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The Earth From the Air

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The author may have thought that the actual years don't matter, but it would still have been nice to know. The purchase of a photograph on this site or from authorised representatives will be by way of « Signed Prints », « Limited Editions of 3 and 8 copies » or as a « Unique Artwork ». The atmosphere changed significantly over time, affected by many factors such as volcanism, life, and weathering. The atmospheric pressure at the top of the stratosphere is roughly 1/1000 the pressure at sea level.

The Earth from the Air - Yann Arthus-Bertrand - Google Books

Didn't do the work justice will take my sons there to see it again, loved the way it was so accessible and no grafitti.

Yann Arthus-Bertrand is a world-renowned aerial photographer, journalist, reporter and environmentalist. This book includes photographs that are accompanied by informative captions that illuminate what we see, and describe the environmental concerns related to each location. It was in the late 70s, in Kenya, while studying with his wife Anne the every day life of a pride of lions that, that he truly became a photographer. With over 100,000 shots in the collection, Yann has chosen the 160 exhibits to communicate his own vision. Google's use of the DART cookie enables it to serve ads to your users based on their visit to your sites and other sites on the Internet.

from the air Aerial View - Views from the air

Still another region of increasing temperature with altitude occurs at very high altitudes, in the aptly-named thermosphere above 90km.However, the temperature has a more complicated profile with altitude, and may remain relatively constant or even increase with altitude in some regions (see the temperature section, below). Numbers are mainly from 2000, with CO 2 and methane from 2019, and do not represent any single source. above Earth's surface to the stratopause at an altitude of about 50 to 55km (31 to 34mi; 164,000 to 180,000ft). billion years ago during the Great Oxygenation Event and its appearance is indicated by the end of the banded iron formations.

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