. Fig. I.—m.\p of the qcest's track. At Cape Lookout, however, an entirely different set of conditions was seen. There is here a meta- morphic sei'ies, which consists of the following in order from the sea towards the north ^ : Quartz hornblende epidote schist. ^ James M. Wordie, , " ; 6 Phyllite is one of the metamorphic rocks. These are rocks which were either originally igneous or deposited by sedimenta- tion from water, but have been modified by heat or crushing, and differ widely from their original forms. Quartz, horn- blende, albite, etc., are various forms
. Fig. I.—m.\p of the qcest's track. At Cape Lookout, however, an entirely different set of conditions was seen. There is here a meta- morphic sei'ies, which consists of the following in order from the sea towards the north ^ : Quartz hornblende epidote schist. ^ James M. Wordie, , " ; 6 Phyllite is one of the metamorphic rocks. These are rocks which were either originally igneous or deposited by sedimenta- tion from water, but have been modified by heat or crushing, and differ widely from their original forms. Quartz, horn- blende, albite, etc., are various forms of the element silicon— familiar to us in the form of flint—-in conjunction with soda, aluminium, iron. etc. ' Dr. C. E. Tilley, , Cambridge.
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