Geology 1
Geology 1
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In our eReader you can find the full English version of the book. Read Geology 1 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 Geology 1
What reading level is Geology 1 book?
To quickly assess the difficulty of the text, read a short excerpt:
The one part travels downward by conduction, the other by the descent of water; the one has to do primarily with the temperature before the melting-point of ice is reached; the other, with the tempera- ture after that point is reached; the first conforms measurably to the warm wave affecting other solid earth-matter, while the second is governed by special laws. After the surface portion of the ice is brought to the melting temperature, the additional heat which it receives melts the ice and is... transformed from sensible into potential heat. Ice charged with water is potentially, but not sensibly, warmer than ice which has just reached the melting temperature.
The warm wave of conduction dies out below like the cold wave.
The warm wave descending by the flow of water stops where the freezing temperature of water is reached. In regions where the average tem- perature is below freezing, the water-wave does not descend so far as the wave of conduction, since the latter descends below the zone where the melting temperature is found.
What to read after Geology 1?
You can find similar books in the "Read Also" column, or choose other free books by Thomas C Thomas Chrowder Chamberlin to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
The one part travels downward by conduction, the other by the descent of water; the one has to do primarily with the temperature before the melting-point of ice is reached; the other, with the tempera- ture after that point is reached; the first conforms measurably to the warm wave affecting other solid earth-matter, while the second is governed by special laws. After the surface portion of the ice is brought to the melting temperature, the additional heat which it receives melts the ice and is... transformed from sensible into potential heat. Ice charged with water is potentially, but not sensibly, warmer than ice which has just reached the melting temperature.
The warm wave of conduction dies out below like the cold wave.
The warm wave descending by the flow of water stops where the freezing temperature of water is reached. In regions where the average tem- perature is below freezing, the water-wave does not descend so far as the wave of conduction, since the latter descends below the zone where the melting temperature is found.
What to read after Geology 1?
You can find similar books in the "Read Also" column, or choose other free books by Thomas C Thomas Chrowder Chamberlin to read onlineMoreLess
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