Image of the watery surface of a churning ocean

Photo by Matt Hardy on Unsplash

Image of the Earth from space

A nearly perfect sphere • NASA/Apollo 17 (Public Domain)

Escaping the human scale

When I was a child I owned a pic­ture book that told the sto­ry of Christo­pher Colum­bus. Sev­er­al of the illus­tra­tions are still clear in my mem­o­ry. One showed Span­ish car­avels, with pen­nants fly­ing, sail­ing off the edge of a flat Earth into the mouth of a wait­ing mon­ster. This sup­pos­ed­ly illus­trat­ed the pre­vail­ing view of the shape of the Earth at the time of Columbus.

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.

Image of the sealed Kola borehole

The sealed and abandoned Kola Superdeep Borehole in 2012 • Photo by Rakot13 (CC BY SA 3.0)

Photo of the Aurora Borealis

Photo by Vincent Guth on Unsplash

Artist's impression of a protoplanetary disc

Artist's impression of a protoplanetary disc • ESO/L. Calçada (CC BY 4.0)

The sands of time

The ingre­di­ents of life on Earth were col­lect­ed by grav­i­ty. The hearth that held the tin­der and received the spark of life was a small heavy-ele­ment plan­et near a yel­low star. Chem­istry was the steel and time the flint that struck the spark. For the spark to catch and the flame to grow required not bib­li­cal days, but hun­dreds of mil­lions of years. The solar sys­tem has been around for four and a half bil­lion years. That’s time enough for miracles.