Government of Yukon

Enrolment by school and grade for all Yukon schools

Enrolment by school and grade for all Yukon schools

This aeromagnetic survey was carried out by Goldak Airborne Surveys from February 17, 2014 to March 21, 2014. The data were collected using split-beam cesium vapour magnetometers mounted in each of the tail booms of 2 Piper Navajo aircraft. Nominal traverse and control line spacings were 400 and...

Guidance, Forms, Templates

Geological map of the Anvil Lake area, central Yukon, parts of NTS 105K/11 and 105K/12

Surficial Geology of Alligator Lake map

Yukon Exploration and Geology 2007

Enrolment by school and grade for all Yukon schools

Enrolment by school and grade for all Yukon schools

Enrolment by school and grade for all Yukon schools

Enrolment by school and grade for all Yukon schools

Map sheets 95C/5 and 95D/8 in southeast Yukon contain eight successions of sedimentary rocks ranging from Proterozoic to Paleocene in age. Early to middle Paleozoic starta are best preserved. Proterozoic strata have been tentativel correlated with Pinguicula Group, Mackenzie Mountains Supergroup...

Enrolment by school and grade for all Yukon schools

Enrolment by school and grade for all Yukon schools

The Talbot Creek map area straddles the Ruby and Nisling ranges. Broad treeless uplands dominate the landscape with summits reaching 2100 m above sea level in the Ruby Range and 1800 m above sea level in the Nisling Range. Upland surfaces are covered with weathered bedrock colluvium and...

YEG 2010 contains up-to-date information on mining and mineral exploration activity, studies by industry, and results of recent geological field studies. Information in this volume comes from prospectors, exploration and government geologists, mining companies and students who are willing to...

Enrolment by school and grade for all Yukon schools

Individual papers from the overview are available for download. The Casino and Minto property descriptions each have an accompanying appendix that is only available digitally.

Geological map of NTS 106B/04, east-central Yukon

The Tantalus Formation developed within confined intermontane river valleys during the late stages of collision and amalgamation of Stikinia and associated arc systems with the North American plate in Upper Jurassic and early Lower Cretaceous times. While most of the extensive chert pebble...