It takes the average reader 7 hours and 26 minutes to read Fluid Movements — Element Transport and the Composition of the Deep Crust by David Bridgwater
Assuming a reading speed of 250 words per minute. Learn more
Many geologists have an equivocal attitude to fluid movements within the crust and the associated changes in the chemical and physical properties of crustal rocks. The controversies earlier this centuary between the "soaks" and the "pontiffs" memorably summarised by H. H. Read (1957) in The Granite Controversy have largely been resolved. Few would now advocate the formation of large granitic bodies by in situ transformation of pre-existing crust as the result of the passage of ichors without the formation of a granitic melt. To many geochemists fluid transport and metasomatism have become...
Fluid Movements — Element Transport and the Composition of the Deep Crust by David Bridgwater is 436 pages long, and a total of 111,616 words.
This makes it 147% the length of the average book. It also has 136% more words than the average book.
The average oral reading speed is 183 words per minute. This means it takes 10 hours and 9 minutes to read Fluid Movements — Element Transport and the Composition of the Deep Crust aloud.
Fluid Movements — Element Transport and the Composition of the Deep Crust is suitable for students ages 12 and up.
Note that there may be other factors that effect this rating besides length that are not factored in on this page. This may include things like complex language or sensitive topics not suitable for students of certain ages.
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