An Introduction to Geology Intended to Convey a Practical Knowledge of the Scie
An Introduction to Geology Intended to Convey a Practical Knowledge of the Scie
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In our eReader you can find the full English version of the book. Read An Introduction to Geology Intended to Convey a Practical Knowledge of the Scie 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 An Introduction to Geology Intended to Convey a Practical Knowledge of the Scie
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To quickly assess the difficulty of the text, read a short excerpt:
General Cockburn.
t Jerome, who resided in Syria in the fourth century, informs us, that the rock of salt was existing in his time ; and fancifully relates certain peculiarities respecting it, which equal in absurdity the legends of the darkest ages of papal superstition.
. Jjk ' ' ROCK SALT IN THE ALPS. ' 209 limestone, and sandstone ; and between the lower gypsum and the upper, there are thick beds of argillaceous limestone, and similar argillaceous limestone forms caps over the upper gypsum.... The gypsum in the large beds is anhydrous, and contains parti- cles of rock salt and common gypsum disseminated through it. The prevailing fossils are ammonites and belemnites. * The mineral characters of the strata at Bex, and the imbedded fossils, incline me rather to -refer the argillaceous limestone, over and under the gypsum and salt beds, to the English lias, than to magnesian limestone. Many beds of the lias in England, con- tain much muriat of soda and sulphat of magnesia.
The saliferous gypsum in the Tarentaise is anhydrous, and contains a.
What to read after An Introduction to Geology Intended to Convey a Practical Knowledge of the Scie?
You can find similar books in the "Read Also" column, or choose other free books by Robert Bakewell to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
General Cockburn.
t Jerome, who resided in Syria in the fourth century, informs us, that the rock of salt was existing in his time ; and fancifully relates certain peculiarities respecting it, which equal in absurdity the legends of the darkest ages of papal superstition.
. Jjk ' ' ROCK SALT IN THE ALPS. ' 209 limestone, and sandstone ; and between the lower gypsum and the upper, there are thick beds of argillaceous limestone, and similar argillaceous limestone forms caps over the upper gypsum.... The gypsum in the large beds is anhydrous, and contains parti- cles of rock salt and common gypsum disseminated through it. The prevailing fossils are ammonites and belemnites. * The mineral characters of the strata at Bex, and the imbedded fossils, incline me rather to -refer the argillaceous limestone, over and under the gypsum and salt beds, to the English lias, than to magnesian limestone. Many beds of the lias in England, con- tain much muriat of soda and sulphat of magnesia.
The saliferous gypsum in the Tarentaise is anhydrous, and contains a.
What to read after An Introduction to Geology Intended to Convey a Practical Knowledge of the Scie?
You can find similar books in the "Read Also" column, or choose other free books by Robert Bakewell to read onlineMoreLess
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