By Richard Fortey
In Earth, the acclaimed writer of Trilobite! and Life takes us on a grand journey of the earth's actual prior, exhibiting how the heritage of plate tectonics is etched within the panorama round us.
Beginning with Mt. Vesuvius, whose eruption in Roman occasions helped spark the technology of geology, and finishing in a lab within the West of britain the place mathematical types and lab experiments substitute direct statement, Richard Fortey tells us what the current says approximately historic geologic procedures. He exhibits how plate tectonics got here to rule the geophysical panorama and the way the proof is written within the hills and within the stones. And within the procedure, he's taking us on an excellent trip world wide to go to essentially the most attention-grabbing and fascinating spots at the planet.
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Extra resources for Earth: An Intimate History
1993. Vendian geology of Svalbard. Norsk Polar Institut Skrifter, 193. H OFFMAN , P. F. & S CHRAG , D. P. 2002. The Snowball Earth hypothesis: testing the limits of global change. Terra Nova, 14, 129–155. J ENKINS , G. S. & F RAKES , L. A. 1998. GCM sensitivity test using increased rotation rate, reduced solar forcing and orography to examine low latitude glaciation in the Neoproterozoic. Geophysical Research Letters, 25, 3525– 3528. K HAIN , V. E. & Y ASAMANOV , N. A. 1987. The paradox of Late Proterozoic glaciations and continental drift (in Russian).
M. & R UZHENTSEV , S. V. 1996. Spatiotemporal relationships of structures of the Pacific and Indo-Atlantic types in the Late Precambrian and Vendian (in Russian). Doklady Akademiy Nauk, 350, 799– 802. M YROW , P. M. 1995. Neoproterozoic rocks of the Newfoundland Avalon Zone. Precambrian Research, 73, 123–136. M YROW , P. M. & K AUFMAN , A. J. 1999. A newly discovered cap carbonate above Varangian-age glacial deposits in Newfoundland, Canada. Journal of Sedimentary Research, 69, 784–793. N ARBONNE , G.
An example of the conversion of a 2D image to 1D profiles of Fe abundance in a cap carbonate from the Rasthof Formation in Namibia. (a) Fe image acquired by SXAM. 1 mm/pixel. The black lines plotted on the image are the isochronous lines calculated by the lamination tracer. Note that the isochronous lines trace the original lamination of the cap carbonate very well; (b) Fe profile (black line) obtained by averaging (a) simply in the horizontal direction and its standard deviation (grey line); (c) Fe profile (black line) obtained by the measurement along the line marked by the narrow rectangle in (a) and its standard deviation (grey line); (d) Fe profile (black line) averaged along the isochronous lines and its standard deviation (grey line).