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Страница 377
Before we'entèr upon a rapid analysis of this series , we must apprize the
uninitiated , that the rocks , as they are here enumerated , have never yet been
found in any part of the world lying all of them one above the other . In some parts
, and ...
Before we'entèr upon a rapid analysis of this series , we must apprize the
uninitiated , that the rocks , as they are here enumerated , have never yet been
found in any part of the world lying all of them one above the other . In some parts
, and ...
Страница 382
The district around it , is composed of slaty rocks . Let our readers suppose to
themselves ten miles square of slaty rocks ; and then the almost inconceivable
fracture of these rocks , by the ascension , from below , of a gigantic mass of
granite ...
The district around it , is composed of slaty rocks . Let our readers suppose to
themselves ten miles square of slaty rocks ; and then the almost inconceivable
fracture of these rocks , by the ascension , from below , of a gigantic mass of
granite ...
Страница 386
In North America , the carboniferous limestone , is the most extensive formation
we possess of the secondary rocks , amongst which it has , by some geologists ,
been classed ; and by them placed at the bottom of the series of secondaries .
In North America , the carboniferous limestone , is the most extensive formation
we possess of the secondary rocks , amongst which it has , by some geologists ,
been classed ; and by them placed at the bottom of the series of secondaries .
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