New Zealand And Adjacent Islands
New Zealand And Adjacent Islands
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In our eReader you can find the full English version of the book. Read New Zealand And Adjacent Islands Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book New Zealand And Adjacent Islands
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Between these two Geological History. (VII. 1. ) 37 relatively well known districts it has always been assumed that the strike gradually bends round. 110 SUESS says of this structure : Two independent unilateral chains meet here in syntaxis. 111 This statement is bas^d on BUTTON'S paper and diagram and from what has been said it is evident that a great deal more detailed work is necessary before it can be definitely accepted. So far as our knowledge goes at present, it can only be said that it ...is highly probable. The country referred to however is extremely mountainous and rugged and will probably remain practically unknown for many years. BUTTON shows some subsidiary branching folds, but these are not properly known at present.
All we are justified in saying at present is that in Otago there is a broad mountain axis directed north-west and south-east, formed of unaltered Mesozoic rocks on both flanks, but with a core of schists probably of Mesozoic age. From the Haast Pass along the axis of the Southern Alps there is a continuous mountain axis directed north -north -east; it is composed of Mesozoic rocks from its eastern margin to the axis, and on its western slopes schists and granite occur; but even here indications are not wanting that a similar development of Mesozoic rocks extend westwards.
What to read after New Zealand And Adjacent Islands?
You can find similar books in the "Read Also" column, or choose other free books by Patrick Marshall to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Between these two Geological History. (VII. 1. ) 37 relatively well known districts it has always been assumed that the strike gradually bends round. 110 SUESS says of this structure : Two independent unilateral chains meet here in syntaxis. 111 This statement is bas^d on BUTTON'S paper and diagram and from what has been said it is evident that a great deal more detailed work is necessary before it can be definitely accepted. So far as our knowledge goes at present, it can only be said that it ...is highly probable. The country referred to however is extremely mountainous and rugged and will probably remain practically unknown for many years. BUTTON shows some subsidiary branching folds, but these are not properly known at present.
All we are justified in saying at present is that in Otago there is a broad mountain axis directed north-west and south-east, formed of unaltered Mesozoic rocks on both flanks, but with a core of schists probably of Mesozoic age. From the Haast Pass along the axis of the Southern Alps there is a continuous mountain axis directed north -north -east; it is composed of Mesozoic rocks from its eastern margin to the axis, and on its western slopes schists and granite occur; but even here indications are not wanting that a similar development of Mesozoic rocks extend westwards.
What to read after New Zealand And Adjacent Islands?
You can find similar books in the "Read Also" column, or choose other free books by Patrick Marshall to read onlineMoreLess
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