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Geology of Gravel Creek (105B/10) and Irvine Lake (105B/11) Map Areas,...
The Irvine Lake and Gravel lake map-areas (NTS 105B/10,11) lie within the northern Omineca Belt, west of the Tintina-Northern Rocky Mountain Trench (NRMT) fault. The eastern...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Geology of Hopkins Lake Map Area, Yukon (NTS 115H/7)
Geological map (1:50,000 scale) of the Hopkins Lake area, southwestern Yukon (NTS 115H/7) including geological cross sections, mineral occurrences and isotopic age determinations.Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Geological Map of Fairchild Lake Map Area (106C/13), Wernecke Mountains
Geological map (1:50,000 scale) of Fairchild Lake area, Wernecke Mountains, central Yukon (NTS 106C/13) including a geological cross section and mineral occurrences.Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Placer Mining and Exploration Compilation (106D)
A placer mining and exploration compilation of NTS map sheet 106D, central Yukon Territory, Canada. This compilation includes the location, history and previous work,...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Placer Mining and Exploration Compilation (115F and G)
A placer mining and exploration compilation of NTS map sheets 115F and 115G, southern Yukon Territory, Canada. This compilation includes the location, history and previous...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Sediment-hosted disseminated gold occurrence, northeast Mayo Lake area
Low to moderate levels of gold are widely distributed within a distinct member of the Mississippian Keno Hill Quartzite northeast of Mayo Lake, demonstrating characteristics of...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Sedimentology of White Channel Placer Deposits, Klondike, West Central Yukon
The White Channel placer deposit in the Klondike area is a Pliocene to early Pleistocene braid plain sequence with tributary alluvial fan and gravity flow deposits. Lithofacies...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Regeneration on Linear Developments Subject to Wildfires in a Zone of...
With assistance from the Yukon Oil and Gas Branch, EDI Environmental Dynamics Inc. developed and submitted a proposal to the Mining and Petroleum Environmental Research Group...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Report on 2002 Geochemical Procedures used during Mineral Resource Assessments
not_specifiedDate updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Protected Areas in Canada
This report is a compilation of designated protected areas in each Canadian province and territory as of April 2001.Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
A short history of the finding of gold in the Klondike
Gold was first reported in the Yukon region by fur traders and missionaries in the mid 1800s. Fur trader Robert Campbell noted the presence of gold near the site of Fort...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Placer Mining and Exploration Compilation (105A/B/C/D)
A placer mining and exploration compilation of parts of the Watson Lake and Whitehorse mining districts, southern Yukon Territory, Canada. This compilation includes the...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
An evaluation of coal-bearing strata at Division Mountain (115 H/8...
The Division Mountain area is underlain primarily by Jurassic to Cretaceous(?) sedimentary rocks of the Laberge Group and Tantalus Formation. The Laberge Group is divisible...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Alteration and zonation in the Kalzas W-Sn-Mo Porphyry-vein deposit, 105 M/7, Yukon
The Kalzas W-Sn-Mo deposit is located in central Yukon, 282 km north of Whitehorse on the northern side of Big Kalzas Lake. Wolframite-molybdenite-cassiterite mineralization...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Biogeochemical prospecting in the Yukon-Tanana Terrane, Yukon Territory
Restoration of the 450 km of right lateral movement on the Tintina Fault brings the massive sulphide-rich Finlayson area of the Yukon-Tanana Terrane to a location southeast of...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Brewery Creek property, west-central Yukon
The Brewery Creek property is a low grade oxide gold deposit hosted by syenitic intrusive rocks in the south Klondike area. The deposit apears to be structurally controlled by...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
'Alpine-type' ultramafic rocks of the Kluane metamorphic assemblage,...
Mica-quartz schist and olivine serpentinites form the Kluane metamorphic assemblage, a 150-km-long belt that is wedged between the Yukon-Tanana Terrane and the Insular...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Age and setting of dinosaur trackways, Ross River area, Yukon Territory (105F/15)
Chert-bearing clastic strata are a common component of Jurassic and younger terrestrial sequences in the Yukon. The discovery of dinosaur trackways in a small inlier of...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Geology of Ogilvie Mountains Breccias, Coal Creek Inlier (116B/11, 13, 14)...
Geological map (1:50,000 scale) of the Ogilvie Mountains Breccias, Coal Creek Inlier, central Yukon (NTS 116B/11, 13, 14) including geological cross sections and mineral...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML -
Blende property, central Yukon
The Blende is a large epigenetic zinc-lead-silver deposit hosted by brecciated middle Proterozoic dolomite. Mineralization occurs intermittently along a zone about 6 km long...Date updated: 2011-04-04Date created: 2011-04-04Publisher: Yukon Geological SurveyFormat: HTML