Annual report . ElliiJSoidal greenstone, Aiuikougunii lake, wiiich lies to the northwest of the map Unconformity between conglomciate of the Timiskaming series and Keewatin L. 1824, Kirkland lake. 1920 Kirkland Lake Gold Area 9 Diabase, occurring as dikes and broad masses, intrudes the fine-grained green-stone at many places. This rock is generally less fresh-looking than the Nipissingdiabase of Cobalt, but occasionally is mistaken for this much younger basic is often light green in colour and coarse in grain like gabbro, while the originalconstituents are usually
Annual report . ElliiJSoidal greenstone, Aiuikougunii lake, wiiich lies to the northwest of the map Unconformity between conglomciate of the Timiskaming series and Keewatin L. 1824, Kirkland lake. 1920 Kirkland Lake Gold Area 9 Diabase, occurring as dikes and broad masses, intrudes the fine-grained green-stone at many places. This rock is generally less fresh-looking than the Nipissingdiabase of Cobalt, but occasionally is mistaken for this much younger basic is often light green in colour and coarse in grain like gabbro, while the originalconstituents are usually altered to secondary minerals. There is a large volume ofthis rock around Amikougami lake and throughout the Keewatin areas in the northpart of Teck and Lebel. The rock is pre-Timiskaming in age, since an unconformity was observed onmining claim L. 1824 on the south shore of the northwest bay of Kirkland of the diabase were found as pebbles in the Timiskaming conglomeratethat rests on the diabase. Numerous narrow rusty carbonate bands occur throughout various parts of thefveewatin. A pr
Size: 1829px × 1366px
Photo credit: © The Reading Room / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1800, bookdecade1890, booksubjectminesandmineralresou
