Image of cross-bedded rocks

Example of cross-bedding in Nova Scotia • Michael C. Rygel (CC BY SA 3.0)

Reading the rocks

In his book Con­ver­sa­tions with the Earth, Ger­man geol­o­gist Hans Cloos described the moment when he “became a geol­o­gist for­ev­er.” It did not hap­pen at uni­ver­si­ty. It did not hap­pen with the pass­ing of an exam or the award­ing of a degree. It hap­pened one morn­ing in Naples, Italy, when Cloos opened the win­dow of his hotel room and saw the smok­ing cone of Vesu­vius loom­ing above the still-sleep­ing city. At that moment he had the real­iza­tion that moti­vat­ed a life­time of cre­ative work in geol­o­gy: The Earth is alive.

Image of the Earth from space

The Hawaiian Islands • eol.jsc.nasa.gov (Public Domain)

CAT scanning Earth

In geol­o­gy, before the 1960s, we were taught the Earth was “as sol­id as a rock.” And we were told the sur­face of the Earth had always looked more or less the way it looks today, the same con­ti­nents, the same ocean basins. Oh yes, there had been changes on the sur­face, crin­klings and fold­ings that lift­ed moun­tains or cracked the crust, ver­ti­cal move­ments most­ly, like the wrin­kles on the skin of an orange.