The Bluebird showing is located on the summit of Evening Ridge, about 9 kilometres southeast of Nelson.
The area is underlain by granite of the Late to Middle Jurassic Nelson Intrusions (Nelson batholith) near the contact with Lower Jurassic Ymir Group sediments.
A quartz vein about 0.25 metre wide has been traced along a strike of 320 degrees in granite. The vein dips 53 degrees north and contains rusty quartz gangue with disseminations of pyrite and galena. Gold assays are variable from 2 to 30 grams per tonne over widths of 20 to 30 centimetres and silver values vary from 13 to 50 grams per tonne (Minister of Mines Annual Report 1928, page 325).