Geologic descriptionJasper (1965) reports that a prospector noted occasional blebs of malachite and chalcopyrite in and above a Late Triassic(?) unfossiliferous and massive to poorly bedded limestone. Locally the limestone occurs as lenses as much as 30 m thick in shear zones within the Early Jurassic to Late Triassic(?) Talkeetna Formation. The extent of mineralization is not known. When Brooks (1918) first reported this occurrence he reported, based on vague data, that the deposit was similar to the occurrence on Moose Creek (ARDF number AN066). |
Geologic map unit |
(-148.502219790386, 61.9494688693844) |
Age of mineralization |
Late Triassic (?) or younger; the mineralization is in limestones within the Early Jurassic to Late Triassic(?) Talkeetna Formation. |
Alteration of deposit |
Oxidation of Cu minerals. |