Annual report . B. Temiskam an sediments with \ertical C. Contorted (iremille sediments. Iin shows Animikean sediments in characteristic horizontal beds; B, more or less schistose Temis-kamian sediments with vertical dip; C, contorted, Bchistose ffrenVille feedhnents. There is a normalprogression in metamorphism from the Animikean through the Temiskamian to the Grenville. 1913 Appendix 125 Moreover, the authors group together, under the name Temiskamian, the Teniis-kaming series of Cobalt, the Sudbury series, the so-called Huronian rocks of the La-cloche mountains and elsewhere of L
Annual report . B. Temiskam an sediments with \ertical C. Contorted (iremille sediments. Iin shows Animikean sediments in characteristic horizontal beds; B, more or less schistose Temis-kamian sediments with vertical dip; C, contorted, Bchistose ffrenVille feedhnents. There is a normalprogression in metamorphism from the Animikean through the Temiskamian to the Grenville. 1913 Appendix 125 Moreover, the authors group together, under the name Temiskamian, the Teniis-kaming series of Cobalt, the Sudbury series, the so-called Huronian rocks of the La-cloche mountains and elsewhere of Lake Huron, and the Hastings series of south-eastern Ontario. These rocks are of pre-Algoman and post-Laurentian age. It is seen, therefore, that according to the view of the authors, there has beenconsiderable confusion in the use of the names Upper and Lower Huronian, and thatthe Huronian has been made to include rocks that arc separated by a profound uncon-formity. It has accordingly been considered advisable not to employ the name Huron-ian in the table
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Keywords: ., bookcentury1800, bookdecade1890, booksubjectminesandmineralresou
