grading 0.24% Cu and 7.4 metres grading 0.49% Cu.2 Additional copper anomalies were identified approximately 5 kilometres southwest of the Flag Lake Showing over an area approximately 5 by 3 kilometres. On the Porcupine block anomalous copper was returned from vegetation sampling in the vicinity of the Tosi showing where bedrock sampling by Transition returned grab samples containing values up to 0.44% Cu. In addition, the vegetation sampling on the Porcupine block highlighted elevated copper signatures, coincident with historical MMI3 Cu anomalies, associated with previously unexplored sedimentary horizons along an approximately 6 kilometre strike length inside the southwest boundary of the property.