It takes the average reader 6 hours and 37 minutes to read Sedimentation History in the Arctic Ocean and Subarctic Seas for the Last 130 kyr by M. A. Levitan
Assuming a reading speed of 250 words per minute. Learn more
The book reflects the results of the study of sedimentation history, paleoclimatology, and paleoceanography of the Arctic and Subarctic during the last 130 ka. The main objects under consideration are marine basins of the West Subarctic (Iceland, Norwegian, and Greenland Seas), the Arctic Ocean (Barents, Pechora, Kara, Laptev, East Siberian, Chukchi Seas and deep-sea Arctic Ocean proper), East Subarctic (Bering and Okhotsk Seas). The modern environment and geological history of water- (ice-) sheds and marine basins have been studied for each region, using different sedimentological and geochemical proxies. Mainly results of the authors' own studies are represented, with special emphasis on glacial/interglacial variability and land-ocean interaction. The book is aimed at sedimentologists, quaternary and marine geologists, paleoclimatologists and paleoceanographers, as well as being of great interest to students in the related fields.
Sedimentation History in the Arctic Ocean and Subarctic Seas for the Last 130 kyr by M. A. Levitan is 387 pages long, and a total of 99,459 words.
This makes it 131% the length of the average book. It also has 122% more words than the average book.
The average oral reading speed is 183 words per minute. This means it takes 9 hours and 3 minutes to read Sedimentation History in the Arctic Ocean and Subarctic Seas for the Last 130 kyr aloud.
Sedimentation History in the Arctic Ocean and Subarctic Seas for the Last 130 kyr 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.
When deciding what to show young students always use your best judgement and consult a professional.
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